{"pageNumber":"1139","pageRowStart":"28450","pageSize":"25","recordCount":46734,"records":[{"id":54250,"text":"wdrNHVT001 - 2001 - Water resources data for New Hampshire and Vermont, water year 2000","interactions":[],"lastModifiedDate":"2012-03-08T17:16:17","indexId":"wdrNHVT001","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":"NH-VT-00-1","title":"Water resources data for New Hampshire and Vermont, water year 2000","docAbstract":"Water-resources data for the 2000 water year for New Hampshire and Vermont consists of stage, discharge, and water quality\r\nof streams; contents of lakes and reservoirs; and ground-water levels. This report contains discharge records for 76 gaging\r\nstations, stage records for 5 lakes, monthend contents for 2 lakes and reservoirs, water levels for 28 observation wells. Also\r\nincluded are data for 43 crest-stage partial-record stations. Additional water data were collected at various sites, which are not\r\npart of the systematic data-collection program and are published as miscellaneous measurements or under Supplemental\r\nNational Water-Quality Assessment Data for Gaging Stations in New Hampshire and Vermont. A few pertinent stations in\r\nbordering states are also included in this report. These data represent that portion of the National Water Data System operated\r\nby the U.S. Geological Survey and cooperating State and Federal agencies in New Hampshire and Vermont.","language":"ENGLISH","doi":"10.3133/wdrNHVT001","usgsCitation":"Coakley, M., Keirstead, C., Brown, R.O., and Kiah, R.G., 2001, Water resources data for New Hampshire and Vermont, water year 2000: U.S. Geological Survey Water Data Report NH-VT-00-1, 208 p., https://doi.org/10.3133/wdrNHVT001.","productDescription":"208 p.","temporalStart":"1999-10-01","temporalEnd":"2000-09-30","costCenters":[{"id":468,"text":"New Hampshire-Vermont Water Science Center","active":false,"usgs":true}],"links":[{"id":5356,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdrnh001/","linkFileType":{"id":5,"text":"html"}},{"id":174403,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2a3c","contributors":{"authors":[{"text":"Coakley, M.F.","contributorId":25228,"corporation":false,"usgs":true,"family":"Coakley","given":"M.F.","email":"","affiliations":[],"preferred":false,"id":249663,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Keirstead, Chandlee","contributorId":10862,"corporation":false,"usgs":true,"family":"Keirstead","given":"Chandlee","email":"","affiliations":[],"preferred":false,"id":249662,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, Robert O. robrown@usgs.gov","contributorId":3942,"corporation":false,"usgs":true,"family":"Brown","given":"Robert","email":"robrown@usgs.gov","middleInitial":"O.","affiliations":[],"preferred":true,"id":249661,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"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":249660,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":50443,"text":"ofr2001368 - 2001 - The Evolution of the Lower Missouri River: Preliminary Results of NMD Research at Lisbon Bottom","interactions":[],"lastModifiedDate":"2017-09-06T14:23:15","indexId":"ofr2001368","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":"2001-368","title":"The Evolution of the Lower Missouri River: Preliminary Results of NMD Research at Lisbon Bottom","docAbstract":"The purpose of this investigation is to determine the relationship between the geomorphology of Lisbon Bottom and the spatial and temporal distribution of its wetlands. The project is focused specifically on the Quaternary geology of the river valley and the relationship between the valley's alluvial architecture and the hydrogeology of its wetlands. The Quaternary geology of the river valley has been determined through a field reconnaissance and visual inspection of topographic maps and digital elevation data. Data describing the morphology of the main channel and the physical properties of Lisbon Bottom have been collected. On the basis of these data, a preliminary model of the alluvial architecture of Lisbon Bottom has been developed, but it lacks subsurface verification owing to equipment failures and unseasonable high water. To date, the publications and presentations describing the project include a U.S. Geological Survey Open-File Report (OFR 01-176), two seminars hosted by the University of Missouri - Rolla, and an abstract that was submitted and accepted by the Geological Society of America for its annual fall meeting in November 2001.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr2001368","usgsCitation":"Spooner, J., 2001, The Evolution of the Lower Missouri River: Preliminary Results of NMD Research at Lisbon Bottom: U.S. Geological Survey Open-File Report 2001-368, 13 p., https://doi.org/10.3133/ofr2001368.","productDescription":"13 p.","numberOfPages":"13","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":175849,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2001/0368/coverthb.jpg"},{"id":345475,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0368/ofr01368.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Lisbon Bottom, Missouri River","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67aff4","contributors":{"authors":[{"text":"Spooner, Jeffrey","contributorId":49010,"corporation":false,"usgs":true,"family":"Spooner","given":"Jeffrey","affiliations":[],"preferred":false,"id":241468,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50459,"text":"ofr01486 - 2001 - Vertical series hydraulic conductance classes to characterize the unsaturated zone in North Carolina","interactions":[],"lastModifiedDate":"2024-03-05T14:00:33.483712","indexId":"ofr01486","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":"01-486","displayTitle":"Vertical Series Hydraulic Conductance Classes to Characterize the Unsaturated Zone in North Carolina","title":"Vertical series hydraulic conductance classes to characterize the unsaturated zone 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. 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/ofr01486","usgsCitation":"Eimers, J., Terziotti, S., and Ferrell, G.M., 2001, Vertical series hydraulic conductance classes to characterize the unsaturated zone in North Carolina (Version 1.0): U.S. Geological Survey Open-File Report 01-486, HTML Document; Metadata, https://doi.org/10.3133/ofr01486.","productDescription":"HTML Document; Metadata","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":4269,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/0486/index.html","linkFileType":{"id":5,"text":"html"}},{"id":176537,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United 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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":"4f4e49f4e4b07f02db5f0649","contributors":{"authors":[{"text":"Eimers, Jo Leslie","contributorId":52946,"corporation":false,"usgs":true,"family":"Eimers","given":"Jo Leslie","affiliations":[],"preferred":false,"id":241506,"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":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true},{"id":476,"text":"North Carolina Water Science Center","active":true,"usgs":true}],"preferred":true,"id":241505,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ferrell, Gloria M. gferrell@usgs.gov","contributorId":1595,"corporation":false,"usgs":true,"family":"Ferrell","given":"Gloria","email":"gferrell@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":241504,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30253,"text":"wri014011 - 2001 - U.S. Geological Survey Karst Interest Group: proceedings, St Petersburg, Florida February 13-16, 2001","interactions":[],"lastModifiedDate":"2024-09-24T15:44:23.12715","indexId":"wri014011","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":"2001-4011","title":"U.S. Geological Survey Karst Interest Group: proceedings, St Petersburg, Florida February 13-16, 2001","docAbstract":"Karst and similar landscapes are found in a wide range of biogeographic classes. In the U.S. for example, Everglades, Mammoth Cave, and Hawaii Volcanoes National Parks have little in common - except karst or pseudokarst, and a cultural past (even though these are very different). This diversity of geologic settings makes karst difficult to categorize and work with when designing a national program such as the recent NPS-USGS Geo-Indicators effort. A GIS-based approach with multiple datalayers is the only sane way to understand and convey the many relationships, in X, Y, and Z axes, between component ecosystems and cultural resources within karst and pseudokarst landscapes. Obviously, karst and cultural landscapes cross modern political as well as biogeographic boundaries. Here again, three-dimensional data are the foundation for understanding similar to that in anatomy and physiology: structure and function. In understanding where the most vulnerable 'pressure points' exist within karst landscapes, we can target landscape-scale ecosystem management to greatest effect. USGS and the National Cave and Karst research Institute could play an extremely significant role in cave and karst management on a national scale beyond NPS or other agency boundaries via cooperative management of three-dimensional karst datasets analogous to programs in several states.","language":"English","publisher":"U.S Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri014011","usgsCitation":"Kuniansky, E.L., 2001, U.S. Geological Survey Karst Interest Group: proceedings, St Petersburg, Florida February 13-16, 2001: U.S. Geological Survey Water-Resources Investigations Report 2001-4011, vi, 211 p., https://doi.org/10.3133/wri014011.","productDescription":"vi, 211 p.","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":160500,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2001/4011/report-thumb.jpg"},{"id":2435,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://water.usgs.gov/ogw/karst/kigconference/proceedings.htm","linkFileType":{"id":5,"text":"html"}},{"id":462205,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2001/4011/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","city":"St. Petersburg","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -82.74767742331497,\n              27.865264784108888\n            ],\n            [\n              -82.74767742331497,\n              27.6622445097143\n            ],\n            [\n              -82.58474782738695,\n              27.6622445097143\n            ],\n            [\n              -82.58474782738695,\n              27.865264784108888\n            ],\n            [\n              -82.74767742331497,\n              27.865264784108888\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2be4b07f02db613143","contributors":{"authors":[{"text":"Kuniansky, Eve L. 0000-0002-5581-0225 elkunian@usgs.gov","orcid":"https://orcid.org/0000-0002-5581-0225","contributorId":932,"corporation":false,"usgs":true,"family":"Kuniansky","given":"Eve","email":"elkunian@usgs.gov","middleInitial":"L.","affiliations":[{"id":509,"text":"Office of the Associate Director for Water","active":true,"usgs":true},{"id":5064,"text":"Southeast Regional Director's Office","active":true,"usgs":true}],"preferred":true,"id":202938,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30764,"text":"fs10101 - 2001 - The National Map: Topographic Maps for the 21st Century","interactions":[],"lastModifiedDate":"2012-03-16T17:16:06","indexId":"fs10101","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":"101-01","title":"The National Map: Topographic Maps for the 21st Century","docAbstract":"The U.S. Geological Survey (USGS) is committed to meeting the Nation's needs for current base geographic data and maps. Our vision is that, by working with partners, we will provide the Nation with access to current, accurate, and nationally consistent digital data and topographic maps derived from those data. This synthesis of information, products, and capabilities, The National Map, will be a seamless, continuously maintained set of geographic base information that will serve as a foundation for integrating, sharing, and using other data easily and consistently.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","publisherLocation":"Reston, VA","doi":"10.3133/fs10101","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2001, The National Map: Topographic Maps for the 21st Century (Superseded by 018-02): U.S. Geological Survey Fact Sheet 101-01, 2 p., https://doi.org/10.3133/fs10101.","productDescription":"2 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":161354,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2001/0101/report-thumb.jpg"},{"id":59486,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2001/0101/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Superseded by 018-02","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b013","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":529247,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30772,"text":"fs12101 - 2001 - The National Map - Florida Pilot Project","interactions":[],"lastModifiedDate":"2012-04-15T17:28:14","indexId":"fs12101","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":"121-01","title":"The National Map - Florida Pilot Project","docAbstract":"Governments depend on a common set of geographic base information as a tool for economic and community development, land and natural resource management, and health and safety services. Emergency management and defense operations rely on this information. Private industry, nongovernmental organizations, and individual citizens use the same geographic data. Geographic information underpins an increasingly large part of the Nation's economy.\r\n\r\nAvailable geographic data often have the following problems:\r\n* They do not align with each other because layers are frequently created or revised separately,\r\n* They do not match across administrative boundaries because each producing organization uses different methods and standards, and\r\n* They are not up to date because of the complexity and cost of revision.\r\n\r\n\r\nThe U.S. Geological Survey (USGS) is developing The National Map to be a seamless, continuously maintained, and nationally consistent set of online, public domain, geographic base information to address these issues. The National Map will serve as a foundation for integrating, sharing, and using other data easily and consistently.\r\n\r\n\r\nIn collaboration with other government agencies, the private sector, academia, and volunteer groups, the USGS will coordinate, integrate, and, where needed, produce and maintain base geographic data.\r\n\r\n\r\nThe National Map will include digital orthorectified imagery; elevation data; vector data for hydrography, transportation, boundary, and structure features; geographic names; and land cover information. The data will be the source of revised paper topographic maps.\r\n\r\n\r\nMany technical and institutional issues must be resolved as The National Map is implemented. To begin the refinement of this new paradigm, pilot projects are being designed to identify and investigate these issues. The pilots are the foundation upon which future partnerships for data sharing and maintenance will be built.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","publisherLocation":"Reston, VA","doi":"10.3133/fs12101","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2001, The National Map - Florida Pilot Project: U.S. Geological Survey Fact Sheet 121-01, 2 p., https://doi.org/10.3133/fs12101.","productDescription":"2 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":160537,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2001/0121/report-thumb.jpg"},{"id":59494,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2001/0121/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb233","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":529255,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44590,"text":"wri014114 - 2001 - Simulations of flooding on the Tennessee River in the vicinity of U.S. Highway 231 near Huntsville, Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:10:30","indexId":"wri014114","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":"2001-4114","title":"Simulations of flooding on the Tennessee River in the vicinity of U.S. Highway 231 near Huntsville, Alabama","docAbstract":"A two-dimensional finite-element surface-water model was used to study the effects of proposed modifications to the U.S. Highway 231 corridor on water-surface elevations and flow distributions during flooding in the Tennessee River Basin south of Huntsville, Madison County, Alabama. Flooding was first simulated for the March 19, 1973, flood for the existing conditions in order to calibrate the model to measured data collected by the U.S. Geological Survey (USGS) and the Tennessee Valley Authority (TVA) during and after the flood. After model calibration, the effects of flooding were simulated for two scenarios---existing and proposed conditions----for the 100-year and 500-year recurrence intervals. The first scenario was to simulate the existing bridge and highway configuration for the U.S. Highway 231 crossing of the Tennessee River flood plain. The second scenario was to simulate the proposed modifications to this bridge and highway configuration.\r\nThe simulation of floodflow for the Tennessee River flood of March 19, 1973, in the study reach compared closely to discharge measurement and flood profile data obtained during and after the flood. The flood of March 19, 1973, had an estimated peak discharge of 323,000 cubic feet per second and was estimated to be about 50-year flood event.\r\nSimulation of the 100-year floodflow for the Tennessee River for the existing conditions at U.S. Highway 231 indicates that of the peak flow, 92.1 percent (316,500 cubic feet per second) was conveyed by the main channel bridge, 4.0 percent (13,800 cubic feet per second) by the northernmost relief bridge, and 3.8 percent (13,200 cubic feet per second) by the southernmost relief bridge. The water-surface elevation predicted in the vicinity of the USGS gaging station was 576.91 feet. No overtopping of U.S. Highway 231 occurrec. For the 500-year flood, the simulation indicates that of the peak flow, 89.2 percent (359,000) cubic feet per second) was conveyed by the main channel bridge, 5.6 percent (22,600 cubic feet per second) by the northernmost relieft bridge, and 5.2 percent (20,900 cubic feet per second) by the southernmost relief bridge. The water-surface elevation predicted in the vicinity of the USGS gaging station was 580.91 feet. No overtopping of U.S. Highway 231 occurred; however, the girders of both relief bridges were partially submerged.\r\nSimulation of the 100-year floodflow for the Tennessee River for the proposed conditions indicates that of the peak flow, 93.2 percent (319,800 cubic feet per second) was conveyed by the proposed main channel bridge, 3.3 percent (11,400 cubic feet per second) by the proposed northernmost relief bridge, and 3.4 percent (11,800 cubic feet per second) by the proposed southernmost relief bridge. The water-surface elevation predicted in the vicinity of the USGS gaging station was 576.93 feet. No overtopping of U.S. Highway 231 occurred. For the 500-year flood, the simulation indicates that of the peak flow, 90.9 percent (365,400 cubic feet per second) was conveyed by the proposed main channel bridge, 4.3 percnet (17,300 cubic feet per second) by the proposed northernmost relief bridge, and 4.8 percent (19,400 cubic feet per second) by the proposed southernmost relief bridge. The water-surface elevation predicted in the vidinity of the USGS gaging station was 580.93 feet. No overtopping of U.S. Highway 231 occurred; however, the girders of both relief bridges were partially submerged.","language":"ENGLISH","doi":"10.3133/wri014114","usgsCitation":"Hedgecock, T.S., 2001, Simulations of flooding on the Tennessee River in the vicinity of U.S. Highway 231 near Huntsville, Alabama: U.S. Geological Survey Water-Resources Investigations Report 2001-4114, iv, 30 p. : col. maps ; 28 cm., https://doi.org/10.3133/wri014114.","productDescription":"iv, 30 p. : col. maps ; 28 cm.","costCenters":[],"links":[{"id":99304,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2001/4114/report.pdf","size":"9708","linkFileType":{"id":1,"text":"pdf"}},{"id":172443,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2001/4114/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602b7d","contributors":{"authors":[{"text":"Hedgecock, T. Scott","contributorId":20783,"corporation":false,"usgs":true,"family":"Hedgecock","given":"T.","email":"","middleInitial":"Scott","affiliations":[],"preferred":false,"id":230051,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44641,"text":"wri014077 - 2001 - Pesticide toxicity index for freshwater aquatic organisms","interactions":[],"lastModifiedDate":"2012-02-02T00:11:01","indexId":"wri014077","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":"2001-4077","title":"Pesticide toxicity index for freshwater aquatic organisms","docAbstract":"The U.S. Geological Survey's National Water-Quality Assessment (NAWQA) Program is designed to assess current water-quality conditions, changes in water quality over time, and the effects of natural and human factors on water quality for the Nation's streams and ground-water resources. For streams, one of the most difficult parts of the assessment is to link chemical conditions to effects on aquatic biota, particularly for pesticides, which tend to occur in streams as complex mixtures with strong seasonal patterns. A Pesticide Toxicity Index (PTI) was developed that combines pesticide exposure of aquatic biota (measured concentrations of pesticides in stream water) with toxicity estimates (standard endpoints from laboratory bioassays) to produce a single index value for a sample or site. The development of the PTI was limited to pesticide compounds routinely measured in NAWQA studies and to toxicity data readily available from existing databases. Qualifying toxicity data were found for one or more types of test organisms for 75 of the 83 pesticide compounds measured in NAWQA samples, but with a wide range of bioassays per compound (1 to 65). There were a total of 2,824 bioassays for the 75 compounds, including 287 48-hour EC50 values (concentration at which 50 percent of test organisms exhibit a nonlethal response) for freshwater cladocerans, 585 96-hour LC50 values (concentration lethal to 50 percent of test organisms) for freshwater benthic invertebrates, and 1,952 96-hour LC50 values for freshwater fish. The PTI for a particular sample is the sum of toxicity quotients (measured concentration divided by the median toxicity concentration from bioassays) for each detected pesticide. The PTI can be calculated for specific groups of pesticides and for specific taxonomic groups.While the PTI does not determine whether water in a sample is toxic, its values can be used to rank or compare the toxicity of samples or sites on a relative basis for use in further analysis or additional assessments. The PTI approach may be useful as a basis for comparing the potential significance of pesticides in different streams on a common basis, for evaluating relations between pesticide exposure and observed biological conditions, and for prioritizing where further studies are most needed.","language":"ENGLISH","doi":"10.3133/wri014077","usgsCitation":"Munn, M.D., and Gilliom, R.J., 2001, Pesticide toxicity index for freshwater aquatic organisms: U.S. Geological Survey Water-Resources Investigations Report 2001-4077, 61 p.; 3 illus.; 7 tables, https://doi.org/10.3133/wri014077.","productDescription":"61 p.; 3 illus.; 7 tables","costCenters":[],"links":[{"id":3731,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri014077","linkFileType":{"id":5,"text":"html"}},{"id":168743,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688359","contributors":{"authors":[{"text":"Munn, Mark D. 0000-0002-7154-7252 mdmunn@usgs.gov","orcid":"https://orcid.org/0000-0002-7154-7252","contributorId":976,"corporation":false,"usgs":true,"family":"Munn","given":"Mark","email":"mdmunn@usgs.gov","middleInitial":"D.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230176,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gilliom, Robert J. rgilliom@usgs.gov","contributorId":488,"corporation":false,"usgs":true,"family":"Gilliom","given":"Robert","email":"rgilliom@usgs.gov","middleInitial":"J.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":true,"id":230175,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44589,"text":"wri014172 - 2001 - Model simulation of the Manasquan water-supply system in Monmouth County, New Jersey","interactions":[],"lastModifiedDate":"2012-02-10T00:11:58","indexId":"wri014172","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":"2001-4172","title":"Model simulation of the Manasquan water-supply system in Monmouth County, New Jersey","docAbstract":"Model simulation of the Manasquan Water Supply System in Monmouth County, New Jersey, was completed using historic hydrologic data to evaluate the effects of operational and withdrawal alternatives on the Manasquan reservoir and pumping system. Changes in the system operations can be simulated with the model using precipitation forecasts.\r\n\r\nThe Manasquan Reservoir system model operates by using daily streamflow values, which were reconstructed from historical U.S. Geological Survey streamflow-gaging station records. The model is able to run in two modes--General Risk analysis Model (GRAM) and Position Analysis Model (POSA). The GRAM simulation procedure uses reconstructed historical streamflow records to provide probability estimates of certain events, such as reservoir storage levels declining below a specific level, when given an assumed set of operating rules and withdrawal rates. POSA can be used to forecast the likelihood of specified outcomes, such as streamflows falling below statutory passing flows, associated with a specific working plan for the water-supply system over a period of months. \r\n\r\nThe user can manipulate the model and generate graphs and tables of streamflows and storage, for example. This model can be used as a management tool to facilitate the development of drought warning and drought emergency rule curves and safe yield values for the water-supply system.\r\n","language":"ENGLISH","doi":"10.3133/wri014172","usgsCitation":"Chang, M., Tasker, G.D., and Nieswand, S., 2001, Model simulation of the Manasquan water-supply system in Monmouth County, New Jersey: U.S. Geological Survey Water-Resources Investigations Report 2001-4172, v, 46 p. : ill., map ; 28 cm., https://doi.org/10.3133/wri014172.","productDescription":"v, 46 p. : ill., map ; 28 cm.","costCenters":[],"links":[{"id":14525,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/2001/wri01-4172/","linkFileType":{"id":5,"text":"html"}},{"id":203854,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -74.38333333333334,40.06666666666667 ], [ -74.38333333333334,40.333333333333336 ], [ -74,40.333333333333336 ], [ -74,40.06666666666667 ], [ -74.38333333333334,40.06666666666667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a00e4b07f02db5f7ce5","contributors":{"authors":[{"text":"Chang, Ming","contributorId":80318,"corporation":false,"usgs":true,"family":"Chang","given":"Ming","email":"","affiliations":[],"preferred":false,"id":230049,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tasker, Gary D.","contributorId":95035,"corporation":false,"usgs":true,"family":"Tasker","given":"Gary","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":230050,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nieswand, Steven","contributorId":34212,"corporation":false,"usgs":true,"family":"Nieswand","given":"Steven","affiliations":[],"preferred":false,"id":230048,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":45039,"text":"wri20014049 - 2001 - Ages and Origins of Calcite and Opal in the Exploratory Studies Facility Tunnel, Yucca Mountain, Nevada","interactions":[],"lastModifiedDate":"2012-02-10T00:10:06","indexId":"wri20014049","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":"2001-4049","title":"Ages and Origins of Calcite and Opal in the Exploratory Studies Facility Tunnel, Yucca Mountain, Nevada","docAbstract":"Deposits of calcite and opal are present as coatings on open fractures and lithophysal cavities in unsaturated-zone tuffs at Yucca Mountain, Nevada, site of a potential high-level radioactive waste repository. Outermost layers of calcite and opal have radiocarbon ages of 16,000 to 44,000 years before present and thorium-230/uranium ages of 28,000 to more than 500,000 years before present. These ages are young relative to the 13-million-year age of the host rocks. Multiple subsamples from the same outer layer typically show a range of ages with youngest ages from the thinnest subsamples. Initial uranium-234/uranium-238 activity ratios between 1 and 9.5 show a distinct negative correlation with thorium-230/uranium age and are greater than 4 for all but one sample younger than 100,000 years before present. These data, along with micrometer-scale layering and distinctive crystal morphologies, are interpreted to indicate that deposits formed very slowly from water films migrating through open cavities. Exchanges of carbon dioxide and water vapor probably took place between downward-migrating liquids and upward-migrating gases at low rates, resulting in oversaturation of mineral constituents at crystal extremities and more or less continuous deposition of very thin layers. Therefore, subsamples represent mixtures of older and younger layers on a scale finer than sampling techniques can resolve. Slow, long-term rates of deposition (less than about 5 millimeters of mineral per million years) are inferred from subsamples of outermost calcite and opal. These growth rates are similar to those calculated assuming that total coating thicknesses of 10 to 40 millimeters accumulated over 12 million years.\r\n\r\nCalcite has a wide range of delta carbon-13 values from about -8.2 to 8.5 per mil and delta oxygen-18 values from about 10 to 21 per mil. Systematic microsampling across individual mineral coatings indicates basal (older) calcite tends to have the largest delta carbon-13 values and smallest delta oxygen-18 values compared to calcite from intermediate and outer positions. Basal calcite has relatively small strontium-87/strontium-86 ratios, between 0.7105 and 0.7120, that are similar to the initial isotopic compositions of the strontium-rich tuff units, whereas outer calcite has more radiogenic strontium-87/strontium-86 ratios between 0.7115 and 0.7127. Isotopic compositions of strontium, oxygen, and carbon in the outer (youngest) unsaturated-zone calcite are coincident with those measured in Yucca Mountain calcrete, which formed by pedogenic processes.\r\n\r\nThe physical and isotopic data from calcite and opal indicate that they formed from solutions of meteoric origin percolating through a limited network of connected fracture pathways in the unsaturated zone rather than by inundation from ascending ground water originating in the saturated zone. Mineral assemblages, textures, and distributions within the unsaturated zone are distinctly different from those deposited below the water table at Yucca Mountain. The calcite and opal typically are present only on footwall surfaces of a small fraction of fractures and only on floors of a small fraction of lithophysal cavities. The similarities in the carbon, oxygen, and strontium isotopic compositions between fracture calcite and soil-zone calcite, as well as the gradation of textures from detritus-rich micrite in the soil to detritus-free spar 10 to 30 meters below the surface, also support a genetic link between the two depositional environments. Older deposits contain oxygen isotope compositions that indicate elevated temperatures of mineral formation during the early stages of deposition; however, in the youngest deposits these values are consistent with deposition under geothermal gradients similar to modern conditions. Correlations between mineral ages and varying Pleistocene climate conditions are not apparent from the current data. Cumulative evidence from calcite and opal deposits indicate","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/wri20014049","collaboration":"Prepared in cooperation with the Nevada Operations Office, U.S. Department of Energy, under Interagency Agreement DE?AI08?97NV12033","usgsCitation":"Paces, J.B., Neymark, L.A., Marshall, B.D., Whelan, J.F., and Peterman, Z., 2001, Ages and Origins of Calcite and Opal in the Exploratory Studies Facility Tunnel, Yucca Mountain, Nevada: U.S. Geological Survey Water-Resources Investigations Report 2001-4049, vi, 95 p., https://doi.org/10.3133/wri20014049.","productDescription":"vi, 95 p.","costCenters":[{"id":687,"text":"Yucca Mountain Project Branch","active":false,"usgs":true}],"links":[{"id":120642,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_2001_4049.jpg"},{"id":13245,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/2001/wri01-4049/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.58333333333333,36.666666666666664 ], [ -116.58333333333333,36.916666666666664 ], [ -116.33333333333333,36.916666666666664 ], [ -116.33333333333333,36.666666666666664 ], [ -116.58333333333333,36.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db689277","contributors":{"authors":[{"text":"Paces, James B. 0000-0002-9809-8493 jbpaces@usgs.gov","orcid":"https://orcid.org/0000-0002-9809-8493","contributorId":2514,"corporation":false,"usgs":true,"family":"Paces","given":"James","email":"jbpaces@usgs.gov","middleInitial":"B.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":230976,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Neymark, Leonid A. lneymark@usgs.gov","contributorId":532,"corporation":false,"usgs":true,"family":"Neymark","given":"Leonid","email":"lneymark@usgs.gov","middleInitial":"A.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":230974,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Marshall, Brian D. 0000-0002-8093-0093 bdmarsha@usgs.gov","orcid":"https://orcid.org/0000-0002-8093-0093","contributorId":520,"corporation":false,"usgs":true,"family":"Marshall","given":"Brian","email":"bdmarsha@usgs.gov","middleInitial":"D.","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":230973,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Whelan, Joseph F.","contributorId":29792,"corporation":false,"usgs":true,"family":"Whelan","given":"Joseph","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":230977,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Peterman, Zell E. 0000-0002-5694-8082 peterman@usgs.gov","orcid":"https://orcid.org/0000-0002-5694-8082","contributorId":620,"corporation":false,"usgs":true,"family":"Peterman","given":"Zell E.","email":"peterman@usgs.gov","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":230975,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":55083,"text":"wdrWI001 - 2001 - Water Resources Data, Wisconsin, Water Year 2000","interactions":[],"lastModifiedDate":"2012-02-02T00:11:52","indexId":"wdrWI001","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":"WI-00-1","title":"Water Resources Data, Wisconsin, Water Year 2000","language":"ENGLISH","doi":"10.3133/wdrWI001","usgsCitation":"Garn, H., Olson, D., and Ellefson, B., 2001, Water Resources Data, Wisconsin, Water Year 2000: U.S. Geological Survey Water Data Report WI-00-1, 586 p., https://doi.org/10.3133/wdrWI001.","productDescription":"586 p.","numberOfPages":"586","costCenters":[],"links":[{"id":174188,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/2000/wi-00-1/report-thumb.jpg"},{"id":87915,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/2000/wi-00-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa6f4","contributors":{"authors":[{"text":"Garn, H.S.","contributorId":42601,"corporation":false,"usgs":true,"family":"Garn","given":"H.S.","affiliations":[],"preferred":false,"id":252611,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olson, D.L.","contributorId":34943,"corporation":false,"usgs":true,"family":"Olson","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":252610,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ellefson, B.R.","contributorId":83927,"corporation":false,"usgs":true,"family":"Ellefson","given":"B.R.","email":"","affiliations":[],"preferred":false,"id":252612,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":50416,"text":"ofr01252 - 2001 - Yosemite Quadrangle, Central Sierra Nevada, California -- Analytic Data","interactions":[],"lastModifiedDate":"2012-02-02T00:11:17","indexId":"ofr01252","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":"2001-252","title":"Yosemite Quadrangle, Central Sierra Nevada, California -- Analytic Data","language":"ENGLISH","doi":"10.3133/ofr01252","isbn":"0607984449","usgsCitation":"Peck, D.L., 2001, Yosemite Quadrangle, Central Sierra Nevada, California -- Analytic Data: U.S. Geological Survey Open-File Report 2001-252, 1 CD-ROM : maps ; 4 3/4 in., https://doi.org/10.3133/ofr01252.","productDescription":"1 CD-ROM : maps ; 4 3/4 in.","costCenters":[],"links":[{"id":176651,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de38c","contributors":{"authors":[{"text":"Peck, Dallas L.","contributorId":60187,"corporation":false,"usgs":true,"family":"Peck","given":"Dallas","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":241414,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":45041,"text":"wri014060 - 2001 - User's guide for polyethylene-based passive diffusion bag samplers to obtain volatile organic compound concentrations in wells. Part I, Deployment, recovery, data interpretation, and quality control and assurance","interactions":[],"lastModifiedDate":"2012-02-02T00:10:43","indexId":"wri014060","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":"2001-4060","title":"User's guide for polyethylene-based passive diffusion bag samplers to obtain volatile organic compound concentrations in wells. Part I, Deployment, recovery, data interpretation, and quality control and assurance","docAbstract":"Diffusion samplers installed in observation wells were found to be capable of yielding representative water samples for chlorinated volatile organic compounds. The samplers consisted of polyethylene bags containing deionized water and relied on diffusion of chlorinated volatile organic compounds through the polyethylene membrane. The known ability of polyethylene to transmit other volatile compounds, such as benzene and toluene, indicates that the samplers can be used for a variety of volatile organic compounds. In wells at the study area, the volatile organic compound concentrations in water samples obtained using the samplers without prior purging were similar to concentrations in water samples obtained from the respective wells using traditional purging and sampling approaches. The low cost associated with this approach makes it a viable option for monitoring large observation-well networks for volatile organic compounds.","language":"ENGLISH","doi":"10.3133/wri014060","usgsCitation":"Vroblesky, D.A., 2001, User's guide for polyethylene-based passive diffusion bag samplers to obtain volatile organic compound concentrations in wells. Part I, Deployment, recovery, data interpretation, and quality control and assurance: U.S. Geological Survey Water-Resources Investigations Report 2001-4060, iv, 18 p. : ill. (some col.) ; 28 cm., https://doi.org/10.3133/wri014060.","productDescription":"iv, 18 p. : ill. (some col.) ; 28 cm.","costCenters":[],"links":[{"id":3902,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri014060","linkFileType":{"id":5,"text":"html"}},{"id":171260,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a16e4b07f02db603eaa","contributors":{"authors":[{"text":"Vroblesky, Don A. vroblesk@usgs.gov","contributorId":413,"corporation":false,"usgs":true,"family":"Vroblesky","given":"Don","email":"vroblesk@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":230979,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":45012,"text":"wri014112 - 2001 - Geochemistry and origins of mineralized waters in the Floridan aquifer system, northeastern Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:10:55","indexId":"wri014112","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":"2001-4112","title":"Geochemistry and origins of mineralized waters in the Floridan aquifer system, northeastern Florida","docAbstract":"Increases in chloride concentration have been observed in water from numerous wells tapping the Floridan aquifer system in northeastern Florida. Although most increases have been in the eastern part of Duval County, Florida, no spatial pattern in elevated chloride concentrations is discernible. Possible sources of the mineralized water include modern seawater intrusion; unflushed Miocene-to-Pleistocene-age seawater or connate water in aquifer sediments; or mineralized water from deeper zones of the aquifer system or from formations beneath the Floridan aquifer system. The purpose of this study was to document the chemical and isotopic characteristics of water samples from various aquifer zones, and from geochemical and hydrogeologic data, to infer the source of the increased mineralization. \r\n\r\nWater samples were collected from 53 wells in northeastern Florida during 1997-1999. Wells tapped various zones of the aquifer including: the Fernandina permeable zone (FPZ), the upper zone of the Lower Floridan aquifer (UZLF), the Upper Floridan aquifer (UFA), and both the UFA and the UZLF. Water samples were analyzed for major ions and trace constituents and for isotopes of carbon, oxygen, hydrogen, sulfur, strontium, chlorine, and boron. Samples of rock from the aquifer were analyzed for isotopes of oxygen, carbon, and strontium. \r\n\r\nIn general, water from various aquifer zones cannot be differentiated based on chemistry, except for water from FPZ wells. Major-ion concentrations vary as much within the upper zone of the Lower Floridan aquifer and the Upper Floridan aquifer as between these two zones. Simple models of mixing between fresh ground water and either modern seawater or water from the FPZ as a mineralized end member show that many water samples from the UZLF aquifer and the UFA are enriched in bicarbonate, calcium, magnesium, sulfate, fluoride, and silica and are depleted in sodium and potassium (as compared to concentrations predicted by simple mixing). Chemical mass-balance models of mixing and reactions between a hypothetical initial seawater and aquifer minerals cannot account for the observed water chemistry in a few wells, implying a source other than seawater, either ancient or modern, or the occurrence of other more complex rock-water reactions. \r\n\r\nHydrogeologic and geochemical data from water and aquifer samples indicate that the most likely source of mineralized water in some wells yielding water with increasing chloride concentrations is water from the FPZ. In other wells, the flushing of Miocene-to-Pleistocene-age seawater can account for the observed chloride concentrations. The fact that most of the water samples collected are a mixture of less than one percent of mineralized water with more than 99 percent fresh or recharge water makes identifying the source of the mineralized water difficult. Differences in carbon-14 and sulfur-34 values probably reflect areal differences in aquifer mineralogy and distribution of organic carbon related to paleokarst features. Geochemical mass-balance models of seawater-rock interaction are unable to account for the chemical and isotopic composition of mineralized water from the FPZ, which implies another source of mineralized water, such as a brine, or the occurrence of more complex water-rock reactions.","language":"ENGLISH","doi":"10.3133/wri014112","usgsCitation":"Phelps, G.G., 2001, Geochemistry and origins of mineralized waters in the Floridan aquifer system, northeastern Florida: U.S. Geological Survey Water-Resources Investigations Report 2001-4112, vi, 64 p. : ill., maps ; 28 cm., https://doi.org/10.3133/wri014112.","productDescription":"vi, 64 p. : ill., maps ; 28 cm.","costCenters":[],"links":[{"id":168391,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3879,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri014112/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab72c","contributors":{"authors":[{"text":"Phelps, G. G.","contributorId":82346,"corporation":false,"usgs":true,"family":"Phelps","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":230915,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":45054,"text":"wri004151 - 2001 - Methodology and Estimates of Scour at Selected Bridge Sites in Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:10:48","indexId":"wri004151","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":"2000-4151","title":"Methodology and Estimates of Scour at Selected Bridge Sites in Alaska","docAbstract":"The U.S. Geological Survey estimated scour depths at 325 bridges in Alaska as part of a cooperative agreement with the Alaska Department of Transportation and Public Facilities. The department selected these sites from approximately 806 State-owned bridges as potentially susceptible to scour during extreme floods. Pier scour and contraction scour were computed for the selected bridges by using methods recommended by the Federal Highway Administration. The U.S. Geological Survey used a four-step procedure to estimate scour: (1) Compute magnitudes of the 100- and 500-year floods. (2) Determine cross-section geometry and hydraulic properties for each bridge site. (3) Compute the water-surface profile for the 100- and 500-year floods. (4) Compute contraction and pier scour. This procedure is unique because the cross sections were developed from existing data on file to make a quantitative estimate of scour. This screening method has the advantage of providing scour depths and bed elevations for comparison with bridge-foundation elevations without the time and expense of a field survey. Four examples of bridge-scour analyses are summarized in the appendix.","language":"ENGLISH","doi":"10.3133/wri004151","usgsCitation":"Heinrichs, T.A., Kennedy, B., Langley, D.E., and Burrows, R.L., 2001, Methodology and Estimates of Scour at Selected Bridge Sites in Alaska: U.S. Geological Survey Water-Resources Investigations Report 2000-4151, iii, 44 p. : ill., map ; 28 cm. , https://doi.org/10.3133/wri004151.","productDescription":"iii, 44 p. : ill., map ; 28 cm. ","costCenters":[],"links":[{"id":171743,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3909,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri004151","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629f86","contributors":{"authors":[{"text":"Heinrichs, Thomas A.","contributorId":93509,"corporation":false,"usgs":true,"family":"Heinrichs","given":"Thomas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":231007,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kennedy, Ben W.","contributorId":104519,"corporation":false,"usgs":true,"family":"Kennedy","given":"Ben W.","affiliations":[],"preferred":false,"id":231008,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Langley, Dustin E.","contributorId":91904,"corporation":false,"usgs":true,"family":"Langley","given":"Dustin","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":231006,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Burrows, Robert L.","contributorId":79473,"corporation":false,"usgs":true,"family":"Burrows","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":231005,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":45036,"text":"wri014028 - 2001 - Vertical gradients in water chemistry in the central High Plains aquifer, southwestern Kansas and Oklahoma panhandle, 1999","interactions":[],"lastModifiedDate":"2012-02-02T00:04:58","indexId":"wri014028","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":"2001-4028","title":"Vertical gradients in water chemistry in the central High Plains aquifer, southwestern Kansas and Oklahoma panhandle, 1999","docAbstract":"The central High Plains aquifer is the primary source of water for domestic, industrial, and irrigation uses in parts of Colorado, Kansas, New Mexico, Oklahoma, and Texas. Water-level declines of more than 100 feet in some areas of the aquifer have increased the demand for water deeper in the aquifer. The maximum saturated thickness of the aquifer ranged from 500 to 600 feet in 1999. As the demand for deeper water increases, it becomes increasingly important for resource managers to understand how the quality of water in the aquifer changes with depth. In 1998?99, 18 monitoring wells at nine sites in southwestern Kansas and the Oklahoma Panhandle were completed at various depths in the central High Plains aquifer, and one monitoring well was completed in sediments of Permian age underlying the aquifer. Water samples were collected once from each well in 1999 to measure vertical gradients in water chemistry in the aquifer. Tritium concentrations measured in ground water indicate that water samples collected in the upper 30 feet of the aquifer were generally recharged within the last 50 years, whereas all of the water samples collected at depths more than 30 feet below the water table were recharged more than 50 years ago. Dissolved oxygen was present throughout the aquifer, with concentrations ranging from 1.7 to 8.4 mg/L. Water in the central High Plains aquifer was predominantly a calcium-bicarbonate type that exhibited little variability in concentrations of dissolved solids with depth (290 to 642 mg/L). Exceptions occurred in some areas where there had been upward movement of mineralized water from underlying sediments of Permian age and areas where there had been downward movement of mineralized Arkansas River water to the aquifer. Calcium-sulfate and sodium-chloride waters dominated and concentrations of dissolved solids were elevated (862 to 4,030 mg/L) near the base of the aquifer in the areas of upward leakage. Dissolution of gypsum or anhydrite and halite in sediments of Permian age by ground water was the likely source of calcium, sulfate, sodium, and chloride in those waters. Calcium-sodium-sulfate waters dominated, and concentrations of dissolved solids were as large as 4,916 mg/L near the water table in the area of downward leakage. Dissolution of minerals in sedimentary deposits of marine origin in upstream areas of the Arkansas River drainage were the likely sources of calcium, sodium, and sulfate in those waters. Nitrate was detected throughout the aquifer and the background concentration was estimated to be 2.45 mg/L as N. The largest nitrate concentrations (8.28, 22, and 54.4 mg/L as N) occurred in recently recharged water collected adjacent to irrigated fields. Three pesticides (atrazine, metolachlor, simazine) and five pesticide degradation products (alachlor ethanesulfonic acid, alachlor oxanilic acid, deethylatrazine, metolachlor ethanesulfonic acid, metolachlor oxanilic acid) were detected in recently recharged water from six water-table wells. Five of the six wells were adjacent to irrigated fields. These data indicate that concentrations of nitrate and pesticides increased over time in some areas of the aquifer as a result of agricultural activities. Results from this study indicate that vertical gradients in water chemistry existed in the central High Plains aquifer. The chemical gradients resulted from chemical inputs to the aquifer from underlying sediments of Permian age, from the Arkansas River, and from agricultural activities. In areas where those chemical inputs occurred, water quality in the aquifer was impaired and may not have been suitable for some intended uses. ","language":"ENGLISH","doi":"10.3133/wri014028","usgsCitation":"McMahon, P.B., 2001, Vertical gradients in water chemistry in the central High Plains aquifer, southwestern Kansas and Oklahoma panhandle, 1999: U.S. Geological Survey Water-Resources Investigations Report 2001-4028, vi, 47 p. : ill. (some col.), col. maps ; 28 cm., https://doi.org/10.3133/wri014028.","productDescription":"vi, 47 p. : ill. (some col.), col. maps ; 28 cm.","costCenters":[],"links":[{"id":3899,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri014028/","linkFileType":{"id":5,"text":"html"}},{"id":135805,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ace4b07f02db5c636b","contributors":{"authors":[{"text":"McMahon, Peter B. 0000-0001-7452-2379 pmcmahon@usgs.gov","orcid":"https://orcid.org/0000-0001-7452-2379","contributorId":724,"corporation":false,"usgs":true,"family":"McMahon","given":"Peter","email":"pmcmahon@usgs.gov","middleInitial":"B.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230970,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":45033,"text":"wri014199 - 2001 - Occurrence of phosphorus, nitrate, and suspended solids in streams of the Cheney Reservoir Watershed, south-central Kansas, 1997–2000","interactions":[],"lastModifiedDate":"2019-05-21T14:48:32","indexId":"wri014199","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":"2001-4199","displayTitle":"Occurrence of Phosphorus, Nitrate, and Suspended Solids in Streams of the Cheney Reservoir Watershed, South-Central Kansas, 1997–2000","title":"Occurrence of phosphorus, nitrate, and suspended solids in streams of the Cheney Reservoir Watershed, south-central Kansas, 1997–2000","docAbstract":"<p>Improving water quality of Cheney Reservoir in south-central Kansas is an important objective of State and local water managers. The reservoir serves as a water supply for about 350,00 people in the Wichita area and an important recreational resource for the area. In 1992, a task force was formed to study and prepare a plan to identify and mitigate potential sources of stream contamination in the Cheney Reservoir watershed. This task force was established to develop stream-water-quality goals to aid in the development and implementation of best-management practices in the watershed. In 1996, the U.S. Geological Survey entered into a cooperative study with the city of Wichita to assess the water quality in the Cheney Reservoir watershed. Water-quality constituents of particular concern in the Cheney Reservoir watershed are phosphorus, nitrate, and total suspended solids. Water-quality samples were collected at five streamflow-gaging sites upstream from the reservoir and at the outflow of the reservoir. The purpose of this report is to present the results of a 4-year (1997-2000) data-collection effort to quantify the occurrence of phosphorus, nitrate, and suspended solids during base-flow, runoff, and long-term streamflow conditions (all available data for 1997-2000) and to compare these results to stream-water-quality goals established by the Cheney Reservoir Task Force. </p><p>Mean concentrations of each of the constituents examined during this study exceeded the Cheney Reservoir Task Force stream-water-quality goal for at least one of the streamflow conditions evaluated. Most notably, mean base-flow and mean long-term concentrations of total phosphorus and mean base-flow concentrations of dissolved nitrate exceeded the goals of 0.05, 0.10, and 0.25 milligram per liter, respectively, at all five sampling sites upstream from the reservoir. Additionally, the long-term stream-water-quality goal for dissolved nitrate was exceeded by the mean concentration at one upstream sampling site, and the base-flow total suspended solids goal (20 milligrams per liter) and long-term total suspended solids goal (100 milligrams per liter) were each exceeded by mean concentrations at three upstream sampling sites. Generally, it seems unlikely that water-quality goals for streams in the Cheney Reservoir watershed will be attainable for mean base-flow and mean long-term total phosphorus and total suspended solids concentrations and for mean base-flow dissolved nitrate concentrations as long as current (2001) watershed conditions and practices persist. However, future changes in these conditions and practices that mitigate the transport of these consitutents may modify this conclusion.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri014199","collaboration":"Prepared in cooperation with the City of Wichita, Kansas","usgsCitation":"Milligan, C.R., and Pope, L.M., 2001, Occurrence of phosphorus, nitrate, and suspended solids in streams of the Cheney Reservoir Watershed, south-central Kansas, 1997–2000: U.S. Geological Survey Water-Resources Investigations Report 2001-4199, Report: iv, 18 p.; Additional Report Piece, https://doi.org/10.3133/wri014199.","productDescription":"Report: iv, 18 p.; Additional Report Piece","costCenters":[{"id":353,"text":"Kansas Water Science 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 \"}}]}","contact":"<p><a href=\"mailto:%20dc_ks@usgs.gov\" data-mce-href=\"mailto:%20dc_ks@usgs.gov\">Director</a>, <a href=\"https://www.usgs.gov/centers/kswsc\" data-mce-href=\"https://www.usgs.gov/centers/kswsc\">Kansas Water Science Center</a><br>U.S. Geological Survey<br>1217 Biltmore Drive<br>Lawrence, KS 66049</p>","tableOfContents":"<ul><li>Abstract</li><li>Background</li><li>Study Methods</li><li>Streamflow Conditions</li><li>Occurrence of Phosphorus, Nitrate, and Suspended Solids</li><li>Comparison to Previous Investigations</li><li>Summary and Conclusions</li><li>References</li></ul>","publishingServiceCenter":{"id":4,"text":"Rolla PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af5e4b07f02db69239e","contributors":{"authors":[{"text":"Milligan, Chad 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,{"id":79766,"text":"mineral2001 - 2001 - Mineral Commodity Summaries 2001","interactions":[],"lastModifiedDate":"2013-02-04T10:59:15","indexId":"mineral2001","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":323,"text":"Mineral Commodity Summaries","code":"MCS","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2001","title":"Mineral Commodity Summaries 2001","docAbstract":"Published on an annual basis, this report is the earliest Government publication to furnish estimates covering nonfuel mineral industry data. Data sheets contain information on the domestic industry structure, Government programs, tariffs, and 5-year salient statistics for over 90 individual minerals and materials.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/mineral2001","usgsCitation":"Mineral Commodity Summaries 2001; 2001; MINERAL; 2001; U.S. Geological Survey","productDescription":"195 p.; 3 Appendixes (4 p.); Individual Commodity Data Sheets; Available Online, Printed, and on CD-ROM","additionalOnlineFiles":"Y","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":194908,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mineral_2001.jpg"},{"id":9445,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://minerals.usgs.gov/minerals/pubs/mcs/2001/mcs2001.pdf","size":"1518","linkFileType":{"id":1,"text":"pdf"}},{"id":9444,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://minerals.usgs.gov/minerals/pubs/mcs/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635741","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":534849,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50372,"text":"ofr00504 - 2000 - Simulation of ground water flow in the Glaciofluvial, Saginaw, Parma-Bayport, and Marshall Aquifers, Central Lower Peninsula of Michigan","interactions":[],"lastModifiedDate":"2026-01-21T17:22:07.762133","indexId":"ofr00504","displayToPublicDate":"2021-12-02T11:05:00","publicationYear":"2000","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":"2000-504","displayTitle":"Simulation of Ground-Water Flow in the Glaciofluvial, Saginaw, Parma-Bayport, and Marshall Aquifers, Central Lower Peninsula of Michigan","title":"Simulation of ground water flow in the Glaciofluvial, Saginaw, Parma-Bayport, and Marshall Aquifers, Central Lower Peninsula of Michigan","docAbstract":"<p>A steady-state finite difference model was developed to simulate ground-water flow in four regional aquifers in Michigan’s Lower Peninsula. The Glaciofluvial, Saginaw, Parma-Bayport, and Marshall aquifers were simulated as layers 1 through 4, respectively, in the model. Separately calculated vertical conductances input to the model were used to simulate the intervening Till/“Red Beds”, Saginaw, and Michigan confining units, respectively. The model domain was laterally bound by a continuous specifiedhead boundary, formed from Lakes Michigan, Huron, St. Clair, and Erie, together with the St. Clair and Detroit River connecting channels.</p><p>The model was developed to quantify regional ground-water flow in the aquifer systems using independently determined recharge estimates. The flow model showed that groundwater heads and flows in the Glaciofluvial aquifer are controlled by local stream stages and discharges, resulting in localized flow cells accounting for 95-percent of the overall model water budget. Simulation of recharge to an unspecified water table also enabled the estimation of ground-water discharge to three Great Lakes.</p><p>A computer diskette contains all MODFLOW and MODFLOWP input files, as well as digital model surfaces and several Fortran processing routines used to construct the surfaces. The diskette also provides the data used for calibration and sensitivity analysis.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr00504","usgsCitation":"Hoaglund, J.R., Huffman, G., and Granneman, N., 2000, Simulation of ground water flow in the Glaciofluvial, Saginaw, Parma-Bayport, and Marshall Aquifers, Central Lower Peninsula of Michigan: U.S. Geological Survey Open-File Report 2000-504, iv, 36 p., https://doi.org/10.3133/ofr00504.","productDescription":"iv, 36 p.","numberOfPages":"36","costCenters":[],"links":[{"id":392379,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2000/0504/ofr00504.pdf","text":"Report","size":"4.73 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 00-504"},{"id":176862,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2000/0504/coverthb2.jpg"}],"country":"United States","state":"Michigan","otherGeospatial":"Saginaw, Parma-Bayport, and Marshall Aquifers","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.3525390625,\n              42.13082130188811\n            ],\n            [\n              -83.3203125,\n              42.13082130188811\n            ],\n            [\n              -83.3203125,\n              44.11914151643737\n            ],\n            [\n              -86.3525390625,\n              44.11914151643737\n            ],\n            [\n              -86.3525390625,\n              42.13082130188811\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://pubs.er.usgs.gov/contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db648545","contributors":{"authors":[{"text":"Hoaglund, John Robert III","contributorId":13685,"corporation":false,"usgs":true,"family":"Hoaglund","given":"John","suffix":"III","email":"","middleInitial":"Robert","affiliations":[],"preferred":false,"id":241296,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Huffman, G.C.","contributorId":44150,"corporation":false,"usgs":true,"family":"Huffman","given":"G.C.","email":"","affiliations":[],"preferred":false,"id":241298,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Granneman, N.J.","contributorId":32978,"corporation":false,"usgs":true,"family":"Granneman","given":"N.J.","email":"","affiliations":[],"preferred":false,"id":241297,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70038037,"text":"70038037 - 2000 - U.S. Geological Survey Activities Related to American Indians and Alaska Natives Fiscal Year 2000","interactions":[],"lastModifiedDate":"2021-08-19T14:41:37.42066","indexId":"70038037","displayToPublicDate":"2021-08-19T10:45:00","publicationYear":"2000","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"U.S. Geological Survey Activities Related to American Indians and Alaska Natives Fiscal Year 2000","docAbstract":"<p>The U.S. Geological Survey (USGS) is an impartial scientific organization that strives to produce scientific results that are relevant to the people of the United States and their land and resource managers. USGS does not improve the quality of its customers' lives; it provides the informational tools for American Indians, Alaska Natives, and other customers to understand and improve their own lives.</p><p>In cooperation with American Indian and Alaska Native governments, the USGS conducts research on water and mineral resources, animals and plants of environmental, economic, or subsistence importance, natural hazards, and geologic resources. Digital data on cartography, mineral resources, stream flows, biota, and other data sets are available to American Indian and Alaska Native institutions. The USGS recognizes the need to learn from and share knowledge with Native peoples. This report describes most of the activities that the USGS conducted with American Indian and Alaska Native governments, educational institutions, and individuals during Federal Fiscal Year 2000. Some of these USGS activities were conducted in concert with the Bureau of Indian Affairs. Others were conducted by Tribes and the USGS.</p><p>In the year 2000, the USGS began examining its activities related to American Indians and Native Alaskans to determine how it can better serve these customers within its mandates. More Tribal governments, educational institutions, and other Tribal organizations are using geographic information systems and other digital technologies in recent years. As Tribes become more interested and more adept at managing digital information, they are seeking such data from the USGS with greater frequency. The increasing use of such technologies allows Tribal governments additional means of managing lands and resources for the benefit of current and future generations. The USGS recognizes the need to make its information available to Tribal governments, and to work with those governments and other institutions to advance data management capabilities.</p><p>The USGS is responding to this need by increasing the transfer of scientific information to American Indian and Alaska Native governments and by training employees of these governments to conduct and improve scientific studies. The USGS is also encouraging American Indians and Alaska Natives to pursue careers in science, and seeking ways to hire Indian and Native students. By identifying, improving, and disseminating information about available hiring mechanisms, the USGS is working to make hiring such students easier, and therefore more likely, for USGS managers.</p><p>The U.S. Geological Survey is the Federal science bureau within the Department of the Interior (DoI). The USGS is non-regulatory and is not a significant manager of Federal or Trust lands or assets. However, there are two types of USGS activities that do involve American Indians, Alaska Natives, and their lands. The first type of activity is the course of formal studies, conducted through existing USGS programs, that involve collection of specific types of data as well as investigative and research projects. These projects have a duration of two or three years, although a few are parts of longer-term activities. Some are funded through cooperative agreements or reimbursable accounts, from monies provided to the USGS by individual Tribal governments or by the Bureau of Indian Affairs (BIA). The USGS provides matching funds for cooperative projects. These formal projects may also receive funding from the U.S. Environmental Protection Agency, the Indian Health Service (part of the Department of Health and Human Services), or other Federal agencies. The USGS routinely works with its sister bureaus in the Department of the Interior to provide the scientific information and expertise needed to meet the Department's science priorities. Within this context, the USGS and the Bureau of Indian Affairs are cooperating to use USGS knowledge for the benefit of American Indian and Native peoples and their lands.</p><p>The second type of USGS activity is less formal, based on initiatives designed and conducted by USGS employees. Frequently involving educational activities, these endeavors are prompted by employee interests, often as collateral issues, that result from an individual or group of USGS employees identifying and responding to an observed need. In these activities, USGS employees help us fulfill a mission of the USGS, to make science relevant, while helping their fellow citizens. USGS employees have also taken the initiative to assist American Indians and Alaska Natives through participation in several organizations that were created to foster knowledge of science among Native peoples and to help build support and communication networks. One such group is the American Indian Science and Engineering Society (AISES). This group sponsors an annual national meeting in which USGS employees participate. USGS employees join this organization on a voluntary basis, paying the costs themselves, yet bringing the benefits of this expanded network to the USGS, as many employees do with other professional organizations.</p><p>Each part of the USGS has identified an American Indian/Alaska Native liaison. As USGS moves to a more regional organizational structure, it will establish contacts in the Western, Central, and Eastern Regions. Within the USGS, this report will help in developing outreach, educational, and program documents for use in future years. It is hoped that USGS employees, American Indians, and Alaska Natives will adapt these activities in new areas and will use the USGS contacts to expand the relevance of the USGS to more Americans.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70038037","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2000, U.S. Geological Survey Activities Related to American Indians and Alaska Natives Fiscal Year 2000, xi, 57 p., https://doi.org/10.3133/70038037.","productDescription":"xi, 57 p.","costCenters":[],"links":[{"id":359902,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70038037/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":254498,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70038037/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bba52e4b08c986b3280e2","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":535180,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70231299,"text":"70231299 - 2000 - Integration of a numerical model and remotely sensed data to study urban/rural land surface climate processes","interactions":[],"lastModifiedDate":"2022-05-05T15:58:48.077773","indexId":"70231299","displayToPublicDate":"2020-03-20T10:53:14","publicationYear":"2000","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1315,"text":"Computers & Geosciences","printIssn":"0098-3004","active":true,"publicationSubtype":{"id":10}},"title":"Integration of a numerical model and remotely sensed data to study urban/rural land surface climate processes","docAbstract":"<p>Simulation of urban/rural land surface climate processes using boundary layer climate models requires accurate input data with regard to surface thermal and radiative properties. The research reported here resulted in development of a procedure to integrate the satellite-derived surface biophysical parameters with a boundary layer climate model for simulating spatial surface energy exchange.</p><p>The procedure was tested through spatial surface energy balance simulation of an urban/rural landscape in eastern Nebraska. The modeled surface temperature and net radiation were compared to those derived from the concurrent satellite data. The errors of the modeled surface temperature were small, and were mainly attributed to uncertainties in the estimation of surface moisture availability and satellite-derived surface radiant temperature. Modeled net radiation was also in agreement with the values calculated from satellite data. Modeled turbulent heat fluxes were in general agreement as compared to those reported in the literature, but the model tended to overestimate the latent heat flux for most rural land cover types. It was concluded that by incorporation of satellite-derived surface physical parameters into a boundary layer model, simulation of spatial land surface climate processes was much improved. The method and procedures developed from this study can be utilized in other boundary layer climate models.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0098-3004(99)00124-7","usgsCitation":"Yang, L., 2000, Integration of a numerical model and remotely sensed data to study urban/rural land surface climate processes: Computers & Geosciences, v. 26, no. 4, p. 451-468, https://doi.org/10.1016/S0098-3004(99)00124-7.","productDescription":"18 p.","startPage":"451","endPage":"468","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":400212,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nebraska","city":"Lincoln, Omaha","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.97357177734375,\n              40.69521661351714\n            ],\n            [\n              -95.82824707031249,\n              40.69521661351714\n            ],\n            [\n              -95.82824707031249,\n              41.498292501398545\n            ],\n            [\n              -96.97357177734375,\n              41.498292501398545\n            ],\n            [\n              -96.97357177734375,\n              40.69521661351714\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"26","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Yang, Limin 0000-0002-2843-6944 lyang@usgs.gov","orcid":"https://orcid.org/0000-0002-2843-6944","contributorId":4305,"corporation":false,"usgs":true,"family":"Yang","given":"Limin","email":"lyang@usgs.gov","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":842268,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70206367,"text":"70206367 - 2000 - Borehole-wall imaging with acoustic and optical televiewers for fractured-bedrock aquifer investigations","interactions":[],"lastModifiedDate":"2019-10-31T09:39:58","indexId":"70206367","displayToPublicDate":"2019-12-31T09:35:21","publicationYear":"2000","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Borehole-wall imaging with acoustic and optical televiewers for fractured-bedrock aquifer investigations","docAbstract":"<p><span>Imaging with acoustic and optical televiewers results in continuous and oriented 360 degree views of the borehole wall from which the character and orientation of lithologic and structural features can be defined for fractured-bedrock aquifer investigations. Fractures are more clearly defined under a wider range of conditions on acoustic images than on optical images including dark-colored rocks, cloudy borehole water, and coated borehole walls. However, optical images allow for the direct viewing of the character of and relation between lithology, fractures, foliation, and bedding. The most powerful approach is the combined application of acoustic and optical imaging with integrated interpretation. Borehole-wall imaging provides information useful for the collection and interpretation of flowmeter and other geophysical logs, core samples, and hydraulic and water-quality data from packer testing and monitoring.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the seventh international symposium on borehole geophysics for minerals, geotechnical, and groundwater applications","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Seventh International Symposium on Borehole Geophysics for Minerals, Geotechnical, and Groundwater Applications","conferenceDate":"October 24-26, 2000","conferenceLocation":"Golden, CO","language":"English","publisher":"Society of Professional Well Log Analysts","usgsCitation":"Williams, J., and Johnson, C.D., 2000, Borehole-wall imaging with acoustic and optical televiewers for fractured-bedrock aquifer investigations, <i>in</i> Proceedings of the seventh international symposium on borehole geophysics for minerals, geotechnical, and groundwater applications, Golden, CO, October 24-26, 2000, p. 43-53.","productDescription":"11 p.","startPage":"43","endPage":"53","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"links":[{"id":368799,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":368798,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://water.usgs.gov/ogw/bgas/publications/mgls2000/"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Williams, John H. 0000-0002-6054-6908 jhwillia@usgs.gov","orcid":"https://orcid.org/0000-0002-6054-6908","contributorId":1553,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"jhwillia@usgs.gov","middleInitial":"H.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":774301,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Carole D. 0000-0001-6941-1578 cjohnson@usgs.gov","orcid":"https://orcid.org/0000-0001-6941-1578","contributorId":1891,"corporation":false,"usgs":true,"family":"Johnson","given":"Carole","email":"cjohnson@usgs.gov","middleInitial":"D.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":774302,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70182118,"text":"70182118 - 2000 - Measurement of 1999 drought conditions in Mississippi","interactions":[],"lastModifiedDate":"2018-03-02T15:55:15","indexId":"70182118","displayToPublicDate":"2017-02-16T00:00:00","publicationYear":"2000","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Measurement of 1999 drought conditions in Mississippi","docAbstract":"<p><span>Accurate and reliable water-resources data collected during drought conditions are critical to regulatory agencies such as the Mississippi Department of Environmental Quality (MDEQ). Droughts have affected Mississippi during 1940-44, 1951-57, 1962-71, 1980-82 and 1983-88. In late summer and early autumn 1999, many areas of Mississippi experienced near record drought conditions causing concern to many private and public interests. Personnel from the U.S. Geological Survey (USGS), in cooperation with the MDEQ Office of Land and Water Resources (MDEQ-OLWR) measured water levels and streamflows throughout the State of Mississippi during drought conditions in August through October 1999. Droughts are normal, recurring hydrological events caused by deficiency of precipitation over an extended period of time that can have adverse effects on anthropogenic use of water. Much of the State of Mississippi has continued to experience drought conditions through late winter of 2000. Data on minimum streamflows are an important factor for determining the regulation of flow control structures, effluent discharge, and surface water withdrawals and other water-management decisions during droughts. Data on minimum streamflows become paramount during drought conditions. This report presents information related to the legal aspects of drought conditions and includes selected data collected at streamgages affected by severe drought conditions in Mississippi during the late summer and early autumn of 1999. Comparisons of low-flow characteristics at selected streamgages to other period-of-record low-flows at selected gages in the State are also presented.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the thirtieth Mississippi Water Resources Conference","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"30th Annual Mississippi Water Resources Conference","conferenceDate":"April 18-19, 2000","conferenceLocation":"Raymond, MS","language":"English","publisher":"Mississippi Water Resources Research Institute, Mississippi State University","doi":"10.13140/2.1.3215.4246","usgsCitation":"Turnipseed, D.P., and Long, L.G., 2000, Measurement of 1999 drought conditions in Mississippi, <i>in</i> Proceedings of the thirtieth Mississippi Water Resources Conference, Raymond, MS, April 18-19, 2000, https://doi.org/10.13140/2.1.3215.4246.","costCenters":[],"links":[{"id":335719,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Mississippi","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58a6c83de4b025c4642862f0","contributors":{"editors":[{"text":"Ballweber, Jeffery A.","contributorId":181569,"corporation":false,"usgs":false,"family":"Ballweber","given":"Jeffery","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":730127,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Turnipseed, D. Phil 0000-0002-9737-3203 pturnip@usgs.gov","orcid":"https://orcid.org/0000-0002-9737-3203","contributorId":298,"corporation":false,"usgs":true,"family":"Turnipseed","given":"D.","email":"pturnip@usgs.gov","middleInitial":"Phil","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":669661,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Long, Loyd G.","contributorId":181820,"corporation":false,"usgs":false,"family":"Long","given":"Loyd","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":669662,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70176057,"text":"ofr00065 - 2000 - Creating a standardized watersheds database for the Lower Rio Grande/Río Bravo, Texas","interactions":[],"lastModifiedDate":"2016-08-24T12:06:18","indexId":"ofr00065","displayToPublicDate":"2016-02-17T00:00:00","publicationYear":"2000","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":"00-065","title":"Creating a standardized watersheds database for the Lower Rio Grande/Río Bravo, Texas","docAbstract":"<p><span size=\"3\" data-mce-style=\"font-size: medium;\" style=\"font-size: medium;\">This report describes the creation of a large-scale watershed database for the lower Rio Grande/Río Bravo Basin in Texas. The watershed database includes watersheds delineated to all 1:24,000-scale mapped stream confluences and other hydrologically significant points, selected watershed characteristics, and hydrologic derivative datasets.</span></p><p><span size=\"3\" data-mce-style=\"font-size: medium;\" style=\"font-size: medium;\">Computer technology allows generation of preliminary watershed boundaries in a fraction of the time needed for manual methods. This automated process reduces development time and results in quality improvements in watershed boundaries and characteristics. These data can then be compiled in a permanent database, eliminating the time-consuming step of data creation at the beginning of a project and providing a stable base dataset that can give users greater confidence when further subdividing watersheds.</span></p><p><span size=\"3\" data-mce-style=\"font-size: medium;\" style=\"font-size: medium;\">A standardized dataset of watershed characteristics is a valuable contribution to the understanding and management of natural resources. Vertical integration of the input datasets used to automatically generate watershed boundaries is crucial to the success of such an effort. The optimum situation would be to use the digital orthophoto quadrangles as the source of all the input datasets. While the hydrographic data from the digital line graphs can be revised to match the digital orthophoto quadrangles, hypsography data cannot be revised to match the digital orthophoto quadrangles. Revised hydrography from the digital orthophoto quadrangle should be used to create an updated digital elevation model that incorporates the stream channels as revised from the digital orthophoto quadrangle. Computer-generated, standardized watersheds that are vertically integrated with existing digital line graph hydrographic data will continue to be difficult to create until revisions can be made to existing source datasets. Until such time, manual editing will be necessary to make adjustments for man-made features and changes in the natural landscape that are not reflected in the digital elevation model data.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr00065","collaboration":"In cooperation with the Texas Natural Resource Conservation Commission","usgsCitation":"Brown, J., Ulery, R.L., and Parcher, J.W., 2000, Creating a standardized watersheds database for the Lower Rio Grande/Río Bravo, Texas: U.S. Geological Survey Open-File Report 00-065, iii, 17 p., https://doi.org/10.3133/ofr00065.","productDescription":"iii, 17 p.","numberOfPages":"21","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":327800,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":327796,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2000/ofr00-065/00-065.pdf","text":"Creating a Standardized Watersheds Database for the Lower Rio Grande/ Río Bravo, Texas","size":"528 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Creating a Standardized Watersheds Database for the Lower Rio Grande/ Río Bravo, Texas"}],"country":"United States","state":"Texas","county":"Webb","city":"Rio Bravo","otherGeospatial":"Lower Rio Grande","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -99.50325965881348,\n              27.362391688477363\n            ],\n            [\n              -99.50325965881348,\n              27.366889032381295\n            ],\n            [\n              -99.45948600769043,\n              27.366889032381295\n            ],\n            [\n              -99.45948600769043,\n              27.362391688477363\n            ],\n            [\n              -99.50325965881348,\n              27.362391688477363\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","tableOfContents":"<p><span face=\"Arial\" data-mce-style=\"font-family: Arial;\" style=\"font-family: Arial;\">CONTENTS</span></p><blockquote><p>Abstract</p><p>Introduction</p><blockquote><p>Purpose and Scope</p><p>Acknowledgments</p><p>Background</p><blockquote><blockquote><p>Watershed-Boundary Delineation</p><p>Standardized Watershed Classification</p><p>Watershed Characteristics</p><p>Topographic Datasets</p></blockquote></blockquote></blockquote><p>Methods Used to Create a Standardized Watersheds Database</p><blockquote><p>Source Datasets</p><p>DEM Processing—Creation of Hydrologic Derivatives&nbsp;</p><p>Watershed Delineation</p><blockquote><blockquote><p>Revision of the Hydrography</p><p>Computer-Generated Watershed Delineations</p><p>Review of Computer-Generated Watershed Delineations and&nbsp;<br>&nbsp;&nbsp;&nbsp;&nbsp; Manual Delineations</p><p>Watershed Region Coverage</p></blockquote></blockquote><p>Watershed Characteristics</p><p>Conflation of RF3 Attributes</p><p>Extending Hydrologic Unit Code (HUC) to 12 Digits</p></blockquote><p>Conclusions</p><p>Selected References</p><p>Appendix - Watershed Characteristic Computations</p></blockquote>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57c6af00e4b0f2f0cebe46f2","contributors":{"authors":[{"text":"Brown, J.R.","contributorId":56872,"corporation":false,"usgs":true,"family":"Brown","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":646963,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ulery, Randy L. rlulery@usgs.gov","contributorId":4679,"corporation":false,"usgs":true,"family":"Ulery","given":"Randy","email":"rlulery@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":646964,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Parcher, Jean W. jwparcher@usgs.gov","contributorId":2209,"corporation":false,"usgs":true,"family":"Parcher","given":"Jean","email":"jwparcher@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":646965,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70170441,"text":"70170441 - 2000 - Effects of food limitation and emigration on self-thinning in experimental minnow cohorts","interactions":[],"lastModifiedDate":"2017-04-03T15:11:32","indexId":"70170441","displayToPublicDate":"2016-01-06T10:45:00","publicationYear":"2000","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2158,"text":"Journal of Animal Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Effects of food limitation and emigration on self-thinning in experimental minnow cohorts","docAbstract":"<p><span>1.</span>&ensp;The theory of food-regulated self-thinning (FST) for mobile animals predicts population density (<i>N</i>) to be an inverse function of mean body mass (<i>W</i>) scaled to an exponent (<i>b</i>), such that&nbsp;<i>N&nbsp;=</i>&nbsp;k&nbsp;<i>W</i><span><i>&minus;b</i></span>, where k is a constant. FST also predicts energy requirements (or energy flow) to remain constant over time (termed energetic equivalence) as losses to cohorts (e.g. emigration and mortality) are balanced by increased growth of surviving individuals.</p>\n<p><span>2.</span>&ensp;To test these predictions, we analysed the dynamics of six experimental minnow cohorts. Replicate populations of fish were held under identical conditions with a constant and limited supply of food over a 126-day period. Half of the cohorts were open to emigration, and half were closed so that fish could only be lost through starvation mortality.</p>\n<p><span>3.</span>&ensp;Patterns of self-thinning indicated non-linear changes in population density and energy flow in relation to changes in mean body mass and time, respectively. Non-linear patterns of self-thinning were probably due to a delayed growth response to changes in population density effected through mortality and/or emigration. Contrary to results of similar experiments on other fish, emigration did not have a significant influence on the pattern of self-thinning.</p>\n<p><span>4.</span>&ensp;These results may be attributed to trophic interactions within cohorts and the importance of social behaviour to cohort dynamics. Both population density and energy flow in our experimental populations appeared to cycle, with episodes of starvation and mortality alternating with food recovery and weight gain, as predicted by recent models of stepwise die-off and stunted growth in animal cohorts.</p>\n<p><span>5.</span>&ensp;Most of the support for FST in mobile animals comes from observational data on mean body mass and population density. Potentially important mechanisms, including the manner in which individuals are lost or retained in populations, are usually not investigated directly. Such tests of FST can only provide equivocal support. Detailed observational study and controlled experiments are needed to understand casual mechanisms.</p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1365-2656.2000.00451.x","usgsCitation":"Dunham, J., Dickerson, B.R., Beever, E., Duncan, R.D., and Vinyard, G., 2000, Effects of food limitation and emigration on self-thinning in experimental minnow cohorts: Journal of Animal Ecology, v. 69, no. 6, p. 927-934, https://doi.org/10.1111/j.1365-2656.2000.00451.x.","productDescription":"7 p.","startPage":"927","endPage":"934","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":320315,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","volume":"69","issue":"6","noUsgsAuthors":false,"publicationDate":"2008-07-07","publicationStatus":"PW","scienceBaseUri":"5718a83ee4b0ef3b7caba533","contributors":{"authors":[{"text":"Dunham, J. B. 0000-0002-6268-0633","orcid":"https://orcid.org/0000-0002-6268-0633","contributorId":96637,"corporation":false,"usgs":true,"family":"Dunham","given":"J. B.","affiliations":[],"preferred":false,"id":627216,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dickerson, B. R.","contributorId":168770,"corporation":false,"usgs":false,"family":"Dickerson","given":"B.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":627217,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Beever, E.","contributorId":168771,"corporation":false,"usgs":false,"family":"Beever","given":"E.","email":"","affiliations":[],"preferred":false,"id":627218,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Duncan, R. D.","contributorId":168772,"corporation":false,"usgs":false,"family":"Duncan","given":"R.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":627219,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Vinyard, G.L.","contributorId":59388,"corporation":false,"usgs":true,"family":"Vinyard","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":627220,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
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