No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr85174","usgsCitation":"Fontaine, R.A., 1989, Hydrologic and meteorologic data for the Bald Mountain area, Aroostook County, Maine: June 1979 through June 1984: U.S. Geological Survey Open-File Report 85-174, iv, 166 p., https://doi.org/10.3133/ofr85174.","productDescription":"iv, 166 p.","costCenters":[],"links":[{"id":410886,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75762.htm","linkFileType":{"id":5,"text":"html"}},{"id":42153,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0174/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146769,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0174/report-thumb.jpg"}],"country":"United States","state":"Maine","county":"Aroostook County","otherGeospatial":"Bald Mountain area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -68.8333,\n 46.8333\n ],\n [\n -68.8333,\n 46.6667\n ],\n [\n -68.6667,\n 46.6667\n ],\n [\n -68.6667,\n 46.8333\n ],\n [\n -68.8333,\n 46.8333\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6117e6","contributors":{"authors":[{"text":"Fontaine, Richard A. rfontain@usgs.gov","contributorId":2379,"corporation":false,"usgs":true,"family":"Fontaine","given":"Richard","email":"rfontain@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":168144,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":12579,"text":"ofr8992 - 1989 - Fractures in outcrops in the vicinity of drill hole USW G-4. Yucca Mountain, Nevada; data analysis and compilation","interactions":[],"lastModifiedDate":"2018-06-04T12:52:34","indexId":"ofr8992","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"89-92","title":"Fractures in outcrops in the vicinity of drill hole USW G-4. Yucca Mountain, Nevada; data analysis and compilation","docAbstract":"Fractures on outcrops in the vicinity of drill hole USW G-4, Yucca Mountain, Nevada, were studied in order to contribute to characterization of fractures for hydrologjc, geomechanical, and tectonic modeling of the Yucca Mountain block and to characterize fractures prior to the excavation of a proposed exploratory shaft located near USW G-4. Yucca Mountain is a prospective site for the construction of an underground repository for high-level nuclear waste.
Measurements were taken and recorded on 5,000 fractures at 50 outcrop stations primarily in the upper lithophysal unit of the Tiva Canyon Member of the Miocene Paintbrush Tuff. Fracture orientation and surface roughness were recorded for each fracture. Additionally, notes were taken on fracture abutting, crossing, and offsetting relations, swarming, curvature, brecciation, slickensides, and fracture fillings.
Frequency distributions of orientation and roughness were plotted and analyzed. Fractures with low roughness coefficients (0-4) group tightly into two sets based on orientation. We conclude that such fractures are cooling joints and that all other fractures are tectonic.
The development of small-scale fractures adjacent, subparallel, and possibly related to the Ghost Dance fault has been addressed in a preliminary way based on data collected in this study. Such sympathetic fractures are abundant in the upper cliff unit but not in the upper lithophysal unit.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8992","usgsCitation":"Barton, C., Page, W.R., and Morgan, T.L., 1989, Fractures in outcrops in the vicinity of drill hole USW G-4. Yucca Mountain, Nevada; data analysis and compilation: U.S. Geological Survey Open-File Report 89-92, ii, 133 p., https://doi.org/10.3133/ofr8992.","productDescription":"ii, 133 p.","costCenters":[],"links":[{"id":146006,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0092/report-thumb.jpg"},{"id":40967,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0092/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a9033","contributors":{"authors":[{"text":"Barton, Christopher C.","contributorId":73133,"corporation":false,"usgs":true,"family":"Barton","given":"Christopher C.","affiliations":[],"preferred":false,"id":166374,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Page, William R. 0000-0002-0722-9911 rpage@usgs.gov","orcid":"https://orcid.org/0000-0002-0722-9911","contributorId":1628,"corporation":false,"usgs":true,"family":"Page","given":"William","email":"rpage@usgs.gov","middleInitial":"R.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":166373,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morgan, Terrance L.","contributorId":205383,"corporation":false,"usgs":false,"family":"Morgan","given":"Terrance","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":166372,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1271,"text":"wsp2345 - 1989 - Water movement in the unsaturated zone at a low-level radioactive-waste burial site near Barnwell, South Carolina","interactions":[{"subject":{"id":13302,"text":"ofr8746 - 1987 - Water movement in the unsaturated zone at a low-level radioactive-waste burial site near Barnwell, South Carolina","indexId":"ofr8746","publicationYear":"1987","noYear":false,"title":"Water movement in the unsaturated zone at a low-level radioactive-waste burial site near Barnwell, South Carolina"},"predicate":"SUPERSEDED_BY","object":{"id":1271,"text":"wsp2345 - 1989 - Water movement in the unsaturated zone at a low-level radioactive-waste burial site near Barnwell, South Carolina","indexId":"wsp2345","publicationYear":"1989","noYear":false,"title":"Water movement in the unsaturated zone at a low-level radioactive-waste burial site near Barnwell, South Carolina"},"id":1}],"lastModifiedDate":"2019-12-30T10:40:13","indexId":"wsp2345","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2345","title":"Water movement in the unsaturated zone at a low-level radioactive-waste burial site near Barnwell, South Carolina","docAbstract":"Four unsaturated-zone monitoring sites and a meteorologic station were installed at the low-level radioactive-waste burial site near Barnwell, S.C., to investigate the geohydrologic and climatologic factors affecting water movement in the unsaturated zone. The study site is located in the Atlantic Coastal Plain. The unsaturated zone consists of a few centimeters to more than 1 meter of surface sand, underlain by up to 15 meters of clayey sand. Two monitoring sites were installed in experimental trenches, and two were installed in radioactive-waste trenches. Two different trench designs were evaluated at the monitoring sites. \r\n\r\nA meteorologic station was used to measure precipitation and to calculate actual evapotranspiration using the Bowen ratio method. Soil-moisture tensiometers, soil-moisture conductance probes, and temperature sensors were used to monitor soil-water movement in and adjacent to the trenches. Tracer tests using sodium chloride were conducted at each monitoring site. Hydrologic properties of unsaturated-zone materials were also determined. Data collection at the monitoring sites began in January 1982 and continued until early May 1984. \r\n\r\nTensiometer data show that the unsaturated materials had their highest percent saturations in winter and spring. Saturations in the backfill sand varied from 20 to 100 percent, and in the adjacent undisturbed and overlying compacted clayey sand, from about 75 to 100 percent. The same pattern generally was observed at all four monitoring sites. The tracer-test data indicate that water movement occurred mainly during the recharge period, winter and spring. The tracer-test results enabled computation of rates of unsaturated flow in the compacted clayey-sand cap, the compacted clayey-sand barrier, and the backfill sand. \r\n\r\nA micro-scale hydrologic budget was determined for an undisturbed part of the site from July 1983 through June 1984.Total precipitation was 144 centimeters, and actual evapotranspiration was 101 centimeters. Additionally, because tensiometer data indicate negligible water-storage changes in the unsaturated zone, it is estimated that approximately 43 centimeters of recharge reached the water table. \r\n\r\nDuring 1984, the rise and fall of ponded water in an experimental trench was continuously monitored with a digital recorder. This water-level record was used to compute the rate of leakage of ponded water from that trench--1 x 10 -5 centimeter per second. A cross-sectional finite-element model of variably saturated flow was used to test the conceptual model of water movement in the unsaturated zone and to illustrate the effect of trench design on water movement into the experimental trenches. \r\n\r\nMonitoring and model results show that precipitation on trenches infiltrated the trench cap and moved vertically into the trench backfill material. Precipitation on the undisturbed material adjacent to the trenches moved vertically through the surface sand and continued either downward into undisturbed clayey sand or laterally along the sand/clayey-sand interface into the backfill sand, depending on trench design. The trench construction practice of placing a compacted clayey-sand barrier around the trench greatly inhibits soil water from entering the trench.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp2345","usgsCitation":"Dennehy, K.F., and McMahon, P.B., 1989, Water movement in the unsaturated zone at a low-level radioactive-waste burial site near Barnwell, South Carolina: U.S. Geological Survey Water Supply Paper 2345, v, 40 p. , https://doi.org/10.3133/wsp2345.","productDescription":"v, 40 p. ","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":26225,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2345/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137503,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2345/report-thumb.jpg"}],"country":"United States","state":"South Carolina","city":"Barnwell","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.5350341796875,\n 33.13065128220441\n ],\n [\n -81.199951171875,\n 33.13065128220441\n ],\n [\n -81.199951171875,\n 33.348884792201694\n ],\n [\n -81.5350341796875,\n 33.348884792201694\n ],\n [\n -81.5350341796875,\n 33.13065128220441\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db69970a","contributors":{"authors":[{"text":"Dennehy, Kevin F. kdennehy@usgs.gov","contributorId":1128,"corporation":false,"usgs":true,"family":"Dennehy","given":"Kevin","email":"kdennehy@usgs.gov","middleInitial":"F.","affiliations":[{"id":509,"text":"Office of the Associate Director for Water","active":true,"usgs":true}],"preferred":true,"id":143476,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McMahon, Peter B. 0000-0001-7452-2379 pmcmahon@usgs.gov","orcid":"https://orcid.org/0000-0001-7452-2379","contributorId":724,"corporation":false,"usgs":true,"family":"McMahon","given":"Peter","email":"pmcmahon@usgs.gov","middleInitial":"B.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":143475,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":12380,"text":"ofr89249 - 1989 - Water Resources Research Grant Program Project Descriptions: Fiscal Year 1988","interactions":[],"lastModifiedDate":"2012-02-02T00:06:40","indexId":"ofr89249","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"89-249","title":"Water Resources Research Grant Program Project Descriptions: Fiscal Year 1988","docAbstract":"This report contains information on the 38 new projects funded by the U.S. Geological Survey's Water Resources Research Grant Program in fiscal year 1988 and on 11 projects completed during the year. For the new projects, the report gives the grant number, project title, performing organization, principal investigator(s), project duration, and a project description that includes: (1) identification of water-related problems and problem-solution approach, (2) contribution to problem solution, (3) objectives, and (4) approach. The 38 projects include 14 in the area of ground-water quality problems, 10 in the science and technology of water-quality management, 4 in climate variability and the hydrologic cycle, 7 in institutional change in water-resources management, and 3 in miscellaneous water-resources management problems.\r\n\r\nFor the 11 completed projects, the report gives the grant number, project title, performing organization, principal investigator(s), starting date, date of receipt of final report, and an abstract of the final report. Each project description provides the information needed to obtain a copy of the final report.\r\n\r\nThe report also contains tables showing (1) proposals received according to \r\narea of research interest, (2) grant awards and funding according to area of \r\nresearch interest, (3) proposals received according to type of submitting \r\norganization, and (4) awards and funding according to type of organization.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr89249","usgsCitation":"Lew, M., and McCoy, B.M., 1989, Water Resources Research Grant Program Project Descriptions: Fiscal Year 1988: U.S. Geological Survey Open-File Report 89-249, v, 97 p. **PUBLICATION PAGES ARE IN INCORRECT ORDER**, https://doi.org/10.3133/ofr89249.","productDescription":"v, 97 p. **PUBLICATION PAGES ARE IN INCORRECT ORDER**","temporalStart":"1987-10-01","temporalEnd":"1988-09-30","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":145650,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0249/report-thumb.jpg"},{"id":40615,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0249/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa3f7","contributors":{"authors":[{"text":"Lew, Melvin (compiler)","contributorId":16022,"corporation":false,"usgs":true,"family":"Lew","given":"Melvin","suffix":"(compiler)","affiliations":[],"preferred":false,"id":166035,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCoy, Beverly M.","contributorId":11620,"corporation":false,"usgs":true,"family":"McCoy","given":"Beverly","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":166034,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70171482,"text":"70171482 - 1989 - Comparison of aquifer storage coefficients computed using anisotropic and isotropic analytical models","interactions":[],"lastModifiedDate":"2016-06-01T14:00:59","indexId":"70171482","displayToPublicDate":"1989-11-29T22:30:00","publicationYear":"1989","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Comparison of aquifer storage coefficients computed using anisotropic and isotropic analytical models","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the Recent Advances in Ground-Water Hydrology, American Institute of Hydrology","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"International conference on Recent advances in ground-water hydrology","conferenceDate":"1989","publisher":"Am. Inst. Hydrol.","publisherLocation":"Minneapolis, MN","usgsCitation":"Quinones-Aponte, V., 1989, Comparison of aquifer storage coefficients computed using anisotropic and isotropic analytical models, in Proceedings of the Recent Advances in Ground-Water Hydrology, American Institute of Hydrology, 1989, p. 349-357.","productDescription":"9 p.","startPage":"349","endPage":"357","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":156,"text":"Caribbean Water Science Center","active":true,"usgs":true}],"links":[{"id":322024,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57500736e4b0ee97d51bb3d4","contributors":{"authors":[{"text":"Quinones-Aponte, Vicente","contributorId":48552,"corporation":false,"usgs":true,"family":"Quinones-Aponte","given":"Vicente","email":"","affiliations":[],"preferred":false,"id":631266,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70170443,"text":"70170443 - 1989 - Hydrologic and water-quality characteristics of a Wetland receiving wastewater effluent in St. Joseph, Minnesota","interactions":[],"lastModifiedDate":"2018-03-05T12:13:22","indexId":"70170443","displayToPublicDate":"1989-11-01T15:15:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3750,"text":"Wetlands","onlineIssn":"1943-6246","printIssn":"0277-5212","active":true,"publicationSubtype":{"id":10}},"title":"Hydrologic and water-quality characteristics of a Wetland receiving wastewater effluent in St. Joseph, Minnesota","docAbstract":"Hydrologic and water-quality characteristics were determined for a wetland being used for tertiary treatment of wastewater in St. Joseph, Minnesota. The wetland consists of spruce-tamarack fen and a cattail marsh, with the wastewater being discharged into the fen, and the fen draining into the marsh. The wetland is underlain by flat-lying glacial outwash that ranges from 0 to greater than 20 m in thickness. Horizontal ground-water movement in the outwash aquifer is toward the wetland from the south, east, and west. There is a strong upward vertical hydraulic gradient (about 0.1) in the ground-water flow system beneath and around the wetland. Regionally, the glacial-outwash aquifer is unconfined, but it is confined or partly confined locally by peat deposits under the wetland. Analysis of the hydrologic balance of the fen from October 1985 through September 1986 indicates that the inflow was 44 percent ground water, 38 percent wastewater, 11 percent runoff (storm sewer), and 7 percent precipitation. The fen outflow was 93 percent surface water and 7 percent evapotranspiration. Inflow to the marsh was 74 percent surface water, 21 percent ground water, and 5 percent precipitation. Outflow from the marsh was 94 percent surface water and 6 percent evapotranspiration. Wastewater contributed 74,996, and 81 percent of the total suspended solids, total phosphorus, and total ammonia plus organic nitrogen in the fen, respectively. Other chemical inputs were from the storm sewer, ground water, and atmospheric deposition. The fen was found to retain 34, 14, and 14 percent of the suspended solids, total phosphorus, and total ammonia plus organic nitrogen, respectively. The marsh retained 44, 18, and 22 percent of these three constituents, respectively.
","language":"English","publisher":"Society of Wetland Scientists","publisherLocation":"McClean, VA","doi":"10.1007/BF03160744","usgsCitation":"Brown, R.G., and Stark, J.R., 1989, Hydrologic and water-quality characteristics of a Wetland receiving wastewater effluent in St. Joseph, Minnesota: Wetlands, v. 9, no. 2, p. 191-206, https://doi.org/10.1007/BF03160744.","productDescription":"16 p.","startPage":"191","endPage":"206","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":320317,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","city":"St. Joseph","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -94.36946868896484,\n 45.51909783811403\n ],\n [\n -94.36946868896484,\n 45.600347177025895\n ],\n [\n -94.24278259277344,\n 45.600347177025895\n ],\n [\n -94.24278259277344,\n 45.51909783811403\n ],\n [\n -94.36946868896484,\n 45.51909783811403\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"9","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5718a843e4b0ef3b7caba59c","contributors":{"authors":[{"text":"Brown, Rob G.","contributorId":68888,"corporation":false,"usgs":true,"family":"Brown","given":"Rob","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":627222,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stark, James R. stark@usgs.gov","contributorId":289,"corporation":false,"usgs":true,"family":"Stark","given":"James","email":"stark@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":627223,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70185886,"text":"70185886 - 1989 - Evaluation of inflow to Mirror Lake, New Hampshire","interactions":[],"lastModifiedDate":"2020-01-12T11:13:46","indexId":"70185886","displayToPublicDate":"1989-10-01T00:00:00","publicationYear":"1989","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":"Evaluation of inflow to Mirror Lake, New Hampshire","docAbstract":"Measured stream discharge plus calculated ground water discharge (total measured runoff) were compared with runoff calculated by the unit-runoff method for the two largest watersheds of Mirror Lake for 1981–1983. Runoff calculated by the unit-runoff method, using Hubbard Brook watershed 3 as the index watershed, was greater than the total measured runoff into Mirror Lake during periods of high flow and slightly less than the total measured runoff into Mirror Lake during periods of low flow. Annual calculated unit runoff was 17 to 37 percent greater than total measured runoff. Differences in monthly runoff are far greater, ranging from 0 to greater than 100 percent. For high flows the calculated unit runoff is about 2 times greater than total measured runoff. For low flows the northwest basin of Mirror Lake has the greatest ground water contribution compared to the other two basins. In contrast, Hubbard Brook watershed 3 has the least ground water contribution.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1752-1688.1989.tb05413.x","usgsCitation":"Winter, T.C., Eaton, J., and Likens, G., 1989, Evaluation of inflow to Mirror Lake, New Hampshire: Journal of the American Water Resources Association, v. 25, no. 5, p. 991-1008, https://doi.org/10.1111/j.1752-1688.1989.tb05413.x.","productDescription":"18 p.","startPage":"991","endPage":"1008","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338634,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Hampshire","otherGeospatial":"Mirror Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.2822151184082,\n 43.608736628843445\n ],\n [\n -71.25097274780272,\n 43.608736628843445\n ],\n [\n -71.25097274780272,\n 43.63545396386518\n ],\n [\n -71.2822151184082,\n 43.63545396386518\n ],\n [\n -71.2822151184082,\n 43.608736628843445\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"25","issue":"5","noUsgsAuthors":false,"publicationDate":"2007-06-08","publicationStatus":"PW","scienceBaseUri":"58dcc820e4b02ff32c685742","contributors":{"authors":[{"text":"Winter, T. C.","contributorId":23485,"corporation":false,"usgs":true,"family":"Winter","given":"T.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":687001,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eaton, J.S.","contributorId":190048,"corporation":false,"usgs":false,"family":"Eaton","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":687002,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Likens, G.E.","contributorId":68893,"corporation":false,"usgs":true,"family":"Likens","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":687003,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70122966,"text":"70122966 - 1989 - Riparian ecosystem creation and restoration: a literature summary","interactions":[],"lastModifiedDate":"2014-08-29T14:59:09","indexId":"70122966","displayToPublicDate":"1989-09-01T14:55:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesNumber":"Biological Report 89(20)","title":"Riparian ecosystem creation and restoration: a literature summary","docAbstract":"Riparian ecosystems generally compose a minor proportion of surrounding\nareas, but typically are more structurally diverse and more productive in plant\nand animal biomass than adjacent upland areas. Riparian areas supply food,\ncover, and water (especially important in the arid West) for a large diversity\nof animals, and serve as migration routes and forest connectors between habitats\nfor a variety of wildlife, particularly ungulates and birds.
\nBecause riparian ecosystems often are relatively small areas and occur in\nconjunction with waterways, they are vulnerable to severe alteration. Riparian\necosystems throughout the U.S. have been heavily impacted by man's activities.\nRiparian ecosystem creation and restoration have been used as mitigation for\nproject impacts from highway, bridge, and pipeline construction; water\ndevelopment; flood control channel modifications; industrial and residential\ndevelopment; agriculture; irrigation; livestock grazing; mining; and accidental\nhabitat loss.
\nCreation of a riparian ecosystem in| a more mesic upland area (e.g.,\n‘grassland or cropland) adjacent to a river requires appropriate water supply and\ngrading the topography to suitable elevations to support plantings of riparian\nvegetation. Restoration involves returning the ecosystem to pre disturbance\nconditions and typically implies revegetation. Removing exotic vegetation or\nrestoring water supplies to pre disturbance level also may be involved.\nEnhancement of riparian ecosystems commonly refers to improving existing\nconditions to increase habitat value, usually by increasing plant or community\ndiversity to increase value for wildlife. Managing a riparian ecosystem\ntypically involves enhancement techniques. However, creation and restoration\nprojects often involve use of techniques considered more management-oriented\n(e.g., fencing to prevent cattle grazing until planted vegetation of a created\nor restored wetland is established).
\nProtection of an existing riparian ecosystem from impact should be of\nutmost importance during planning and construction phases of development\nprojects. If loss or damage is unavoidable, wetland creation or restoration\ncan be used as mitigation. Compared to other wetland types (e.g., coastal\nwetlands), projects and techniques involving creation or restoration of riparian\necosystems are not well documented. For example, only 8% of the records in the\nWCR Data Base contained information on riparian ecosystems, whereas 31% of the\nrecords contained information on coastal emergent or forested ecosystems. To\nprovide a source of currently available literature, riparian information from\n92 records (primarily published papers or reports) in the U.S. Fish and Wildlife\nService's (FWS) Wetland Creation-Restoration (WCR) Data Base (Schneller-McDonald\net al. 1988) was used to develop a literature summary of creation and restoration\nof riparian ecosystems.
\nThe summary provides an overview of the status of riparian ecosystems in\nthe U.S., a discussion of several riparian functions, and a review of some\ntechniques used for planning, implementing, monitoring, and measuring project\nsuccess of creation-restoration efforts. Case studies of various creation or\nrestoration projects are used to demonstrate these techniques and to report some\nresults of their use. Several well-documented case studies are discussed in\ndetail to illustrate more extensive efforts to plan, implement, or monitor\nriparian ecosystem creation-restoration projects.
\nFor the purpose of this report, riparian ecosystems are defined as\nlandscapes adjacent to drainageways of floodplains that exhibit vegetation, soil,\nand hydrologic mosaics along topographic and moisture gradients that are distinct\nfrom the predominant landscape surface types. Major plant communities are\ndescribed under palustrine system in Cowardin et al. (1979).
\nLiterature from the WCR Data Base was used to provide a summary of riparian\necosystem creation-restoration literature. Thus, information concerning natural\nsystems is not included unless discussed in these articles. This focus allows\nthe reader to compare relative information available on riparian ecosystem\ncreation-restoration efforts. However, this focus also results in limited\ninformation in some sections of the report (e.g., Status of Riparian Ecosystems\nin the U.S.).
\nIndividuals involved in riparian ecosystem creation-restoration efforts\nare encouraged to thoroughly examine available literature on natural and altered\nsystems. Brinson et al. (1981) provide a comprehensive review and synthesis of\nthe ecology and status of riparian ecosystems. Over 500 articles are cited in\ntheir 124-page report. Chapters include the following topics: status of\nriparian ecosystems in the U.S., ecological functions and properties of riparian\necosystems (e.g., geomorphology, primary productivity, nutrient cycling,\nhydrology), importance of riparian ecosystems to fish and wildlife, and\nconsiderations in valuation (ecologic and economic) of riparian ecosystems.\nBrinson et al. (1981) also discuss management of riparian ecosystems. Riparian\necosystem management literature was not included in the WCR Data Base, unless\nthe article also discussed creation or restoration.
","language":"English","publisher":"U.S. Dept. of the Interior, Fish and Wildlife Service, Research and Development","publisherLocation":"Washington, D.C.","usgsCitation":"Manci, K.M., 1989, Riparian ecosystem creation and restoration: a literature summary, vi, 59 p.","productDescription":"vi, 59 p.","numberOfPages":"65","costCenters":[],"links":[{"id":293213,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"540193cfe4b0ae951d96063f","contributors":{"authors":[{"text":"Manci, Karen M.","contributorId":8389,"corporation":false,"usgs":true,"family":"Manci","given":"Karen","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":499789,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70175215,"text":"70175215 - 1989 - Selenate reduction to elemental selenium by anaerobic bacteria in sediments and culture: Biogeochemical significance of a novel, sulfate-independent respiration","interactions":[],"lastModifiedDate":"2023-01-26T16:32:25.602528","indexId":"70175215","displayToPublicDate":"1989-09-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":850,"text":"Applied and Environmental Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Selenate reduction to elemental selenium by anaerobic bacteria in sediments and culture: Biogeochemical significance of a novel, sulfate-independent respiration","docAbstract":"Interstitial water profiles of SeO42−, SeO32−, SO42−, and Cl− in anoxic sediments indicated removal of the seleno-oxyanions by a near-surface process unrelated to sulfate reduction. In sediment slurry experiments, a complete reductive removal of SeO42− occurred under anaerobic conditions, was more rapid with H2 or acetate, and was inhibited by O2, NO3−, MnO2, or autoclaving but not by SO42− or FeOOH. Oxidation of acetate in sediments could be coupled to selenate but not to molybdate. Reduction of selenate to elemental selenium was determined to be the mechanism for loss from solution. Selenate reduction was inhibited by tungstate and chromate but not by molybdate. A small quantity of the elemental selenium precipitated into sediments from solution could be resolublized by oxidation with either nitrate or FeOOH, but not with MnO2. A bacterium isolated from estuarine sediments demonstrated selenate-dependent growth on acetate, forming elemental selenium and carbon dioxide as respiratory end products. These results indicate that dissimilatory selenate reduction to elemental selenium is the major sink for selenium oxyanions in anoxic sediments. In addition, they suggest application as a treatment process for removing selenium oxyanions from wastewaters and also offer an explanation for the presence of selenite in oxic waters.
","language":"English","publisher":"American Society for Microbiology","doi":"10.1128/aem.55.9.2333-2343.1989","usgsCitation":"Oremland, R.S., Hollibaugh, J., Maest, A.S., Presser, T.S., Miller, L., and Culbertson, C.W., 1989, Selenate reduction to elemental selenium by anaerobic bacteria in sediments and culture: Biogeochemical significance of a novel, sulfate-independent respiration: Applied and Environmental Microbiology, v. 55, no. 9, p. 2333-2343, https://doi.org/10.1128/aem.55.9.2333-2343.1989.","productDescription":"11 p.","startPage":"2333","endPage":"2343","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":479872,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1128/aem.55.9.2333-2343.1989","text":"Publisher Index Page"},{"id":325974,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Joaquin Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -118.81161865745477,\n 34.87820418385651\n ],\n [\n -118.62485107932994,\n 35.166108724612116\n ],\n [\n -118.58090576682974,\n 35.426145028011504\n ],\n [\n -118.745700688705,\n 35.604993007449664\n ],\n [\n -118.66879639182977,\n 36.11251865524609\n ],\n [\n -118.9104956105799,\n 36.493233439497644\n ],\n [\n -119.15219482932972,\n 36.537381882172994\n ],\n [\n -119.20712646995467,\n 36.73133559168423\n ],\n [\n -119.54770264182997,\n 37.0213495255132\n ],\n [\n -119.88827881370489,\n 37.37140271952916\n ],\n [\n -120.0530737355798,\n 37.563239296564504\n ],\n [\n -120.47055420432966,\n 38.06662625255325\n ],\n [\n -120.69028076682986,\n 38.583751288800556\n ],\n [\n -120.99789795432974,\n 39.04600325246474\n ],\n [\n -121.21762451682964,\n 39.19941990493476\n ],\n [\n -121.4043920949548,\n 39.606895659228854\n ],\n [\n -121.89877686057986,\n 40.213637551075266\n ],\n [\n -121.66806396995466,\n 40.30586058511415\n ],\n [\n -121.55820068870472,\n 40.514990649222966\n ],\n [\n -121.94272217307952,\n 40.79836385920754\n ],\n [\n -122.32724365745464,\n 40.80668013926589\n ],\n [\n -122.9754370168295,\n 40.41468932443129\n ],\n [\n -122.87656006370469,\n 40.18007073973777\n ],\n [\n -122.70077881370466,\n 39.96990187137982\n ],\n [\n -122.6678198293296,\n 39.64074445479304\n ],\n [\n -122.67880615745472,\n 39.26749780037491\n ],\n [\n -122.28329834495446,\n 38.85804057098295\n ],\n [\n -122.07455811057972,\n 38.549391138431474\n ],\n [\n -122.0855444387045,\n 38.23941110128712\n ],\n [\n -121.7779272512046,\n 37.954096714873785\n ],\n [\n -121.65707764182955,\n 37.60676983461319\n ],\n [\n -121.51425537620455,\n 37.54581995469749\n ],\n [\n -121.29452881370466,\n 37.16156555778515\n ],\n [\n -121.01987061057947,\n 36.71372361604804\n ],\n [\n -120.77817139182966,\n 36.66967601152351\n ],\n [\n -120.43759521995472,\n 36.28097061856451\n ],\n [\n -120.4705542043292,\n 36.0602428538586\n ],\n [\n -120.12997803245426,\n 35.87351401211042\n ],\n [\n -120.11899170432947,\n 35.686344038957\n ],\n [\n -119.75644287620428,\n 35.265846284716346\n ],\n [\n -119.37192139182947,\n 34.95128398250456\n ],\n [\n -119.13022217307935,\n 34.960288315672685\n ],\n [\n -118.81161865745477,\n 34.87820418385651\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"55","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57a1c433e4b006cb45552c48","contributors":{"authors":[{"text":"Oremland, Ronald S. 0000-0001-7382-0147 roremlan@usgs.gov","orcid":"https://orcid.org/0000-0001-7382-0147","contributorId":931,"corporation":false,"usgs":true,"family":"Oremland","given":"Ronald","email":"roremlan@usgs.gov","middleInitial":"S.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":644357,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hollibaugh, James T.","contributorId":6878,"corporation":false,"usgs":true,"family":"Hollibaugh","given":"James T.","affiliations":[],"preferred":false,"id":644358,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Maest, Ann S.","contributorId":26003,"corporation":false,"usgs":true,"family":"Maest","given":"Ann","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":644359,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Presser, Theresa S. 0000-0001-5643-0147 tpresser@usgs.gov","orcid":"https://orcid.org/0000-0001-5643-0147","contributorId":2467,"corporation":false,"usgs":true,"family":"Presser","given":"Theresa","email":"tpresser@usgs.gov","middleInitial":"S.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":644360,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Miller, Laurence G. 0000-0002-7807-3475 lgmiller@usgs.gov","orcid":"https://orcid.org/0000-0002-7807-3475","contributorId":2460,"corporation":false,"usgs":true,"family":"Miller","given":"Laurence G.","email":"lgmiller@usgs.gov","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":644361,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Culbertson, Charles W. cculbert@usgs.gov","contributorId":1607,"corporation":false,"usgs":true,"family":"Culbertson","given":"Charles","email":"cculbert@usgs.gov","middleInitial":"W.","affiliations":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true}],"preferred":true,"id":644362,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70123426,"text":"70123426 - 1989 - Correspondence between vegetation and soils in wetlands and nearby uplands","interactions":[],"lastModifiedDate":"2014-09-04T13:37:40","indexId":"70123426","displayToPublicDate":"1989-06-01T13:36:37","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3750,"text":"Wetlands","onlineIssn":"1943-6246","printIssn":"0277-5212","active":true,"publicationSubtype":{"id":10}},"title":"Correspondence between vegetation and soils in wetlands and nearby uplands","docAbstract":"The association between vegetation and soils from a geographically broad sampling of wetlands and adjoining uplands is reported for 38 hydric and 26 nonhydric soils, as recognized in the hydric soils list of the Soil Conservation Service. Wetlands represented in the study include estuaries, pitcher plant bogs, prairie depressional wetlands, and western riparian lands. The agreement between vegetation and soils is clear with few exceptions. In general, hydric soils support hydrophytic plant communities, and nonhydric soils support upland communities. Only 10% of the hydric soils sampled support upland communities and only 15% of the nonhydric soils support wetland communities. Exceptions to the correspondence between vegetation and soils are discussed; local hydrology, the transitional nature of some soils, and other determinants of wetland vegetation structure (e.g., salinity, disturbance) seem to account for many of the observed discrepancies. A method that simplifies the complexity of soils and vegetation cannot be expected to represent accurately all details of their interrelations.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wetlands","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Society of Wetland Scientists","publisherLocation":"McClean, VA","doi":"10.1007/BF03160767","usgsCitation":"Scott, M.L., Slauson, W.L., Segelquist, C.A., and Auble, G.T., 1989, Correspondence between vegetation and soils in wetlands and nearby uplands: Wetlands, v. 9, no. 1, p. 41-60, https://doi.org/10.1007/BF03160767.","productDescription":"20 p.","startPage":"41","endPage":"60","numberOfPages":"20","costCenters":[],"links":[{"id":293406,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":293405,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF03160767"}],"volume":"9","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"542a74c3e4b01535cb42757b","contributors":{"authors":[{"text":"Scott, Michael L. scottm@usgs.gov","contributorId":1169,"corporation":false,"usgs":true,"family":"Scott","given":"Michael","email":"scottm@usgs.gov","middleInitial":"L.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":500112,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Slauson, William L.","contributorId":78652,"corporation":false,"usgs":true,"family":"Slauson","given":"William","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":500115,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Segelquist, Charles A.","contributorId":27368,"corporation":false,"usgs":true,"family":"Segelquist","given":"Charles","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":500114,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Auble, Gregor T. 0000-0002-0843-2751 aubleg@usgs.gov","orcid":"https://orcid.org/0000-0002-0843-2751","contributorId":2187,"corporation":false,"usgs":true,"family":"Auble","given":"Gregor","email":"aubleg@usgs.gov","middleInitial":"T.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":500113,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70123398,"text":"70123398 - 1989 - Stream temperature investigations: field and analytic methods","interactions":[],"lastModifiedDate":"2014-09-04T11:18:57","indexId":"70123398","displayToPublicDate":"1989-06-01T11:13:37","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesNumber":"Biological Report 89(17)","title":"Stream temperature investigations: field and analytic methods","docAbstract":"This document provides guidance to the user of the U.S. Fish and Wildlife Service’s Stream Network Temperature Model (SNTEMP). Planning a temperature study is discussed in terms of understanding the management objectives and ensuring that the questions will be accurately answered with the modeling approach being used.
\nA sensitivity analysis of SNTEMP is presented to illustrate which input variables are most important in predicting stream temperatures. This information helps prioritize data collection activities, highlights the need for quality control, focuses on which parameters can be estimated rather than measured, and offers a broader perspective on management options in terms of knowing where the biggest temperature response will be felt.
\nAll of the major input variables for stream geometry, meteorology, and hydrology are discussed in detail. Each variable is defined, with guidance given on how to measure it, what kind of equipment to use, where to obtain it from another agency, and how to calculate it if the data are in a form other than that required by SNTEMP. Examples are presented for the various forms in which water temperature, discharge, and meteorological data are commonly found. Ranges of values for certain input variables that are difficult to measure of estimate are given. Particular attention is given to those variables not commonly understood by field biologists likely to be involved in a stream temperature study. Pertinent literature is cited for each variable, with emphasis on how other people have treated particular problems and on results they have found.
\nSome special cases dealing with ice and reservoir temperature are mentioned. Special attention is given to understanding micro-thermal habitats that act as important thermal refugia under low flow conditions; their causes, extent, and management implications are discussed.
\nAppendices provide information on State and Federal agencies that are good data sources, vendors for field instrumentation, and small computer programs useful in data reduction.
","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, D.C.","usgsCitation":"Bartholow, J., 1989, Stream temperature investigations: field and analytic methods, 139 p.","productDescription":"139 p.","numberOfPages":"139","costCenters":[],"links":[{"id":293379,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"542a7550e4b01535cb427bb5","contributors":{"authors":[{"text":"Bartholow, J.M.","contributorId":54530,"corporation":false,"usgs":true,"family":"Bartholow","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":500081,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70123427,"text":"70123427 - 1989 - Physical habitat simulation and sedimentation","interactions":[],"lastModifiedDate":"2014-09-04T13:39:37","indexId":"70123427","displayToPublicDate":"1989-05-01T13:38:00","publicationYear":"1989","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":12,"text":"Conference publication"},"title":"Physical habitat simulation and sedimentation","docAbstract":"No abstract available.","largerWorkTitle":"Proceedings of the Symposium Sediment and the Environment, the Third Scientific Assembly of the International Association of Hydrological Sciences","conferenceTitle":"Sediment and the environment","conferenceDate":"1989-05-01T00:00:00","conferenceLocation":"Baltimore, MD","language":"English","publisher":"IAHS Press","publisherLocation":"Wallingford","usgsCitation":"Milhous, R.T., 1989, Physical habitat simulation and sedimentation, 8 p.","productDescription":"8 p.","numberOfPages":"8","costCenters":[],"links":[{"id":293407,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"542a7511e4b01535cb4279dc","contributors":{"authors":[{"text":"Milhous, Robert T.","contributorId":28646,"corporation":false,"usgs":true,"family":"Milhous","given":"Robert","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":500116,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70123419,"text":"70123419 - 1989 - Hydraulics in physical habitat simulation: a 1989 review","interactions":[],"lastModifiedDate":"2014-09-04T13:11:10","indexId":"70123419","displayToPublicDate":"1989-04-21T13:09:55","publicationYear":"1989","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":12,"text":"Conference publication"},"title":"Hydraulics in physical habitat simulation: a 1989 review","docAbstract":"No abstract available.","largerWorkTitle":"Proceedings of the Ninth Annual AGU Front Range Branch Hydrology Days","conferenceTitle":"Ninth Annual AGU Front Range Branch Hydrology Days","conferenceDate":"1989-04-18T00:00:00","conferenceLocation":"Fort Collins, CO","language":"English","publisher":"Hydrology Days Publications","publisherLocation":"Fort Collins, CO","usgsCitation":"Milhous, R.T., 1989, Hydraulics in physical habitat simulation: a 1989 review, 2 p.","productDescription":"2 p.","numberOfPages":"2","costCenters":[],"links":[{"id":293400,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"542a74eae4b01535cb42779b","contributors":{"authors":[{"text":"Milhous, Robert T.","contributorId":28646,"corporation":false,"usgs":true,"family":"Milhous","given":"Robert","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":500105,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70015546,"text":"70015546 - 1989 - Regression models for estimating urban storm-runoff quality and quantity in the United States","interactions":[],"lastModifiedDate":"2025-04-24T16:38:47.224298","indexId":"70015546","displayToPublicDate":"1989-04-14T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Regression models for estimating urban storm-runoff quality and quantity in the United States","docAbstract":"Urban planners and managers need information about the local quantity of precipitation and the quality and quantity of storm runoff if they are to plan adequately for the effects of storm runoff from urban areas. As result of this need, linear regression models were developed for the estimation of storm-runoff loads and volumes from physical, land-use, and climatic characteristics of urban watersheds throughout the United States. Three statistically different regions were delineated, based on mean annual rainfall, to improve linear regression models. One use of these models is to estimate storm-runoff loads and volumes are gaged and ungaged urban watersheds.
The most significant explanatory variables in all linear regression models were total storm rainfall and total contributing drainage area. Impervious area, land-use, and mean annual climatic characteristics were also significant explanatory variables in some linear regression models. Models for dissolved solids, total nitrogen, and total ammonia plus organic nitrogen as nitrogen were the most accurate models for most areas, whereas models for suspended solids were the least accurate. The most accurate models were those for the more arid western United States, and the least accurate were those for areas that had large quantities of mean annual rainfall.
","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(89)90017-6","issn":"00221694","usgsCitation":"Driver, N.E., and Troutman, B., 1989, Regression models for estimating urban storm-runoff quality and quantity in the United States: Journal of Hydrology, v. 109, no. 3-4, p. 221-236, https://doi.org/10.1016/0022-1694(89)90017-6.","productDescription":"16 p.","startPage":"221","endPage":"236","costCenters":[],"links":[{"id":224159,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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States\"}}]}","volume":"109","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e4a5d0e4b0e8fec6cdc00e","contributors":{"authors":[{"text":"Driver, N. E.","contributorId":63398,"corporation":false,"usgs":true,"family":"Driver","given":"N.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":371198,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Troutman, B.M.","contributorId":73638,"corporation":false,"usgs":true,"family":"Troutman","given":"B.M.","email":"","affiliations":[],"preferred":false,"id":371199,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70015607,"text":"70015607 - 1989 - Snow cover of the Upper Colorado River Basin from satellite passive microwave and visual imagery","interactions":[],"lastModifiedDate":"2025-05-22T15:43:06.204483","indexId":"70015607","displayToPublicDate":"1989-04-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2880,"text":"Nordic Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Snow cover of the Upper Colorado River Basin from satellite passive microwave and visual imagery","docAbstract":"A comparison of passive microwave images from the Nimbus-7 Scanning Multichannel Microwave Radiometer (SMMR) and visual images from the Defense Meteorological Satellite Program (DMSP) of the Upper Colorado River Basin shows that passive microwave satellite imagery can be used to determine the extent of the snow cover. Eight cloud-free DMSP images throughout the winter of 1985-1986 show the extent of the snowpack, which, when compared to the corresponding SMMR images, determine the threshold microwave characteristics for snow-covered pixels. With these characteristics, the 27 sequential SMMR images give a unique view of the temporal history of the snow cover extent through the first half of the water year. Beginning mid-November, the snow-covered area rapidly increases from near zero to 80 percent by the middle of January. During late February the snow-covered area decreases as a result of basin-wide warming. The microwave determinations initially overestimate the decrease in snow cover, as a result of liquid water in the snowpack, but the return of cooler temperatures restores the veracity of the passive microwave determinations.
","language":"English","publisher":"IWA Publishing","doi":"10.2166/nh.1989.0006","issn":"00291277","usgsCitation":"Josberger, E., and Beauvillain, E., 1989, Snow cover of the Upper Colorado River Basin from satellite passive microwave and visual imagery: Nordic Hydrology, v. 20, no. 2, p. 73-84, https://doi.org/10.2166/nh.1989.0006.","productDescription":"12 p.","startPage":"73","endPage":"84","costCenters":[],"links":[{"id":490147,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2166/nh.1989.0006","text":"Publisher Index Page"},{"id":224323,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah, Wyoming","otherGeospatial":"Upper Colorado River Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -110.50635197912666,\n 43.09070038977103\n ],\n [\n -111.24806206301143,\n 40.996826941047615\n ],\n [\n -111.68033570473634,\n 39.51165818243791\n ],\n [\n -109.8495981109781,\n 39.31181965625984\n ],\n [\n -109.26235421062083,\n 42.9435236465097\n ],\n [\n -110.50635197912666,\n 43.09070038977103\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"20","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b91b3e4b08c986b319a47","contributors":{"authors":[{"text":"Josberger, E.G.","contributorId":61161,"corporation":false,"usgs":true,"family":"Josberger","given":"E.G.","email":"","affiliations":[],"preferred":false,"id":371354,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beauvillain, E.","contributorId":47918,"corporation":false,"usgs":true,"family":"Beauvillain","given":"E.","email":"","affiliations":[],"preferred":false,"id":371353,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70185851,"text":"70185851 - 1989 - Irrigation-induced contamination--How real a problem","interactions":[],"lastModifiedDate":"2020-01-12T10:47:33","indexId":"70185851","displayToPublicDate":"1989-02-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5351,"text":"Journal on Irrigation Drainage Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Irrigation-induced contamination--How real a problem","docAbstract":"The U.S. Department of the Interior has embarked on a series of reconnaissance‐level investigations throughout the western states to identify, evaluate, and respond to irrigation‐induced water quality problems. A series of water, sediment, and biological samples are being analyzed for 17 inorganic constituents and a number of pesticides. 19 studies in 13 states have been undertaken. Seven have been completed to date. Results of the seven studies that have been completed are presented and compared to baselines, standards, criteria, and other guidelines helpful for assessing the potential of observed constituent concentrations in water, bottom sediment, and biota, to result in physiological harm to fish, wildlife, or humans. These initial results indicate that a new environmental problem of major proportions does not exist, but that some localized problems of significant magnitude do exist and should be addressed.
","language":"English","publisher":"American Society of Civil Engineers","doi":"10.1061/(ASCE)0733-9437(1989)115:1(9)","usgsCitation":"Deason, J.P., 1989, Irrigation-induced contamination--How real a problem: Journal on Irrigation Drainage Engineering, v. 115, no. 1, https://doi.org/10.1061/(ASCE)0733-9437(1989)115:1(9).","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338615,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"115","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58dcc820e4b02ff32c685744","contributors":{"authors":[{"text":"Deason, Jonathan P.","contributorId":69299,"corporation":false,"usgs":true,"family":"Deason","given":"Jonathan","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":686914,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":748,"text":"748 - 1989 - U.S. Geological Survey state water-data reports water year 1987-: hydrologic records of the United States","interactions":[],"lastModifiedDate":"2014-08-05T15:17:34","indexId":"748","displayToPublicDate":"1989-01-01T15:15:56","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"U.S. Geological Survey state water-data reports water year 1987-: hydrologic records of the United States","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/748","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1989, U.S. Geological Survey state water-data reports water year 1987-: hydrologic records of the United States, computer laser optical disks, https://doi.org/10.3133/748.","productDescription":"computer laser optical disks","costCenters":[],"links":[{"id":291727,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e1efdfe4b0fe532be2dea1","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527682,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70100276,"text":"70100276 - 1989 - Subsurface-water flow and solute transport: federal glossary of selected terms","interactions":[],"lastModifiedDate":"2015-10-22T10:16:01","indexId":"70100276","displayToPublicDate":"1989-01-01T12:37:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Subsurface-water flow and solute transport: federal glossary of selected terms","docAbstract":"The purpose of this report is to provide a glossary of selected terms for saturated and unsaturated flow and related processes involved in transport of contaminants in the subsurface. The glossary contains five tables. Table 1 is a list of parameters with associated symbols and units. Tables 2 to 5 are conversion charts. The original manuscript was prepared by Thomas J. Nicholson, U.S. Nuclear Regulatory Commission. It was subsequently examined by the Ground-Water Glossary Working Group and experts within and outside the Federal Government, whose recommendations were accommodated where appropriate in the glossary. It is hoped that the glossary will aid in the communications between soil scientists, hydrologists, and hydrogeologists.
\nThe terms defined in the glossary were selected after an extensive survey of glossaries and reports in the areas of (1) ground-water geology, hydraulics, and chemistry, (2) soil-water physics and chemistry, (3) contaminant transport, (4) unsaturated-zone hydrology, (5) chemistry and transport of solutes, and (6) ground-water quality. Some of the definitions have been modified for clarity from a variety of technical sources. Where more than one definition appears for the selected term, the first one was determined by the working group to be the most appropriate general definition, followed by other, more specialized, definitions. Some terms and definitions are not currently in use by all agencies; however, they are included in the glossary because they can be found in the literature. The reader is encouraged to consult with the original source cited for more explanatory comments. Additional regulatory definitions, which are underlined and are taken directly from the Code of Federal Regulations (CFR) and Federal laws (USC), were added following review by the various Federal agencies in May 1986.
\nThe definitions and conversion charts are from two principal sources provided herein. The first is the 11Glossary11 compiled by A. I. Johnson in the 1981 report by the American Society of Testing and Materials titled Permeability and Groundwater Contaminant Transport. The second is Manu a 1 40, 11Ground-water Management, 11 produced by the American Society of Civil Engineers in 1985.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70100276","usgsCitation":"Isensee, A.R., Johnson, L., Thornhill, J., Nicholson, T.J., Meyer, G., Vecchioli, J., and Laney, R., 1989, Subsurface-water flow and solute transport: federal glossary of selected terms, iii, 38 p., https://doi.org/10.3133/70100276.","productDescription":"iii, 38 p.","numberOfPages":"46","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":309917,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70100276.PNG"},{"id":310364,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70100276/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53559597e4b0120853e8c232","contributors":{"authors":[{"text":"Isensee, Alan R.","contributorId":149234,"corporation":false,"usgs":false,"family":"Isensee","given":"Alan","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":577569,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Lynn","contributorId":149235,"corporation":false,"usgs":false,"family":"Johnson","given":"Lynn","affiliations":[],"preferred":false,"id":577570,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thornhill, Jerry","contributorId":149236,"corporation":false,"usgs":false,"family":"Thornhill","given":"Jerry","email":"","affiliations":[],"preferred":false,"id":577571,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nicholson, Thomas J.","contributorId":77790,"corporation":false,"usgs":true,"family":"Nicholson","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":577572,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Meyer, Gerald","contributorId":76721,"corporation":false,"usgs":true,"family":"Meyer","given":"Gerald","email":"","affiliations":[],"preferred":false,"id":577573,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Vecchioli, John","contributorId":36113,"corporation":false,"usgs":true,"family":"Vecchioli","given":"John","email":"","affiliations":[],"preferred":false,"id":577574,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Laney, Robert","contributorId":149237,"corporation":false,"usgs":false,"family":"Laney","given":"Robert","email":"","affiliations":[],"preferred":false,"id":577575,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":70006521,"text":"70006521 - 1989 - Hydrological, morphometrical, and biological characteristics of the connecting rivers of the International Great Lakes: a review","interactions":[],"lastModifiedDate":"2019-08-23T11:09:57","indexId":"70006521","displayToPublicDate":"1989-01-01T10:26:18","publicationYear":"1989","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":12,"text":"Conference publication"},"seriesTitle":{"id":429,"text":"Canadian Special Publication of Fisheries and Aquatic Sciences","active":false,"publicationSubtype":{"id":12}},"title":"Hydrological, morphometrical, and biological characteristics of the connecting rivers of the International Great Lakes: a review","docAbstract":"The connecting channels of the Great Lakes are large rivers (1, 200-9, 900 m3 • s-1) with limited tributary drainage systems and relatively stable hydrology (about 2:1 ration of maximum to minimum flow). The rivers, from headwaters to outlet, are the St. Marys, St. Clair, Detroit, Niagara, and St. Lawrence. They share several characteristics with certain other large rivers: the fish stocks that historically congregated for spawning or feeding have been overfished, extensive channel modification have been made, and they have been used as a repository for domestic and industrial wastes and for hydroelectric energy generation. Levels of phosphorus, chlorophyll a, and particulate organic matter increase 3- to 5-fold from the St. Marys River to the St. Lawrence River. Biological communities dependent on nutrients in the water column, such as phytoplankton, periphyton, and zooplankton similarly increase progressively downstream through the system. The standing crop of emergent macrophytes is similar in all of the rivers, reflecting the relatively large nutrient pools in the sediments and atmosphere. Consequently, emergent macrophytes are an important source of organic matter (67% of total primary production) in the nutrient poor waters of the St. Marys River, whereas phytoplankton production dominates (76%) in the enriched St. Lawrence River. Submersed and emergent macrophytes and the associated periphyton are major producers of organic matter in the connecting channels. Another major source of organic matter (measured as ash free dry weight, AFDW) in the Detroit River is sewage, introduced at a rate of 26, 000 t per year. The production of benthos ranges from a low 5.4 g AFDW•m-2 in the Detroit River to a high of 15.5 g AFDW•m-2 in the St. Marys River. The rivers lack the organic transport from riparian sources upstream but receive large amounts of high quality phytoplankton and zooplankton from the Great Lakes.
","largerWorkTitle":"Proceedings of the International Large River Symposium","conferenceTitle":"Proceedings of the International Large River Symposium","language":"English","publisher":"Canadian Special Publication of Fisheries and Aquatic Sciences","usgsCitation":"Edwards, C.J., Hudson, P.L., Duffy, W.G., Nepszy, S.J., McNabb, C.D., Haas, R.C., Liston, C.R., Manny, B., and Busch, W.N., 1989, Hydrological, morphometrical, and biological characteristics of the connecting rivers of the International Great Lakes: a review: Canadian Special Publication of Fisheries and Aquatic Sciences, 25 p.","productDescription":"25 p.","startPage":"240","endPage":"264","numberOfPages":"25","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true},{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"links":[{"id":289184,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53b286f1e4b07b8813a554c4","contributors":{"editors":[{"text":"Dodge, D.P.","contributorId":112637,"corporation":false,"usgs":true,"family":"Dodge","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":508345,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Edwards, Clayton J.","contributorId":99897,"corporation":false,"usgs":true,"family":"Edwards","given":"Clayton","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":354674,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hudson, Patrick L. 0000-0002-7646-443X phudson@usgs.gov","orcid":"https://orcid.org/0000-0002-7646-443X","contributorId":5616,"corporation":false,"usgs":true,"family":"Hudson","given":"Patrick","email":"phudson@usgs.gov","middleInitial":"L.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":354666,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Duffy, Walter G. wgd7001@usgs.gov","contributorId":66750,"corporation":false,"usgs":true,"family":"Duffy","given":"Walter","email":"wgd7001@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":false,"id":354671,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nepszy, Stephen J.","contributorId":40548,"corporation":false,"usgs":true,"family":"Nepszy","given":"Stephen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":354668,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"McNabb, Clarence D.","contributorId":34977,"corporation":false,"usgs":true,"family":"McNabb","given":"Clarence","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":354667,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Haas, Robert C.","contributorId":97450,"corporation":false,"usgs":true,"family":"Haas","given":"Robert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":354673,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Liston, Charles R.","contributorId":71603,"corporation":false,"usgs":true,"family":"Liston","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":354672,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Manny, Bruce","contributorId":49275,"corporation":false,"usgs":true,"family":"Manny","given":"Bruce","affiliations":[],"preferred":false,"id":354670,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Busch, Wolf-Dieter N.","contributorId":46039,"corporation":false,"usgs":true,"family":"Busch","given":"Wolf-Dieter","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":354669,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":70199824,"text":"70199824 - 1989 - Transport and degradation of water-soluble creosote-derived compounds","interactions":[],"lastModifiedDate":"2018-11-20T12:48:02","indexId":"70199824","displayToPublicDate":"1989-01-01T10:16:16","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Transport and degradation of water-soluble creosote-derived compounds","docAbstract":"Creosote is the most extensively used insecticide and industrial wood preservative today. It is estimated that there are more than 600 wood-preserving plants in the United States, and their collective use of creosote exceeds 4.5xl06 kg/yr (von Rumker et al., 1975). Creosote is a complex mixture of more than 200 major individual organic compounds with differing molecular weights, polarities, and functionalities, along with dispersed solids and products of polymerization (Novotny et al., 1981). The major classes of compounds previously identified in creosote show that it consists of ∼85% (w/w) polynuclear aromatic compounds (PAH), ∼12% phenolic compounds, and ∼3% heterocyclic nitrogen, sulfur, and oxygen containing compounds (NSO).
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Intermedia pollutant transport: Modeling and field measurements ","language":"English","publisher":"Plenum","usgsCitation":"Godsy, E.M., Goerlitz, D., and Grbic-Galic, D., 1989, Transport and degradation of water-soluble creosote-derived compounds, chap. of Intermedia pollutant transport: Modeling and field measurements , p. 213-236.","productDescription":"24 p.","startPage":"213","endPage":"236","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":359610,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.springer.com/us/book/9780306432576"},{"id":357933,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5bf52b6ce4b045bfcae2802a","contributors":{"editors":[{"text":"Allen, D.","contributorId":86955,"corporation":false,"usgs":true,"family":"Allen","given":"D.","email":"","affiliations":[],"preferred":false,"id":746804,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Godsy, E. Michael","contributorId":45842,"corporation":false,"usgs":true,"family":"Godsy","given":"E.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":746801,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goerlitz, D.F.","contributorId":8445,"corporation":false,"usgs":true,"family":"Goerlitz","given":"D.F.","affiliations":[],"preferred":false,"id":746802,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grbic-Galic, Dunja","contributorId":33463,"corporation":false,"usgs":true,"family":"Grbic-Galic","given":"Dunja","email":"","affiliations":[],"preferred":false,"id":746803,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70199823,"text":"70199823 - 1989 - Theoretical considerations of the partition uptake of nonionic organic compounds by soil organic matter","interactions":[],"lastModifiedDate":"2018-10-01T10:12:08","indexId":"70199823","displayToPublicDate":"1989-01-01T10:10:05","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Theoretical considerations of the partition uptake of nonionic organic compounds by soil organic matter","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Reactions and movement of organic chemicals in soils","language":"English","publisher":"Soil Science Society of America","publisherLocation":"Madison, Wisconsin","usgsCitation":"Chiou, C.T., 1989, Theoretical considerations of the partition uptake of nonionic organic compounds by soil organic matter, chap. of Reactions and movement of organic chemicals in soils, p. 1-29.","productDescription":"29 p.","startPage":"1","endPage":"29","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":357932,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5c112c64e4b034bf6a822741","contributors":{"editors":[{"text":"Sawhney, B.J.","contributorId":208341,"corporation":false,"usgs":false,"family":"Sawhney","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":746799,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Brown, K.","contributorId":49166,"corporation":false,"usgs":true,"family":"Brown","given":"K.","affiliations":[],"preferred":false,"id":746800,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Chiou, C. T.","contributorId":97080,"corporation":false,"usgs":true,"family":"Chiou","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":746798,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70199822,"text":"70199822 - 1989 - Partition and adsorption on soil and mobility of organic pollutants and pesticides","interactions":[],"lastModifiedDate":"2018-10-01T10:03:33","indexId":"70199822","displayToPublicDate":"1989-01-01T10:02:17","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Partition and adsorption on soil and mobility of organic pollutants and pesticides","docAbstract":"The mechanism for sorption of organic pollutants and pesticides by soil has long been a subject of profound interest because of its direct impacts on the mobility and activity of the compounds in soil. Although a large volume of laboratory and field data on many aspects of soil behavior had been gathered between the 1950s and 1970s, during which period the use of organic pesticides was increased, no general agreement was reached regarding the sorptive mechanism involved. Since the 1970s, the outgrowth of public concern over environmental contamination further stimulated research in this subject. The development of this field of research has now reached a point that the diverse characteristics of soil sorption can be placed in a much better perspective. This enables researchers to reexamine old and new data for consistency and for assessing the activity of organic pollutants and pesticides in soil.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Toxic organic chemicals in porous media","language":"English","publisher":"Springer","publisherLocation":"Berlin, Heidelberg","doi":"10.1007/978-3-642-74468-6_7","usgsCitation":"Chiou, C.T., 1989, Partition and adsorption on soil and mobility of organic pollutants and pesticides, chap. of Toxic organic chemicals in porous media, p. 163-175, https://doi.org/10.1007/978-3-642-74468-6_7.","productDescription":"13 p.","startPage":"163","endPage":"175","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":357931,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5c112c65e4b034bf6a822744","contributors":{"authors":[{"text":"Chiou, C. T.","contributorId":97080,"corporation":false,"usgs":true,"family":"Chiou","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":746797,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70198774,"text":"70198774 - 1989 - Aqueous equilibrium data for a mononuclear aluminum species","interactions":[],"lastModifiedDate":"2018-08-17T09:18:39","indexId":"70198774","displayToPublicDate":"1989-01-01T09:17:17","publicationYear":"1989","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Aqueous equilibrium data for a mononuclear aluminum species","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The environmental chemistry of aluminum","language":"English","publisher":"CRC Press","publisherLocation":"Boca Raton, Florida ","usgsCitation":"Nordstrom, D.K., and May, H.M., 1989, Aqueous equilibrium data for a mononuclear aluminum species, chap. of The environmental chemistry of aluminum, p. 27-53.","productDescription":"27 p.","startPage":"27","endPage":"53","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":356575,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5c112c65e4b034bf6a822746","contributors":{"editors":[{"text":"Sposito, Garrison","contributorId":178194,"corporation":false,"usgs":false,"family":"Sposito","given":"Garrison","email":"","affiliations":[],"preferred":false,"id":742930,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Nordstrom, D. Kirk 0000-0003-3283-5136 dkn@usgs.gov","orcid":"https://orcid.org/0000-0003-3283-5136","contributorId":749,"corporation":false,"usgs":true,"family":"Nordstrom","given":"D.","email":"dkn@usgs.gov","middleInitial":"Kirk","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":false,"id":742928,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"May, Howard M.","contributorId":27202,"corporation":false,"usgs":true,"family":"May","given":"Howard","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":742929,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}