{"pageNumber":"963","pageRowStart":"24050","pageSize":"25","recordCount":46896,"records":[{"id":70555,"text":"sir20055009 - 2005 - Effects of best-management practices in Otter Creek in the Sheboygan River Priority Watershed, Wisconsin, 1990-2002","interactions":[],"lastModifiedDate":"2015-11-16T08:58:43","indexId":"sir20055009","displayToPublicDate":"2005-05-13T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5009","title":"Effects of best-management practices in Otter Creek in the Sheboygan River Priority Watershed, Wisconsin, 1990-2002","docAbstract":"<p>The U.S. Geological Survey and the Wisconsin Department of Natural Resources began a comprehensive, multidisciplinary evaluation-monitoring program in 1989 to assess the effectiveness of the Wisconsin Nonpoint Source Program. Hydrologic, water-quality, habitat, and fish data were collected at Otter Creek from 1990 to 2002 with the pre-BMP (best-management practice) period ending in September 1993 and the post-BMP period beginning in October 1999. BMPs installed in this basin included streambank protection and fencing, stream crossings, grade stabilization, buffer strips, various barnyard-runoff controls, nutrient management, and a low degree of upland BMPs. Reductions between pre- and post-BMP periods were detected in median concentrations of base-flow samples for total suspended solids and BOD5 but not for total phosphorus or dissolved ammonia nitrogen; fecal coliform concentrations in base-flow samples increased over the study period.</p>\n<p>Reductions in rainfall storm loads between the pre- and post-BMP periods during the non-vegetative season (November through May) were detected for all three constituents monitored (total suspended solids, total phosphorus, and dissolved ammonia nitrogen). Differences in rainfall storm loads of these three constituents for the vegetative season (June through October) were not detected. When considering rainfall data from the entire year, reductions in storm loads were detected for total suspended solids and dissolved ammonia nitrogen (reductions were estimated at 58 percent for total suspended solids and 41 percent for dissolved ammonia nitrogen). Annual reductions in rainfall storm loads for the non-vegetative season were estimated at 58 percent for total suspended solids, 48 percent for total phosphorus, and 41 percent for dissolved ammonia nitrogen.</p>\n<p>Habitat and fish data were collected each year of the study to track the effects of BMPs on stream habitat and fish communities. Final trend analysis was performed using habitat quality index scores, an index of biotic integrity, and some of the originally measured fish and habitat variables. Habitat was improved for stream segments that had either natural riparian buffer or where streambank fencing was installed, but not at the station where the riparian area was pasture and no streambank fencing was installed. The results also suggest that BMP implementation in Otter Creek substantially modified fish community structure, but the overall community quality was not improved.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055009","collaboration":"In cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Corsi, S., Walker, J.F., Wang, L., Horwatich, J.A., and Bannerman, R.T., 2005, Effects of best-management practices in Otter Creek in the Sheboygan River Priority Watershed, Wisconsin, 1990-2002: U.S. Geological Survey Scientific Investigations Report 2005-5009, vi, 26 p., https://doi.org/10.3133/sir20055009.","productDescription":"vi, 26 p.","numberOfPages":"34","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1990-01-01","temporalEnd":"1992-01-01","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":192946,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6936,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir20055009/","linkFileType":{"id":5,"text":"html"}},{"id":311331,"rank":101,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5009/pdf/SIR_2005-5009.pdf"}],"country":"United States","state":"Wisconsin","county":"Manitowoc County, Sheboygan County","otherGeospatial":"Gerber Lake, Little Gerber Lake, Otter Creek, Sheboygan River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.01284790039062,\n              43.74803313328719\n            ],\n            [\n              -88.01284790039062,\n              43.865722960678376\n            ],\n            [\n              -87.86796569824217,\n              43.865722960678376\n            ],\n            [\n              -87.86796569824217,\n              43.74803313328719\n            ],\n            [\n              -88.01284790039062,\n              43.74803313328719\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624a0b","contributors":{"authors":[{"text":"Corsi, Steven R. srcorsi@usgs.gov","contributorId":511,"corporation":false,"usgs":true,"family":"Corsi","given":"Steven R.","email":"srcorsi@usgs.gov","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":false,"id":282640,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walker, John F. jfwalker@usgs.gov","contributorId":1081,"corporation":false,"usgs":true,"family":"Walker","given":"John","email":"jfwalker@usgs.gov","middleInitial":"F.","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282641,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wang, Lizhu","contributorId":44888,"corporation":false,"usgs":true,"family":"Wang","given":"Lizhu","affiliations":[],"preferred":false,"id":282644,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Horwatich, Judy A. 0000-0003-0582-0836 jahorwat@usgs.gov","orcid":"https://orcid.org/0000-0003-0582-0836","contributorId":1388,"corporation":false,"usgs":true,"family":"Horwatich","given":"Judy","email":"jahorwat@usgs.gov","middleInitial":"A.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282642,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bannerman, Roger T. 0000-0001-9221-2905 rbannerman@usgs.gov","orcid":"https://orcid.org/0000-0001-9221-2905","contributorId":5560,"corporation":false,"usgs":true,"family":"Bannerman","given":"Roger","email":"rbannerman@usgs.gov","middleInitial":"T.","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282643,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70554,"text":"wdrOH041 - 2005 - Ohio water resources data, water year 2004 : volume 1. Ohio River basin excluding project data","interactions":[],"lastModifiedDate":"2012-02-02T00:14:05","indexId":"wdrOH041","displayToPublicDate":"2005-05-13T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"OH-04-1","title":"Ohio water resources data, water year 2004 : volume 1. Ohio River basin excluding project data","docAbstract":"Water-resources data for the 2004 water year for Ohio consist of records of stage, discharge, and water quality of streams; stage and contents of lakes and reservoirs; and water levels and water quality of ground-water wells. This report, in two volumes, contains records for water discharge at 137 gaging stations and various partial-record sites; water levels at 243 observation wells and 38 crest-stage gages; and water quality at 18 gaging stations, 34 observation wells, and no partial-record sites. Also included are data from miscellaneous and synoptic sites. Additional water data were collected at various sites not involved in the systematic data-collection program and are published as miscellaneous measurements and analyses. These data represent that part of the National Water Information System collected by the U.S. Geological Survey and cooperating Federal, State, and local agencies in Ohio.","language":"ENGLISH","doi":"10.3133/wdrOH041","usgsCitation":"Shindel, H., Mangus, J., and Frum, S., 2005, Ohio water resources data, water year 2004 : volume 1. Ohio River basin excluding project data: U.S. Geological Survey Water Data Report OH-04-1, 380 p., https://doi.org/10.3133/wdrOH041.","productDescription":"380 p.","costCenters":[],"links":[{"id":6935,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdroh04/","linkFileType":{"id":5,"text":"html"}},{"id":192945,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691ec2","contributors":{"authors":[{"text":"Shindel, H.L.","contributorId":17652,"corporation":false,"usgs":true,"family":"Shindel","given":"H.L.","affiliations":[],"preferred":false,"id":282637,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mangus, J.P.","contributorId":28301,"corporation":false,"usgs":true,"family":"Mangus","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":282638,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Frum, S.R.","contributorId":84843,"corporation":false,"usgs":true,"family":"Frum","given":"S.R.","email":"","affiliations":[],"preferred":false,"id":282639,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70550,"text":"sir20045251 - 2005 - Geochemical characterization of water, sediment, and biota affected by mercury contamination and acidic drainage from historical gold mining, Greenhorn Creek, Nevada County, California, 1999-2001","interactions":[],"lastModifiedDate":"2020-01-27T06:49:55","indexId":"sir20045251","displayToPublicDate":"2005-05-13T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-5251","title":"Geochemical characterization of water, sediment, and biota affected by mercury contamination and acidic drainage from historical gold mining, Greenhorn Creek, Nevada County, California, 1999-2001","docAbstract":"<p>In 1999, the U.S. Geological Survey (USGS) initiated studies of mercury and methylmercury occurrence, transformation, and transport in the Bear River and Yuba River watersheds of the northwestern Sierra Nevada. Because these watersheds were affected by large-scale, historical gold extraction using mercury amalgamation beginning in the 1850s, they were selected for a pilot study of mercury transport by the USGS and other cooperating agencies. This report presents data on methylmercury (MeHg) and total mercury (THg) concentrations in water, bed sediment, invertebrates, and frogs collected at 40 stations during 1999-2001 in the Greenhorn Creek drainage, a major tributary to Bear River. Results document several mercury contamination “hot spots” that represent potential targets for ongoing and future remediation efforts at abandoned mine sites in the study area.</p><p>Water-quality samples were collected one or more times at each of 29 stations. The concentrations of total mercury in 45 unfiltered water samples ranged from 0.80 to 153,000 nanograms per liter (ng/L); the median was 9.6 ng/L. Total mercury concentrations in filtered water (41 samples) ranged from less than 0.3 to 8,000 ng/L; the median was 2.7 ng/L. Concentrations of methylmercury in the unfiltered water (40 samples) ranged from less than 0.04 to 9.1 ng/L; the median was 0.07 ng/L. Methylmercury in filtered water (13 samples) ranged from less than 0.04 to 0.27 ng/L; the median was 0.04 ng/L. Acidic drainage with pH values as low as 3.4 was encountered in some of the mined areas. Elevated concentrations of aluminum, cadmium, copper, iron, manganese, nickel, and zinc were found at several stations, especially in the more acidic water samples.</p><p>Total mercury concentrations in sediment were determined by laboratory and field methods. Total mercury concentrations (determined by laboratory methods) in ten samples from eight stations ranged from about 0.0044 to 12 µg/g (microgram per gram, equivalent to parts per million). Methylmercury concentrations in these samples ranged from less than 0.00011 to 0.0095 µg/g. A field panning method was used to determine the concentration of liquid elemental mercury in 22&nbsp;samples from 14 stations. Measured quantities of elemental mercury recovered by panning ranged from a trace amount estimated at 100 milligrams per kilogram (equivalent to parts per million) to 45,000 milligrams per kilogram (equivalent to 4.5 per cent, by weight).</p><p>In total, 194 invertebrate samples were collected at 31&nbsp;stations; 78 of the samples were analyzed for concentrations of THg and MeHg and used to calculate MeHg to THg ratios. A total of 69 frog samples were collected at 19 stations, and all were analyzed only for THg. Ranges of MeHg concentrations (µg/g, wet weight) in invertebrate samples and number of samples (n) were 0.0012-0.048 for banana slugs (Arionidae, n = 27), 0.027-0.39 for dobsonflies (Corydalidae, n = 14), 0.029-0.50 for predaceous diving beetles (Dytiscidae, n = 31), 0.026-0.52 for predaceous stoneflies (Perlidae, n = 18), 0.011-1.6 for dragonflies (Odonata, n = 46), and 0.061-0.55 for water striders (Gerridae, n = 56). The ratio of MeHg to THg in invertebrates was greater than 50 percent for 74 of 78 samples.</p><p>&nbsp;The data from this reconnaissance sampling effort have been used by land-management agencies in selecting abandoned mine sites for remediation. The Forest Service has remediated the Sailor Flat site, and the Bureau of Land Management has initiated plans to remediate the Boston Mine drainage tunnel.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20045251","usgsCitation":"Alpers, C.N., Hunerlach, M.P., May, J., Hothem, R.L., Taylor, H.E., Antweiler, R.C., De Wild, J.F., and Lawler, D.A., 2005, Geochemical characterization of water, sediment, and biota affected by mercury contamination and acidic drainage from historical gold mining, Greenhorn Creek, Nevada County, California, 1999-2001: U.S. Geological Survey Scientific Investigations Report 2004-5251, 293 p., https://doi.org/10.3133/sir20045251.","productDescription":"293 p.","onlineOnly":"Y","costCenters":[{"id":589,"text":"Toxic Substances Hydrology 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Charles N. 0000-0001-6945-7365 cnalpers@usgs.gov","orcid":"https://orcid.org/0000-0001-6945-7365","contributorId":411,"corporation":false,"usgs":true,"family":"Alpers","given":"Charles","email":"cnalpers@usgs.gov","middleInitial":"N.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282629,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hunerlach, Michael P.","contributorId":66668,"corporation":false,"usgs":true,"family":"Hunerlach","given":"Michael","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":282636,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"May, Jason T. 0000-0002-5699-2112","orcid":"https://orcid.org/0000-0002-5699-2112","contributorId":14791,"corporation":false,"usgs":true,"family":"May","given":"Jason T.","affiliations":[],"preferred":false,"id":282633,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hothem, Roger L. roger_hothem@usgs.gov","contributorId":1721,"corporation":false,"usgs":true,"family":"Hothem","given":"Roger","email":"roger_hothem@usgs.gov","middleInitial":"L.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":282632,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Taylor, Howard E. hetaylor@usgs.gov","contributorId":1551,"corporation":false,"usgs":true,"family":"Taylor","given":"Howard","email":"hetaylor@usgs.gov","middleInitial":"E.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":282631,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Antweiler, Ronald C. 0000-0001-5652-6034 antweil@usgs.gov","orcid":"https://orcid.org/0000-0001-5652-6034","contributorId":1481,"corporation":false,"usgs":true,"family":"Antweiler","given":"Ronald","email":"antweil@usgs.gov","middleInitial":"C.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":282630,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"De Wild, John F.","contributorId":31800,"corporation":false,"usgs":true,"family":"De Wild","given":"John","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":282634,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Lawler, David A.","contributorId":39474,"corporation":false,"usgs":true,"family":"Lawler","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":282635,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70547,"text":"ofr20041410 - 2005 - Generalized geologic map of bedrock lithologies and surficial deposits in the Great Smoky Mountains National Park region, Tennessee and North Carolina","interactions":[{"subject":{"id":70547,"text":"ofr20041410 - 2005 - Generalized geologic map of bedrock lithologies and surficial deposits in the Great Smoky Mountains National Park region, Tennessee and North Carolina","indexId":"ofr20041410","publicationYear":"2005","noYear":false,"title":"Generalized geologic map of bedrock lithologies and surficial deposits in the Great Smoky Mountains National Park region, Tennessee and North Carolina"},"predicate":"SUPERSEDED_BY","object":{"id":70040740,"text":"sim2997 - 2012 - Geologic map of the Great Smoky Mountains National Park region, Tennessee and North Carolina","indexId":"sim2997","publicationYear":"2012","noYear":false,"title":"Geologic map of the Great Smoky Mountains National Park region, Tennessee and North Carolina"},"id":1}],"supersededBy":{"id":70040740,"text":"sim2997 - 2012 - Geologic map of the Great Smoky Mountains National Park region, Tennessee and North Carolina","indexId":"sim2997","publicationYear":"2012","noYear":false,"title":"Geologic map of the Great Smoky Mountains National Park region, Tennessee and North Carolina"},"lastModifiedDate":"2016-04-19T12:19:06","indexId":"ofr20041410","displayToPublicDate":"2005-05-13T00:00:00","publicationYear":"2005","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":"2004-1410","title":"Generalized geologic map of bedrock lithologies and surficial deposits in the Great Smoky Mountains National Park region, Tennessee and North Carolina","docAbstract":"<p><span>The geology of the Great Smoky Mountain National Park (GSMNP) region of Tennessee and North Carolina was studied from 1993 to 2003 as part of a cooperative investigation with the National Park Service (NPS). This work has been compiled as a 1:100,000-scale map derived from mapping done at 1:24,000 and 1:62,500 scale. The geologic data are intended to support cooperative investigations with NPS, the development of a new soil map by the Natural Resources Conservation Service, and the All Taxa Biodiversity Inventory (</span><a href=\"http://www.discoverlifeinamerica.org/\" target=\"_blank\">http://www.discoverlifeinamerica.org/</a><span>). At the request of NPS, we mapped areas previously not visited, revised the geology where stratigraphic and structural problems existed, and developed a map database for use in interdisciplinary research, land management, and interpretive programs for park visitors.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20041410","usgsCitation":"Southworth, S., Schultz, A., and Denenny, D., 2005, Generalized geologic map of bedrock lithologies and surficial deposits in the Great Smoky Mountains National Park region, Tennessee and North Carolina (Online only): U.S. Geological Survey Open-File Report 2004-1410, Report: 109 p.;  Plate: 54.25 x 39.42 inches; Shapefiles; Database, https://doi.org/10.3133/ofr20041410.","productDescription":"Report: 109 p.;  Plate: 54.25 x 39.42 inches; Shapefiles; Database","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":193187,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":110560,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_71380.htm","linkFileType":{"id":5,"text":"html"},"description":"71380"},{"id":6931,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1410/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"North Carolina, Tennessee","otherGeospatial":"Great Smoky Mountains National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84,\n              35.3\n            ],\n            [\n              -84,\n              35.88\n            ],\n            [\n              -83,\n              35.88\n            ],\n            [\n              -83,\n              35.3\n            ],\n            [\n              -84,\n              35.3\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af30b","contributors":{"authors":[{"text":"Southworth, Scott","contributorId":93933,"corporation":false,"usgs":true,"family":"Southworth","given":"Scott","affiliations":[],"preferred":false,"id":282619,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schultz, Art","contributorId":44982,"corporation":false,"usgs":true,"family":"Schultz","given":"Art","email":"","affiliations":[],"preferred":false,"id":282617,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Denenny, Danielle","contributorId":78804,"corporation":false,"usgs":true,"family":"Denenny","given":"Danielle","affiliations":[],"preferred":false,"id":282618,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70541,"text":"ds107 - 2005 - Data on dissolved pesticides and volatile organic compounds in surface and ground waters in the San Joaquin-Tulare basins, California, water years 1992-1995","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"ds107","displayToPublicDate":"2005-05-13T00:00:00","publicationYear":"2005","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":"107","title":"Data on dissolved pesticides and volatile organic compounds in surface and ground waters in the San Joaquin-Tulare basins, California, water years 1992-1995","docAbstract":"This report contains pesticide, volatile organic compound, major ion, nutrient, tritium, stable isotope, organic carbon, and trace-metal data collected from 149 ground-water wells, and pesticide data collected from 39 surface-water stream sites in the San Joaquin Valley of California. Included with the ground-water data are field measurements of pH, specific conductance, alkalinity, temperature, and dissolved oxygen. This report describes data collection procedures, analytical methods, quality assurance, and quality controls used by the National Water-Quality Assessment Program to ensure data reliability. Data contained in this report were collected during a four year period by the San Joaquin?Tulare Basins Study Unit of the United States Geological Survey's National Water-Quality Assessment Program.\r\n\r\n \r\n\r\nSurface-water-quality data collection began in April 1992, with sampling done three times a week at three sites as part of a pilot study conducted to provide background information for the surface-water-study design. Monthly samples were collected at 10 sites for major ions and nutrients from January 1993 to March 1995. Additional samples were collected at four of these sites, from January to December 1993, to study spatial and temporal variability in dissolved pesticide concentrations. Samples for several synoptic studies were collected from 1993 to 1995.\r\n\r\n \r\n\r\nGround-water-quality data collection was restricted to the eastern alluvial fans subarea of the San Joaquin Valley. Data collection began in 1993 with the sampling of 21 wells in vineyard land-use settings. In 1994, 29 wells were sampled in almond land-use settings and 9 in vineyard land-use settings; an additional 11 wells were sampled along a flow path in the eastern Fresno County vineyard land-use area. Among the 79 wells sampled in 1995, 30 wells were in the corn, alfalfa, and vegetable land-use setting, and 1 well was in the vineyard land-use setting; an additional 20 were flow-path wells. Also sampled in 1995 were 28 wells used for a regional assessment of ground-water quality in the eastern San Joaquin Valley.","language":"ENGLISH","doi":"10.3133/ds107","usgsCitation":"Kinsey, W.B., Johnson, M.V., and Gronberg, J.M., 2005, Data on dissolved pesticides and volatile organic compounds in surface and ground waters in the San Joaquin-Tulare basins, California, water years 1992-1995 (Online only): U.S. Geological Survey Data Series 107, 372 p., https://doi.org/10.3133/ds107.","productDescription":"372 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":6906,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ds107/","linkFileType":{"id":5,"text":"html"}},{"id":185998,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c848","contributors":{"authors":[{"text":"Kinsey, Willie B.","contributorId":16925,"corporation":false,"usgs":true,"family":"Kinsey","given":"Willie","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":282604,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Mark V.","contributorId":22436,"corporation":false,"usgs":true,"family":"Johnson","given":"Mark","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":282605,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gronberg, JoAnn M. 0000-0003-4822-7434 jmgronbe@usgs.gov","orcid":"https://orcid.org/0000-0003-4822-7434","contributorId":3548,"corporation":false,"usgs":true,"family":"Gronberg","given":"JoAnn","email":"jmgronbe@usgs.gov","middleInitial":"M.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282603,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70529,"text":"wdrNHVT041 - 2005 - Water resources data for New Hampshire and Vermont, water year 2004","interactions":[],"lastModifiedDate":"2012-03-08T17:16:17","indexId":"wdrNHVT041","displayToPublicDate":"2005-05-09T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NH-VT-04-1","title":"Water resources data for New Hampshire and Vermont, water year 2004","docAbstract":"Water-resources data for the 2004 water year for New Hampshire and Vermont consists of stage, discharge, and water quality of streams; contents of lakes and reservoirs; and ground-water levels. This report contains discharge records for 93 gaging stations, stage records for 6 lakes, monthend contents for 2 lakes and reservoirs, water levels for 38 observation wells. Also included are data for 37 crest-stage partial-record stations. Additional water data were collected at various sites, which are not part of the systematic data-collection program and are published as miscellaneous measurements for gaging stations in New Hampshire and Vermont. A few pertinent stations in bordering States are also included in this report. These data represent that portion of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in New Hampshire and Vermont.","language":"ENGLISH","doi":"10.3133/wdrNHVT041","usgsCitation":"Keirstead, C., Kiah, R.G., Ward, S.L., and Hilgendorf, G.S., 2005, Water resources data for New Hampshire and Vermont, water year 2004: U.S. Geological Survey Water Data Report NH-VT-04-1, 353 p., https://doi.org/10.3133/wdrNHVT041.","productDescription":"353 p.","temporalStart":"2003-10-01","temporalEnd":"2004-09-30","costCenters":[{"id":468,"text":"New Hampshire-Vermont Water Science Center","active":false,"usgs":true}],"links":[{"id":186076,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6903,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/2004/wdr-nh-04-1/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2986","contributors":{"authors":[{"text":"Keirstead, Chandlee","contributorId":10862,"corporation":false,"usgs":true,"family":"Keirstead","given":"Chandlee","email":"","affiliations":[],"preferred":false,"id":282593,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kiah, Richard G. 0000-0001-6236-2507 rkiah@usgs.gov","orcid":"https://orcid.org/0000-0001-6236-2507","contributorId":2637,"corporation":false,"usgs":true,"family":"Kiah","given":"Richard","email":"rkiah@usgs.gov","middleInitial":"G.","affiliations":[{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282590,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ward, Sanborn L. sward@usgs.gov","contributorId":5147,"corporation":false,"usgs":true,"family":"Ward","given":"Sanborn","email":"sward@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":282592,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hilgendorf, Gregory S. gshilgen@usgs.gov","contributorId":5144,"corporation":false,"usgs":true,"family":"Hilgendorf","given":"Gregory","email":"gshilgen@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":282591,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70525,"text":"ofr20051176 - 2005 - Flooding of the Androscoggin River during December 18-19, 2003, in Canton, Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"ofr20051176","displayToPublicDate":"2005-05-06T00:00:00","publicationYear":"2005","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":"2005-1176","title":"Flooding of the Androscoggin River during December 18-19, 2003, in Canton, Maine","docAbstract":"The Androscoggin River flooded the town of Canton, Maine in December 2003, resulting in damage to and (or) evacuation of 44 homes. Streamflow records at the U.S. Geological Survey (USGS) streamflow-gaging stations at Rumford (USGS station identification number 01054500) and Auburn (01059000) were used to estimate the peak streamflow for the Androscoggin in the town of Canton for this flood (December 18-19, 2003). The estimated peak flood streamflow at Canton was approximately 39,800 ft3/s, corresponding to an estimated recurrence interval of 4.4 years; however, an ice jam downstream from Canton Point on December 18-19 obstructed river flow resulting in a high-water elevation commensurate with an open-water flood approximately equal to a 15-year event. The high water-surface elevations attained during the December 18-19 flood event in Canton were higher than the expected open-water flood water-surface elevations; this verified the assumption that the water-surface elevation was augmented due to the downstream ice jam\r\n\r\nThe change in slope of the riverbed from upstream of Canton to the impoundment at the downstream corporate limits, and the river bend near Stevens Island are principal factors in ice-jam formation near Canton. The U.S. Army Corps of Engineers Ice Jam Database indicates five ice-jam-related floods (including December 2003) for the town of Canton: March 13, 1936; January 1978; March 12, 1987; January 29, 1996; and December 18-19, 2003. There have been more ice-jam-related flood events in Canton than these five documented events, but the exact number and nature of ice jams in Canton cannot be determined without further research.","language":"ENGLISH","doi":"10.3133/ofr20051176","usgsCitation":"Dudley, R.W., 2005, Flooding of the Androscoggin River during December 18-19, 2003, in Canton, Maine (Online only): U.S. Geological Survey Open-File Report 2005-1176, 13 p., https://doi.org/10.3133/ofr20051176.","productDescription":"13 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":6902,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr2005-1176/","linkFileType":{"id":5,"text":"html"}},{"id":186075,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478fe4b07f02db48a621","contributors":{"authors":[{"text":"Dudley, Robert W. 0000-0002-0934-0568 rwdudley@usgs.gov","orcid":"https://orcid.org/0000-0002-0934-0568","contributorId":2223,"corporation":false,"usgs":true,"family":"Dudley","given":"Robert","email":"rwdudley@usgs.gov","middleInitial":"W.","affiliations":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282589,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70524,"text":"sir20045248 - 2005 - Evaluation of volatile organic compounds in two Mojave Desert basins-Mojave River and Antelope Valley-in San Bernardino, Los Angeles, and Kern Counties, California, June-October 2002","interactions":[],"lastModifiedDate":"2026-06-12T18:33:38.485783","indexId":"sir20045248","displayToPublicDate":"2005-05-06T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-5248","title":"Evaluation of volatile organic compounds in two Mojave Desert basins-Mojave River and Antelope Valley-in San Bernardino, Los Angeles, and Kern Counties, California, June-October 2002","docAbstract":"The California Aquifer Susceptibility Assessment of the Ground-Water Ambient Monitoring and Assessment Program was developed to assess water quality and susceptibility of ground-water resources to contamination from surficial sources. This study focuses on the Mojave River and the Antelope Valley ground-water basins in southern California. \r\n\r\nVolatile organic compound (VOC) data were evaluated in conjunction with tritium data to determine a potential correlation with aquifer type, depth to top of perforations, and land use to VOC distribution and occurrence in the Mojave River and the Antelope Valley Basins. Detection frequencies for VOCs were compiled and compared to assess the distribution in each area. Explanatory variables were evaluated by comparing detection frequencies for VOCs and tritium and the number of compounds detected. Thirty-three wells were sampled in the Mojave River Basin (9 in the floodplain aquifer, 15 in the regional aquifer, and 9 in the sewered subset of the regional aquifer). Thirty-two wells were sampled in the Antelope Valley Basin. Quality-control samples also were collected to identify, quantify, and document bias and variability in the data.\r\n\r\nResults show that VOCs generally were detected slightly more often in the Antelope Valley Basin samples than in the Mojave River Basin samples. VOCs were detected more frequently in the floodplain aquifer than in the regional aquifer and the sewered subset. Tritium was detected more frequently in the Mojave River Basin samples than in the Antelope Valley Basin samples, and it was detected more frequently in the floodplain aquifer than in the regional aquifer and the sewered subset. Most of the samples collected in both basins for this study contained old water (water recharged prior to 1952). In general, in these desert basins, tritium need not be present for VOCs to be present. When VOCs were detected, young water (water recharge after 1952) was slightly more likely to be contaminated than old water.\r\n\r\nTrihalomethanes (THMs) were detected less frequently in the Mojave River Basin samples than in the Antelope Valley Basin samples. The THMs that were detected in the Mojave River Basin were detected more frequently in the floodplain aquifer than in the regional aquifer and sewered subset. Solvents were detected more frequently in the Mojave River samples than in the Antelope Valley samples. In the Mojave River Basin samples, solvents were detected less frequently in the floodplain aquifer than in the regional aquifer and the sewered subset. Benzene, toluene, ethylbenzene and xylene (BTEX) were not detected in either study area. Methyl tert-butyl ether (MTBE) was detected in one sample from both the Mojave River and Antelope Valley Basins. \r\n\r\nThe most frequently detected compound (detected in more than 10 percent of the wells) in the Mojave River Basin was chloroform. The two most frequently detected compounds in the Antelope Valley Basin were chloroform and tetrachloroethylene (PCE). \r\n\r\nIn the Mojave River Basin, aquifer type and land use within 1,640 ft (500 m) of the well head were not statistically correlated with the number of VOCs detected, although VOCs were detected more frequently in the floodplain aquifer than in the regional aquifer and the sewered subset. Depth to the top of the perforations was an explanatory factor for the number of VOCs detected in the Mojave River Basin; the detection frequency was greater for shallow wells than for deep wells. \r\n\r\nIn the Antelope Valley Basin, neither aquifer type, depth to the top of the perforations, nor land use within 1,640 ft of the well head were explanatory factors for the number of VOCs detected. Although aquifer type and depth to top of the perforations did explain the presence of tritium in the Mojave River Basin, land use within 1,640 ft of the well head was not a statistically significant explanatory factor for the presence of tritium in this basin. Aquifer type, depth to the top of the perfora","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20045248","usgsCitation":"Densmore, J., Belitz, K., Wright, M.T., Dawson, B.J., and Johnson, T.D., 2005, Evaluation of volatile organic compounds in two Mojave Desert basins-Mojave River and Antelope Valley-in San Bernardino, Los Angeles, and Kern Counties, California, June-October 2002 (Online only): U.S. Geological Survey Scientific Investigations Report 2004-5248, 51 p., https://doi.org/10.3133/sir20045248.","productDescription":"51 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":186074,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6901,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2004/5248/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611a26","contributors":{"authors":[{"text":"Densmore, Jill N. 0000-0002-5345-6613","orcid":"https://orcid.org/0000-0002-5345-6613","contributorId":89179,"corporation":false,"usgs":true,"family":"Densmore","given":"Jill N.","affiliations":[],"preferred":false,"id":282588,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Belitz, Kenneth 0000-0003-4481-2345 kbelitz@usgs.gov","orcid":"https://orcid.org/0000-0003-4481-2345","contributorId":442,"corporation":false,"usgs":true,"family":"Belitz","given":"Kenneth","email":"kbelitz@usgs.gov","affiliations":[{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":true,"id":282584,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wright, Michael T. 0000-0003-0653-6466 mtwright@usgs.gov","orcid":"https://orcid.org/0000-0003-0653-6466","contributorId":1508,"corporation":false,"usgs":true,"family":"Wright","given":"Michael","email":"mtwright@usgs.gov","middleInitial":"T.","affiliations":[],"preferred":false,"id":282587,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dawson, Barbara J. 0000-0002-0209-8158 bjdawson@usgs.gov","orcid":"https://orcid.org/0000-0002-0209-8158","contributorId":1102,"corporation":false,"usgs":true,"family":"Dawson","given":"Barbara","email":"bjdawson@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":282585,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Johnson, Tyler D. 0000-0002-7334-9188 tyjohns@usgs.gov","orcid":"https://orcid.org/0000-0002-7334-9188","contributorId":1440,"corporation":false,"usgs":true,"family":"Johnson","given":"Tyler","email":"tyjohns@usgs.gov","middleInitial":"D.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":false,"id":282586,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70523,"text":"ofr20051130 - 2005 - Geologic and hydrogeologic framework of the Espanola basin -- Proceedings of the 4th annual Espanola Basin Workshop, Santa Fe, New Mexico, March 1-3, 2005","interactions":[],"lastModifiedDate":"2022-04-26T21:01:24.783283","indexId":"ofr20051130","displayToPublicDate":"2005-05-06T00:00:00","publicationYear":"2005","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":"2005-1130","title":"Geologic and hydrogeologic framework of the Espanola basin -- Proceedings of the 4th annual Espanola Basin Workshop, Santa Fe, New Mexico, March 1-3, 2005","docAbstract":"<p class=\"textindent\">This report presents abstracts of technical studies that pertain to the hydrogeologic framework of the</p><p class=\"textindent\">This report presents abstracts of technical studies that pertain to the hydrogeologic framework of the Española basin, a major subbasin of the Cenozoic Rio Grande rift. Sediments and interbedded volcanic rocks that fill the Española basin comprise an aquifer system that is an important source of water for many residents of the basin, including people in the cities of Santa Fe, Española, and Los Alamos as well as Native Americans in eleven Pueblos.</p><p class=\"textindent\">The abstracts describe results of technical studies that were presented either as poster exhibits or oral presentations at the forth-annual Española basin workshop, held March 1-2 of 2005 in Santa Fe, New Mexico. The principal goal of this workshop was to share information about ongoing studies.</p><p class=\"textindent\">The Española basin workshop was hosted by the Española basin technical advisory group (EBTAG) and sponsored by the U.S. Geological Survey, the New Mexico Bureau of Geology and Mineral Resources, and both the Water Research Technical Assistance Office and the Groundwater Protection Program of Los Alamos National Laboratory. Abstracts in this report have been grouped into six information themes: Basic Water Data, Water Quality and Water Chemistry, Water Balance and Stream/Aquifer Interaction, Data Integration and Hydrologic Model Testing, Three-Dimensional Hydrogeological Architecture, and Geologic Framework.</p><p class=\"textindent\">Taken together, the abstracts in this report provide a view of the current status of hydrogeologic research within the Española basin.</p><p class=\"textindent\">, a major subbasin of the Cenozoic Rio Grande rift. Sediments and interbedded volcanic rocks that fill the Española basin comprise an aquifer system that is an important source of water for many residents of the basin, including people in the cities of Santa Fe, Española, and Los Alamos as well as Native Americans in eleven Pueblos.</p><p class=\"textindent\">The abstracts describe results of technical studies that were presented either as poster exhibits or oral presentations at the forth-annual Española basin workshop, held March 1-2 of 2005 in Santa Fe, New Mexico. The principal goal of this workshop was to share information about ongoing studies.</p><p class=\"textindent\">The Española basin workshop was hosted by the Española basin technical advisory group (EBTAG) and sponsored by the U.S. Geological Survey, the New Mexico Bureau of Geology and Mineral Resources, and both the Water Research Technical Assistance Office and the Groundwater Protection Program of Los Alamos National Laboratory. Abstracts in this report have been grouped into six information themes: Basic Water Data, Water Quality and Water Chemistry, Water Balance and Stream/Aquifer Interaction, Data Integration and Hydrologic Model Testing, Three-Dimensional Hydrogeological Architecture, and Geologic Framework.</p><p class=\"textindent\">Taken together, the abstracts in this report provide a view of the current status of hydrogeologic research within the Española basin.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051130","usgsCitation":"McKinney, K.C., 2005, Geologic and hydrogeologic framework of the Espanola basin -- Proceedings of the 4th annual Espanola Basin Workshop, Santa Fe, New Mexico, March 1-3, 2005 (Version 1.0): U.S. Geological Survey Open-File Report 2005-1130, 33 p., https://doi.org/10.3133/ofr20051130.","productDescription":"33 p.","costCenters":[],"links":[{"id":186073,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6900,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1130/","linkFileType":{"id":5,"text":"html"}},{"id":399711,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_71262.htm"}],"country":"United States","state":"New Mexico","otherGeospatial":"Española basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.35314941406249,\n              35.66622234103479\n            ],\n            [\n              -105.77636718749999,\n              35.66622234103479\n            ],\n            [\n              -105.77636718749999,\n              36.38149043210595\n            ],\n            [\n              -106.35314941406249,\n              36.38149043210595\n            ],\n            [\n              -106.35314941406249,\n              35.66622234103479\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8237","contributors":{"authors":[{"text":"McKinney, Kevin C. kcmckinney@usgs.gov","contributorId":3406,"corporation":false,"usgs":true,"family":"McKinney","given":"Kevin","email":"kcmckinney@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":282583,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70517,"text":"wdrKY041 - 2005 - Water resources data, Kentucky, water year 2004","interactions":[],"lastModifiedDate":"2012-02-02T00:13:32","indexId":"wdrKY041","displayToPublicDate":"2005-05-05T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"KY-04-1","title":"Water resources data, Kentucky, water year 2004","docAbstract":"Water resources data for the 2004 water year for Kentucky consist of records of stage, discharge, and water-quality of streams and lakes; and water levels of wells. This report includes daily discharge records for 131 stream-stations. It also includes water-quality data for 15 stations sampled at regular intervals, continuous temperature at 7 stations, and continuous water-quality at 11 stations. Ground-water levels are published for 8 recording and 22 partial record sites. Precipitation data at a regular interval are published for two sites. Additional water data were collected at various sites not involved in the systematic data-collection program and are published as miscellaneous measurements and analyses. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Kentucky.","language":"ENGLISH","doi":"10.3133/wdrKY041","usgsCitation":"McClain, D.L., Moses, C.R., and Darnell, R.S., 2005, Water resources data, Kentucky, water year 2004: U.S. Geological Survey Water Data Report KY-04-1, v., 675 p. : charts, maps ; 28 cm. \r\n, https://doi.org/10.3133/wdrKY041.","productDescription":"v., 675 p. : charts, maps ; 28 cm. \r\n","costCenters":[],"links":[{"id":6476,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdr-ky-04-1/","linkFileType":{"id":5,"text":"html"}},{"id":187900,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f1326","contributors":{"authors":[{"text":"McClain, Dennis L.","contributorId":43860,"corporation":false,"usgs":true,"family":"McClain","given":"Dennis","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":282566,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moses, Clifford R.","contributorId":69245,"corporation":false,"usgs":true,"family":"Moses","given":"Clifford","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":282567,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Darnell, Roy S.","contributorId":25641,"corporation":false,"usgs":true,"family":"Darnell","given":"Roy","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":282565,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70514,"text":"sir20045290 - 2005 - Distribution and mass of nitrate in the unconfined aquifer beneath the intensively cultivated area north of the Rio Grande, San Luis Valley, Colorado, 1997 through 2001","interactions":[],"lastModifiedDate":"2012-02-02T00:13:32","indexId":"sir20045290","displayToPublicDate":"2005-05-04T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-5290","title":"Distribution and mass of nitrate in the unconfined aquifer beneath the intensively cultivated area north of the Rio Grande, San Luis Valley, Colorado, 1997 through 2001","docAbstract":"Current (1997?2001) and historical (1948?49, 1968?69) nitrate-concentration and water-level data collected from wells completed in the unconfined aquifer in the intensively cultivated area north of the Rio Grande in south-central Colorado were used to determine the distribution and mass of nitrate and to determine short- and long-term trends in the concentration and mass of nitrate in the unconfined aquifer. ","language":"ENGLISH","doi":"10.3133/sir20045290","usgsCitation":"Stogner, 2005, Distribution and mass of nitrate in the unconfined aquifer beneath the intensively cultivated area north of the Rio Grande, San Luis Valley, Colorado, 1997 through 2001 (Online only): U.S. Geological Survey Scientific Investigations Report 2004-5290, v, 62 p., https://doi.org/10.3133/sir20045290.","productDescription":"v, 62 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":6475,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir20045290/","linkFileType":{"id":5,"text":"html"}},{"id":187899,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649659","contributors":{"authors":[{"text":"Stogner 0000-0002-3185-1452 rstogner@usgs.gov","orcid":"https://orcid.org/0000-0002-3185-1452","contributorId":938,"corporation":false,"usgs":true,"family":"Stogner","email":"rstogner@usgs.gov","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":false,"id":282564,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70512,"text":"sir20055063 - 2005 - Variability of differences between two approaches for determining ground-water discharge and pumpage, including effects of time trends, Lower Arkansas River Basin, southeastern Colorado, 1998-2002","interactions":[],"lastModifiedDate":"2012-02-02T00:13:32","indexId":"sir20055063","displayToPublicDate":"2005-05-04T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5063","title":"Variability of differences between two approaches for determining ground-water discharge and pumpage, including effects of time trends, Lower Arkansas River Basin, southeastern Colorado, 1998-2002","docAbstract":"In the mid-1990s, the Colorado Division of Water Resources (CDWR) adopted rules governing measurement of tributary ground-water pumpage for the Arkansas River Basin. The rules allowed ground-water pumpage to be determined using one of two approaches?power conversion coefficient (PCC) or totalizing flowmeters (TFM). In addition, the rules allowed a PCC to be applied to the electrical power usage up to 4 years in the future to estimate ground-water pumpage. \r\n\r\nAs a result of concerns about potential errors in applying the PCC approach forward in time, a study was done by the U.S. Geological Survey, in cooperation with CDWR and Colorado Water Conservation Board, to evaluate the variability in differences in pumpage between the two approaches, including the effects of time trends.\r\n\r\nThis report compared measured ground-water pumpage using TFMs to computed ground-water pumpage using PCCs by developing statistical models of relations between explanatory variables, such as site, time, and pumping water level, and dependent variables, which are based on discharge, PCC, and pumpage. When differences in pumpage (diffP) were computed using PCC measurements and power consumption for the same year (1998-2002), the median diffP, depending on the year, ranged from +0.1 to -2.9 percent; the median diffP for the entire period was -1.5 percent. However, when diffP was computed using PCC measurements applied to the next year's power consumption, the median diffP was -0.3 percent; and when PCC measurements were applied 2, 3, or 4 years into the future, median diffPs were +1.8 percent for a 2-year forward lag and +5.3 percent for a 4-year forward lag, indicating that pumpage computed with the PCC approach, as generally applied under the ground-water pumpage measurement rules by CDWR, tended to overestimate pumpage as compared to pumpage using TFMs when PCC measurement was applied to future years of measured power consumption. \r\n\r\nAnalyses were done to better understand the causes of the time trend; an estimate of the overall trend with time (uncorrected for pumping water-level changes) yielded a trend of about 2.2 percent per lag year for diffP. A separate analysis that incorporated a surface-water diversion term in the statistical model rendered the time-trend term insignificant, indicating that the time trend in the models served as a surrogate for other variables, some of which reflect underlying hydrologic conditions. A more precise explanation of the potential causes of the time trend was not obtained with the available data. However, the model results with the surface-water diversion term indicate that much of the trend of 2.2 percent per lag year in diffP resulted from applying a PCC to estimate pumpage under hydrologic conditions different from those under which the PCC was measured. Although there is no evidence to conclude that the upward time trend determined in the data for this 5-year period would hold in the future, historical static ground-water levels in the study area generally have exhibited small variations over multidecadal time scales. Therefore, the approximately 2 percent per lag year trend determined in these data is expected to be a reasonable guideline for estimating potential errors in the PCC approach resulting from temporally varying hydrologic conditions between time of PCC measurement and pumpage estimation. \r\n\r\nComparisons also were made between total, or aggregated, pumpage for a network of wells as computed by the PCC approach and the TFM approach. For 100 wells and a lag of 4 years between PCC measurement and pumpage estimation, there was a 95-percent probability that the difference between total network pumpage measured by the PCC approach and that measured using a TFM would be between 5.2 and 14.4 percent. These estimates were based on a bias of 2.2 percent per lag year estimated for the period 1998-2002 during which hydrologic conditions were known to have changed. Using the same assumptions, the estimated d","language":"ENGLISH","doi":"10.3133/sir20055063","usgsCitation":"Troutman, B., Edelmann, P., and Dash, R.G., 2005, Variability of differences between two approaches for determining ground-water discharge and pumpage, including effects of time trends, Lower Arkansas River Basin, southeastern Colorado, 1998-2002 (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5063, 166 p., https://doi.org/10.3133/sir20055063.","productDescription":"166 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":6474,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5063/","linkFileType":{"id":5,"text":"html"}},{"id":120986,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2005_5063.jpg"}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602bb2","contributors":{"authors":[{"text":"Troutman, Brent M.","contributorId":41040,"corporation":false,"usgs":true,"family":"Troutman","given":"Brent M.","affiliations":[],"preferred":false,"id":282561,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Edelmann, Patrick","contributorId":86305,"corporation":false,"usgs":true,"family":"Edelmann","given":"Patrick","affiliations":[],"preferred":false,"id":282563,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dash, Russell G.","contributorId":64695,"corporation":false,"usgs":true,"family":"Dash","given":"Russell","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":282562,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70507,"text":"sim2884 - 2005 - Precambrian crystalline basement map of Idaho: An interpretation of aeromagnetic anomalies","interactions":[],"lastModifiedDate":"2022-12-14T21:20:58.248532","indexId":"sim2884","displayToPublicDate":"2005-05-03T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":333,"text":"Scientific Investigations Map","code":"SIM","onlineIssn":"2329-132X","printIssn":"2329-1311","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2884","title":"Precambrian crystalline basement map of Idaho: An interpretation of aeromagnetic anomalies","docAbstract":"Idaho lies within the northern sector of the U.S. Cordillera astride the \r\n        boundary between the Proterozoic continent (Laurentia) to the east and \r\n        the Permian to Jurassic accreted terranes to the west.  The continental \r\n        basement is mostly covered by relatively undeformed Mesoproterozoic \r\n        metasedimentary rocks and intruded or covered by Phanerozoic igneous \r\n        rocks; accordingly, knowledge of the basement geology is poorly \r\n        constrained.  Incremental knowledge gained since the pioneering studies \r\n        by W. Lindgren, C.P. Ross, A.L. Anderson, A. Hietanen, and others during \r\n        the early- and mid-1900's has greatly advanced our understanding of the \r\n        general geology of Idaho.  However, knowledge of the basement geology \r\n        remains relatively poor, partly because of the remoteness of much of the \r\n        region plus the lack of a stimulus to decipher the complex assemblage of \r\n        high-grade gneisses and migmatite of central Idaho.  The availability of \r\n        an updated aeromagnetic anomaly map of Idaho (North American Magnetic \r\n        Anomaly Group, 2002) provides a means to determine the regional \r\n        Precambrian geologic framework of the State.  The combined geologic and \r\n        aeromagnetic data permit identification of previously unrecognized \r\n        crystalline basement terranes, assigned to Archean and Paleoproterozoic \r\n        ages, and the delineation of major shear zones, which are expressed in \r\n        the aeromagnetic data as linear negative anomalies (Finn and Sims, \r\n        2004).  Limited geochronologic data on exposed crystalline basement \r\n        aided by isotopic studies of zircon inheritance, particularly Bickford \r\n        and others (1981) and Mueller and others (1995), provide much of the \r\n        geologic background for our interpretation of the basement geology.  In \r\n        northwestern United States, inhomogeneities in the basement inherited \r\n        from Precambrian tectogenesis controlled many large-scale tectonic \r\n        features that developed during the Phanerozoic.  Two basement \r\n        structures, in particular, provided zones of weakness that were \r\n        repeatedly rejuvenated:  (1) northeast-trending ductile shear zones \r\n        developed on the northwest margin of the Archean Wyoming province during \r\n        the Paleoproterozoic Trans-Montana orogeny (Sims and others, 2004), and \r\n        (2) northwest-trending intra-continental faults of the Mesoproterozoic \r\n        Trans-Rocky Mountain strike-slip fault system (Sims, unpub. data, 2003).  \r\n        In this report, geologic ages are reported in millions of years (Ma) and \r\n        generalized ages are given in billions of years (Ga).  The subdivision \r\n        of Precambrian rocks used herein is the time classification recommended \r\n        by the International Union of Geological Sciences (Plumb, 1991).","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sim2884","usgsCitation":"Sims, P., Lund, K., and Anderson, E., 2005, Precambrian crystalline basement map of Idaho: An interpretation of aeromagnetic anomalies (Version 1.0): U.S. Geological Survey Scientific Investigations Map 2884, Report: 21 p.; 1 Plate: 56.50 × 36.50 inches; Metadata: Downloads Directory, https://doi.org/10.3133/sim2884.","productDescription":"Report: 21 p.; 1 Plate: 56.50 × 36.50 inches; Metadata: Downloads Directory","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":187804,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":110559,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_71261.htm","linkFileType":{"id":5,"text":"html"},"description":"71261"},{"id":6472,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/2005/2884/","linkFileType":{"id":5,"text":"html"}}],"country":"United 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Carolina\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0b3a","contributors":{"authors":[{"text":"Cooney, T.W.","contributorId":25194,"corporation":false,"usgs":true,"family":"Cooney","given":"T.W.","email":"","affiliations":[],"preferred":false,"id":282552,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Drewes, P.A.","contributorId":31022,"corporation":false,"usgs":true,"family":"Drewes","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":282553,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ellisor, S.W.","contributorId":100930,"corporation":false,"usgs":true,"family":"Ellisor","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":282556,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lanier, T. H.","contributorId":41469,"corporation":false,"usgs":true,"family":"Lanier","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":282554,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Melendez, F.","contributorId":91922,"corporation":false,"usgs":true,"family":"Melendez","given":"F.","email":"","affiliations":[],"preferred":false,"id":282555,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70156332,"text":"70156332 - 2005 - Integration of CO2 flux and remotely-sensed data for primary production and ecosystem respiration analyses in the Northern Great Plains: potential for quantitative spatial extrapolation","interactions":[],"lastModifiedDate":"2021-09-22T13:51:21.076775","indexId":"70156332","displayToPublicDate":"2005-05-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1839,"text":"Global Ecology and Biogeography","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Integration of CO<sub>2</sub> flux and remotely-sensed data for primary production and ecosystem respiration analyses in the Northern Great Plains: potential for quantitative spatial extrapolation","title":"Integration of CO2 flux and remotely-sensed data for primary production and ecosystem respiration analyses in the Northern Great Plains: potential for quantitative spatial extrapolation","docAbstract":"<div class=\"para\">\n<p><strong>Aim&ensp;</strong>&nbsp;Extrapolation of tower CO<sub>2</sub>&nbsp;fluxes will be greatly facilitated if robust relationships between flux components and remotely sensed factors are established. Long-term measurements at five Northern Great Plains locations were used to obtain relationships between CO<sub>2</sub>fluxes and photosynthetically active radiation (<i>Q</i>), other on-site factors, and Normalized Difference Vegetation Index (<i>NDVI</i>) from the SPOT VEGETATION data set.</p>\n</div>\n<div class=\"para\">\n<p><strong>Location&ensp;</strong>&nbsp;CO<sub>2</sub>&nbsp;flux data from the following stations and years were analysed: Lethbridge, Alberta 1998&ndash;2001; Fort Peck, MT 2000, 2002; Miles City, MT 2000&ndash;01; Mandan, ND 1999&ndash;2001; and Cheyenne, WY 1997&ndash;98.</p>\n</div>\n<div class=\"para\">\n<p><strong>Results&ensp;</strong>&nbsp;Analyses based on light-response functions allowed partitioning net CO<sub>2</sub>&nbsp;flux (<i>F</i>) into gross primary productivity (<i>P</i><sub><i>g</i></sub>) and ecosystem respiration (<i>R</i><sub><i>e</i></sub>). Weekly averages of daytime respiration, &gamma;<sub><i>day</i></sub>, estimated from light responses were closely correlated with weekly averages of measured night-time respiration, &gamma;<sub><i>night</i></sub>&nbsp;(<i>R</i><sup>2</sup>&nbsp;0.64 to 0.95). Daytime respiration tended to be higher than night-time respiration, and regressions of &gamma;<sub><i>day</i></sub>&nbsp;on &gamma;<sub><i>night</i></sub>&nbsp;for all sites were different from 1&nbsp;:&nbsp;1 relationships. Over 13 site-years, gross primary production varied from 459 to 2491&nbsp;g CO<sub>2</sub>&nbsp;m<sup>&minus;2</sup>&nbsp;year<sup>&minus;1</sup>, ecosystem respiration from 996 to 1881&nbsp;g CO<sub>2</sub>&nbsp;m<sup>&minus;2</sup>&nbsp;year<sup>&minus;1</sup>, and net ecosystem exchange from &minus;537 (source) to +610&nbsp;g CO<sub>2</sub>&nbsp;m<sup>&minus;2</sup>&nbsp;year<sup>&minus;1</sup>&nbsp;(sink). Maximum daily ecological light-use efficiencies, ɛ<sub><i>d</i>,<i>max</i></sub>&nbsp;=&nbsp;<i>P</i><sub><i>g</i></sub><i>/Q</i>, were in the range 0.014 to 0.032&nbsp;mol CO<sub>2</sub>&nbsp;(mol incident quanta)<sup>&minus;1</sup>.</p>\n</div>\n<div class=\"para\">\n<p><strong>Main conclusions&ensp;</strong>&nbsp;Ten-day average&nbsp;<i>P</i><sub><i>g</i></sub>&nbsp;was significantly more highly correlated with&nbsp;<i>NDVI</i>&nbsp;than 10-day average daytime flux,&nbsp;<i>P</i><sub><i>d</i></sub>&nbsp;(<i>R</i><sup>2</sup>&nbsp;=&nbsp;0.46 to 0.77 for&nbsp;<i>P</i><sub><i>g</i></sub><i>-NDVI</i>&nbsp;and 0.05 to 0.58 for&nbsp;<i>P</i><sub><i>d</i></sub><i>-NDVI</i>&nbsp;relationships). Ten-day average&nbsp;<i>R</i><sub><i>e</i></sub>&nbsp;was also positively correlated with&nbsp;<i>NDVI</i>, with&nbsp;<i>R</i><sup>2</sup>values from 0.57 to 0.77. Patterns of the relationships of&nbsp;<i>P</i><sub><i>g</i></sub>&nbsp;and&nbsp;<i>R</i><sub><i>e</i></sub>&nbsp;with&nbsp;<i>NDVI</i>&nbsp;and other factors indicate possibilities for establishing multivariate functions allowing scaling-up local fluxes to larger areas using GIS data, temporal NDVI, and other factors.</p>\n</div>","language":"English","publisher":"Wiley","doi":"10.1111/j.1466-822X.2005.00151.x","usgsCitation":"Gilmanov, T.G., Tieszen, L.L., Wylie, B.K., Flanagan, L.B., Frank, A.B., Haferkamp, M.R., Meyers, T.P., and Morgan, J.A., 2005, Integration of CO2 flux and remotely-sensed data for primary production and ecosystem respiration analyses in the Northern Great Plains: potential for quantitative spatial extrapolation: Global Ecology and Biogeography, v. 14, no. 3, p. 271-292, https://doi.org/10.1111/j.1466-822X.2005.00151.x.","productDescription":"22 p.","startPage":"271","endPage":"292","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":306970,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"3","noUsgsAuthors":false,"publicationDate":"2005-03-18","publicationStatus":"PW","scienceBaseUri":"55d5a8b2e4b0518e3546a4cd","contributors":{"authors":[{"text":"Gilmanov, Tagir G.","contributorId":146124,"corporation":false,"usgs":false,"family":"Gilmanov","given":"Tagir","email":"","middleInitial":"G.","affiliations":[{"id":5089,"text":"South Dakota State University","active":true,"usgs":false}],"preferred":false,"id":568722,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tieszen, Larry L. tieszen@usgs.gov","contributorId":2831,"corporation":false,"usgs":true,"family":"Tieszen","given":"Larry","email":"tieszen@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":568723,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wylie, Bruce K. 0000-0002-7374-1083 wylie@usgs.gov","orcid":"https://orcid.org/0000-0002-7374-1083","contributorId":750,"corporation":false,"usgs":true,"family":"Wylie","given":"Bruce","email":"wylie@usgs.gov","middleInitial":"K.","affiliations":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true},{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":568724,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Flanagan, Lawrence B.","contributorId":146690,"corporation":false,"usgs":false,"family":"Flanagan","given":"Lawrence","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":568725,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Frank, Albert B.","contributorId":146693,"corporation":false,"usgs":false,"family":"Frank","given":"Albert","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":568726,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Haferkamp, Marshall R.","contributorId":98548,"corporation":false,"usgs":true,"family":"Haferkamp","given":"Marshall","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":568727,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Meyers, Tilden P.","contributorId":146138,"corporation":false,"usgs":false,"family":"Meyers","given":"Tilden","email":"","middleInitial":"P.","affiliations":[{"id":16598,"text":"NOAA/ATDD","active":true,"usgs":false}],"preferred":false,"id":568728,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Morgan, Jack A.","contributorId":66982,"corporation":false,"usgs":true,"family":"Morgan","given":"Jack","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":568729,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70179573,"text":"70179573 - 2005 - Assessment of the White Salmon watershed using the ecosystem diagnosis and treatment model ","interactions":[],"lastModifiedDate":"2017-04-25T09:46:31","indexId":"70179573","displayToPublicDate":"2005-05-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Assessment of the White Salmon watershed using the ecosystem diagnosis and treatment model ","docAbstract":"<p>Salmon habitat models provide managers the ability to identify habitat limitations and prioritize restoration activities. Ecosystem Diagnosis and Treatment (EDT) has become a widely used tool for salmonid habitat analysis in the Pacific Northwest. The EDT model is a rule-based habitat rating system that provides reach-level diagnosis of habitat conditions for the major salmonid species of the Pacific Northwest. The EDT process itself is a complex modeling program with defined data needs. The program is a product developed by Mobrand Biometrics Incorporated (MBI) largely through funding by the Northwest Power and Conservation Council (NPCC). The NPCC had provided a free version of the program accessible through a website that required user registration. </p><p>The EDT model allows the user to rate the quality, quantity, and diversity of fish habitat along a waterway. The model uses diagnostic species such as steelhead and Chinook salmon to identify the most significant limiting factors in a river and to help identify reaches for protection and restoration. The model includes a set of tools to help organize environmental information and rate the habitat elements that pertain to specific life stages of the diagnostic species. A major benefit of EDT is that it can show the potential of a river under current conditions and possible future conditions. The result is a scientifically-based assessment of fish habitat and a prioritization of restoration needs. </p>","language":"English","publisher":"Yakama Nation ","usgsCitation":"Allen, B., and Connolly, P., 2005, Assessment of the White Salmon watershed using the ecosystem diagnosis and treatment model , 55 p., Appendix A-C.","productDescription":"55 p., Appendix A-C","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":340231,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59006082e4b0e85db3a5df01","contributors":{"authors":[{"text":"Allen, Brady ballen@usgs.gov","contributorId":147932,"corporation":false,"usgs":true,"family":"Allen","given":"Brady","email":"ballen@usgs.gov","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":657786,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Connolly, Patrick J. 0000-0001-7365-7618 pconnolly@usgs.gov","orcid":"https://orcid.org/0000-0001-7365-7618","contributorId":2920,"corporation":false,"usgs":true,"family":"Connolly","given":"Patrick J.","email":"pconnolly@usgs.gov","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":657787,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70500,"text":"ofr20041274 - 2005 - Future petroleum supply - exploration or development?","interactions":[],"lastModifiedDate":"2012-02-02T00:13:32","indexId":"ofr20041274","displayToPublicDate":"2005-04-29T00:00:00","publicationYear":"2005","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":"2004-1274","title":"Future petroleum supply - exploration or development?","docAbstract":"The presentation is titled 'Future Petroleum Supply - Exploration or Development?' and provides a general overview of the magnitude and significance of reserve growth around the world. Reserve growth is defined as the increase in successive estimates of recoverable crude oil, natural gas, and natural-gas liquids and condensates in discovered fields. Analysis of recent exploration and production data shows that petroleum (both crude oil and natural gas) volumes added to reserves by reserve growth in the world are comparable to, if not greater than, the volumes added by new-field discoveries.\r\nThis presentation describes the examination of recoverable volumes of crude oil in 186 giant oil fields (excluding those of the United States (U.S.) and Canada) reported through time from 1981 to 2003 and describes a comparison of the successive increases in these volumes (reserve growth) with recoverable volumes added from new-field discoveries. Examples from the ongoing USGS study of reserve growth in the North Sea also are shown in this presentation.","language":"ENGLISH","doi":"10.3133/ofr20041274","usgsCitation":"Klett, T., 2005, Future petroleum supply - exploration or development? (Version 1.0): U.S. Geological Survey Open-File Report 2004-1274, 38 p., https://doi.org/10.3133/ofr20041274.","productDescription":"38 p.","costCenters":[],"links":[{"id":187698,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6468,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1274/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4224","contributors":{"authors":[{"text":"Klett, Timothy R. 0000-0001-9779-1168 tklett@usgs.gov","orcid":"https://orcid.org/0000-0001-9779-1168","contributorId":709,"corporation":false,"usgs":true,"family":"Klett","given":"Timothy R.","email":"tklett@usgs.gov","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":282545,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70498,"text":"wdrCA044 - 2005 - Water resources data-California, water year 2004. volume 4. northern central valley basins and the Great Basin from Honey Lake basin to Oregon state line","interactions":[],"lastModifiedDate":"2012-02-02T00:13:32","indexId":"wdrCA044","displayToPublicDate":"2005-04-29T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CA-04-4","title":"Water resources data-California, water year 2004. volume 4. northern central valley basins and the Great Basin from Honey Lake basin to Oregon state line","docAbstract":"Water-resources data for the 2004 water year for California consist of records of stage, discharge, and water quality of streams, stage and contents in lakes and reservoirs, and water levels and water quality in wells. Volume 4 contains discharge records for 188 gaging stations, stage and contents for 62 lakes and reservoirs, gage-height records for 1 station, water quality for 20 streamflow-gaging stations and 1 partial-record stations. Also included are 4 miscellaneous partial-record sites. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in California.","language":"ENGLISH","doi":"10.3133/wdrCA044","usgsCitation":"Webster, M., Rockwell, G., Friebel, M., and Brockner, S., 2005, Water resources data-California, water year 2004. volume 4. northern central valley basins and the Great Basin from Honey Lake basin to Oregon state line: U.S. Geological Survey Water Data Report CA-04-4, 482 p., https://doi.org/10.3133/wdrCA044.","productDescription":"482 p.","costCenters":[],"links":[{"id":6466,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdr-ca-04-4/","linkFileType":{"id":5,"text":"html"}},{"id":187607,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0973","contributors":{"authors":[{"text":"Webster, M.D.","contributorId":68385,"corporation":false,"usgs":true,"family":"Webster","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":282541,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rockwell, G.L.","contributorId":47408,"corporation":false,"usgs":true,"family":"Rockwell","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":282539,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Friebel, M.F.","contributorId":23207,"corporation":false,"usgs":true,"family":"Friebel","given":"M.F.","email":"","affiliations":[],"preferred":false,"id":282538,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brockner, S.J.","contributorId":56307,"corporation":false,"usgs":true,"family":"Brockner","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":282540,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70491,"text":"cir1281 - 2005 - Geography for a Changing World - A science strategy for the geographic research of the U.S. Geological Survey, 2005-2015","interactions":[],"lastModifiedDate":"2018-04-02T16:33:28","indexId":"cir1281","displayToPublicDate":"2005-04-29T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1281","title":"Geography for a Changing World - A science strategy for the geographic research of the U.S. Geological Survey, 2005-2015","docAbstract":"<p>This report presents a science strategy for the geographic research of the U.S. Geological Survey (USGS) for the years 2005-2015. The common thread running through the vision, mission, and science goals presented in the plan is that USGS geographers will provide national leadership to understand coupled human-environmental systems in the face of land change and will deliver pertinent information to decisionmakers on the vulnerability and resilience of these systems. We define land change science as the study of the human and environment dynamics that give rise to changed land use, cover, and surface form.</p><p>A number of realities shape the strategic context of this plan:</p><ul><li>The Department of Interior Strategic Plan focuses on meeting society’s resource needs and sustaining the Nation’s life support systems, underscoring the importance of characterizing and understanding coupled human-environmental systems.</li><li>In redefining its mission in the mid-1990s, the USGS envisions itself as an integrated natural science and information agency. The USGS will assume a national leadership role in the use of science to develop knowledge about the web of relations that couple biophysical and human systems and translate this knowledge into unbiased, reliable information that meets important societal information needs.</li><li>The following trends will influence USGS geography-oriented science activities over the next decade. Most of the emerging earth science issues that the USGS will address are geographic phenomena. A growing international concern for aligning society’s development activities with environmental limits has led to an articulation of a science agenda associated with global environmental change, vulnerability, and resilience. Earth science investigations have evolved toward the study of very large areas, and the resulting huge volumes of data are challenging to manage and understand. Finally, scientists and the public face the challenge of gaining intelligent insights about geographic and environmental processes from these data, with the ultimate goal of guiding resource-management decisions.</li></ul><p>The first four science goals in the plan support understanding the human and environmental dynamics of land change. Each science goal has an associated set of strategic actions to achieve the goal. These goals and actions are consistent with national science priorities and the Department of Interior and USGS missions, take advantage of existing expertise, and lead to the strengthening of critical geographic research capacities that do not exist in other USGS disciplines.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/cir1281","isbn":"0607971797","usgsCitation":"McMahon, G., Benjamin, S.P., Clarke, K., Findley, J.E., Fisher, R.N., Graf, W.L., Gundersen, L.C., Jones, J., Loveland, T., Roth, K.S., Usery, E.L., and Wood, N.J., 2005, Geography for a Changing World - A science strategy for the geographic research of the U.S. Geological Survey, 2005-2015: U.S. Geological Survey Circular 1281, xviii, 54 p., https://doi.org/10.3133/cir1281.","productDescription":"xviii, 54 p.","temporalStart":"2005-01-01","temporalEnd":"2015-12-31","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":124507,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/cir_1281.jpg"},{"id":338604,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1281/pdf/circ1281.pdf"},{"id":94173,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/circ/1281/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8fac","contributors":{"authors":[{"text":"McMahon, Gerard 0000-0001-7675-777X gmcmahon@usgs.gov","orcid":"https://orcid.org/0000-0001-7675-777X","contributorId":191488,"corporation":false,"usgs":true,"family":"McMahon","given":"Gerard","email":"gmcmahon@usgs.gov","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true},{"id":565,"text":"Southeast Climate Science Center","active":true,"usgs":true}],"preferred":true,"id":282521,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Benjamin, Susan P. sbenjamin@usgs.gov","contributorId":354,"corporation":false,"usgs":true,"family":"Benjamin","given":"Susan","email":"sbenjamin@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":282522,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clarke, Keith","contributorId":13861,"corporation":false,"usgs":true,"family":"Clarke","given":"Keith","affiliations":[],"preferred":false,"id":282527,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Findley, John E.","contributorId":72259,"corporation":false,"usgs":true,"family":"Findley","given":"John","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":282529,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fisher, Robert N. 0000-0002-2956-3240 rfisher@usgs.gov","orcid":"https://orcid.org/0000-0002-2956-3240","contributorId":1529,"corporation":false,"usgs":true,"family":"Fisher","given":"Robert","email":"rfisher@usgs.gov","middleInitial":"N.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":282523,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Graf, William L.","contributorId":92415,"corporation":false,"usgs":true,"family":"Graf","given":"William","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":282530,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Gundersen, Linda C. lgundersen@usgs.gov","contributorId":238,"corporation":false,"usgs":true,"family":"Gundersen","given":"Linda","email":"lgundersen@usgs.gov","middleInitial":"C.","affiliations":[{"id":501,"text":"Office of Science Quality and Integrity","active":true,"usgs":true}],"preferred":true,"id":282520,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Jones, John W. 0000-0001-6117-3691 jwjones@usgs.gov","orcid":"https://orcid.org/0000-0001-6117-3691","contributorId":2220,"corporation":false,"usgs":true,"family":"Jones","given":"John","email":"jwjones@usgs.gov","middleInitial":"W.","affiliations":[{"id":37786,"text":"WMA - Observing Systems Division","active":true,"usgs":true},{"id":242,"text":"Eastern Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":282524,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Loveland, Thomas R. 0000-0003-3114-6646 loveland@usgs.gov","orcid":"https://orcid.org/0000-0003-3114-6646","contributorId":3005,"corporation":false,"usgs":true,"family":"Loveland","given":"Thomas R.","email":"loveland@usgs.gov","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":false,"id":282525,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Roth, Keven S.","contributorId":46820,"corporation":false,"usgs":true,"family":"Roth","given":"Keven","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":282528,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Usery, E. Lynn 0000-0002-2766-2173 usery@usgs.gov","orcid":"https://orcid.org/0000-0002-2766-2173","contributorId":231,"corporation":false,"usgs":true,"family":"Usery","given":"E.","email":"usery@usgs.gov","middleInitial":"Lynn","affiliations":[{"id":423,"text":"National Geospatial Program","active":true,"usgs":true}],"preferred":true,"id":282519,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Wood, Nathan J. 0000-0002-6060-9729 nwood@usgs.gov","orcid":"https://orcid.org/0000-0002-6060-9729","contributorId":3347,"corporation":false,"usgs":true,"family":"Wood","given":"Nathan","email":"nwood@usgs.gov","middleInitial":"J.","affiliations":[{"id":508,"text":"Office of the AD Hazards","active":true,"usgs":true}],"preferred":true,"id":282526,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}}
,{"id":70478,"text":"sir20045293 - 2005 - Water withdrawals for irrigation, municipal, mining, thermoelectric-power, and drainage uses in Arizona outside of active management areas, 1991-2000","interactions":[],"lastModifiedDate":"2022-12-29T21:56:32.435388","indexId":"sir20045293","displayToPublicDate":"2005-04-27T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-5293","title":"Water withdrawals for irrigation, municipal, mining, thermoelectric-power, and drainage uses in Arizona outside of active management areas, 1991-2000","docAbstract":"<p>Economic development in Arizona is largely influenced by access to adequate water supplies owing to the State's predominantly semiarid to arid climate. Water demand is met by pumping ground water from aquifers or by con­veying surface water through a system of reservoirs and canals. Water-withdrawal data provide important information on how water demand affects the State's water resources. Information on water withdrawals also can help planners and managers assess the effectiveness of water-management policies, regulations, and conservation activities.</p><p>This report includes water-withdrawal data for irrigation, municipal, mining, thermoelectric-power, and drainage uses for 1991-2000, and describes the methods used to collect, compile, and estimate the data. Data are reported for the Arizona Department of Water Resources ground-water basins outside of Active Management Areas.</p><p>Because of the climate, ground water and surface water are used to irrigate nearly all agricultural fields in Arizona. Irrigation accounted for the largest use of water in the study area during 1991-2000. The amount of water withdrawn for irrigation varies greatly from year to year for some of the basins, primarily because of differences in the consumptive water requirement for different crops and because of changes in irrigated acreage.</p><p>The population of Arizona increased about 35 percent from 1991 to 2000-from about 3.79 million in 1991 to about 5.13 million in 2000. Correspondingly, water withdrawal for municipal use increased steadily in most of the basins during 1991-2000.</p><p>Ground-water withdrawals for mining did not show any consistent trends during 1991-2000. Increases and decreases in withdrawals for mining were most likely due to variations in mineral production. Mineral prices and competition from mining in other States and foreign countries probably result in annual increases or decreases in mineral production in Arizona.</p><p>Between 1991 and 2000, ground-water withdrawals for thermoelectric-power generation generally increased owing to an increase in production of electricity. Ground-water withdrawals for drainage of agricultural lands in the Lower Gila and Yuma Basins varied irregularly from year to year. Annual total water withdrawals are not presented in this report because for some years irrigation values for some of the basins are reported as \"less than 1,000 acre-feet,\" and municipal and mining values for some of the basins are reported as \"less than 300 acre-feet.\"</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20045293","usgsCitation":"Tadayon, S., 2005, Water withdrawals for irrigation, municipal, mining, thermoelectric-power, and drainage uses in Arizona outside of active management areas, 1991-2000: U.S. Geological Survey Scientific Investigations Report 2004-5293, vi, 28 p., https://doi.org/10.3133/sir20045293.","productDescription":"vi, 28 p.","costCenters":[],"links":[{"id":438870,"rank":4,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9GY1WFR","text":"USGS data release","linkHelpText":"Estimated crop irrigation water use withdrawals in Hualapai Valley Groundwater Basin, Arizona for 2021"},{"id":438869,"rank":4,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9N8PR8C","text":"USGS data release","linkHelpText":"Estimated crop irrigation water use withdrawals in Sacramento Valley Groundwater Basin, Arizona for 2021"},{"id":438868,"rank":4,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9Q22ID2","text":"USGS data release","linkHelpText":"Estimated crop irrigation water use withdrawals in Willcox Groundwater Basin, Arizona for 2020"},{"id":438867,"rank":4,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9FWMMOX","text":"USGS data release","linkHelpText":"Estimated crop irrigation water use withdrawals in Lower San Pedro Groundwater Basin, Arizona for 2020"},{"id":438866,"rank":4,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9KF6CBV","text":"USGS data release","linkHelpText":"Estimated crop irrigation water use withdrawals in Sacramento Valley Groundwater Basin, Arizona for 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,{"id":70479,"text":"tm2A2 - 2005 - Sampling protocol for monitoring abiotic and biotic characteristics of mountain ponds and lakes","interactions":[],"lastModifiedDate":"2012-02-02T00:13:35","indexId":"tm2A2","displayToPublicDate":"2005-04-27T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":335,"text":"Techniques and Methods","code":"TM","onlineIssn":"2328-7055","printIssn":"2328-7047","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2-A2","title":"Sampling protocol for monitoring abiotic and biotic characteristics of mountain ponds and lakes","docAbstract":"This document describes field techniques and procedures used for sampling mountain ponds and lakes. These techniques and procedures will be used primarily to monitor, as part of long-term programs in National Parks and other protected areas, the abiotic and biotic characteristics of naturally occurring permanent montane lentic systems up to 75 ha in surface area. However, the techniques and procedures described herein also can be used to sample temporary or ephemeral montane lentic sites. Each Standard Operating Procedure (SOP) section addresses a specific component of the limnological investigation, and describes in detail field sampling methods pertaining to parameters to be measured for each component.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Book 2. Collection of environmental data, Section A. Biological science","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/tm2A2","usgsCitation":"Hoffman, R.L., Tyler, T.J., Larson, G.L., Adams, M.J., Wente, W., and Galvan, S., 2005, Sampling protocol for monitoring abiotic and biotic characteristics of mountain ponds and lakes: U.S. Geological Survey Techniques and Methods 2-A2, 99 p., https://doi.org/10.3133/tm2A2.","productDescription":"99 p.","costCenters":[],"links":[{"id":188361,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6436,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/tm/2005/tm2a2/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fddb7","contributors":{"authors":[{"text":"Hoffman, Robert L.","contributorId":52931,"corporation":false,"usgs":true,"family":"Hoffman","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":282508,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tyler, Torrey J.","contributorId":91199,"corporation":false,"usgs":true,"family":"Tyler","given":"Torrey","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":282510,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Larson, Gary L. gary_l._larson@usgs.gov","contributorId":2990,"corporation":false,"usgs":true,"family":"Larson","given":"Gary","email":"gary_l._larson@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":282505,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Adams, M. J. 0000-0001-8844-042X mjadams@usgs.gov","orcid":"https://orcid.org/0000-0001-8844-042X","contributorId":3133,"corporation":false,"usgs":false,"family":"Adams","given":"M.","email":"mjadams@usgs.gov","middleInitial":"J.","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":282506,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wente, Wendy","contributorId":60497,"corporation":false,"usgs":true,"family":"Wente","given":"Wendy","email":"","affiliations":[],"preferred":false,"id":282509,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Galvan, Stephanie 0000-0002-9864-3674 stephanie_galvan@usgs.gov","orcid":"https://orcid.org/0000-0002-9864-3674","contributorId":3135,"corporation":false,"usgs":true,"family":"Galvan","given":"Stephanie","email":"stephanie_galvan@usgs.gov","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":true,"id":282507,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70465,"text":"sir20045002 - 2005 - Water Quality in the Halawa, Haiku, and Kaneohe Drainage Basins Before, During, and After H-3 Highway Construction, Oahu, Hawaii, 1983-1999","interactions":[],"lastModifiedDate":"2017-08-28T14:23:54","indexId":"sir20045002","displayToPublicDate":"2005-04-25T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-5002","title":"Water Quality in the Halawa, Haiku, and Kaneohe Drainage Basins Before, During, and After H-3 Highway Construction, Oahu, Hawaii, 1983-1999","docAbstract":"Selected water-quality data collected before, during, and after construction of the H-3 Highway at 13 water-quality stations were compared to the State of Hawaii Department of Health water-quality standards to determine the effects of highway construction on the water quality of the affected streams. Highway construction had no effect on the high concentrations of total nitrogen and nitrite plus nitrate nitrogen observed except for increased nitrite plus nitrate nitrogen concentrations at one station on Hooleinaiwa Stream. Exceedences of the 10- and 2-percent-of-the-time concentration standards for total phosphorus, total suspended solids, and turbidity, all constituents associated with sediment, occurred more commonly and at more stations during construction than either before or after. These exceedences may be, in part, due to land disturbance caused by highway construction. Highway construction had no effect on the physical water-quality properties of pH, dissolved oxygen, temperature, and specific conductance except at North Halawa and Kuou Streams, where specific-conductance values increased throughout the study period, most likely due to highway construction. No effects on selected trace metals and organic chemical compounds were observed due to highway construction. No effects due to highway construction were observed in the water quality of Waimaluhia Reservoir. Runoff from areas of urban land use in the Kaneohe drainage basin contributed more to the higher loads of selected water-quality constituents than did runoff from areas affected by highway construction.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20045002","collaboration":"Prepared in cooperation with the State of Hawaii Department of Transportation","usgsCitation":"Wong, M.F., 2005, Water Quality in the Halawa, Haiku, and Kaneohe Drainage Basins Before, During, and After H-3 Highway Construction, Oahu, Hawaii, 1983-1999: U.S. Geological Survey Scientific Investigations Report 2004-5002, vi, 45 p., https://doi.org/10.3133/sir20045002.","productDescription":"vi, 45 p.","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":188689,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6427,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2004/5002/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48d0e4b07f02db546610","contributors":{"authors":[{"text":"Wong, Michael F.","contributorId":43815,"corporation":false,"usgs":true,"family":"Wong","given":"Michael","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":282488,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70469,"text":"sir20055068 - 2005 - Water-quality, phytoplankton, and trophic-status characteristics of Big Base and Little Base lakes, Little Rock Air Force Base, Arkansas, 2003-2004","interactions":[],"lastModifiedDate":"2012-02-02T00:13:32","indexId":"sir20055068","displayToPublicDate":"2005-04-25T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5068","title":"Water-quality, phytoplankton, and trophic-status characteristics of Big Base and Little Base lakes, Little Rock Air Force Base, Arkansas, 2003-2004","docAbstract":"Little Rock Air Force Base is the largest C-130 base in the Air Force and is the only C-130 training base in the Department of Defense. Little Rock Air Force Base is located in central Arkansas near the eastern edge of the Ouachita Mountains, near the Mississippi Alluvial Plain, and within the Arkansas Valley Ecoregion. Habitats include upland pine forests, upland deciduous forest, broad-leaved deciduous swamps, and two small freshwater lakes?Big Base Lake and Little Base Lake. Big Base and Little Base Lakes are used primarily for recreational fishing by base personnel and the civilian public. Under normal (rainfall) conditions, Big Base Lake has a surface area of approximately 39 acres while surface area of Little Base Lake is approximately 1 acre. \r\n\r\nLittle Rock Air Force Base personnel are responsible for managing the fishery in these two lakes and since 1999 have started a nutrient enhancement program that involves sporadically adding fertilizer to Big Base Lake. As a means of determining the relations between water quality and primary production, Little Rock Air Force Base personnel have a need for biological (phytoplankton density), chemical (dissolved-oxygen and nutrient concentrations), and physical (water temperature and light transparency) data. To address these monitoring needs, the U.S. Geological Survey in cooperation with Little Rock Air Force Base, conducted a study to collect and analyze biological, chemical, and physical data. The U.S. Geological Survey sampled water quality in Big Base Lake and Little Base Lake on nine occasions from July 2003 through June 2004. Because of the difference in size, two sampling sites were established on Big Base Lake, while only one site was established on Little Base Lake. \r\n\r\nLake profile data for Big Base Lake indicate that low dissolved- oxygen concentrations in the hypolimnion probably constrain most fish species to the upper 5-6 feet of depth during the summer stratification period. Dissolved-oxygen concentrations in Big Base Lake below a depth of 6 feet generally were less than 3 milligrams per liter for summer months that were sampled in 2003 and 2004. \r\n\r\nSome evidence indicates that phosphorus was limiting primary production during the sampling period. Dissolved nitrogen constituents frequently were detected in water samples (indicating availability) but dissolved phosphorus constituents-orthophosphorus and dissolved phosphorus-were not detected in any samples collected at the two lakes. The absence of dissolved phosphorus constituents and presence of total phosphorus indicates that all phosphorus was bound to suspended material (sediment particles and living organisms). Nitrogen:phosphorus ratios on most sampling occasions tended to be slightly higher than 16:1, which can be interpreted as further indication that phosphorus could be limiting primary production to some extent. \r\n\r\nAn alkalinity of 20 milligrams per liter of calcium carbonate or higher is recommended to optimize nutrient availability and buffering capacity in recreational fishing lakes and ponds. Median values for water samples collected at the three sites ranged from 12-13 milligrams per liter of calcium carbonate. Alkalinities ranged from 9-60 milligrams per liter of calcium carbonate, but 13 of 17 samples collected at the deepest site had alkalinities less than 20 milligrams per liter of calcium carbonate. \r\n\r\nResults of three trophic-state indices, and a general trophic classification, as well as abundant green algae and large growths of blue-green algae indicate that Big Base Lake may be eutrophic. Trophic-state index values calculated using total phosphorus, chlorophyll a, and Secchi disc measurements from both lakes generally exceeded criteria at which lakes are considered to be eutrophic. A second method of determining lake trophic status-the general trophic classification-categorized the three sampling sites as mesotrophic or eutrophic. Green algae were found to be in abundance throughout mos","language":"ENGLISH","doi":"10.3133/sir20055068","usgsCitation":"Justus, B., 2005, Water-quality, phytoplankton, and trophic-status characteristics of Big Base and Little Base lakes, Little Rock Air Force Base, Arkansas, 2003-2004: U.S. Geological Survey Scientific Investigations Report 2005-5068, 37 p., https://doi.org/10.3133/sir20055068.","productDescription":"37 p.","costCenters":[],"links":[{"id":6431,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5068/","linkFileType":{"id":5,"text":"html"}},{"id":188859,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e5191","contributors":{"authors":[{"text":"Justus, B. G.","contributorId":49825,"corporation":false,"usgs":true,"family":"Justus","given":"B. G.","affiliations":[],"preferred":false,"id":282499,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70467,"text":"sir20055078 - 2005 - Evaluating regional trends in ground-water nitrate concentrations of the Columbia Basin ground water management area, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:13:32","indexId":"sir20055078","displayToPublicDate":"2005-04-25T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5078","title":"Evaluating regional trends in ground-water nitrate concentrations of the Columbia Basin ground water management area, Washington","docAbstract":"Trends in nitrate concentrations in water from 474 wells in 17 subregions in the Columbia Basin Ground Water Management Area (GWMA) in three counties in eastern Washington were evaluated using a variety of statistical techniques, including the Friedman test and the Kendall test. The Kendall test was modified from its typical 'seasonal' version into a 'regional' version by using well locations in place of seasons. No statistically significant trends in nitrate concentrations were identified in samples from wells in the GWMA, the three counties, or the 17 subregions from 1998 to 2002 when all data were included in the analysis. For wells in which nitrate concentrations were greater than 10 milligrams per liter (mg/L), however, a significant downward trend of -0.4 mg/L per year was observed between 1998 and 2002 for the GWMA as a whole, as well as for Adams County (-0.35 mg/L per year) and for Franklin County (-0.46 mg/L per year). Trend analysis for a smaller but longer-term 51-well dataset in Franklin County found a statistically significant upward trend in nitrate concentrations of 0.1 mg/L per year between 1986 and 2003. The largest increase of nitrate concentrations occurred between 1986 and 1991. No statistically significant differences were observed in this dataset between 1998 and 2003 indicating that the increase in nitrate concentrations has leveled off.","language":"ENGLISH","doi":"10.3133/sir20055078","usgsCitation":"Frans, L.M., and Helsel, D., 2005, Evaluating regional trends in ground-water nitrate concentrations of the Columbia Basin ground water management area, Washington: U.S. Geological Survey Scientific Investigations Report 2005-5078, 14 p., https://doi.org/10.3133/sir20055078.","productDescription":"14 p.","costCenters":[],"links":[{"id":188775,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6429,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5078/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db655599","contributors":{"authors":[{"text":"Frans, Lonna M. 0000-0002-3217-1862 lmfrans@usgs.gov","orcid":"https://orcid.org/0000-0002-3217-1862","contributorId":1493,"corporation":false,"usgs":true,"family":"Frans","given":"Lonna","email":"lmfrans@usgs.gov","middleInitial":"M.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282496,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Helsel, Dennis R.","contributorId":85569,"corporation":false,"usgs":true,"family":"Helsel","given":"Dennis R.","affiliations":[],"preferred":false,"id":282497,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70466,"text":"sir20045146 - 2005 - Chemical characteristics of ground-water discharge along the south rim of Grand Canyon in Grand Canyon National Park, Arizona, 2000-2001","interactions":[],"lastModifiedDate":"2020-02-04T09:14:13","indexId":"sir20045146","displayToPublicDate":"2005-04-25T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-5146","title":"Chemical characteristics of ground-water discharge along the south rim of Grand Canyon in Grand Canyon National Park, Arizona, 2000-2001","docAbstract":"Springs flowing from the south rim of Grand Canyon are an important resource of Grand Canyon National Park, offering refuge to endemic and exotic terrestrial wildlife species and maintaining riparian areas. Population growth on the Coconino Plateau has increased the demand for additional development of ground-water resources, and such development could reduce spring discharge and affect the sustainability of riparian areas within the park. In addition, springs are an important source of drinking water for hikers and are culturally and economically important to Native Americans living in the region.\r\n\r\n\r\nWater samples were collected from May 2000 to September 2001 from 20 spring and creek sites that discharge water from the Redwall-Muav Limestone aquifer along the south rim of Grand Canyon. Sample collection sites were described and samples were analyzed for major ions, nutrients, trace elements, radioactivity, and selected isotopes, and potential sources of ground-water flow to the springs. Rock samples representing the major stratigraphic units of Grand Canyon were collected near the Bright Angel Fault and analyzed for mineralogy, strontium-87/strontium-86, and \r\ncarbon-13/carbon-12.\r\n\r\n\r\nThe chemical composition of water samples collected from a given spring did not vary appreciably over the course of the study. Although water at each spring had a temporally constant composition, the composition was chemically distinct from that of every other spring sampled, indicating spatial variability in the ground-water composition. Most samples had a calcium magnesium bicarbonate composition; a few had a substantial sulfate component. Concentrations of arsenic, nitrate, selenium, uranium, and gross alpha approached or exceeded U.S. Environmental Protection Agency Maximum Contaminant Levels in water discharging from some springs. Oxygen and hydrogen isotopic compositions varied little among samples, and for most sites the isotopic data plot close to the global meteoric water line or below the local meteoric water line. Isotopic enrichment indicates fractionation due to evaporation occurs at some sites. The evaporative process may occur prior to recharge or post-discharge. Flow paths are differentiated between the eastern part of the study area where strontium-87/strontium-86 values for water from springs and creeks are more radiogenic than strontium-87/strontium-86 values for water that discharges from sites farther west. Tritium and carbon isotope analyses indicate that residence time of ground-water discharge from springs and creeks ranges from less than 50 years to about 3,400 years. Water with a residence time of less than 50 years is absent at several sites. Discharge of most springs and creeks is a mixture of younger and older waters.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20045146","usgsCitation":"Monroe, S.A., Antweiler, R.C., Hart, R.J., Taylor, H.E., Truini, M., Rihs, J.R., and Felger, T.J., 2005, Chemical characteristics of ground-water discharge along the south rim of Grand Canyon in Grand Canyon National Park, Arizona, 2000-2001: U.S. Geological Survey Scientific Investigations Report 2004-5146, 71 p., https://doi.org/10.3133/sir20045146.","productDescription":"71 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":188774,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6428,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2004-5146/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Arizona","otherGeospatial":"Grand Canyon National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.587890625,\n              35.96689214303232\n            ],\n            [\n              -111.84356689453125,\n              35.96689214303232\n            ],\n            [\n              -111.84356689453125,\n              36.48093224547937\n            ],\n            [\n              -112.587890625,\n              36.48093224547937\n            ],\n            [\n              -112.587890625,\n              35.96689214303232\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e4742","contributors":{"authors":[{"text":"Monroe, Stephen A.","contributorId":103313,"corporation":false,"usgs":true,"family":"Monroe","given":"Stephen","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":282495,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Antweiler, Ronald C. 0000-0001-5652-6034 antweil@usgs.gov","orcid":"https://orcid.org/0000-0001-5652-6034","contributorId":1481,"corporation":false,"usgs":true,"family":"Antweiler","given":"Ronald","email":"antweil@usgs.gov","middleInitial":"C.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":282492,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hart, Robert J. bhart@usgs.gov","contributorId":598,"corporation":false,"usgs":true,"family":"Hart","given":"Robert","email":"bhart@usgs.gov","middleInitial":"J.","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282489,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Taylor, Howard E. hetaylor@usgs.gov","contributorId":1551,"corporation":false,"usgs":true,"family":"Taylor","given":"Howard","email":"hetaylor@usgs.gov","middleInitial":"E.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":282493,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Truini, Margot mtruini@usgs.gov","contributorId":599,"corporation":false,"usgs":true,"family":"Truini","given":"Margot","email":"mtruini@usgs.gov","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282490,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Rihs, John R.","contributorId":57954,"corporation":false,"usgs":true,"family":"Rihs","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":282494,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Felger, Tracey J. 0000-0003-0841-4235 tfelger@usgs.gov","orcid":"https://orcid.org/0000-0003-0841-4235","contributorId":1117,"corporation":false,"usgs":true,"family":"Felger","given":"Tracey","email":"tfelger@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":282491,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
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