{"pageNumber":"3158","pageRowStart":"78925","pageSize":"25","recordCount":184883,"records":[{"id":38190,"text":"fs06900 - 2001 - Status of shallow-aquifer mapping in the Northern Front Range Area, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:09:53","indexId":"fs06900","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"069-00","title":"Status of shallow-aquifer mapping in the Northern Front Range Area, Colorado","docAbstract":"Mapping of shallow aquifers in the northern Front Range area of Colorado has been completed as part of the U.S. Geological Survey Front Range Infrastructure Resources Project. The aquifer mapping was undertaken as part of a comprehensive effort to better define the mineral, energy, cartographic, biological, and water resources that are critical to the support and development of the area's infrastructure, such as streets. highways, airports, and buildings. The aquifer mapping was undertaken in cooperation with the Colorado Division of Water Resources and the Colorado Water Conservation Board.\r\n\r\nThe shallow aquifers have been mapped in a 2,450-square-mile area extending as an approximately 30-mile-wide band from north of Fort Collins to the Arapahoe-Douglas County line south of Denver (fig. I). The shallow aquifer mapping in the Denver metropolitan area was published in 1996 as Hydrologic Investigations Atlas HA-736 (Robson. 1996). Shallow aquifer mapping in the Greeley-Nunn area was published as HA-746A (Robson, Arnold, and Heiny, 2000a); mapping in the Fort Collins-Loveland area was published as HA-746B (Robson, Arnold, and Heiny, 2000b); mapping in the Fort Lupton-Gilcrest area was published as HA-746C (Robson, Heiny, and Arnold, 2000c); and mapping in the Boulder-Longmont area was published as HA-746D (Robson, Heiny, and Arnold, 2000d).\r\n\r\nEach of the five atlases contains five map sheets at 1:50,000 scale showing: \r\n1. The thickness and extent of the unconsolidated sediments (loose gravel. sand. silt, and clay) that overlie the bedrock formations in the area (fig. 2). \r\n2. The altitude and configuration of the bedrock surface. \r\n3. The altitude of the water table and direction of ground-water movement. \r\n4. The saturated thickness of the shallow aquifers. \r\n5. The depth to the water table in the shallow aquifers.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/fs06900","usgsCitation":"Robson, S.G., 2001, Status of shallow-aquifer mapping in the Northern Front Range Area, Colorado: U.S. Geological Survey Fact Sheet 069-00, 2 p., https://doi.org/10.3133/fs06900.","productDescription":"2 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":126820,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2000/0069/report-thumb.jpg"},{"id":64481,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2000/0069/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df6de","contributors":{"authors":[{"text":"Robson, Stanley G.","contributorId":73187,"corporation":false,"usgs":true,"family":"Robson","given":"Stanley","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":219296,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":54169,"text":"wdrGA011 - 2001 - Water Resources Data, Georgia, 2001, Volume 1: Continuous water-level, streamflow, water-quality data, and periodic water-quality data, Water Year 2001","interactions":[],"lastModifiedDate":"2017-01-18T13:37:58","indexId":"wdrGA011","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","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":"GA-01-1","title":"Water Resources Data, Georgia, 2001, Volume 1: Continuous water-level, streamflow, water-quality data, and periodic water-quality data, Water Year 2001","docAbstract":"Water resources data for the 2001 water year for Georgia consists of records of stage, discharge, and water quality of streams; and the stage and contents of lakes and reservoirs published in two volumes in a digital format on a CD-ROM. Volume one of this report contains water resources data for Georgia collected during water year 2001, including: discharge records of 133 gaging stations; stage for 144 gaging stations; precipitation for 58 gaging stations; information for 19 lakes and reservoirs; continuous water-quality records for 17 stations; the annual peak stage and annual peak discharge for 76 crest-stage partial-record stations; and miscellaneous streamflow measurements at 27 stations, and miscellaneous water-quality data recorded by the NAWQA program in Georgia. Volume two of this report contains water resources data for Georgia collected during calendar year 2001, including continuous water-level records of 159 ground-water wells and periodic records at 138 water-quality stations. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Georgia.\r\n\r\nNote: Historically, this report was published as a paper report. For the 1999 and subsequent water-year reports, the Water Resources Data for Georgia changed to a new, more informative and functional format on CD-ROM. The format is based on a geographic information system (GIS) user interface that allows the user to view map locations of the hydrologic monitoring stations and networks within respective river basins.","language":"ENGLISH","doi":"10.3133/wdrGA011","usgsCitation":"McCallum, B.E., Kerestes, J.F., and Hickey, A.C., 2001, Water Resources Data, Georgia, 2001, Volume 1: Continuous water-level, streamflow, water-quality data, and periodic water-quality data, Water Year 2001: U.S. Geological Survey Water Data Report GA-01-1, 1120 p., https://doi.org/10.3133/wdrGA011.","productDescription":"1120 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":181280,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5615,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdrga01/","linkFileType":{"id":5,"text":"html"}}],"country":"United 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478ee4b07f02db489fb8","contributors":{"authors":[{"text":"McCallum, Brian E. 0000-0002-8935-0343 bemccall@usgs.gov","orcid":"https://orcid.org/0000-0002-8935-0343","contributorId":1591,"corporation":false,"usgs":true,"family":"McCallum","given":"Brian","email":"bemccall@usgs.gov","middleInitial":"E.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":249411,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kerestes, John F.","contributorId":72061,"corporation":false,"usgs":true,"family":"Kerestes","given":"John","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":249413,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hickey, Andrew C.","contributorId":60713,"corporation":false,"usgs":true,"family":"Hickey","given":"Andrew","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":249412,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":54170,"text":"wdrGA012 - 2001 - Water Resources Data, Georgia, 2001, Volume 2: Continuous ground-water level data, and periodic surface-water- and ground-water-quality data, Calendar Year 2001","interactions":[],"lastModifiedDate":"2017-01-18T13:39:54","indexId":"wdrGA012","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","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":"GA-01-2","title":"Water Resources Data, Georgia, 2001, Volume 2: Continuous ground-water level data, and periodic surface-water- and ground-water-quality data, Calendar Year 2001","docAbstract":"Water resources data for the 2001 water year for Georgia consists of records of stage, discharge, and water quality of streams; and the stage and contents of lakes and reservoirs published in two volumes in a digital format on a CD-ROM. Volume one of this report contains water resources data for Georgia collected during water year 2001, including: discharge records of 133 gaging stations; stage for 144 gaging stations; precipitation for 58 gaging stations; information for 19 lakes and reservoirs; continuous water-quality records for 17 stations; the annual peak stage and annual peak discharge for 76 crest-stage partial-record stations; and miscellaneous streamflow measurements at 27 stations, and miscellaneous water-quality data recorded by the NAWQA program in Georgia. Volume two of this report contains water resources data for Georgia collected during calendar year 2001, including continuous water-level records of 159 ground-water wells and periodic records at 138 water-quality stations. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Georgia.\r\n\r\nNote: Historically, this report was published as a paper report. For the 1999 and subsequent water-year reports, the Water Resources Data for Georgia changed to a new, more informative and functional format on CD-ROM. The format is based on a geographic information system (GIS) user interface that allows the user to view map locations of the hydrologic monitoring stations and networks within respective river basins.\r\n\r\n\r\nTo obtain a copy of the CD version of this report, you may call the U.S. Geological Survey office in Atlanta at (770) 903-9100, or send e-mail to request the publication. Please include your name and mailing address in your e-mail.","language":"ENGLISH","doi":"10.3133/wdrGA012","usgsCitation":"Coffin, R., Grams, S.C., Cressler, A.M., and Leeth, D.C., 2001, Water Resources Data, Georgia, 2001, Volume 2: Continuous ground-water level data, and periodic surface-water- and ground-water-quality data, Calendar Year 2001: U.S. Geological Survey Water Data Report GA-01-2, 590 p., https://doi.org/10.3133/wdrGA012.","productDescription":"590 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":181365,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5616,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdrga01/","linkFileType":{"id":5,"text":"html"}}],"country":"United 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,{"id":54680,"text":"wdrMI001 - 2001 - Water resources data, Michigan, water year 2000","interactions":[],"lastModifiedDate":"2017-07-26T15:06:05","indexId":"wdrMI001","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","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":"MI-00-1","title":"Water resources data, Michigan, water year 2000","docAbstract":"<p>Water resources data for the 2000 water year for Michigan consists of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water quality of groundwater wells. This report contains discharge records for 147 streamflow-gaging stations; stage only records for 2 stream-gaging stations and 25 lake-gaging stations; stage and contents for 1 reservoir; water-quality records for 29 streamflow-gaging stations and 1 lake-gaging station; and water-level records for 40 ground-water wells. Also included are 30 crest-stage partial-record stations. Additional water data were collected at various sites not involved in the systematic data-collection program. Miscellaneous data were collected at 76 discharge measuring sites and 34 ground water special-study sites. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State, local, and Federal agencies in Michigan.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMI001","collaboration":"Prepared in cooperation with the State of Michigan and with other agencies","usgsCitation":"Blumer, S.P., Behrendt, T., Ellis, J., Minnerick, R., LeuVoy, R., and Whited, C., 2001, Water resources data, Michigan, water year 2000: U.S. Geological Survey Water Data Report MI-00-1, xviii, 408 p., https://doi.org/10.3133/wdrMI001.","productDescription":"xviii, 408 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":87896,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/2000/mi-00-1/report.pdf","text":"Report","size":"7.96 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":182201,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/2000/mi-00-1/report-thumb.jpg"}],"country":"United 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,{"id":54286,"text":"wdrMDDEDC002 - 2001 - Water resources data Maryland, Delaware, and Washington, D.C., water year 2000, volume 2. ground-water data","interactions":[],"lastModifiedDate":"2012-02-02T00:11:53","indexId":"wdrMDDEDC002","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","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":"MD-DE-DC-00-2","title":"Water resources data Maryland, Delaware, and Washington, D.C., water year 2000, volume 2. ground-water data","docAbstract":"Water resources data for the 2000 water year for Maryland and Delaware consist of records of water levels and water quality of ground-water wells. This report (Volume 2. Ground-Water Data) contains water levels at 347 observation wells, discharge records for 5 springs, and water quality at 225 wells, 13 piezometers, and 4 springs. Locations of ground-water level wells are shown on figures 5 and 6. Locations of ground-water-quality sites are shown on figure 7. The data in this report represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State, local, and Federal agencies in Maryland and Delaware.","language":"ENGLISH","doi":"10.3133/wdrMDDEDC002","usgsCitation":"Smigaj, M.J., Saffer, R.W., and Marchand, E., 2001, Water resources data Maryland, Delaware, and Washington, D.C., water year 2000, volume 2. ground-water data: U.S. Geological Survey Water Data Report MD-DE-DC-00-2, 568 p., https://doi.org/10.3133/wdrMDDEDC002.","productDescription":"568 p.","costCenters":[],"links":[{"id":5400,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdr-md-de-dc-00-2/","linkFileType":{"id":5,"text":"html"}},{"id":174198,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a02e4b07f02db5f804a","contributors":{"authors":[{"text":"Smigaj, Michael J.","contributorId":27917,"corporation":false,"usgs":true,"family":"Smigaj","given":"Michael","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":249766,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Saffer, Richard W.","contributorId":79951,"corporation":false,"usgs":true,"family":"Saffer","given":"Richard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":249768,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Marchand, Elizabeth H.","contributorId":29874,"corporation":false,"usgs":true,"family":"Marchand","given":"Elizabeth H.","affiliations":[],"preferred":false,"id":249767,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":54481,"text":"wdrFL003A - 2001 - Water resources data, Florida, water year 2000; Volume 3A. Southwest Florida surface water","interactions":[],"lastModifiedDate":"2023-01-23T21:25:00.093271","indexId":"wdrFL003A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","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":"FL-00-3A","title":"Water resources data, Florida, water year 2000; Volume 3A. Southwest Florida surface water","docAbstract":"<p>The Water Resources Division of the U.S. Geological Survey, in cooperation with local, State, and Federal agencies, obtains a large amount of data pertaining to the water resources of Florida each water year. These data, accumulated during many water years, constitute a valuable data base for developing an improved understanding of the water resources of the State. To make these data readily available to interested parties outside the Geological Survey, the data are published annually in this report series entitled \"Water Resources Data - Florida.\"</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrFL003A","collaboration":"Prepared in cooperation with the State of Florida and with other agencies","usgsCitation":"Coffin, J., and Fletcher, W., 2001, Water resources data, Florida, water year 2000; Volume 3A. 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,{"id":50465,"text":"ofr01494 - 2001 - Average annual precipitation classes to characterize watersheds in North Carolina","interactions":[],"lastModifiedDate":"2024-03-05T13:51:03.205271","indexId":"ofr01494","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","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":"01-494","displayTitle":"Average Annual Precipitation Classes to Characterize Watersheds in North Carolina","title":"Average annual precipitation classes to characterize watersheds in North Carolina","docAbstract":"This web site contains the Federal Geographic Data Committee-compliant metadata (documentation) for digital data produced for the North Carolina, Department of Environment and Natural Resources, Public Water Supply Section, Source Water Assessment Program. 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Carolina\",\"nation\":\"USA  \"}}]}","edition":"Version 1.0","contact":"<p><a href=\"mailto:dc_sc@usgs.gov\" data-mce-href=\"mailto:dc_sc@usgs.gov\">Director</a>, <a href=\"https://www.usgs.gov/centers/sawsc\" data-mce-href=\"https://www.usgs.gov/centers/sawsc\">South Atlantic Water Science Center</a><br>U.S. Geological Survey<br>720 Gracern Road<br>Columbia, SC 29210</p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Purpose</li><li>Contents</li><li>Links to Metadata</li><li>References</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649cc6","contributors":{"authors":[{"text":"Terziotti, Silvia 0000-0003-3559-5844 seterzio@usgs.gov","orcid":"https://orcid.org/0000-0003-3559-5844","contributorId":1613,"corporation":false,"usgs":true,"family":"Terziotti","given":"Silvia","email":"seterzio@usgs.gov","affiliations":[{"id":476,"text":"North Carolina Water Science Center","active":true,"usgs":true},{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":241518,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eimers, Jo Leslie","contributorId":52946,"corporation":false,"usgs":true,"family":"Eimers","given":"Jo Leslie","affiliations":[],"preferred":false,"id":241519,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":50460,"text":"ofr01487 - 2001 - Estimated depth to water, North Carolina","interactions":[],"lastModifiedDate":"2024-03-05T13:59:23.549941","indexId":"ofr01487","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","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":"01-487","displayTitle":"Estimated Depth to Water, North Carolina","title":"Estimated depth to water, North Carolina","docAbstract":"This web site contains the Federal Geographic Data Committee-compliant metadata (documentation) for digital data produced for the North Carolina, Department of Environment and Natural Resources, Public Water Supply Section, Source Water Assessment Program. The metadata are for 11 individual Geographic Information System data sets. An overlay and indexing method was used with the data to derive a rating for unsaturated zone and watershed characteristics for use by the State of North Carolina in assessing more than 11,000 public water-supply wells and approximately 245 public surface-water intakes for susceptibility to contamination. For ground-water supplies, the digital data sets used in the assessment included unsaturated zone rating, vertical series hydraulic conductance, land-surface slope, and land cover. For assessment of public surface-water intakes, the data sets included watershed characteristics rating, average annual precipitation, land-surface slope, land cover, and ground-water contribution. Documentation for the land-use data set applies to both the unsaturated zone and watershed characteristics ratings. Documentation for the estimated depth-to-water map used in the calculation of the vertical series hydraulic conductance also is included.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr01487","usgsCitation":"Eimers, J., Terziotti, S., and Giorgino, M.J., 2001, Estimated depth to water, North Carolina (Version 1.0): U.S. Geological Survey Open-File Report 01-487, HTML Document; Metadata, https://doi.org/10.3133/ofr01487.","productDescription":"HTML Document; Metadata","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":4270,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/0487/index.html","linkFileType":{"id":5,"text":"html"}},{"id":176633,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"North 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Carolina\",\"nation\":\"USA  \"}}]}","edition":"Version 1.0","contact":"<p><a href=\"mailto:dc_sc@usgs.gov\" data-mce-href=\"mailto:dc_sc@usgs.gov\">Director</a>, <a href=\"https://www.usgs.gov/centers/sawsc\" data-mce-href=\"https://www.usgs.gov/centers/sawsc\">South Atlantic Water Science Center</a> <br>U.S. Geological Survey<br>720 Gracern Road<br>Columbia, SC 29210</p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Purpose</li><li>Contents</li><li>Links to Metadata</li><li>References</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd145","contributors":{"authors":[{"text":"Eimers, Jo Leslie","contributorId":52946,"corporation":false,"usgs":true,"family":"Eimers","given":"Jo Leslie","affiliations":[],"preferred":false,"id":241508,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Terziotti, Silvia 0000-0003-3559-5844 seterzio@usgs.gov","orcid":"https://orcid.org/0000-0003-3559-5844","contributorId":1613,"corporation":false,"usgs":true,"family":"Terziotti","given":"Silvia","email":"seterzio@usgs.gov","affiliations":[{"id":476,"text":"North Carolina Water Science Center","active":true,"usgs":true},{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":241507,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Giorgino, Mary J.","contributorId":55862,"corporation":false,"usgs":true,"family":"Giorgino","given":"Mary","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":241509,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":45051,"text":"wri20014095 - 2001 - Isotopic and chemical composition of inorganic and organic water-quality samples from the Mississippi River Basin, 1997-98","interactions":[],"lastModifiedDate":"2020-02-23T17:04:31","indexId":"wri20014095","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4095","title":"Isotopic and chemical composition of inorganic and organic water-quality samples from the Mississippi River Basin, 1997-98","docAbstract":"<p>Nitrate (NO<sub>3</sub>) and other nutrients discharged by the Mississippi River combined with seasonal stratification of the water column are known to cause a zone of depleted dissolved oxygen (hypoxic zone) in the Gulf of Mexico each summer. About 120 water and suspended sediment samples collected in 1997 and 1998 from 24 locations in the Mississippi River Basin were analyzed for the isotope ratios δ<sup>15</sup>N and δ<sup>18</sup>O of dissolved NO<sub>3</sub>, and δ<sup>15</sup>N and δ<sup>13</sup>C of suspended particulate organic material (POM). Sampling stations include both large rivers (drainage areas more than 30,000 square kilometers) that integrate the effects of many land uses, and smaller streams (drainage areas less than 2,500 square kilometers) that have relatively uniform land use within their drainage areas. The data are used to determine sources and transformations of NO<sub>3</sub> in the Mississippi River.</p><p>Results of this study demonstrate that much of the NO<sub>3</sub> in the Mississippi River originates in the agriculturally dominated basins of the upper midwestern United States and is transported without significant transformation or other loss to the Gulf of Mexico. Results from major tributaries that drain into the Mississippi River suggest that NO<sub>3</sub> is not significantly altered by denitrification in its journey, ultimately, to the Gulf of Mexico. The spatial variability of isotope ratios among the smaller streams appears to be related to the dominant nitrogen source in the basins. There are some distinct isotope differences among land-use types. For example, for both NO<sub>3</sub> and POM, the majority of δ<sup>15</sup>N isotope ratio values from basins dominated by urban and undeveloped land are less than +5 per mil, whereas the majority of values from basins dominated by row crops and row crops and/or livestock production are greater than +5 per mil. Also, the median δ<sup>18</sup>O of NO<sub>3</sub> isotope ratio value (+14.0 per mil) from undeveloped basins is more than 6 per mil higher than the median value (+7.3 per mil) from the row crop dominated basins and 5 per mil higher than the median value (+9.0 per mil) from the row crop and/or livestock production dominated basins. The median δ<sup>18</sup>O of NO<sub>3</sub> isotope ratio value (+21.5 per mil) from urban basins is 6.5 per mil higher than the median value (+14.0 per mil) from the undeveloped basins. The majority of NO<sub>3</sub> concentrations are greater than 3 milligrams per liter (mg/L) in basins dominated by row crops and row crops and/or livestock production, whereas all NO<sub>3</sub> concentrations are less than 2 mg/L in basins dominated by urban and undeveloped land.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/wri20014095","usgsCitation":"Battaglin, W.A., Kendall, C., Chang, C., Silva, S., and Campbell, D.H., 2001, Isotopic and chemical composition of inorganic and organic water-quality samples from the Mississippi River Basin, 1997-98: U.S. Geological Survey Water-Resources Investigations Report 2001-4095, v, 57 p., https://doi.org/10.3133/wri20014095.","productDescription":"v, 57 p.","costCenters":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true},{"id":595,"text":"U.S. Geological 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ckendall@usgs.gov","orcid":"https://orcid.org/0000-0002-0247-3405","contributorId":1462,"corporation":false,"usgs":true,"family":"Kendall","given":"Carol","email":"ckendall@usgs.gov","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":230995,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chang, Cecily C.Y.","contributorId":62668,"corporation":false,"usgs":true,"family":"Chang","given":"Cecily C.Y.","affiliations":[],"preferred":false,"id":230999,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Silva, Steven R.","contributorId":59102,"corporation":false,"usgs":true,"family":"Silva","given":"Steven R.","affiliations":[],"preferred":false,"id":230998,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Campbell, Donald H. dhcampbe@usgs.gov","contributorId":1670,"corporation":false,"usgs":true,"family":"Campbell","given":"Donald","email":"dhcampbe@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":230997,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":44662,"text":"fs10701 - 2001 - Ciencia, Sociedad, Soluciones: Una Introduccion al USGS","interactions":[],"lastModifiedDate":"2026-01-30T19:18:51.711783","indexId":"fs10701","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"107-01","title":"Ciencia, Sociedad, Soluciones: Una Introduccion al USGS","language":"Spanish","publisher":"U.S. Geological Survey","doi":"10.3133/fs10701","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2001, Ciencia, Sociedad, Soluciones: Una Introduccion al USGS (Spanish edition of FS-010-01): U.S. Geological Survey Fact Sheet 107-01, -, https://doi.org/10.3133/fs10701.","productDescription":"-","costCenters":[],"links":[{"id":81964,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2001/0107/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":125245,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2001/0107/report-thumb.jpg"}],"edition":"Spanish edition of FS-010-01","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db672d17","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531552,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21661,"text":"ofr0127 - 2001 - Chemical and radiochemical constituents in water from wells in the vicinity of the Naval Reactors Facility, Idaho National Engineering and Environmental Laboratory, Idaho, 1999","interactions":[],"lastModifiedDate":"2024-01-12T21:55:31.755811","indexId":"ofr0127","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","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":"2001-27","title":"Chemical and radiochemical constituents in water from wells in the vicinity of the Naval Reactors Facility, Idaho National Engineering and Environmental Laboratory, Idaho, 1999","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0127","issn":"0566-8174","usgsCitation":"Bartholomay, R.C., Knobel, L., Tucker, B., and Twining, B., 2001, Chemical and radiochemical constituents in water from wells in the vicinity of the Naval Reactors Facility, Idaho National Engineering and Environmental Laboratory, Idaho, 1999: U.S. Geological Survey Open-File Report 2001-27, iv, 37 p., https://doi.org/10.3133/ofr0127.","productDescription":"iv, 37 p.","costCenters":[],"links":[{"id":424393,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_37083.htm","linkFileType":{"id":5,"text":"html"}},{"id":156094,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2001/0027/report-thumb.jpg"},{"id":95448,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0027/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -112.952,\n              43.709\n            ],\n            [\n              -112.952,\n              43.612\n            ],\n            [\n              -112.875,\n              43.612\n            ],\n            [\n              -112.875,\n              43.709\n            ],\n            [\n              -112.952,\n              43.709\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e47d2","contributors":{"authors":[{"text":"Bartholomay, R. C.","contributorId":66271,"corporation":false,"usgs":true,"family":"Bartholomay","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":185142,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knobel, L.L.","contributorId":83115,"corporation":false,"usgs":true,"family":"Knobel","given":"L.L.","affiliations":[],"preferred":false,"id":185143,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tucker, B.J.","contributorId":42230,"corporation":false,"usgs":true,"family":"Tucker","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":185140,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Twining, B.V.","contributorId":57102,"corporation":false,"usgs":true,"family":"Twining","given":"B.V.","email":"","affiliations":[],"preferred":false,"id":185141,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":45009,"text":"wri014101 - 2001 - Hydrologic conditions and water quality in an agricultural area in Kleberg and Nueces Counties, Texas, 1996-98","interactions":[],"lastModifiedDate":"2016-09-09T13:06:43","indexId":"wri014101","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4101","title":"Hydrologic conditions and water quality in an agricultural area in Kleberg and Nueces Counties, Texas, 1996-98","docAbstract":"During 1996?98, rainfall and runoff were\r\nmonitored on a 49,680-acre agricultural watershed\r\nin Kleberg and Nueces Counties in South Texas.\r\nNineteen rainfall samples were analyzed for\r\nselected nutrients, and runoff samples from 29\r\nstorms were analyzed for major ions, nutrients, and\r\npesticides. Loads of nutrients in rainfall and loads\r\nof nutrients and pesticides in runoff were computed.\r\nFor a 40,540-acre part of the watershed\r\n(lower study area), constituent loads entering the\r\nwatershed in rainfall, in runoff from the upper\r\nstudy area, and from agricultural chemical applications\r\nto the lower study area were compared with\r\nrunoff loads exiting the lower study area.\r\nTotal rainfall for 1996?98 averaged 25.86\r\ninches per year, which is less than the long-term\r\nannual average rainfall of 29.80 inches for the area.\r\nRainfall and runoff during 1996?98 were typical of\r\nhistorical patterns, with periods of below average\r\nrainfall and runoff interspersed with extreme\r\nevents. Five individual storms accounted for about\r\n38 percent of the total rainfall and 94 percent of the\r\ntotal runoff.\r\nDuring the 3-year study, the total nitrogen\r\nrunoff yield from the lower study area was 1.3\r\npounds per acre per year, compared with 49 pounds\r\nper acre per year applied as fertilizer and 3.1\r\npounds per acre per year from rainfall. While\r\nalmost all of the fertilizer and rainfall nitrogen was\r\nammonia and nitrate, most of the nitrogen in runoff\r\nwas particulate organic nitrogen, associated with\r\ncrop residue. Total nitrogen exiting the lower study\r\narea in surface-water runoff was about 2.5 percent\r\nof the nitrogen inputs (fertilizer and rainfall nitrogen).\r\nAnnual deposition of total nitrogen entering\r\nthe lower study area in rainfall exceeded net yields\r\nof total nitrogen exiting the watershed in runoff\r\nbecause most of the rainfall does not contribute to\r\nrunoff.\r\nDuring the study, the total phosphorus runoff\r\nyield from the lower study area was 0.48 pound per\r\nacre per year compared with 4.2 pounds per acre\r\nper year applied as fertilizer and 0.03 pound per\r\nacre per year from rainfall.\r\nTwenty-one pesticides were detected in\r\nrunoff with varying degrees of frequency during\r\nthe study. The herbicide atrazine was detected in\r\nall runoff samples. All of the most frequently\r\ndetected pesticides (atrazine, trifluralin, simazine,\r\npendimethalin, and diuron) exhibited higher concentrations\r\nduring the pre-harvest period (March?\r\nMay) than during the post-harvest period (August?\r\nOctober).\r\nDuring 1996?98, an average of 0.37 pound\r\nper acre per year of atrazine was applied to the\r\nlower study area. During the same period, 0.0027\r\npound per acre per year of atrazine and its breakdown\r\nproduct deethylatrazine exited the lower\r\nstudy area in runoff (about 0.7 percent of the total\r\natrazine applied to the cropland). During 1997,\r\nwhen heavy rainfall occurred during the months of\r\nApril and May, the atrazine plus deethylatrazine\r\nexiting the lower study area was 1.8 percent of the\r\napplied atrazine.\r\nThe 1996?98 average sediment yield was\r\n610 pounds per acre per year. Sediment loads from\r\nthe study area are associated with large storm\r\nevents. Of the 45,300 tons of sediment transported\r\nfrom the study area during 1996?98 about 87 percent\r\nwas transported during the three largest runoff events (April 1997, October 1997, and October\r\n1998).\r\nRunoff-weighted average concentrations\r\nwere computed for selected nutrients and pesticides.\r\nThe 1996?98 runoff-weighted concentrations\r\nfor total nitrogen and total phosphorus were\r\n1.3 and 0.50 milligrams per liter, respectively. The\r\n1996?98 runoff-weighted concentration for atrazine\r\nplus deethylatrazine was 2.7 micrograms per\r\nliter.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri014101","usgsCitation":"Ockerman, D.J., and Petri, B.L., 2001, Hydrologic conditions and water quality in an agricultural area in Kleberg and Nueces Counties, Texas, 1996-98: U.S. Geological Survey Water-Resources Investigations Report 2001-4101, iv, 36 p., https://doi.org/10.3133/wri014101.","productDescription":"iv, 36 p.","numberOfPages":"54","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":168175,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":328443,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/wri01-4101/pdf/01-4101.pdf"},{"id":3877,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri014101/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d5e4b07f02db5ddafb","contributors":{"authors":[{"text":"Ockerman, Darwin J. 0000-0003-1958-1688 ockerman@usgs.gov","orcid":"https://orcid.org/0000-0003-1958-1688","contributorId":1579,"corporation":false,"usgs":true,"family":"Ockerman","given":"Darwin","email":"ockerman@usgs.gov","middleInitial":"J.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230907,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Petri, Brian L.","contributorId":64712,"corporation":false,"usgs":true,"family":"Petri","given":"Brian","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":230908,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":45048,"text":"wri014073 - 2001 - An alternative regionalization scheme for defining nutrient criteria for rivers and streams","interactions":[],"lastModifiedDate":"2018-02-06T12:32:25","indexId":"wri014073","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4073","title":"An alternative regionalization scheme for defining nutrient criteria for rivers and streams","docAbstract":"<p>To protect and manage rivers and streams (hereafter, collectively referred to as streams) in the United States, the U.S. Environmental Protection Agency (USEPA) is establishing regionally based nutrient criteria that reflect the natural variability in water quality. As a basic approach to establish these criteria, the USEPA has divided the country into nutrient ecoregions (delineated on the basis of natural and anthropogenic factors) to minimize variability within regions and maximize variability among regions. The USEPA has allowed states and tribes flexibility to modify or improve on this basic approach. As part of activities of a Regional Technical Assistance Group, whose role it is to examine and refine this basic approach, an alternative regionalization scheme was developed for the Upper Midwest. In this refined approach, the relative importance of various environmental characteristics affecting nutrient concentrations are determined by use of regression-tree analysis. The area is then subdivided into relatively homogeneous areas called &ldquo;environmental nutrient zones&rdquo; on the basis of distributions of only the most statistically significant environmental characteristics.</p>\n<p>On the basis of data from 234 sites, the most statistically significant environmental characteristics affecting nutrient concentrations were the percentage of agriculture (or absence of forest) and factors describing the climate and geology in the watershed. Environmental nutrient zones were then delineated that incorporated distributions in land use (similar to the ecoregion approach) and also delineated with land-use information excluded so the criteria should reflect only the naturally occurring variability in water quality. With the environmental nutrient zone stratification scheme, the variability in total phosphorus concentrations among zones was reduced by approximately 50 percent compared to that among nutrient ecoregions, whereas the variability in total nitrogen concentrations was reduced only slightly. Frequency distributions of data from each zone were then used to define the potential water quality of each zone.</p>\n<p>The environmental nutrient zone approach can be applied to specific states or nutrient ecoregions and used to develop criteria as a function of stream type. This approach can also be applied on the basis of environmental characteristics of the watershed alone rather than the general environmental characteristics from the region in which the site is located. The environmental nutrient zone approach will enable states to refine the basic nutrient criteria established by the USEPA by developing attainable criteria given the environmental characteristics where the streams are located.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri014073","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency, Regions V and VII","usgsCitation":"Robertson, D.M., Saad, D.A., and Wieben, A.M., 2001, An alternative regionalization scheme for defining nutrient criteria for rivers and streams: U.S. Geological Survey Water-Resources Investigations Report 2001-4073, v, 57 p., https://doi.org/10.3133/wri014073.","productDescription":"v, 57 p.","numberOfPages":"63","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science 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,{"id":50427,"text":"ofr01315 - 2001 - Spectral induced polarization measurements at the main iron incline mine dump near Leadville, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:11:20","indexId":"ofr01315","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","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":"2001-315","title":"Spectral induced polarization measurements at the main iron incline mine dump near Leadville, Colorado","language":"ENGLISH","doi":"10.3133/ofr01315","usgsCitation":"Campbell, D.L., 2001, Spectral induced polarization measurements at the main iron incline mine dump near Leadville, Colorado (Version 1.0): U.S. Geological Survey Open-File Report 2001-315, 9 p., 4 figs., https://doi.org/10.3133/ofr01315.","productDescription":"9 p., 4 figs.","numberOfPages":"9","costCenters":[],"links":[{"id":179669,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4224,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/ofr-01-0315/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db634ea0","contributors":{"authors":[{"text":"Campbell, D. L.","contributorId":90726,"corporation":false,"usgs":true,"family":"Campbell","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":241440,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":69756,"text":"i2754 - 2001 - The International Geometric Reference Field, 2000","interactions":[],"lastModifiedDate":"2012-02-02T00:13:50","indexId":"i2754","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2754","title":"The International Geometric Reference Field, 2000","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/i2754","isbn":"0607978333","usgsCitation":"Rukstales, K.S., and Quinn, J.M., 2001, The International Geometric Reference Field, 2000 (Version 1.0): U.S. Geological Survey IMAP 2754, 1 over-sized sheet; 54 by 36 inches; sheet 2 of 5 linked below, https://doi.org/10.3133/i2754.","productDescription":"1 over-sized sheet; 54 by 36 inches; sheet 2 of 5 linked below","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":191031,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c1f6","contributors":{"authors":[{"text":"Rukstales, Kenneth S. 0000-0003-2818-078X rukstales@usgs.gov","orcid":"https://orcid.org/0000-0003-2818-078X","contributorId":775,"corporation":false,"usgs":true,"family":"Rukstales","given":"Kenneth","email":"rukstales@usgs.gov","middleInitial":"S.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":281206,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Quinn, John M.","contributorId":47469,"corporation":false,"usgs":true,"family":"Quinn","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":281207,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":55097,"text":"wdrWV001 - 2001 - Water resources data, West Virginia, water year 2000","interactions":[],"lastModifiedDate":"2023-03-06T20:13:41.252952","indexId":"wdrWV001","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","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":"WV-00-1","title":"Water resources data, West Virginia, water year 2000","docAbstract":"<p>The Water Resources Division of the U.S. Geological Survey, in cooperation with State and Federal agencies, obtains a large amount of data pertaining to the water resources of West Virginia each water year. These data, accumulated during many water years, constitute a valuable data base for developing an improved understanding of the water resources of the State. 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I.","contributorId":80336,"corporation":false,"usgs":true,"family":"O'Dell","given":"I.","affiliations":[],"preferred":false,"id":250756,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":45045,"text":"wri014062 - 2001 - Ammonia in ground water from the Mississippi River alluvium, Fort Madison, Iowa","interactions":[],"lastModifiedDate":"2019-04-29T11:17:35","indexId":"wri014062","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4062","displayTitle":"Ammonia in Ground Water from the Mississippi River Alluvium, Fort Madison, Iowa","title":"Ammonia in ground water from the Mississippi River alluvium, Fort Madison, Iowa","docAbstract":"<p>The U.S. Geological Survey, in cooperation with the City of Fort Madison, conducted a study of the potential sources and possible processes that might produce ammonia in ground water from the Mississippi River alluvium near Fort Madison, Iowa. High ammonia concentrations of 3.0 to 6.4 milligrams per liter were detected in water produced from municipal well Fort Madison #4 from 1992 through 1996. Total organic carbon concentrations of about 5 milligrams per liter were also reported during the same time period.</p>\n<p>Water-level measurements from two municipal wells and one well at Iowa State Penitentiary were used to determine that the general direction of ground-water flow during the two days of sampling was from northeast to southwest toward wells Fort Madison #4 and Fort Madison #5. Continuous pumping of other nearby wells probably influenced the direction of ground-water flow on these days. Because of a till confining unit separating the Mississippi River and the alluvial aquifer, it is uncertain to what extent induced recharge occurs to the alluvial aquifer from the river.</p>\n<p>Water samples were collected from three municipal wells, two industrial wells, one watersupply well at the Iowa State Penitentiary, one domestic well, two creeks, and the Mississippi River. Tritium analytical results indicate that the time of recharge was after 1953 for water from the municipal wells (where tritium samples were collected). The ammonia concentration, 5.1 milligrams per liter, was considerably higher in ground water collected from well Fort Madison #4 compared to samples collected from other wells. The dissolved organic carbon concentration was also highest in ground water collected from well Fort Madison #4 (5.5 milligrams per liter) although samples from other wells were also relatively high, 2.6 to 5.3 milligrams per liter. The most likely process producing the high ammonia concentration in ground water in the vicinity of well Fort Madison #4 is decomposition of organic matter (ammonification). Nitrogen isotope values, when compared to nitrogen isotope values found in ground water in the vicinity of some of the other wells, indicate the possibility that a higher percentage of the ammonia found in ground water in the vicinity of well Fort Madison #4 may be from human and(or) other animal wastes. Higher concentrations of dissolved phosphorus, orthophosphate, and a higher chloride-to-sodium mole ratio found in ground water sampled from well Fort Madison #4 could be indicative of a sewage or septic source. Potential sources include existing or abandoned septic systems, leaking sanitary sewer lines, commercial or residential waste-disposal sites, and agricultural runoff upgradient from well Fort Madison #4, or possibly, bed sediments of the Mississippi River.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri014062","collaboration":"Prepared in cooperation with the City of Fort Madison, Iowa","usgsCitation":"Linhart, S., 2001, Ammonia in ground water from the Mississippi River alluvium, Fort Madison, Iowa: U.S. Geological Survey Water-Resources Investigations Report 2001-4062, iv, 21 p., https://doi.org/10.3133/wri014062.","productDescription":"iv, 21 p.","numberOfPages":"25","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science 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           -91.29973411560059,\n              40.62887131028398\n            ],\n            [\n              -91.307373046875,\n              40.62841532435384\n            ],\n            [\n              -91.31458282470702,\n              40.62808961821176\n            ],\n            [\n              -91.31758689880371,\n              40.6275684850803\n            ],\n            [\n              -91.32084846496582,\n              40.62574448709567\n            ],\n            [\n              -91.32393836975098,\n              40.623659856971535\n            ],\n            [\n              -91.32883071899414,\n              40.62222663601859\n            ],\n            [\n              -91.33389472961426,\n              40.62124942228214\n            ],\n            [\n              -91.33569717407227,\n              40.621966047086744\n            ],\n            [\n              -91.33870124816895,\n              40.62457189065689\n            ],\n            [\n              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Survey<br>400 South Clinton Street, Suite 269<br>Iowa City, IA 52240</p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Approach and Methods</li><li>Ground-Water Flow</li><li>Water Chemistry</li><li>Possible Processes and Potential Sources Contributing Ammonia to Ground Water</li><li>Summary and Conclusions</li><li>Selected References</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db68684e","contributors":{"authors":[{"text":"Linhart, S. Mike","contributorId":61073,"corporation":false,"usgs":true,"family":"Linhart","given":"S. Mike","affiliations":[],"preferred":false,"id":230983,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44989,"text":"wri014228 - 2001 - Use of ground-water tracers to evaluate the hydraulic connection between Key Cave and the proposed industrial site near Florence, Alabama, 2000 and 2001","interactions":[],"lastModifiedDate":"2012-02-02T00:10:12","indexId":"wri014228","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4228","title":"Use of ground-water tracers to evaluate the hydraulic connection between Key Cave and the proposed industrial site near Florence, Alabama, 2000 and 2001","docAbstract":"In an effort to attract new industries and jobs, the city of Florence, Alabama has proposed development of an industrial park southwest of the city. Carbonate rock under-lines the area and sinkholes, springs, caves, and sinking streams are common. Key Cave, located about 5 miles southwest of the proposed park, is the only know habitat for the Alabama Cavefish (Speoplatyrhinus poulsoni). The Alabama Cavefish is a Federally designated Endangered Species, and Key Cave has been designated as Critical Habitat. The U.S. Geological Survey was requested by the city of Florence and the U.S. Fish and Wildlife Service to assist in determining if a hydraulic connection exists between the proposed industrial park and Key Cave.\r\n Dye tracing methods were used in the investigation to determine if a hydraulic connection exists. Dye tracing is a technique that involves labeling a discrete quantity of ground water with a fluorescent dye so that its flow in the subsurface can be tracked to a ground-water discharge point. Monitoring for dyes involved the use of passive dye detectors placed in springs, wells, caves and surface streams. During the passage of ground water containing fluorescent dye, the dye is absorbed and concentrated on the detectors. Spectrofluorometric analyses of the detectors determines the presence or absence of dye.\r\n Dye injected in well I-1 on January 10, 2001, was recovered from site 67, Cypress Creek at General John Coffee Highway (State Highway 20) on January 17, 2001. No dye was recovered from site 68, Cypress Creek at Waterloo Road (County Road 14), indicating an east-southeast flow path from well I-1 to Cypress Creek. No positive dye recovery was made from dye injected in well I-2 on January 10, 2001. Water samples collected from the well February 1 and 15, 2001, showed little movement into the ground-water system. Dye injected in well I-3 on January 10, 2001, was recovered at two sites in Key Cave and at other locations. This test indicates a hydraulic connection exists between Key Cave and the proposed industrial site.","language":"ENGLISH","doi":"10.3133/wri014228","usgsCitation":"Kidd, R.E., Taylor, C.J., and Stricklin, V.E., 2001, Use of ground-water tracers to evaluate the hydraulic connection between Key Cave and the proposed industrial site near Florence, Alabama, 2000 and 2001: U.S. Geological Survey Water-Resources Investigations Report 2001-4228, iv, 20 p. : ill., col. maps ; 28 cm., https://doi.org/10.3133/wri014228.","productDescription":"iv, 20 p. : ill., col. maps ; 28 cm.","costCenters":[],"links":[{"id":99359,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2001/4228/report.pdf","size":"3641","linkFileType":{"id":1,"text":"pdf"}},{"id":162710,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2001/4228/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685933","contributors":{"authors":[{"text":"Kidd, Robert E.","contributorId":21523,"corporation":false,"usgs":true,"family":"Kidd","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":230859,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, Charles J.","contributorId":93100,"corporation":false,"usgs":true,"family":"Taylor","given":"Charles","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":230861,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stricklin, Victor E.","contributorId":69193,"corporation":false,"usgs":true,"family":"Stricklin","given":"Victor","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":230860,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":44910,"text":"wri20014054 - 2001 - User's Guide for Mixed-Size Sediment Transport Model for Networks of One-Dimensional Open Channels","interactions":[],"lastModifiedDate":"2012-02-02T00:10:11","indexId":"wri20014054","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4054","title":"User's Guide for Mixed-Size Sediment Transport Model for Networks of One-Dimensional Open Channels","docAbstract":"This user's guide describes a mathematical model for predicting the transport of mixed sizes of sediment by flow in networks of one-dimensional open channels. The simulation package is useful for general sediment routing problems, prediction of erosion and deposition following dam removal, and scour in channels at road embankment crossings or other artificial structures. The model treats input hydrographs as stepwise steady-state, and the flow computation algorithm automatically switches between sub- and supercritical flow as dictated by channel geometry and discharge. A variety of boundary conditions including weirs and rating curves may be applied both external and internal to the flow network. The model may be used to compute flow around islands and through multiple openings in embankments, but the network must be 'simple' in the sense that the flow directions in all channels can be specified before simulation commences. The location and shape of channel banks are user specified, and all bedelevation changes take place between these banks and above a user-specified bedrock elevation. Computation of sediment-transport emphasizes the sand-size range (0.0625-2.0 millimeter) but the user may select any desired range of particle diameters including silt and finer (<0.0625 millimeter). As part of data input, the user may set the original bed-sediment composition of any number of layers of known thickness. The model computes the time evolution of total transport and the size composition of bed- and suspended-load sand through any cross section of interest. It also tracks bed -surface elevation and size composition. The model is written in the FORTRAN programming language for implementation on personal computers using the WINDOWS operating system and, along with certain graphical output display capability, is accessed from a graphical user interface (GUI). The GUI provides a framework for selecting input files and parameters of a number of components of the sediment-transport process. There are no restrictions in the use of the model as to numbers of channels, channel junctions, cross sections per channel, or points defining the cross sections. Following completion of the simulation computations, the GUI accommodates display of longitudinal plots of either bed elevation and size composition, or of transport rate and size composition of the various components, for individual channels and selected times during the simulation period. For individual cross sections, the GUI also allows display of time series of transport rate and size composition of the various components and of bed elevation and size composition.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/wri20014054","usgsCitation":"Bennett, J.P., 2001, User's Guide for Mixed-Size Sediment Transport Model for Networks of One-Dimensional Open Channels: U.S. Geological Survey Water-Resources Investigations Report 2001-4054, iv, 33 p., https://doi.org/10.3133/wri20014054.","productDescription":"iv, 33 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":162704,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2001/4054/report-thumb.jpg"},{"id":82248,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2001/4054/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db60423c","contributors":{"authors":[{"text":"Bennett, James P.","contributorId":100323,"corporation":false,"usgs":true,"family":"Bennett","given":"James","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":230664,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44912,"text":"wri014123 - 2001 - Relations Among River Stage, Rainfall, Ground-Water Levels, and Stage at Two Missouri River Flood-Plain Wetlands","interactions":[],"lastModifiedDate":"2012-02-02T00:10:11","indexId":"wri014123","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4123","title":"Relations Among River Stage, Rainfall, Ground-Water Levels, and Stage at Two Missouri River Flood-Plain Wetlands","docAbstract":"The source of water is important to the ecological function of Missouri River flood-plain wetlands. There are four potential sources of water to flood-plain wetlands: direct flow from the river channel during high river stage, ground-water movement into the wetlands in response to river-stage changes and aquifer recharge, direct precipitation, and runoff from surrounding uplands. Concurrent measurements of river stage, rainfall, ground-water level, and wetland stage were compared for two Missouri River flood-plain wetlands located near Rocheport, Missouri, to characterize the spatial and temporal relations between river stage, rainfall, ground-water levels and wetland stage, determine the source of water to each wetland, and compare measured and estimated stage and ground-water levels at each site. The two sites chosen for this study were wetland NC-5, a non-connected, 50 feet deep scour constantly filled with water, formed during the flood of 1993, and wetland TC-1, a shallow, temporary wetland intermittently filled with water. Because these two wetlands bracket a range of wetland types of the Missouri River flood plain, the responses of other Missouri River wetlands to changes in river stage, rainfall, and runoff should be similar to the responses exhibited by wetlands NC-5 and TC-1.\r\n\r\nFor wetlands deep enough to intersect the ground-water table in the alluvial aquifer, such as wetland NC-5, the ground-water response factor can estimate flood-plain wetland stage changes in response to known river-stage changes. Measured maximum stage and ground-water-level changes at NC-5 fall within the range of estimated changes using the ground-water response factor. Measured maximum ground-water-level changes at TC-1 are similar to, but consistently greater than the estimated values, and are most likely the result of alluvial deposits with higher than average hydraulic conductivity located between wetland TC-1 and the Missouri River.\r\n\r\nSimilarity between ground-water level and stage hydrography at wetland NC-5 indicate that ground-water-level fluctuations caused by river-stage changes control the stage of wetland NC-5. A 2-day lag time exists between river-stage changes and ground water and stage changes at wetland NC-5. The lack of a measurable response of wetland NC-5 stage to rainfall indicate that rainfall is not a large source of water to wetland NC-5. Stage in wetland TC-1 only increased at high river stage in June and July 1999, and from runoff caused by local rainfall during the winter. The 2-day lag time between peak stages at wetland TC-1 and peak Missouri River stages compared to the 1-day lag time between Missouri River stage and ground-water peaks at wetland TC-1 indicates ground-water flow does not directly affect wetland stage at TC-1, but surface-water flow does affect wetland stage at TC-1 during high river stage. Comparing wetland TC-1 stage to potential water sources indicates the most likely explanation for the rise in stage at wetland TC-1 is surface runoff supplied via seepage through the levees and upward flow of ground water through alluvial deposits of higher hydraulic conductivity during high river stage. The rate of decrease in wetland TC-1 stage was limited by the rate at which ground-water level decreased. Stage response to rainfall at wetland TC-1 during the winter months and no response to greater rainfall amounts during spring and summer months indicate that evapotranspiration may limit the affect of rainfall on stage at wetland TC-1 during the growing season.","language":"ENGLISH","doi":"10.3133/wri014123","usgsCitation":"Kelly, B.P., 2001, Relations Among River Stage, Rainfall, Ground-Water Levels, and Stage at Two Missouri River Flood-Plain Wetlands: U.S. Geological Survey Water-Resources Investigations Report 2001-4123, iii, 18 p. : ill. (some col.), col. map ; 28 cm., https://doi.org/10.3133/wri014123.","productDescription":"iii, 18 p. : ill. (some col.), col. map ; 28 cm.","costCenters":[],"links":[{"id":162705,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3793,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://mo.water.usgs.gov/Reports/01-4123-kelly/index.htm","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cec8","contributors":{"authors":[{"text":"Kelly, Brian P. 0000-0001-6378-2837 bkelly@usgs.gov","orcid":"https://orcid.org/0000-0001-6378-2837","contributorId":897,"corporation":false,"usgs":true,"family":"Kelly","given":"Brian","email":"bkelly@usgs.gov","middleInitial":"P.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true},{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230667,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50400,"text":"ofr01180 - 2001 - Science Plan, U.S. Geological Survey Florida District","interactions":[],"lastModifiedDate":"2025-04-23T15:57:12.156537","indexId":"ofr01180","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","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":"2001-180","title":"Science Plan, U.S. Geological Survey Florida District","docAbstract":"<p>This Science Plan has been prepared by the Florida District of the U.S. Geological Survey (USGS) as a tool to provide direction for the scientific work to be accomplished in the District during the next 5-10 years. A Science Plan can serve as a guide to determine the optimum use of the limited financial resources of the USGS in Florida to address water resource issues. The Florida District has four primary operational centers geographically distributed across the State, in Tallahassee, Orlando, Tampa, and Miami, with a laboratory in Ocala and field offices in Jacksonville and Fort Myers. Other USGS discipline offices in Florida are located in Gainesville (biology), St. Petersburg (geology), and Miami (restoration ecology) (fig.1). Although some differences exist in programs among the four water-resource offices because of differing physiographic settings and information needs, many common elements are present and these common elements are the focus of this District Science Plan. Science Plan development was based on other planning documents including individual Science Plans prepared by personnel in each of the four primary Florida water resource offices, and strategic planning documents of the Southeastern Region, Water Resources Discipline (WRD), and the USGS.</p><p>A broad cross-section of District staff, representing all primary offices, a number of different scientific disciplines, and different programs of the District (data collection, investigations, and research) collaborated on the development of this Science Plan. As part of the development process, input was solicited from staff in every office and considered for inclusion in the plan. The Science Plan will be evaluated on an ongoing basis to ensure its continued relevancy to recognized water resources needs in Florida, and to guide future program development and collaboration with our existing and potential partners and customers, both within and outside the USGS.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr01180","usgsCitation":"Science Plan, U.S. Geological Survey Florida District; 2001; OFR; 2001-180; Hammett, Kathleen M.; Katz, Brian G.; McPherson, Benjamin F.; Patino, Eduardo; Schiffer, Donna M.; Wedderburn, Leslie; Yobbi, Dann K.","productDescription":"v, 28 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":4195,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0180/ofr01-180.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Open-File Report 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 \"}}]}","edition":"Version 1.0","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","publishedDate":"2001-10-01","noUsgsAuthors":false,"publicationDate":"2001-10-01","publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd39e","contributors":{"authors":[{"text":"Hammett, Kathleen M.","contributorId":34995,"corporation":false,"usgs":true,"family":"Hammett","given":"Kathleen","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":241371,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Katz, Brian G. bkatz@usgs.gov","contributorId":1093,"corporation":false,"usgs":true,"family":"Katz","given":"Brian","email":"bkatz@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":241366,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McPherson, Benjamin F.","contributorId":17965,"corporation":false,"usgs":true,"family":"McPherson","given":"Benjamin","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":241370,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Patino, Eduardo 0000-0003-1016-3658 epatino@usgs.gov","orcid":"https://orcid.org/0000-0003-1016-3658","contributorId":1743,"corporation":false,"usgs":true,"family":"Patino","given":"Eduardo","email":"epatino@usgs.gov","affiliations":[{"id":270,"text":"FLWSC-Tampa","active":true,"usgs":true},{"id":269,"text":"FLWSC-Ft. Lauderdale","active":true,"usgs":true}],"preferred":true,"id":241367,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schiffer, Donna M. schiffer@usgs.gov","contributorId":2138,"corporation":false,"usgs":true,"family":"Schiffer","given":"Donna","email":"schiffer@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":241368,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Wedderburn, Leslie","contributorId":83195,"corporation":false,"usgs":true,"family":"Wedderburn","given":"Leslie","email":"","affiliations":[],"preferred":false,"id":241372,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Yobbi, Dann K.","contributorId":15247,"corporation":false,"usgs":true,"family":"Yobbi","given":"Dann","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":241369,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":38188,"text":"fs08001 - 2001 - Number and size of black bass reflect water quality in the lower Mississippi River Delta","interactions":[],"lastModifiedDate":"2012-02-02T00:09:53","indexId":"fs08001","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"080-01","title":"Number and size of black bass reflect water quality in the lower Mississippi River Delta","language":"ENGLISH","doi":"10.3133/fs08001","usgsCitation":"Justus, B., Caskey, B.J., and Kleiss, B., 2001, Number and size of black bass reflect water quality in the lower Mississippi River Delta: U.S. Geological Survey Fact Sheet 080-01, 4 p., https://doi.org/10.3133/fs08001.","productDescription":"4 p.","costCenters":[],"links":[{"id":3483,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://ms.water.usgs.gov/publications/FS%5F080%5F01.html","linkFileType":{"id":5,"text":"html"}},{"id":122164,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2001/0080/report-thumb.jpg"},{"id":64479,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2001/0080/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69686a","contributors":{"authors":[{"text":"Justus, B. G. 0000-0002-3458-9656 bjustus@usgs.gov","orcid":"https://orcid.org/0000-0002-3458-9656","contributorId":2052,"corporation":false,"usgs":true,"family":"Justus","given":"B. G.","email":"bjustus@usgs.gov","affiliations":[{"id":129,"text":"Arkansas Water Science Center","active":true,"usgs":true}],"preferred":false,"id":219292,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Caskey, Brian J.","contributorId":104119,"corporation":false,"usgs":true,"family":"Caskey","given":"Brian","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":219294,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kleiss, Barbara A.","contributorId":87536,"corporation":false,"usgs":true,"family":"Kleiss","given":"Barbara A.","affiliations":[],"preferred":false,"id":219293,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":50428,"text":"ofr01317 - 2001 - Sedimentation profiles in Lake Tuscaloosa, Alabama, 2000","interactions":[],"lastModifiedDate":"2012-02-02T00:11:19","indexId":"ofr01317","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","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":"2001-317","title":"Sedimentation profiles in Lake Tuscaloosa, Alabama, 2000","docAbstract":"Lake Tuscaloosa, created in 1969 by the impoundment of North River, is the primary water supply for the cities of Tuscaloosa and Northport, Alabama, and surrounding areas. In 1982, 17 cross-sections were established in the principal tributaries of the lake, which include North River, Dry Creek, Turkey Creek, Binion Creek, Tierce Creek, Carroll Creek, and Brush Creek. These cross-sections were resurveyed in 1986 to determine the amount of sedimentation or scour occurring in the lake at these areas. In May 2000, 14 of the 17 cross-sections were located for resurveying to determine the amount of sedimentation or scour since 1986.\r\nThe maximum amount of sediment deposition determined from the 2000 survey occurred in the upper end of the Carroll Creek tributary at cross-section CC8 (3.0 feet). The maximum amount of scour occurred in the Turkey Creek tributary at cross-section TRC2 (7.0 feet). Of the 14 cross-sections, 6 indicated increased amounts of sediment deposition, 5 indicated scouring of bottom sediments, and 3 indicated little or no change.","language":"ENGLISH","doi":"10.3133/ofr01317","usgsCitation":"Stricklin, V.E., 2001, Sedimentation profiles in Lake Tuscaloosa, Alabama, 2000: U.S. Geological Survey Open-File Report 2001-317, iii, 19 p. : ill., maps ; 28 cm., https://doi.org/10.3133/ofr01317.","productDescription":"iii, 19 p. : ill., maps ; 28 cm.","costCenters":[],"links":[{"id":175515,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2001/0317/report-thumb.jpg"},{"id":86322,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0317/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fbc4d","contributors":{"authors":[{"text":"Stricklin, Victor E.","contributorId":69193,"corporation":false,"usgs":true,"family":"Stricklin","given":"Victor","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":241441,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}