{"pageNumber":"366","pageRowStart":"9125","pageSize":"25","recordCount":16506,"records":[{"id":45053,"text":"wri004140 - 2000 - A hydrologic primer for New Jersey watershed management","interactions":[],"lastModifiedDate":"2016-02-29T11:23:52","indexId":"wri004140","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2000","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":"2000-4140","title":"A hydrologic primer for New Jersey watershed management","docAbstract":"

The U.S. Geological Survey (USGS) and the N.J. Department of Environmental Protection (NJDEP), and many other agencies and organizations are striving to educate the public about New Jersey’s water resources. In 1996, the NJDEP began implementing a “watershed management approach” to maintain the physical, chemical, and biological integrity of New Jersey’s waters. This approach concentrates on managing individual watershed areas by (1) defining the physical geographic boundaries of the watersheds, (2) basing water policy on sound scientific principles, and (3) developing partnerships with the public--the people most affected by watershed-management policies.

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New Jersey can be divided into five water regions as defined by the NJDEP: the Northeast, Raritan, Northwest, Lower Delaware, and Atlantic Coastal water regions (fig. 1). Each water region has been divided into three to five “watershed-management areas,” each of which encompasses a particular group of major rivers (fig. 2a-e). Each watershed management area consists of many smaller watersheds.

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Hydrologic data collected by Federal and State government agencies are invaluable as resources to policymakers who make decisions that affect the use of water in a particular watershed. The purpose of this report is to educate water-resource managers, policymakers, government officials, and the public about hydrologic concepts and the water-resource data needed to make informed decisions about water-management issues. (“Hydrologic” means relating to the occurrence, distribution, movement, and chemistry of all waters of the Earth (Fetter, 1980)). The first part of the report describes basic hydrologic concepts and includes explanations of the hydrologic cycle, the water budget, the surfacewater and ground-water flow systems, water-quality concepts and standards, and water use. The second part of the report summarizes the types of waterresource data that are available from Federal and State government agencies. Instructions on how to obtain the data and contact the appropriate Federal and State agencies, as well as suggestions for additional reading, also are included.

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Jersey\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae39c","contributors":{"authors":[{"text":"Watt, Martha K. 0000-0001-5651-3428 mwatt@usgs.gov","orcid":"https://orcid.org/0000-0001-5651-3428","contributorId":3275,"corporation":false,"usgs":true,"family":"Watt","given":"Martha","email":"mwatt@usgs.gov","middleInitial":"K.","affiliations":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"preferred":true,"id":231004,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":50370,"text":"ofr00478 - 2000 - Hydrologic data for water years 1933-97 used in the River and Reservoir Operations Model, Truckee River basin, California and Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:11:19","indexId":"ofr00478","displayToPublicDate":"1994-01-01T00:00:00","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":"2000-478","title":"Hydrologic data for water years 1933-97 used in the River and Reservoir Operations Model, Truckee River basin, California and Nevada","docAbstract":"Title II of Public Law 101-618, the Truckee?Carson?Pyramid Lake Water Rights Settlement Act of 1990, provides direction, authority, and a mechanism for resolving conflicts over water rights in the Truckee and Carson River Basins. The Truckee Carson Program of the U.S. Geological Survey, to support implementation of Public Law 101-618, has developed an operations model to simulate lake/reservoir and river operations for the Truckee River Basin including diversion of Truckee River water to the Truckee Canal for transport to the Carson River Basin. Several types of hydrologic data, formatted in a chronological order with a daily time interval called 'time series,' are described in this report. Time series from water years 1933 to 1997 can be used to run the operations model. Auxiliary hydrologic data not currently used by the model are also described. The time series of hydrologic data consist of flow, lake/reservoir elevation and storage, precipitation, evaporation, evapotranspiration, municipal and industrial (M&I) demand, and streamflow and lake/reservoir level forecast data.","language":"ENGLISH","doi":"10.3133/ofr00478","usgsCitation":"Berris, S.N., Hess, G.W., and Bohman, L.R., 2000, Hydrologic data for water years 1933-97 used in the River and Reservoir Operations Model, Truckee River basin, California and Nevada: U.S. Geological Survey Open-File Report 2000-478, 43 p.; map, https://doi.org/10.3133/ofr00478.","productDescription":"43 p.; map","costCenters":[],"links":[{"id":4176,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr00478","linkFileType":{"id":5,"text":"html"}},{"id":176755,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db6077d4","contributors":{"authors":[{"text":"Berris, Steven N. snberris@usgs.gov","contributorId":1736,"corporation":false,"usgs":true,"family":"Berris","given":"Steven","email":"snberris@usgs.gov","middleInitial":"N.","affiliations":[],"preferred":true,"id":241290,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hess, Glen W.","contributorId":19136,"corporation":false,"usgs":true,"family":"Hess","given":"Glen","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":241292,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bohman, Larry R. lrbohman@usgs.gov","contributorId":4769,"corporation":false,"usgs":true,"family":"Bohman","given":"Larry","email":"lrbohman@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":241291,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":54236,"text":"wdrMARI991 - 2000 - Water Resources Data Massachusetts and Rhode Island Water Year 1999","interactions":[],"lastModifiedDate":"2012-03-08T17:16:17","indexId":"wdrMARI991","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2000","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":"MA-RI-99-1","title":"Water Resources Data Massachusetts and Rhode Island Water Year 1999","docAbstract":"INTRODUCTION\r\n\r\nThe 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 Massachusetts and Rhode Island 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 States. 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-Massachusetts and Rhode Island.'\r\n\r\nHydrologic data are also available through the Massachusetts-Rhode Island District Home Page on the world-wide web (http://ma.water.usgs.gov). Historical data and real-time data (for sites equipped with satellite gage-height telemeter) are also available. The home page also contains a link to the U.S. Geological Survey National Home Page where streamflow data from locations throughout the United States can be retrieved.\r\n\r\nThis report series includes records of stage, discharge, and water quality of streams; contents of lakes and reservoirs; water levels of ground-water wells; and water quality of ground-water wells. This volume contains discharge records at 90 gaging stations; stage records at 2 gaging stations; monthend contents of 4 lakes and reservoirs; water quality at 31 gaging stations; water quality at 27 observation wells; and water levels for 139 observation wells. Locations of these sites are shown in figures 1 and 2. Short-term water-quality data were collected at 21 gaging stations and 27 observation wells and are shown in figure 3. Miscellaneous hydrologic data were collected at various sites that were not involved in the systematic data-collection program and are published as miscellaneous discharge measurements. The data in this report represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Massachusetts and Rhode Island.\r\n\r\nThis series of annual reports for Massachusetts and Rhode Island began with the 1961 water year with a report that contained only data relating to the quantities of surface water. For the 1964 water year, a similar report was introduced that contained only data relating to water quality. Beginning with the 1975 water year, the report format was changed to present, in one volume, data on quantities of surface water, quality of surface and ground water, and ground-water levels.\r\n\r\nPrior to introduction of this series and for several water years concurrent with it, water-resources data for Massachusetts and Rhode Island were published in U.S. Geological Survey Water-Supply Papers. Data on stream discharge and stage and on lake or reservoir contents and stage, through September 1960, were published annually under the title 'Surface-Water Supply of the United States, Parts 1A and 1B.' For the 1961 through 1970 water years, the data were published in two 5-year reports. Data on chemical quality, temperature, and suspended sediment for the 1941 through 1970 water years were published annually under the title 'Quality of Surface Waters of the United States,' and water levels for the 1939 through 1974 water years were published under the title 'Ground-Water Levels in the United States.' The above mentioned Water-Supply Papers may be consulted in the libraries of the principal cities of the United States and may be purchased from U.S. Geological Survey, Information Services, Box 25286, Denver Federal Center, Box 25425, Denver, CO 80225-0286.\r\n\r\nPublications similar to this report are published annually by the Geological Survey for all States. These official Survey reports have an identification number consisting of the two-letter State abbreviation, the last two digits of the water year, and the volume number. For example, this volume is identified as 'U.S. Geological Survey Water-Data Report MARI-98-1.' For archiving and general d","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/wdrMARI991","usgsCitation":"Socolow, R., Zanca, J., Murino, D., and Ramsbey, L., 2000, Water Resources Data Massachusetts and Rhode Island Water Year 1999: U.S. Geological Survey Water Data Report MA-RI-99-1, xvi, 401 p., https://doi.org/10.3133/wdrMARI991.","productDescription":"xvi, 401 p.","additionalOnlineFiles":"Y","costCenters":[{"id":377,"text":"Massachusetts-Rhode Island Water Science Center","active":false,"usgs":true}],"links":[{"id":173850,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9701,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/wdr-ma-ri-99-1/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9fed","contributors":{"authors":[{"text":"Socolow, R.S.","contributorId":17639,"corporation":false,"usgs":true,"family":"Socolow","given":"R.S.","affiliations":[],"preferred":false,"id":249620,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zanca, J.L.","contributorId":63087,"corporation":false,"usgs":true,"family":"Zanca","given":"J.L.","affiliations":[],"preferred":false,"id":249622,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Murino, Domenic Jr.","contributorId":42649,"corporation":false,"usgs":true,"family":"Murino","given":"Domenic","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":249621,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ramsbey, L.R.","contributorId":78393,"corporation":false,"usgs":true,"family":"Ramsbey","given":"L.R.","email":"","affiliations":[],"preferred":false,"id":249623,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":54777,"text":"wdrND992 - 2000 - Water Resources Data, North Dakota, Water Year 1998. Volume 2. Ground Water","interactions":[],"lastModifiedDate":"2018-03-22T14:01:25","indexId":"wdrND992","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2000","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":"ND-99-2","title":"Water Resources Data, North Dakota, Water Year 1998. Volume 2. Ground Water","docAbstract":"

This edition of the annual hydrologic data report of North Dakota is one of a series of annual reports that document hydrologic data collected from the U.S. Geological Survey's collection networks in each State, Puerto Rico, and the Trust Territories. These records of streamflow, ground-water levels, and quality of water provide the hydrologic information needed by Federal, State, local agencies, and the private sector for developing and managing land and water resources in North Dakota. 

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrND992","usgsCitation":"Harkness, R., and Wald, J.D., 2000, Water Resources Data, North Dakota, Water Year 1998. Volume 2. Ground Water: U.S. Geological Survey Water Data Report ND-99-2, 176 p., https://doi.org/10.3133/wdrND992.","productDescription":"176 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":174465,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5425,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://nd.water.usgs.gov/pubs/wdr/wdrnd992/index.html","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fafa8","contributors":{"authors":[{"text":"Harkness, R.E.","contributorId":24412,"corporation":false,"usgs":true,"family":"Harkness","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":251513,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wald, J. D.","contributorId":30993,"corporation":false,"usgs":true,"family":"Wald","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":251514,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":53981,"text":"wri004075 - 2000 - Hydrology, Geomorphology, and Sediment Transport of the San Miguel River, Southwest Colorado","interactions":[],"lastModifiedDate":"2017-08-29T21:41:29","indexId":"wri004075","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2000","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":"2000-4075","title":"Hydrology, Geomorphology, and Sediment Transport of the San Miguel River, Southwest Colorado","docAbstract":"

No abstract available.

","language":"English","doi":"10.3133/wri004075","usgsCitation":"Allred, T.M., and Andrews, E., 2000, Hydrology, Geomorphology, and Sediment Transport of the San Miguel River, Southwest Colorado: U.S. Geological Survey Water-Resources Investigations Report 2000-4075, 52 p., https://doi.org/10.3133/wri004075.","productDescription":"52 p.","costCenters":[],"links":[{"id":177505,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc736","contributors":{"authors":[{"text":"Allred, Tyler M.","contributorId":173170,"corporation":false,"usgs":false,"family":"Allred","given":"Tyler","email":"","middleInitial":"M.","affiliations":[{"id":27172,"text":"Allred Restoration, Inc., Tremonton, UT","active":true,"usgs":false}],"preferred":false,"id":248839,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andrews, E.D.","contributorId":13922,"corporation":false,"usgs":true,"family":"Andrews","given":"E.D.","email":"","affiliations":[],"preferred":false,"id":248838,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":22774,"text":"ofr00279 - 2000 - Stable hydrogen and oxygen isotope ratios for selected sites of the National Oceanic and Atmospheric Administration's Atmospheric Integrated Research Monitoring Network (AIRMoN)","interactions":[],"lastModifiedDate":"2012-10-05T17:16:22","indexId":"ofr00279","displayToPublicDate":"1994-01-01T00:00:00","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":"2000-279","title":"Stable hydrogen and oxygen isotope ratios for selected sites of the National Oceanic and Atmospheric Administration's Atmospheric Integrated Research Monitoring Network (AIRMoN)","docAbstract":"Increasingly, hydrologic studies require information on the isotopic composition of natural waters. This report presents stable hydrogen (δ2H) and oxygen isotope ratios (δ180) of precipitation samples from seven selected sites of the National Oceanic and Atmospheric Administration's Atmospheric Integrated Research Monitoring Network (AIRMoN) collected during the years 1992-1994.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr00279","issn":"0094-9140","usgsCitation":"Coplen, T.B., and Huang, R., 2000, Stable hydrogen and oxygen isotope ratios for selected sites of the National Oceanic and Atmospheric Administration's Atmospheric Integrated Research Monitoring Network (AIRMoN): U.S. Geological Survey Open-File Report 2000-279, iv, 54 p., https://doi.org/10.3133/ofr00279.","productDescription":"iv, 54 p.","numberOfPages":"60","costCenters":[{"id":543,"text":"Reston Stable Isotope Laboratory","active":false,"usgs":true}],"links":[{"id":156941,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2000_279.jpg"},{"id":262300,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2000/0279/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Delaware;Illinois;New York;Ohio;Pennsylvania;Tennessee;Vermont","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89.41666666666667,35 ], [ -89.41666666666667,45 ], [ -71.45,45 ], [ -71.45,35 ], [ -89.41666666666667,35 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e4942","contributors":{"authors":[{"text":"Coplen, Tyler B. 0000-0003-4884-6008 tbcoplen@usgs.gov","orcid":"https://orcid.org/0000-0003-4884-6008","contributorId":508,"corporation":false,"usgs":true,"family":"Coplen","given":"Tyler","email":"tbcoplen@usgs.gov","middleInitial":"B.","affiliations":[{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true}],"preferred":true,"id":188852,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Huang, Richard","contributorId":10457,"corporation":false,"usgs":true,"family":"Huang","given":"Richard","email":"","affiliations":[],"preferred":false,"id":188853,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28984,"text":"wri004199 - 2000 - A decision support system for prioritizing forested wetland restoration in the Yazoo Backwater Area, Mississippi","interactions":[],"lastModifiedDate":"2012-02-02T00:08:48","indexId":"wri004199","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2000","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":"2000-4199","title":"A decision support system for prioritizing forested wetland restoration in the Yazoo Backwater Area, Mississippi","docAbstract":"A working prototype decision support system (DSS) was developed for the Yazoo Backwater Area, Mississippi, to help planners and managers prioritize, plan, conduct, and optimize forested wetland restoration activities. The DSS comprises geographic information system (GIS) spatial data themes, application programs that provide a cumulative analysis of the relative ability of sites to function as wetlands, and output data that are specific to a given restoration analysis scenario. The DSS input includes GIS data themes such as geomorphology, soils, land use, elevation, farmed wetlands, flood frequency, topographic depressions, streams, public lands, roads, and permanent water bodies, which can be used as spatial templates to define areal hydrologic settings. These GIS data themes can then be ranked and combined to estimate the relative suitability of a potential wetland restoration site, thereby, determining relative wetland equivalence on the landscape. The GIS applications used in this DSS perform the following three functions: assess the ecology (the Eco-Assessor); reclassify land-use in areas selected for restoration (the Tree-Translator); and generate output data to compare restoration scenarios (the Parameter-Generator). Areas selected for reforestation are translated (in the GIS) into ?forested? land use, and the tree species that are ?planted? on the landscape (in the DSS) either compose an ecologically optimal or an economically optimal community of tree species. Output from the DSS can be compared and analyzed by using economic, statistical, graphical, and tabular methods. Output data for seven selected scenarios were generated for the Yazoo Backwater Area and are presented as examples to illustrate the flexibility of the DSS to identify areas that meet restoration objectives. ","language":"ENGLISH","publisher":"U.S. Department of the Interior, U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/wri004199","usgsCitation":"O'Hara, C., Davis, A.A., and Kleiss, B., 2000, A decision support system for prioritizing forested wetland restoration in the Yazoo Backwater Area, Mississippi: U.S. Geological Survey Water-Resources Investigations Report 2000-4199, 43 p., https://doi.org/10.3133/wri004199.","productDescription":"43 p.","costCenters":[],"links":[{"id":2268,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://ms.water.usgs.gov/ms_proj/wetlands/restoration_dss/wrir00-4199.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159147,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af1da","contributors":{"authors":[{"text":"O'Hara, Charles G.","contributorId":83911,"corporation":false,"usgs":true,"family":"O'Hara","given":"Charles G.","affiliations":[],"preferred":false,"id":200733,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, Angela A.","contributorId":22001,"corporation":false,"usgs":true,"family":"Davis","given":"Angela","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200732,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kleiss, Barbara A.","contributorId":87536,"corporation":false,"usgs":true,"family":"Kleiss","given":"Barbara A.","affiliations":[],"preferred":false,"id":200734,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":21657,"text":"ofr0081 - 2000 - Chemical and isotopic composition and gas concentrations of ground water and surface water from selected sites at and near the Idaho National Engineering and Environmental Laboratory, Idaho, 1994-97","interactions":[],"lastModifiedDate":"2020-02-23T17:36:00","indexId":"ofr0081","displayToPublicDate":"1994-01-01T00:00:00","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":"2000-81","title":"Chemical and isotopic composition and gas concentrations of ground water and surface water from selected sites at and near the Idaho National Engineering and Environmental Laboratory, Idaho, 1994-97","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0081","issn":"0566-8174","usgsCitation":"Busenberg, E., Plummer, N., Doughten, M., Widman, P., and Bartholomay, R.C., 2000, Chemical and isotopic composition and gas concentrations of ground water and surface water from selected sites at and near the Idaho National Engineering and Environmental Laboratory, Idaho, 1994-97: U.S. Geological Survey Open-File Report 2000-81, iv, 51 p. , https://doi.org/10.3133/ofr0081.","productDescription":"iv, 51 p. ","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":155980,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2000/0081/report-thumb.jpg"},{"id":95447,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2000/0081/report.pdf","size":"3701","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","otherGeospatial":"Idaho National Engineering and Environmental Laboratory","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.25,43.25 ], [ -114.25,44.25 ], [ -112.25,44.25 ], [ -112.25,43.25 ], [ -114.25,43.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e48d8","contributors":{"authors":[{"text":"Busenberg, Eurybiades ebusenbe@usgs.gov","contributorId":2271,"corporation":false,"usgs":true,"family":"Busenberg","given":"Eurybiades","email":"ebusenbe@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":185107,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":185110,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Doughten, M. W.","contributorId":101648,"corporation":false,"usgs":true,"family":"Doughten","given":"M. W.","affiliations":[],"preferred":false,"id":185111,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Widman, P.K.","contributorId":19589,"corporation":false,"usgs":true,"family":"Widman","given":"P.K.","email":"","affiliations":[],"preferred":false,"id":185108,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bartholomay, R. C.","contributorId":66271,"corporation":false,"usgs":true,"family":"Bartholomay","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":185109,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":54356,"text":"wdrIA002 - 2000 - Water Resources Data, Iowa, Water Year 2000, Volume 2. surface water--Missouri River Basin, and ground water","interactions":[],"lastModifiedDate":"2016-02-08T13:28:57","indexId":"wdrIA002","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2000","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":"IA-00-2","title":"Water Resources Data, Iowa, Water Year 2000, Volume 2. surface water--Missouri River Basin, and ground water","docAbstract":"

This volume of the annual hydrologic data report of Iowa is one of a series of annual reports that document hydrologic
data gathered from the U.S. Geological Survey’s surface- and ground-water data-collection networks in each State, Puerto
Rico, and the Trust Territories. These records of streamflow, ground-water levels, and quality of water provide the hydrologic
information needed by local, State, and Federal agencies, and the private sector for developing and managing our Nation’s land
and water resources.

\n

This report is the culmination of a concerted effort by dedicated personnel of the U.S. Geological Survey who collected,
compiled, analyzed, verified, and organized the data, and who typed, edited, and assembled the report. The authors had
primary responsibility for assuring that the information contained herein is accurate, complete, and adheres to Geological
Survey policy and established guidelines.

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These decisions may include discharge requirements for an extension of the San Luis Drain (SLD) to the estuary to convey subsurface agricultural drainage from the western San Joaquin Valley (SJV), a renewal of an agreement to allow the existing portion of the SLD to convey subsurface agricultural drainage to a tributary of the San Joaquin River (SJR) (coincident with changes in flow patterns of the lower SJR), and refinements to promulgated Se criteria for the protection of aquatic life for the estuary.\r\rUnderstanding the biotransfer of Se is essential to evaluating the fate and impact of proposed changes in Se discharges to the Bay-Delta. However, past monitoring programs have not addressed the specific protocols necessary for an element that bioaccumulates. Confusion about Se threats in the past have stemmed from failure to consider the full complexity of the processes that result in Se toxicity. Past studies show that predators are more at risk from Se contamination than their prey, making it difficult to use traditional methods to predict risk from environmental concentrations alone. In this report, we employ a novel procedure to model the fate of Se under different, potentially realistic load scenarios from the SJV. For each potential load, we progressively forecast the resulting environmental concentrations, speciation, transformation to particulate form, bioaccumulation by invertebrates, trophic transfer to predators, and effects in those predators. Enough is known to establish a first order understanding of effects should Se be discharged directly into the North Bay via a conveyance such as the SLD.\r\rOur approach uses 1) existing knowledge concerning the biogeochemical reactions of Se (e.g., speciation, partitioning between dissolved and particulate forms, and bivalve assimilation efficiency) and 2) site-specific data mainly from 1986 to 1996 on clams and bottom-feeding fish and birds. Forecasts of Se loading from oil refineries and agricultural drainage from the SJV enable the calculation of a composite freshwater endmember Se concentration at the head of the estuary and at Carquinez Strait as a foundation for modeling. Our analysis of effects also takes into account the mode of conveyance for agricultural drainage (i.e., the SLD or SJR). The effects of variable flows on a seasonal or monthly basis from the Sacramento River and SJR are also considered.\r\rThe results of our forecasts for external SJV watershed sources of Se mirror predictions made since 1955 of a worsening salt (and by inference, Se) buildup exacerbated by the arid climate and irrigation for agricultural use. We show that the reservoir of Se in the SJV is sufficient to provide loading at an annual rate of approximately 42,500 pounds (lbs) of Se to a Bay-Delta disposal point for 63 to 304 years at the lower range of our projections, even if influx of Se from the California Coast Ranges could be curtailed. Disposal of wastewaters on an annual basis outside of the SJV may slow the degradation of valley resources, but drainage alone cannot alleviate the salt and Se buildup in the SJV, at least within a century.\r\rOur forecasts show the different proportions of Se loading to the Bay-Delta. Oil refinery loads from 1986 to 1992 ranged from 11 to 15 lbs Se per day; with treatment and cleanup, loads decreased to 3 lbs Se per day in 1999. In contrast, SJV agricultural drainage loads could range from of 45 to 117 lbs Se per day across a set of reasonable conditions. Components of this valley-wide load include five source subareas (i.e., Grassland, Westlands, Tulare, Kern, and Northern) based on water and drainage management. 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No abstract available.

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No abstract available. 

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The U.S. Geological Survey (USGS), U.S. Department of the Interior, is the Nation's largest Earth-science information agency. Among its many responsibilities, such as map making and providing information on earthquakes and other natural hazards, the USGS provides information on the Nation's water resources. The USGS has collected and analyzed hydrologic (water-related) information for more than 100 years. In 1889, the first streamflow-gaging station (a site where regular observations of streamflow data are collected) operated in the United States by the USGS was established on the Rio Grande near Embudo, New Mexico. As the need for streamflow data increased, the USGS's streamflow-gaging program has grown to include more than 7,000 continuous-record streamflow-gaging stations. More than 90 percent of these stations are operated with at least partial support from State, local, and other Federal agencies.

In Virginia, the Department of Environmental Quality (DEQ) is a major cooperator in the streamflow-gaging program, which consists of 152 continuous-record streamflow-gaging stations located throughout the State (fig. 1). The USGS and DEQ cooperate to publish the annual USGS State data report, \"Water Resources Data-Virginia;\" this two-volume publication includes streamflow data collected at the 152 streamflow-gaging stations, chemical data collected at more than 24 streamflow-gaging stations, and ground-water data collected from more than 338 wells.

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\"}}]}","edition":"Revised in 1999","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5878a4b6e4b04df303d95867","contributors":{"authors":[{"text":"Moberg, Roger M. rmmoberg@usgs.gov","contributorId":3655,"corporation":false,"usgs":true,"family":"Moberg","given":"Roger","email":"rmmoberg@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":658329,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rice, Karen C. 0000-0002-9356-5443 kcrice@usgs.gov","orcid":"https://orcid.org/0000-0002-9356-5443","contributorId":1998,"corporation":false,"usgs":true,"family":"Rice","given":"Karen","email":"kcrice@usgs.gov","middleInitial":"C.","affiliations":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"preferred":false,"id":658330,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Powell, Eugene D.","contributorId":80309,"corporation":false,"usgs":true,"family":"Powell","given":"Eugene","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":658331,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70179677,"text":"70179677 - 1999 - Hydrology and geochemistry of carbonate springs in Mantua Valley, northern Utah","interactions":[],"lastModifiedDate":"2017-01-19T14:42:31","indexId":"70179677","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5260,"text":"Utah Geological Association Publications","active":true,"publicationSubtype":{"id":10}},"title":"Hydrology and geochemistry of carbonate springs in Mantua Valley, northern Utah","docAbstract":"

Water chemistry, tritium data, precipitation-discharge relations, geology, topography, and dye tracing were used to determine recharge areas, ground-water residence times, factors influencing ground-water flow, and aquifer characteristic for five springs that discharge from Paleozoic limestones and dolostones along the margin of Manuta Valley, northern Utah.

Temperature of Mantua Valley spring water ranged between 6.0 and 15.0 degrees Celsius. Spring-water temperature indicates that depth of circulation of ground water could be as shallow as 80 feet (25 meters) to as much as 1,150 feet (350 meters). Dissolved-solids concentration in the water from springs ranged from 176 to 268 milligrams per liter. Average total hardness of spring water ranged from 157 to 211 milligrams per liter. Water from all of the springs is a calcium-magnesium-bicarbonate type that generally is undersaturated with respect to calcite and dolomite. The molar calcium/magnesium ratio in spring water ranged from 1.21 to 1.88, and indicates that ground water flows through impure dolostone or a mixed limestone and dolostone terrace.

Discharge from carbonate springs in Mantua Valley ranges from about to 10 to 4,300 gallons per minute (0.6 to 271 liters per second). Seasonal variations in chemical parameters and discharge indicate that the aquifers supplying water to most of these springs are predominantly diffuse-flow systems that have been locally enhanced by bedrock dissolution. Estimated recharge area for th springs ranges from 2.7 to 7 square miles (7 to 18 square kilometers).

On the basis of tritium age dating, the mean residence time of ground water discharges from Olsens-West Hallins and Maple Springs was determined to be from 3 to 9, and from 4 to 15 years, respectively. Dye tracing from point sources 2.65 miles (4.26 kilometers) southeast of Maple Spring, however, indicates a substantially faster component of flow during snowmelt runoff, with a travel time of about 5 days, or an average ground-water velocity of about 2,700 feet per day (823 meters per day).

","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Geology of northern Utah and vicinity (Utah Geological Association Publication 27)","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Utah Geological Association Publication 1999 field Symposium","conferenceDate":"September 11, 1999","language":"English","publisher":"Utah Geological Association","publisherLocation":"Salt Lake City, UT","usgsCitation":"Rice, K.C., and Spangler, L.E., 1999, Hydrology and geochemistry of carbonate springs in Mantua Valley, northern Utah: Utah Geological Association Publications, p. 337-352.","productDescription":"16 p.","startPage":"337","endPage":"352","costCenters":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"links":[{"id":333035,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333037,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.utahgeology.org/wp/publications"}],"country":"United States","state":"Utah","otherGeospatial":"Mantua Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.00149536132812,\n 41.32010701725659\n ],\n [\n -112.00149536132812,\n 41.56562822121977\n ],\n [\n -111.78520202636719,\n 41.56562822121977\n ],\n [\n -111.78520202636719,\n 41.32010701725659\n ],\n [\n -112.00149536132812,\n 41.32010701725659\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58774c9de4b0315b4c11ff2c","contributors":{"editors":[{"text":"Spangler, Lawrence E. 0000-0003-3928-8809 spangler@usgs.gov","orcid":"https://orcid.org/0000-0003-3928-8809","contributorId":973,"corporation":false,"usgs":true,"family":"Spangler","given":"Lawrence","email":"spangler@usgs.gov","middleInitial":"E.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":658197,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Allen, Constance J.","contributorId":178204,"corporation":false,"usgs":false,"family":"Allen","given":"Constance","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":658198,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Rice, Karen C. 0000-0002-9356-5443 kcrice@usgs.gov","orcid":"https://orcid.org/0000-0002-9356-5443","contributorId":1998,"corporation":false,"usgs":true,"family":"Rice","given":"Karen","email":"kcrice@usgs.gov","middleInitial":"C.","affiliations":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"preferred":false,"id":658195,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spangler, Lawrence E. 0000-0003-3928-8809 spangler@usgs.gov","orcid":"https://orcid.org/0000-0003-3928-8809","contributorId":973,"corporation":false,"usgs":true,"family":"Spangler","given":"Lawrence","email":"spangler@usgs.gov","middleInitial":"E.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":658196,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70157373,"text":"70157373 - 1999 - Characterizing hydrology and the importance of ground-water discharge in natural and constructed wetlands","interactions":[],"lastModifiedDate":"2018-12-19T10:38:20","indexId":"70157373","displayToPublicDate":"2015-06-07T08:30:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3750,"text":"Wetlands","onlineIssn":"1943-6246","printIssn":"0277-5212","active":true,"publicationSubtype":{"id":10}},"title":"Characterizing hydrology and the importance of ground-water discharge in natural and constructed wetlands","docAbstract":"

Although considered the most important component for the establishment and persistence of wetlands, hydrology has been hard to characterize and linkages between hydrology and other environmental conditions are often poorly understood. In this work, methods for characterizing a wetland’s hydrology from hydrographs were developed, and the importance of ground water to the physical and geochemical conditions in the root zone was investigated. Detailed sampling of nearly continuous hydrographs showed that sites with greater ground-water discharge had higher water tables and more stable hydrographs. Subsampling of the continuous hydrograph failed to characterize the sites correctly, even though the wetland complex is located in a strong regional ground-water-discharge area. By comparing soil-moisture-potential measurements to the water-table hydrograph at one site, we noted that the amount of root-zone saturation was not necessarily driven by the water-table hydrograph but can be a result of other soil parameters (i.e., soil texture and associated capillary fringe). Ground-water discharge was not a significant determinant of maximum or average temperatures in the root zone. High ground-water discharge was associated with earliest date of thaw and shortest period of time that the root zone was frozen, however. Finally, the direction and magnitude of shallow ground-water flow was found to affect the migration and importance of a geochemical species. Areas of higher ground-water discharge had less downward penetration of CO2 generated in the root zone. In contrast, biotically derived CO2 was able to penetrate the deeper ground-water system in areas of ground-water recharge. Although ground-water flows are difficult to characterize, understanding these components is critical to the success of wetland restoration and creation efforts.

","language":"English","publisher":"Springer","doi":"10.1007/BF03161777","usgsCitation":"Hunt, R.J., Walker, J.F., and Krabbenhoft, D.P., 1999, Characterizing hydrology and the importance of ground-water discharge in natural and constructed wetlands: Wetlands, v. 19, no. 2, p. 458-472, https://doi.org/10.1007/BF03161777.","productDescription":"15 p.","startPage":"458","endPage":"472","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":308361,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wisconsin","county":"Monroe County","otherGeospatial":"Kickapoo River, Wilton, Wilton wetland","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -90.626220703125,\n 43.736623487867654\n ],\n [\n -90.626220703125,\n 43.86200998554792\n ],\n [\n -90.4343032836914,\n 43.86200998554792\n ],\n [\n -90.4343032836914,\n 43.736623487867654\n ],\n [\n -90.626220703125,\n 43.736623487867654\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"19","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56027bb5e4b03bc34f544805","contributors":{"authors":[{"text":"Hunt, Randall J. 0000-0001-6465-9304 rjhunt@usgs.gov","orcid":"https://orcid.org/0000-0001-6465-9304","contributorId":1129,"corporation":false,"usgs":true,"family":"Hunt","given":"Randall","email":"rjhunt@usgs.gov","middleInitial":"J.","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":true,"id":572904,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walker, John F. jfwalker@usgs.gov","contributorId":1081,"corporation":false,"usgs":true,"family":"Walker","given":"John","email":"jfwalker@usgs.gov","middleInitial":"F.","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":true,"id":572905,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krabbenhoft, David P. 0000-0003-1964-5020 dpkrabbe@usgs.gov","orcid":"https://orcid.org/0000-0003-1964-5020","contributorId":1658,"corporation":false,"usgs":true,"family":"Krabbenhoft","given":"David","email":"dpkrabbe@usgs.gov","middleInitial":"P.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true},{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":true,"id":572906,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70073906,"text":"70073906 - 1999 - Canadian Geophysical Union Hydrology Section special issue","interactions":[],"lastModifiedDate":"2018-09-13T18:29:01","indexId":"70073906","displayToPublicDate":"2014-01-01T14:07:37","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1924,"text":"Hydrological Processes","active":true,"publicationSubtype":{"id":10}},"title":"Canadian Geophysical Union Hydrology Section special issue","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Hydrological Processes","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Canadian Geophysical Union","usgsCitation":"1999, Canadian Geophysical Union Hydrology Section special issue: Hydrological Processes, v. 13, no. 6, p. 2483-2638.","productDescription":"156 p.","startPage":"2483","endPage":"2638","costCenters":[],"links":[{"id":281424,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd5020e4b0b290850f3248","contributors":{"editors":[{"text":"Anderson, M.G.","contributorId":112540,"corporation":false,"usgs":true,"family":"Anderson","given":"M.G.","email":"","affiliations":[],"preferred":false,"id":509770,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Peters, Norman E. nepeters@usgs.gov","contributorId":1324,"corporation":false,"usgs":true,"family":"Peters","given":"Norman","email":"nepeters@usgs.gov","middleInitial":"E.","affiliations":[{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true}],"preferred":true,"id":744913,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Walling, D.","contributorId":112963,"corporation":false,"usgs":true,"family":"Walling","given":"D.","email":"","affiliations":[],"preferred":false,"id":744914,"contributorType":{"id":2,"text":"Editors"},"rank":3}]}} ,{"id":70038383,"text":"70038383 - 1999 - Pesticides in stream sediment and aquatic biota: distribution, trends, and governing factors","interactions":[],"lastModifiedDate":"2012-05-18T01:01:33","indexId":"70038383","displayToPublicDate":"2012-01-01T15:59:00","publicationYear":"1999","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"Pesticides in stream sediment and aquatic biota: distribution, trends, and governing factors","docAbstract":"More than 20 years after the ban of DDT and other organochlorine pesticides, pesticides continue to be detected in air, rain, soil, surface water, bed sediment, and aquatic and terrestrial biota throughout the world. Recent research suggests that low levels of some of these pesticides may have the potential to affect the development, reproduction, and behavior of fish and wildlife, and possibly humans. Pesticides in Stream Sediment and Aquatic Biota: Distribution, Trends, and Governing Factors assesses the occurrence and behavior of pesticides in bed sediment and aquatic biota-the two major compartments of the hydrologic system where organochlorine pesticides are most likely to accumulate. This book collects, for the first time, results from several hundred monitoring studies and field experiments, ranging in scope from individual sites to the entire nation. Comprehensive tables provide concise summaries of study locations, pesticides analyzed, and study outcomes. Comprehensive and extensively illustrated, Pesticides in Stream Sediment and Aquatic Biota: Distribution, Trends, and Governing Factors evaluates the sources, environmental fate, geographic distribution, and long-term trends of pesticides in bed sediment and aquatic biota. The book focuses on organochlorine pesticides, but also assesses the potential for currently used pesticides to be found in bed sediment and aquatic biota. Topics covered in depth include the effect of land use on pesticide occurrence, mechanisms of pesticide uptake and accumulation by aquatic biota, and the environmental significance of observed levels of pesticides in stream sediment and aquatic biota.","largerWorkTitle":"Pesticides in the Hydrologic System","language":"English","publisher":"CRC Press","publisherLocation":"Boca Raton, FL","usgsCitation":"Nowell, L.H., and Capel, P.D., 1999, Pesticides in stream sediment and aquatic biota: distribution, trends, and governing factors, v. 4, 1040 p.","productDescription":"1040 p.","numberOfPages":"1040","costCenters":[{"id":453,"text":"National Water-Quality Assessment Program","active":false,"usgs":true}],"links":[{"id":256883,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":256882,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.crcpress.com/product/isbn/9781566704694","linkFileType":{"id":5,"text":"html"}}],"volume":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a775de4b0c8380cd78498","contributors":{"authors":[{"text":"Nowell, Lisa H. 0000-0001-5417-7264 lhnowell@usgs.gov","orcid":"https://orcid.org/0000-0001-5417-7264","contributorId":490,"corporation":false,"usgs":true,"family":"Nowell","given":"Lisa","email":"lhnowell@usgs.gov","middleInitial":"H.","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":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":464024,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Capel, Peter D.","contributorId":44773,"corporation":false,"usgs":true,"family":"Capel","given":"Peter","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":464025,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70005239,"text":"wdrNJ981 - 1999 - Water Resources Data: New Jersey, Water Year 1998, Volume 1, Surface-Water Data","interactions":[],"lastModifiedDate":"2014-07-17T09:39:52","indexId":"wdrNJ981","displayToPublicDate":"2011-08-22T00:00:00","publicationYear":"1999","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":"NJ-98-1","title":"Water Resources Data: New Jersey, Water Year 1998, Volume 1, Surface-Water Data","docAbstract":"This volume of the annual hydrologic data report of New Jersey is one of a series of annual reports that document hydrologic data gathered from the U.S. Geological Survey's surface- and ground-water data-collection networks in each State, Puerto Rico, and the Trust Territories. These records of streamflow, ground-water levels, and water quality provide the hydrologic information needed by state, local and federal agencies, and the private sector for developing and managing our Nation's land and water resources.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNJ981","collaboration":"Prepared in coooperation with the New Jersey Department of Environmental Protection and with other agencies","usgsCitation":"Reed, T., Centinaro, G., Dudek, J., Corcino, V., Stekroadt, G., and McTigure, R., 1999, Water Resources Data: New Jersey, Water Year 1998, Volume 1, Surface-Water Data: U.S. Geological Survey Water Data Report NJ-98-1, xx, 281 p., https://doi.org/10.3133/wdrNJ981.","productDescription":"xx, 281 p.","costCenters":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"links":[{"id":121120,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_nj_98_1.gif"},{"id":91777,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/1998/nj-98-1/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New Jersey","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.58333333333333,38.916666666666664 ], [ -75.58333333333333,41.35055555555556 ], [ -73.88416666666667,41.35055555555556 ], [ -73.88416666666667,38.916666666666664 ], [ -75.58333333333333,38.916666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd32b","contributors":{"authors":[{"text":"Reed, T.J. 0000-0002-9943-4081","orcid":"https://orcid.org/0000-0002-9943-4081","contributorId":15224,"corporation":false,"usgs":true,"family":"Reed","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":352121,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Centinaro, G.L.","contributorId":61892,"corporation":false,"usgs":true,"family":"Centinaro","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":352124,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dudek, J.F.","contributorId":31818,"corporation":false,"usgs":true,"family":"Dudek","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":352123,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Corcino, V.","contributorId":28653,"corporation":false,"usgs":true,"family":"Corcino","given":"V.","email":"","affiliations":[],"preferred":false,"id":352122,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Stekroadt, G.C.","contributorId":106249,"corporation":false,"usgs":true,"family":"Stekroadt","given":"G.C.","email":"","affiliations":[],"preferred":false,"id":352126,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"McTigure, R.C.","contributorId":104203,"corporation":false,"usgs":true,"family":"McTigure","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":352125,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":29323,"text":"wri994154 - 1999 - Relation of pesticide concentrations to season, streamflow, and land use in seven New Jersey streams","interactions":[],"lastModifiedDate":"2012-03-08T17:16:15","indexId":"wri994154","displayToPublicDate":"2011-07-25T00:00:00","publicationYear":"1999","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":"99-4154","title":"Relation of pesticide concentrations to season, streamflow, and land use in seven New Jersey streams","docAbstract":"The presence and variability of pesticides in seven New Jersey streams was documented by analyzing 146 samples collected from the streams from April 1996 through June 1998. The samples were analyzed for 85 pesticides, including 50 herbicides, 28 insecticides, and 7 degradation products, at method detection limits that ranged from 0.001 to 0.018 μg/L (micrograms per liter). Pesticides were frequently detected; however, concentrations were generally low. The pesticides most frequently detected were atrazine, in 97 percent of the samples; prometon, 96 percent; metolachlor, 95 percent; desethyl-atrazine, 91 percent; simazine, 88 percent; diazinon, 58 percent; alachlor, 56 percent; and carbaryl, 54 percent. Detection frequencies were highest during the growing season (April-September). At least one pesticide was detected in all but one of these samples, and 49 percent of the samples contained 9 or more pesticides. The numbers of pesticides detected at a given site ranged from 13 to 29.\n\nTen pesticides were detected at concentrations that exceeded established water-quality criteria. Thirty-one of these detections were in samples collected during the growing season and one during the nongrowing season. The pesticides that exceeded the U.S. Environmental Protection Agency (USEPA) maximum contaminant level for drinking water were atrazine, which exceeded 3 μg/L in four samples, and alachlor, 2 μg/L in two samples. Cyanazine exceeded the USEPA liftime health advisory level (HAL) of 1 μg/L in two samples. These eight detections occurred during runoff shortly after spring pesticide applications and represent a potential threat to municipal water supplies in the Raritan River basin. Concentrations of chlorpyrifos, chlorthalonil, diazinon, ethyl-parathion, and methyl-azinphos exceeded the chronic life criteria for the protection of aquatic life (ACQR) in 20 samples at four sites during the growing season. Dieldrin was detected in four samples and DDE in two samples at concentrations that exceeded New Jersey Department of Environmental Protection (NJDEP) human health criteria. \n\nIndividual and total-pesticide concentrations and total numbers of pesticides detected in the samples varied with season and flow conditions. Median and maximum concentrations of most of the pesticides were highest during runoff in the growing season. Pesticide concentrations were typically lower and less variable in the nongrowing season than in the growing season, regardless of changes in hydrologic conditions; however, median concentrations of most pesticides were slightly lower during runoff than during base flow. The median total-pesticide concentration and median total number of pesticides detected were highest and most variable in runoff samples in the growing season. In the nongrowing season, the median total-pesticide concentration was lowest in runoff samples and least variable during base-flow conditions. Median total numbers of pesticides were lowest and least varibale in the nongrowing season during base-flow conditions at most sites. \n\nThe highest total-pesticide concentrations were detected in samples from the two small agricultural basins (greater than 25 percent of land use is agricultural) during runoff in late spring and early summer. In general, insecticides were detected more frequently and in greater concentrations at urban sites. Concentrations of agricultural herbicides generally decreased with increasing flow at the four sites with less than 10 percent agriculture land use and increased with increasing flow at the three sites with more than 25 percent agricultural land use. Most of the pesticides that correlated positively with streamflow were detected at sites where land use in the basin would indicate the use of those particular pesticides. Most of the pesticides that correlated negatively with streamflow were present at the site in the Coastal Plain or at sites in which the land use in the basin would not indicate heavy u","language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri994154","usgsCitation":"Reiser, R.G., 1999, Relation of pesticide concentrations to season, streamflow, and land use in seven New Jersey streams: U.S. Geological Survey Water-Resources Investigations Report 99-4154, 19 p., https://doi.org/10.3133/wri994154.","productDescription":"19 p.","costCenters":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"links":[{"id":116680,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_99_4154.gif"},{"id":24437,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/1999/4154/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New Jersey;New York","otherGeospatial":"Long Island","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.58333333333333,38.81666666666667 ], [ -75.58333333333333,41.416666666666664 ], [ -71.45,41.416666666666664 ], [ -71.45,38.81666666666667 ], [ -75.58333333333333,38.81666666666667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c2b6","contributors":{"authors":[{"text":"Reiser, Robert G. 0000-0001-5140-2745 rreiser@usgs.gov","orcid":"https://orcid.org/0000-0001-5140-2745","contributorId":4083,"corporation":false,"usgs":true,"family":"Reiser","given":"Robert","email":"rreiser@usgs.gov","middleInitial":"G.","affiliations":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"preferred":true,"id":201348,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5224555,"text":"5224555 - 1999 - Fifty-eighth Christmas Bird Count. 166. Ocean City, Md","interactions":[],"lastModifiedDate":"2012-02-02T00:15:41","indexId":"5224555","displayToPublicDate":"2010-06-16T12:18:55","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3750,"text":"Wetlands","onlineIssn":"1943-6246","printIssn":"0277-5212","active":true,"publicationSubtype":{"id":10}},"title":"Fifty-eighth Christmas Bird Count. 166. Ocean City, Md","docAbstract":"Gauging the impact of manipulative activities, such as rehabilitation or management, on wetlands requires having a notion of the unmanipulated condition as a reference. An understanding of the reference condition requires knowledge of dominant factors influencing ecosystem processes and biological communities. In this paper, we focus on natural physical factors (conditions and processes) that drive coastal wetland ecosystems of the Laurentian Great Lakes. Great Lakes coastal wetlands develop under conditions of large-lake hydrology and disturbance imposed at a hierarchy of spatial and temporal scales and contain biotic communities adapted to unstable and unpredictable conditions. Coastal wetlands are configured along a continuum of hydrogeomorphic types: open coastal wetlands, drowned river mouth and flooded delta wetlands, and protected wetlands, each developing distinct ecosystem properties and biotic communities. Hydrogeomorphic factors associated with the lake and watershed operate at a hierarchy of scales: a) local and short-term (seiches and ice action), b) watershed / lakewide / annual (seasonal water- level change), and c) larger or year-to-year and longer ( regional and/or greater than one-year). Other physical factors include the unique water quality features of each lake. The aim of this paper is to provide scientists and managers with a framework for considering regional and site-specific geomorphometry and a hierarchy of physical processes in planning management and conservation projects.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wetlands","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Robbins, C., 1999, Fifty-eighth Christmas Bird Count. 166. Ocean City, Md: Wetlands, v. 19, no. 4, p. 117-118.","productDescription":"821-834","startPage":"117","endPage":"118","numberOfPages":"2","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":200171,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48d6e4b07f02db54920a","contributors":{"authors":[{"text":"Robbins, C.S.","contributorId":53907,"corporation":false,"usgs":true,"family":"Robbins","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":341961,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5223817,"text":"5223817 - 1999 - Fifty-year trends in a box turtle population in Maryland","interactions":[],"lastModifiedDate":"2016-01-04T15:51:40","indexId":"5223817","displayToPublicDate":"2010-06-16T12:18:49","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1015,"text":"Biological Conservation","active":true,"publicationSubtype":{"id":10}},"title":"Fifty-year trends in a box turtle population in Maryland","docAbstract":"

A survey conducted in 1995 investigated long term declines reported in a population of box turtles Terrapene Carolina monitored each decade since 1945 in bottomland hardwood forest at the Patuxent Wildlife Research Center, Maryland. Methods duplicated past surveys in most respects, but were supplemented by radiotelemetry and a survey of dominant vegetation. Seventy different turtles were found on the 11.8 ha study area, a decline of >75% since peak populations were recorded in 1955. Searchers were less efficient in 1995 than in 1945-1975 for a variety of possible reasons. Among turtles recorded, approximately equal numbers persisted from each of the past five decades, with some individuals surviving >70 years. A sex ratio strongly favoring males was first recorded in 1975 and continued in 1995, but juveniles and subadults were found in greater proportion in 1995 than in any other survey. Six of nine radio-marked turtles left the bottomland study area and migrated to the adjoining bluffs to hibernate, suggesting more extensive movements and perhaps less stable home ranges than formerly thought. Age structure of trees indicated a gradual change to more shade-tolerant species. Examination of rates of change from survey data suggested that major losses probably resulted from changes in hydrology that exacerbated flooding in 1972, with recovery only beginning in 1995 and perhaps limited both by repeated flood events and successional changes in the forest. Slow recovery from losses may indicate that populations of the species would respond poorly to exploitation.

","language":"English","publisher":"Elsevier","doi":"10.1016/S0006-3207(98)00107-4","usgsCitation":"Hall, R., Henry, P., and Bunck, C., 1999, Fifty-year trends in a box turtle population in Maryland: Biological Conservation, v. 88, no. 2, p. 165-172, https://doi.org/10.1016/S0006-3207(98)00107-4.","productDescription":"8 p.","startPage":"165","endPage":"172","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":202191,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"88","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f4883","contributors":{"authors":[{"text":"Hall, R.J.","contributorId":32885,"corporation":false,"usgs":true,"family":"Hall","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":339593,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Henry, P.F.P.","contributorId":14531,"corporation":false,"usgs":true,"family":"Henry","given":"P.F.P.","email":"","affiliations":[],"preferred":false,"id":339592,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bunck, C.M.","contributorId":72337,"corporation":false,"usgs":true,"family":"Bunck","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":339594,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":25552,"text":"wri994013 - 1999 - Ground-water hydrology of the Tacoma-Puyallup area, Pierce County, Washington","interactions":[],"lastModifiedDate":"2023-03-13T19:48:34.165639","indexId":"wri994013","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"1999","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":"99-4013","title":"Ground-water hydrology of the Tacoma-Puyallup area, Pierce County, Washington","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri994013","usgsCitation":"Jones, M., Orr, L.A., Ebbert, J., and Sumioka, S.S., 1999, Ground-water hydrology of the Tacoma-Puyallup area, Pierce County, Washington: U.S. Geological Survey Water-Resources Investigations Report 99-4013, v, 154 p., https://doi.org/10.3133/wri994013.","productDescription":"v, 154 p.","costCenters":[],"links":[{"id":414039,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16364.htm","linkFileType":{"id":5,"text":"html"}},{"id":260319,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1999/4013/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":260320,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1999/4013/report-thumb.jpg"}],"country":"United States","state":"Washington","county":"Pierce County","otherGeospatial":"Tacoma-Puyallup area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -122.55,\n 47.322\n ],\n [\n -122.55,\n 47.092\n ],\n [\n -122.208,\n 47.092\n ],\n [\n -122.208,\n 47.322\n ],\n [\n -122.55,\n 47.322\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668ccc","contributors":{"authors":[{"text":"Jones, M. A.","contributorId":37736,"corporation":false,"usgs":true,"family":"Jones","given":"M. A.","affiliations":[],"preferred":false,"id":194162,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Orr, L. A.","contributorId":27894,"corporation":false,"usgs":true,"family":"Orr","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":194161,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ebbert, J.C.","contributorId":57451,"corporation":false,"usgs":true,"family":"Ebbert","given":"J.C.","affiliations":[],"preferred":false,"id":194163,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sumioka, S. S.","contributorId":20747,"corporation":false,"usgs":true,"family":"Sumioka","given":"S.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":194160,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":27119,"text":"wri994170 - 1999 - Hydrologic effects of the Pymatuning earthquake of September 25, 1998, in northwestern Pennsylvania","interactions":[],"lastModifiedDate":"2025-01-10T18:32:29.611521","indexId":"wri994170","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"1999","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":"99-4170","title":"Hydrologic effects of the Pymatuning earthquake of September 25, 1998, in northwestern Pennsylvania","docAbstract":"Within hours after the Pymatuning earthquake of September 25, 1998, in northwestern Pennsylvania, local residents reported wells becoming dry, wells beginning to flow, and the formation of new springs. About 120 household-supply wells reportedly went dry within 3 months after the earthquake. About 80 of these wells were on a ridge between Jamestown and Greenville, where water-level declines of as much as 100 feet were documented. Accompanying the decline in water levels beneath the ridge was an increase in water levels in valley wells of as much as 62 feet. One possible explanation of the observed hydrologic effects is that the earthquake increased the vertical hydraulic conductivity of shales beneath the ridge, which allowed ground water to drain from the hilltops. Computer simulations of ground-water flow beneath the ridge between Jamestown and Greenville indicate that increasing the vertical hydraulic conductivity of shale confining beds about 10 to 60 times from their pre-quake values could cause the general pattern of decreased water levels on hilltops and increased levels in valleys.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri994170","usgsCitation":"Fleeger, G.M., Goode, D., Buckwalter, T.F., and Risser, D.W., 1999, Hydrologic effects of the Pymatuning earthquake of September 25, 1998, in northwestern Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 99-4170, 8 p., https://doi.org/10.3133/wri994170.","productDescription":"8 p.","onlineOnly":"Y","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":394831,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22563.htm"},{"id":158705,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1999/4170/coverthb.jpg"},{"id":2235,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1999/4170/wri19994170.pdf","text":"Report","size":"1.23 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRIR 1999-4170"}],"country":"United States","state":"Pennsylvania","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.35,\n 41.394\n ],\n [\n -80.45,\n 41.394\n ],\n [\n -80.45,\n 41.483\n ],\n [\n -80.35,\n 41.483\n ],\n [\n -80.35,\n 41.394\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"

Director, Pennsylvania Water Science Center
U.S. Geological Survey
215 Limekiln Road
New Cumberland, PA 17070

","tableOfContents":"","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606e0f","contributors":{"authors":[{"text":"Fleeger, Gary M.","contributorId":63436,"corporation":false,"usgs":true,"family":"Fleeger","given":"Gary","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":197586,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goode, Daniel J. 0000-0002-8527-2456 djgoode@usgs.gov","orcid":"https://orcid.org/0000-0002-8527-2456","contributorId":2433,"corporation":false,"usgs":true,"family":"Goode","given":"Daniel J.","email":"djgoode@usgs.gov","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":false,"id":197587,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Buckwalter, Theodore F.","contributorId":90719,"corporation":false,"usgs":true,"family":"Buckwalter","given":"Theodore","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":197585,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Risser, Dennis W. 0000-0001-9597-5406 dwrisser@usgs.gov","orcid":"https://orcid.org/0000-0001-9597-5406","contributorId":898,"corporation":false,"usgs":true,"family":"Risser","given":"Dennis","email":"dwrisser@usgs.gov","middleInitial":"W.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":197584,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":25479,"text":"wri974260 - 1999 - Environmental setting and natural factors and human influences affecting water quality in the White River Basin, Indiana","interactions":[],"lastModifiedDate":"2016-06-01T16:02:03","indexId":"wri974260","displayToPublicDate":"2002-03-01T00:00:00","publicationYear":"1999","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":"97-4260","title":"Environmental setting and natural factors and human influences affecting water quality in the White River Basin, Indiana","docAbstract":"

The White River Basin drains 11,349 square miles of central and southern Indiana and is one of 59 Study Units selected for water-quality assessment as part of the U.S. Geological Survey's National WaterQuality Assessment Program. Defining the environmental setting of the basin and identifying the natural factors and human influences that affect water quality are important parts of the assessment.

\n

Interrelated natural factors help determine the quality of surface and ground water in a river basin. The White River Basin has a humid continental climate, characterized by well-defined winter and summer seasons. Geologic features in the basin include glaciated and nonglaciated areas; a region of karst geomorphology that is characterized by caves and sinkholes; and a thick, sedimentary bedrock sequence underlying the entire basin. Unconsolidated glacial deposits of clay, silt, sand and gravel cover more than 60 percent of the basin. Soils developed in unconsolidated glacial deposits are typically fertile, naturally or artificially well drained, and farmed. Soils in the unglaciated south-central part of the basin are thin, have low fertility, and are best suited for forest or pasture.

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Agriculture is the principal land use in the White River Basin. Approximately 70 percent of the basin is used for agriculture, and about 50 percent of the basin is cropland. Corn and soybeans are the major crops. Other significant land uses are forest (22 percent) and urban and residential (7 percent). The population of the basin was 2.1 million in 1990. Water use in the White River Basin totaled 1,284 million gallons per day in 1995, of which 84.5 percent was surface water and 15.5 percent was ground water. Despite the predominant use of surface water, ground water was the primary source of drinking water for approximately 56 percent of the population.

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The general water chemistry in the White River Basin is determined by natural factors such as soils and geologic materials that water contacts as it moves through the hydrologic system. In the southern part of the basin, bedrock upland areas are dominated by non-carbonate bedrock, thin soils, and high runoff-rainfall ratios. These areas have small chemical concentrations in streamwater. Conversely, in the northern part of the basin where glacial deposits are thick and in the southwestern part of the basin where loess deposits are thick, water has longer periods of time to react with soils and aquifers and to acquire substantial quantities of dissolved constituents. As a result, streams in the till plain and glacial lowland have higher concentrations of most constituents than streams in the unglaciated parts of the basin. Water quality is significantly modified by human influences. Water quality is affected locally by point sources of contamination that include combined-sewer overflows, power-generation-plant cooling stations, and wastewater-treatment-plant effluents that are generally associated with densely populated areas. Water quality is additionally affected by non-point sources of contamination related to agriculture, urban runoff, and mining.

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Six hydrogeomorphic regions of the White River Basin are delineated on the basis of distinct and relatively homogeneous natural characteristics. These six regions are used in the White River Basin study as a framework for examining the effects of natural factors on water quality in the basin. Bedrock is exposed or near the surface in three hydrogeomorphic regions the bedrock uplands, bedrock lowland and plain, and karst plain; streams and shallow aquifers in these regions are susceptible to contamination, especially in the karst plain, and show rapid response to rainfall. The other three hydrogeomorphic regions the fluvial deposits, till plain, and glacial lowland are in the glaciated part of the basin. Where thick fine-grained unconsolidated sediments are present, primarily in the till plain, ground-water supplies are protected from contamination, and extreme high and low streamflows are moderated.

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The landfill is built on \r\nthe Hueco Bolson, a deposit that yields water to five public-supply \r\nwells within 1.1 miles of the landfill boundary on all sides. \r\nThe bolson deposits consist of lenses and mixtures of sand, clay, \r\nsilt, gravel, and caliche. The unsaturated zone at the landfill \r\nis about 300 feet thick. The Hydrologic Evaluation of Landfill \r\nPerformance (HELP) and the Multimedia Exposure Assessment \r\nModel for Evaluating the Land Disposal of Wastes (MULTIMED) \r\ncomputer models were used to simulate the time of first arrival \r\nof landfill leachate at the water table. \r\n\r\nSite-specific data were collected for model input. At five \r\nsites on the landfill cover, hydraulic conductivity was \r\nmeasured by an in situ method; in addition, laboratory values were \r\nobtained for porosity, moisture content at field capacity, and \r\nmoisture content at wilting point. Twenty-seven sediment samples were \r\ncollected from two adjacent boreholes drilled near the \r\nsouthwest corner of the landfill. Of these, 23 samples were assumed \r\nto represent the unsaturated zone beneath the landfill. The core \r\nsamples were analyzed in the laboratory for various \r\ncharacteristics required for the HELP and MULTIMED models: initial \r\nmoisture content, dry bulk density, porosity, saturated \r\nhydraulic conductivity, moisture retention percentages at various \r\nsuction values, total organic carbon, and pH. Parameters were \r\ncalculated for the van Genuchten and Brooks-Corey equations that \r\nrelate hydraulic conductivity to saturation. A reported recharge \r\nvalue of 0.008 inch per year was estimated on the basis of soil-\r\nwater chloride concentration.\r\n\r\nThe HELP model was implemented using input values that were based \r\nmostly on site-specific data or assumed in a conservative manner. \r\nExceptions were the default values used for waste characteristics. \r\nFlow through the landfill was assumed to be at steady state. The \r\nHELP-estimated landfill leakage rate was 101.6 millimeters per \r\nyear, approximately 500 times the estimated recharge rate for the \r\narea near the landfill. \r\n\r\nThe MULTIMED model was implemented using input values \r\nthat were based mainly on site-specific data and some \r\nconservatively assumed values. Landfill leakage was assumed to \r\nbegin when the landfill was established and to continue at a \r\nsteady-state rate of 101.6 millimeters per year as estimated \r\nby the HELP model. By using an assumed solute concentration in \r\nthe leachate of 1 milligram per liter and assuming no delay or \r\ndecay of solute, the solute serves as a tracer to indicate the first \r\narrival of landfill leachate. The simulated first arrival of \r\nleachate at the water table was 204 to 210 years after the \r\nestablishment of the landfill.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri974036","usgsCitation":"Frenzel, P.F., and Abeyta, C.G., 1999, Geohydrology of the unsaturated zone and simulated time of arrival of landfill leachate at the water table, Municipal Solid Waste Landfill Facility, U.S. Army Air Defense Artillery Center and Fort Bliss, El Paso County, Texas: U.S. Geological Survey Water-Resources Investigations Report 97-4036, Report: iv, 26 p.; 1 Plate: 7.94 × 19.99 inches, https://doi.org/10.3133/wri974036.","productDescription":"Report: iv, 26 p.; 1 Plate: 7.94 × 19.99 inches","costCenters":[],"links":[{"id":394223,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22935.htm"},{"id":56061,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1997/4036/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56060,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1997/4036/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124479,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1997/4036/report-thumb.jpg"}],"country":"United States","state":"Texas","county":"El Paso County","otherGeospatial":"U.S. Army Air Defense Artillery Center and Fort Bliss","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.388,\n 31.8760\n ],\n [\n -106.397,\n 31.8760\n ],\n [\n -106.397,\n 31.885\n ],\n [\n -106.388,\n 31.885\n ],\n [\n -106.388,\n 31.8760\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a87ee","contributors":{"authors":[{"text":"Frenzel, Peter F.","contributorId":59442,"corporation":false,"usgs":true,"family":"Frenzel","given":"Peter","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":197708,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Abeyta, Cynthia G.","contributorId":52187,"corporation":false,"usgs":true,"family":"Abeyta","given":"Cynthia","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":197707,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}