{"pageNumber":"803","pageRowStart":"20050","pageSize":"25","recordCount":68925,"records":[{"id":70037049,"text":"70037049 - 2010 - Development of a macrophyte-based index of biotic integrity for Minnesota lakes","interactions":[],"lastModifiedDate":"2012-03-12T17:22:11","indexId":"70037049","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1456,"text":"Ecological Indicators","active":true,"publicationSubtype":{"id":10}},"title":"Development of a macrophyte-based index of biotic integrity for Minnesota lakes","docAbstract":"Traditional approaches for managing aquatic resources have often failed to account for effects of anthropogenic disturbances on biota that are not directly reflected by chemical and physical proxies of environmental condition. The index of biotic integrity (IBI) is a potentially effective assessment method to integrate ecological, functional, and structural aspects of aquatic systems. A macrophyte-based IBI was developed for Minnesota lakes to assess the ability of aquatic plant communities to indicate environmental condition. The index was developed using quantitative point intercept vegetation surveys for 97 lakes that represent a range of limnological and watershed characteristics. We followed an approach similar to that used in Wisconsin to develop the aquatic macrophyte community index (AMCI). Regional adaptation of the AMCI required the identification of species representative of macrophyte communities in Minnesota. Metrics and scaling methods were also substantially modified to produce a more empirically robust index. Regression analyses indicated that IBI scores reflected statewide differences in lake trophic state (R2 = 0.57, F = 130.3, df = 1, 95, p < 0.005), agricultural (R2 = 0.51, F = 83.0, df = 1, 79, p < 0.005), urban (R2 = 0.22, F = 23.0, df = 1, 79, p < 0.005), and forested land uses (R2 = 0.51, F = 84.7, df = 1, 79, p < 0.005), and county population density (R2 = 0.14, F = 16.6, df = 1, 95, p < 0.005). Variance partitioning analyses using multiple regression models indicated a unique response of the IBI to human-induced stress separate from a response to natural lake characteristics. The IBI was minimally affected by differences in sample point density as indicated by Monte Carlo analyses of reduced sampling effort. Our analysis indicates that a macrophyte IBI calibrated for Minnesota lakes could be useful for identifying differences in environmental condition attributed to human-induced stress gradients. ?? 2010 Elsevier Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ecological Indicators","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.ecolind.2010.02.006","issn":"1470160X","usgsCitation":"Beck, M., Hatch, L., Vondracek, B., and Valley, R., 2010, Development of a macrophyte-based index of biotic integrity for Minnesota lakes: Ecological Indicators, v. 10, no. 5, p. 968-979, https://doi.org/10.1016/j.ecolind.2010.02.006.","startPage":"968","endPage":"979","numberOfPages":"12","costCenters":[],"links":[{"id":475924,"rank":10000,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/11299/183538","text":"External Repository"},{"id":217043,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.ecolind.2010.02.006"},{"id":244954,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a003ce4b0c8380cd4f667","contributors":{"authors":[{"text":"Beck, M.W.","contributorId":48004,"corporation":false,"usgs":true,"family":"Beck","given":"M.W.","email":"","affiliations":[],"preferred":false,"id":459149,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hatch, L.K.","contributorId":39615,"corporation":false,"usgs":true,"family":"Hatch","given":"L.K.","email":"","affiliations":[],"preferred":false,"id":459148,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vondracek, B.","contributorId":69930,"corporation":false,"usgs":true,"family":"Vondracek","given":"B.","affiliations":[],"preferred":false,"id":459150,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Valley, R.D.","contributorId":25798,"corporation":false,"usgs":true,"family":"Valley","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":459147,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70037174,"text":"70037174 - 2010 - A new capture fraction method to map how pumpage affects surface water flow","interactions":[],"lastModifiedDate":"2012-03-12T17:22:07","indexId":"70037174","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1861,"text":"Ground Water","active":true,"publicationSubtype":{"id":10}},"title":"A new capture fraction method to map how pumpage affects surface water flow","docAbstract":"All groundwater pumped is balanced by removal of water somewhere, initially from storage in the aquifer and later from capture in the form of increase in recharge and decrease in discharge. Capture that results in a loss of water in streams, rivers, and wetlands now is a concern in many parts of the United States. Hydrologists commonly use analytical and numerical approaches to study temporal variations in sources of water to wells for select points of interest. Much can be learned about coupled surface/groundwater systems, however, by looking at the spatial distribution of theoretical capture for select times of interest. Development of maps of capture requires (1) a reasonably well-constructed transient or steady state model of an aquifer with head-dependent flow boundaries representing surface water features or evapotranspiration and (2) an automated procedure to run the model repeatedly and extract results, each time with a well in a different location. This paper presents new methods for simulating and mapping capture using three-dimensional groundwater flow models and presents examples from Arizona, Oregon, and Michigan. Journal compilation ?? 2010 National Ground Water Association. No claim to original US government works.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ground Water","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1745-6584.2010.00701.x","issn":"0017467X","usgsCitation":"Leake, S.A., Reeves, H.W., and Dickinson, J., 2010, A new capture fraction method to map how pumpage affects surface water flow: Ground Water, v. 48, no. 5, p. 690-700, https://doi.org/10.1111/j.1745-6584.2010.00701.x.","startPage":"690","endPage":"700","numberOfPages":"11","costCenters":[],"links":[{"id":244962,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217051,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1745-6584.2010.00701.x"}],"volume":"48","issue":"5","noUsgsAuthors":false,"publicationDate":"2010-08-19","publicationStatus":"PW","scienceBaseUri":"5059e49de4b0c8380cd4677f","contributors":{"authors":[{"text":"Leake, S. A.","contributorId":52164,"corporation":false,"usgs":true,"family":"Leake","given":"S.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":459734,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reeves, H. W.","contributorId":53739,"corporation":false,"usgs":true,"family":"Reeves","given":"H.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":459735,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dickinson, J.E.","contributorId":28790,"corporation":false,"usgs":true,"family":"Dickinson","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":459733,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70037050,"text":"70037050 - 2010 - Sapflow and water use of freshwater wetland trees exposed to saltwater incursion in a tidally influenced South Carolina watershed","interactions":[],"lastModifiedDate":"2016-11-30T11:38:45","indexId":"70037050","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1170,"text":"Canadian Journal of Forest Research","active":true,"publicationSubtype":{"id":10}},"title":"Sapflow and water use of freshwater wetland trees exposed to saltwater incursion in a tidally influenced South Carolina watershed","docAbstract":"Sea-level rise and anthropogenic activity promote salinity incursion into many tidal freshwater forested wetlands. Interestingly, individual trees can persist for decades after salt impact. To understand why, we documented sapflow (J<sub>s</sub>), reduction in J<sub>s</sub> with sapwood depth, and water use (F) of baldcypress (Taxodium distichum (L.) Rich.) trees undergoing exposure to salinity. The mean J<sub>s</sub> of individual trees was reduced by 2.8 g H<sub>2</sub>O??m<sup>-2</sup>??s<sup>-1</sup> (or by 18%) in the outer sapwood on a saline site versus a freshwater site; however, the smallest trees, present only on the saline site, also registered the lowest J<sub>s</sub>. Hence, tree size significantly influenced the overall site effect on J<sub>s</sub>. Trees undergoing perennial exposure to salt used greater relative amounts of water in outer sapwood than in inner sapwood depths, which identifies a potentially different strategy for baldcypress trees coping with saline site conditions over decades. Overall, individual trees used 100 kg H<sub>2</sub>O??day<sup>-1</sup> on a site that remained relatively fresh versus 23.9 kg H<sub>2</sub>O??day<sup>-1</sup> on the saline site. We surmise that perennial salinization of coastal freshwater forests forces shifts in individual-tree osmotic balance and water-use strategy to extend survival time on suboptimal sites, which further influences growth and morphology.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Canadian Journal of Forest Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1139/x09-204","issn":"00455067","usgsCitation":"Krauss, K., and Duberstein, J., 2010, Sapflow and water use of freshwater wetland trees exposed to saltwater incursion in a tidally influenced South Carolina watershed: Canadian Journal of Forest Research, v. 40, no. 3, p. 525-535, https://doi.org/10.1139/x09-204.","startPage":"525","endPage":"535","numberOfPages":"11","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":244985,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217073,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1139/x09-204"}],"country":"United States","state":"South Carolina","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.2879867553711,\n              33.25246979589199\n            ],\n            [\n              -79.2879867553711,\n              33.40221152741838\n            ],\n            [\n              -79.1400146484375,\n              33.40221152741838\n            ],\n            [\n              -79.1400146484375,\n              33.25246979589199\n            ],\n            [\n              -79.2879867553711,\n              33.25246979589199\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"40","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b86bee4b08c986b3160e4","contributors":{"authors":[{"text":"Krauss, K. W. 0000-0003-2195-0729","orcid":"https://orcid.org/0000-0003-2195-0729","contributorId":19517,"corporation":false,"usgs":true,"family":"Krauss","given":"K. W.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":459151,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Duberstein, J.A.","contributorId":44381,"corporation":false,"usgs":true,"family":"Duberstein","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":459152,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70033972,"text":"70033972 - 2010 - Decadal-timescale estuarine geomorphic change under future scenarios of climate and sediment supply","interactions":[],"lastModifiedDate":"2018-09-18T09:53:44","indexId":"70033972","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1584,"text":"Estuaries and Coasts","active":true,"publicationSubtype":{"id":10}},"title":"Decadal-timescale estuarine geomorphic change under future scenarios of climate and sediment supply","docAbstract":"Future estuarine geomorphic change, in response to climate change, sea-level rise, and watershed sediment supply, may govern ecological function, navigation, and water quality. We estimated geomorphic changes in Suisun Bay, CA, under four scenarios using a tidal-timescale hydrodynamic/sediment transport model. Computational expense and data needs were reduced using the morphological hydrograph concept and the morphological acceleration factor. The four scenarios included (1) present-day conditions; (2) sea-level rise and freshwater flow changes of 2030; (3) sea-level rise and decreased watershed sediment supply of 2030; and (4) sea-level rise, freshwater flow changes, and decreased watershed sediment supply of 2030. Sea-level rise increased water levels thereby reducing wave-induced bottom shear stress and sediment redistribution during the wind-wave season. Decreased watershed sediment supply reduced net deposition within the estuary, while minor changes in freshwater flow timing and magnitude induced the smallest overall effect. In all future scenarios, net deposition in the entire estuary and in the shallowest areas did not keep pace with sea-level rise, suggesting that intertidal and wetland areas may struggle to maintain elevation. Tidal-timescale simulations using future conditions were also used to infer changes in optical depth: though sea-level rise acts to decrease mean light irradiance, decreased suspended-sediment concentrations increase irradiance, yielding small changes in optical depth. The modeling results also assisted with the development of a dimensionless estuarine geomorphic number representing the ratio of potential sediment import forces to sediment export forces; we found the number to be linearly related to relative geomorphic change in Suisun Bay. The methods implemented here are widely applicable to evaluating future scenarios of estuarine change over decadal timescales. ?? The Author(s) 2009.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Estuaries and Coasts","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s12237-009-9244-y","issn":"15592723","usgsCitation":"Ganju, N., and Schoellhamer, D., 2010, Decadal-timescale estuarine geomorphic change under future scenarios of climate and sediment supply: Estuaries and Coasts, v. 33, no. 1, p. 15-29, https://doi.org/10.1007/s12237-009-9244-y.","startPage":"15","endPage":"29","numberOfPages":"15","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":475812,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1007/s12237-009-9244-y","text":"Publisher Index Page"},{"id":244760,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":216862,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/s12237-009-9244-y"}],"volume":"33","issue":"1","noUsgsAuthors":false,"publicationDate":"2009-12-19","publicationStatus":"PW","scienceBaseUri":"5059fe01e4b0c8380cd4ea75","contributors":{"authors":[{"text":"Ganju, N. K. 0000-0002-1096-0465","orcid":"https://orcid.org/0000-0002-1096-0465","contributorId":64782,"corporation":false,"usgs":true,"family":"Ganju","given":"N. K.","affiliations":[],"preferred":false,"id":443462,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schoellhamer, D. H. 0000-0001-9488-7340","orcid":"https://orcid.org/0000-0001-9488-7340","contributorId":85624,"corporation":false,"usgs":true,"family":"Schoellhamer","given":"D. H.","affiliations":[],"preferred":false,"id":443463,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70037028,"text":"70037028 - 2010 - Fate of trace organic compounds during vadose zone soil treatment in an onsite wastewater system","interactions":[],"lastModifiedDate":"2018-10-10T10:31:11","indexId":"70037028","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","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":"Fate of trace organic compounds during vadose zone soil treatment in an onsite wastewater system","docAbstract":"<p>During onsite wastewater treatment, trace organic compounds are often present in the effluents applied to subsurface soils for advanced treatment during vadose zone percolation and groundwater recharge. The fate of the endocrine-disrupting surfactant metabolites 4-nonylphenol (NP), 4-nonylphenolmonoethoxylate (NP1EO), and 4-nonylphenolmonoethoxycarboxylate (NP1EC), metal-chelating agents ethylenediaminetetraacetic acid (EDTA) and nitrilotriacetic acid (NTA), antimicrobial agent triclosan, stimulant caffeine, and antibiotic sulfamethoxazole during transport through an unsaturated sandy loam soil was studied at a field-scale test site. To assess the effects of effluent quality and hydraulic loading rate (HLR) on compound fate in the soil profile, two effluents (septic tank or textile biofilter) were applied at two design HLRs (2 or 8 cm/d). Chemical concentrations were determined in the two effluents and soil pore water at 60, 120, and 240 cm below the soil infiltrative surface. Concentrations of trace organic compounds in septic tank effluent were reduced by more than 90% during transport through 240 cm (often within 60 cm) of soil, likely due to sorption and biotransformation. However, the concentration of NP increased with depth in the shallow soil profile. Additional treatment of anaerobic septic tank effluent with an aerobic textile biofilter reduced effluent concentrations of many compounds, but generally did not affect any changes in pore water concentrations. The soil profile receiving septic tank effluent (vs. textile biofilter effluent) generally had greater percent removal efficiencies. EDTA, NP, NP1EC, and sulfamethoxazole were measured in soil pore water, indicating the ability of some trace organic compounds to reach shallow groundwater. Risk is highly dependent on the degree of further treatment in the saturated zone and the types and proximity of uses for the receiving groundwater environment.</p>","language":"English","publisher":"Society of Environmental Toxicology and Chemistry","doi":"10.1002/etc.40","issn":"07307268","usgsCitation":"Conn, K., Siegrist, R., Barber, L.B., and Meyer, M.T., 2010, Fate of trace organic compounds during vadose zone soil treatment in an onsite wastewater system: Environmental Toxicology and Chemistry, v. 29, no. 2, p. 285-293, https://doi.org/10.1002/etc.40.","productDescription":"9 p.","startPage":"285","endPage":"293","numberOfPages":"9","ipdsId":"IP-012835","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"links":[{"id":487208,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1002/etc.40","text":"Publisher Index Page"},{"id":245109,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217187,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1002/etc.40"}],"volume":"29","issue":"2","noUsgsAuthors":false,"publicationDate":"2009-10-08","publicationStatus":"PW","scienceBaseUri":"505a0f14e4b0c8380cd53757","contributors":{"authors":[{"text":"Conn, K.E.","contributorId":64433,"corporation":false,"usgs":true,"family":"Conn","given":"K.E.","email":"","affiliations":[],"preferred":false,"id":459040,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Siegrist, R.L.","contributorId":54005,"corporation":false,"usgs":true,"family":"Siegrist","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":459039,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barber, Larry B. 0000-0002-0561-0831 lbbarber@usgs.gov","orcid":"https://orcid.org/0000-0002-0561-0831","contributorId":921,"corporation":false,"usgs":true,"family":"Barber","given":"Larry","email":"lbbarber@usgs.gov","middleInitial":"B.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":459041,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Meyer, Michael T. 0000-0001-6006-7985 mmeyer@usgs.gov","orcid":"https://orcid.org/0000-0001-6006-7985","contributorId":866,"corporation":false,"usgs":true,"family":"Meyer","given":"Michael","email":"mmeyer@usgs.gov","middleInitial":"T.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":true,"id":459042,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70034258,"text":"70034258 - 2010 - Sources of suspended-sediment flux in streams of the chesapeake bay watershed: A regional application of the sparrow model","interactions":[],"lastModifiedDate":"2012-03-12T17:21:46","indexId":"70034258","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2529,"text":"Journal of the American Water Resources Association","active":true,"publicationSubtype":{"id":10}},"title":"Sources of suspended-sediment flux in streams of the chesapeake bay watershed: A regional application of the sparrow model","docAbstract":"We describe the sources and transport of fluvial suspended sediment in nontidal streams of the Chesapeake Bay watershed and vicinity. We applied SPAtially Referenced Regressions on Watershed attributes, which spatially correlates estimated mean annual flux of suspended sediment in nontidal streams with sources of suspended sediment and transport factors. According to our model, urban development generates on average the greatest amount of suspended sediment per unit area (3,928 Mg/km2/year), although agriculture is much more widespread and is the greatest overall source of suspended sediment (57 Mg/km2/year). Factors affecting sediment transport from uplands to streams include mean basin slope, reservoirs, physiography, and soil permeability. On average, 59% of upland suspended sediment generated is temporarily stored along large rivers draining the Coastal Plain or in reservoirs throughout the watershed. Applying erosion and sediment controls from agriculture and urban development in areas of the northern Piedmont close to the upper Bay, where the combined effects of watershed characteristics on sediment transport have the greatest influence may be most helpful in mitigating sedimentation in the bay and its tributaries. Stream restoration efforts addressing floodplain and bank stabilization and incision may be more effective in smaller, headwater streams outside of the Coastal Plain. ?? 2010 American Water Resources Association. No claim to original U.S. government works.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the American Water Resources Association","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1752-1688.2010.00450.x","issn":"1093474X","usgsCitation":"Brakebill, J., Ator, S., and Schwarz, G., 2010, Sources of suspended-sediment flux in streams of the chesapeake bay watershed: A regional application of the sparrow model: Journal of the American Water Resources Association, v. 46, no. 4, p. 757-776, https://doi.org/10.1111/j.1752-1688.2010.00450.x.","startPage":"757","endPage":"776","numberOfPages":"20","costCenters":[],"links":[{"id":475988,"rank":10000,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1752-1688.2010.00450.x","text":"Publisher Index Page"},{"id":216764,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1752-1688.2010.00450.x"},{"id":244651,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-07-26","publicationStatus":"PW","scienceBaseUri":"505b9394e4b08c986b31a58c","contributors":{"authors":[{"text":"Brakebill, J. W.","contributorId":48206,"corporation":false,"usgs":true,"family":"Brakebill","given":"J. W.","affiliations":[],"preferred":false,"id":444951,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ator, S.W. 0000-0002-9186-4837","orcid":"https://orcid.org/0000-0002-9186-4837","contributorId":104100,"corporation":false,"usgs":true,"family":"Ator","given":"S.W.","affiliations":[],"preferred":false,"id":444952,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schwarz, G. E. 0000-0002-9239-4566","orcid":"https://orcid.org/0000-0002-9239-4566","contributorId":14852,"corporation":false,"usgs":true,"family":"Schwarz","given":"G. E.","affiliations":[],"preferred":false,"id":444950,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70036480,"text":"70036480 - 2010 - Effects of coalbed natural gas development on fish assemblages in tributary streams of the Powder and Tongue rivers","interactions":[],"lastModifiedDate":"2012-03-12T17:22:04","indexId":"70036480","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1696,"text":"Freshwater Biology","active":true,"publicationSubtype":{"id":10}},"title":"Effects of coalbed natural gas development on fish assemblages in tributary streams of the Powder and Tongue rivers","docAbstract":"1. Extraction of coalbed natural gas (CBNG) often results in disposal of large quantities of CBNG product water, which may affect aquatic ecosystems. We evaluated the effects of CBNG development on fish assemblages in tributary streams of the Powder and Tongue rivers. We used treatment and control, impact versus reference sites comparisons, surveys of CBNG product-water streams and in situ fish survival approaches to determine if CBNG development affected fish assemblages.2. Several of our results suggested that CBNG development did not affect fish assemblages. Species richness and index of biotic integrity (IBI) scores were similar in streams with and streams without CBNG development, and overall biotic integrity was not related to the number or density of CBNG wells. Fish occurred in one stream that was composed largely or entirely of CBNG product water. Sentinel fish survived in cages at treatment sites where no or few fish were captured, suggesting that factors such as lack of stream connectivity rather than water quality limited fish abundance at these sites. Fish species richness did not differ significantly from 1994 to 2006 in comparisons of CBNG-developed and undeveloped streams. Biotic integrity declined from 1994 to 2006; however, declines occurred at both impact and reference sites, possibly because of long-term drought.3. Some evidence suggested that CBNG development negatively affected fish assemblages, or may do so over time. Specific conductivity was on average higher in treatment streams and was negatively related to biotic integrity. Four IBI species richness metrics were negatively correlated with the number or density of CBNG wells in the catchment above sampling sites. Bicarbonate, one of the primary ions in product water, was significantly higher in developed streams and may have limited abundance of longnose dace (Rhinichthys cataractae). Total dissolved solids, alkalinity, magnesium and sulphate were significantly higher in developed streams.4. Biological monitoring conducted before the development of CBNG, and continuing through the life of development and reclamation, together with data on the quantity, quality and fate of CBNG product water will allow robust assessment of potential effects of future CBNG development worldwide. ?? 2010 Blackwell Publishing Ltd.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Freshwater Biology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1365-2427.2010.02480.x","issn":"00465070","usgsCitation":"Davis, W., Bramblett, R., and Zale, A., 2010, Effects of coalbed natural gas development on fish assemblages in tributary streams of the Powder and Tongue rivers: Freshwater Biology, v. 55, no. 12, p. 2612-2625, https://doi.org/10.1111/j.1365-2427.2010.02480.x.","startPage":"2612","endPage":"2625","numberOfPages":"14","costCenters":[],"links":[{"id":218264,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1365-2427.2010.02480.x"},{"id":246260,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"55","issue":"12","noUsgsAuthors":false,"publicationDate":"2010-08-24","publicationStatus":"PW","scienceBaseUri":"505a06b6e4b0c8380cd513ab","contributors":{"authors":[{"text":"Davis, W.N.","contributorId":107543,"corporation":false,"usgs":true,"family":"Davis","given":"W.N.","email":"","affiliations":[],"preferred":false,"id":456344,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bramblett, R.G.","contributorId":76576,"corporation":false,"usgs":true,"family":"Bramblett","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":456343,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zale, A.V.","contributorId":15793,"corporation":false,"usgs":true,"family":"Zale","given":"A.V.","affiliations":[],"preferred":false,"id":456342,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70154833,"text":"70154833 - 2010 - Factors associated with mortality of walleyes and saugers caught in live-release tournaments","interactions":[],"lastModifiedDate":"2021-04-02T15:31:29.733098","indexId":"70154833","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Factors associated with mortality of walleyes and saugers caught in live-release tournaments","docAbstract":"<p><span>We measured the initial mortality (fish judged nonreleasable at weigh-in), prerelease mortality (fish judged nonreleasable 1&ndash;2 h after weigh-in [which includes initial mortality]), and postrelease mortality (fish that died during a 5-d retention in net-pens) in 14 live-release tournaments for walleye&nbsp;</span><i>Sander vitreus</i><span>&nbsp;conducted in April&ndash;October 2006 and April&ndash;July 2007 in lakes and rivers in Michigan, Minnesota, North Dakota, South Dakota, and Wisconsin. Among the 14 events, initial mortality was 0&ndash;28%, prerelease mortality was 3&ndash;54%, and postrelease mortality was 0&ndash;100%; the mortality of reference fish (walleyes &ge;31 cm long that were captured by electrofishing and held in net-pens with tournament-caught walleyes to measure postrelease mortality) was 0&ndash;97%. Mortality was generally low in events conducted when water temperatures were below 14&deg;C but substantially higher in events when water temperatures were above 18&deg;C. The mortality of reference fish suggests that capture by electrofishing and minimal handling when the water temperature exceeds 19&deg;C results in high mortality of walleyes that is largely the result of the thermal conditions immediately after capture. Mortality was not related to the size of the tournaments (number of boats), the total number or weight of walleyes weighed in, or the mean number or weight of walleyes weighed in per boat. Mortality was positively related to the depth at which walleyes were caught and the live-well temperature and negatively related to the live-well dissolved oxygen concentration. Surface water temperature was the best predictor of mortality, and models were developed to predict the probability of prerelease and postrelease mortality of 10, 20, and 30% or less of tournament-caught walleyes due to water temperature.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/M09-003.1","usgsCitation":"Schramm, H., Vondracek, B.C., French, W.E., and Gerard, P., 2010, Factors associated with mortality of walleyes and saugers caught in live-release tournaments: North American Journal of Fisheries Management, v. 30, no. 1, p. 238-253, https://doi.org/10.1577/M09-003.1.","productDescription":"16 p.","startPage":"238","endPage":"253","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-011354","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"links":[{"id":475826,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/11299/183646","text":"External 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Atlanta","active":true,"usgs":true}],"preferred":false,"id":564247,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vondracek, Bruce C. bcv@usgs.gov","contributorId":904,"corporation":false,"usgs":true,"family":"Vondracek","given":"Bruce","email":"bcv@usgs.gov","middleInitial":"C.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":568233,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"French, William E.","contributorId":97355,"corporation":false,"usgs":true,"family":"French","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":568234,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gerard, Patrick D.","contributorId":140181,"corporation":false,"usgs":false,"family":"Gerard","given":"Patrick D.","affiliations":[{"id":7084,"text":"Clemson University","active":true,"usgs":false}],"preferred":false,"id":568235,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70037165,"text":"70037165 - 2010 - Environmental tolerance of an invasive riparian tree and its potential for continued spread in the southwestern US","interactions":[],"lastModifiedDate":"2012-03-12T17:22:10","indexId":"70037165","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2490,"text":"Journal of Vegetation Science","active":true,"publicationSubtype":{"id":10}},"title":"Environmental tolerance of an invasive riparian tree and its potential for continued spread in the southwestern US","docAbstract":"Questions: Exotic plant invasion may be aided by facilitation and broad tolerance of environmental conditions, yet these processes are poorly understood in species-rich ecosystems such as riparian zones. In the southwestern United States (US) two plant species have invaded riparian zones: tamarisk (Tamarix ramosissima, T. chinensis, and their hybrids) and Russian olive (Elaeagnus angustifolia). We addressed the following questions: (1) is Russian olive able to tolerate drier and shadier conditions than cottonwood and tamarisk? (2) Can tamarisk and cottonwood facilitate Russian olive invasion? Location: Arid riparian zones, southwestern US. Methods: We analyzed riparian tree seedling requirements in a controlled experiment, performed empirical field studies, and analyzed stable oxygen isotopes to determine the water sources used by Russian olive. Results: Russian olive survival was significantly higher in dense shade and low moisture conditions than tamarisk and cottonwood. Field observations indicated Russian olive established where flooding cannot occur, and under dense canopies of tamarisk, cottonwood, and Russian olive. Tamarisk and native riparian plant species seedlings cannot establish in these dry, shaded habitats. Russian olive can rely on upper soil water until 15 years of age, before utilizing groundwater. Conclusions: We demonstrate that even though there is little evidence of facilitation by cottonwood and tamarisk, Russian olive is able to tolerate dense shade and low moisture conditions better than tamarisk and cottonwood. There is great potential for continued spread of Russian olive throughout the southwestern US because large areas of suitable habitat exist that are not yet inhabited by this species. ?? 2010 International Association for Vegetation Science.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Vegetation Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1111/j.1654-1103.2010.01179.x","issn":"11009233","usgsCitation":"Reynolds, L., and Cooper, D., 2010, Environmental tolerance of an invasive riparian tree and its potential for continued spread in the southwestern US: Journal of Vegetation Science, v. 21, no. 4, p. 733-743, https://doi.org/10.1111/j.1654-1103.2010.01179.x.","startPage":"733","endPage":"743","numberOfPages":"11","costCenters":[],"links":[{"id":245311,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217367,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1654-1103.2010.01179.x"}],"volume":"21","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a09eae4b0c8380cd520f1","contributors":{"authors":[{"text":"Reynolds, L.V.","contributorId":56482,"corporation":false,"usgs":true,"family":"Reynolds","given":"L.V.","email":"","affiliations":[],"preferred":false,"id":459685,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooper, D.J.","contributorId":89489,"corporation":false,"usgs":true,"family":"Cooper","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":459686,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70035295,"text":"70035295 - 2010 - Predicting the retreat and migration of tidal forests along the northern Gulf of Mexico under sea-level rise","interactions":[],"lastModifiedDate":"2020-01-09T15:29:31","indexId":"70035295","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1687,"text":"Forest Ecology and Management","active":true,"publicationSubtype":{"id":10}},"title":"Predicting the retreat and migration of tidal forests along the northern Gulf of Mexico under sea-level rise","docAbstract":"Tidal freshwater forests in coastal regions of the southeastern United States are undergoing dieback and retreat from increasing tidal inundation and saltwater intrusion attributed to climate variability and sea-level rise. In many areas, tidal saltwater forests (mangroves) contrastingly are expanding landward in subtropical coastal reaches succeeding freshwater marsh and forest zones. Hydrological characteristics of these low-relief coastal forests in intertidal settings are dictated by the influence of tidal and freshwater forcing. In this paper, we describe the application of the Sea Level Over Proportional Elevation (SLOPE) model to predict coastal forest retreat and migration from projected sea-level rise based on a proxy relationship of saltmarsh/mangrove area and tidal range. The SLOPE model assumes that the sum area of saltmarsh/mangrove habitat along any given coastal reach is determined by the slope of the landform and vertical tide forcing. Model results indicated that saltmarsh and mangrove migration from sea-level rise will vary by county and watershed but greater in western Gulf States than in the eastern Gulf States where millions of hectares of coastal forest will be displaced over the next century with a near meter rise in relative sea level alone. Substantial losses of coastal forests will also occur in the eastern Gulf but mangrove forests in subtropical zones of Florida are expected to replace retreating freshwater forest and affect regional biodiversity. Accelerated global eustacy from climate change will compound the degree of predicted retreat and migration of coastal forests with expected implications for ecosystem management of State and Federal lands in the absence of adaptive coastal management.","language":"English","publisher":"Elsevier","doi":"10.1016/j.foreco.2009.10.023","issn":"03781127","usgsCitation":"Doyle, T., Krauss, K., Conner, W., and From, A., 2010, Predicting the retreat and migration of tidal forests along the northern Gulf of Mexico under sea-level rise: Forest Ecology and Management, v. 259, no. 4, p. 770-777, https://doi.org/10.1016/j.foreco.2009.10.023.","productDescription":"8 p.","startPage":"770","endPage":"777","numberOfPages":"8","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":242936,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alabama, Florida, Louisiana, Mississippi, Texas","otherGeospatial":"Gulf of Mexico","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.8154296875,\n              25.284437746983055\n            ],\n            [\n              -83.232421875,\n              30.259067203213018\n            ],\n            [\n              -84.814453125,\n              30.41078179084589\n            ],\n            [\n              -88.681640625,\n              30.751277776257812\n            ],\n            [\n              -91.1865234375,\n              30.107117887092357\n            ],\n            [\n              -94.9658203125,\n              29.954934549656144\n            ],\n            [\n              -98.1298828125,\n              27.761329874505233\n            ],\n            [\n              -97.2509765625,\n              25.878994400196202\n            ],\n            [\n              -80.8154296875,\n              25.284437746983055\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"259","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a81d8e4b0c8380cd7b781","contributors":{"authors":[{"text":"Doyle, T.W. 0000-0001-5754-0671","orcid":"https://orcid.org/0000-0001-5754-0671","contributorId":16783,"corporation":false,"usgs":true,"family":"Doyle","given":"T.W.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":450059,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krauss, K. W. 0000-0003-2195-0729","orcid":"https://orcid.org/0000-0003-2195-0729","contributorId":19517,"corporation":false,"usgs":true,"family":"Krauss","given":"K. W.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":450060,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Conner, W.H.","contributorId":54165,"corporation":false,"usgs":true,"family":"Conner","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":450062,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"From, A.S. 0000-0002-6543-2627","orcid":"https://orcid.org/0000-0002-6543-2627","contributorId":34346,"corporation":false,"usgs":true,"family":"From","given":"A.S.","affiliations":[],"preferred":false,"id":450061,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70035207,"text":"70035207 - 2010 - Early viral replication and induced or constitutive immunity in rainbow trout families with differential resistance to Infectious hematopoietic necrosis virus (IHNV)","interactions":[],"lastModifiedDate":"2013-05-07T09:52:59","indexId":"70035207","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1653,"text":"Fish and Shellfish Immunology","active":true,"publicationSubtype":{"id":10}},"title":"Early viral replication and induced or constitutive immunity in rainbow trout families with differential resistance to Infectious hematopoietic necrosis virus (IHNV)","docAbstract":"The main objective of this study was to assess correlates of innate resistance in rainbow trout full-sibling families that differ in susceptibility to Infectious hematopoietic necrosis virus (IHNV). As part of a commercial breeding program, full-sibling families were challenged with IHNV by waterborne exposure at the 1 g size to determine susceptibility to IHNV. Progeny from select families (N = 7 families) that varied in susceptibility (ranging from 32 to 90% cumulative percent mortality (CPM)) were challenged again at the 10 g size by intra-peritoneal injection and overall mortality, early viral replication and immune responses were evaluated. Mortality challenges included 20–40 fish per family while viral replication and immune response studies included 6 fish per family at each time point (24, 48 and 72 h post-infection (hpi)). CPM at the 1 g size was significantly correlated with CPM at the 10 g size, indicating that inherent resistance was a stable trait irrespective of size. In the larger fish, viral load was measured by quantitative reverse-transcriptase PCR in the anterior kidney and was a significant predictor of family disease outcome at 48 hpi. Type I interferon (IFN) transcript levels were significantly correlated with an individual's viral load at 48 and 72 hpi, while type II IFN gene expression was significantly correlated with an individual's viral load at 24 and 48 hpi. Mean family type I but not type II IFN gene expression was weakly associated with susceptibility at 72 hpi. There was no association between mean family susceptibility and the constitutive expression of a range of innate immune genes (e.g. type I and II IFN pathway genes, cytokine and viral recognition receptor genes). The majority of survivors from the challenge had detectable serum neutralizing antibody titers but no trend was observed among families. This result suggests that even the most resistant families experienced sufficient levels of viral replication to trigger specific immunity. In summary, disease outcome for each family was determined very early in the infection process and resistance was associated with lower early viral replication.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Fish and Shellfish Immunology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/j.fsi.2009.10.005","issn":"10504648","usgsCitation":"Purcell, M.K., LaPatra, S., Woodson, J., Kurath, G., and Winton, J., 2010, Early viral replication and induced or constitutive immunity in rainbow trout families with differential resistance to Infectious hematopoietic necrosis virus (IHNV): Fish and Shellfish Immunology, v. 28, no. 1, p. 98-105, https://doi.org/10.1016/j.fsi.2009.10.005.","productDescription":"8 p.","startPage":"98","endPage":"105","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":215302,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.fsi.2009.10.005"},{"id":243097,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0493e4b0c8380cd50a7d","contributors":{"authors":[{"text":"Purcell, M. K.","contributorId":78464,"corporation":false,"usgs":true,"family":"Purcell","given":"M.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":449726,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LaPatra, S. E.","contributorId":55371,"corporation":false,"usgs":false,"family":"LaPatra","given":"S. E.","affiliations":[],"preferred":false,"id":449724,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Woodson, J.C.","contributorId":58477,"corporation":false,"usgs":true,"family":"Woodson","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":449725,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kurath, Gael 0000-0003-3294-560X gkurath@usgs.gov","orcid":"https://orcid.org/0000-0003-3294-560X","contributorId":100522,"corporation":false,"usgs":true,"family":"Kurath","given":"Gael","email":"gkurath@usgs.gov","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":449728,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Winton, J. R. 0000-0002-3505-5509","orcid":"https://orcid.org/0000-0002-3505-5509","contributorId":82441,"corporation":false,"usgs":true,"family":"Winton","given":"J. R.","affiliations":[],"preferred":false,"id":449727,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70033887,"text":"70033887 - 2010 - Incubating rainbow trout in soft water increased their later sensitivity to cadmium and zinc","interactions":[],"lastModifiedDate":"2016-10-19T15:40:23","indexId":"70033887","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3728,"text":"Water, Air, & Soil Pollution","onlineIssn":"1573-2932","printIssn":"0049-6979","active":true,"publicationSubtype":{"id":10}},"title":"Incubating rainbow trout in soft water increased their later sensitivity to cadmium and zinc","docAbstract":"<p>Water hardness is well known to affect the toxicity of some metals; however, reports on the influence of hardness during incubation or acclimation on later toxicity to metals have been conflicting. We incubated rainbow trout (<i class=\"EmphasisTypeItalic \">Oncorhynchus mykiss</i>) near the confluence of two streams, one with soft water and one with very-soft water (average incubation hardnesses of about 21 and 11&nbsp;mg/L as CaCO<sub>3</sub>, respectively). After developing to the swim-up stage, the fish were exposed for 96-h to a mixture of cadmium (Cd) and zinc (Zn) in water with a hardness of 27&nbsp;mg/L as CaCO<sub>3</sub>. The fish incubated in the higher hardness water were about two times more resistant than the fish incubated in the extremely soft water. This difference was similar or greater than the difference that would have been predicted by criteria hardness equations had the fish been tested in the different acclimation waters. We think it is plausible that the energy demands for fish to maintain homeostasis in the lower hardness water make the fish more sensitive to metals that inhibit ionoregulation such as Cd and Zn. We suggest that if important decisions were to be based upon test results, assumptions of adequate hardness acclimation should be carefully considered and short acclimation periods avoided. If practical, incubating rainbow trout in the control waters to be tested may reduce uncertainties in the possible influences of differing rearing water hardness on the test results.</p>","language":"English","publisher":"Kluwer Academic Publishers","doi":"10.1007/s11270-009-0070-4","issn":"00496979","usgsCitation":"Mebane, C.A., Hennessy, D.P., and Dillon, F.S., 2010, Incubating rainbow trout in soft water increased their later sensitivity to cadmium and zinc: Water, Air, & Soil Pollution, v. 205, no. 1-4, p. 245-250, https://doi.org/10.1007/s11270-009-0070-4.","productDescription":"6 p.","startPage":"245","endPage":"250","costCenters":[],"links":[{"id":241877,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"205","issue":"1-4","noUsgsAuthors":false,"publicationDate":"2009-04-29","publicationStatus":"PW","scienceBaseUri":"505a3a0be4b0c8380cd61b1c","contributors":{"authors":[{"text":"Mebane, Christopher A. 0000-0002-9089-0267 cmebane@usgs.gov","orcid":"https://orcid.org/0000-0002-9089-0267","contributorId":110,"corporation":false,"usgs":true,"family":"Mebane","given":"Christopher","email":"cmebane@usgs.gov","middleInitial":"A.","affiliations":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"preferred":true,"id":443025,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hennessy, Daniel P.","contributorId":44782,"corporation":false,"usgs":true,"family":"Hennessy","given":"Daniel","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":443023,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dillon, Frank S.","contributorId":81740,"corporation":false,"usgs":true,"family":"Dillon","given":"Frank","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":443024,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70033824,"text":"70033824 - 2010 - Geologie study off gravels of the Agua Fria River, Phoenix, AZ","interactions":[],"lastModifiedDate":"2013-02-13T09:25:55","indexId":"70033824","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2755,"text":"Mining Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Geologie study off gravels of the Agua Fria River, Phoenix, AZ","docAbstract":"The annual consumption of sand and gravel aggregate in 2006 in the Phoenix, AZ metropolitan area was about 76 Mt (84 million st) (USGS, 2009), or about 18 t (20 st) per capita. Quaternary alluvial deposits in the modern stream channel of the Agua Fria River west of Phoenix are mined and processed to provide some of this aggregate to the greater Phoenix area. The Agua Fria drainage basin (Fig. 1) is characterized by rugged mountains with high elevations and steep stream gradients in the north, and by broad alluvial filled basins separated by elongated faultblock mountain ranges in the south. The Agua Fria River, the basin’s main drainage, flows south from Prescott, AZ and west of Phoenix to the Gila River. The Waddel Dam impounds Lake Pleasant and greatly limits the flow of the Agua Fria River south of the lake. The southern portion of the watershed, south of Lake Pleasant, opens out into a broad valley where the river flows through urban and agricultural lands to its confluence with the Gila River, a tributary of the Colorado River.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Mining Engineering","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society for Mining, Metallurgy and Exploration","issn":"00265187","usgsCitation":"Langer, W.H., Dewitt, E., Adams, D., and O’Briens, T., 2010, Geologie study off gravels of the Agua Fria River, Phoenix, AZ: Mining Engineering, v. 62, no. 2, p. 27-31.","startPage":"27","endPage":"31","numberOfPages":"5","costCenters":[],"links":[{"id":241907,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267311,"type":{"id":15,"text":"Index Page"},"url":"https://me.smenet.org/abstract.cfm?preview=1&articleID=490&page=27"}],"volume":"62","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2287e4b0c8380cd57118","contributors":{"authors":[{"text":"Langer, W. H.","contributorId":44932,"corporation":false,"usgs":true,"family":"Langer","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":442711,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dewitt, E.","contributorId":108257,"corporation":false,"usgs":true,"family":"Dewitt","given":"E.","email":"","affiliations":[],"preferred":false,"id":442713,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Adams, D.T.","contributorId":44439,"corporation":false,"usgs":true,"family":"Adams","given":"D.T.","email":"","affiliations":[],"preferred":false,"id":442710,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"O’Briens, T.","contributorId":99020,"corporation":false,"usgs":true,"family":"O’Briens","given":"T.","email":"","affiliations":[],"preferred":false,"id":442712,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70178483,"text":"70178483 - 2010 - Post-construction monitoring of a Core-Loc™ breakwater using tripod-based LiDAR","interactions":[],"lastModifiedDate":"2017-01-20T10:59:44","indexId":"70178483","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Post-construction monitoring of a Core-Loc™ breakwater using tripod-based LiDAR","docAbstract":"<p>The goal of the technology application described herein is to determine whether breakwater monitoring data collected using Tripod (or Terrestrial) Light Detection and Ranging (T-LiDAR) can give insight into processes such as how Core-Loc™ concrete armour units nest following construction, and in turn how settlement affects armour layer stability, concrete cap performance, and armour unit breakage. &nbsp;A further objective is that this information can then be incorporated into the design of future projects using concrete armour units. &nbsp;The results of this application of T-LiDAR, including the challenges encountered and the conclusions drawn regarding initial concrete armour unit movement will be presented in this paper.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Coasts, marine structures and breakwaters: Adapting to change","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Thomas Telford Limitied","doi":"10.1680/cmsb.41301.0039","usgsCitation":"Podoski, J.H., Bawden, G.W., Bond, S., Smith, T.D., and Foster, J., 2010, Post-construction monitoring of a Core-Loc™ breakwater using tripod-based LiDAR, chap. <i>of</i> Coasts, marine structures and breakwaters: Adapting to change, https://doi.org/10.1680/cmsb.41301.0039.","ipdsId":"IP-012418","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":333550,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publishingServiceCenter":{"id":1,"text":"Sacramento PSC"},"noUsgsAuthors":false,"publicationDate":"2010-07-02","publicationStatus":"PW","scienceBaseUri":"58833023e4b0d002316377a2","contributors":{"authors":[{"text":"Podoski, Jessica H.","contributorId":178488,"corporation":false,"usgs":false,"family":"Podoski","given":"Jessica","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":659195,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bawden, Gerald W. gbawden@usgs.gov","contributorId":1071,"corporation":false,"usgs":true,"family":"Bawden","given":"Gerald","email":"gbawden@usgs.gov","middleInitial":"W.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":659196,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bond, Sandra 0000-0003-0522-5287 sbond@usgs.gov","orcid":"https://orcid.org/0000-0003-0522-5287","contributorId":3328,"corporation":false,"usgs":true,"family":"Bond","given":"Sandra","email":"sbond@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":659197,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, Thomas D.","contributorId":178489,"corporation":false,"usgs":false,"family":"Smith","given":"Thomas","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":659198,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Foster, James","contributorId":38598,"corporation":false,"usgs":true,"family":"Foster","given":"James","affiliations":[],"preferred":false,"id":659199,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70035554,"text":"70035554 - 2010 - Faunal assemblages and multi-scale habitat patterns in headwater tributaries of the South Fork Trinity River - an unregulated river embedded within a multiple-use landscape","interactions":[],"lastModifiedDate":"2012-06-23T01:01:39","indexId":"70035554","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":771,"text":"Animal Biodiversity and Conservation","active":true,"publicationSubtype":{"id":10}},"title":"Faunal assemblages and multi-scale habitat patterns in headwater tributaries of the South Fork Trinity River - an unregulated river embedded within a multiple-use landscape","docAbstract":"Headwaters can represent 80% of stream kilometers in a watershed, and they also have unique physical and biological properties that have only recently been recognized for their importance in sustaining healthy functioning stream networks and their ecological services. We sampled 60 headwater tributaries in the South Fork Trinity River, a 2,430 km2, mostly forested, multiple-use watershed in northwestern California. Our objectives were: (1) to differentiate unique headwater types using 69 abiotic and vegetation variables measured at three spatial scales, and then to reduce these to informative subsets; (2) determine if distinct biota occupied the different tributary types; (3) determine the environmental attributes associated with the presence and abundance of these biotic assemblages; and (4) using niche modeling, determine key attribute thresholds to illustrate how these biota could be employed as metrics of system integrity and ecological services. Several taxa were sufficiently abundant and widespread to use as bio-indicators: the presence and abundance of steelhead trout (Oncorhynchus mykiss), herpetofauna (reptile and amphibian) species richness, and signal crayfish (Pacifastacus leniusculus) represented different trophic positions, value as commercial resources (steelhead), sensitivity to environmental stress (amphibians), and indicators of biodiversity (herpetofauna species richness). Herpetofauna species richness did not differ, but abundances of steelhead trout, signal crayfish, and amphibian richness all differed significantly among tributary types. Niche models indicated that distribution and abundance patterns in both riparian and aquatic environments were associated with physical and structural attributes at multiple spatial scales, both within and around reaches. The bio-indicators responded to unique sets of attributes, reflecting the high environmental heterogeneity in headwater tributaries across this large watershed. These niche attributes represented a wide range of headwater environments, indicating responses to a number of natural and anthropogenic conditions, and demonstrated the value of using a suite of bio-indicators to elucidate watershed conditions, and to examine numerous disturbances that may influence ecological integrity.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Animal Biodiversity and Conservation","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"1578665X","usgsCitation":"Welsh, H., Hodgson, G., Duda, J., and Emlen, J., 2010, Faunal assemblages and multi-scale habitat patterns in headwater tributaries of the South Fork Trinity River - an unregulated river embedded within a multiple-use landscape: Animal Biodiversity and Conservation, v. 33, no. 1, p. 63-87.","startPage":"63","endPage":"87","numberOfPages":"25","costCenters":[],"links":[{"id":243908,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":257807,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://abc.museucienciesjournals.cat/volum-33-1-2010-abc/faunal-assemblages-and-multi-scale-habitat-patterns-in-headwater-tributaries-of-the-south-fork-trinity-river-an-unregulated-river-embedded-within-a-multiple-use-landscape/?lang=en","linkFileType":{"id":5,"text":"html"}}],"volume":"33","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0f2ce4b0c8380cd537de","contributors":{"authors":[{"text":"Welsh, H.H.","contributorId":41240,"corporation":false,"usgs":true,"family":"Welsh","given":"H.H.","affiliations":[],"preferred":false,"id":451214,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hodgson, G.R.","contributorId":30475,"corporation":false,"usgs":true,"family":"Hodgson","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":451213,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Duda, J.J. 0000-0001-7431-8634","orcid":"https://orcid.org/0000-0001-7431-8634","contributorId":105073,"corporation":false,"usgs":true,"family":"Duda","given":"J.J.","affiliations":[],"preferred":false,"id":451216,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Emlen, J.M.","contributorId":63979,"corporation":false,"usgs":true,"family":"Emlen","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":451215,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70037170,"text":"70037170 - 2010 - Response of aquatic macrophytes to human land use perturbations in the watersheds of Wisconsin lakes, U.S.A.","interactions":[],"lastModifiedDate":"2017-05-10T13:57:48","indexId":"70037170","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":861,"text":"Aquatic Botany","active":true,"publicationSubtype":{"id":10}},"title":"Response of aquatic macrophytes to human land use perturbations in the watersheds of Wisconsin lakes, U.S.A.","docAbstract":"<p><span>Aquatic macrophyte communities were assessed in 53 lakes in Wisconsin, U.S.A. along environmental and land use development gradients to determine effects human land use perturbations have on aquatic macrophytes at the watershed and riparian development scales. Species richness and relative frequency were surveyed in lakes from two ecoregions: the Northern Lakes and Forests Ecoregion and the Southeastern Wisconsin Till Plain Ecoregion. Lakes were selected along a gradient of watershed development ranging from undeveloped (i.e., forested), to agricultural to urban development. Land uses occurring in the watershed and in perimeters of different width (0&ndash;100, 0&ndash;200, 0&ndash;500, and 0&ndash;1000&nbsp;m from shore, in the watershed) were used to assess effects on macrophyte communities. Snorkel and SCUBA were used to survey aquatic macrophyte species in 18 quadrats of 0.25&nbsp;m</span><sup>2</sup><span><span class=\"Apple-converted-space\">&nbsp;</span>along 14 transects placed perpendicular to shore in each lake. Effects of watershed development (e.g., agriculture and/or urban) were tested at whole-lake (entire littoral zone) and near-shore (within 7&nbsp;m of shore) scales using canonical correspondence analysis (CCA) and linear regression. Overall, species richness was negatively related to watershed development, while frequencies of individual species and groups differed in level of response to different land use perturbations. Effects of land use in the perimeters on macrophytes, with a few exceptions, did not provide higher correlations compared to land use at the watershed scale. In lakes with higher total watershed development levels, introduced species, particularly<span class=\"Apple-converted-space\">&nbsp;</span></span><i>Myriophyllum</i><i>spicatum</i><span>, increased in abundance and native species, especially potamids, isoetids, and floating-leaved plants, declined in abundance. Correlations within the northern and southeastern ecoregions separately were not significant. Multivariate analyses suggested species composition is driven by environmental responses as well as human development pressures. Both water chemistry and land use variables loaded positively with the first CCA axis indicating that these factors are correlated. Land use pressures in Wisconsin are greater in the southeastern portion of the state where lakes have higher concentrations of water chemistry variables including alkalinity, conductivity, pH, calcium, magnesium, and nitrogen. This creates a complex gradient that influences species composition of macrophyte communities from lake to lake.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.aquabot.2010.02.001","issn":"03043770","usgsCitation":"Sass, L.L., Bozek, M.A., Hauxwell, J.A., Wagner, K., and Knight, S., 2010, Response of aquatic macrophytes to human land use perturbations in the watersheds of Wisconsin lakes, U.S.A.: Aquatic Botany, v. 93, no. 1, p. 1-8, https://doi.org/10.1016/j.aquabot.2010.02.001.","productDescription":"8 p.","startPage":"1","endPage":"8","numberOfPages":"8","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-014144","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":244901,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":216994,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.aquabot.2010.02.001"}],"country":"United States","state":"Wisconsin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.978515625,\n              42.49235259142821\n            ],\n            [\n              -89.82421875,\n              42.512601715736665\n            ],\n            [\n              -89.8681640625,\n              43.06086137134326\n            ],\n            [\n              -89.593505859375,\n              43.42898792344155\n            ],\n            [\n              -92.274169921875,\n              45.62940492064501\n            ],\n            [\n              -92.296142578125,\n              46.36967413462374\n            ],\n            [\n              -90.0714111328125,\n              46.33555079758302\n            ],\n            [\n              -89.0716552734375,\n              46.145588688591964\n            ],\n            [\n              -88.802490234375,\n              46.01985337287631\n            ],\n            [\n              -88.5333251953125,\n              44.44554600843545\n            ],\n            [\n              -87.528076171875,\n              44.201897151875094\n            ],\n            [\n              -87.659912109375,\n              44.09942068528651\n            ],\n            [\n              -87.747802734375,\n              43.878097874251736\n            ],\n            [\n              -88.0389404296875,\n              42.88803956056295\n            ],\n            [\n              -87.978515625,\n              42.49235259142821\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"93","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aaa30e4b0c8380cd861c5","contributors":{"authors":[{"text":"Sass, Laura L.","contributorId":38813,"corporation":false,"usgs":false,"family":"Sass","given":"Laura","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":459713,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bozek, Michael A.","contributorId":51030,"corporation":false,"usgs":true,"family":"Bozek","given":"Michael","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":459716,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hauxwell, Jennifer A.","contributorId":53628,"corporation":false,"usgs":false,"family":"Hauxwell","given":"Jennifer","email":"","middleInitial":"A.","affiliations":[{"id":7242,"text":"Wisconsin Department of Natural Resources, Madison, WI, USA","active":true,"usgs":false}],"preferred":false,"id":459717,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wagner, Kelly","contributorId":45930,"corporation":false,"usgs":false,"family":"Wagner","given":"Kelly","email":"","affiliations":[{"id":7242,"text":"Wisconsin Department of Natural Resources, Madison, WI, USA","active":true,"usgs":false}],"preferred":false,"id":459715,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Knight, Susan","contributorId":44010,"corporation":false,"usgs":false,"family":"Knight","given":"Susan","affiliations":[{"id":7191,"text":"Trout Lake Station, Center for Limnology, University of Wisconsin-Madison, Boulder Junction, WI, USA","active":true,"usgs":false}],"preferred":false,"id":459714,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70034457,"text":"70034457 - 2010 - A shallow subsurface controlled release facility in Bozeman, Montana, USA, for testing near surface CO2 detection techniques and transport models","interactions":[],"lastModifiedDate":"2018-10-10T11:30:02","indexId":"70034457","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1534,"text":"Environmental Earth Sciences","active":true,"publicationSubtype":{"id":10}},"title":"A shallow subsurface controlled release facility in Bozeman, Montana, USA, for testing near surface CO2 detection techniques and transport models","docAbstract":"<p>A controlled field pilot has been developed in Bozeman, Montana, USA, to study near surface CO2 transport and detection technologies. A slotted horizontal well divided into six zones was installed in the shallow subsurface. The scale and CO2 release rates were chosen to be relevant to developing monitoring strategies for geological carbon storage. The field site was characterized before injection, and CO2 transport and concentrations in saturated soil and the vadose zone were modeled. Controlled releases of CO2 from the horizontal well were performed in the summers of 2007 and 2008, and collaborators from six national labs, three universities, and the U.S. Geological Survey investigated movement of CO2 through the soil, water, plants, and air with a wide range of near surface detection techniques. An overview of these results will be presented.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Earth Sciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1007/s12665-009-0400-2","issn":"18666280","usgsCitation":"Spangler, L., Dobeck, L., Repasky, K., Nehrir, A., Humphries, S., Keith, C., Shaw, J., Rouse, J., Cunningham, A., Benson, S., Oldenburg, C., Lewicki, J., Wells, A., Diehl, J., Strazisar, B., Fessenden, J., Rahn, T., Amonette, J., Barr, J., Pickles, W., Jacobson, J., Silver, E.A., Male, E., Rauch, H., Gullickson, K., Trautz, R., Kharaka, Y.K., Birkholzer, J., and Wielopolski, L., 2010, A shallow subsurface controlled release facility in Bozeman, Montana, USA, for testing near surface CO2 detection techniques and transport models: Environmental Earth Sciences, v. 60, no. 2, p. 227-239, https://doi.org/10.1007/s12665-009-0400-2.","productDescription":"13 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,{"id":70034000,"text":"70034000 - 2010 - Silica-rich deposits and hydrated minerals at Gusev Crater, Mars: Vis-NIR spectral characterization and regional mapping","interactions":[],"lastModifiedDate":"2012-03-12T17:21:48","indexId":"70034000","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Silica-rich deposits and hydrated minerals at Gusev Crater, Mars: Vis-NIR spectral characterization and regional mapping","docAbstract":"The Mars Exploration Rover (MER) Spirit has discovered surprisingly high concentrations of amorphous silica in soil and nodular outcrops in the Inner Basin of the Columbia Hills. In Pancam multispectral observations, we find that an absorption feature at the longest Pancam wavelength (1009 nm) appears to be characteristic of these silica-rich materials; however, spectral analyses of amorphous silica suggest that the ???1009 nm spectral feature is not a direct reflection of their silica-rich nature. Based on comparisons with spectral databases, we hypothesize that the presence of H<sub>2</sub>O or OH, either free (as water ice), adsorbed or bound in a mineral structure, is responsible for the spectral feature observed by Pancam. The Gertrude Weise soil, which is nearly pure opaline silica, may have adsorbed water cold-trapped on mineral grains. The origin of the ???1009 nm Pancam feature observed in the silica-rich nodular outcrops may result from the presence of additional hydrated minerals (specific sulfates, halides, chlorides, sodium silicates, carbonates or borates). Using the ???1009 nm feature with other spectral parameters as a \"hydration signature\" we have mapped the occurrence of hydrated materials along the extent of Spirit's traverse across the Columbia Hills from West Spur to Home Plate (sols 155-1696). We have also mapped this hydration signature across large panoramic images to understand the regional distribution of materials that are spectrally similar to the silica-rich soil and nodular outcrops. Our results suggest that hydrated materials are common in the Columbia Hills. ?? 2009 Elsevier Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Icarus","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.icarus.2009.03.035","issn":"00191035","usgsCitation":"Rice, M., Bell, J., Cloutis, E., Wang, A., Ruff, S.W., Craig, M., Bailey, D., Johnson, J.R., De Souza, P., and Farrand, W.H., 2010, Silica-rich deposits and hydrated minerals at Gusev Crater, Mars: Vis-NIR spectral characterization and regional mapping: Icarus, v. 205, no. 2, p. 375-395, https://doi.org/10.1016/j.icarus.2009.03.035.","startPage":"375","endPage":"395","numberOfPages":"21","costCenters":[],"links":[{"id":244731,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":216835,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.icarus.2009.03.035"}],"volume":"205","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8f33e4b08c986b318db3","contributors":{"authors":[{"text":"Rice, M.S.","contributorId":105027,"corporation":false,"usgs":true,"family":"Rice","given":"M.S.","affiliations":[],"preferred":false,"id":443593,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bell, J.F. 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,{"id":70037116,"text":"70037116 - 2010 - Redwoods, restoration, and implications for carbon budgets","interactions":[],"lastModifiedDate":"2018-03-21T14:41:28","indexId":"70037116","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1801,"text":"Geomorphology","active":true,"publicationSubtype":{"id":10}},"title":"Redwoods, restoration, and implications for carbon budgets","docAbstract":"The coast redwoods (Sequoia sempervirens) of California have several unique characteristics that influence interactions between vegetation and geomorphic processes. Case studies, using a combination of in-channel wood surveys and an air photo inventory of landslides, illustrate current conditions in a redwood-dominated watershed undergoing restoration work, and the influence of wood loading and landslides on the carbon budget. Redwood trees have extremely large biomass (trunk wood volumes of 700 to 1000 m<sup>3</sup>) and are very decay-resistant; consequently, they have a large and persistent influence on in-channel wood loading. Large wood surveys indicate high wood loading in streams in uncut forests (0.3-0.5 m<sup>3</sup>/m<sup>2</sup> of channel), but also show that high wood loading can persist in logged basin with unlogged riparian buffers because of the slow decay of fallen redwoods. Through a watershed restoration program, Redwood National Park increases in-channel wood loading in low-order streams, but the effectiveness of this technique has not yet been tested by a large flood. Another unique characteristic of redwood is its ability to resprout from basal burls after cutting, so that root strength may not decline as sharply following logging as in other types of forests. An air photo inventory of landslides following a large storm in 1997 indicated: 1) that in the Redwood Creek watershed the volume of material displaced by landslides in harvested areas was not related to the time elapsed since logging, suggesting that the loss of root strength was not a decisive factor in landslide initiation, 2) landslide production on decommissioned logging roads was half that of untreated roads, and 3) landslides removed an estimated 28 Mg of organic carbon/km<sup>2</sup> from hillslopes. The carbon budget of a redwood-dominated catchment is dominated by the vegetative component, but is also influenced by the extent of mass movement, erosion control work, and in-channel storage of wood.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geomorphology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.geomorph.2009.11.012","issn":"0169555X","usgsCitation":"Madej, M.A., 2010, Redwoods, restoration, and implications for carbon budgets: Geomorphology, v. 116, no. 3-4, p. 264-273, https://doi.org/10.1016/j.geomorph.2009.11.012.","startPage":"264","endPage":"273","numberOfPages":"10","costCenters":[],"links":[{"id":245023,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217106,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.geomorph.2009.11.012"}],"volume":"116","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e4a413e4b0e8fec6cdba2f","contributors":{"authors":[{"text":"Madej, Mary Ann 0000-0003-2831-3773 mary_ann_madej@usgs.gov","orcid":"https://orcid.org/0000-0003-2831-3773","contributorId":40304,"corporation":false,"usgs":true,"family":"Madej","given":"Mary","email":"mary_ann_madej@usgs.gov","middleInitial":"Ann","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":459464,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70192568,"text":"70192568 - 2010 - BRIDGES: Evolution of basic and applied linkages in benthic science","interactions":[],"lastModifiedDate":"2017-10-26T12:41:57","indexId":"70192568","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2564,"text":"Journal of the North American Benthological Society","onlineIssn":"1937-237X","printIssn":"0887-3593","active":true,"publicationSubtype":{"id":10}},"title":"BRIDGES: Evolution of basic and applied linkages in benthic science","docAbstract":"<p>Growing awareness of environmental degradation resulted in stricter environmental regulations and laws for aquatic ecosystems. These regulations were followed by an increase in applied research and monitoring beginning in the early 1970s. The number of applied scientists who were members of the North American Benthological Society grew at a commensurate rate. The editors of <i>J-NABS</i> recognized that, despite these increases, submitted manuscripts mostly addressed basic science. In response, the <i>BRIDGES</i> section of <i>J-NABS</i> was created in 1994 to provide a forum for linking basic ecological principles to applied science problems and issues. We examined the emergence of applied science topics in <i>J-NABS</i> and its predecessor, <i>Freshwater Invertebrate Biology</i>, from their beginning in 1982 to 2009. We classified papers among 11 categories that included a basic/applied science linkage. In the 1980s, applied papers were predominantly on effects of eutrophication/pollution and landuse changes. When <i>BRIDGES</i> was established in 1994, papers were solicited by editors and <i>BRIDGES</i> sections usually included &gt;1 paper on a common theme to express complementary or alternate viewpoints. Forty-two papers appeared in <i>BRIDGES</i> between 1994 and 2009, but the number per issue declined after 2001. The total number of applied science papers in <i>J-NABS</i> has increased since ∼1994. Citation analysis of <i>BRIDGES</i> papers illustrates how information is being cited, but applied papers often are used in ways that might not lead to citations. <i>BRIDGES</i> transitioned to a new format in September 2009 to address new types of complex, multifaceted linkages. All new <i>BRIDGES</i> articles will be open access, and authors will be encouraged to produce lay-language fact sheets and to post them on the web.</p>","language":"English","publisher":"University of Chicago Press","doi":"10.1899/08-031.1","usgsCitation":"Aumen, N.G., Gurtz, M.E., Barbour, M.T., and Moerke, A., 2010, BRIDGES: Evolution of basic and applied linkages in benthic science: Journal of the North American Benthological Society, v. 29, no. 1, p. 359-371, https://doi.org/10.1899/08-031.1.","productDescription":"13 p.","startPage":"359","endPage":"371","ipdsId":"IP-014513","costCenters":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"links":[{"id":347465,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"1","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a07f62ee4b09af898c8cdf4","contributors":{"authors":[{"text":"Aumen, Nicholas G. 0000-0002-5277-2630 naumen@usgs.gov","orcid":"https://orcid.org/0000-0002-5277-2630","contributorId":5418,"corporation":false,"usgs":true,"family":"Aumen","given":"Nicholas","email":"naumen@usgs.gov","middleInitial":"G.","affiliations":[{"id":5064,"text":"Southeast Regional Director's Office","active":true,"usgs":true},{"id":13415,"text":"Everglades National Park","active":true,"usgs":false}],"preferred":true,"id":716268,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gurtz, Martin E. megurtz@usgs.gov","contributorId":2987,"corporation":false,"usgs":true,"family":"Gurtz","given":"Martin","email":"megurtz@usgs.gov","middleInitial":"E.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":false,"id":716269,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barbour, Michael T.","contributorId":198484,"corporation":false,"usgs":false,"family":"Barbour","given":"Michael","email":"","middleInitial":"T.","affiliations":[{"id":16286,"text":"Tetra Tech","active":true,"usgs":false}],"preferred":false,"id":716270,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Moerke, Ashley","contributorId":198485,"corporation":false,"usgs":false,"family":"Moerke","given":"Ashley","email":"","affiliations":[{"id":35243,"text":"Lake Superior State University","active":true,"usgs":false}],"preferred":false,"id":716271,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70034209,"text":"70034209 - 2010 - Growth, carbon-isotope discrimination, and drought-associated mortality across a Pinus ponderosa elevational transect","interactions":[],"lastModifiedDate":"2018-01-23T11:05:20","indexId":"70034209","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1837,"text":"Global Change Biology","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Growth, carbon-isotope discrimination, and drought-associated mortality across a <i>Pinus ponderosa</i> elevational transect","title":"Growth, carbon-isotope discrimination, and drought-associated mortality across a Pinus ponderosa elevational transect","docAbstract":"<p>Drought- and insect-associated tree mortality at low-elevation ecotones is a widespread phenomenon but the underlying mechanisms are uncertain. Enhanced growth sensitivity to climate is widely observed among trees that die, indicating that a predisposing physiological mechanism(s) underlies tree mortality. We tested three, linked hypotheses regarding mortality using a ponderosa pine (<i>Pinus ponderosa</i>) elevation transect that experienced low-elevation mortality following prolonged drought. The hypotheses were: (1) mortality was associated with greater growth sensitivity to climate, (2) mortality was associated with greater sensitivity of gas exchange to climate, and (3) growth and gas exchange were correlated. Support for all three hypotheses would indicate that mortality results at least in part from gas exchange constraints. We assessed growth using basal area increment normalized by tree basal area [basal area increment (BAI)/basal area (BA)] to account for differences in tree size. Whole-crown gas exchange was indexed via estimates of the CO<sub>2</sub> partial pressure difference between leaf and atmosphere (<i>p</i><sub>a</sub>−<i>p</i><sub>c</sub>) derived from tree ring carbon isotope ratios (<i>δ</i><sup>13</sup>C), corrected for temporal trends in atmospheric CO<sub>2</sub> and <i>δ</i><sup>13</sup>C and elevation trends in pressure. Trees that survived the drought exhibited strong correlations among and between BAI, BAI/BA, <i>p</i><sub>a</sub>−<i>p</i><sub>c</sub>, and climate. In contrast, trees that died exhibited greater growth sensitivity to climate than trees that survived, no sensitivity of <i>p</i><sub>a</sub>−<i>p</i><sub>c</sub> to climate, and a steep relationship between <i>p</i><sub>a</sub>−<i>p</i><sub>c</sub> and BAI/BA. The <i>p</i><sub>a</sub>−<i>p</i><sub>c</sub> results are consistent with predictions from a theoretical hydraulic model, suggesting trees that died had a limited buffer between mean water availability during their lifespan and water availability during drought – i.e., chronic water stress. It appears that chronic water stress predisposed low-elevation trees to mortality during drought via constrained gas exchange. Continued intensification of drought in mid-latitude regions may drive increased mortality and ecotone shifts in temperate forests and woodlands.</p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1365-2486.2009.01994.x","usgsCitation":"McDowell, N., Allen, C.D., and Marshall, L., 2010, Growth, carbon-isotope discrimination, and drought-associated mortality across a Pinus ponderosa elevational transect: Global Change Biology, v. 16, no. 1, p. 399-415, https://doi.org/10.1111/j.1365-2486.2009.01994.x.","productDescription":"17 p.","startPage":"399","endPage":"415","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":244396,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"1","noUsgsAuthors":false,"publicationDate":"2009-12-02","publicationStatus":"PW","scienceBaseUri":"505a2e0fe4b0c8380cd5c288","contributors":{"authors":[{"text":"McDowell, N.G.","contributorId":93296,"corporation":false,"usgs":true,"family":"McDowell","given":"N.G.","email":"","affiliations":[],"preferred":false,"id":444618,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allen, Craig D. 0000-0002-8777-5989 craig_allen@usgs.gov","orcid":"https://orcid.org/0000-0002-8777-5989","contributorId":2597,"corporation":false,"usgs":true,"family":"Allen","given":"Craig","email":"craig_allen@usgs.gov","middleInitial":"D.","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":444617,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Marshall, L.","contributorId":37171,"corporation":false,"usgs":true,"family":"Marshall","given":"L.","email":"","affiliations":[],"preferred":false,"id":444616,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70187016,"text":"70187016 - 2010 - Interpreting canopy water balance and fog screen observations: separating cloud water from wind-blown rainfall at two contrasting forest sites in Hawai'i","interactions":[],"lastModifiedDate":"2017-04-19T10:02:29","indexId":"70187016","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Interpreting canopy water balance and fog screen observations: separating cloud water from wind-blown rainfall at two contrasting forest sites in Hawai'i","docAbstract":"<p>No abstract available.<br></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Tropical montane cloud forests: science for conservation and management","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Cambridge University Press","usgsCitation":"Giambelluca, T.W., DeLay, J.K., Nullet, M., Scholl, M.A., and 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,{"id":70037206,"text":"70037206 - 2010 - Timing and duration of garnet granulite metamorphism in magmatic arc crust, Fiordland, New Zealand","interactions":[],"lastModifiedDate":"2012-03-12T17:22:07","indexId":"70037206","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Timing and duration of garnet granulite metamorphism in magmatic arc crust, Fiordland, New Zealand","docAbstract":"Pembroke Granulite from Fiordland, New Zealand provides a window into the mid- to lower crust of magmatic arcs. Garnet Sm-Nd and zircon U-Pb ages constrain the timing and duration of high-P partial melting that produced trondhjemitic high Sr/Y magma. Trace element zoning in large, euhedral garnet is compatible with little post growth modification and supports the interpretation that garnet Sm-Nd ages of 126.1??2.0 and 122.6??2.0. Ma date crystal growth. Integration of the garnet ages with U-Pb zircon ages elucidates a history of intrusion(?) and a protracted period of high-temperature metamorphism and partial melting. The oldest zircon ages of 163 to 150. Ma reflect inheritance or intrusion and a cluster of zircon ages ca. 134. Ma date orthopyroxene-bearing mineral assemblages that may be magmatic or metamorphic in origin. Zircon and garnet ages from unmelted gneiss and garnet reaction zones record garnet granulite facies metamorphism at 128 to 126. Ma. Peritectic garnet and additional zircon ages from trondhjemite veins and garnet reaction zones indicate that garnet growth and partial melting lasted until ca. 123. Ma. Two single fraction garnet ages and young zircon ages suggest continued high-temperature re-equilibration until ca. 95. Ma. Phase diagram sections constrain orthopyroxene assemblages to <0.6 GPa @ 650??C, peak garnet granulite facies metamorphic conditions to 680-815??C @ 1.1-1.4. GPa, and a P-T path with a P increase of???0.5. GPa. These sections are compatible with water contents???0.28wt.%, local dehydration during garnet granulite metamorphism, and <0.3. GPa P increases during garnet growth. Results demonstrate the utility of integrated U-Pb zircon and Sm-Nd garnet ages, and phase diagram sections for understanding the nature, duration, and conditions of deep crustal metamorphism and melting. Geochronologic and thermobarometric data for garnet granulite indicate that thickening of arc crust, which caused high-pressure metamorphism in northern Fiordland, must have occurred prior to 126. Ma, that loading occurred at a rate of ca. 0.06. GPa/m.y., and that garnet granulite metamorphism lasted 3-7m.y. Locally-derived partial melts formed and crystallized in considerably less than 10 and perhaps as little as 3m.y. ?? 2010 Elsevier B.V.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/j.chemgeo.2010.02.015","issn":"00092541","usgsCitation":"Stowell, H., Tulloch, A., Zuluaga, C., and Koenig, A., 2010, Timing and duration of garnet granulite metamorphism in magmatic arc crust, Fiordland, New Zealand: Chemical Geology, v. 273, no. 1-2, p. 91-110, https://doi.org/10.1016/j.chemgeo.2010.02.015.","startPage":"91","endPage":"110","numberOfPages":"20","costCenters":[],"links":[{"id":244964,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":217053,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/j.chemgeo.2010.02.015"}],"volume":"273","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb3e4e4b08c986b326051","contributors":{"authors":[{"text":"Stowell, H.","contributorId":19409,"corporation":false,"usgs":true,"family":"Stowell","given":"H.","email":"","affiliations":[],"preferred":false,"id":459899,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tulloch, A.","contributorId":10645,"corporation":false,"usgs":true,"family":"Tulloch","given":"A.","email":"","affiliations":[],"preferred":false,"id":459898,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zuluaga, C.","contributorId":37177,"corporation":false,"usgs":true,"family":"Zuluaga","given":"C.","email":"","affiliations":[],"preferred":false,"id":459900,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Koenig, A. 0000-0002-5230-0924","orcid":"https://orcid.org/0000-0002-5230-0924","contributorId":64037,"corporation":false,"usgs":true,"family":"Koenig","given":"A.","affiliations":[],"preferred":false,"id":459901,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70037180,"text":"70037180 - 2010 - Influence of coal-tar sealcoat and other carbonaceous materials on polycyclic aromatic hydrocarbon loading in an urban watershed","interactions":[],"lastModifiedDate":"2012-03-12T17:22:11","indexId":"70037180","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","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":"Influence of coal-tar sealcoat and other carbonaceous materials on polycyclic aromatic hydrocarbon loading in an urban watershed","docAbstract":"Carbonaceous material (CM) particles are the principal vectors transporting polycyclic aromatic hydrocarbons (PAHs) into urban waters via runoff; however, characteristics of CM particles in urban watersheds and their relative contributions to PAH contamination remain unclear. Our objectives were to identify the sources and distribution of CM particles in an urban watershed and to determine the types of CMs that were the dominant sources of PAHs in the lake and stream sediments. Samples of soils, parking lot and street dust, and streambed and lake sediment were collected from the Lake Como watershed in Fort Worth, Texas. Characteristics of CM particles determined by organic petrography and a significant correlation between PAH concentrations and organic carbon in coal tar, asphalt, and soot indicate that these three CM particle types are the major sources and carriers of PAHs in the watershed. Estimates of the distribution of PAHs in CM particles indicate that coal-tar pitch, usedinsomepavementsealcoats, isadominant source of PAHs in the watershed, and contributes as much as 99% of the PAHs in sealed parking lot dust, 92% in unsealed parking lot dust, 88% in commercial area soil, 71% in streambed sediment, and 84% in surficial lake sediment. ?? 2010 American Chemical Society.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Science and Technology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1021/es902657h","issn":"0013936X","usgsCitation":"Yang, Y., Van Metre, P., Mahler, B., Wilson, J., Ligouis, B., Razzaque, M., Schaeffer, D., and Werth, C., 2010, Influence of coal-tar sealcoat and other carbonaceous materials on polycyclic aromatic hydrocarbon loading in an urban watershed: Environmental Science & Technology, v. 44, no. 4, p. 1217-1223, https://doi.org/10.1021/es902657h.","startPage":"1217","endPage":"1223","numberOfPages":"7","costCenters":[],"links":[{"id":217140,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es902657h"},{"id":245059,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-01-27","publicationStatus":"PW","scienceBaseUri":"505a3b1ae4b0c8380cd62223","contributors":{"authors":[{"text":"Yang, Y.","contributorId":105563,"corporation":false,"usgs":true,"family":"Yang","given":"Y.","email":"","affiliations":[],"preferred":false,"id":459779,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Metre, P. C.","contributorId":92999,"corporation":false,"usgs":true,"family":"Van Metre","given":"P. C.","affiliations":[],"preferred":false,"id":459777,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mahler, B.J.","contributorId":36888,"corporation":false,"usgs":true,"family":"Mahler","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":459773,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wilson, J.T.","contributorId":97489,"corporation":false,"usgs":true,"family":"Wilson","given":"J.T.","affiliations":[],"preferred":false,"id":459778,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ligouis, B.","contributorId":59228,"corporation":false,"usgs":true,"family":"Ligouis","given":"B.","email":"","affiliations":[],"preferred":false,"id":459774,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Razzaque, M.","contributorId":74986,"corporation":false,"usgs":true,"family":"Razzaque","given":"M.","email":"","affiliations":[],"preferred":false,"id":459776,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Schaeffer, D.J.","contributorId":65038,"corporation":false,"usgs":true,"family":"Schaeffer","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":459775,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Werth, C.J.","contributorId":26481,"corporation":false,"usgs":true,"family":"Werth","given":"C.J.","affiliations":[],"preferred":false,"id":459772,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70046697,"text":"dds49104 - 2010 - Attributes for MRB_E2RF1 Catchments by Major River Basins in the Conterminous United States: Base-Flow Index, 2002","interactions":[],"lastModifiedDate":"2013-11-25T16:07:07","indexId":"dds49104","displayToPublicDate":"2010-01-01T00:00:00","publicationYear":"2010","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":"491-04","title":"Attributes for MRB_E2RF1 Catchments by Major River Basins in the Conterminous United States: Base-Flow Index, 2002","docAbstract":"This tabular data set represents the mean base-flow index expressed as a percent, compiled for every catchment of MRB_E2RF1 catchments of Major River Basins (MRBs, Crawford and others, 2006). Base flow is the component of streamflow that can be attributed to ground-water discharge into streams. The source data set is Base-Flow Index for the Conterminous United States (Wolock, 2003). The MRB_E2RF1 catchments are based on a modified version of the U.S. Environmental Protection Agency's (USEPA) ERF1_2 and include enhancements to support national and regional-scale surface-water quality modeling (Nolan and others, 2002; Brakebill and others, 2011). Data were compiled for every catchment of MRB_E2RF1 catchments for the conterminous United States covering New England and Mid-Atlantic (MRB1), South Atlantic-Gulf and Tennessee (MRB2), the Great Lakes, Ohio, Upper Mississippi, and Souris-Red-Rainy (MRB3), the Missouri (MRB4), the Lower Mississippi, Arkansas-White-Red, and Texas-Gulf (MRB5), the Rio Grande, Colorado, and the Great basin (MRB6), the Pacific Northwest (MRB7) river basins, and California (MRB8).","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/dds49104","usgsCitation":"Wieczorek, M., and LaMotte, A.E., 2010, Attributes for MRB_E2RF1 Catchments by Major River Basins in the Conterminous United States: Base-Flow Index, 2002: U.S. Geological Survey Data Series 491-04, Dataset, https://doi.org/10.3133/dds49104.","productDescription":"Dataset","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":274228,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":274227,"type":{"id":16,"text":"Metadata"},"url":"https://water.usgs.gov/GIS/metadata/usgswrd/XML/mrb_e2rf1_bfi.xml"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -127.910792,23.243486 ], [ -127.910792,51.657387 ], [ -65.327751,51.657387 ], [ -65.327751,23.243486 ], [ -127.910792,23.243486 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51cabbe0e4b0d298e5434c2c","contributors":{"authors":[{"text":"Wieczorek, Michael mewieczo@usgs.gov","contributorId":2309,"corporation":false,"usgs":true,"family":"Wieczorek","given":"Michael","email":"mewieczo@usgs.gov","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":false,"id":480034,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LaMotte, Andrew E. 0000-0002-1434-6518 alamotte@usgs.gov","orcid":"https://orcid.org/0000-0002-1434-6518","contributorId":2842,"corporation":false,"usgs":true,"family":"LaMotte","given":"Andrew","email":"alamotte@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":480035,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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