{"pageNumber":"1449","pageRowStart":"36200","pageSize":"25","recordCount":184717,"records":[{"id":70059292,"text":"70059292 - 2013 - PCB concentrations and activity of sea lamprey Petromyzon marinus vary by sex","interactions":[],"lastModifiedDate":"2013-12-20T14:00:06","indexId":"70059292","displayToPublicDate":"2013-12-19T13:48:44","publicationYear":"2013","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":887,"text":"Archives of Environmental Contamination and Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"PCB concentrations and activity of sea lamprey Petromyzon marinus vary by sex","docAbstract":"We determined the polychlorinated biphenyl (PCB) concentrations of 40 male and 40 female adult sea lampreys Petromyzon marinus captured in the Cheboygan River, a tributary to Lake Huron, during May 2011. In addition, we performed a laboratory experiment using passive integrated transponder tags to determine whether male adult sea lampreys were more active than female adult sea lampreys. Sex had a significant effect on PCB concentration, and PCB concentration at a given level of sea lamprey condition was approximately 25 % greater in males than in females. Adjusting for the difference in condition between the sexes, males averaged a 17 % greater PCB concentration compared with females. Results from the laboratory experiment indicated that males were significantly more active than females. The observed sex difference in PCB concentrations was not due to female sea lampreys releasing eggs at spawning because the sea lamprey is semelparous, and we caught the sea lampreys before spawning. Rather, we attributed the sex difference in PCB concentrations to a greater rate of energy expenditure in males compared with females. We proposed that this greater rate of energy expenditure was likely due to greater activity. Our laboratory experiment results supported this hypothesis. A greater resting metabolic rate may also have contributed to a greater rate of energy expenditure. Our findings should eventually be applicable toward improving control of sea lamprey, a pest responsible for considerable damage to fisheries in lakes where it is not native.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Archives of Environmental Contamination and Toxicology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer","doi":"10.1007/s00244-013-9936-y","usgsCitation":"Madenjian, C.P., Johnson, N.S., Binder, T., Rediske, R.R., and O'Keefe, J., 2013, PCB concentrations and activity of sea lamprey Petromyzon marinus vary by sex: Archives of Environmental Contamination and Toxicology, v. 65, no. 4, p. 693-703, https://doi.org/10.1007/s00244-013-9936-y.","productDescription":"11 p.","startPage":"693","endPage":"703","ipdsId":"IP-049146","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":280484,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":280483,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s00244-013-9936-y"}],"country":"United States","state":"Michigan","otherGeospatial":"Cheboygan River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.4804,45.6375 ], [ -84.4804,45.6558 ], [ -84.4651,45.6558 ], [ -84.4651,45.6375 ], [ -84.4804,45.6375 ] ] ] } } ] }","volume":"65","issue":"4","noUsgsAuthors":false,"publicationDate":"2013-07-18","publicationStatus":"PW","scienceBaseUri":"53cd6a69e4b0b290851033a3","contributors":{"authors":[{"text":"Madenjian, Charles P. 0000-0002-0326-164X cmadenjian@usgs.gov","orcid":"https://orcid.org/0000-0002-0326-164X","contributorId":2200,"corporation":false,"usgs":true,"family":"Madenjian","given":"Charles","email":"cmadenjian@usgs.gov","middleInitial":"P.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":487657,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Nicholas S. 0000-0002-7419-6013 njohnson@usgs.gov","orcid":"https://orcid.org/0000-0002-7419-6013","contributorId":597,"corporation":false,"usgs":true,"family":"Johnson","given":"Nicholas","email":"njohnson@usgs.gov","middleInitial":"S.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":487656,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Binder, Thomas R.","contributorId":23056,"corporation":false,"usgs":false,"family":"Binder","given":"Thomas R.","affiliations":[{"id":7019,"text":"Great Lakes Fishery Commission","active":true,"usgs":false}],"preferred":false,"id":487658,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rediske, Richard R.","contributorId":79053,"corporation":false,"usgs":true,"family":"Rediske","given":"Richard","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":487659,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"O'Keefe, James P.","contributorId":99499,"corporation":false,"usgs":true,"family":"O'Keefe","given":"James P.","affiliations":[],"preferred":false,"id":487660,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70059278,"text":"70059278 - 2013 - Performance of human fecal anaerobe-associated PCR-based assays in a multi-laboratory method evaluation study","interactions":[],"lastModifiedDate":"2013-12-20T13:07:35","indexId":"70059278","displayToPublicDate":"2013-12-19T11:52:31","publicationYear":"2013","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3716,"text":"Water Research","onlineIssn":"1879-2448","printIssn":"0043-1354","active":true,"publicationSubtype":{"id":10}},"title":"Performance of human fecal anaerobe-associated PCR-based assays in a multi-laboratory method evaluation study","docAbstract":"A number of PCR-based methods for detecting human fecal material in environmental waters have been developed over the past decade, but these methods have rarely received independent comparative testing in large multi-laboratory studies. Here, we evaluated ten of these methods (BacH, BacHum-UCD, Bacteroides thetaiotaomicron (BtH), BsteriF1, gyrB, HF183 endpoint, HF183 SYBR, HF183 Taqman®, HumM2, and Methanobrevibacter smithii nifH (Mnif)) using 64 blind samples prepared in one laboratory. The blind samples contained either one or two fecal sources from human, wastewater or non-human sources. The assay results were assessed for presence/absence of the human markers and also quantitatively while varying the following: 1) classification of samples that were detected but not quantifiable (DNQ) as positive or negative; 2) reference fecal sample concentration unit of measure (such as culturable indicator bacteria, wet mass, total DNA, etc); and 3) human fecal source type (stool, sewage or septage). Assay performance using presence/absence metrics was found to depend on the classification of DNQ samples. The assays that performed best quantitatively varied based on the fecal concentration unit of measure and laboratory protocol. All methods were consistently more sensitive to human stools compared to sewage or septage in both the presence/absence and quantitative analysis. Overall, HF183 Taqman® was found to be the most effective marker of human fecal contamination in this California-based study.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Water Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"ScienceDirect","doi":"10.1016/j.watres.2013.05.060","usgsCitation":"Layton, B.A., Cao, Y., Ebentier, D.L., Hanley, K., Balleste, E., Brandao, J., Byappanahalli, M., Converse, R., Farnleitner, A.H., Gentry-Shields, J.G., Gourmelon, M., Lee, C.S., Lee, J., Lozach, S., Madi, T., Meijer, W.G., Noble, R., Peed, L., Reischer, G.H., Rodrigues, R., Rose, J.B., Schriewer, A., Sinigalliano, C., Srinivasan, S., Stewart, J., Van De Werfhorst, Laurie, C., Wang, D., Whitman, R., Wuertz, S., Jay, J., Holden, P.A., Boehm, A., Shanks, O., and Griffith, J.F., 2013, Performance of human fecal anaerobe-associated PCR-based assays in a multi-laboratory method evaluation study: Water Research, v. 47, no. 18, p. 6897-6908, https://doi.org/10.1016/j.watres.2013.05.060.","productDescription":"12 p.","startPage":"6897","endPage":"6908","ipdsId":"IP-044795","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":280471,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":280470,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.watres.2013.05.060"}],"volume":"47","issue":"18","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd6ad1e4b0b29085103818","contributors":{"authors":[{"text":"Layton, Blythe A.","contributorId":20644,"corporation":false,"usgs":true,"family":"Layton","given":"Blythe","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":487569,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cao, Yiping","contributorId":37633,"corporation":false,"usgs":true,"family":"Cao","given":"Yiping","affiliations":[],"preferred":false,"id":487575,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ebentier, Darcy L.","contributorId":13524,"corporation":false,"usgs":true,"family":"Ebentier","given":"Darcy","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":487567,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hanley, Kaitlyn","contributorId":97416,"corporation":false,"usgs":true,"family":"Hanley","given":"Kaitlyn","affiliations":[],"preferred":false,"id":487599,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Balleste, Elisenda","contributorId":96580,"corporation":false,"usgs":true,"family":"Balleste","given":"Elisenda","email":"","affiliations":[],"preferred":false,"id":487598,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Brandao, Joao","contributorId":59716,"corporation":false,"usgs":true,"family":"Brandao","given":"Joao","email":"","affiliations":[],"preferred":false,"id":487585,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Byappanahalli, Muruleedhara N.","contributorId":47335,"corporation":false,"usgs":true,"family":"Byappanahalli","given":"Muruleedhara N.","affiliations":[],"preferred":false,"id":487578,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Converse, Reagan","contributorId":26617,"corporation":false,"usgs":true,"family":"Converse","given":"Reagan","email":"","affiliations":[],"preferred":false,"id":487573,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Farnleitner, Andreas H.","contributorId":23430,"corporation":false,"usgs":true,"family":"Farnleitner","given":"Andreas","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":487571,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Gentry-Shields, Jennifer Gidley Gidley, Maribeth L.","contributorId":45218,"corporation":false,"usgs":true,"family":"Gentry-Shields","given":"Jennifer","suffix":"Gidley, Maribeth L.","email":"","middleInitial":"Gidley","affiliations":[],"preferred":false,"id":487577,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Gourmelon, Michele","contributorId":17128,"corporation":false,"usgs":true,"family":"Gourmelon","given":"Michele","email":"","affiliations":[],"preferred":false,"id":487568,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Lee, Chang Soo","contributorId":64988,"corporation":false,"usgs":true,"family":"Lee","given":"Chang","email":"","middleInitial":"Soo","affiliations":[],"preferred":false,"id":487587,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Lee, Jiyoung","contributorId":67401,"corporation":false,"usgs":true,"family":"Lee","given":"Jiyoung","email":"","affiliations":[],"preferred":false,"id":487590,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Lozach, Solen","contributorId":48086,"corporation":false,"usgs":true,"family":"Lozach","given":"Solen","email":"","affiliations":[],"preferred":false,"id":487579,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Madi, Tania","contributorId":95379,"corporation":false,"usgs":true,"family":"Madi","given":"Tania","email":"","affiliations":[],"preferred":false,"id":487597,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Meijer, Wim G.","contributorId":67001,"corporation":false,"usgs":true,"family":"Meijer","given":"Wim","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":487589,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Noble, 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B.","contributorId":81791,"corporation":false,"usgs":true,"family":"Rose","given":"Joan","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":487594,"contributorType":{"id":1,"text":"Authors"},"rank":21},{"text":"Schriewer, Alexander","contributorId":34420,"corporation":false,"usgs":true,"family":"Schriewer","given":"Alexander","email":"","affiliations":[],"preferred":false,"id":487574,"contributorType":{"id":1,"text":"Authors"},"rank":22},{"text":"Sinigalliano, Chris","contributorId":54877,"corporation":false,"usgs":true,"family":"Sinigalliano","given":"Chris","email":"","affiliations":[],"preferred":false,"id":487583,"contributorType":{"id":1,"text":"Authors"},"rank":23},{"text":"Srinivasan, Sangeetha","contributorId":21451,"corporation":false,"usgs":true,"family":"Srinivasan","given":"Sangeetha","email":"","affiliations":[],"preferred":false,"id":487570,"contributorType":{"id":1,"text":"Authors"},"rank":24},{"text":"Stewart, Jill","contributorId":9951,"corporation":false,"usgs":true,"family":"Stewart","given":"Jill","affiliations":[],"preferred":false,"id":487566,"contributorType":{"id":1,"text":"Authors"},"rank":25},{"text":"Van De Werfhorst","contributorId":128045,"corporation":true,"usgs":false,"organization":"Van De Werfhorst","id":535614,"contributorType":{"id":1,"text":"Authors"},"rank":26},{"text":"Laurie, C.","contributorId":69466,"corporation":false,"usgs":true,"family":"Laurie","given":"C.","email":"","affiliations":[],"preferred":false,"id":487592,"contributorType":{"id":1,"text":"Authors"},"rank":27},{"text":"Wang, Dan","contributorId":88644,"corporation":false,"usgs":true,"family":"Wang","given":"Dan","affiliations":[],"preferred":false,"id":487596,"contributorType":{"id":1,"text":"Authors"},"rank":28},{"text":"Whitman, Richard","contributorId":100811,"corporation":false,"usgs":true,"family":"Whitman","given":"Richard","affiliations":[],"preferred":false,"id":487600,"contributorType":{"id":1,"text":"Authors"},"rank":29},{"text":"Wuertz, Stefan","contributorId":64549,"corporation":false,"usgs":true,"family":"Wuertz","given":"Stefan","email":"","affiliations":[],"preferred":false,"id":487586,"contributorType":{"id":1,"text":"Authors"},"rank":30},{"text":"Jay, Jenny","contributorId":25858,"corporation":false,"usgs":true,"family":"Jay","given":"Jenny","email":"","affiliations":[],"preferred":false,"id":487572,"contributorType":{"id":1,"text":"Authors"},"rank":31},{"text":"Holden, Patricia A.","contributorId":56090,"corporation":false,"usgs":true,"family":"Holden","given":"Patricia","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":487584,"contributorType":{"id":1,"text":"Authors"},"rank":32},{"text":"Boehm, Alexandria B.","contributorId":51616,"corporation":false,"usgs":true,"family":"Boehm","given":"Alexandria B.","affiliations":[],"preferred":false,"id":487581,"contributorType":{"id":1,"text":"Authors"},"rank":33},{"text":"Shanks, Orin","contributorId":67794,"corporation":false,"usgs":true,"family":"Shanks","given":"Orin","affiliations":[],"preferred":false,"id":487591,"contributorType":{"id":1,"text":"Authors"},"rank":34},{"text":"Griffith, John F.","contributorId":41325,"corporation":false,"usgs":true,"family":"Griffith","given":"John","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":487576,"contributorType":{"id":1,"text":"Authors"},"rank":35}]}}
,{"id":70049014,"text":"fs20133109 - 2013 - Real-time continuous nitrate monitoring in Illinois in 2013","interactions":[],"lastModifiedDate":"2013-12-19T11:47:58","indexId":"fs20133109","displayToPublicDate":"2013-12-19T11:39:00","publicationYear":"2013","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2013-3109","title":"Real-time continuous nitrate monitoring in Illinois in 2013","docAbstract":"Many sources contribute to the nitrogen found in surface water in Illinois. Illinois is located in the most productive agricultural area in the country, and nitrogen fertilizer is commonly used to maximize corn production in this area. Additionally, septic/wastewater systems, industrial emissions, and lawn fertilizer are common sources of nitrogen in urban areas of Illinois. In agricultural areas, the use of fertilizer has increased grain production to meet the needs of a growing population, but also has resulted in increases in nitrogen concentrations in many streams and aquifers (Dubrovsky and others, 2010). The urban sources can increase nitrogen concentrations, too. The Federal limit for nitrate nitrogen in water that is safe to drink is 10 milligrams per liter (mg/L) (http://water.epa.gov/drink/contaminants/basicinformation/nitrate.cfm, accessed on May 24, 2013). In addition to the concern with nitrate nitrogen in drinking water, nitrogen, along with phosphorus, is an aquatic concern because it feeds the intensive growth of algae that are responsible for the hypoxic zone in the Gulf of Mexico. The largest nitrogen flux to the waters feeding the Gulf of Mexico is from Illinois (Alexander and others, 2008). Most studies of nitrogen in surface water and groundwater include samples for nitrate nitrogen collected weekly or monthly, but nitrate concentrations can change rapidly and these discrete samples may not capture rapid changes in nitrate concentrations that can affect human and aquatic health. Continuous monitoring for nitrate could inform scientists and water-resource managers of these changes and provide information on the transport of nitrate in surface water and groundwater.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20133109","usgsCitation":"Warner, K., Terrio, P.J., Straub, T., Roseboom, D., and Johnson, G.P., 2013, Real-time continuous nitrate monitoring in Illinois in 2013: U.S. Geological Survey Fact Sheet 2013-3109, 3 p., https://doi.org/10.3133/fs20133109.","productDescription":"3 p.","ipdsId":"IP-045559","costCenters":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"links":[{"id":280431,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs20133109.jpg"},{"id":280429,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2013/3109/pdf/fs2013-3109.pdf"},{"id":280430,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2013/3109/"}],"country":"United States","state":"Illinois","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -91.51,36.97 ], [ -91.51,42.51 ], [ -87.5,42.51 ], [ -87.5,36.97 ], [ -91.51,36.97 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52b41581e4b029a4958c9d20","contributors":{"authors":[{"text":"Warner, Kelly L. klwarner@usgs.gov","contributorId":655,"corporation":false,"usgs":true,"family":"Warner","given":"Kelly L.","email":"klwarner@usgs.gov","affiliations":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"preferred":true,"id":486024,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Terrio, Paul J. 0000-0002-1515-9570 pjterrio@usgs.gov","orcid":"https://orcid.org/0000-0002-1515-9570","contributorId":3313,"corporation":false,"usgs":true,"family":"Terrio","given":"Paul","email":"pjterrio@usgs.gov","middleInitial":"J.","affiliations":[{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":486027,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Straub, Timothy D. 0000-0002-5896-0851 tdstraub@usgs.gov","orcid":"https://orcid.org/0000-0002-5896-0851","contributorId":2273,"corporation":false,"usgs":true,"family":"Straub","given":"Timothy D.","email":"tdstraub@usgs.gov","affiliations":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"preferred":false,"id":486025,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Roseboom, Donald roseboom@usgs.gov","contributorId":3974,"corporation":false,"usgs":true,"family":"Roseboom","given":"Donald","email":"roseboom@usgs.gov","affiliations":[],"preferred":true,"id":486028,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Johnson, Gary P. 0000-0003-0363-9873 gjohnson@usgs.gov","orcid":"https://orcid.org/0000-0003-0363-9873","contributorId":2959,"corporation":false,"usgs":true,"family":"Johnson","given":"Gary","email":"gjohnson@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":486026,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70059277,"text":"70059277 - 2013 - Shallow groundwater and soil chemistry response to 3 years of subsurface drip irrigation using coalbed-methane-produced water","interactions":[],"lastModifiedDate":"2013-12-20T11:33:09","indexId":"70059277","displayToPublicDate":"2013-12-19T11:28:29","publicationYear":"2013","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1923,"text":"Hydrogeology Journal","active":true,"publicationSubtype":{"id":10}},"title":"Shallow groundwater and soil chemistry response to 3 years of subsurface drip irrigation using coalbed-methane-produced water","docAbstract":"Disposal of produced waters, pumped to the surface as part of coalbed methane (CBM) development, is a significant environmental issue in the Wyoming portion of the Powder River Basin, USA. High sodium adsorption ratios (SAR) of the waters could degrade agricultural land, especially if directly applied to the soil surface. One method of disposing of CBM water, while deriving beneficial use, is subsurface drip irrigation (SDI), where acidified CBM waters are applied to alfalfa fields year-round via tubing buried 0.92 m deep. Effects of the method were studied on an alluvial terrace with a relatively shallow depth to water table (∼3 m). Excess irrigation water caused the water table to rise, even temporarily reaching the depth of drip tubing. The rise corresponded to increased salinity in some monitoring wells. Three factors appeared to drive increased groundwater salinity: (1) CBM solutes, concentrated by evapotranspiration; (2) gypsum dissolution, apparently enhanced by cation exchange; and (3) dissolution of native Na–Mg–SO<sub>4</sub> salts more soluble than gypsum. Irrigation with high SAR (∼24) water has increased soil saturated paste SAR up to 15 near the drip tubing. Importantly though, little change in SAR has occurred at the surface.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Hydrogeology Journal","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer","doi":"10.1007/s10040-013-1058-0","usgsCitation":"Bern, C., Boehlke, A., Engle, M.A., Geboy, N., Schroeder, K., and Zupancic, J., 2013, Shallow groundwater and soil chemistry response to 3 years of subsurface drip irrigation using coalbed-methane-produced water: Hydrogeology Journal, v. 21, no. 8, p. 1803-1820, https://doi.org/10.1007/s10040-013-1058-0.","productDescription":"18 p.","startPage":"1803","endPage":"1820","ipdsId":"IP-041437","costCenters":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":280469,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":280455,"type":{"id":15,"text":"Index Page"},"url":"https://link.springer.com/article/10.1007/s10040-013-1058-0"},{"id":280454,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s10040-013-1058-0"}],"country":"United States","state":"Wyoming","county":"Johnson","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -107.372,43.4937 ], [ -107.372,44.5653 ], [ -106.0076,44.5653 ], [ -106.0076,43.4937 ], [ -107.372,43.4937 ] ] ] } } ] }","volume":"21","issue":"8","noUsgsAuthors":false,"publicationDate":"2013-10-04","publicationStatus":"PW","scienceBaseUri":"53cd7295e4b0b2908510865d","contributors":{"authors":[{"text":"Bern, Carleton R.","contributorId":59325,"corporation":false,"usgs":true,"family":"Bern","given":"Carleton R.","affiliations":[],"preferred":false,"id":487564,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boehlke, Adam R. 0000-0003-4980-431X","orcid":"https://orcid.org/0000-0003-4980-431X","contributorId":23835,"corporation":false,"usgs":true,"family":"Boehlke","given":"Adam R.","affiliations":[],"preferred":false,"id":487562,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Engle, Mark A. 0000-0001-5258-7374 engle@usgs.gov","orcid":"https://orcid.org/0000-0001-5258-7374","contributorId":584,"corporation":false,"usgs":true,"family":"Engle","given":"Mark","email":"engle@usgs.gov","middleInitial":"A.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":487560,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Geboy, Nicholas J. ngeboy@usgs.gov","contributorId":3860,"corporation":false,"usgs":true,"family":"Geboy","given":"Nicholas J.","email":"ngeboy@usgs.gov","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":487561,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schroeder, K.T.","contributorId":102113,"corporation":false,"usgs":true,"family":"Schroeder","given":"K.T.","email":"","affiliations":[],"preferred":false,"id":487565,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Zupancic, J.W.","contributorId":42808,"corporation":false,"usgs":true,"family":"Zupancic","given":"J.W.","affiliations":[],"preferred":false,"id":487563,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70059285,"text":"70059285 - 2013 - Spatial and temporal genetic diversity of lake whitefish (Coregonus clupeaformis (Mitchill)) from Lake Huron and Lake Erie","interactions":[],"lastModifiedDate":"2021-01-05T14:53:31.566917","indexId":"70059285","displayToPublicDate":"2013-12-19T11:14:05","publicationYear":"2013","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":656,"text":"Advances in Limnology","active":true,"publicationSubtype":{"id":10}},"title":"Spatial and temporal genetic diversity of lake whitefish (Coregonus clupeaformis (Mitchill)) from Lake Huron and Lake Erie","docAbstract":"Lake whitefish (Coregonus clupeaformis (Mitchill)) are important commercially, culturally, and ecologically in the Laurentian Great Lakes. Stocks of lake whitefish in the Great Lakes have recovered from low levels of abundance in the 1960s. Reductions in abundance, loss of habitat and environmental degradation can be accompanied by losses of genetic diversity and overall fitness that may persist even as populations recover demographically. Therefore, it is important to be able to identify stocks that have reduced levels of genetic diversity. In this study, we investigated patterns of genetic diversity at microsatellite DNA loci in lake whitefish collected between 1927 and 1929 (historical period) and between 1997 and 2005 (contemporary period) from Lake Huron and Lake Erie. Genetic analysis of lake whitefish from Lakes Huron and Erie shows that the amount of population structuring varies from lake to lake. Greater genetic divergences among collections from Lake Huron may be the result of sampling scale, migration patterns and demographic processes. Fluctuations in abundance of lake whitefish populations may have resulted in periods of increased genetic drift that have resulted in changes in allele frequencies over time, but periodic genetic drift was not severe enough to result in a significant loss of genetic diversity. Migration among stocks may have decreased levels of genetic differentiation while not completely obscuring stock boundaries. Recent changes in spatial boundaries to stocks, the number of stocks and life history characteristics of stocks further demonstrate the potential of coregonids for a swift and varied response to environmental change and emphasise the importance of incorporating both spatial and temporal considerations into management plans to ensure that diversity is preserved.","language":"English","publisher":"Schweizerbart Science Publishers","doi":"10.1127/1612-166X/2013/0064-0015","usgsCitation":"Stott, W., Ebener, M.P., Mohr, L., Hartman, T., Johnson, J., and Roseman, E., 2013, Spatial and temporal genetic diversity of lake whitefish (Coregonus clupeaformis (Mitchill)) from Lake Huron and Lake Erie: Advances in Limnology, v. 64, p. 205-222, https://doi.org/10.1127/1612-166X/2013/0064-0015.","productDescription":"18 p.","startPage":"205","endPage":"222","ipdsId":"IP-038640","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":280468,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Lake Erie, Lake Huron","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.93,41.38 ], [ -84.93,46.38 ], [ -78.85,46.38 ], [ -78.85,41.38 ], [ -84.93,41.38 ] ] ] } } ] }","volume":"64","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd737be4b0b29085108fc5","contributors":{"authors":[{"text":"Stott, Wendylee","contributorId":8058,"corporation":false,"usgs":true,"family":"Stott","given":"Wendylee","affiliations":[],"preferred":false,"id":487645,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ebener, Mark P.","contributorId":25099,"corporation":false,"usgs":false,"family":"Ebener","given":"Mark","email":"","middleInitial":"P.","affiliations":[{"id":12957,"text":"Chippewa Ottawa Resource Authority","active":true,"usgs":false}],"preferred":false,"id":487646,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mohr, Lloyd","contributorId":34001,"corporation":false,"usgs":true,"family":"Mohr","given":"Lloyd","affiliations":[],"preferred":false,"id":487647,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hartman, Travis","contributorId":66583,"corporation":false,"usgs":true,"family":"Hartman","given":"Travis","affiliations":[],"preferred":false,"id":487649,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Johnson, Jim","contributorId":54500,"corporation":false,"usgs":true,"family":"Johnson","given":"Jim","email":"","affiliations":[],"preferred":false,"id":487648,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Roseman, Edward F.","contributorId":100334,"corporation":false,"usgs":true,"family":"Roseman","given":"Edward F.","affiliations":[],"preferred":false,"id":487650,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70059283,"text":"70059283 - 2013 - Morphometric variation among spawning cisco aggregations in the Laurentian Great Lakes: are historic forms still present?","interactions":[],"lastModifiedDate":"2013-12-20T11:11:24","indexId":"70059283","displayToPublicDate":"2013-12-19T10:58:48","publicationYear":"2013","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":656,"text":"Advances in Limnology","active":true,"publicationSubtype":{"id":10}},"title":"Morphometric variation among spawning cisco aggregations in the Laurentian Great Lakes: are historic forms still present?","docAbstract":"Cisco (Coregonus artedi Leseur, formerly lake herring Leucichthys artedi Leseur) populations in each of the Laurentian Great Lakes collapsed between the late 1920s and early 1960s following a multitude of stressors, and never recovered in Lakes Michigan, Erie and Ontario. Prior to their collapse, Koelz (1929) studied Leucichthys spp. in the Great Lakes basin and provided a description of their diversity. Three cisco morphotypes were described; a ‘slim terete’morphotype (L. artedi artedi), a ‘deep compressed’ morphotype (L. artedi albus), and a deep-bodied form resembling tullibee in western Canadian lakes (L. artedi manitoulinus). Based on body measurements of 159 individuals (Koelz 1929), we used discriminant function analysis (DFA) to discriminate historic morphotypes. Shapes of historic morphotypes were found to vary significantly (Pillai’s trace = 1.16, P < 0.0001). The final DFA model used nine body measurements and correctly classified 90% of the historic cisco. Important discriminating measurements included body depth, eye diameter, and dorsal fin base and height. Between October-November of 2007-2011, we sampled cisco from 16 Great Lakes sites collecting digital photographs of over 1, 700 individuals. We applied the DFA model to their body measurements and classified each individual to a morphotype. Contemporary cisco from Lakes Superior, Ontario and Michigan were predominantly classified as artedi, while the most common classifications from northern Lake Huron were albus and manitoulinus. Finding historic morphotypes is encouraging because it suggests that the morphological variation present prior to their collapse still exists. We conclude that contemporary cisco having shapes matching the missing historic morphotypes in the lower lakes warrant special consideration as potential donor populations in reestablishment efforts.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Advances in Limnology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Schweizerbart Science Publishers","doi":"10.1127/1612-166X/2013/0064-0022","usgsCitation":"Yule, D., Moore, S.A., Ebener, M.P., Claramunt, R., Pratt, T., Salawater, L.L., and Connerton, M., 2013, Morphometric variation among spawning cisco aggregations in the Laurentian Great Lakes: are historic forms still present?: Advances in Limnology, v. 64, p. 119-132, https://doi.org/10.1127/1612-166X/2013/0064-0022.","productDescription":"14 p.","startPage":"119","endPage":"132","ipdsId":"IP-038761","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":280463,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":280462,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1127/1612-166X/2013/0064-0022"}],"country":"United States","otherGeospatial":"Lake Michigan;Lake Erie;Lake Ontario;Lake Huron;Lake Superior","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -92.11,41.38 ], [ -92.11,48.85 ], [ -76.3,48.85 ], [ -76.3,41.38 ], [ -92.11,41.38 ] ] ] } } ] }","volume":"64","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd6837e4b0b29085101e4e","contributors":{"authors":[{"text":"Yule, Daniel L.","contributorId":92130,"corporation":false,"usgs":true,"family":"Yule","given":"Daniel L.","affiliations":[],"preferred":false,"id":487644,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, Seth A.","contributorId":32490,"corporation":false,"usgs":true,"family":"Moore","given":"Seth","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":487643,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ebener, Mark P.","contributorId":25099,"corporation":false,"usgs":false,"family":"Ebener","given":"Mark","email":"","middleInitial":"P.","affiliations":[{"id":12957,"text":"Chippewa Ottawa Resource Authority","active":true,"usgs":false}],"preferred":false,"id":487641,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Claramunt, Randall M.","contributorId":19047,"corporation":false,"usgs":true,"family":"Claramunt","given":"Randall M.","affiliations":[],"preferred":false,"id":487638,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pratt, Thomas C.","contributorId":24672,"corporation":false,"usgs":true,"family":"Pratt","given":"Thomas C.","affiliations":[],"preferred":false,"id":487640,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Salawater, Lorrie L.","contributorId":31298,"corporation":false,"usgs":true,"family":"Salawater","given":"Lorrie","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":487642,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Connerton, Michael J.","contributorId":21435,"corporation":false,"usgs":true,"family":"Connerton","given":"Michael J.","affiliations":[],"preferred":false,"id":487639,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70059281,"text":"70059281 - 2013 - Trophic shift, not collapse","interactions":[],"lastModifiedDate":"2013-12-20T10:50:46","indexId":"70059281","displayToPublicDate":"2013-12-19T10:46:38","publicationYear":"2013","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Trophic shift, not collapse","docAbstract":"Jerald Schnoor’s editorial describes the recent changes in Lake Huron’s aquatic ecosystem as a trophic collapse and attributes this collapse to invasive species dominating energy and nutrient flows in the food web. As state and federal\nscientists who are closely monitoring Lake Huron’s food web, we believe that the ongoing changes are more accurately characterized as a trophic shift in which benthic pathways have become more prominent. While decreases in abundance have occurred for some species, others are experiencing improved reproduction resulting in the restoration of several important native species.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Science and Technology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"ACS Publications","doi":"10.1021/es404089y","usgsCitation":"Madenjian, C.P., Rutherford, E.S., Stow, C., Roseman, E., and He, J.X., 2013, Trophic shift, not collapse: Environmental Science & Technology, v. 47, no. 21, p. 11915-11916, https://doi.org/10.1021/es404089y.","productDescription":"2 p.","startPage":"11915","endPage":"11916","ipdsId":"IP-051398","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":280461,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":280460,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es404089y"}],"volume":"47","issue":"21","noUsgsAuthors":false,"publicationDate":"2013-10-15","publicationStatus":"PW","scienceBaseUri":"53cd79b4e4b0b2908510d025","contributors":{"authors":[{"text":"Madenjian, Charles P. 0000-0002-0326-164X cmadenjian@usgs.gov","orcid":"https://orcid.org/0000-0002-0326-164X","contributorId":2200,"corporation":false,"usgs":true,"family":"Madenjian","given":"Charles","email":"cmadenjian@usgs.gov","middleInitial":"P.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":487633,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rutherford, Edward S.","contributorId":54161,"corporation":false,"usgs":true,"family":"Rutherford","given":"Edward","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":487636,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stow, Craig A.","contributorId":49733,"corporation":false,"usgs":true,"family":"Stow","given":"Craig A.","affiliations":[],"preferred":false,"id":487634,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Roseman, Edward F.","contributorId":100334,"corporation":false,"usgs":true,"family":"Roseman","given":"Edward F.","affiliations":[],"preferred":false,"id":487637,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"He, Ji X.","contributorId":53254,"corporation":false,"usgs":true,"family":"He","given":"Ji","email":"","middleInitial":"X.","affiliations":[],"preferred":false,"id":487635,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70059177,"text":"70059177 - 2013 - Analysis of H<sub>2</sub>O in silicate glass using attenuated total reflectance (ATR) micro-FTIR spectroscopy","interactions":[],"lastModifiedDate":"2013-12-19T09:30:27","indexId":"70059177","displayToPublicDate":"2013-12-19T09:17:00","publicationYear":"2013","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":738,"text":"American Mineralogist","active":true,"publicationSubtype":{"id":10}},"title":"Analysis of H<sub>2</sub>O in silicate glass using attenuated total reflectance (ATR) micro-FTIR spectroscopy","docAbstract":"We present a calibration for attenuated total reflectance (ATR) micro-FTIR for analysis of H2O in hydrous glass. A Ge ATR accessory was used to measure evanescent wave absorption by H<sub>2</sub>O within hydrous rhyolite and other standards. Absorbance at 3450 cm<sup>−1</sup> (representing total H<sub>2</sub>O or H<sub>2</sub>O<sub>t</sub>) and 1630 cm<sup>−1</sup> (molecular H<sub>2</sub>O or H<sub>2</sub>O<sub>m</sub>) showed high correlation with measured H<sub>2</sub>O in the glasses as determined by transmission FTIR spectroscopy and manometry. For rhyolite,\n\nwt%H<sub>2</sub>O=245(&plusmn;9)&times;A<sub>3450</sub>-0.22(&plusmn;0.03)\n\nand\n\nwt%H<sub>2</sub>O<sub>m</sub>=235(&plusmn;11)&times;A<sub>1630</sub>-0.20(&plusmn;0.03)\n\nwhere A<sub>3450</sub> and A<sub>1630</sub> represent the ATR absorption at the relevant infrared wavelengths. The calibration permits determination of volatiles in singly polished glass samples with spot size down to ~5 μm (for H<sub>2</sub>O-rich samples) and detection limits of ~0.1 wt% H<sub>2</sub>O. Basaltic, basaltic andesite and dacitic glasses of known H<sub>2</sub>O concentrations fall along a density-adjusted calibration, indicating that ATR is relatively insensitive to glass composition, at least for calc-alkaline glasses. The following equation allows quantification of H<sub>2</sub>O in silicate glasses that range in composition from basalt to rhyolite:\n\nwt%H<sub>2</sub>O=(ω&times;A<sub>3450</sub>/ρ)+<i>b</i>\n\nwhere ω = 550 ± 21, b = −0.19 ± 0.03, ρ = density, in g/cm<sup>3</sup>, and A<sub>3450</sub> is the ATR absorbance at 3450 cm<sup>−1</sup>.\n\nThe ATR micro-FTIR technique is less sensitive than transmission FTIR, but requires only a singly polished sample for quantitative results, thus minimizing time for sample preparation. Compared with specular reflectance, it is more sensitive and better suited for imaging of H<sub>2</sub>O variations in heterogeneous samples such as melt inclusions. One drawback is that the technique can damage fragile samples and we therefore recommend mounting of unknowns in epoxy prior to polishing. Our calibration should hold for any Ge ATR crystals with the same incident angle (31°). Use of a different crystal type or geometry would require measurement of several H<sub>2</sub>O-bearing standards to provide a crystal-specific calibration.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Mineralogist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Mineralogical Society of America","doi":"10.2138/am.2013.4466","usgsCitation":"Lowenstern, J.B., and Pitcher, B.W., 2013, Analysis of H<sub>2</sub>O in silicate glass using attenuated total reflectance (ATR) micro-FTIR spectroscopy: American Mineralogist, v. 98, no. 10, p. 1660-1668, https://doi.org/10.2138/am.2013.4466.","productDescription":"9 p.","startPage":"1660","endPage":"1668","numberOfPages":"9","ipdsId":"IP-045223","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":280426,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":280425,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2138/am.2013.4466"}],"volume":"98","issue":"10","noUsgsAuthors":false,"publicationDate":"2013-10-01","publicationStatus":"PW","scienceBaseUri":"52b4155ee4b029a4958c9c70","contributors":{"authors":[{"text":"Lowenstern, Jacob B. 0000-0003-0464-7779 jlwnstrn@usgs.gov","orcid":"https://orcid.org/0000-0003-0464-7779","contributorId":2755,"corporation":false,"usgs":true,"family":"Lowenstern","given":"Jacob","email":"jlwnstrn@usgs.gov","middleInitial":"B.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":487513,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pitcher, Bradley W.","contributorId":37248,"corporation":false,"usgs":true,"family":"Pitcher","given":"Bradley","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":487514,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70125318,"text":"70125318 - 2013 - Correction of locality records for the endangered arroyo toad (Anaxyrus californicus) from the desert region of southern California","interactions":[],"lastModifiedDate":"2014-09-16T11:32:59","indexId":"70125318","displayToPublicDate":"2013-12-18T11:31:21","publicationYear":"2013","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1136,"text":"Bulletin of the Southern California Academy of Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Correction of locality records for the endangered arroyo toad (Anaxyrus californicus) from the desert region of southern California","docAbstract":"The recovery strategy for an endangered species requires accurate knowledge of its distribution and geographic range. Although the best available information is used when developing a recovery plan, uncertainty often remains in regard to a species actual geographic extent. The arroyo toad (<i>Anaxyrus californicus</i>) occurs almost exclusively in coastal drainages, from Monterey County, California, south into northwestern Baja California, Mexico. Through field reconnaissance and the study of preserved museum specimens we determined that the four reported populations of the arroyo toad from the Sonoran Desert region of Riverside, San Diego, and Imperial counties, California are in error. Two additional sites in the Sonoran Desert are discussed regarding the possibility that the arroyo toad occurs there. We recommend the continued scrutiny of arroyo toad records to maintain a high level of accuracy of its distribution and geographic extent.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of the Southern California Academy of Sciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Southern California Academy of Sciences","publisherLocation":"Los Angeles, CA","doi":"10.3160/0038-3872-112.3.197","usgsCitation":"Ervin, E.L., Beaman, K.R., and Fisher, R.N., 2013, Correction of locality records for the endangered arroyo toad (Anaxyrus californicus) from the desert region of southern California: Bulletin of the Southern California Academy of Sciences, v. 112, no. 3, p. 197-205, https://doi.org/10.3160/0038-3872-112.3.197.","productDescription":"9 p.","startPage":"197","endPage":"205","numberOfPages":"9","ipdsId":"IP-051247","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":293933,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.3160/0038-3872-112.3.197"},{"id":293934,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.39,32.53 ], [ -122.39,37.07 ], [ -114.13,37.07 ], [ -114.13,32.53 ], [ -122.39,32.53 ] ] ] } } ] }","volume":"112","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5419512ae4b091c7ffc8e62d","contributors":{"authors":[{"text":"Ervin, Edward L.","contributorId":7640,"corporation":false,"usgs":true,"family":"Ervin","given":"Edward","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":501248,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beaman, Kent R.","contributorId":26638,"corporation":false,"usgs":true,"family":"Beaman","given":"Kent","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":501249,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fisher, Robert N. 0000-0002-2956-3240 rfisher@usgs.gov","orcid":"https://orcid.org/0000-0002-2956-3240","contributorId":1529,"corporation":false,"usgs":true,"family":"Fisher","given":"Robert","email":"rfisher@usgs.gov","middleInitial":"N.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":501247,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70056150,"text":"fs20133112 - 2013 - Interactive energy atlas for Colorado and New Mexico: an online resource for decisionmakers","interactions":[],"lastModifiedDate":"2018-08-10T16:12:15","indexId":"fs20133112","displayToPublicDate":"2013-12-18T11:23:00","publicationYear":"2013","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2013-3112","title":"Interactive energy atlas for Colorado and New Mexico: an online resource for decisionmakers","docAbstract":"Throughout the western United States, increased demand for energy is driving the rapid development of nonrenewable and renewable energy resources. Resource managers must balance the benefits of energy development with the potential consequences for ecological resources and ecosystem services. To facilitate access to geospatial data related to energy resources, energy infrastructure, and natural resources that may be affected by energy development, the U.S. Geological Survey has developed an online <a href=\"http://my.usgs.gov/eerma/\" target=\"_blank\">Interactive Energy Atlas</a> (Energy Atlas) for Colorado and New Mexico. The Energy Atlas is designed to meet the needs of varied users who seek information about energy in the western United States. The Energy Atlas has two primary capabilities: a geographic information system (GIS) data viewer and an interactive map gallery. The GIS data viewer allows users to preview and download GIS data related to energy potential and development in Colorado and New Mexico. The interactive map gallery contains a collection of maps that compile and summarize thematically related data layers in a user-friendly format. The maps are dynamic, allowing users to explore data at different resolutions and obtain information about the features being displayed. The Energy Atlas also includes an interactive decision-support tool, which allows users to explore the potential consequences of energy development for species that vary in their sensitivity to disturbance.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20133112","usgsCitation":"Carr, N.B., Ignizio, D., Diffendorfer, J., Latysh, N., Matherne, A.M., Linard, J.I., Leib, K.J., and Hawkins, S.J., 2013, Interactive energy atlas for Colorado and New Mexico: an online resource for decisionmakers: U.S. Geological Survey Fact Sheet 2013-3112, 2 p., https://doi.org/10.3133/fs20133112.","productDescription":"2 p.","numberOfPages":"2","onlineOnly":"Y","ipdsId":"IP-045619","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true},{"id":37226,"text":"Core Science Analytics, Synthesis, and Libraries","active":true,"usgs":true}],"links":[{"id":280402,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs20133112.jpg"},{"id":280400,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2013/3112/"},{"id":280401,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2013/3112/pdf/fs2013-3112.pdf"}],"country":"United States","state":"Colorado;New Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.06,31.33 ], [ -109.06,41.0 ], [ -102.04,41.0 ], [ -102.04,31.33 ], [ -109.06,31.33 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52b2c405e4b08e3289f15709","contributors":{"authors":[{"text":"Carr, Natasha B. 0000-0002-4842-0632 carrn@usgs.gov","orcid":"https://orcid.org/0000-0002-4842-0632","contributorId":1918,"corporation":false,"usgs":true,"family":"Carr","given":"Natasha","email":"carrn@usgs.gov","middleInitial":"B.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":486345,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ignizio, Drew A. 0000-0001-8054-5139 dignizio@usgs.gov","orcid":"https://orcid.org/0000-0001-8054-5139","contributorId":4822,"corporation":false,"usgs":true,"family":"Ignizio","given":"Drew A.","email":"dignizio@usgs.gov","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":false,"id":486348,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Diffendorfer, James E. 0000-0003-1093-6948 jediffendorfer@usgs.gov","orcid":"https://orcid.org/0000-0003-1093-6948","contributorId":3208,"corporation":false,"usgs":true,"family":"Diffendorfer","given":"James E.","email":"jediffendorfer@usgs.gov","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true},{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":486346,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Latysh, Natalie 0000-0003-0149-3962 nlatysh@usgs.gov","orcid":"https://orcid.org/0000-0003-0149-3962","contributorId":1356,"corporation":false,"usgs":true,"family":"Latysh","given":"Natalie","email":"nlatysh@usgs.gov","affiliations":[{"id":208,"text":"Core Science Analytics and Synthesis","active":true,"usgs":true},{"id":5060,"text":"Data Preservation Program","active":true,"usgs":true}],"preferred":true,"id":486343,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Matherne, Ann Marie","contributorId":73909,"corporation":false,"usgs":true,"family":"Matherne","given":"Ann","email":"","middleInitial":"Marie","affiliations":[],"preferred":false,"id":486349,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Linard, Joshua I. jilinard@usgs.gov","contributorId":1465,"corporation":false,"usgs":true,"family":"Linard","given":"Joshua","email":"jilinard@usgs.gov","middleInitial":"I.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":486344,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Leib, Kenneth J. 0000-0002-0373-0768 kjleib@usgs.gov","orcid":"https://orcid.org/0000-0002-0373-0768","contributorId":701,"corporation":false,"usgs":true,"family":"Leib","given":"Kenneth","email":"kjleib@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":486342,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Hawkins, Sarah J. 0000-0002-1878-9121 shawkins@usgs.gov","orcid":"https://orcid.org/0000-0002-1878-9121","contributorId":4818,"corporation":false,"usgs":true,"family":"Hawkins","given":"Sarah","email":"shawkins@usgs.gov","middleInitial":"J.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":486347,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70049023,"text":"fs20133058 - 2013 - The 3D Elevation Program: summary for Florida","interactions":[],"lastModifiedDate":"2016-08-17T16:00:47","indexId":"fs20133058","displayToPublicDate":"2013-12-18T11:04:00","publicationYear":"2013","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2013-3058","title":"The 3D Elevation Program: summary for Florida","docAbstract":"<p>Elevation data are essential to a broad range of applications, including forest resources management, wildlife and habitat management, national security, recreation, and many others. For the State of Florida, elevation data are critical for natural resources conservation; flood risk management; infrastructure and construction management; coastal zone management; sea level rise and subsidence; wildfire management, planning, and response; and other business uses. Today, high-density light detection and ranging (lidar) data are the primary sources for deriving elevation models and other datasets. Federal, State, and local agencies work in partnership to (1) replace data that are older and of lower quality and (2) provide coverage where publicly accessible data do not exist. A joint goal of State and Federal partners is to acquire consistent, statewide coverage to support existing and emerging applications enabled by lidar data.</p>\n<p>The National Enhanced Elevation Assessment evaluated multiple elevation data acquisition options to determine the optimal data quality and data replacement cycle relative to cost to meet the identified requirements of the user community. The evaluation demonstrated that lidar acquisition at quality level 2 for the conterminous United States and quality level 5 ifsar data for Alaska with a 6- to 10-year acquisition cycle provided the highest benefit/cost ratios.The new 3D Elevation Program (3DEP) initiative selected an 8-year acquisition cycle for the respective quality levels. 3DEP, managed by the U.S. Geological Survey, the OMB Circular A&ndash;16 lead agency for terrestrial elevation data, responds to the growing need for high-quality topographic data and a wide range of other 3D representations of the Nation&rsquo;s natural and constructed features.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20133058","usgsCitation":"Carswell, W., 2013, The 3D Elevation Program: summary for Florida: U.S. Geological Survey Fact Sheet 2013-3058, 2 p., https://doi.org/10.3133/fs20133058.","productDescription":"2 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,{"id":70059025,"text":"70059025 - 2013 - Interactions between a group of Golden Eagles and a herd of North American elk","interactions":[],"lastModifiedDate":"2013-12-18T08:52:19","indexId":"70059025","displayToPublicDate":"2013-12-18T08:37:00","publicationYear":"2013","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2442,"text":"Journal of Raptor Research","active":true,"publicationSubtype":{"id":10}},"title":"Interactions between a group of Golden Eagles and a herd of North American elk","docAbstract":"Raptors are generally considered solitary predators (Schoener 1969), but occasionally they interact socially (Brown and Amadon 1968). Certain raptor species (e.g., Swallow-tailed Kites [<i>Elanoides forficatus</i>] and Swainson's Hawks [<i>Buteo swainsoni</i>]) concentrate in aggregations in response to localized, abundant food sources (Ellis et al. 1993). Many raptor species engage in group hunting (Ellis et al. 1993), and social foraging is a routine strategy for some species (e.g., Harris's Hawks [<i>Parabuteo unicinctus</i>]; Bednarz 1988, Ellis et al. 1993]. Raptors generally engage in group hunting to pursue elusive or large prey (Ellis et al. 1993). Occasionally individuals of conspecific raptors engage in play as a group sometimes involving chases of prey species (Palmer 1988). In this letter, we report interactions between a large group of Golden Eagles and a herd of adult and juvenile Rocky Mountain elk (<i>Cervus canadensis nelsoni</i>) in late autumn.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Raptor Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"The Raptor Research Foundation","doi":"10.3356/JRR-13-00027JRR-12-03.1","usgsCitation":"O’Connell, M.P., and Kochert, M.N., 2013, Interactions between a group of Golden Eagles and a herd of North American elk: Journal of Raptor Research, v. 47, no. 4, p. 416-418, https://doi.org/10.3356/JRR-13-00027JRR-12-03.1.","productDescription":"3 p.","startPage":"416","endPage":"418","numberOfPages":"3","ipdsId":"IP-049541","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":280392,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":280363,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.3356/JRR-13-00027JRR-12-03.1"}],"country":"United States","state":"Idaho","otherGeospatial":"Arrowrock Reservoir;Boise River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.939559,43.579867 ], [ -115.939559,43.659807 ], [ -115.819759,43.659807 ], [ -115.819759,43.579867 ], [ -115.939559,43.579867 ] ] ] } } ] }","volume":"47","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52b2c3e1e4b08e3289f15650","contributors":{"authors":[{"text":"O’Connell, Matt P.","contributorId":87054,"corporation":false,"usgs":true,"family":"O’Connell","given":"Matt","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":487432,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kochert, Michael N. 0000-0002-4380-3298 mkochert@usgs.gov","orcid":"https://orcid.org/0000-0002-4380-3298","contributorId":3037,"corporation":false,"usgs":true,"family":"Kochert","given":"Michael","email":"mkochert@usgs.gov","middleInitial":"N.","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":true,"id":487431,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70057871,"text":"ds807 - 2013 - Thermal profiles for reaches of Snee-Oosh and Fornsby Creeks, Swinomish Indian Reservation, northwestern Washington, July 2013","interactions":[],"lastModifiedDate":"2013-12-18T08:33:59","indexId":"ds807","displayToPublicDate":"2013-12-18T08:21:00","publicationYear":"2013","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"807","title":"Thermal profiles for reaches of Snee-Oosh and Fornsby Creeks, Swinomish Indian Reservation, northwestern Washington, July 2013","docAbstract":"Longitudinal profiles of streambed temperatures were measured in approximately 225-m-long reaches of the Snee-Oosh and Fornsby Creeks in the Swinomish Indian Reservation, northwestern Washington, during July 2013, to provide information about areas of groundwater discharge to streams. During summer, groundwater discharge is a source of cold water to streams and typically cools the surface water into which it discharges and buffers diurnal temperature fluctuations. Near-streambed temperatures were averaged over 1-m-long sections of cable during 1-minute periods every 30 minutes for 1-week periods using a fiber-optic distributed temperature sensor positioned on top of the streambed. The position of the fiber-optic cable was surveyed with a Global Positioning System. Stream temperatures and survey data are presented as Microsoft Excel<sup>®</sup> files consisting of date and time, water temperature, and geographical coordinates.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds807","collaboration":"Prepared in cooperation with the Swinomish Indian Tribal Community","usgsCitation":"Gendaszek, A.S., and Opatz, C.C., 2013, Thermal profiles for reaches of Snee-Oosh and Fornsby Creeks, Swinomish Indian Reservation, northwestern Washington, July 2013: U.S. Geological Survey Data Series 807, Report: iv, 5 p.; Tables 1-4, https://doi.org/10.3133/ds807.","productDescription":"Report: iv, 5 p.; Tables 1-4","numberOfPages":"14","onlineOnly":"Y","additionalOnlineFiles":"Y","ipdsId":"IP-052762","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":280391,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds807.GIF"},{"id":280389,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ds/807/pdf/ds807.pdf"},{"id":280390,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/ds/807/downloads/ds807_tables.xlsx"},{"id":280388,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/807/"}],"scale":"100000","projection":"Washington State Plane North FIPS","datum":"North American Datum of 1983","country":"United States","state":"Washington","otherGeospatial":"Fornsby Creek;Snee-oosh Creek;Swinomish Indian Reservation","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.591005,48.369938 ], [ -122.591005,48.466653 ], [ -122.48269,48.466653 ], [ -122.48269,48.369938 ], [ -122.591005,48.369938 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52b2c406e4b08e3289f15718","contributors":{"authors":[{"text":"Gendaszek, Andrew S. 0000-0002-2373-8986 agendasz@usgs.gov","orcid":"https://orcid.org/0000-0002-2373-8986","contributorId":3509,"corporation":false,"usgs":true,"family":"Gendaszek","given":"Andrew","email":"agendasz@usgs.gov","middleInitial":"S.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":486891,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Opatz, Chad C. 0000-0002-5272-0195 copatz@usgs.gov","orcid":"https://orcid.org/0000-0002-5272-0195","contributorId":48857,"corporation":false,"usgs":true,"family":"Opatz","given":"Chad","email":"copatz@usgs.gov","middleInitial":"C.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":false,"id":486892,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70193776,"text":"70193776 - 2013 - Catchment-scale stormwater management via economic incentives – An overview and lessons-learned","interactions":[],"lastModifiedDate":"2017-12-19T10:47:30","indexId":"70193776","displayToPublicDate":"2013-12-18T00:00:00","publicationYear":"2013","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Catchment-scale stormwater management via economic incentives – An overview and lessons-learned","docAbstract":"<p>Long-term field studies of the effectiveness and sustainability of decentralized stormwater management are rare. From 2005-2011, we tested an incentive-based approach to citizen participation in stormwater management in the Shepherd Creek catchment, located in Cincinnati, OH, USA. Hydrologic, biological, and water quality data were characterized in a baseline monitoring effort 2005- 2007. Reverse auctions held successively in 2007 and 2008 engaged citizens to voluntarily bid on stormwater control measures (SCMs); and successful bids led to implementation of SCMs, which led to an enhancement of catchment detention capacity. We tested for attributes of sustainability (coconsideration of social, economic, and environmental (hydrologic, soils, aquatic biology) aspects), and summarize lessons-learned. Our results and outcomes provide a basis for planning future field studies that more fully determine the effectiveness of stormwater management in terms of sustainability. </p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Novatech 2013: international conference on strategies and solutions for integrated and sustainable water management in the city Lyon, France","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Novatech 2013: international conference on strategies and solutions for integrated and sustainable water management in the city Lyon, France","conferenceDate":"June 23-27, 2013","conferenceLocation":"Lyon, France","language":"English","publisher":"Graie","publisherLocation":"Lyon, France","usgsCitation":"Schuster, W., Garmestani, A., Green, O., Rhea, L., Roy, A.H., and Thurston, H., 2013, Catchment-scale stormwater management via economic incentives – An overview and lessons-learned, <i>in</i> Novatech 2013: international conference 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,{"id":70058703,"text":"ofr20131287 - 2013 - Integrating Federal and State data records to report progress in establishing agricultural conservation practices on Chesapeake Bay farms","interactions":[],"lastModifiedDate":"2021-07-02T13:55:07.911183","indexId":"ofr20131287","displayToPublicDate":"2013-12-17T15:35:00","publicationYear":"2013","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2013-1287","title":"Integrating Federal and State data records to report progress in establishing agricultural conservation practices on Chesapeake Bay farms","docAbstract":"In response to the Executive Order for Chesapeake Bay Protection and Restoration (E.O. #13508, May 12, 2009), the U.S. Geological Survey (USGS) took on the task of acquiring and assessing agricultural conservation practice data records for U.S. Department of Agriculture (USDA) programs, and transferred those datasets in aggregated format to State jurisdictional agencies for use in reporting conservation progress to the Chesapeake Bay Program Partnership (CBP Partnership). Under the guidelines and regulations that have been developed to protect and restore water-quality in the Chesapeake Bay, the six State jurisdictions that fall within the Chesapeake Bay watershed are required to report their progress in promoting agricultural conservation practices to the CBP Partnership on an annual basis. The installation and adoption of agricultural best management practices is supported by technical and financial assistance from both Federal and State conservation programs. The farm enrollment data for USDA conservation programs are confidential, but agencies can obtain access to the privacy-protected data if they are established as USDA Conservation Cooperators. The datasets can also be released to the public if they are first aggregated to protect farmer privacy. In 2012, the USGS used its Conservation Cooperator status to obtain implementation data for conservation programs sponsored by the USDA Natural Resources Conservation Service (NRCS) and the USDA Farm Service Agency (FSA) for farms within the Chesapeake Bay watershed. Three jurisdictions (Delaware, Pennsylvania, and West Virginia) used the USGS-provided aggregated dataset to report conservation progress in 2012, whereas the remaining three jurisdictions (Maryland, New York, and Virginia) used jurisdictional Conservation Cooperator Agreements to obtain privacy-protected data directly from the USDA. This report reviews the status of conservation data sharing between the USDA and the various jurisdictions, discusses the methods that were used by the USGS in 2012 to collect and process USDA agricultural conservation data, and also documents methods that were used by the jurisdictions to integrate Federal and State data records, reduce double counting, and provide an accurate reporting of conservation practices to the CBP Partnership’s Annual Progress Review. A similar tracking, reporting, and assessment will occur in future years, as State and Federal governments and nongovernmental organizations continue to work with farmers and conservation districts to reduce the impacts of agriculture on water-quality.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20131287","issn":"2331-1258","usgsCitation":"Hively, W., Devereux, O.H., and Claggett, P.R., 2013, Integrating Federal and State data records to report progress in establishing agricultural conservation practices on Chesapeake Bay farms: U.S. Geological Survey Open-File Report 2013-1287, Report: vii, 37 p.; Downloads Directory, https://doi.org/10.3133/ofr20131287.","productDescription":"Report: vii, 37 p.; Downloads Directory","numberOfPages":"46","onlineOnly":"Y","ipdsId":"IP-049633","costCenters":[{"id":242,"text":"Eastern Geographic Science 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Dean 0000-0002-5383-8064","orcid":"https://orcid.org/0000-0002-5383-8064","contributorId":9391,"corporation":false,"usgs":true,"family":"Hively","given":"W. Dean","affiliations":[],"preferred":false,"id":487265,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Devereux, Olivia H.","contributorId":97238,"corporation":false,"usgs":true,"family":"Devereux","given":"Olivia","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":487267,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Claggett, Peter R. 0000-0002-5335-2857 pclaggett@usgs.gov","orcid":"https://orcid.org/0000-0002-5335-2857","contributorId":176287,"corporation":false,"usgs":true,"family":"Claggett","given":"Peter","email":"pclaggett@usgs.gov","middleInitial":"R.","affiliations":[{"id":24708,"text":"Lower Mississippi-Gulf Water Science Center","active":true,"usgs":true},{"id":242,"text":"Eastern Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":487266,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70056038,"text":"sir20135209 - 2013 - A preliminary assessment of streamflow gains and losses for selected stream reaches in the lower Guadalupe River Basin, Texas, 2010-12","interactions":[],"lastModifiedDate":"2016-08-05T13:18:32","indexId":"sir20135209","displayToPublicDate":"2013-12-17T12:40:00","publicationYear":"2013","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2013-5209","title":"A preliminary assessment of streamflow gains and losses for selected stream reaches in the lower Guadalupe River Basin, Texas, 2010-12","docAbstract":"<p>The U.S. Geological Survey, in cooperation with the U.S. Army Corps of Engineers&ndash;Fort Worth District, the Texas Water Development Board, the Guadalupe-Blanco River Authority, and the Edwards Aquifer Authority, investigated streamflow gains and losses in the lower Guadalupe River Basin during four selected base-flow periods in March 2010, April 2011, August 2011, and, for a stream reach between Seguin, Tex., and Gonzales, Tex., in September 2012. Major sources of streamflow in this basin include releases from Canyon Lake, inflow from major springs (Comal Springs, San Marcos Springs, and Hueco Springs), and base flow (groundwater seeping to streams). Streamflow and spring-flow data were collected at 35 streamflow-gaging stations (including 6 deployed for this study) during the base-flow periods. This report describes streamflow in the lower Guadalupe River Basin, which consists of the Guadalupe River drainage basin downstream from Canyon Lake to the Guadalupe River near Tivoli, Tex.</p>\n<p>Streamflow conditions in the lower Guadalupe River Basin were analyzed by computing surface-water budgets for reaches of the lower Guadalupe River and tributary streams. Streamflow gains and losses were mapped for reaches where the computed gain or loss was greater than the uncertainty in the computed streamflow at the upstream and downstream ends of the reach.</p>\n<p>During the March 15&ndash;21, 2010, base-flow period, five reaches had gains greater than the uncertainty in the computed streamflow, including reach 1 on the Guadalupe River, which gained 130 cubic feet per second (ft<sup>3</sup>/s), and reach 3 on the Comal River, which gained 359 ft<sup>3</sup>/s. Streamflow gains during March 2010 primarily were derived from (1) inflow from the Edwards aquifer outcrop, including Hueco Springs and Comal Springs; (2) flow conveyed through the alluvium of the streambed; (3) inflows from the Carrizo-Wilcox aquifer and the Yegua Jackson aquifer; and (4) groundwater inflows from the Gulf Coast aquifer, which are enhanced by seepage losses from Coleto Creek Reservoir. During this base-flow period, none of the reaches had a loss greater in magnitude than the uncertainty in the computed streamflow.</p>\n<p>During the April 10&ndash;16, 2011, base-flow period, three reaches had gains greater than the uncertainty in the computed streamflow. Among these three reaches were reach 1 on the Guadalupe River, which gained 40.7 ft<sup>3</sup>/s, and reach 3 on the Comal River, which gained 271 ft<sup>3</sup>/s&mdash;reaches where streamflow gains were also measured in March 2010. Streamflow gains during April 2011 primarily were derived from (1) inflow from the Edwards aquifer outcrop, including Hueco Springs and Comal Springs; and (2) inflows from the Carrizo-Wilcox aquifer. During this base-flow period, three reaches had losses greater in magnitude than the uncertainty in the computed streamflow. A reach of the Blanco River near Kyle, Tex. (reach 10), lost 18.7 cubic feet per second (ft3/s). Much of this loss likely entered the groundwater system through the numerous faults that intersect the stream channel northwest of Kyle. The reach that included the confluence of the Guadalupe and San Marcos Rivers (reach 17) lost 155 ft<sup>3</sup>/s, likely as recharge to the Sparta and Queen City aquifers.</p>\n<p>During the August 19&ndash;25, 2011, base-flow period, three reaches had gains greater than the uncertainty in the computed streamflow, including reach 3 on the Comal River (168 ft<sup>3</sup>/s gain), which was one of the reaches where gains in streamflow also were measured in March 2010 and April 2011. Streamflow gains in August 2011 were primarily from (1) inflows from Comal Springs, (2) inflows from the Yegua Jackson aquifer, and (3) groundwater inflows from the Gulf Coast aquifer, which are enhanced by seepage losses from Coleto Creek Reservoir. During this base-flow period, five reaches had losses greater in magnitude than the uncertainty in the computed streamflow. The reach including the confluence of the Guadalupe and Comal Rivers lost 82.8 ft<sup>3</sup>/s. Much of that loss likely seeped into the local groundwater system. The reach of the Guadalupe River south of New Braunfels, Tex., to Seguin, Tex., lost 53.5 ft<sup>3</sup>/s. Part of that loss may have been from seepage through streambed alluvium. Reaches 9 and 10 of the Blanco River near Kyle lost 2.20 and 6.60 ft<sup>3</sup>/s, respectively, likely as infiltration through numerous faults intersecting the stream channel northwest of Kyle. Plum Creek between Lockhart, Tex., and Luling, Tex., lost 2.11 ft<sup>3</sup>/s, likely as recharge to the Carrizo-Wilcox aquifer. A base-flow period during September 22&ndash;28, 2012, was studied for the reach of the Guadalupe River between Seguin and Gonzalez, including flows from San Marcos River and Plum Creek. During this period, for the Guadalupe River reach between Seguin and Oak Forest, no computed gains or losses were greater in magnitude than the uncertainty in the computed streamflow.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20135209","issn":"2328-0328","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers–Fort Worth District, the Texas Water Development Board, the Guadalupe-Blanco River Authority, and the Edwards Aquifer Authority","usgsCitation":"Wehmeyer, L.L., Winters, K.E., and Ockerman, D.J., 2013, A preliminary assessment of streamflow gains and losses for selected stream reaches in the lower Guadalupe River Basin, Texas, 2010-12: U.S. Geological Survey Scientific Investigations Report 2013-5209, v, 30 p., https://doi.org/10.3133/sir20135209.","productDescription":"v, 30 p.","numberOfPages":"39","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"2010-01-01","temporalEnd":"2012-12-01","ipdsId":"IP-050892","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":280374,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir20135209.jpg"},{"id":280372,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2013/5209/"},{"id":280373,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2013/5209/pdf/sir2013-5209.pdf"}],"scale":"100000","datum":"North American Datum of 1983","country":"United States","state":"Texas","otherGeospatial":"Guadalupe River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -100.0,28.0 ], [ -100.0,30.2 ], [ -96.0,30.2 ], [ -96.0,28.0 ], [ -100.0,28.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52b17262e4b0d9b325224481","contributors":{"authors":[{"text":"Wehmeyer, Loren L.","contributorId":90412,"corporation":false,"usgs":true,"family":"Wehmeyer","given":"Loren","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":486301,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Winters, Karl E. kwinters@usgs.gov","contributorId":3554,"corporation":false,"usgs":true,"family":"Winters","given":"Karl","email":"kwinters@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":486300,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ockerman, Darwin J. 0000-0003-1958-1688 ockerman@usgs.gov","orcid":"https://orcid.org/0000-0003-1958-1688","contributorId":1579,"corporation":false,"usgs":true,"family":"Ockerman","given":"Darwin","email":"ockerman@usgs.gov","middleInitial":"J.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":486299,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70059032,"text":"70059032 - 2013 - Crystallization of oxidized, moderately hydrous arc basalt at mid- to lower-crustal pressures: Implications for andesite genesis","interactions":[],"lastModifiedDate":"2019-03-26T08:36:47","indexId":"70059032","displayToPublicDate":"2013-12-17T12:08:41","publicationYear":"2013","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1336,"text":"Contributions to Mineralogy and Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Crystallization of oxidized, moderately hydrous arc basalt at mid- to lower-crustal pressures: Implications for andesite genesis","docAbstract":"This study focuses on the production of convergent margin calc-alkaline andesites by crystallization–differentiation of basaltic magmas in the lower to middle crust. Previous experimental studies show that dry, reduced, subalkaline basalts differentiate to tholeiitic (high Fe/Mg) daughter liquids, but the influences of H<sub>2</sub>O and oxidation on differentiation are less well established. Accordingly, we performed crystallization experiments at controlled oxidized fO<sub>2</sub> (Re–ReO<sub>2</sub> ≈ ΔNi–NiO + 2) on a relatively magnesian basalt (8.7 wt% MgO) typical of mafic magmas erupted in the Cascades near Mount Rainier, Washington. The basalt was synthesized with 2 wt% H2O and run at 900, 700, and 400 MPa and 1,200 to 950 °C. A broadly clinopyroxenitic crystallization interval dominates near the liquidus at 900 and 700 MPa, consisting of augite + olivine + orthopyroxene + Cr-spinel (in decreasing abundance). With decreasing temperature, plagioclase crystallizes, Fe–Ti-oxide replaces spinel, olivine dissolves, and finally amphibole appears, producing gabbroic and then amphibole gabbroic crystallization stages. Enhanced plagioclase stability at lower pressure narrows the clinopyroxenitic interval and brings the gabbroic interval toward the liquidus. Liquids at 900 MPa track along Miyashiro’s (Am J Sci 274(4):321–355, 1974) tholeiitic versus calc-alkaline boundary, whereas those at 700 and 400 MPa become calc-alkaline at silica contents ≥56 wt%. This difference is chiefly due to higher temperature appearance of magnetite (versus spinel) at lower pressures. Although the evolved liquids are similar in many respects to common calc-alkaline andesites, the 900 and 700 MPa liquids differ in having low CaO concentrations due to early and abundant crystallization of augite, with the result that those liquids become peraluminous (ASI: molar Al/(Na + K + 2Ca) > 1) at ≥61 wt% SiO<sub>2</sub>, similar to liquids reported in other studies of the high-pressure crystallization of hydrous basalts (Müntener and Ulmer in Geophys Res Lett 33(21):L21308, 2006). The lower-pressure liquids (400 MPa) have this same trait, but to a lesser extent due to more abundant near-liquidus plagioclase crystallization. A compilation of >6,500 analyses of igneous rocks from the Cascades and the Sierra Nevada batholith, representative of convergent margin (arc) magmas, shows that ASI increases continuously and linearly with SiO2 from basalts to rhyolites or granites and that arc magmas are not commonly peraluminous until SiO<sub>2</sub> exceeds 69 wt%. These relations are consistent with plagioclase accompanying mafic silicates over nearly all the range of crystallization (or remelting). The scarcity of natural peraluminous andesites shows that progressive crystallization–differentiation of primitive basalts in the deep crust, producing early clinopyroxenitic cumulates and evolved liquids, does not dominate the creation of intermediate arc magmas or of the continental crust. Instead, mid- to upper-crustal differentiation and/or open-system processes are critical to the production of intermediate arc magmas. Primary among the open-system processes may be extraction of highly evolved (granitic, rhyolitic) liquids at advanced degrees of basalt solidification (or incipient partial melting of predecessor gabbroic intrusions) and mixing of such liquids into replenishing basalts. Furthermore, if the andesitic-composition continents derived from basaltic sources, the arc ASI–SiO<sub>2</sub> relation shows that the mafic component returned to the mantle was gabbroic in composition, not pyroxenitic.","language":"English","publisher":"Springer","doi":"10.1007/s00410-013-0920-3","usgsCitation":"Blatter, D., Sisson, T.W., and Hankins, W., 2013, Crystallization of oxidized, moderately hydrous arc basalt at mid- to lower-crustal pressures: Implications for andesite genesis: Contributions to Mineralogy and Petrology, v. 166, no. 3, p. 861-886, https://doi.org/10.1007/s00410-013-0920-3.","productDescription":"26 p.","startPage":"861","endPage":"886","ipdsId":"IP-048906","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":280407,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"166","issue":"3","noUsgsAuthors":false,"publicationDate":"2013-08-22","publicationStatus":"PW","scienceBaseUri":"53cd5394e4b0b290850f5397","contributors":{"authors":[{"text":"Blatter, Dawnika L.","contributorId":23427,"corporation":false,"usgs":true,"family":"Blatter","given":"Dawnika L.","affiliations":[],"preferred":false,"id":487441,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sisson, Thomas W. 0000-0003-3380-6425 tsisson@usgs.gov","orcid":"https://orcid.org/0000-0003-3380-6425","contributorId":2341,"corporation":false,"usgs":true,"family":"Sisson","given":"Thomas","email":"tsisson@usgs.gov","middleInitial":"W.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":487440,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hankins, W. Ben 0000-0001-9881-9468","orcid":"https://orcid.org/0000-0001-9881-9468","contributorId":28618,"corporation":false,"usgs":true,"family":"Hankins","given":"W. Ben","affiliations":[],"preferred":true,"id":487442,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70059027,"text":"fs20133118 - 2013 - Methane occurrence in groundwater of south-central New York State, 2012: summary of findings","interactions":[],"lastModifiedDate":"2013-12-17T11:33:28","indexId":"fs20133118","displayToPublicDate":"2013-12-17T11:27:00","publicationYear":"2013","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2013-3118","title":"Methane occurrence in groundwater of south-central New York State, 2012: summary of findings","docAbstract":"A survey of methane in groundwater was undertaken to document methane occurrence on the basis of hydrogeologic setting within a glaciated 1,810-square-mile area of south-central New York that has not seen shale-gas resource development. The adjacent region in northeastern Pennsylvania has undergone shale-gas resource development from the Marcellus Shale.\n\nWell construction and subsurface data were required for each well sampled so that the local hydrogeologic setting could be classified. All wells were also at least 1 mile from any known gas well (active, exploratory, or abandoned). Sixty-six domestic wells and similar purposed supply wells were sampled during summer 2012. Field water-quality characteristics (pH, specific conductance, dissolved oxygen, and temperature) were measured at each well, and samples were collected and analyzed for dissolved gases, including methane and short-chain hydrocarbons. Carbon and hydrogen isotopic ratios of methane were measured in 21 samples that had at least 0.3 milligram per liter (mg/L) methane.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20133118","issn":"2327-6932","usgsCitation":"Heisig, P.M., and Scott, T., 2013, Methane occurrence in groundwater of south-central New York State, 2012: summary of findings: U.S. Geological Survey Fact Sheet 2013-3118, 2 p., https://doi.org/10.3133/fs20133118.","productDescription":"2 p.","numberOfPages":"2","onlineOnly":"Y","ipdsId":"IP-053308","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":280366,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs20133118.jpg"},{"id":280365,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2013/3118/pdf/fs2013-3118.pdf"},{"id":280364,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2013/3118"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -78.0,41.0 ], [ -78.0,43.0 ], [ -75.0,43.0 ], [ -75.0,41.0 ], [ -78.0,41.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52b172c0e4b0d9b3252245f6","contributors":{"authors":[{"text":"Heisig, Paul M. 0000-0003-0338-4970 pmheisig@usgs.gov","orcid":"https://orcid.org/0000-0003-0338-4970","contributorId":793,"corporation":false,"usgs":true,"family":"Heisig","given":"Paul","email":"pmheisig@usgs.gov","middleInitial":"M.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":487438,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, Tia-Marie 0000-0002-5677-0544 tia-mariescott@usgs.gov","orcid":"https://orcid.org/0000-0002-5677-0544","contributorId":5122,"corporation":false,"usgs":true,"family":"Scott","given":"Tia-Marie","email":"tia-mariescott@usgs.gov","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":487439,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70058769,"text":"70058769 - 2013 - Differential preservation in the geologic record of intraoceanic arc sedimentary and tectonic processes","interactions":[],"lastModifiedDate":"2013-12-17T10:17:40","indexId":"70058769","displayToPublicDate":"2013-12-17T10:06:00","publicationYear":"2013","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1431,"text":"Earth-Science Reviews","active":true,"publicationSubtype":{"id":10}},"title":"Differential preservation in the geologic record of intraoceanic arc sedimentary and tectonic processes","docAbstract":"Records of ancient intraoceanic arc activity, now preserved in continental suture zones, are commonly used to reconstruct paleogeography and plate motion, and to understand how continental crust is formed, recycled, and maintained through time. However, interpreting tectonic and sedimentary records from ancient terranes after arc–continent collision is complicated by preferential preservation of evidence for some arc processes and loss of evidence for others. In this synthesis we examine what is lost, and what is preserved, in the translation from modern processes to the ancient record of intraoceanic arcs.\n\nComposition of accreted arc terranes differs as a function of arc–continent collision geometry. ‘Forward-facing’ collision can accrete an oceanic arc on to either a passive or an active continental margin, with the arc facing the continent and colliding trench- and forearc-side first. In a ‘backward-facing’ collision, involving two subduction zones with similar polarity, the arc collides backarc-first with an active continental margin. The preservation of evidence for contemporary sedimentary and tectonic arc processes in the geologic record depends greatly on how well the various parts of the arc survive collision and orogeny in each case.\n\nPreservation of arc terranes likely is biased towards those that were in a state of tectonic accretion for tens of millions of years before collision, rather than tectonic erosion. The prevalence of tectonic erosion in modern intraoceanic arcs implies that valuable records of arc processes are commonly destroyed even before the arc collides with a continent. Arc systems are most likely to undergo tectonic accretion shortly before forward-facing collision with a continent, and thus most forearc and accretionary-prism material in ancient arc terranes likely is temporally biased toward the final stages of arc activity, when sediment flux to the trench was greatest and tectonic accretion prevailed. Collision geometry and tectonic erosion vs. accretion are important controls on the ultimate survival of material from the trench, forearc, arc massif, intra-arc basins, and backarc basins, and thus on how well an ancient arc terrane preserves evidence for tectonic processes such as subduction of aseismic ridges and seamounts, oblique plate convergence, and arc rifting. Forward-facing collision involves substantial recycling, melting, and fractionation of continent-derived material during and after collision, and so produces melts rich in silica and incompatible trace elements. As a result, forward-facing collision can drive the composition of accreted arc crust toward that of average continental crust.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth-Science Reviews","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","usgsCitation":"Draut, A., and Clift, P.D., 2013, Differential preservation in the geologic record of intraoceanic arc sedimentary and tectonic processes: Earth-Science Reviews, v. 116, p. 57-84.","productDescription":"28 p.","startPage":"57","endPage":"84","numberOfPages":"28","ipdsId":"IP-037534","costCenters":[],"links":[{"id":280360,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"116","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52b172bde4b0d9b3252245e0","contributors":{"authors":[{"text":"Draut, Amy","contributorId":18792,"corporation":false,"usgs":true,"family":"Draut","given":"Amy","affiliations":[],"preferred":false,"id":487370,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clift, Peter D.","contributorId":17711,"corporation":false,"usgs":true,"family":"Clift","given":"Peter","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":487369,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70058837,"text":"70058837 - 2013 - Chronic toxicity of nickel-spiked freshwater sediments: variation in toxicity among eight invertebrate taxa and eight sediments","interactions":[],"lastModifiedDate":"2016-11-04T11:11:34","indexId":"70058837","displayToPublicDate":"2013-12-17T09:35:00","publicationYear":"2013","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Chronic toxicity of nickel-spiked freshwater sediments: variation in toxicity among eight invertebrate taxa and eight sediments","docAbstract":"<p><span>This study evaluated the chronic toxicity of Ni-spiked freshwater sediments to benthic invertebrates. A 2-step spiking procedure (spiking and sediment dilution) and a 2-stage equilibration period (10 wk anaerobic and 1 wk aerobic) were used to spike 8 freshwater sediments with wide ranges of acid-volatile sulfide (AVS; 0.94–38 µmol/g) and total organic carbon (TOC; 0.42–10%). Chronic sediment toxicity tests were conducted with 8 invertebrates (</span><i>Hyalella azteca, Gammarus pseudolimnaeus</i><span>, </span><i>Chironomus riparius, Chironomus dilutus</i><span>, </span><i>Hexagenia</i><span> sp., </span><i>Lumbriculus variegatus, Tubifex tubifex</i><span>, and </span><i>Lampsilis siliquoidea</i><span>) in 2 spiked sediments. Nickel toxicity thresholds estimated from species-sensitivity distributions were 97 µg/g and 752 µg/g (total recoverable Ni; dry wt basis) for sediments with low and high concentrations of AVS and TOC, respectively. Sensitive species were tested with 6 additional sediments. The 20% effect concentrations (EC20s) for </span><i>Hyalella</i><span> and </span><i>Gammarus</i><span>, but not </span><i>Hexagenia</i><span>, were consistent with US Environmental Protection Agency benchmarks based on Ni in porewater and in simultaneously extracted metals (SEM) normalized to AVS and TOC. For </span><i>Hexagenia</i><span>, sediment EC20s increased at less than an equimolar basis with increased AVS, and toxicity occurred in several sediments with Ni concentrations in SEM less than AVS. The authors hypothesize that circulation of oxygenated water by </span><i>Hexagenia</i><span> led to oxidation of AVS in burrows, creating microenvironments with high Ni exposure. Despite these unexpected results, a strong relationship between </span><i>Hexagenia</i><span> EC20s and AVS could provide a basis for conservative site-specific sediment quality guidelines for Ni. </span></p>","language":"English","publisher":"Wiley","doi":"10.1002/etc.2271","usgsCitation":"Besser, J.M., Brumbaugh, W.G., Ingersoll, C.G., Ivey, C.D., Kunz, J.L., Kemble, N.E., Schlekat, C.E., and Garman, E.R., 2013, Chronic toxicity of nickel-spiked freshwater sediments: variation in toxicity among eight invertebrate taxa and eight sediments: Environmental Toxicology and Chemistry, v. 32, no. 11, p. 2495-2506, https://doi.org/10.1002/etc.2271.","productDescription":"12 p.","startPage":"2495","endPage":"2506","numberOfPages":"12","ipdsId":"IP-041871","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":280355,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":280354,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/etc.2271"}],"volume":"32","issue":"11","noUsgsAuthors":false,"publicationDate":"2013-05-08","publicationStatus":"PW","scienceBaseUri":"52b172bbe4b0d9b3252245d0","contributors":{"authors":[{"text":"Besser, John M. 0000-0002-9464-2244 jbesser@usgs.gov","orcid":"https://orcid.org/0000-0002-9464-2244","contributorId":2073,"corporation":false,"usgs":true,"family":"Besser","given":"John","email":"jbesser@usgs.gov","middleInitial":"M.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":487384,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brumbaugh, William G. 0000-0003-0081-375X bbrumbaugh@usgs.gov","orcid":"https://orcid.org/0000-0003-0081-375X","contributorId":493,"corporation":false,"usgs":true,"family":"Brumbaugh","given":"William","email":"bbrumbaugh@usgs.gov","middleInitial":"G.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":487382,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ingersoll, Christopher G. 0000-0003-4531-5949 cingersoll@usgs.gov","orcid":"https://orcid.org/0000-0003-4531-5949","contributorId":2071,"corporation":false,"usgs":true,"family":"Ingersoll","given":"Christopher","email":"cingersoll@usgs.gov","middleInitial":"G.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":487383,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ivey, Chris D. 0000-0002-0485-7242 civey@usgs.gov","orcid":"https://orcid.org/0000-0002-0485-7242","contributorId":3308,"corporation":false,"usgs":true,"family":"Ivey","given":"Chris","email":"civey@usgs.gov","middleInitial":"D.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":487386,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kunz, James L. 0000-0002-1027-158X jkunz@usgs.gov","orcid":"https://orcid.org/0000-0002-1027-158X","contributorId":3309,"corporation":false,"usgs":true,"family":"Kunz","given":"James","email":"jkunz@usgs.gov","middleInitial":"L.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":487387,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kemble, Nile E. 0000-0002-3608-0538 nkemble@usgs.gov","orcid":"https://orcid.org/0000-0002-3608-0538","contributorId":2626,"corporation":false,"usgs":true,"family":"Kemble","given":"Nile","email":"nkemble@usgs.gov","middleInitial":"E.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":487385,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Schlekat, Christian E.","contributorId":28519,"corporation":false,"usgs":true,"family":"Schlekat","given":"Christian","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":487389,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Garman, Emily R.","contributorId":19461,"corporation":false,"usgs":true,"family":"Garman","given":"Emily","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":487388,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70058836,"text":"70058836 - 2013 - Characterizing response of total suspended solids and total phosphorus loading to weather and watershed characteristics for rainfall and snowmelt events in agricultural watersheds","interactions":[],"lastModifiedDate":"2013-12-17T09:32:07","indexId":"70058836","displayToPublicDate":"2013-12-17T09:20:00","publicationYear":"2013","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Characterizing response of total suspended solids and total phosphorus loading to weather and watershed characteristics for rainfall and snowmelt events in agricultural watersheds","docAbstract":"Understanding the response of total suspended solids (TSS) and total phosphorus (TP) to influential weather and watershed variables is critical in the development of sediment and nutrient reduction plans. In this study, rainfall and snowmelt event loadings of TSS and TP were analyzed for eight agricultural watersheds in Wisconsin, with areas ranging from 14 to 110 km2 and having four to twelve years of data available. The data showed that a small number of rainfall and snowmelt runoff events accounted for the majority of total event loading. The largest 10% of the loading events for each watershed accounted for 73–97% of the total TSS load and 64–88% of the total TP load. More than half of the total annual TSS load was transported during a single event for each watershed at least one of the monitored years. Rainfall and snowmelt events were both influential contributors of TSS and TP loading. TSS loading contributions were greater from rainfall events at five watersheds, from snowmelt events at two watersheds, and nearly equal at one watershed. The TP loading contributions were greater from rainfall events at three watersheds, from snowmelt events at two watersheds and nearly equal at three watersheds. Stepwise multivariate regression models for TSS and TP event loadings were developed separately for rainfall and snowmelt runoff events for each individual watershed and for all watersheds combined by using a suite of precipitation, melt, temperature, seasonality, and watershed characteristics as predictors. All individual models and the combined model for rainfall events resulted in two common predictors as most influential for TSS and TP. These included rainfall depth and the antecedent baseflow. Using these two predictors alone resulted in an R<sup>2</sup> greater than 0.7 in all but three individual models and 0.61 or greater for all individual models. The combined model yielded an R<sup>2</sup> of 0.66 for TSS and 0.59 for TP. Neither the individual nor the combined models were substantially improved by using additional predictors. Snowmelt event models were statistically significant for individual and combined watershed models, but the model fits were not all as good as those for rainfall events (R<sup>2</sup> between 0.19 and 0.87). Predictor selection varied from watershed to watershed, and the common variables that were selected were not always selected in the same order. Influential variables were commonly direct measures of moisture in the watershed such as snowmelt, rainfall + snowmelt, and antecedent baseflow, or measures of potential snowmelt volume in the watershed such as air temperature.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Hydrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"doi":"10.1016/j.jhydrol.2013.09.038","usgsCitation":"Danz, M., Corsi, S., Brooks, W.R., and Bannerman, R.T., 2013, Characterizing response of total suspended solids and total phosphorus loading to weather and watershed characteristics for rainfall and snowmelt events in agricultural watersheds: Journal of Hydrology, v. 507, p. 249-261, https://doi.org/10.1016/j.jhydrol.2013.09.038.","productDescription":"13 p.","startPage":"249","endPage":"261","numberOfPages":"13","ipdsId":"IP-045989","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":280353,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":280312,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.jhydrol.2013.09.038"}],"country":"United States","state":"Wisconsin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -92.8894,42.4919 ], [ -92.8894,47.0807 ], [ -86.764,47.0807 ], [ -86.764,42.4919 ], [ -92.8894,42.4919 ] ] ] } } ] }","volume":"507","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52b172bae4b0d9b3252245c6","contributors":{"authors":[{"text":"Danz, Mari E. medanz@usgs.gov","contributorId":3349,"corporation":false,"usgs":true,"family":"Danz","given":"Mari E.","email":"medanz@usgs.gov","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":true,"id":487378,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Corsi, Steven","contributorId":106002,"corporation":false,"usgs":true,"family":"Corsi","given":"Steven","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":false,"id":487381,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brooks, Wesley R. wrbrooks@usgs.gov","contributorId":4217,"corporation":false,"usgs":true,"family":"Brooks","given":"Wesley","email":"wrbrooks@usgs.gov","middleInitial":"R.","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":true,"id":487379,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bannerman, Roger T. 0000-0001-9221-2905 rbannerman@usgs.gov","orcid":"https://orcid.org/0000-0001-9221-2905","contributorId":5560,"corporation":false,"usgs":true,"family":"Bannerman","given":"Roger","email":"rbannerman@usgs.gov","middleInitial":"T.","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":true,"id":487380,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70058768,"text":"70058768 - 2013 - Assessing grain-size correspondence between flow and deposits of controlled floods in the Colorado River, USA","interactions":[],"lastModifiedDate":"2013-12-17T09:18:34","indexId":"70058768","displayToPublicDate":"2013-12-17T09:13:00","publicationYear":"2013","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2451,"text":"Journal of Sedimentary Research","onlineIssn":"1938-3681","printIssn":"1527-1404","active":true,"publicationSubtype":{"id":10}},"title":"Assessing grain-size correspondence between flow and deposits of controlled floods in the Colorado River, USA","docAbstract":"Flood-deposited sediment has been used to decipher environmental parameters such as variability in watershed sediment supply, paleoflood hydrology, and channel morphology. It is not well known, however, how accurately the deposits reflect sedimentary processes within the flow, and hence what sampling intensity is needed to decipher records of recent or long-past conditions. We examine these problems using deposits from dam-regulated floods in the Colorado River corridor through Marble Canyon–Grand Canyon, Arizona, U.S.A., in which steady-peaked floods represent a simple end-member case. For these simple floods, most deposits show inverse grading that reflects coarsening suspended sediment (a result of fine-sediment-supply limitation), but there is enough eddy-scale variability that some profiles show normal grading that did not reflect grain-size evolution in the flow as a whole. To infer systemwide grain-size evolution in modern or ancient depositional systems requires sampling enough deposit profiles that the standard error of the mean of grain-size-change measurements becomes small relative to the magnitude of observed changes. For simple, steady-peaked floods, 5–10 profiles or fewer may suffice to characterize grain-size trends robustly, but many more samples may be needed from deposits with greater variability in their grain-size evolution.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Sedimentary Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society for Sedimentary Geology","doi":"10.2110/jsr.2013.79","usgsCitation":"Draut, A., and Rubin, D.M., 2013, Assessing grain-size correspondence between flow and deposits of controlled floods in the Colorado River, USA: Journal of Sedimentary Research, v. 83, no. 11, p. 962-973, https://doi.org/10.2110/jsr.2013.79.","productDescription":"12 p.","startPage":"962","endPage":"973","numberOfPages":"12","ipdsId":"IP-051517","costCenters":[],"links":[{"id":280352,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":280351,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2110/jsr.2013.79"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.82,32.49 ], [ -114.82,40.43 ], [ -105.82,40.43 ], [ -105.82,32.49 ], [ -114.82,32.49 ] ] ] } } ] }","volume":"83","issue":"11","noUsgsAuthors":false,"publicationDate":"2013-11-01","publicationStatus":"PW","scienceBaseUri":"52b172b8e4b0d9b3252245bc","contributors":{"authors":[{"text":"Draut, Amy","contributorId":18792,"corporation":false,"usgs":true,"family":"Draut","given":"Amy","affiliations":[],"preferred":false,"id":487368,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rubin, David M. 0000-0003-1169-1452 drubin@usgs.gov","orcid":"https://orcid.org/0000-0003-1169-1452","contributorId":3159,"corporation":false,"usgs":true,"family":"Rubin","given":"David","email":"drubin@usgs.gov","middleInitial":"M.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":487367,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70055672,"text":"sir20135035 - 2013 - Erosional and depositional changes wrought by the flood of May 1978 in the channels of Powder River, southeastern Montana","interactions":[],"lastModifiedDate":"2013-12-17T08:42:46","indexId":"sir20135035","displayToPublicDate":"2013-12-17T08:31:00","publicationYear":"2013","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2013-5035","title":"Erosional and depositional changes wrought by the flood of May 1978 in the channels of Powder River, southeastern Montana","docAbstract":"Powder River’s second largest flood of record (1919–2012) moved through northeastern Wyoming and southeastern Montana during May 1978. Within a ninety-kilometer reach of the channel in southeastern Montana, the most prominent planform effects of the flood were the growth of meander bends by bank erosion (this was most intense just downriver of bend apexes, causing 1–2 channel widths of lateral displacement) and the erosion of new cutoff channels through the necks of two large and two small meanders. Surveys of cross sections, made before and after the flood, show the responses of the channel to the flood waters, which ranged from minimal (bedrock control) to large (maximum channel curvature in unconsolidated bank and terrace deposits). Geomorphic work done during two weeks of extreme flooding in May 1978, as measured by cross-channel erosion and new sediment deposition, was approximately equal in magnitude to the work done during the two decades (1978–1998) that followed the flood.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20135035","usgsCitation":"Meade, R.H., and Moody, J.A., 2013, Erosional and depositional changes wrought by the flood of May 1978 in the channels of Powder River, southeastern Montana: U.S. Geological Survey Scientific Investigations Report 2013-5035, Report: iv, 29 p.; Map: 46.0 x 42.0 inches, https://doi.org/10.3133/sir20135035.","productDescription":"Report: iv, 29 p.; Map: 46.0 x 42.0 inches","numberOfPages":"36","onlineOnly":"Y","additionalOnlineFiles":"Y","ipdsId":"IP-032505","costCenters":[{"id":435,"text":"National Research Program - Central Region","active":false,"usgs":true}],"links":[{"id":280350,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir20135035.gif"},{"id":280348,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2013/5035/pdf/sir2013-5035.pdf"},{"id":280349,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/sir/2013/5035/pdf/sir2013_plate1.pdf"},{"id":280347,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2013/5035/"}],"scale":"20570","projection":"Universal Transverse Mercator projection","datum":"North American Datum of 1927","country":"United States","state":"Montana","county":"Powder River County","otherGeospatial":"Powder River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.999321,44.993622 ], [ -105.999321,45.501641 ], [ -105.24974,45.501641 ], [ -105.24974,44.993622 ], [ -105.999321,44.993622 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52b172bee4b0d9b3252245e5","contributors":{"authors":[{"text":"Meade, Robert H. 0000-0002-4965-3040 rhmeade@usgs.gov","orcid":"https://orcid.org/0000-0002-4965-3040","contributorId":2744,"corporation":false,"usgs":true,"family":"Meade","given":"Robert","email":"rhmeade@usgs.gov","middleInitial":"H.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":486199,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moody, John A. 0000-0003-2609-364X jamoody@usgs.gov","orcid":"https://orcid.org/0000-0003-2609-364X","contributorId":771,"corporation":false,"usgs":true,"family":"Moody","given":"John","email":"jamoody@usgs.gov","middleInitial":"A.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":486198,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70049030,"text":"sir20135190 - 2013 - Occurrence of methane in groundwater of south-central New York State, 2012-systematic evaluation of a glaciated region by hydrogeologic setting","interactions":[],"lastModifiedDate":"2013-12-16T13:35:48","indexId":"sir20135190","displayToPublicDate":"2013-12-17T08:00:00","publicationYear":"2013","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2013-5190","title":"Occurrence of methane in groundwater of south-central New York State, 2012-systematic evaluation of a glaciated region by hydrogeologic setting","docAbstract":"A survey of methane in groundwater was undertaken to document methane occurrence on the basis hydrogeologic setting within a glaciated 1,810-square-mile area of south-central New York along the Pennsylvania border. Sixty-six wells were sampled during the summer of 2012. All wells were at least 1 mile from any known gas well (active, exploratory, or abandoned). Results indicate strong positive and negative associations between hydrogeologic settings and methane occurrence. The hydrogeologic setting classes are based on topographic position (valley and upland), confinement or non-confinement of groundwater by glacial deposits, well completion in fractured bedrock or sand and gravel, and hydrogeologic subcategories. Only domestic wells and similar purposed supply wells with well-construction and log information were selected for classification. Field water-quality characteristics (pH, specific conductance, dissolved oxygen, and temperature) were measured at each well, and samples were collected and analyzed for dissolved gases, including methane and short-chain hydrocarbons. Carbon and hydrogen isotopic ratios of methane were measured in 21 samples that had at least 0.3 milligram per liter (mg/L) of methane.\n\nResults of sampling indicate that occurrence of methane in groundwater of the region is common—greater than or equal to 0.001 mg/L in 78 percent of the groundwater samples. Concentrations of methane ranged over five orders of magnitude. Methane concentrations at which monitoring or mitigation are indicated (greater than or equal to 10 mg/L) were measured in 15 percent of the samples. Methane concentrations greater than 0.1 mg/L were associated with specific hydrogeologic settings. Wells completed in bedrock within valleys and under confined groundwater conditions were most closely associated with the highest methane concentrations. Fifty-seven percent of valley wells had greater than or equal to 0.1 mg/L of methane, whereas only 10 percent of upland wells equaled or exceeded that concentration. Isotopic signatures differed between these groups as well. Methane in valley wells was predominantly thermogenic in origin, likely as a result of close vertical proximity to underlying methane-bearing saline groundwater and brine and possibly as a result of enhanced bedrock fracture permeability beneath valleys that provides an avenue for upward gas migration. Isotopic signatures of methane from four upland well samples indicated a microbial origin (carbon-dioxide reduction) with one sample possibly altered by microbial methane oxidation. Water samples from wells in a valley setting that indicate a mix of thermogenic and microbial methane reflect the close proximity of regional groundwater flow and underlying saline water and brine in valley areas. The microbial methane is likely produced by bacteria that utilize carbon dioxide or formational organic matter in highly reducing environments within the subregional groundwater flow system. This characterization of groundwater methane shows the importance of subsurface information (hydrogeology, well construction) in understanding methane occurrence and provides an initial conceptual framework that can be utilized in investigation of stray gas in south-central New York.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20135190","usgsCitation":"Heisig, P.M., and Scott, T., 2013, Occurrence of methane in groundwater of south-central New York State, 2012-systematic evaluation of a glaciated region by hydrogeologic setting: U.S. Geological Survey Scientific Investigations Report 2013-5190, Report: vii, 32 p.; 4 Appendices: XLS files, https://doi.org/10.3133/sir20135190.","productDescription":"Report: vii, 32 p.; 4 Appendices: XLS files","numberOfPages":"44","additionalOnlineFiles":"Y","ipdsId":"IP-049514","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":280331,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir20135190.jpg"},{"id":280328,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2013/5190/pdf/sir2013-5190.pdf"},{"id":280330,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/sir/2013/5190/appendix/sir2013-5190_heisig_apend01-04.xlsx"},{"id":280329,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2013/5190/"}],"projection":"Universal Transverse Mercator, Zone 18","country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.4125,42.0025 ], [ -77.4125,42.4601 ], [ -75.3196,42.4601 ], [ -75.3196,42.0025 ], [ -77.4125,42.0025 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52b172c0e4b0d9b3252245fd","contributors":{"authors":[{"text":"Heisig, Paul M. 0000-0003-0338-4970 pmheisig@usgs.gov","orcid":"https://orcid.org/0000-0003-0338-4970","contributorId":793,"corporation":false,"usgs":true,"family":"Heisig","given":"Paul","email":"pmheisig@usgs.gov","middleInitial":"M.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":486052,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, Tia-Marie 0000-0002-5677-0544 tia-mariescott@usgs.gov","orcid":"https://orcid.org/0000-0002-5677-0544","contributorId":5122,"corporation":false,"usgs":true,"family":"Scott","given":"Tia-Marie","email":"tia-mariescott@usgs.gov","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":486053,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70048934,"text":"sim3266 - 2013 - Maps showing thermal maturity of Upper Cretaceous marine shales in the Wind River Basin, Wyoming","interactions":[],"lastModifiedDate":"2013-12-16T16:10:13","indexId":"sim3266","displayToPublicDate":"2013-12-16T15:56:00","publicationYear":"2013","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":333,"text":"Scientific Investigations Map","code":"SIM","onlineIssn":"2329-132X","printIssn":"2329-1311","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"3266","title":"Maps showing thermal maturity of Upper Cretaceous marine shales in the Wind River Basin, Wyoming","docAbstract":"The Wind River Basin is a large Laramide (Late Cretaceous through Eocene) structural and sedimentary basin that encompasses about 7,400 square miles in central Wyoming. The basin is bounded by the Washakie Range, Owl Creek, and southern Bighorn Mountains on the north, the Casper arch on the east and northeast, the Granite Mountains on the south, and the Wind River Range on the west. Important conventional and unconventional oil and gas resources have been discovered and produced from reservoirs ranging in age from Mississippian through Tertiary. It has been suggested that various Upper Cretaceous marine shales are the principal hydrocarbon source rocks for many of these accumulations. Numerous source rock studies of various Upper Cretaceous marine shales throughout the Rocky Mountain region have led to the conclusion that these rocks have generated, or are capable of generating, oil and (or) gas. With recent advances and success in horizontal drilling and multistage fracture stimulation there has been an increase in exploration and completion of wells in these marine shales in other Rocky Mountain Laramide basins that were traditionally thought of only as hydrocarbon source rocks. Important parameters that control hydrocarbon production from shales include: reservoir thickness, amount and type of organic matter, and thermal maturity. The purpose of this report is to present maps and a structural cross section showing levels of thermal maturity, based on vitrinite reflectance (Ro), for Upper Cretaceous marine shales in the Wind River Basin.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sim3266","usgsCitation":"Finn, T.M., and Pawlewicz, M.J., 2013, Maps showing thermal maturity of Upper Cretaceous marine shales in the Wind River Basin, Wyoming: U.S. Geological Survey Scientific Investigations Map 3266, Report: iv, 13 p.; Map: 27.00 inches x 54.25 inches, https://doi.org/10.3133/sim3266.","productDescription":"Report: iv, 13 p.; Map: 27.00 inches x 54.25 inches","onlineOnly":"Y","additionalOnlineFiles":"Y","ipdsId":"IP-041254","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":280345,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sim3266.jpg"},{"id":280344,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/sim/3266/pdf/sim3266_map.pdf"},{"id":280343,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sim/3266/pdf/sim3266.pdf"},{"id":280341,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/3266/"}],"country":"United States","state":"Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.083,41.7016 ], [ -110.083,43.6838 ], [ -106.6223,43.6838 ], [ -106.6223,41.7016 ], [ -110.083,41.7016 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52b0211fe4b0242fceec858b","contributors":{"authors":[{"text":"Finn, Thomas M. 0000-0001-6396-9351 finn@usgs.gov","orcid":"https://orcid.org/0000-0001-6396-9351","contributorId":778,"corporation":false,"usgs":true,"family":"Finn","given":"Thomas","email":"finn@usgs.gov","middleInitial":"M.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":485824,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pawlewicz, Mark J. pawlewicz@usgs.gov","contributorId":752,"corporation":false,"usgs":true,"family":"Pawlewicz","given":"Mark","email":"pawlewicz@usgs.gov","middleInitial":"J.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":485823,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}