{"pageNumber":"3041","pageRowStart":"76000","pageSize":"25","recordCount":184769,"records":[{"id":50073,"text":"fs07402 - 2002 - Chronic Wasting Disease (CWD): Just the Facts","interactions":[],"lastModifiedDate":"2023-09-01T14:20:47.459938","indexId":"fs07402","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":"074-02","displayTitle":"Chronic Wasting Disease (CWD): Just the Facts","title":"Chronic Wasting Disease (CWD): Just the Facts","docAbstract":"<p>Chronic Wasting Disease (CWD) has appeared widely in the media lately, but has actually been around for a while. It was first recognized in Colorado in 1967, in a captive research herd of mule deer. Its rapid expansion, to include eight states and two provinces by the year 2002, has created a crisis.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs07402","usgsCitation":"Roffe, T.J., and Jachowski, D., 2002, Chronic Wasting Disease (CWD): Just the Facts: U.S. Geological Survey Fact Sheet 074-02, 2 p., https://doi.org/10.3133/fs07402.","productDescription":"2 p.","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":120696,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2002/0074/coverthb.jpg"},{"id":4261,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2002/0074/fs07402.pdf","text":"Report","size":"507 KB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 074-02"}],"contact":"<p><a href=\"https://pubs.er.usgs.gov/contact\" data-mce-href=\"https://pubs.er.usgs.gov/contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dde4b07f02db5e1fba","contributors":{"authors":[{"text":"Roffe, Thomas J.","contributorId":56596,"corporation":false,"usgs":true,"family":"Roffe","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":240730,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jachowski, Dick","contributorId":29878,"corporation":false,"usgs":true,"family":"Jachowski","given":"Dick","email":"","affiliations":[],"preferred":false,"id":240729,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":50082,"text":"fs10402 - 2002 - Effects of wastewater on forested wetlands","interactions":[],"lastModifiedDate":"2016-09-15T10:21:21","indexId":"fs10402","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":"104-02","title":"Effects of wastewater on forested wetlands","docAbstract":"<p>Cycling nutrient-enriched wastewater from holding ponds through natural, forested wetlands is a practice that municipal waste treatment managers are considering as a viable option for disposing of wastewater. In this wastewater cycling process, sewer effluent that has been circulated through aerated ponds is discharged into neighboring wetland systems. To understand how wastewater cycling affects forest and species productivity, researchers at the USGS National Wetlands Research Center conducted dendroecological investigations in a swamp system and in a bog system that have been exposed to wastewater effluent for many decades. </p><p>Dendroecology involves the study of forest changes over time as interpreted from tree rings. Tree-ring chronologies describe the pattern and history of growth suppression and release that can be associated with aging and disturbances such as hurricanes, floods, and fires. But because of limited monitoring, little is known about the potential for long-term effects on forested wetlands as a result of wastewater flooding. USGS researchers used tree rings to detect the effect of wastewater cycling on tree growth. Scientists expected to find that tree-ring width would be increased as a result of added nutrients. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs10402","usgsCitation":"Doyle, T.W., 2002, Effects of wastewater on forested wetlands: U.S. Geological Survey Fact Sheet 104-02, 2 p., https://doi.org/10.3133/fs10402.","productDescription":"2 p.","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"links":[{"id":4265,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://archive.usgs.gov/archive/sites/www.nwrc.usgs.gov/factshts/104-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":125350,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_104_02.jpg"},{"id":10936,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://archive.usgs.gov/archive/sites/www.nwrc.usgs.gov/factshts/104-02/104-02.htm","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624c10","contributors":{"authors":[{"text":"Doyle, Thomas W. 0000-0001-5754-0671 doylet@usgs.gov","orcid":"https://orcid.org/0000-0001-5754-0671","contributorId":703,"corporation":false,"usgs":true,"family":"Doyle","given":"Thomas","email":"doylet@usgs.gov","middleInitial":"W.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":240741,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50079,"text":"fs09302 - 2002 - State Water Resources Research Institute Program","interactions":[],"lastModifiedDate":"2012-02-02T00:11:15","indexId":"fs09302","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":"093-02","title":"State Water Resources Research Institute Program","language":"ENGLISH","doi":"10.3133/fs09302","usgsCitation":"Schefter, J.E., 2002, State Water Resources Research Institute Program: U.S. Geological Survey Fact Sheet 093-02, 2 p., https://doi.org/10.3133/fs09302.","productDescription":"2 p.","costCenters":[],"links":[{"id":176345,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2002/0093/report-thumb.jpg"},{"id":86287,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2002/0093/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e3f98","contributors":{"authors":[{"text":"Schefter, John E.","contributorId":21155,"corporation":false,"usgs":true,"family":"Schefter","given":"John","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":240734,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50089,"text":"fs12102 - 2002 - National Civil Applications Program","interactions":[],"lastModifiedDate":"2014-04-10T09:38:30","indexId":"fs12102","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":"121-02","title":"National Civil Applications Program","docAbstract":"The National Civil Applications Program\n(NCAP) is a component of the U.S.\nGeological Survey's (USGS) Mapping,\nRemote Sensing, and Geographic\nInvestigations Program. The NCAP\nserves Federal civil agencies by providing\nfor the acquisition, dissemination,\nand exploitation of classified remote\nsensing systems and data in support of\nmission responsibilities for land and\nresource management, environmental and\nscientific studies, homeland security, and\nhazards/disaster management.\nCivil applications of classified remotely\nsensed imagery began in 1969 when the\nUSGS provided Federal civil agencies\nwith access to imagery for various uses,\nincluding mapping, charting, geodesy,\nand management of the Nation's lands\nand resources. The Civil Applications\nCommittee (CAC) was established in\n1975 to provide oversight and\ncoordination of these activities. The CAC\nis composed of 11 Federal departments\nand independent agencies. The USGS,\nthrough the Secretary of the Interior, is\ndelegated responsibility to chair the\nCAC.\nThe use of classified remotely sensed\ndata has increased dramatically over the\npast 10 years. There has been an\nexpanded emphasis on using data for\nenvironmental monitoring and research\nand for hazards detection, warning, and\nemergency response. To address the\ngrowing requirements and better serve\nthe Federal civil community, the USGS\nexpanded its investment in NCAP\nfacilities and infrastructure during the\n1990s. The USGS Advanced Systems\nCenter (ASC) in Reston, Va., was built in\n1993 and serves as the hub of NCAP\noperations. The USGS operates regional\nfacilities in Denver, Colo.; Rolla, Mo.;\nSioux Falls, S. Dak.; and Menlo Park,\nCalif. An interagency NCAP facility is\nlocated in Anchorage, Alaska. Each\nUSGS facility provides the infrastructure,\nsystems, and expertise required to\nsupport the growing diversity of civil\napplications.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs12102","usgsCitation":"Budd, W.A., 2002, National Civil Applications Program: U.S. Geological Survey Fact Sheet 121-02, 2 p., https://doi.org/10.3133/fs12102.","productDescription":"2 p.","numberOfPages":"2","costCenters":[],"links":[{"id":286124,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/0121-02/report-thumb.jpg"},{"id":286123,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/0121-02/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b444c","contributors":{"authors":[{"text":"Budd, Wendy A.","contributorId":12780,"corporation":false,"usgs":true,"family":"Budd","given":"Wendy","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":240749,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50080,"text":"fs09802 - 2002 - Modeling the bathymetry of Catahoula Lake: Specialized technology for wetland management","interactions":[],"lastModifiedDate":"2016-09-15T10:19:08","indexId":"fs09802","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":"098-02","title":"Modeling the bathymetry of Catahoula Lake: Specialized technology for wetland management","docAbstract":"Catahoula Lake is the largest natural freshwater lake in Louisiana, covering more than 46 square miles (120 km2) (fig. 1). The lake is a principal stopover and wintering site for hundreds of thousands of migratory waterfowl and shorebirds. Scientists from the USGS National Wetlands Research Center are applying some of the research facility's specialties?wetland plant research, aerial and ground surveys, digital mapping, and computer modeling?to facilitate wetland management at Catahoula Lake.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs09802","usgsCitation":"Doyle, T., Michot, T., and Wells, C., 2002, Modeling the bathymetry of Catahoula Lake: Specialized technology for wetland management: U.S. Geological Survey Fact Sheet 098-02, 2 p., https://doi.org/10.3133/fs09802.","productDescription":"2 p.","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"links":[{"id":4263,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://archive.usgs.gov/archive/sites/www.nwrc.usgs.gov/factshts/098-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":10938,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://archive.usgs.gov/archive/sites/www.nwrc.usgs.gov/factshts/098-02/098-02.htm","linkFileType":{"id":5,"text":"html"}},{"id":123577,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_098_02.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db6997d9","contributors":{"authors":[{"text":"Doyle, T.W. 0000-0001-5754-0671","orcid":"https://orcid.org/0000-0001-5754-0671","contributorId":16783,"corporation":false,"usgs":true,"family":"Doyle","given":"T.W.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":240735,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Michot, T.C. 0000-0002-7044-987X","orcid":"https://orcid.org/0000-0002-7044-987X","contributorId":43426,"corporation":false,"usgs":true,"family":"Michot","given":"T.C.","affiliations":[],"preferred":false,"id":240737,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wells, C.","contributorId":29051,"corporation":false,"usgs":true,"family":"Wells","given":"C.","affiliations":[],"preferred":false,"id":240736,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":44970,"text":"wri024038 - 2002 - Evaluation of trends in pH in the Yampa River, northwestern Colorado, 1950-2000","interactions":[],"lastModifiedDate":"2012-02-02T00:10:12","indexId":"wri024038","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":"2002-4038","title":"Evaluation of trends in pH in the Yampa River, northwestern Colorado, 1950-2000","docAbstract":"In 1999, the U.S. Geological Survey began a study of pH trends in the Yampa River from near its headwaters to its mouth. The study was prompted by an apparent historical increase in measured pH at the Yampa River near Maybell, from an average of about 7.6 in the 1950's and 1960's to about 8.3 in the 1980's and 1990's. If real, further increase could cause more frequent exceedances of the Colorado water-quality standard of 9.0 and adversely affect aquatic life in the Yampa River Basin, including Dinosaur National Monument. The principal conclusion of this study is that this apparent historical increase in measured pH was caused mostly by changes in measurement protocol. \r\n\r\nSynoptic sampling during August 16-19, 1999, a period of relatively warm weather and base flow, showed that late afternoon pH of the Yampa River ranged from 8.46 to 9.20. The largest pH (9.20) exceeded the Colorado water-quality standard and was measured at Yampa River above Elk River, about 1.8 miles downstream from the Steamboat Springs Regional Waste Water Treatment Plant outfall, where nutrient enrichment caused photosynthesis by algae to dominate. Here, the dissolved oxygen concentration was 161 percent of saturation and carbon dioxide (CO2 was at 26 percent of saturation. At Yampa River downstream from a diversion near Hayden, 16.3 miles downstream, the effects of photosynthesis were still dominant, though attenuated by reaeration and dilution with freshwater from the Elk River. About 37.2 miles farther downstream, at Yampa River below Craig, which is about 6.2 miles downstream from the Craig Waste Water Treatment Plant, the effects of photosynthesis increased slightly, and pH rose to 8.80. Respiration plus oxidation of organic matter became dominant at Yampa River at Deerlodge Park in Dinosaur National Monument, where pH was 8.51, dissolved oxygen concentration was at 109 percent of saturation, and CO2 was at 189 percent of saturation. Respiration plus oxidation of organic matter, though diminished, apparently extended to the mouth of the Yampa River.\r\n\r\nDiurnal measurements on the Yampa River during August 23-26, 1999, show that the effects of photosynthesis and respiration plus oxidation of organic matter decreased downstream with distance from the developed urban area in the eastern part of the basin. Larger night-time values of pH in Dinosaur National Monument at Deerlodge Park and at the mouth of the Yampa River indicate that source waters varied with respect to capacity for respiration plus oxidation and photo-synthesis, that photosynthesis was minor, and that pH was largely controlled by respiration plus oxidation of organic matter.\r\n\r\nSynoptic sampling was repeated during March 13-16, 2000, when discharge was larger in response to late-winter melting of snow and ice at lower altitudes in the basin. Concentrations of nitrite plus nitrate were about 9 times greater in the Yampa River during March 2000 than during August 1999, and the largest increase (greater than 1,200 percent) was at Yampa River below Craig. At and downstream from Steamboat Springs, Colorado, pH at Yampa River sites averaged 8.85 during synoptic sampling in March 2000 compared to 8.70 in August 1999, with the partial pressure of carbon dioxide gas (PCO2) averaging 67 percent of saturation (compared to 99 percent during August 1999). The apparently larger effects of photosynthesis on pH and dissolved oxygen concentrations during March 2000 compared to August 1999 probably were caused by (1) slower rates of exchange of CO2 into and dissolved oxygen out of the river because of colder and deeper water and (2) slower rates of CO2 production and oxygen consumption resulting from slower rates of respiration by organisms and from slower rates of aerobic decomposition of organic matter in the colder river water and streambed sediment.\r\n\r\nHypothetical thermodynamic simulations were done for samples collected in the lower Yampa River Basin to simulate the same amount of photosynthesis th","language":"ENGLISH","doi":"10.3133/wri024038","usgsCitation":"Chafin, D.T., 2002, Evaluation of trends in pH in the Yampa River, northwestern Colorado, 1950-2000: U.S. Geological Survey Water-Resources Investigations Report 2002-4038, iv, 41 p. : ill., maps ; 28 cm., https://doi.org/10.3133/wri024038.","productDescription":"iv, 41 p. : ill., maps ; 28 cm.","costCenters":[],"links":[{"id":3843,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024038/","linkFileType":{"id":5,"text":"html"}},{"id":162446,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9dfe","contributors":{"authors":[{"text":"Chafin, Daniel T.","contributorId":77500,"corporation":false,"usgs":true,"family":"Chafin","given":"Daniel","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":230797,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44918,"text":"wri024193 - 2002 - Hydrogeology and water-quality characteristics of the Lower Floridan aquifer in east-central Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:10:11","indexId":"wri024193","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":"2002-4193","title":"Hydrogeology and water-quality characteristics of the Lower Floridan aquifer in east-central Florida","docAbstract":"The hydrogeology and water-quality characteristics of the Lower Floridan aquifer and the relation of the Lower Floridan aquifer to the framework of the Floridan aquifer system were evaluated during a 6-year (1995-2001) study. The study area, a 7,500 square-mile area of east-central Florida, is underlain by three principal hydrogeologic units: the surficial aquifer system, the intermediate confining unit, and the Floridan aquifer system. The Floridan aquifer system, a carbonate-rock aquifer system composed of the Upper Floridan aquifer, a middle semiconfining unit, a middle confining unit, and the Lower Floridan aquifer, is the major source of water supply to east-central Florida. The Upper Floridan aquifer provides much of the water required to meet the current (2002) demand; however, the Lower Floridan aquifer is being used increasingly as a source of freshwater, particularly for municipal needs. For this reason, a better understanding of the aquifer is needed. The Lower Floridan aquifer is present throughout east-central Florida. The aquifer is composed of alternating beds of limestone and dolomite, and is characterized by abundant fractured dolomite zones and solution cavities. The altitude of the top of the Lower Floridan aquifer ranges from less than 600 feet below sea level in the northern part of the study area to more than 1,600 feet below sea level in the southwestern part. Thickness of the unit ranges from about 910 to 1,180 feet. The top of the Lower Floridan aquifer generally is marked by an increase in formation resistivity and by an increase in the occurrence of fractures and solution cavities within the carbonates. Also, a noticeable increase in borehole flow often marks the top of the unit. The bottom of the Lower Floridan aquifer is based on the first occurrence of evaporites. Ground-water in the Lower Floridan aquifer generally moves in a southwest-to-northeast direction across the study area. In September 1998, the altitude of the potentiometric surface of the Lower Floridan aquifer ranged from about 16 to 113 feet above sea level, and altitudes in May 1999 were about 2 to 7 feet lower than those measured in September 1998. The potentiometric surface of the Floridan aquifer system is constantly fluctuating, mainly in response to seasonal variations in rainfall and ground-water withdrawals. Seasonal fluctuations in the Lower Floridan aquifer typically range from about 2 to 10 feet. Water samples from 50 Lower Floridan aquifer wells were collected during this study. Most samples were analyzed in the field for temperature, pH, and specific conductance, and in the laboratory for major cations and anions. Specific conductance ranged from 147 to 6,710 microsiemens per centimeter. Chloride concentrations ranged from 3.0 to 2,188 milligrams per liter; sulfate concentrations ranged from 0.2 to 750 milli-grams per liter; and hardness ranged from 69 to 940 milligrams per liter. Water was least mineralized in the recharge areas of the Lower Floridan aquifer in the western part of the study area. The most mineralized water in the Lower Floridan aquifer occurred along parts of the Wekiva and St. Johns Rivers and in much of the eastern and southern parts of the study area. The altitude of the base of freshwater in the Floridan aquifer system (where chloride concentrations are equal to 250 milligrams per liter) is variable throughout the study area. The estimated position of the 250 milligram per liter isochlor surface is less than 200 feet below sea level in much of the eastern part of the study area, including the areas along the St. Johns River in Lake, Seminole, and Volusia Counties and near the Wekiva River in western Seminole County. The altitude of the 250 milligram per liter isochlor exceeds 3,000 feet below sea level in the extreme southwestern part of the study area.","language":"ENGLISH","doi":"10.3133/wri024193","usgsCitation":"O’Reilly, A.M., Spechler, R.M., and McGurk, B.E., 2002, Hydrogeology and water-quality characteristics of the Lower Floridan aquifer in east-central Florida: U.S. Geological Survey Water-Resources Investigations Report 2002-4193, vi, 60 p. : col. ill., col. maps ; 28 cm., https://doi.org/10.3133/wri024193.","productDescription":"vi, 60 p. : col. ill., col. maps ; 28 cm.","costCenters":[],"links":[{"id":3797,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024193/","linkFileType":{"id":5,"text":"html"}},{"id":162003,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a54d4","contributors":{"authors":[{"text":"O’Reilly, Andrew M. 0000-0003-3220-1248 aoreilly@usgs.gov","orcid":"https://orcid.org/0000-0003-3220-1248","contributorId":2184,"corporation":false,"usgs":true,"family":"O’Reilly","given":"Andrew","email":"aoreilly@usgs.gov","middleInitial":"M.","affiliations":[{"id":5051,"text":"FLWSC-Orlando","active":true,"usgs":true}],"preferred":true,"id":230678,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spechler, Rick M. spechler@usgs.gov","contributorId":1364,"corporation":false,"usgs":true,"family":"Spechler","given":"Rick","email":"spechler@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":230677,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McGurk, Brian E.","contributorId":16058,"corporation":false,"usgs":true,"family":"McGurk","given":"Brian","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":230679,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":44921,"text":"wri024226 - 2002 - Magnitude and extent of arsenic and thallium concentrations in ground water and sediments at the Charleston Naval Complex, North Charleston, South Carolina, 1994-99","interactions":[],"lastModifiedDate":"2014-04-09T15:28:58","indexId":"wri024226","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":"2002-4226","title":"Magnitude and extent of arsenic and thallium concentrations in ground water and sediments at the Charleston Naval Complex, North Charleston, South Carolina, 1994-99","docAbstract":"Water-quality samples were collected quarterly\nduring 1994-99 from 604 wells screened in the\nsurficial aquifer system beneath the Charleston Naval\nComplex, North Charleston, South Carolina. Arsenic\nand thallium were selected for analysis because\nconcentrations of these metals in some wells\nconsistently exceeded the established (2001) drinking water\nmaximum contaminant levels of 10 and\n2 micrograms per liter, respectively. The analysis was\nconducted to determine the magnitude and spatial\ndistribution of arsenic and thallium in ground water at\nthe Charleston Naval Complex and to quantify arsenic\nand thallium concentrations in a dated sediment core\nfrom Shipyard Creek marsh near the southern\nboundary of the Naval Complex.\nThe surficial aquifer system beneath the\nCharleston Naval Complex consists of an unconfined\nupper surficial aquifer and a confined lower surficial\naquifer. Hydraulic connection between the two aquifers\nis limited or nonexistent throughout the system at the\nNaval Complex. The Charleston Naval Complex is\ndivided into nine operational units designated as zones\nA through I. Arsenic and thallium concentration data\nwere compiled and interpreted for the two surficial\naquifers within each zone.\nMean arsenic (n=603) and thallium (n=604)\nconcentrations were calculated for water samples from\neach well screened in the upper and lower surficial\naquifers. In the upper surficial aquifer, mean arsenic\nconcentrations ranged from 0.9 to 339 micrograms\nper liter and exceeded 10 micrograms per liter in\n29 percent of the wells. In the lower surficial aquifer,\nmean arsenic concentrations ranged from 1.0 to\n97.4 micrograms per liter and exceeded 10 micrograms\nper liter in 23 percent of the wells. The greatest number\nof water samples with mean arsenic concentrations\nexceeding 10 micrograms per liter were collected from\nwells in the upper surficial aquifer at zone E in the\nnorthwestern part of the study area.\nWell clusters, defined as three or more wells in\na solid-waste management unit or area of concern,\nwhere the mean arsenic concentration exceeded\n10 micrograms per liter, were identified in association\nwith 12 sites in the upper surficial aquifer-solid-waste\nmanagement unit 039 (a drum-storage area) in zone A;\nsolid-waste management units 044 (coal-storage area)\nand 047 (burning dump) in zone C; solid-waste\nmanagement unit 065 (lead-storage area) and area of\nconcern 556 (dry docks 3 and 4) in zone E; areas of\nconcern 609 (building 1346 gas station) and 613\n(locomotive shop) in zone F; solid-waste management\nunits 006 (public works storage yard) and 008 (oil\nsludge pit), and area of concern 709 (fuel-delivery\nsystem wells 12, 13, and 14) in zone G; and solid-waste\nmanagement units 009 (closed landfill) and 196 (south\nlandfill) in zone H. One well cluster was identified in\nthe lower surficial aquifer in association with solidwaste\nmanagement unit 009 (closed landfill) in zone H.\nMean thallium concentrations in water from all\nwells ranged from less than 1.6 to 32.6 micrograms per\nliter in water samples from the upper surficial aquifer,\nand from less than 1.6 to 67.7 micrograms per liter in\nwater samples from the lower surficial aquifer. Mean\nthallium concentrations equal to or greater than\n10 micrograms per liter were present in water samples\nfrom 21 of 604 wells (3.5 percent). Of the 21 wells,\n14 wells were located at solid-waste management unit\n009 (closed landfill) in zone H near Shipyard Creek,\n8 wells in the upper aquifer, and 6 wells in the lower aquifer. One well cluster where thallium exceeded\n10 micrograms per liter was identified in association\nwith solid-waste management unit 009 (closed landfill)\nin the upper surficial aquifer.\nMean arsenic and thallium concentrations in\nwater were calculated for all wells screened in one\naquifer and located in a single zone, and are referred to\nas zone mean concentration in this report. Zone mean\narsenic concentrations in all nine zones ranged from\n3.2 to 18 micrograms per liter in water samples from\nthe upper surficial aquifer and from 2.7 to 22 micrograms\nper liter in water samples from the lower\nsurficial aquifer. Zone mean thallium concentrations in\nall nine zones ranged from 3.2 to 13 micrograms per\nliter in water samples from the upper surficial aquifer\nand from 3.2 to 14 micrograms per liter in water\nsamples from the lower surficial aquifer.\nGround-water samples rarely had elevated\n(equal to or greater than 10 micrograms per liter)\nconcentrations of both arsenic and thallium. Water\nsamples had coincident elevated arsenic and thallium\nconcentrations in 10 wells in zone H, 1 well in zone A,\nand 1 well in zone B.\nSediment quality at Shipyard Creek marsh was\ninvestigated by collecting an 11.8-foot -long sediment\ncore (SYC-1) adjacent to zone I. The mean arsenic\nconcentration in sediment samples from SYC-1\n(n= 160) was 3.05 milligrams per kilogram plus or\nminus 0.92. The mean arsenic concentration and\nstandard deviation calculated for SYC-1 sediment\nsamples fall within the standard error for the\nbackground mean arsenic concentration reported for\nSouth Carolina sediments (1.5 milligrams per kilogram\nplus or minus 2. 7). All but one sample (core depth\n=50 inches) was less than the threshold-effects level of\n7.24 milligrams per kilogram. Acid extracts of the\nsediment samples were analyzed for thallium\nconcentration, but none were detected. These data\nindicate no obvious change in arsenic or thallium\nconcentrations with depth in the core.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Columbia, SC","doi":"10.3133/wri024226","collaboration":"Prepared in cooperation with the Southern Division Naval Facilities Engineering Command","usgsCitation":"Mirecki, J.E., and Falls, W.F., 2002, Magnitude and extent of arsenic and thallium concentrations in ground water and sediments at the Charleston Naval Complex, North Charleston, South Carolina, 1994-99: U.S. Geological Survey Water-Resources Investigations Report 2002-4226, Report: v, 37 p.;. Plate 1: 33.12 inches x 42.37 inches; Plate 2: 32.76 inches x 42.26 inches, https://doi.org/10.3133/wri024226.","productDescription":"Report: v, 37 p.;. Plate 1: 33.12 inches x 42.37 inches; Plate 2: 32.76 inches x 42.26 inches","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":162166,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri024226.jpg"},{"id":286077,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4226/report.pdf"},{"id":286075,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/2002/4226/plate-1.pdf"},{"id":286076,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/2002/4226/plate-2.pdf"}],"country":"United States","state":"South Carolina","city":"Charleston","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.973339,32.829574 ], [ -79.973339,32.871134 ], [ -79.934701,32.871134 ], [ -79.934701,32.829574 ], [ -79.973339,32.829574 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6494f6","contributors":{"authors":[{"text":"Mirecki, June Elizabeth","contributorId":48225,"corporation":false,"usgs":true,"family":"Mirecki","given":"June","email":"","middleInitial":"Elizabeth","affiliations":[],"preferred":false,"id":230683,"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":230684,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44958,"text":"wri024176 - 2002 - Interdecadal changes in the hydrometeorological regime of the Pacific Northwest and in the regional-to-hemispheric climate regimes, and their linkages","interactions":[],"lastModifiedDate":"2012-02-02T00:10:12","indexId":"wri024176","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":"2002-4176","title":"Interdecadal changes in the hydrometeorological regime of the Pacific Northwest and in the regional-to-hemispheric climate regimes, and their linkages","docAbstract":"Selected hydrometeorological (HM) data for the Pacific Northwest, and regional-to-hemispheric atmospheric-circulation data and sea-surface temperature (SST) data for the North Pacific, are examined for three successive interdecadal periods that are subsets of the instrumental record in order to estimate if their characteristics have changed. The HM data included monthly precipitation totals for 50 sites in western Washington and 29 climate divisions of the Pacific Northwest, and streamflow averages for 112 sites in Washington, Oregon, and Idaho. The atmospheric data included the Southern Oscillation Index (SOI), an index of the Pacific/North America (PNA) circulation pattern, measures of the westerly and northerly components of geostrophic flow, and a subset of the Northern Hemisphere 700-millibar geopotential height data; this subset of 162 grid points includes the area between 15 degrees and 75 degrees N, 110 degrees W and 130 degrees E. The SST data are for a 5-degree grid between 20 degrees N and 60 degrees N, 110 degrees W and 130 degrees E. The atmospheric and SST data were examined not only because the HM regime is linked to regional-to-hemispheric climate regimes, but also to estimate the extent of climate shifts displayed by these data. \r\n\r\nThree subsets of the record were identified as pre-1947 (PRE), 1947-76 (BASE), and post-1976 (POST) water years, based on an analysis of the HM data and previous studies. For each subset, means were calculated for the water year (October-September), the runoff season (March-August), the winter season (October-February), and a baseflow season (August-September). Differences in means and in ratios of the means between the BASE period and the PRE and POST periods were examined for changes.\r\n\r\nWinter-season mean precipitation during both the PRE and POST periods was smaller than the BASE period, indicating a spatially consistent and distinct change in the HM regime during winter during the PRE and POST periods. For the runoff season, mean precipitation at most sites, in comparison to the BASE period, was smaller during the PRE period and larger during POST period, indicating that different HM regimes occurred during the runoff season for the PRE and POST periods. Water-year mean precipitation was less for both the PRE and POST periods because of decreases in winter-season precipitation; however, the water-year values for the POST period were not as small as those of the PRE period because more precipitation was concentrated in the runoff season. \r\n\r\nDuring both the PRE and POST periods, the mean water-year discharge was less than the BASE period for all but 15 of the 112 sites. Fourteen of the 15 sites were in a well-defined region (southern Idaho and southeastern Oregon), and 13 of the 14 had larger means only during the POST period. Winter-season streamflow was less for all but 11 sites during both PRE and POST periods; the largest decreases in the mean, more than 30 percent, were for an area in central Oregon. Except for the sites that had larger mean water-year discharge, runoff-season means also were less than those during the BASE period. \r\n\r\nChanges in the SOI and PNA index from the BASE period were generally similar to and consistent with those of the majority of the hydrologic data; dissimilarities were in well-defined regions and are attributed to the evolutionary nature of the regime shifts. Negative values of the SOI for the POST period were more persistent than those that have occurred during both the PRE and BASE periods. The changes in the PNA index and the geostrophic flow components during the POST period are consistent with drier and warmer conditions in the Pacific Northwest. The 700-millibar data display trends and differences between the BASE and POST periods; differences in composite anomalies for selected winter months between these periods show a well-defined PNA pattern. For many areas of the North Pacific, the record of SSTs shows a significant long-term trend","language":"ENGLISH","doi":"10.3133/wri024176","usgsCitation":"Vaccaro, J.J., 2002, Interdecadal changes in the hydrometeorological regime of the Pacific Northwest and in the regional-to-hemispheric climate regimes, and their linkages: U.S. Geological Survey Water-Resources Investigations Report 2002-4176, 105 p., https://doi.org/10.3133/wri024176.","productDescription":"105 p.","costCenters":[],"links":[{"id":3832,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024176","linkFileType":{"id":5,"text":"html"}},{"id":161927,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e0973","contributors":{"authors":[{"text":"Vaccaro, J. J.","contributorId":48173,"corporation":false,"usgs":true,"family":"Vaccaro","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":230770,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44960,"text":"wri024181 - 2002 - Response of the St. Croix River pools, Wisconsin and Minnesota, to various phosphorus-loading scenarios","interactions":[],"lastModifiedDate":"2018-02-06T12:32:08","indexId":"wri024181","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":"2002-4181","title":"Response of the St. Croix River pools, Wisconsin and Minnesota, to various phosphorus-loading scenarios","docAbstract":"<p>The pools in the lower reach of the St. Croix National Scenic Riverway, Wisconsin and Minnesota, and the adjoining Lake Mallalieu, are eutrophic because of high phosphorus loading. To determine how changes in phosphorus loading would affect the trophic status of these pools, the water-quality model, BATHTUB, was used to simulate existing (1999) water quality and simulate the water quality with various phosphorus-loading scenarios. Water quality in the pools may respond differently during different flow regimes; therefore, sensitivity and scenario evaluations were performed not only for 1999, but also for a simulated period with relatively low flows throughout the basin (using flow data from 1988) and for a simulated period with relatively high flows throughout the basin (using flow data from 1996).</p>\n<p>On the basis of the BATHTUB simulations, linear increases in phosphorus loading should cause the following changes in water quality in each of the pools: linear increases in phosphorus concentrations, although at a smaller rate than the increase in loading; non-linear increases in chlorophyll a concentrations, with a smaller relative response with higher phosphorus loading; increase in the frequency of algal blooms, with a higher frequency of intense algal blooms; and slightly decreased water clarity.</p>\n<p>The response in water quality to changes in the phosphorus loading should be relatively similar regardless of the flow regime. Reducing phosphorus loading by about 50 percent would be necessary for the Lake St. Croix pools to be classified as mesotrophic with respect to phosphorus and chlorophyll a concentrations, whereas a larger reduction in phosphorus loading would be needed for Lake Mallalieu to be classified as mesotrophic. Even with these reductions, water clarity will remain poor because of the high non-algal turbidity and stained water in the pools.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri024181","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Robertson, D.M., and Lenz, B.N., 2002, Response of the St. Croix River pools, Wisconsin and Minnesota, to various phosphorus-loading scenarios: U.S. Geological Survey Water-Resources Investigations Report 2002-4181, vi, 36 p., https://doi.org/10.3133/wri024181.","productDescription":"vi, 36 p.","numberOfPages":"43","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":3834,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://wi.water.usgs.gov/pubs/wrir-02-4181/","linkFileType":{"id":5,"text":"html"}},{"id":82252,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4181/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162006,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2002/4181/report-thumb.jpg"}],"country":"United States","state":"Minnesota, Wisconsin","otherGeospatial":"St. Croix River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -92.8729248046875,\n              46.1912395780416\n            ],\n            [\n              -93.394775390625,\n              45.924408558629004\n            ],\n            [\n              -93.5980224609375,\n              45.60250901510302\n            ],\n            [\n              -93.71337890625,\n              45.251688256117646\n            ],\n            [\n              -93.5650634765625,\n              45.19752230305685\n            ],\n            [\n              -93.306884765625,\n              45.023067895446175\n            ],\n            [\n              -93.0267333984375,\n              44.87144275016589\n            ],\n            [\n              -92.9608154296875,\n              44.695992981720714\n            ],\n            [\n              -92.625732421875,\n              44.50434127765394\n            ],\n            [\n              -92.274169921875,\n              44.35920579433503\n            ],\n            [\n              -91.9940185546875,\n              44.42593442145313\n            ],\n            [\n              -91.93359375,\n              44.55133484083592\n            ],\n            [\n              -92.1148681640625,\n              45.42544355958045\n            ],\n            [\n              -92.16430664062499,\n              45.67932023569538\n            ],\n            [\n              -92.0599365234375,\n              46.00459325574482\n            ],\n            [\n              -92.3236083984375,\n              46.3886223381617\n            ],\n            [\n              -92.74108886718749,\n              46.426499019253\n            ],\n            [\n              -92.8729248046875,\n              46.1912395780416\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f782f","contributors":{"authors":[{"text":"Robertson, Dale M. 0000-0001-6799-0596 dzrobert@usgs.gov","orcid":"https://orcid.org/0000-0001-6799-0596","contributorId":150760,"corporation":false,"usgs":true,"family":"Robertson","given":"Dale","email":"dzrobert@usgs.gov","middleInitial":"M.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230773,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lenz, Bernard N.","contributorId":85170,"corporation":false,"usgs":true,"family":"Lenz","given":"Bernard","email":"","middleInitial":"N.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":230774,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44969,"text":"wri024037 - 2002 - Traveltime characteristics of Gore Creek and Black Gore Creek, upper Colorado River basin, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:10:12","indexId":"wri024037","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":"2002-4037","title":"Traveltime characteristics of Gore Creek and Black Gore Creek, upper Colorado River basin, Colorado","docAbstract":"In the Rocky Mountains of Colorado, major highways are often constructed in stream valleys. In the event of a vehicular accident involving hazardous materials, the close proximity of highways to the streams increases the risk of contamination entering the streams. Recent population growth has contributed to increased traffic volume along Colorado highways and has resulted in increased movement of hazardous materials, particularly along Interstate 70. \r\n\r\nGore Creek and its major tributary, Black Gore Creek, are vulnerable to such contamination from vehicular accidents along Interstate 70. Gore Creek, major tributary of the Eagle River, drains approximately 102 square miles, some of which has recently undergone significant urban development. The headwaters of Gore Creek originate in the Gore Range in the eastern part of the Gore Creek watershed. Gore Creek flows west to the Eagle River. Beginning at the watershed boundary on Vail Pass, southeast of Vail Ski Resort, Interstate 70 parallels Black Gore Creek and then closely follows Gore Creek the entire length of the watershed. Interstate 70 crosses Gore Creek and tributaries 20 times in the watershed. \r\n\r\nIn the event of a vehicular accident involving a contaminant spill into Gore Creek or Black Gore Creek, a stepwise procedure has been developed for water-resource managers to estimate traveltimes of the leading edge and peak concentration of a conservative contaminant. An example calculating estimated traveltimes for a hypothetical contaminant release in Black Gore Creek is provided. \r\n\r\nTraveltime measurements were made during May and September along Black Gore Creek and Gore Creek from just downstream from the Black Lakes to the confluence with the Eagle River to account for seasonal variability in stream discharge. Fluorometric dye injection of rhodamine WT and downstream dye detection by fluorometry were used to measure traveltime characteristics of Gore Creek and Black Gore Creek. During the May traveltime measurements, discharges ranged from 82 cubic feet per second (ft3/s) at Black Gore Creek near Minturn (U.S. Geological Survey station number 09066000) to 724 ft3/s at Gore Creek at mouth near Minturn (U.S. Geological Survey station number 09066510), whereas during the September traveltime measurements, discharges ranged from 3.6 ft3/s at Black Gore Creek near Minturn to 62 ft3/s at Gore Creek at mouth near Minturn. Cumulative traveltimes for the peak dye concentration during the May traveltime measurements ranged from 3.45 hours (site 1 to site 3) in Black Gore Creek to 2.50 hours (site 8 to site 12) in Gore Creek, whereas cumulative traveltimes for the peak dye concentration during the September traveltime measurements ranged from 15.33 hours (site 1 to site 3) in Black Gore Creek to 8.65 hours (site 8 to site 12) in Gore Creek. During the September dye injections, beaver dams on Black Gore Creek, between site 1 and the confluence with Gore Creek, substantially delayed movement of the rhodamine WT. \r\n\r\nEstimated traveltimes were developed using relations established from linear-regression methods of relating measured peak traveltime to discharge during those measurements, which were obtained at Black Gore Creek near Minturn and Gore Creek at mouth near Minturn. Resulting estimated peak traveltimes for Black Gore Creek (sites 1 to 5) ranged from 5.4 to 0.4 hour for 20 to 200 ft3/s and for Gore Creek (sites 5 to 12), 5.5 to 0.3 hour for 20 to 800 ft3/s. \r\n\r\nLongitudinal-dispersion coefficients that were calculated for selected stream reaches ranged from 17.2 square feet per second at 4 ft3/s between sites 2 and 3 to 650 square feet per second at 144 ft3/s between sites 7 and 8. Longitudinal-dispersion coefficients are necessary variables for future stream-contaminant modeling in the Gore Creek watershed.","language":"ENGLISH","doi":"10.3133/wri024037","usgsCitation":"Gurdak, J., Spahr, N.E., and Szmajter, R.J., 2002, Traveltime characteristics of Gore Creek and Black Gore Creek, upper Colorado River basin, Colorado: U.S. Geological Survey Water-Resources Investigations Report 2002-4037, vi, 14 p. : ill. (some col.), col. map ; 28 cm., https://doi.org/10.3133/wri024037.","productDescription":"vi, 14 p. : ill. (some col.), col. map ; 28 cm.","costCenters":[],"links":[{"id":3842,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri02-4037","linkFileType":{"id":5,"text":"html"}},{"id":162445,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697dd5","contributors":{"authors":[{"text":"Gurdak, Jason J.","contributorId":65125,"corporation":false,"usgs":true,"family":"Gurdak","given":"Jason J.","affiliations":[],"preferred":false,"id":230796,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spahr, Norman E. nspahr@usgs.gov","contributorId":1977,"corporation":false,"usgs":true,"family":"Spahr","given":"Norman","email":"nspahr@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":230794,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Szmajter, Richard J.","contributorId":58315,"corporation":false,"usgs":true,"family":"Szmajter","given":"Richard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":230795,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":44971,"text":"wri024039 - 2002 - Hydrology and water quality of Geneva Lake, Walworth County, Wisconsin","interactions":[],"lastModifiedDate":"2018-02-06T12:32:00","indexId":"wri024039","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":"2002-4039","title":"Hydrology and water quality of Geneva Lake, Walworth County, Wisconsin","docAbstract":"<p>As part of continuing efforts to improve the water quality of Geneva Lake, a collaborative effort between the U.S. Geological Survey, the Wisconsin Department of Natural Resources, and the Geneva Lake Environmental Agency was initiated in 1997 to document the present quality of the lake and its sediments, compute detailed hydrologic and nutrient (primarily phosphorus) budgets for the lake, estimate how changes in nutrient loading may affect water quality, and describe changes in the lake over the past 170 years by comparing water quality measured in this study with historical measurements and sediment-core information. This report presents the results of this collaborative study.</p>\n<p>Measurements collected during this study (1997.2000) indicate that the trophic status of the lake ranges from mesotrophic to oligotrophic: the mean Secchi depth was 4.8 m (meters), mean surface phosphorus concentration was 9 ?g/L (micrograms per liter), mean surface nitrogen concentration was 550 ?g/L, and mean surface chlorophyll a concentration was 3 ?g/L. Surface nitrogen: phosphorus ratios indicated that, if just these nutrients are considered, phosphorus should be the limiting nutrient.</p>\n<p>Phosphorus budgets constructed for water years 1998 and 1999 indicate that recent annual phosphorus loads were about 2,000 kg (kilograms) less than that estimated in 1975 (total annual input was about 3,200 kg in 1998 and about 8,500 kg in 1999). The major source of phosphorus to the lake was from its tributaries, which contributed about 84 percent of the total load. The primary difference from the phosphorus load estimates for 1975 was the decrease in loading from the Fontana sewage-treatment plant.</p>\n<p>Direct measurements and indirect measurements based on sediment-core analyses indicate that the water quality of Geneva Lake has degraded in the last 170 years, the greatest effects resulting from urbanization. Sedimentation rates were highest between 1900 to 1930, and phosphorus concentrations were highest between the 1930s to early 1980s. As a result of the recent reduction in phosphorus loading, in-lake near-surface phosphorus concentrations decreased from 20.25 ?g/L to about 10.15 ?g/L and are similar to those estimated for the lake in the early 1900s. Concentrations of other chemical constituents associated with urban areas, however, have continually increased, especially in Williams Bay and Geneva Bay.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri024039","collaboration":"Prepared in cooperation with the Geneva Lake Environmental Agency, Wisconsin Department of Natural Resources","usgsCitation":"Robertson, D.M., Goddard, G.L., Mergener, E.A., Rose, W., and Garrision, P.J., 2002, Hydrology and water quality of Geneva Lake, Walworth County, Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 2002-4039, viii, 73 p., https://doi.org/10.3133/wri024039.","productDescription":"viii, 73 p.","numberOfPages":"86","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":82254,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4039/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":125128,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2002/4039/report-thumb.jpg"},{"id":3844,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://wi.water.usgs.gov/pubs/wrir-02-4039/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Wisconsin","county":"Walworth County","otherGeospatial":"Lake Geneva","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.42277526855469,\n              42.62082311949496\n            ],\n            [\n              -88.44543457031249,\n              42.609200852328264\n      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dzrobert@usgs.gov","orcid":"https://orcid.org/0000-0001-6799-0596","contributorId":150760,"corporation":false,"usgs":true,"family":"Robertson","given":"Dale","email":"dzrobert@usgs.gov","middleInitial":"M.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230798,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goddard, Gerald L.","contributorId":35721,"corporation":false,"usgs":true,"family":"Goddard","given":"Gerald","email":"","middleInitial":"L.","affiliations":[{"id":676,"text":"Wisconsin Water Resource Division","active":false,"usgs":true}],"preferred":false,"id":230800,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mergener, Elizabeth A.","contributorId":43442,"corporation":false,"usgs":true,"family":"Mergener","given":"Elizabeth","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":230801,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rose, William J. wjrose@usgs.gov","contributorId":2182,"corporation":false,"usgs":true,"family":"Rose","given":"William J.","email":"wjrose@usgs.gov","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":230799,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Garrision, Paul J.","contributorId":84628,"corporation":false,"usgs":true,"family":"Garrision","given":"Paul","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":230802,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":44977,"text":"wri024086 - 2002 - Testing the sensitivity of pumpage to increases in surficial aquifer system heads in the Cypress Creek well-field area, west-central Florida — An optimization technique","interactions":[],"lastModifiedDate":"2021-12-14T22:59:39.732938","indexId":"wri024086","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":"2002-4086","title":"Testing the sensitivity of pumpage to increases in surficial aquifer system heads in the Cypress Creek well-field area, west-central Florida — An optimization technique","docAbstract":"Tampa Bay depends on ground water for most of the water supply. Numerous wetlands and lakes in Pasco County have been impacted by the high demand for ground water. Central Pasco County, particularly the area within the Cypress Creek well field, has been greatly affected. Probable causes for the decline in surface-water levels are well-field pumpage and a decade-long drought. Efforts are underway to increase surface-water levels by developing alternative sources of water supply, thus reducing the quantity of well-field pumpage. \r\n\r\nNumerical ground-water flow simulations coupled with an optimization routine were used in a series of simulations to test the sensitivity of optimal pumpage to desired increases in surficial aquifer system heads in the Cypress Creek well field. The ground-water system was simulated using the central northern Tampa Bay ground-water flow model. Pumping solutions for 1987 equilibrium conditions and for a transient 6-month timeframe were determined for five test cases, each reflecting a range of desired target recovery heads at different head control sites in the surficial aquifer system. Results are presented in the form of curves relating average head recovery to total optimal pumpage. Pumping solutions are sensitive to the location of head control sites formulated in the optimization problem and as expected, total optimal pumpage decreased when desired target head increased. The distribution of optimal pumpage for individual production wells also was significantly affected by the location of head control sites. \r\n\r\nA pumping advantage was gained for test-case formulations where hydraulic heads were maximized in cells near the production wells, in cells within the steady-state pumping center cone of depression, and in cells within the area of the well field where confining-unit leakance is the highest. More water was pumped and the ratio of head recovery per unit decrease in optimal pumpage was more than double for test cases where hydraulic heads are maximized in cells located at or near the production wells. \r\n\r\nAdditionally, the ratio of head recovery per unit decrease in pumpage was about three times more for the area where confining-unit leakance is the highest than for other leakance zone areas of the well field. For many head control sites, optimal heads corresponding to optimal pumpage deviated from the desired target recovery heads. Overall, pumping solutions were constrained by the limiting recovery values, initial head conditions, and by upper boundary conditions of the ground-water flow model.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri024086","usgsCitation":"Yobbi, D.K., 2002, Testing the sensitivity of pumpage to increases in surficial aquifer system heads in the Cypress Creek well-field area, west-central Florida — An optimization technique: U.S. Geological Survey Water-Resources Investigations Report 2002-4086, iv, 20 p., https://doi.org/10.3133/wri024086.","productDescription":"iv, 20 p.","costCenters":[],"links":[{"id":162266,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":392919,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52032.htm"},{"id":3850,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024086","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Florida","otherGeospatial":"Cypress Creek well-field area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.935791015625,\n              27.950738722228763\n            ],\n            [\n              -82.2930908203125,\n              27.950738722228763\n            ],\n            [\n              -82.2930908203125,\n              28.53144857631924\n            ],\n            [\n              -82.935791015625,\n              28.53144857631924\n            ],\n            [\n              -82.935791015625,\n              27.950738722228763\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db6846d3","contributors":{"authors":[{"text":"Yobbi, Dann K.","contributorId":15247,"corporation":false,"usgs":true,"family":"Yobbi","given":"Dann","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":230819,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":45034,"text":"wri014025 - 2002 - Aquifer geochemistry and effects of pumping on ground-water quality at the Green Belt Parkway Well Field, Holbrook, Long Island, New York","interactions":[],"lastModifiedDate":"2017-04-04T13:42:05","indexId":"wri014025","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":"2001-4025","title":"Aquifer geochemistry and effects of pumping on ground-water quality at the Green Belt Parkway Well Field, Holbrook, Long Island, New York","docAbstract":"<p>Geochemistry, microbiology, and water quality of the Magothy aquifer at a new supply well in Holbrook were studied to help identify factors that contribute to iron-related biofouling of public-supply wells. The organic carbon content of borehole sediments from the screen zone, and the dominant terminal electron-accepting processes (TEAPs), varied by depth. TEAP assays of core sediments indicated that iron reduction, sulfate reduction, and undetermined (possibly oxic) reactions and microbial activity are correlated with organic carbon (lignite) content. The quality of water from this well, therefore, reflects the wide range of aquifer microenvironments at this site.</p><p>High concentrations of dissolved iron (3.6 to 6.4 micromoles per liter) in water samples from this well indicate that some water is derived from Fe(III)-reducing sediments within the aquifer, but traces of dissolved oxygen indicate inflow of shallow, oxygenated water from shallow units that overlie the local confining units. Water-quality monitoring before and during a 2-day pumping test indicates that continuous pumping from the Magothy aquifer at this site can induce downward flow of shallow, oxygenated water despite the locally confined conditions. Average concentrations of dissolved oxygen are high (5.2 milligrams per liter, or mg/L) in the overlying upper glacial aquifer and at the top of the Magothy aquifer (4.3 mg/L), and low ( &lt; 0.1 mg/L) in the deeper, anaerobic part of the Magothy; average concentrations of phosphate are high (0.4 mg/L) in the upper glacial aquifer and lower (0.008 mg/L) at the top of the Magothy aquifer and in the deeper part of the Magothy (0.013 mg/L). Concentrations of both constituents increased during the 2 days of pumping. The δ<sup>34</sup>S of sulfate in shallow ground water from observation wells (3.8 to 6.4 per mil) was much heavier than that in the supplywell water (-0.1 per mil) and was used to help identify sources of water entering the supply well. The δ<sup>34</sup>S of sulfate in a deep observation well adjacent to the supply well increased from 2.4 per mil before pumping to 3.3 per mil after pumping; this confirms that the pumping induced downward migration of water. The lighter δ<sup>34</sup>S value in the pumped water than in the adjacent observation well probably indicates FeS<sub>2</sub> oxidation (which releases light δ<sup>34</sup>S in adjacent sediments) by the downward flow of oxygenated water.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri014025","collaboration":"Prepared in cooperation with the Suffolk County Water Authority","usgsCitation":"Brown, C., Colabufo, S., and Coates, J.D., 2002, Aquifer geochemistry and effects of pumping on ground-water quality at the Green Belt Parkway Well Field, Holbrook, Long Island, New York: U.S. Geological Survey Water-Resources Investigations Report 2001-4025, v, 21 p., https://doi.org/10.3133/wri014025.","productDescription":"v, 21 p.","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":3897,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2001/4025/wri014025.pdf","text":"Report","size":"539 KB","linkFileType":{"id":1,"text":"pdf"},"description":"WRIR 2001-4025"},{"id":135785,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2001/4025/coverthb.jpg"}],"country":"United States","state":"New York","city":"Holbrook","otherGeospatial":"Long Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.23898315429688,\n              40.68584503000695\n            ],\n            [\n              -72.87918090820312,\n              40.68584503000695\n            ],\n            [\n              -72.87918090820312,\n              40.99855696412671\n            ],\n            [\n              -73.23898315429688,\n              40.99855696412671\n            ],\n            [\n              -73.23898315429688,\n              40.68584503000695\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p>Director, New York Water Science Center<br> U.S. Geological Survey<br> 425 Jordan Rd<br> Troy, NY 12180<br> (518) 285-5695 <br> <a href=\"http://ny.water.usgs.gov\" data-mce-href=\"http://ny.water.usgs.gov\">http://ny.water.usgs.gov/</a></p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Study Methods</li><li>Aquifer Geochemistry</li><li>Effects of Pumping on Ground-Water Quality</li><li>Conclusions</li><li>References Cited</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679f8d","contributors":{"authors":[{"text":"Brown, Craig J.","contributorId":104450,"corporation":false,"usgs":true,"family":"Brown","given":"Craig J.","affiliations":[],"preferred":false,"id":230967,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Colabufo, Steven","contributorId":94652,"corporation":false,"usgs":true,"family":"Colabufo","given":"Steven","affiliations":[],"preferred":false,"id":230966,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coates, John D.","contributorId":107667,"corporation":false,"usgs":true,"family":"Coates","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":230968,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":40858,"text":"ofr02244 - 2002 - Potentiometric surface of the Aquia aquifer in southern Maryland, September 2000","interactions":[],"lastModifiedDate":"2022-10-04T20:29:33.761672","indexId":"ofr02244","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":"2002-244","title":"Potentiometric surface of the Aquia aquifer in southern Maryland, September 2000","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02244","usgsCitation":"Curtin, S.E., Andreasen, D., and Wheeler, J.C., 2002, Potentiometric surface of the Aquia aquifer in southern Maryland, September 2000: U.S. Geological Survey Open-File Report 2002-244, 1 Plate: 11.38 × 14.67 inches, https://doi.org/10.3133/ofr02244.","productDescription":"1 Plate: 11.38 × 14.67 inches","costCenters":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"links":[{"id":407883,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52799.htm","linkFileType":{"id":5,"text":"html"}},{"id":78735,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0244/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":171430,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2002/0244/report-thumb.jpg"}],"country":"United States","state":"Maryland","otherGeospatial":"Aquia aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77,\n              38.1083\n            ],\n            [\n              -76,\n              38.1083\n            ],\n            [\n              -76,\n              39.0778\n            ],\n            [\n              -77,\n              39.0778\n            ],\n            [\n              -77,\n              38.1083\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db68307b","contributors":{"authors":[{"text":"Curtin, Stephen E. securtin@usgs.gov","contributorId":3703,"corporation":false,"usgs":true,"family":"Curtin","given":"Stephen","email":"securtin@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":224060,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreasen, David C.","contributorId":59003,"corporation":false,"usgs":true,"family":"Andreasen","given":"David C.","affiliations":[],"preferred":false,"id":224062,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wheeler, Judith C.","contributorId":13620,"corporation":false,"usgs":true,"family":"Wheeler","given":"Judith","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":224061,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":69627,"text":"i2776 - 2002 - Geologic map of the southern Ivrea-Verbano zone, northwestern Italy","interactions":[],"lastModifiedDate":"2012-02-10T00:11:34","indexId":"i2776","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":"2776","title":"Geologic map of the southern Ivrea-Verbano zone, northwestern Italy","language":"ENGLISH","doi":"10.3133/i2776","isbn":"060792120X","usgsCitation":"Quick, J.E., Sinigoi, S., Snoke, A., Kalakay, T., Mayer, A., and Peressini, G., 2002, Geologic map of the southern Ivrea-Verbano zone, northwestern Italy: U.S. Geological Survey IMAP 2776, 1 map : col. ; 111 x 78 cm., on sheet 145 x 102 cm., folded in envelope 30 x 24 cm. + 1 pamphlet (22 p. : ill., maps ; 28 cm.) , https://doi.org/10.3133/i2776.","productDescription":"1 map : col. ; 111 x 78 cm., on sheet 145 x 102 cm., folded in envelope 30 x 24 cm. + 1 pamphlet (22 p. : ill., maps ; 28 cm.) ","costCenters":[],"links":[{"id":191650,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/2776/report-thumb.jpg"},{"id":91721,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2776/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91722,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/2776/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 80.08333333333333,45.65 ], [ 80.08333333333333,45.9 ], [ 80.33333333333333,45.9 ], [ 80.33333333333333,45.65 ], [ 80.08333333333333,45.65 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688896","contributors":{"authors":[{"text":"Quick, James E.","contributorId":21552,"corporation":false,"usgs":true,"family":"Quick","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":280757,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sinigoi, S.","contributorId":77245,"corporation":false,"usgs":true,"family":"Sinigoi","given":"S.","affiliations":[],"preferred":false,"id":280760,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Snoke, A.W.","contributorId":14899,"corporation":false,"usgs":true,"family":"Snoke","given":"A.W.","email":"","affiliations":[],"preferred":false,"id":280756,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kalakay, T.J.","contributorId":46180,"corporation":false,"usgs":true,"family":"Kalakay","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":280758,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mayer, A.","contributorId":96780,"corporation":false,"usgs":true,"family":"Mayer","given":"A.","email":"","affiliations":[],"preferred":false,"id":280761,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Peressini, G.","contributorId":49876,"corporation":false,"usgs":true,"family":"Peressini","given":"G.","email":"","affiliations":[],"preferred":false,"id":280759,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":54168,"text":"wdrGA022 - 2002 - Water Resources Data, Georgia, 2002--Volume 2: Continuous ground-water-level data, and periodic surface-water- and ground-water-quality data, Calendar Year 2002","interactions":[],"lastModifiedDate":"2018-12-04T10:50:15","indexId":"wdrGA022","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":"GA-02-2","title":"Water Resources Data, Georgia, 2002--Volume 2: Continuous ground-water-level data, and periodic surface-water- and ground-water-quality data, Calendar Year 2002","docAbstract":"Water resources data for the 2002 water year for Georgia consists of records of stage, discharge, and water quality of streams; and the stage and contents of lakes and reservoirs published in two volumes in a digital format on a CD-ROM. Volume one of this report contains water resources data for Georgia collected during water year 2002, including: discharge records of 154 gaging stations; stage for 165 gaging stations; precipitation for 105 gaging stations; information for 20 lakes and reservoirs; continuous water-quality records for 27 stations; the annual peak stage and annual peak discharge for 72 crest-stage partial-record stations; and miscellaneous streamflow measurements at 50 stations, and miscellaneous water-quality data recorded by the NAWQA program in Georgia. Volume two of this report contains water resources data for Georgia collected during calendar year 2002, including continuous water-level records of 155 ground-water wells and periodic records at 132 water-quality stations. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Georgia.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrGA022","collaboration":"Prepared in cooperation with the State of Georgia and other agencies","usgsCitation":"Coffin, R., Grams, S.C., Leeth, D.C., and Peck, M., 2002, Water Resources Data, Georgia, 2002--Volume 2: Continuous ground-water-level data, and periodic surface-water- and ground-water-quality data, Calendar Year 2002: U.S. Geological Survey Water Data Report GA-02-2, vii, 564 p., https://doi.org/10.3133/wdrGA022.","productDescription":"vii, 564 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":5614,"rank":100,"type":{"id":15,"text":"Index 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,{"id":32684,"text":"fs07802 - 2002 - Availability of Ground-Water Data for California, Water Year 2001","interactions":[],"lastModifiedDate":"2012-02-02T00:09:15","indexId":"fs07802","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":"078-02","title":"Availability of Ground-Water Data for California, Water Year 2001","language":"ENGLISH","doi":"10.3133/fs07802","usgsCitation":"Huff, J., 2002, Availability of Ground-Water Data for California, Water Year 2001: U.S. Geological Survey Fact Sheet 078-02, NA, https://doi.org/10.3133/fs07802.","productDescription":"NA","costCenters":[],"links":[{"id":119422,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_078_02.jpg"},{"id":3260,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/FS/fs07802/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667fa7","contributors":{"authors":[{"text":"Huff, Julia A.","contributorId":23130,"corporation":false,"usgs":true,"family":"Huff","given":"Julia A.","affiliations":[],"preferred":false,"id":208923,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":54182,"text":"wdrNC011A - 2002 - Water resources data, North Carolina, water year 2001. Volume 1A: Surface-water records","interactions":[],"lastModifiedDate":"2017-01-18T14:32:58","indexId":"wdrNC011A","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":"NC-01-1A","title":"Water resources data, North Carolina, water year 2001. Volume 1A: Surface-water records","docAbstract":"Water-resources data for the 2001 water year for North Carolina consist of records of stage, discharge, water-quality for streams; stage and contents for lakes and reservoirs; precipitation; and ground water levels and water-quality of ground-water. Volume 1 contains discharge records for 209 gaging stations; stage and contents for 62 lakes and reservoirs; stage for 52 gaging stations; water quality for 101 gaging stations and 91 miscellaneous sites; continuous daily tide stage at 4 sites; and continuous precipitation at 98 sites. Volume 2 contains ground-water-level data from 136 observation wells and ground-water-quality data from 68 wells. Additional water data were collected at 84 sites not involved in the systematic data-collection program, and are published as miscellaneous measurements in Volume 1. The collection of water-resources data in North Carolina is a part of the National Water-Data System operated by the U.S. Geological Survey in cooperation with State, municipal, and Federal agencies.","language":"ENGLISH","doi":"10.3133/wdrNC011A","usgsCitation":"Ragland, B., Walters, D.A., Cartano, G., and Taylor, J., 2002, Water resources data, North Carolina, water year 2001. 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A.","contributorId":21994,"corporation":false,"usgs":true,"family":"Walters","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":249447,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cartano, G.D.","contributorId":87201,"corporation":false,"usgs":true,"family":"Cartano","given":"G.D.","email":"","affiliations":[],"preferred":false,"id":249450,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Taylor, J.E.","contributorId":23613,"corporation":false,"usgs":true,"family":"Taylor","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":249448,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":54280,"text":"wdrWV011 - 2002 - Water resources data West Virginia water wear 2001","interactions":[],"lastModifiedDate":"2012-02-02T00:11:59","indexId":"wdrWV011","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":"WV-01-1","title":"Water resources data West Virginia water wear 2001","docAbstract":"Water-resources data for the 2001 water year for West Virginia consist of records of discharge and water quality\r\nof streams and water levels of observation wells. This report contains discharge records for 65 streamflow-gaging\r\nstations; discharge records provided by adjacent states for 7 streamflow-gaging stations; annual maximum\r\ndischarge at 18 crest-stage partial-record stations; water-quality records for 4 stations; and water-level records for\r\n10 observation wells. Locations of these sites are shown on figures 4 and 5. Additional water data were collected\r\nat various sites, not involved in the systematic data collection program, and are published as miscellaneous sites.\r\nThese data represent that part of the National Water Data System collected by the U.S. Geological Survey and\r\ncooperating State and Federal agencies in West Virginia.","language":"ENGLISH","doi":"10.3133/wdrWV011","usgsCitation":"Ward, S., Taylor, B., and Crosby, G., 2002, Water resources data West Virginia water wear 2001: U.S. Geological Survey Water Data Report WV-01-1, 280 p., https://doi.org/10.3133/wdrWV011.","productDescription":"280 p.","costCenters":[],"links":[{"id":182129,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5394,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/WDR-WV-01-1/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a01e4b07f02db5f7f01","contributors":{"authors":[{"text":"Ward, S.M.","contributorId":93920,"corporation":false,"usgs":true,"family":"Ward","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":249747,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, B.C.","contributorId":30686,"corporation":false,"usgs":true,"family":"Taylor","given":"B.C.","email":"","affiliations":[],"preferred":false,"id":249745,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crosby, G.R.","contributorId":59875,"corporation":false,"usgs":true,"family":"Crosby","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":249746,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":54167,"text":"wdrGA021 - 2002 - Water Resources Data, Georgia, 2002--Volume 1: Continuous water-level, streamflow, water-quality data, and periodic water-quality data, Water Year 2002","interactions":[],"lastModifiedDate":"2018-12-04T10:47:56","indexId":"wdrGA021","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":"GA-02-1","title":"Water Resources Data, Georgia, 2002--Volume 1: Continuous water-level, streamflow, water-quality data, and periodic water-quality data, Water Year 2002","docAbstract":"Water resources data for the 2002 water year for Georgia consists of records of stage, discharge, and water quality of streams; and the stage and contents of lakes and reservoirs published in two volumes in a digital format on a CD-ROM. Volume one of this report contains water resources data for Georgia collected during water year 2002, including: discharge records of 154 gaging stations; stage for 165 gaging stations; precipitation for 105 gaging stations; information for 20 lakes and reservoirs; continuous water-quality records for 27 stations; the annual peak stage and annual peak discharge for 72 crest-stage partial-record stations; and miscellaneous streamflow measurements at 50 stations, and miscellaneous water-quality data recorded by the NAWQA program in Georgia. Volume two of this report contains water resources data for Georgia collected during calendar year 2002, including continuous water-level records of 155 ground-water wells and periodic records at 132 water-quality stations. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Georgia.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrGA021","collaboration":"Prepared in cooperation with the State of Georgia and other agencies","usgsCitation":"Hickey, A.C., Kerestes, J.F., and McCallum, B.E., 2002, Water Resources Data, Georgia, 2002--Volume 1: Continuous water-level, streamflow, water-quality data, and periodic water-quality data, Water Year 2002: U.S. Geological Survey Water Data Report GA-02-1, vii, 1766 p., https://doi.org/10.3133/wdrGA021.","productDescription":"vii, 1766 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":5613,"rank":100,"type":{"id":15,"text":"Index 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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 cover","indexId":"70188493","publicationYear":"2002","noYear":false,"chapter":"2","title":"Land cover"},"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":6},{"subject":{"id":70188494,"text":"70188494 - 2002 - The porcupine caribou herd","indexId":"70188494","publicationYear":"2002","noYear":false,"chapter":"3","title":"The porcupine 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":7},{"subject":{"id":70188496,"text":"70188496 - 2002 - The central arctic caribou 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":"<p>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.</p><p>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.</p><p>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.</p><p>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.</p><p>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.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"2002, Arctic Refuge coastal plain terrestrial wildlife research summaries: Biological Science Report 2002-0001, x, 75 p.","productDescription":"x, 75 p.","startPage":"1","endPage":"75","numberOfPages":"90","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":177857,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bsr/2002/0001/report-thumb.jpg"},{"id":14106,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bsr/2002/0001/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Canada, United States","state":"Alaska, Northwest Territories, Yukon Territory","otherGeospatial":"Arctic Refuge Coastal Plain, Arctic National Wildlife Refuge","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -152.2265625,\n              66.16051056018838\n            ],\n            [\n              -129.5947265625,\n              66.16051056018838\n            ],\n            [\n              -129.5947265625,\n              70.74347779138229\n            ],\n            [\n              -152.2265625,\n              70.74347779138229\n            ],\n            [\n              -152.2265625,\n              66.16051056018838\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e499fe4b07f02db5bd2d4","contributors":{"editors":[{"text":"Douglas, David C. 0000-0003-0186-1104 ddouglas@usgs.gov","orcid":"https://orcid.org/0000-0003-0186-1104","contributorId":150115,"corporation":false,"usgs":true,"family":"Douglas","given":"David C.","email":"ddouglas@usgs.gov","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true},{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":694664,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Reynolds, Patricia E.","contributorId":71056,"corporation":false,"usgs":true,"family":"Reynolds","given":"Patricia","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":694665,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Rhode, E. 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,{"id":54877,"text":"wdrOH012 - 2002 - Water resources data, Ohio, water year 2001, volume 2. St. Lawrence River Basin and statewide project data","interactions":[],"lastModifiedDate":"2019-05-21T16:20:47","indexId":"wdrOH012","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–01–2","displayTitle":"Water Resources Data, Ohio, Water Year 2001, Volume 2. St. Lawrence River Basin and Statewide Project Data","title":"Water resources data, Ohio, water year 2001, volume 2. St. Lawrence River Basin and statewide 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/wdrOH012","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 2. 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 \"}}]}","contact":"<p><a href=\"https://www.usgs.gov/centers/oki-water/\" data-mce-href=\"https://www.usgs.gov/centers/oki-water/\">Director, Ohio Water Science Center</a><br>U.S. Geological Survey<br>6460 Busch Blvd.<br>Columbus, OH 43229-1737</p>","tableOfContents":"<ul><li>Preface</li><li>Report documentation page</li><li>Surface-water stations, in downstream order, for which records are published</li><li>Ground-water stations for which records are published</li><li>List of discontinued surface-water-discharge stations</li><li>List of discontinued surface-water-quality stations</li><li>Introduction</li><li>Cooperation</li><li>Summary of hydrologic conditions</li><li>Special networks and program</li><li>Explanation of the records</li><li>Access to USGS water data</li><li>Definition of terms</li><li>Publications on techniques of water-resources investigations</li><li>Surface-water records</li><li>Peak discharge and stage at continuous-record surface discharge stations</li><li>Ground-water records</li><li>Project data</li><li>Index</li><li>Factors for converting inch-pound units to International System units (SI)</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faee2","contributors":{"authors":[{"text":"Shindel, H.L.","contributorId":17652,"corporation":false,"usgs":true,"family":"Shindel","given":"H.L.","affiliations":[],"preferred":false,"id":251860,"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":251861,"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":251862,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"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":"<p>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.\"</p>","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 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