{"pageNumber":"3033","pageRowStart":"75800","pageSize":"25","recordCount":184752,"records":[{"id":55051,"text":"wdrVA011 - 2002 - Water resources data, Virginia, water year 2001; Volume 1: Surface-water discharge and surface-water quality records","interactions":[],"lastModifiedDate":"2022-12-30T18:30:46.999532","indexId":"wdrVA011","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"VA-01-1","title":"Water resources data, Virginia, water year 2001; Volume 1: Surface-water discharge and surface-water quality records","docAbstract":"

The Water Resources Division of the U.S. Geological Survey, in cooperation with State agencies, obtains a large amount of data pertaining to the water resources of Virginia each water year. These data, accumulated during many water years, constitute a valuable data base for developing an improved understanding of the water resources of the State. To make these data readily available to interested parties outside the Geological Survey, the data are published annually in this report series entitled \"Water Resources Data - Virginia.\"

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrVA011","collaboration":"Prepared in cooperation with the Virginia Department of Environmental Quality and with other agencies","usgsCitation":"White, R., Hayes, D.C., Guyer, J.R., and Herman, P., 2002, Water resources data, Virginia, water year 2001; Volume 1: Surface-water discharge and surface-water quality records: U.S. Geological Survey Water Data Report VA-01-1, xxiii, 493 p., https://doi.org/10.3133/wdrVA011.","productDescription":"xxiii, 493 p.","costCenters":[],"links":[{"id":411233,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/2001/va-01-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":181656,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/2001/va-01-1/report-thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa70a","contributors":{"authors":[{"text":"White, R.K.","contributorId":96338,"corporation":false,"usgs":true,"family":"White","given":"R.K.","email":"","affiliations":[],"preferred":false,"id":252481,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hayes, Donald C.","contributorId":14000,"corporation":false,"usgs":true,"family":"Hayes","given":"Donald","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":252478,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Guyer, Joel R.","contributorId":47446,"corporation":false,"usgs":true,"family":"Guyer","given":"Joel","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":252479,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Herman, P.E.","contributorId":73671,"corporation":false,"usgs":true,"family":"Herman","given":"P.E.","email":"","affiliations":[],"preferred":false,"id":252480,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":53871,"text":"bsr20020001 - 2002 - Arctic Refuge coastal plain terrestrial wildlife research summaries","interactions":[{"subject":{"id":2002049,"text":"2002049 - 2002 - Polar Bears","indexId":"2002049","publicationYear":"2002","noYear":false,"chapter":"8","title":"Polar Bears"},"predicate":"IS_PART_OF","object":{"id":53871,"text":"bsr20020001 - 2002 - Arctic Refuge coastal plain terrestrial wildlife research summaries","indexId":"bsr20020001","publicationYear":"2002","noYear":false,"title":"Arctic Refuge coastal plain terrestrial wildlife research summaries"},"id":1},{"subject":{"id":70187586,"text":"70187586 - 2002 - Snow geese","indexId":"70187586","publicationYear":"2002","noYear":false,"chapter":"9","title":"Snow 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Predators","indexId":"70187591","publicationYear":"2002","noYear":false,"chapter":"6","title":"Predators"},"predicate":"IS_PART_OF","object":{"id":53871,"text":"bsr20020001 - 2002 - Arctic Refuge coastal plain terrestrial wildlife research summaries","indexId":"bsr20020001","publicationYear":"2002","noYear":false,"title":"Arctic Refuge coastal plain terrestrial wildlife research summaries"},"id":4},{"subject":{"id":70188490,"text":"70188490 - 2002 - Introduction","indexId":"70188490","publicationYear":"2002","noYear":false,"chapter":"1","title":"Introduction"},"predicate":"IS_PART_OF","object":{"id":53871,"text":"bsr20020001 - 2002 - Arctic Refuge coastal plain terrestrial wildlife research summaries","indexId":"bsr20020001","publicationYear":"2002","noYear":false,"title":"Arctic Refuge coastal plain terrestrial wildlife research summaries"},"id":5},{"subject":{"id":70188493,"text":"70188493 - 2002 - Land 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herd","indexId":"70188496","publicationYear":"2002","noYear":false,"chapter":"4","title":"The central arctic caribou herd"},"predicate":"IS_PART_OF","object":{"id":53871,"text":"bsr20020001 - 2002 - Arctic Refuge coastal plain terrestrial wildlife research summaries","indexId":"bsr20020001","publicationYear":"2002","noYear":false,"title":"Arctic Refuge coastal plain terrestrial wildlife research summaries"},"id":8},{"subject":{"id":70188497,"text":"70188497 - 2002 - Muskoxen","indexId":"70188497","publicationYear":"2002","noYear":false,"chapter":"7","title":"Muskoxen"},"predicate":"IS_PART_OF","object":{"id":53871,"text":"bsr20020001 - 2002 - Arctic Refuge coastal plain terrestrial wildlife research summaries","indexId":"bsr20020001","publicationYear":"2002","noYear":false,"title":"Arctic Refuge coastal plain terrestrial wildlife research summaries"},"id":9}],"lastModifiedDate":"2018-05-06T11:01:40","indexId":"bsr20020001","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":9,"text":"Biological Science Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"2002-0001","title":"Arctic Refuge coastal plain terrestrial wildlife research summaries","docAbstract":"

In 1980, when the U.S. Congress enacted the Alaska National Interest Lands Conservation Act (ANILCA), it also mandated a study of the coastal plain of the Arctic National Wildlife Refuge. Section 1002 of ANILCA stated that a comprehensive inventory of fish and wildlife resources would be conducted on 1.5 million acres of the Arctic Refuge coastal plain (1002 Area). Potential petroleum reserves in the 1002 Area were also to be evaluated from surface geological studies and seismic exploration surveys. Results of these studies and recommendations for future management of the Arctic Refuge coastal plain were to be prepared in a report to Congress.

In 1987, the Department of the Interior published the Arctic National Wildlife Refuge, Alaska, Coastal Plain Resource Assessment - Report and Recommendations to the Congress of the United States and Final Environmental Impact Statement. This report to Congress identified the potential for oil and gas production (updated* most recently by the U.S. Geological Survey in 2001), described the biological resources, and evaluated the potential adverse effects to fish and wildlife resources. The 1987 report analyzed the potential environmental consequences of five management alternatives for the coastal plain, ranging from wilderness designation to opening the entire area to lease for oil and gas developement. The report's summary recommended opening the 1002 Area to an orderly oil and gas leasing program, but cautioned that adverse effects to some wildlife populations were possible.

Congress did not act on this recommendation nor any other alternative for the 1002 Area, and scientists continued studies of key wildlife species and habitats on the coastal plain of the Arctic Refuge and surrounding areas. This report contains updated summaries of those scientific investigations of caribou, muskoxen, predators (grizzly bears, wolves, golden eagles), polar bears, snow geese, and their wildlife habitats.

Contributions to this report were made by scientists affiliated with the U.S. Geological Survey; U.S. Fish and Wildlife Service; Alaska Department of Fish and Game; University of Alaska-Fairbanks; Canadian Wildlife Service; Yukon Department of Renewable Resources; and the Northwest Territories Department of Resources, Wildlife, and Economic Development.

Sections of the report presenting new information on caribou and forage plants were peer-reviewed by three independent, non-affiliated scientists. The remaining sections summarize previously published peer-reviewed scientific papers and were reviewed by a single independent scientist. The U.S. Geological Survey and the U.S. Fish and Wildlife Service collaborated in the publication of this report.

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Water resources data for the 2001 water year for New York consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and ground-water levels. This volume contains records for water discharge at 144 gaging stations; stage only at 10 gaging stations; stage and contents at 4 gaging stations, and 18 other lakes and reservoirs; water quality at 34 gaging stations; and water levels at 7 observation wells. Also included are data for 34 crest-stage partial-record stations. Locations of all these sites are shown on figure 8. Additional water data were collected at various sites not involved in the systematic data-collection program, and are published as miscellaneous measurements and analyses. These data together with the data in volumes 2 and 3 represent that part of the National Water Data System operated by the U.S. Geological Survey in cooperation with State, Municipal, and Federal agencies in New York.

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Introduction

The Greater Everglades Ecosystem comprises a vast swath of wetlands beginning in central Florida with the headwaters of the Kissimmee River and continuing southward through Lake Okeechobee and then to Florida Bay (Davis 1943). The ecosystem runs some 450 km, north to south, and over 100 km east to west, comprising almost 30,000 km2 of total area. Beginning in the late 19th century, a succession of programs were implemented for land reclamation and flood protection (Blake 1980; Steinman and others, 2002).

At present, the greater Everglades is the subject of a restoration effort with almost $8 billion dollars of planned expenditures over 20 years. The Comprehensive Everglades Restoration Plan (CERP) sets guidelines and goals for the project. Numerous federal, State of Florida, and local agencies are involved in the restoration process, as are not-for-profit non-governmental organizations. A foundation for Everglades restoration must be a clear understanding of the pre-drainage south Florida landscape (Davis and others, 1994; Fennema 1994). Knowledge of the spatial organization and structure of the pre-drainage landscape communities (mangrove forests, marshes, sloughs, wet prairies, pinelands) is necessary to provide potential endpoints, restoration goals, and performance measures to gauge restoration success.

Analyses of information contained in historical aerial photographs of the Everglades can aid in the endeavor. For example, the earliest known aerial photographs are from the mid-to-late 1920s and resulted in the production of what are called T-sheets (for Topographic Sheets) for the coasts and shorelines of far south Florida. The position of the boundary between differing vegetation communities (the ecotone) can be accurately measured. If followed through time, changes in the position of these ecotones could potentially be used to judge effects of drainage on the Everglades ecosystem and also to monitor restoration success (Smith and others, 2002).

The Florida Integrated Science Center (FISC), a center of the U.S. Geological Survey (USGS), in collaboration with USGS Eastern Region Geography, has created digital versions of existing aerial photographs from a survey conducted in early 1940 of south Florida and the Florida Everglades region. Via this Open-File Report, we make available digital versions of the photographs. We have not attempted to rectify, mosaic, or georeference the images. The aspect of our work will be completed in due course and a supplemental Open-File Report will be issued. At present the digital files are available on this website in a manner designed to facilitate access to the product by those intending to integrate the data with other spatial data, particularly those interested in the restoration and management of the Florida Everglades.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02327","usgsCitation":"Smith, T.J., Foster, A.M., Briere, P.R., Coffin, A.W., Jones, J., Van Arsdall, C., and Frye, L.J., 2002, Historical Aerial Photography for the Greater Everglades of South Florida: The 1940, 1:40,000 Photoset: U.S. Geological Survey Open-File Report 2002-327, https://doi.org/10.3133/ofr02327.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":4160,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0327/index.html","linkFileType":{"id":5,"text":"html"}},{"id":464950,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"contact":"

Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314

Contact Pubs Warehouse

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Water resources data for the 2001 water year for Mississippi consist of records of surface water and ground water in the State. Specifically, it contains: (1) Discharge records for 95 streamflow-gaging stations, stage records for 20 of these gaging stations, discharge records for 83 partial-record or miscellaneous streamflow stations, including 8 flood hydrograph partial-record stations, 70 crest-stage partial-record stations, and 5 special study and miscellaneous sites; (2) stage only at 1 gaging station; (3) water-quality records for 8 streamflow-gaging stations, 0 partial-record or miscellaneous sites, 9 short-term study sites, and 27 wells; and (4) water-level records for 18 observation wells. Records obtained from water-resources investigations are also included in special sections of the report. These data represent that part of the National Water Data System operated by the U.S. Geological Survey, and cooperating local, State, and Federal agencies in Mississippi.

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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb595","contributors":{"authors":[{"text":"Morris, F.","contributorId":17299,"corporation":false,"usgs":true,"family":"Morris","given":"F.","affiliations":[],"preferred":false,"id":251302,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Turnipseed, D.P.","contributorId":59824,"corporation":false,"usgs":true,"family":"Turnipseed","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":251304,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Storm, J.B.","contributorId":51838,"corporation":false,"usgs":true,"family":"Storm","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":251303,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":54681,"text":"wdrMI011 - 2002 - Water resources data, Michigan, water year 2001","interactions":[],"lastModifiedDate":"2017-09-29T08:58:41","indexId":"wdrMI011","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MI-01-1","title":"Water resources data, Michigan, water year 2001","docAbstract":"

Water resources data for the 2001 water year for Michigan consists of records of stage, discharge, and water quality of streams; stage and contents of lakes and reservoirs; and water levels and water quality of ground-water wells. This report contains discharge records for 157 streamflow-gaging stations; stage only records for 2 stream-gaging stations and 25 lake-gaging stations; stage and contents for 1 reservoir; water-quality records for 38 streamflow-gaging stations; and water-level records for 47 ground-water wells. Also included are 30 crest-stage partial-record stations. Additional water data were collected at various sites not involved in the systematic data-collection program. Miscellaneous data were collected at 85 discharge measuring sites and 32 ground water special-study sites. These data represent that part of the National Water Data

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\"}}]}\n","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb6f0","contributors":{"authors":[{"text":"Blumer, S. P.","contributorId":23938,"corporation":false,"usgs":true,"family":"Blumer","given":"S.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":251141,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Behrendt, T.E.","contributorId":27887,"corporation":false,"usgs":true,"family":"Behrendt","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":251142,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ellis, J.M.","contributorId":29502,"corporation":false,"usgs":true,"family":"Ellis","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":251143,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Minnerick, R. J.","contributorId":52255,"corporation":false,"usgs":true,"family":"Minnerick","given":"R. J.","affiliations":[],"preferred":false,"id":251144,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"LeuVoy, R.L.","contributorId":56706,"corporation":false,"usgs":true,"family":"LeuVoy","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":251145,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":44878,"text":"wri20014275 - 2002 - Design of a real-time ground-water level monitoring network and portrayal of hydrologic data in southern Florida","interactions":[],"lastModifiedDate":"2020-11-24T14:54:35.187585","indexId":"wri20014275","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2001-4275","title":"Design of a real-time ground-water level monitoring network and portrayal of hydrologic data in southern Florida","docAbstract":"

Ground-water resources in southern Florida are under increasing stress caused a rapid growth in population. As a result of increased demands on aquifers, water managers need more timely and accurate assessments of ground-water conditions in order to avoid or reduce adverse effects such as saltwater intrusion, loss of pumpage in residential water-supply wells, land-surface subsidence, and aquifer compaction.

Hydrologic data were analyzed from three aquifer systems in southern Florida: the surficial aquifer system, which includes the Biscayne aquifer; the intermediate aquifer system, which includes the sandstone and mid-Hawthorn aquifers; and the Florida aquifer system represented by the lower Hawthorn producing zone. Long-term water-level trends were analyzed using the Seasonal Kendall trend test in 83 monitoring wells with a daily-value record spanning 26 years (1974-99). The majority of the wells with data for this period were in the Biscayne aquifer in southeastern Florida. Only 14 wells in southwestern Florida aquifers and 9 in the surficial aquifer system of Martin and Palm Beach Counties had data for the full period. Because many monitoring wells did not have data for this full period, several shorter periods were evaluated as well. The trend tests revealed small but statistically significant upward trends in most aquifers, but large and localized downward trends in the sandstone and mid-Hawthorn aquifers.

Monthly means of maximum daily water levels from 246 wells were compared to monthly rainfall totals from rainfall stations in southwestern and southeastern Florida in order to determine which monitoring wells most clearly indicated decreases in water levels that corresponded to prolonged rainfall shortages. Of this total, 104 wells had periods of record over 20 years and could be compared against several drought periods. After factors such as lag, seasonal cyclicity, and cumulative functions were considered, the timing of minimum values of water level from 15 ground-water monitoring wells and average minimum rainfall values agreed 57 to 62 percent of the time over a 20 to 26 year period. On average, the timing of water-level minimums and rainfall minimums agreed about 52 percent of the time, and in some cases only agreed 29 percent of the time.

A regression analysis was used to evaluate daily water levels from 203 monitoring wells that are currently, or recently had been, part of the network to determine which wells were most representative of each aquifer. The regression also was used to determine which wells provided data that could be used to provide estimations of water levels at other wells in the aquifer with a coefficient of determination (R2 value) from the regression of 0.64 or greater. In all, the regression analysis alone indicated that 35 wells generally had 10 years or more of data and could be used to directly monitor water levels or to estimate water levels at 180 of 203 wells (89 percent of the network). Ultimately, factors such as existing instrumentation, well construction, long-term water-level trends, and variations of water level and chloride concentration were considered together with the R2 results in designing the final network.

The Seasonal Kendall trend test was used to examine trends in ground-water chloride concentrations in 113 wells. Of these wells, 61 showed statistically significant trends. Fifty-six percent (34 of 61 wells) of the observed trends in chloride concentration were upward and 44 percent (27 of 61 wells) were downward. The relation between water level and chloride concentration in 114 ground-water wells was examined using Spearman's r and Pearson's r correlation coefficients. Statistically significant results showed both positive and negative relations. Based on the results of statistical analyses, period of record, well construction, and existing satellite telemetry, 33 monitoring wells were selected that could be used to assess ground-water conditions in 167 monitoring wells in southern Florida on an interim basis.

A real-time ground-water level monitoring network (http://www.sflorida.er.usgs.gov/ddn_data/index.html) was designed to provide this information, and a prototype website was constructed to provide water managers with daily updates on ground-water conditions in southern Florida. Many of the same analytical tools used to select monitoring wells representative of aquifer conditions are also employed to analyze data for this website. These tools include regression analysis, the Seasonal Kendall trend test, and frequency analysis. The website also includes image maps showing the current conditions for stations in selected geographical areas and aquifers and statistical comparison plots for each station.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri20014275","usgsCitation":"Prinos, S.T., Lietz, A., and Irvin, R., 2002, Design of a real-time ground-water level monitoring network and portrayal of hydrologic data in southern Florida: U.S. Geological Survey Water-Resources Investigations Report 2001-4275, vi, 108 p., https://doi.org/10.3133/wri20014275.","productDescription":"vi, 108 p.","costCenters":[],"links":[{"id":134789,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":380743,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://permanent.fdlp.gov/lps100464/fl.water.usgs.gov/PDF_files/wri01_4275_prinos.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.254638671875,\n 25.085598897064752\n ],\n [\n -80.0244140625,\n 25.085598897064752\n ],\n [\n -80.0244140625,\n 27.581329075043357\n ],\n [\n -82.254638671875,\n 27.581329075043357\n ],\n [\n -82.254638671875,\n 25.085598897064752\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667e25","contributors":{"authors":[{"text":"Prinos, Scott T. 0000-0002-5776-8956 stprinos@usgs.gov","orcid":"https://orcid.org/0000-0002-5776-8956","contributorId":4045,"corporation":false,"usgs":true,"family":"Prinos","given":"Scott","email":"stprinos@usgs.gov","middleInitial":"T.","affiliations":[{"id":269,"text":"FLWSC-Ft. Lauderdale","active":true,"usgs":true},{"id":156,"text":"Caribbean Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230602,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lietz, A.C.","contributorId":40957,"corporation":false,"usgs":true,"family":"Lietz","given":"A.C.","email":"","affiliations":[],"preferred":false,"id":230604,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Irvin, R.B.","contributorId":10014,"corporation":false,"usgs":true,"family":"Irvin","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":230603,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":50654,"text":"ofr02241 - 2002 - Preliminary data used in estimating ground-water recharge, pumpage, and evapotranspiration in part of the Republican River Basin, Nebraska, Kansas, and Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:10:25","indexId":"ofr02241","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-241","title":"Preliminary data used in estimating ground-water recharge, pumpage, and evapotranspiration in part of the Republican River Basin, Nebraska, Kansas, and Colorado","language":"ENGLISH","doi":"10.3133/ofr02241","usgsCitation":"Johnson, M., and Landon, M.K., 2002, Preliminary data used in estimating ground-water recharge, pumpage, and evapotranspiration in part of the Republican River Basin, Nebraska, Kansas, and Colorado: U.S. Geological Survey Open-File Report 2002-241, 42 p. plus electronic files, https://doi.org/10.3133/ofr02241.","productDescription":"42 p. plus electronic files","costCenters":[],"links":[{"id":169894,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c686","contributors":{"authors":[{"text":"Johnson, Michaela R. 0000-0001-6133-0247 mrjohns@usgs.gov","orcid":"https://orcid.org/0000-0001-6133-0247","contributorId":1013,"corporation":false,"usgs":true,"family":"Johnson","given":"Michaela R.","email":"mrjohns@usgs.gov","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true},{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":242013,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Landon, Matthew K. 0000-0002-5766-0494 landon@usgs.gov","orcid":"https://orcid.org/0000-0002-5766-0494","contributorId":392,"corporation":false,"usgs":true,"family":"Landon","given":"Matthew","email":"landon@usgs.gov","middleInitial":"K.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":242012,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":54876,"text":"wdrOH011 - 2002 - Water resources data, Ohio, water year 2001, volume 1. Ohio River Basin excluding project data","interactions":[],"lastModifiedDate":"2019-05-21T16:17:20","indexId":"wdrOH011","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"OH–01–1","displayTitle":"Water Resources Data, Ohio, Water Year 2001, Volume 1. Ohio River Basin Excluding Project Data","title":"Water resources data, Ohio, water year 2001, volume 1. Ohio River Basin excluding project data","docAbstract":"Water-resources data for the 2001 water year for Ohio consist of records of stage, discharge, and water quality of streams; stage\r\nand contents of lakes and reservoirs; and water levels and water quality of ground-water wells. This report, in two volumes,\r\ncontains records for water discharge at 130 gaging stations and 65 partial-record sites; water levels at 160 observation wells and\r\n25 crest-stage gages; and water quality at 25 gaging stations, 31 observation wells, and 9 partial-record sites. Also included are\r\ndata from miscellaneous and synoptic sites. Additional water data were collected at various sites not involved in the systematic\r\ndata-collection program and are published as miscellaneous measurements and analyses. These data represent that part of the\r\nNational Water Information System collected by the U.S. Geological Survey and cooperating Federal, State, and local agencies\r\nin Ohio.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrOH011","collaboration":"Prepared in cooperation with the State of Ohio and with other agencies","usgsCitation":"Shindel, H., Mangus, J., and Trimble, L., 2002, Water resources data, Ohio, water year 2001, volume 1. 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\"}}]}","contact":"

Director, Ohio Water Science Center
U.S. Geological Survey
6460 Busch Blvd.
Columbus, OH 43229-1737

","tableOfContents":"","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faeda","contributors":{"authors":[{"text":"Shindel, H.L.","contributorId":17652,"corporation":false,"usgs":true,"family":"Shindel","given":"H.L.","affiliations":[],"preferred":false,"id":251857,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mangus, J.P.","contributorId":28301,"corporation":false,"usgs":true,"family":"Mangus","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":251858,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Trimble, L.E.","contributorId":101732,"corporation":false,"usgs":true,"family":"Trimble","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":251859,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":54734,"text":"wdrMT011 - 2002 - Water resources data, Montana, water year 2001","interactions":[],"lastModifiedDate":"2023-02-08T00:21:30.357233","indexId":"wdrMT011","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"MT-01-1","title":"Water resources data, Montana, water year 2001","docAbstract":"

The U.S. Geological Survey (USGS), in cooperation with other Federal, State, and local agencies, and Tribal governments, collects a large amount of data pertaining to the water resources of Montana each water year. These data, accumulated over many years, constitute a valuable data base for developing an improved understanding of the water resources of the State. To make these data readily available to interested parties outside the USGS, the data are published annually, by water year, in this report series entitled, \"Water Resources Data, Montana.\"

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMT011","collaboration":"Prepared in cooperation with the State of Montana and with other agencies","usgsCitation":"Shields, R., White, M.K., Ladd, P., Chambers, C.L., and Dodge, K.A., 2002, Water resources data, Montana, water year 2001: U.S. Geological Survey Water Data Report MT-01-1, xii, 671 p., https://doi.org/10.3133/wdrMT011.","productDescription":"xii, 671 p.","costCenters":[],"links":[{"id":181815,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/2001/mt-01-1/report-thumb.jpg"},{"id":412837,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/2001/mt-01-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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A.","contributorId":40615,"corporation":false,"usgs":true,"family":"Dodge","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":251347,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":47810,"text":"fs14202 - 2002 - Earth Observing-1 Extended Mission Cooperative Project","interactions":[],"lastModifiedDate":"2012-02-02T00:10:40","indexId":"fs14202","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"142-02","title":"Earth Observing-1 Extended Mission Cooperative Project","language":"ENGLISH","doi":"10.3133/fs14202","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2002, Earth Observing-1 Extended Mission Cooperative Project: U.S. Geological Survey Fact Sheet 142-02, 2 p., https://doi.org/10.3133/fs14202.","productDescription":"2 p.","costCenters":[],"links":[{"id":4022,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://erg.usgs.gov/isb/pubs/factsheets/fs03203.html","linkFileType":{"id":5,"text":"html"}},{"id":173327,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c214","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":531763,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":69760,"text":"i2698B - 2002 - Sun-Illuminated Sea Floor Topography of Quadrangle 1 in the Great South Channel, Western Georges Bank","interactions":[],"lastModifiedDate":"2014-08-29T15:09:16","indexId":"i2698B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2698","subseriesTitle":"GIS","chapter":"B","title":"Sun-Illuminated Sea Floor Topography of Quadrangle 1 in the Great South Channel, Western Georges Bank","docAbstract":"The Great South Channel separates the western part of Georges Bank from Nantucket Shoals and is a major conduit for the exchange of water between the Gulf of Maine to the north and the Atlantic Ocean to the south. Water depths range mostly between 65 and 80 m in the region. A minimum depth of 45 m occurs in the east-central part of the mapped area, and a maximum depth of 100 m occurs in the northwest corner. The channel region is characterized by strong tidal and storm currents that flow dominantly north and south. Major topographic features of the seabed were formed by glacial and postglacial processes. Ice containing rock debris moved from north to south, sculpting the region into a broad shallow depression and depositing sediment to form the irregular depressions and low gravelly mounds and ridges that are visible in parts of the mapped area. Many other smaller glacial featuresprobably have been eroded by waves and currents at worksince the time when the region, formerly exposed bylowered sea level or occupied by ice, was invaded by the sea. The low, irregular and somewhat lumpy fabric formed by the glacial deposits is obscured in places by drifting sand and by the linear, sharp fabric formed by modern sand features. Today, sand transported by the strong north-south-flowing tidal and storm currents has formed large, east-west-trending dunes. These bedforms (ranging between 5 and 20 m in height) contrast strongly with, and partly mask, the subdued topography of the older glacial features.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Maps Showing Sea Floor Topography, Sun-Illuminated Sea Floor Topography, and Backscatter Intensity of Quadrangles 1 and 2 in the Great South Channel Region, Western Georges Bank","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/i2698B","isbn":"0607998253","collaboration":"Prepared in cooperation with the U.S. National Oceanic and Atmospheric Administration","usgsCitation":"Valentine, P.C., Middleton, T.J., and Malczyk, J.T., 2002, Sun-Illuminated Sea Floor Topography of Quadrangle 1 in the Great South Channel, Western Georges Bank (Version 1.0): U.S. Geological Survey IMAP 2698, 1 Sheet: 39 x 39 inches; Also available on CD-ROM, https://doi.org/10.3133/i2698B.","productDescription":"1 Sheet: 39 x 39 inches; Also available on CD-ROM","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":191099,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9789,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i2698/index.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"25000","projection":"Universal Transverse Mercator","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -69.05,40.09 ], [ -69.05,41.016667 ], [ -68.783333,41.016667 ], [ -68.783333,40.09 ], [ -69.05,40.09 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697bee","contributors":{"authors":[{"text":"Valentine, Page C. 0000-0002-0485-6266 pvalentine@usgs.gov","orcid":"https://orcid.org/0000-0002-0485-6266","contributorId":1947,"corporation":false,"usgs":true,"family":"Valentine","given":"Page","email":"pvalentine@usgs.gov","middleInitial":"C.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":281215,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Middleton, Tammie J.","contributorId":27532,"corporation":false,"usgs":true,"family":"Middleton","given":"Tammie","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":281217,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Malczyk, Jeremy T.","contributorId":10106,"corporation":false,"usgs":true,"family":"Malczyk","given":"Jeremy","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":281216,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":47802,"text":"fs12502 - 2002 - Assessing rangelands","interactions":[],"lastModifiedDate":"2017-03-31T11:49:38","indexId":"fs12502","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"125-02","title":"Assessing rangelands","docAbstract":"It is important for land managers and technical assistance specialists to be able to assess the health of rangelands in order to know where to focus management efforts. The complexity of ecological processes, and the inherent expense of directly measuring site integrity, suggests a need for an evaluation process that focuses instead on biological and physical attributes.\r\n\r\nIn a collaborative effort, the USGS, ARS, BLM, and NRCS have jointly developed a system in which 17 indicators are used to gauge three attributes of rangeland health. A qualitative, observational procedure provides an assessment of the functional status of these indicators. This quick assessment technique, by providing an understanding about each attribute, helps interpret rangeland health.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs12502","usgsCitation":"Pyke, D.A., 2002, Assessing rangelands: U.S. Geological Survey Fact Sheet 125-02, 2 p., https://doi.org/10.3133/fs12502.","productDescription":"2 p.","onlineOnly":"Y","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":4014,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2002/0125/fs12502.pdf","text":"Report","size":"692 KB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 125-02"},{"id":120206,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2002/0125/coverthb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672aa7","contributors":{"authors":[{"text":"Pyke, David A. 0000-0002-4578-8335 david_a_pyke@usgs.gov","orcid":"https://orcid.org/0000-0002-4578-8335","contributorId":3118,"corporation":false,"usgs":true,"family":"Pyke","given":"David","email":"david_a_pyke@usgs.gov","middleInitial":"A.","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":true,"id":236270,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52911,"text":"wri014024 - 2002 - Nitrogen and Phosphorus Concentrations and Fluxes of Streams in the Mississippi Embayment Study Unit, 1996-98","interactions":[],"lastModifiedDate":"2012-02-02T00:11:41","indexId":"wri014024","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2001-4024","title":"Nitrogen and Phosphorus Concentrations and Fluxes of Streams in the Mississippi Embayment Study Unit, 1996-98","language":"ENGLISH","doi":"10.3133/wri014024","usgsCitation":"Coupe, R., 2002, Nitrogen and Phosphorus Concentrations and Fluxes of Streams in the Mississippi Embayment Study Unit, 1996-98: U.S. Geological Survey Water-Resources Investigations Report 2001-4024, 65 p., https://doi.org/10.3133/wri014024.","productDescription":"65 p.","costCenters":[],"links":[{"id":247765,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2001/4024/report.pdf","size":"10894","linkFileType":{"id":1,"text":"pdf"}},{"id":252110,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2001/4024/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697294","contributors":{"authors":[{"text":"Coupe, R.H. Jr.","contributorId":84755,"corporation":false,"usgs":true,"family":"Coupe","given":"R.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":246214,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":47803,"text":"fs12602 - 2002 - Born of fire - restoring sagebrush steppe","interactions":[],"lastModifiedDate":"2017-03-31T11:48:22","indexId":"fs12602","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"126-02","title":"Born of fire - restoring sagebrush steppe","docAbstract":"Fire is a natural feature of sagebrush grasslands in the Great Basin. The invasion of exotic annual grasses, such as Bromus tectorum (cheatgrass), has changed the environment in these ecosystems. Invasive annual grasses provide a dense and continuous source of fuel that extends the season for fires and increases the frequency of fires in the region. Frequent fires eventually eliminate the native sagebrush. These annual grasses also change soil nutrients, especially carbon and nitrogen, such that invasive annual grasses are favored over the native plants. The Forest and Rangeland Ecosystem Science Center of the U.S. Geological Survey (USGS) is studying how to reduce the problems caused by these invasive annual grasses and restore native sagebrush grasslands. The areas of research include understanding disturbance regimes, especially fire, discerning the role of nutrients in restoring native plants, determining the potential to restore forbs important for wildlife, and ascertaining the past and present use of native and nonnative plants in revegetation projects.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs12602","usgsCitation":"Pyke, D.A., 2002, Born of fire - restoring sagebrush steppe: U.S. Geological Survey Fact Sheet 126-02, 2 p., https://doi.org/10.3133/fs12602.","productDescription":"2 p.","onlineOnly":"Y","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":125708,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2002/0126/coverthb.jpg"},{"id":4015,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2002/0126/fs12602.pdf","text":"Report","size":"665 KB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 126-02"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc6ba","contributors":{"authors":[{"text":"Pyke, David A. 0000-0002-4578-8335 david_a_pyke@usgs.gov","orcid":"https://orcid.org/0000-0002-4578-8335","contributorId":3118,"corporation":false,"usgs":true,"family":"Pyke","given":"David","email":"david_a_pyke@usgs.gov","middleInitial":"A.","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":true,"id":236271,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44940,"text":"wri024202 - 2002 - Hydrology and chemistry of floodwaters in the Yolo Bypass, Sacramento River system, California, during 2000","interactions":[],"lastModifiedDate":"2020-02-18T19:52:55","indexId":"wri024202","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-4202","title":"Hydrology and chemistry of floodwaters in the Yolo Bypass, Sacramento River system, California, during 2000","docAbstract":"

Discharges to and floodwaters in the Yolo Bypass were sampled during winter and spring, 2000. The primary purpose of the study was to link changes in water quality in the Yolo Bypass to inflows from the Sacramento River (over Fremont Weir) and from four local streams that discharge to the west side of the floodplain. Specific conductance, chloride, sulfate, dissolved inorganic nutrients, dissolved organic carbon, particulate carbon and nitrogen, suspended particulate matter (mass), and selected dissolved metals were measured in most of the samples. When the Sacramento River was spilling over Fremont Weir, the water chemistry in the Yolo Bypass was very similar to that in the river except along the western margin of the floodplain where influences of local stream inflow were evident. When flow over Fremont Weir stopped, floodwaters drained from the Yolo Bypass, and the local streams were the major discharges as the floodwaters receded eventually to the perennial channel along the eastern margin of the floodplain. After the initial draining of the floodplain, chemical concentrations at sites along the perennial channel showed strong influences of inflows from Cache Creek and Ridge Cut, which are sources of nutrients and contaminants that are potentially hazardous to wildlife. Runoff from spring storms increased flow in the perennial channel and flushed accumulated nutrients and organic matter to the tidal river. Releases of freshwater to the perennial channel might be beneficial in maintaining habitat quality for aquatic species during the dry seasons.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri024202","usgsCitation":"Schemel, L.E., Cox, M.H., Hager, S.W., and Sommer, T.R., 2002, Hydrology and chemistry of floodwaters in the Yolo Bypass, Sacramento River system, California, during 2000: U.S. Geological Survey Water-Resources Investigations Report 2002-4202, 71 p., https://doi.org/10.3133/wri024202.","productDescription":"71 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":135172,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3815,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024202","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","otherGeospatial":"Yolo Bypass","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.69692993164062,\n 38.23494411562881\n ],\n [\n -121.54586791992188,\n 38.23494411562881\n ],\n [\n -121.54586791992188,\n 38.78941577989049\n ],\n [\n -121.69692993164062,\n 38.78941577989049\n ],\n [\n -121.69692993164062,\n 38.23494411562881\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688486","contributors":{"authors":[{"text":"Schemel, Laurence E. lschemel@usgs.gov","contributorId":4085,"corporation":false,"usgs":true,"family":"Schemel","given":"Laurence","email":"lschemel@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":230726,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cox, Marisa H.","contributorId":52146,"corporation":false,"usgs":true,"family":"Cox","given":"Marisa","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":230729,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hager, Stephen W.","contributorId":48935,"corporation":false,"usgs":true,"family":"Hager","given":"Stephen","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":230728,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sommer, Theodore R.","contributorId":41396,"corporation":false,"usgs":true,"family":"Sommer","given":"Theodore","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":230727,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":55143,"text":"wdrKY011 - 2002 - Water Resources Data, Kentucky, Water Year 2001","interactions":[],"lastModifiedDate":"2012-02-02T00:11:54","indexId":"wdrKY011","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"KY-01-1","title":"Water Resources Data, Kentucky, Water Year 2001","docAbstract":"Water resources data for the 2001 water year for Kentucky consist of records of stage, discharge, and water quality of streams and lakes; and water levels of wells. This report includes daily discharge records for 120 streamgaging stations. It also includes water-quality data for eight stations sampled at regular intervals, continuous temperature at four stations, and continuous water quality at eight stations. Ground-water levels are published for 7 recording and 23 partial-record sites. Precipitation data at regular intervals are published for one site. Additional water data were collected at various sites not involved in the systematic data-collection program and are published as miscellaneous measurement and analyses. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Kentucky.","language":"ENGLISH","doi":"10.3133/wdrKY011","usgsCitation":"McClain, D., Byrd, F., and Brown, A., 2002, Water Resources Data, Kentucky, Water Year 2001: U.S. Geological Survey Water Data Report KY-01-1, 550 p., https://doi.org/10.3133/wdrKY011.","productDescription":"550 p.","costCenters":[],"links":[{"id":5338,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://ky.water.usgs.gov/pubs/default.htm","linkFileType":{"id":5,"text":"html"}},{"id":174207,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb7c5","contributors":{"authors":[{"text":"McClain, D.L.","contributorId":72402,"corporation":false,"usgs":true,"family":"McClain","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":252777,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Byrd, F.D.","contributorId":25227,"corporation":false,"usgs":true,"family":"Byrd","given":"F.D.","email":"","affiliations":[],"preferred":false,"id":252775,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, A.C.","contributorId":30276,"corporation":false,"usgs":true,"family":"Brown","given":"A.C.","email":"","affiliations":[],"preferred":false,"id":252776,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":44983,"text":"wri024103 - 2002 - Diazinon and chlorpyrifos loads in the San Joaquin River basin, California, January and February 2000","interactions":[],"lastModifiedDate":"2012-02-02T00:10:12","indexId":"wri024103","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-4103","title":"Diazinon and chlorpyrifos loads in the San Joaquin River basin, California, January and February 2000","docAbstract":"The application of diazinon and chlorpyrifos on dormant orchards in 2000 in the San Joaquin River Basin was less than 21 percent of application in 1993 and 1994. A total of 13 sites were sampled weekly during nonstorm periods and more frequently during two storm periods. The sites included five major river and eight minor tributary sites. The highest concentrations of diazinon and chlorpyrifos occurred during the storm periods. Four samples from major river sites (Tuolumne River and two San Joaquin River sites) had diazinon concentrations greater than 0.08 microgram per liter, the concentration being considered by the state of California as its criterion maximum concentration for the protection of aquatic habitat. One sample from a major river site (San Joaquin River) exceeded the equivalent State guideline of 0.02 microgram per liter for chlorpyrifos. At the eight minor tributary sites, 24 samples exceeded the diazinon guideline and four samples exceeded the chlorpyrifos guideline. The total diazinon load in the San Joaquin River near Vernalis during January and February 2000 was 19.6 pounds active ingredient; of this, 8.17 pounds active ingredient was transported during two storms. In 1994, 27.4 pounds active ingredient was transported during two storms. The total chlorpyrifos load in the San Joaquin River near Vernalis during January and February 2000 was 5.68 pounds active ingredient; of this, 2.17 pounds active ingredient was transported during the two storms. During the frequently sampled February 2000 storm, the main sources of diazinon in the San Joaquin River Basin were the San Joaquin River near Stevinson Basin (25 percent), Tuolumne River Basin (14 percent), and the Stanislaus River Basin (10 percent). The main sources of chlorpyrifos in the San Joaquin River Basin were the San Joaquin River near Stevinson Basin (17 percent), Tuolumne River Basin (13 percent), and the Merced River Basin (11 percent). The total January and February diazinon load in the San Joaquin River near Vernalis was 0.17 percent of dormant application; total January and February chlorpyrifos load was 0.16 percent of dormant application.","language":"ENGLISH","doi":"10.3133/wri024103","usgsCitation":"Kratzer, C.R., Zamora, C., and Knifong, D.L., 2002, Diazinon and chlorpyrifos loads in the San Joaquin River basin, California, January and February 2000: U.S. Geological Survey Water-Resources Investigations Report 2002-4103, 45 p., https://doi.org/10.3133/wri024103.","productDescription":"45 p.","costCenters":[],"links":[{"id":161721,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3858,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri02-4103","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcc59","contributors":{"authors":[{"text":"Kratzer, Charles R.","contributorId":30619,"corporation":false,"usgs":true,"family":"Kratzer","given":"Charles","email":"","middleInitial":"R.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":230837,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zamora, Celia 0000-0003-1456-4360 czamora@usgs.gov","orcid":"https://orcid.org/0000-0003-1456-4360","contributorId":1514,"corporation":false,"usgs":true,"family":"Zamora","given":"Celia","email":"czamora@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true}],"preferred":true,"id":230835,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Knifong, Donna L. dknifong@usgs.gov","contributorId":1517,"corporation":false,"usgs":true,"family":"Knifong","given":"Donna","email":"dknifong@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":230836,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":44975,"text":"wri024075 - 2002 - Ground-water levels in the Floridan-Midville aquifer in the Breezy Hill area, Aiken and Edgefield Counties, South Carolina, April 1999-November 2000","interactions":[],"lastModifiedDate":"2023-01-11T20:40:17.522486","indexId":"wri024075","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-4075","title":"Ground-water levels in the Floridan-Midville aquifer in the Breezy Hill area, Aiken and Edgefield Counties, South Carolina, April 1999-November 2000","docAbstract":"

The Breezy Hill area in Aiken and Edgefield Counties of west-central South Carolina is a rapidly growing region in need of increasing amounts of ground water. From 1995 to 1998, the local water utility increased ground-water withdrawals in the Breezy Hill area from 1.4 to 2.1 million gallons per day to meet water-supply demands. As development continues, future demands for ground water will likely put stress on the surfaceand ground-water resources of the area. To address this issue, the U.S. Geological Survey, in cooperation with Aiken County, compiled and interpreted geologic and hydrologic data needed to map the ground-water system in the Breezy Hill study area.

The Breezy Hill study area consists of four interfluvial areas comprising the regions between Horse and Little Horse Creeks, Little Horse and Hightower Creeks, Hightower Creek and Franklin Branch, and Franklin Branch and Mims Branch. Across the interfluvial areas, the average elevation of the water-level surface ranged from 200 to 480 feet above sea level, and the average saturated thickness of the Floridan-Midville aquifer ranged from less than 20 to 70 feet thick. A water-level contour map of the surface of the Floridan-Midville aquifer indicates that recharge to the aquifer occurs mainly within the interfluves. Recharge is derived principally from precipitation, although there is some potential for ground-water recharge from underlying crystalline rocks. Ground water discharges along the flanks of the interfluves into the bounding streams where the elevations of the ground water and streams coincide.

From April 1999 to November 2000, calculated long-term normal precipitation totaled about 84.0 inches; however, actual recorded precipitation totaled 69.2 inches, representing about a 17.6 percent decrease in precipitation during this period. Published estimates of annual evapotranspiration range from 30 to 35 inches.

A U.S. Geological Survey surface-water gaging station located near the center of the study area on Little Horse Creek monitors runoff from a drainage area of 26.6 square miles. Average annual flow for the station for water years 1990-2000 was 33.8 cubic feet per second. From April 1999 to November 2000, the monthly average flow was less than the average monthly flow for the longterm record, excluding December 1999 to March 2000 when no data were collected. Monthly average flow for Little Horse Creek exceeded the normal monthly flow during June and July 1999.

Ground water in the Breezy Hill area is principally withdrawn from the unconfined Floridan- Midville aquifer. Ground-water withdrawals by the local water utility increased 37 percent from 1989 to 2000 (315.2 to 500 million gallons, respectively). From January 1999 to December 2000, the utility exceeded the long-term monthly average groundwater withdrawals for every month except September and December 2000. Calculated long-term monthly ground-water withdrawals by the utility for a 20-month period from April 1999 to November 2000 totaled 674 million gallons; however, actual ground-water withdrawals totaled 883 million gallons, which is 31 percent more than the long-term average ground-water withdrawals for the production wells.

Published estimates of average annual ground-water recharge rates for the study area range from 13 to 15 inches per year. A base-flow recession analysis of streamflow data for Little Horse Creek provided an estimated recharge rate of 14.9 inches per year for the drainage area. Using an estimated average porosity ranging from 30 to 35 percent observed in sand-aquifer cores, the average annual recharge of 13 to 15 inches would cause a 3.6- to 4.1-foot water-level change to the saturated thickness of the aquifer, if applied instantaneously. The water-level declines observed in wells from April 1999 to November 2000 approximated an average decline of 4 feet.

From November 1999 to November 2000, ground-water levels in six wells near utility pumping centers declined 2 to 5 feet. Long-term waterlevel declines of 10.27 and 11.50 feet were measured in two wells between May 1992 and April 2000, respectively.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri024075","usgsCitation":"Harrelson, L.G., Falls, W.F., and Prowell, D.C., 2002, Ground-water levels in the Floridan-Midville aquifer in the Breezy Hill area, Aiken and Edgefield Counties, South Carolina, April 1999-November 2000: U.S. Geological Survey Water-Resources Investigations Report 2002-4075, iv, 36 p., https://doi.org/10.3133/wri024075.","productDescription":"iv, 36 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":162173,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":411738,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51833.htm","linkFileType":{"id":5,"text":"html"}},{"id":3848,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024075/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"South Carolina","county":"Aiken County, Edgefield County","otherGeospatial":"Floridan-Midville aquifer","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -81.9542,\n 33.6583\n ],\n [\n -81.9542,\n 33.48\n ],\n [\n -81.7747,\n 33.48\n ],\n [\n -81.7747,\n 33.6583\n ],\n [\n -81.9542,\n 33.6583\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667573","contributors":{"authors":[{"text":"Harrelson, Larry G.","contributorId":70059,"corporation":false,"usgs":true,"family":"Harrelson","given":"Larry","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":230813,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Falls, W. Fred 0000-0003-2928-9795 wffalls@usgs.gov","orcid":"https://orcid.org/0000-0003-2928-9795","contributorId":107754,"corporation":false,"usgs":true,"family":"Falls","given":"W.","email":"wffalls@usgs.gov","middleInitial":"Fred","affiliations":[],"preferred":false,"id":230814,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Prowell, David C.","contributorId":46956,"corporation":false,"usgs":true,"family":"Prowell","given":"David","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":230812,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":44978,"text":"wri024093 - 2002 - Characterization and analysis of temporal and spatial variations in habitat and macroinvertebrate community structure, Fountain Creek basin, Colorado Springs and vicinity, Colorado, 1998-2001","interactions":[],"lastModifiedDate":"2012-02-02T00:10:12","indexId":"wri024093","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-4093","title":"Characterization and analysis of temporal and spatial variations in habitat and macroinvertebrate community structure, Fountain Creek basin, Colorado Springs and vicinity, Colorado, 1998-2001","docAbstract":"The Fountain Creek Basin in and around Colorado Springs, Colorado, is affected by various land- and water-use activities. Biological, hydrological, water-quality, and land-use data were collected at 10 sites in the Fountain Creek Basin from April 1998 through April 2001 to provide a baseline characterization of macroinvertebrate communities and habitat conditions for comparison in subsequent studies; and to assess variation in macroinvertebrate community structure relative to habitat quality. Analysis of variance results indicated that instream and riparian variables were not affected by season, but significant differences were found among sites. Nine metrics were used to describe and evaluate macroinvertebrate community structure. Statistical analysis indicated that for six of the nine metrics, significant variability occurred between spring and fall seasons for 60 percent of the sites. Cluster analysis (unweighted pair group method average) using macroinvertebrate presence-absence data showed a well-defined separation between spring and fall samples. Six of the nine metrics had significant spatial variation. Cluster analysis using Sorenson?s Coefficient of Community values computed from macroinvertebrate density (number of organisms per square meter) data showed that macroinvertebrate community structure was more similar among tributary sites than main-stem sites. Canonical correspondence analysis identified a substrate particle-size gradient from site-specific species-abundance data and environmental correlates that decreased the 10 sites to 5 site clusters and their associated taxa.","language":"ENGLISH","doi":"10.3133/wri024093","usgsCitation":"Bruce, J.F., 2002, Characterization and analysis of temporal and spatial variations in habitat and macroinvertebrate community structure, Fountain Creek basin, Colorado Springs and vicinity, Colorado, 1998-2001: U.S. Geological Survey Water-Resources Investigations Report 2002-4093, 1 v., 28 p. : col. ill., col. map ; 28 cm., https://doi.org/10.3133/wri024093.","productDescription":"1 v., 28 p. : col. ill., col. map ; 28 cm.","costCenters":[],"links":[{"id":3851,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024093/","linkFileType":{"id":5,"text":"html"}},{"id":162267,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3624","contributors":{"authors":[{"text":"Bruce, James F. 0000-0003-3125-2932 jbruce@usgs.gov","orcid":"https://orcid.org/0000-0003-3125-2932","contributorId":916,"corporation":false,"usgs":true,"family":"Bruce","given":"James","email":"jbruce@usgs.gov","middleInitial":"F.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":false,"id":230820,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44974,"text":"wri024061 - 2002 - Report of hydrologic investigations in the Three Sisters area of central Oregon, Summer 2001","interactions":[],"lastModifiedDate":"2012-02-02T00:10:12","indexId":"wri024061","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-4061","title":"Report of hydrologic investigations in the Three Sisters area of central Oregon, Summer 2001","docAbstract":"An ongoing episode of crustal uplift centered in the Separation Creek drainage of the Three Sisters area, central Oregon Cascades, may result from a magmatic intrusion that began in 1998. An investigation of springs in this drainage in summer 2001 revealed slightly elevated water temperatures and chloride (Cl-) concentrations of up to about 5?C and 20 milligrams per liter (mg/L), respectively, above background. The total discharge of anomalous Cl- in Separation Creek was 9.2 grams per second, which in combination with the temperature-Cl- relation in the springs results in a total advective heat discharge of 16 MW (megawatts). Comparison with similar findings obtained a decade earlier suggests that total Cl- and heat discharges in the groundwater drainage are unaffected by the current uplift. However, the isotopic composition of the dissolved inorganic carbon (DIC) in the spring waters (delta carbon-13 (13C) = -9.03 to -11.6?; carbon-14 (14C) <25 pmC) combined with helium-3/helium-4 (3He/4He) ratios near 8 RA and C/3He ratios <1010 in two of the springs are indicative of a magmatic source. The high 3He/4He ratios indicate that the magmatic gas is derived from a relatively recent, if not ongoing, intrusion. The concentration of magmatic carbon is low, a few millimoles per liter (mmol/L) at most, with an average value of 1.53 mmol/L for all the springs sampled in the drainage. Combining this average with the late-summer water flow in Separation Creek suggests a discharge of 21 tonnes/day of magmatic carbon dioxide (CO2). The presence of magmatic carbon in the shallow groundwater system, and the fact that DIC is uncorrelated with Cl-, suggests that some magmatic gas could escape diffusely through the soils.","language":"ENGLISH","doi":"10.3133/wri024061","usgsCitation":"Evans, W.C., Mariner, R.H., Ingebritsen, S.E., Kennedy, B.M., van Soest, M.C., and Huebner, M., 2002, Report of hydrologic investigations in the Three Sisters area of central Oregon, Summer 2001: U.S. Geological Survey Water-Resources Investigations Report 2002-4061, 16 p., https://doi.org/10.3133/wri024061.","productDescription":"16 p.","costCenters":[],"links":[{"id":3847,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024061","linkFileType":{"id":5,"text":"html"}},{"id":162627,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bec9","contributors":{"authors":[{"text":"Evans, William C. 0000-0001-5942-3102 wcevans@usgs.gov","orcid":"https://orcid.org/0000-0001-5942-3102","contributorId":2353,"corporation":false,"usgs":true,"family":"Evans","given":"William","email":"wcevans@usgs.gov","middleInitial":"C.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":230807,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mariner, Robert H. rmariner@usgs.gov","contributorId":3290,"corporation":false,"usgs":true,"family":"Mariner","given":"Robert","email":"rmariner@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":230808,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ingebritsen, Steven E. 0000-0001-6917-9369 seingebr@usgs.gov","orcid":"https://orcid.org/0000-0001-6917-9369","contributorId":818,"corporation":false,"usgs":true,"family":"Ingebritsen","given":"Steven","email":"seingebr@usgs.gov","middleInitial":"E.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":230806,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kennedy, B. Mack","contributorId":82758,"corporation":false,"usgs":true,"family":"Kennedy","given":"B.","email":"","middleInitial":"Mack","affiliations":[],"preferred":false,"id":230810,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"van Soest, Matthias C.","contributorId":102537,"corporation":false,"usgs":true,"family":"van Soest","given":"Matthias","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":230811,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Huebner, Mark A.","contributorId":27902,"corporation":false,"usgs":true,"family":"Huebner","given":"Mark A.","affiliations":[],"preferred":false,"id":230809,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":44973,"text":"wri024058 - 2002 - Geophysical logging to determine construction, contributing zones, and appropriate use of water levels measured in confined-aquifer network wells, San Luis Valley, Colorado, 1998-2000","interactions":[],"lastModifiedDate":"2012-02-02T00:10:12","indexId":"wri024058","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-4058","title":"Geophysical logging to determine construction, contributing zones, and appropriate use of water levels measured in confined-aquifer network wells, San Luis Valley, Colorado, 1998-2000","docAbstract":"Geophysical logs were recorded in 32 wells in the confined-aquifer monitoring well network maintained by the Rio Grande Water Conservation District. Logging results were used to determine well construction, zones contributing water to the wells, and the purposes for which the ground-water levels measured in the wells can be used. The confined-aquifer well network consists of 42 flowing and nonflowing wells. This network consists of wells used to supply water for irrigation, household use, wildlife refuge supply, and stock use, and wells for water-level monitoring. Geophysical logs recorded in the wells included video, caliper, water specific conductance, water temperature, and water flow. Most wells in the confined-aquifer well network yield a composite water level representing water levels in multiple permeable zones in the confined-aquifer system of the San Luis Valley. A potentiometric-surface map constructed using November 2000 water levels indicates that water levels from most wells in the network are correlated with water levels from nearby network wells. Potentiometric-surface maps that are constructed from water levels measured in most of the wells in the network can be used to understand long-term local and regional changes in water levels in the confined-aquifer system. Water levels measured in 8 of the 42 wells in the confined-aquifer network are not representative of water levels in the confined-aquifer system.","language":"ENGLISH","doi":"10.3133/wri024058","usgsCitation":"Brendle, D., 2002, Geophysical logging to determine construction, contributing zones, and appropriate use of water levels measured in confined-aquifer network wells, San Luis Valley, Colorado, 1998-2000: U.S. Geological Survey Water-Resources Investigations Report 2002-4058, iv, 58 p. : ill. (some col.), maps (some col.) ; 28 cm., https://doi.org/10.3133/wri024058.","productDescription":"iv, 58 p. : ill. (some col.), maps (some col.) ; 28 cm.","costCenters":[],"links":[{"id":162546,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3846,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024058/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b79d","contributors":{"authors":[{"text":"Brendle, D. L.","contributorId":68343,"corporation":false,"usgs":true,"family":"Brendle","given":"D. L.","affiliations":[],"preferred":false,"id":230805,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55164,"text":"wdrNE011 - 2002 - Water resources data, Nebraska, water year 2001","interactions":[],"lastModifiedDate":"2019-10-02T12:51:30","indexId":"wdrNE011","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"NE-01-1","title":"Water resources data, Nebraska, water year 2001","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNE011","usgsCitation":"Hitch, D., Hull, S., Steele, G.V., and Turner, M., 2002, Water resources data, Nebraska, water year 2001: U.S. Geological Survey Water Data Report NE-01-1, 440 p., https://doi.org/10.3133/wdrNE011.","productDescription":"440 p.","costCenters":[],"links":[{"id":173974,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/2001/ne-01-1/report-thumb.jpg"},{"id":367927,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/2001/ne-01-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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V.","contributorId":62543,"corporation":false,"usgs":true,"family":"Steele","given":"G.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":252838,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Turner, M.J.","contributorId":91562,"corporation":false,"usgs":true,"family":"Turner","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":252840,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":44967,"text":"wri024034 - 2002 - Hydrologic investigation of Powell Marsh and its relation to Dead Pike Lake, Vilas County, Wisconsin","interactions":[],"lastModifiedDate":"2015-10-27T12:13:18","indexId":"wri024034","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-4034","title":"Hydrologic investigation of Powell Marsh and its relation to Dead Pike Lake, Vilas County, Wisconsin","docAbstract":"

An analytic element ground-water-flow model was constructed to help understand the ground- and surface-water hydrology in the vicinity of Dead Pike Lake and Powell Marsh, Vilas County, Wisconsin. The model was used to simulate the effect of removing Powell Marsh control structures (ditches and Vista Pond) on the hydrology of Dead Pike Lake. Measurements and model simulation results show that ground water in the vicinity of Powell Marsh moves to the northwest and west. If Powell Marsh structures are removed from the simulation, it does not affect the general direction of ground-water flow nor the total flow to Dead Pike Lake. Without the simulated structures, slightly more ground-water flow enters Dead Pike Lake and slightly less surface-water flows at the Dead Pike Lake inlet than with the simulated structures.

\n

Ground-water levels measured in piezometers installed along a flow path indicated that ground-water flow primarily is horizontal in the marsh and moves upward in the vicinity of a ditch where it discharges. Flow from Vista Pond is downward to the ground-water system but eventually also discharges upward to the ditches. Based on analyses of water samples from piezometers, the ditch, and Vista Pond, it was shown that dissolved iron is transported in the ground water. When ground water is discharged, iron and manganese react with dissolved oxygen, then precipitates, and forms the oxyhydroxide floc present in the Powell Marsh ditches. The processes involved in the transport and floc formation are not unique to the ditches, but are an expected outcome where discharging ground water and oxygenated surface water meet. Therefore, although floc formed in the ditches would no longer be available for transport if ditches were removed, it is likely that the floc formation would be redirected to the near-shore areas of Dead Pike Lake where increased groundwater discharge is expected.

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