{"pageNumber":"1847","pageRowStart":"46150","pageSize":"25","recordCount":68934,"records":[{"id":57628,"text":"wdrFL881A - 1989 - Water Resources Data for Florida, Water Year 1988. Volume 1A. Northeast Florida - Surface Water","interactions":[],"lastModifiedDate":"2025-05-27T16:53:47.993773","indexId":"wdrFL881A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"FL-88-1A","title":"Water Resources Data for Florida, Water Year 1988. Volume 1A. Northeast Florida - Surface Water","docAbstract":"<p>Water-resources data for the 1988 water year in Florida consist of continuous or daily discharge for 338 streams, periodic discharge for 34 streams, miscellaneous discharge for 28 streams, continuous or daily stage for 152 streams, periodic stage for 29 streams, peak discharge for 71 streams, continuous daily tide stage 8, and peak stage for 84 streams; continuous or daily elevations for 73 lakes, periodic elevations for 72 lakes; continuous ground-water levels for 490 wells, periodic ground-water levels for 1,620 wells, and miscellaneous water-level measurements for 2,678 wells; quality-of-water data for 158 surface-water sites and 884 wells.</p><p>The data for northeast Florida include continuous or daily discharge for 132 streams, periodic discharge for 15 streams, miscellaneous discharge for 14 streams, continuous or daily stage for 45 streams, periodic stage for 27 streams, peak discharge for 26 streams, and peak stage for 27 streams; continuous or daily elevations for 39 lakes, periodic elevations for 53 lakes; continuous ground-water levels for 81 wells, periodic ground-water levels for 150 wells, and miscellaneous water-level measurements for 970 wells; quality-of-water data for 59 surface-water sites and 100 wells.</p><p>These data represent the National Water Data System records collected by the U.S. Geological Survey and cooperating local, state and federal agencies in Florida.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrFL881A","collaboration":"Prepared in cooperation with the State of Florida and other agencies.","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1989, Water Resources Data for Florida, Water Year 1988. Volume 1A. Northeast Florida - Surface Water: U.S. Geological Survey Water Data Report FL-88-1A, xiii, 440 p., https://doi.org/10.3133/wdrFL881A.","productDescription":"xiii, 440 p.","costCenters":[],"links":[{"id":181517,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1988/fl-88-1-a/report-thumb.jpg"},{"id":486596,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1988/fl-88-1-a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":29081,"text":"wri894045 - 1989 - Flow characteristics of the Clearwater River and tributaries from Clearbrook to Plummer, northwestern Minnesota","interactions":[],"lastModifiedDate":"2018-03-19T10:45:06","indexId":"wri894045","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-4045","title":"Flow characteristics of the Clearwater River and tributaries from Clearbrook to Plummer, northwestern Minnesota","docAbstract":"<p>During March through October 1986, 52,560 acre-feet of water passed the continuous-record stream gaging station on the Clearwater River near Clearbrook, Minnesota, 4.8 river miles upstream from the Red Lake Indian Reservation. Flow at the downstream boundary of the Reservation totaled 93,770 acre-feet. The increase in Clearwater River flow in the reach bordering the Reservation equaled 32,950 acre-feet; 60 percent of the increase occurred during March, April, and May. During those months, flow in the Clearwater River was augmented by flow from Kiwosay Reservoir and Butcher Knife Creek, which are located on the Reservation. Daily streamflow records showed that flow in the river increased in the Reservation reach throughout the study except for 13 days during October when losses occurred. At the downstream Reservation boundary, all daily mean flows exceeded the 36 cubic feet per second minimum flow required by the Minnesota Department of Natural Resources for the gaging station at Plummer, Minnesota located 29.9 miles downstream from the Reservation boundary. Monthly flows generally followed expected seasonal trends, with the highest monthly totals occurring in April and May and the lowest monthly totals occurring during August, September, and October. Seasonal trends were modified by reservoir releases, withdrawals for irrigation, and return flows that resulted from drainage of adjacent wild-rice fields. A series of flow measurements showed that localized withdrawals and return flows at times exceeded 20 percent of total streamflow. Discharge measurements made during low flow indicated higher rates of groundwater discharge in the vicinity of the Kiwosay Reservoir than in other parts of the study reach. Measurements made during August indicated that groundwater discharge in the reach of the river bordering the Reservation resulted in a flow gain of about 20 percent. Analysis of long-term streamflow records showed that near-average hydrologic conditions prevailed during the study period.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri894045","usgsCitation":"Payne, G.A., 1989, Flow characteristics of the Clearwater River and tributaries from Clearbrook to Plummer, northwestern Minnesota: U.S. Geological Survey Water-Resources Investigations Report 89-4045, iv, 25 p., https://doi.org/10.3133/wri894045.","productDescription":"iv, 25 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":118931,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4045/report-thumb.jpg"},{"id":57937,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4045/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.08,\n              48\n            ],\n            [\n              -95.125,\n              48\n            ],\n            [\n              -95.125,\n              47.5\n            ],\n            [\n              -95.33,\n              47.5\n            ],\n            [\n              -96.08,\n              47.875\n            ],\n            [\n              -96.08,\n              48\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aefaf","contributors":{"authors":[{"text":"Payne, G. A.","contributorId":62190,"corporation":false,"usgs":true,"family":"Payne","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200920,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21373,"text":"ofr87540 - 1989 - Ground-water use in the coastal plain of Maryland, 1900-1980","interactions":[],"lastModifiedDate":"2012-02-02T00:07:55","indexId":"ofr87540","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"87-540","title":"Ground-water use in the coastal plain of Maryland, 1900-1980","docAbstract":"This report presents groundwater withdrawal data from 1900 through 1980 for Maryland counties lying with the Coastal Plain physiographic province, as well as a summary section for the total Maryland Coastal Plain. The types of water use included are domestic, military, water supplier, industrial/commercial, and irrigation. The data were obtained from state and county reports, biannual pumpage reports submitted to the Maryland Water Resources Administration, communication with individual owners, and estimates based on existing published data. The amount of groundwater withdrawn from aquifers in the Maryland Coastal Plain in 1900 was approximately 26 million gallons per day (Mgal/d) compared to nearly 134 Mgal/d in 1980. Jurisdictions withdrawing more than 10 Mgal/d for most of the 80-year period were Anne Arundel and Baltimore Counties and Baltimore City. The greatest withdrawals for most of the early part of the period were for domestic and industrial/commercial uses; however, water-supplier use dominated after 1965. Groundwater use for irrigation became important in the Coastal Plain around 1960 and increased steadily from approximately 2 Mgal/d in 1960 to nearly 12 Mgal/d in 1980. (USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/ofr87540","usgsCitation":"Wheeler, J.C., and Wilde, F., 1989, Ground-water use in the coastal plain of Maryland, 1900-1980: U.S. Geological Survey Open-File Report 87-540, xii, 173 p. :ill. ;28 cm., https://doi.org/10.3133/ofr87540.","productDescription":"xii, 173 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":154358,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0540/report-thumb.jpg"},{"id":50932,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0540/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69675e","contributors":{"authors":[{"text":"Wheeler, J. C.","contributorId":66225,"corporation":false,"usgs":true,"family":"Wheeler","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":184311,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilde, F.D.","contributorId":50933,"corporation":false,"usgs":true,"family":"Wilde","given":"F.D.","email":"","affiliations":[],"preferred":false,"id":184310,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28800,"text":"wri894108 - 1989 - Geohydrology and ground-water quality at selected sites in Meade County, Kentucky, 1987-88","interactions":[],"lastModifiedDate":"2012-02-02T00:08:44","indexId":"wri894108","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-4108","title":"Geohydrology and ground-water quality at selected sites in Meade County, Kentucky, 1987-88","docAbstract":"Meade County in north-central Kentucky is about 305 sq mi in size, and is underlain by thick beds of limestone and dolomite which are the principal sources of drinking water for about 8 ,500 residents. About half the area contains mature, karst terrain with abundant sinkholes, springs, and caves. Because of this karst terrain, groundwater is susceptible to rapid changes in water quality and contamination from human sources. Thirty-seven wells and 12 springs were selected as sampling points to characterize groundwater quality in the area. Water was analyzed for major anions and cations, nitrates, trace elements, and organic compounds. Water from selected sites was also analyzed for fecal species of coliform streptococci bacteria and total coliform content. Except for fluoride and lead, the water quality was within the range expected for carbonate aquifers.The fluoride content was significantly higher in water from wells than in water from springs. Concentrations of detectable lead ranged from 10 to 50 micrograms/L and had a median value of 7.5 microg/L. Dissolved solids ranged from 100 to 2,200 mg/L and the median value was 512 mg/L. Hardness ranged from 20 to 1,100 mg/L and the median value was 290 mg/L. Organic compounds detected by the gas chromatographic/flame ionization detection scans, did not indicate evidence of concentrations in excess of the current Federal drinking water standards. Analysis for specific organic compounds indicated that the presence of these compounds was associated with agricultural chemicals, usually pesticides. Total coliform content exceeded drinking water standards in water from all 12 springs and in 18 wells. Statistical analysis of the groundwater quality data indicates that the variance of the concentrations of fluoride and chloride may be attributed to the site type. There was strong correlation between hardness and dissolved solids, hardness and sulfate, and sulfate and dissolved solids. No apparent relations were detected between water quality and the geographic location of sampling sites. However, seasonal variations were detected in the concentrations of dissolved solids, hardness, and iron. (Lantz-PTT)","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri894108","usgsCitation":"Mull, D.S., Alexander, A., and Schultz, P., 1989, Geohydrology and ground-water quality at selected sites in Meade County, Kentucky, 1987-88: U.S. Geological Survey Water-Resources Investigations Report 89-4108, vi, 67 p. :ill. ;28 cm., https://doi.org/10.3133/wri894108.","productDescription":"vi, 67 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":124216,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4108/report-thumb.jpg"},{"id":57668,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4108/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688591","contributors":{"authors":[{"text":"Mull, D. S.","contributorId":43331,"corporation":false,"usgs":true,"family":"Mull","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":200415,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alexander, A.G.","contributorId":93938,"corporation":false,"usgs":true,"family":"Alexander","given":"A.G.","email":"","affiliations":[],"preferred":false,"id":200416,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schultz, P.E.","contributorId":28634,"corporation":false,"usgs":true,"family":"Schultz","given":"P.E.","email":"","affiliations":[],"preferred":false,"id":200414,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":17863,"text":"ofr89592 - 1989 - Water-resources activities of the U.S. Geological Survey in Kansas; fiscal years 1987 and 1988","interactions":[],"lastModifiedDate":"2012-02-02T00:07:19","indexId":"ofr89592","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-592","title":"Water-resources activities of the U.S. Geological Survey in Kansas; fiscal years 1987 and 1988","docAbstract":"The principal mission of the U.S. Geological Survey, Water Resources Division, in Kansas is to investigate the occurrence, quantity, quality, distribution, and movement of surface and groundwater throughout the State. Primary activities include the systematic collection, analysis, and interpretation of hydrologic data, evaluation of water demands, and water resources research. Hydrologic investigations are conducted through four types of studies: (1) data collection programs; (2) statewide or regional investigations; (3) local or area investigations; and (4) research. These studies are funded through cooperative agreements with State and local agencies, transfer of funds from other agencies, and direct Federal funds. Thirty-six water related studies were ongoing during fiscal years 1987 and 1988 in Kansas. This report describes for each study the problem that initiated the study, the objectives of the study, the approach designed to achieve the objectives, and significant milestones and publications that resulted during fiscal years 1987 and 1988. Information on more than 2,100 data collection stations in Kansas is presented in maps and tables. A list of 46 reports and abstracts published or released by the U.S. Geological Survey, its cooperators, or technical and scientific organizations during 1987 and 1988 is provided. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr89592","usgsCitation":"Combs, L.J., 1989, Water-resources activities of the U.S. Geological Survey in Kansas; fiscal years 1987 and 1988: U.S. Geological Survey Open-File Report 89-592, iv, 97 p. :ill. ;28 cm., https://doi.org/10.3133/ofr89592.","productDescription":"iv, 97 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":150245,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0592/report-thumb.jpg"},{"id":47101,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0592/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4fb0","contributors":{"authors":[{"text":"Combs, L. J. (compiler)","contributorId":9271,"corporation":false,"usgs":true,"family":"Combs","given":"L.","suffix":"(compiler)","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":178087,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29419,"text":"wri854225C - 1989 - Floods of October 1983 in southeastern Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:08:57","indexId":"wri854225C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"85-4225","chapter":"C","title":"Floods of October 1983 in southeastern Arizona","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distibutor],","doi":"10.3133/wri854225C","usgsCitation":"Roeske, R., Garrett, J.M., and Eychaner, J.H., 1989, Floods of October 1983 in southeastern Arizona: U.S. Geological Survey Water-Resources Investigations Report 85-4225, v, 77 p. :chiefly ill. (some col.) ;22 x 29 cm., https://doi.org/10.3133/wri854225C.","productDescription":"v, 77 p. :chiefly ill. (some col.) ;22 x 29 cm.","costCenters":[],"links":[{"id":119414,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4225c/report-thumb.jpg"},{"id":58266,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4225c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df8c7","contributors":{"authors":[{"text":"Roeske, R.H.","contributorId":72366,"corporation":false,"usgs":true,"family":"Roeske","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":201499,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garrett, Joanne M.","contributorId":51796,"corporation":false,"usgs":true,"family":"Garrett","given":"Joanne","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":201498,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eychaner, James H.","contributorId":102050,"corporation":false,"usgs":true,"family":"Eychaner","given":"James","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":201500,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":21287,"text":"ofr89399 - 1989 - Ground-water, surface-water, and bottom-sediment contamination in the O-Field area, Aberdeen Proving Ground, Maryland, and the possible effects of selected remedial actions on ground water","interactions":[],"lastModifiedDate":"2012-02-02T00:07:59","indexId":"ofr89399","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-399","title":"Ground-water, surface-water, and bottom-sediment contamination in the O-Field area, Aberdeen Proving Ground, Maryland, and the possible effects of selected remedial actions on ground water","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr89399","usgsCitation":"Vroblesky, D.A., Lorah, M.M., and Oliveros, J.P., 1989, Ground-water, surface-water, and bottom-sediment contamination in the O-Field area, Aberdeen Proving Ground, Maryland, and the possible effects of selected remedial actions on ground water: U.S. Geological Survey Open-File Report 89-399, x, 162 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr89399.","productDescription":"x, 162 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":155288,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0399/report-thumb.jpg"},{"id":50839,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0399/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6965fe","contributors":{"authors":[{"text":"Vroblesky, Don A. vroblesk@usgs.gov","contributorId":413,"corporation":false,"usgs":true,"family":"Vroblesky","given":"Don","email":"vroblesk@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":184150,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lorah, Michelle M. 0000-0002-9236-587X mmlorah@usgs.gov","orcid":"https://orcid.org/0000-0002-9236-587X","contributorId":1437,"corporation":false,"usgs":true,"family":"Lorah","given":"Michelle","email":"mmlorah@usgs.gov","middleInitial":"M.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":184151,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Oliveros, James P.","contributorId":72367,"corporation":false,"usgs":true,"family":"Oliveros","given":"James","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":184152,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":13109,"text":"ofr8968 - 1989 - Ground-water level data for North Carolina, 1987","interactions":[],"lastModifiedDate":"2016-12-16T09:03:56","indexId":"ofr8968","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-68","title":"Ground-water level data for North Carolina, 1987","docAbstract":"Continuous and periodic measurements in 54 key wells and water-level measurements emplaced in Coastal Plain aquifers across North Carolina in 193 supplemental wells are presented in this report. Hydrographs of selected wells show changes in ground-water storage in the State. The water table in the shallow aquifers was higher throughout most of the State in 1987 than in 1986, indicating that rain had recharged these aquifers sufficiently to replenish the deficit in ground water storage that accumulated in the western and central parts of the State during 1986. Water levels in the heavily pumped Coastal Plain aquifers show a general downward trend for the year, indicating ground water is being withdrawn from aquifer storage. Record low water levels were measured in 4 of 13 wells in the Castle Hayne aquifer; the greatest decline measured during 1987 was 0.3 ft. Water levels in wells in the Peedee, Black Creek, upper Cape Fear, and lower Cape Fear aquifers generally show downward trends. Record low water levels were measured in 4 of 8 wells in the Peedee aquifer; the maximum decline measured during 1987 was 1.5 ft. All wells in the Black Creek, upper Cape Fear, and lower Cape Fear aquifers had record low water levels for 1987, with maximum measured declines in 1987 of 8.6, 3.1, and 3.1 ft., respectively. Record high water levels were measured in two wells, one each in the Castle Hayne and Peedee aquifers. Potentiometric surface maps show the effects of major centers of pumping for the Castle Hayne, Black Creek, and lower Cape Fear aquifers of the Coastal Plain.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8968","usgsCitation":"Coble, R.W., Strickland, A., and Bailey, M.C., 1989, Ground-water level data for North Carolina, 1987: U.S. Geological Survey Open-File Report 89-68, x, 152 p. :chiefly ill. ;28 cm., https://doi.org/10.3133/ofr8968.","productDescription":"x, 152 p. :chiefly ill. ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":41508,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0068/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144539,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0068/report-thumb.jpg"}],"country":"United States","state":"North 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Carolina\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dae9","contributors":{"authors":[{"text":"Coble, Ronald W.","contributorId":63813,"corporation":false,"usgs":true,"family":"Coble","given":"Ronald","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":167253,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Strickland, A.G.","contributorId":99959,"corporation":false,"usgs":true,"family":"Strickland","given":"A.G.","email":"","affiliations":[],"preferred":false,"id":167254,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bailey, M. Carl","contributorId":52584,"corporation":false,"usgs":true,"family":"Bailey","given":"M.","email":"","middleInitial":"Carl","affiliations":[],"preferred":false,"id":167252,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":49404,"text":"ofr89400D - 1989 - New information resources of the U.S. Geological Survey Library System, April 1989","interactions":[],"lastModifiedDate":"2012-02-02T00:10:05","indexId":"ofr89400D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-400","chapter":"D","title":"New information resources of the U.S. Geological Survey Library System, April 1989","language":"ENGLISH","doi":"10.3133/ofr89400D","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1989, New information resources of the U.S. Geological Survey Library System, April 1989: U.S. Geological Survey Open-File Report 89-400, 74 p. ; 28 cm., https://doi.org/10.3133/ofr89400D.","productDescription":"74 p. ; 28 cm.","costCenters":[],"links":[{"id":162483,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0400d/report-thumb.jpg"},{"id":86048,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0400d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69773d","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531924,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29012,"text":"wri884071 - 1989 - Simulation of streamflow in small drainage basins in the southern Yampa River basin, Colorado","interactions":[],"lastModifiedDate":"2022-09-16T21:38:16.366533","indexId":"wri884071","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4071","title":"Simulation of streamflow in small drainage basins in the southern Yampa River basin, Colorado","docAbstract":"Coal mining operations in northwestern Colorado commonly are located in areas that have minimal available water-resource information. Drainage-basin models can be a method for extending water-resource information to include periods for which there are no records or to transfer the information to areas that have no streamflow-gaging stations. To evaluate the magnitude and variability of the components of the water balance in the small drainage basins monitored, and to provide some method for transfer of hydrologic data, the U.S. Geological Survey 's Precipitation-Runoff Modeling System was used for small drainage basins in the southern Yampa River basin to simulate daily mean streamflow using daily precipitation and air-temperature data. The study area was divided into three hydrologic regions, and in each of these regions, three drainage basins were monitored. Two of the drainage basins in each region were used to calibrate the Precipitation-Runoff Modeling System. The model was not calibrated for the third drainage basin in each region; instead, parameter values were transferred from the model that was calibrated for the two drainage basins. For all of the drainage basins except one, period of record used for calibration and verification included water years 1976-81. Simulated annual volumes of streamflow for drainage basins used in calibration compared well with observed values; individual hydrographs indicated timing differences between the observed and simulated daily mean streamflow. Observed and simulated annual average streamflows compared well for the periods of record, but values of simulated high and low streamflows were different than observed values. Similar results were obtained when calibrated model parameter values were transferred to drainage basins that were uncalibrated. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884071","usgsCitation":"Parker, R.S., and Norris, J.M., 1989, Simulation of streamflow in small drainage basins in the southern Yampa River basin, Colorado: U.S. Geological Survey Water-Resources Investigations Report 88-4071, v, 47 p., https://doi.org/10.3133/wri884071.","productDescription":"v, 47 p.","costCenters":[],"links":[{"id":406892,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_46991.htm","linkFileType":{"id":5,"text":"html"}},{"id":57878,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4071/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159499,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4071/report-thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Yampa River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108,\n              40.1\n            ],\n            [\n              -106.8333,\n              40.1\n            ],\n            [\n              -106.8333,\n              40.5\n            ],\n            [\n              -108,\n              40.5\n            ],\n            [\n              -108,\n              40.1\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f78f2","contributors":{"authors":[{"text":"Parker, R. S.","contributorId":104510,"corporation":false,"usgs":true,"family":"Parker","given":"R.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":200786,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Norris, J. M.","contributorId":87953,"corporation":false,"usgs":true,"family":"Norris","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":200785,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38595,"text":"pp1200SD - 1989 - The National Gazetteer of the United States of America; South Dakota 1989","interactions":[],"lastModifiedDate":"2012-02-02T00:10:20","indexId":"pp1200SD","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1200","chapter":"SD","title":"The National Gazetteer of the United States of America; South Dakota 1989","language":"ENGLISH","doi":"10.3133/pp1200SD","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1989, The National Gazetteer of the United States of America; South Dakota 1989: U.S. Geological Survey Professional Paper 1200, 235 p., https://doi.org/10.3133/pp1200SD.","productDescription":"235 p.","costCenters":[],"links":[{"id":119149,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1200sd/report-thumb.jpg"},{"id":65407,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1200sd/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f100d","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529867,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13226,"text":"ofr89259 - 1989 - Natural ground-water quality in Michigan, 1974-87","interactions":[],"lastModifiedDate":"2016-09-16T11:43:33","indexId":"ofr89259","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-259","title":"Natural ground-water quality in Michigan, 1974-87","docAbstract":"<p>Wide variations occur in the chemical and physical characteristics of natural groundwaters in Michigan. Dissolved-solids concentrations range from 20 to 76,000 mg/L. Waters having low dissolved-solids concentrations are calcium bicarbonate-type waters. Sodium, sulfate, and chloride increase as mineralization increases. Iron, aluminum, and titanium concentrations are higher at some locations than is common in most natural waters. Lead concentrations exceed U.S. Environmental Protection Agency 's primary drinking-water regulations at some locations in the northern part of the lower Peninsula. Generalized areal patterns of water-quality variability indicate that geology is a primary cause of differences across the State. Examples of chemical associations in water indicate that chemical analyses may be valuable in tracing and identifying mineral deposits.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/ofr89259","collaboration":"Prepared in cooperation with the Michigan Department of Natural Resources","usgsCitation":"Cummings, T.R., 1989, Natural ground-water quality in Michigan, 1974-87: U.S. Geological Survey Open-File Report 89-259, vi, 50 p., https://doi.org/10.3133/ofr89259.","productDescription":"vi, 50 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":41609,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0259/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146141,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0259/report-thumb.jpg"}],"country":"United 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Ray","contributorId":20722,"corporation":false,"usgs":true,"family":"Cummings","given":"T.","email":"","middleInitial":"Ray","affiliations":[],"preferred":false,"id":167436,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":17796,"text":"ofr89409 - 1989 - U.S. Geological Survey second national symposium on Water quality; abstracts of the technical sessions, Orlando, Florida, November 12-17, 1989","interactions":[],"lastModifiedDate":"2018-08-19T21:59:48","indexId":"ofr89409","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-409","title":"U.S. Geological Survey second national symposium on Water quality; abstracts of the technical sessions, Orlando, Florida, November 12-17, 1989","docAbstract":"<p>The U.S Geological Survey (USGS) compiled and analyzed existing hydrologic and water-quality data from over 200 stream and estuary stations of the Abemarle-Pamlico estuarine system (A/P) to identify long-term temporal and spatial trends. The dataset included seven stations of the USGS National Stream Quality Accounting Network, two stations of the National Atmospheric Precipitation Deposition monitoring network, stations of the N.C. Department of Natural Resources and Community Development, and stations from 25 reports by individual investigators. Regression-residuals analysis, the seasonal Kendall's Tau test for trends, and graphical analysis using annual box plots were employed to determine trends. Profound change has occurred in the water quality of the A/P area over the last 30 years. Analysis of water-quality data upstream from the estuaries indicates increases of discharge-adjusted values of specific conductance, alkalinity, phosphorous, hardness, chloride, and dissolved solids. In the estuaries, pH is increasing except in the Pamlico River, where it is decreasing. There is a generalized decrease in suspended inorganic material in the system. Salinities are decreasing for sections of the Pamlico River, and increasing for parts of Albemarle Sound. Nitrogen concentrations are decreasing except in the Pamlico River, where they are increasing. Phosphorus concentrations are increasing in the Pamlico River and decreasing elsewhere. Annual average data show that nitrogen is the limiting nutrient in the Neuse and Pamlico Rivers. Phosphorus is limiting in the rest of the area. Chlorophyll-a levels are increasing in parts of the Neuse and Pamlico Rivers and decreasing in parts of the Chowan River. To evaluate the effect of basin characteristics on water quality, linear correlation was used. Agricultural crop variables produced the most correlations with water-quality data. Fertilizer usage had little detectable relation to water quality in the study area. In the section of the Pamlico River near Aurora, relations between employment, road mileages, and water quality indicated effects of development in the area.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr89409","usgsCitation":"1989, U.S. Geological Survey second national symposium on Water quality; abstracts of the technical sessions, Orlando, Florida, November 12-17, 1989: U.S. Geological Survey Open-File Report 89-409, 150 p., https://doi.org/10.3133/ofr89409.","productDescription":"150 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true},{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":47037,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0409/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149108,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0409/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db6998c5","contributors":{"compilers":[{"text":"Pederson, Gary L.","contributorId":81084,"corporation":false,"usgs":true,"family":"Pederson","given":"Gary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":743024,"contributorType":{"id":3,"text":"Compilers"},"rank":1},{"text":"Smith, Martha M.","contributorId":121281,"corporation":false,"usgs":true,"family":"Smith","given":"Martha","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":743025,"contributorType":{"id":3,"text":"Compilers"},"rank":2}]}}
,{"id":12361,"text":"ofr89270 - 1989 - Water resources activities in Michigan, 1989","interactions":[],"lastModifiedDate":"2012-02-02T00:06:32","indexId":"ofr89270","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-270","title":"Water resources activities in Michigan, 1989","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr89270","usgsCitation":"Spicer, T., 1989, Water resources activities in Michigan, 1989: U.S. Geological Survey Open-File Report 89-270, viii, 78 p. :ill. ;28 cm., https://doi.org/10.3133/ofr89270.","productDescription":"viii, 78 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":143750,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0270/report-thumb.jpg"},{"id":40597,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0270/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f96f9","contributors":{"authors":[{"text":"Spicer, T.J.","contributorId":34135,"corporation":false,"usgs":true,"family":"Spicer","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":166006,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":17869,"text":"ofr89621 - 1989 - Water-resources activities of the U.S. Geological Survey in Missouri, fiscal year 1989","interactions":[],"lastModifiedDate":"2012-02-02T00:07:20","indexId":"ofr89621","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-621","title":"Water-resources activities of the U.S. Geological Survey in Missouri, fiscal year 1989","docAbstract":"Water resources activities of the U.S. Geological Survey in Missouri consist of collecting hydrologic data and making interpretive studies. Hydrologic studies in Missouri are made through three basic types of projects: hydrologic data collection programs; local or areal hydrologic investigations; and statewide or regional studies. These projects are funded through cooperative joint-funding agreements with State and local agencies, transfer of funds from other Federal agencies, and direct Federal funds. The data and the results of the investigations are published or released by either the U.S. Geological Survey or by cooperating agencies. The report describes the hydrologic data collection programs and local or areal hydrologic investigations in Missouri for fiscal year 1989 and provides a list of selected water resources references for Missouri. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr89621","usgsCitation":"Jenkins, K.L., 1989, Water-resources activities of the U.S. Geological Survey in Missouri, fiscal year 1989: U.S. Geological Survey Open-File Report 89-621, x, 54 p. :ill. ;28 cm., https://doi.org/10.3133/ofr89621.","productDescription":"x, 54 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":150042,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0621/report-thumb.jpg"},{"id":47107,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0621/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9ea8","contributors":{"authors":[{"text":"Jenkins, K. L. (compiler)","contributorId":61053,"corporation":false,"usgs":true,"family":"Jenkins","given":"K.","suffix":"(compiler)","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":178095,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29205,"text":"wri894010 - 1989 - Hydrologic evaluation and water-supply considerations for five Paiute Indian land parcels, Millard, Sevier, and Iron counties, southwestern Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:08:48","indexId":"wri894010","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-4010","title":"Hydrologic evaluation and water-supply considerations for five Paiute Indian land parcels, Millard, Sevier, and Iron counties, southwestern Utah","docAbstract":"The hydrologic resources in and adjacent to five parcels of land held in trust for the Paiute Indian Tribe of Utah were evaluated. The land, located in southwestern Utah, is generally arid and has had only limited use for grazing. The parcels are located near the towns of Cove Fort, Joseph, Koosharem, and Kanarraville. On the basis of available geohydrologic and hydrologic data, water of suitable quality is locally available in the areas of all parcels for domestic, stock, recreation, and limited irrigation use. Developing this water for use on the parcels would potentially involve obtaining water rights, drilling wells, and constructing diversion structures. Surface water apparently is the most favorable source of supply available for the Joseph parcel, and groundwater apparently is the most favorable source of supply available for the other parcels. (USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nU.S. Geological Survey, Books and Open-File Reports [distributor],","doi":"10.3133/wri894010","usgsCitation":"Price, D., Stephens, D.W., and Conroy, L., 1989, Hydrologic evaluation and water-supply considerations for five Paiute Indian land parcels, Millard, Sevier, and Iron counties, southwestern Utah: U.S. Geological Survey Water-Resources Investigations Report 89-4010, v, 39 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri894010.","productDescription":"v, 39 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119787,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4010/report-thumb.jpg"},{"id":58064,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4010/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db606f88","contributors":{"authors":[{"text":"Price, Don","contributorId":30608,"corporation":false,"usgs":true,"family":"Price","given":"Don","email":"","affiliations":[],"preferred":false,"id":201143,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stephens, D. W.","contributorId":68335,"corporation":false,"usgs":true,"family":"Stephens","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":201144,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Conroy, L.S.","contributorId":6051,"corporation":false,"usgs":true,"family":"Conroy","given":"L.S.","email":"","affiliations":[],"preferred":false,"id":201142,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26668,"text":"wri874130 - 1989 - Hydrogeology of the Cocheco River basin, southeastern New Hampshire","interactions":[],"lastModifiedDate":"2012-02-02T00:08:30","indexId":"wri874130","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"87-4130","title":"Hydrogeology of the Cocheco River basin, southeastern New Hampshire","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri874130","usgsCitation":"Cotton, J.E., 1989, Hydrogeology of the Cocheco River basin, southeastern New Hampshire: U.S. Geological Survey Water-Resources Investigations Report 87-4130, v, 47 p. :ill., map ;28 cm., https://doi.org/10.3133/wri874130.","productDescription":"v, 47 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":119082,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4130/report-thumb.jpg"},{"id":55535,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4130/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55536,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4130/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ee4b07f02db6151c4","contributors":{"authors":[{"text":"Cotton, J. E.","contributorId":52976,"corporation":false,"usgs":true,"family":"Cotton","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":196799,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26898,"text":"wri894100 - 1989 - Geohydrology, simulation of ground-water flow, and ground-water quality at two landfills, Marion County, Indiana","interactions":[],"lastModifiedDate":"2016-05-16T08:14:13","indexId":"wri894100","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-4100","title":"Geohydrology, simulation of ground-water flow, and ground-water quality at two landfills, Marion County, Indiana","docAbstract":"<p>Geologic, hydrologic, and water-quality data were collected at the Julietta and Tibbs-Banta landfills in Marion County. Both landfills were closed in the mid-1970's, and sewage sludge mixed with dirt was spread on the landfills in the mid-1980's as part of a revegetation project.</p>\n<p>The landfills were constructed in unconsolidated glacial sediments that consist of sand, gravel, silt, and clay. The maximum thickness of the sediments is 180 feet at Julietta and 100 feet at Tibbs-Banta. Both landfills are underlain by sand and gravel aquifers and are adjacent to gaining streams. Ground water flows toward and into the streams at each study area. Two sand and gravel aquifers were mapped at Julietta and four were mapped at TibbsBanta. The aquifers are separated in places by discontinuous clay layers.</p>\n<p>Ground-water-flow models, calibrated to simulate steady-state low-flow conditions, indicate that about 19,000 gallons of water per day move through the refuse at Julietta and 42,000 gallons per day move through the refuse at Tibbs-Banta. The Julietta model also indicates that recharge through the surface of the landfill is less than in the surrounding natural areas, probably because of the addition and compaction of the sludge/soil mixture.</p>\n<p>Concentrations of dissolved inorganic substances in ground-water samples indicate that leachate from both landfills is reaching the shallow aquifers. The effect on deeper aquifers is small because of the predominance of horizontal ground-water flow and discharge to the streams. Increases in almost all dissolved constituents were observed in shallow wells that are screened beneath and downgradient from the landfills. Several analyses, especially those for bromide, dissolved solids, and ammonia, were useful in delineating the plume of leachate at both landfills.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/wri894100","collaboration":"City of Indianapolis, Department of Public Works","usgsCitation":"Duwelius, R., and Greeman, T., 1989, Geohydrology, simulation of ground-water flow, and ground-water quality at two landfills, Marion County, Indiana: U.S. Geological Survey Water-Resources Investigations Report 89-4100, viii, 135 p. :ill. ;28 cm., https://doi.org/10.3133/wri894100.","productDescription":"viii, 135 p. :ill. ;28 cm.","startPage":"1","endPage":"135","numberOfPages":"143","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":121864,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4100/report-thumb.jpg"},{"id":55779,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4100/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Indiana","county":"Marion","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-85.9369,39.9272],[-85.9379,39.87],[-85.9541,39.8696],[-85.9518,39.6969],[-85.9523,39.638],[-86.248,39.6335],[-86.3268,39.6318],[-86.3281,39.8526],[-86.328,39.8662],[-86.325,39.8662],[-86.3267,39.9238],[-86.2967,39.9246],[-86.2757,39.925],[-86.2385,39.9259],[-85.9801,39.9269],[-85.9411,39.9272],[-85.9369,39.9272]]]},\"properties\":{\"name\":\"Marion\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8763","contributors":{"authors":[{"text":"Duwelius, R.F.","contributorId":28250,"corporation":false,"usgs":true,"family":"Duwelius","given":"R.F.","affiliations":[],"preferred":false,"id":197210,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Greeman, T. K.","contributorId":58275,"corporation":false,"usgs":true,"family":"Greeman","given":"T. K.","affiliations":[],"preferred":false,"id":197211,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44833,"text":"wri884202 - 1989 - Hydrogeology of the western part of the Salt River Valley area, Maricopa County, Arizona","interactions":[],"lastModifiedDate":"2013-12-13T14:03:39","indexId":"wri884202","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4202","title":"Hydrogeology of the western part of the Salt River Valley area, Maricopa County, Arizona","docAbstract":"The Salt River Valley is a major population and agricultural center of more than 3,000 mi<sup>2</sup> in central Arizona (fig. 1). The western part of the Salt River Valley area (area of this report) covers about 1,500 mi<sup>2</sup>. The Phoenix metropolitan area with a population of more than 1.6 million in 1985 (Valley National Bank, 1987) is located within the valley. The watersheds of the Salt, Verde, and Agua Fria Rivers provide the valley with a reliable but limited surface-water supply that must be augmented with ground water even in years of plentiful rainfall. Large-scale ground-water withdrawals began in the Salt River Valley in the early part of the 20th century; between 1915 and 1983, the total estimated ground-water pumpage was 81 million acre-ft (U.S. Geological Survey, 1984). Because of the low average annual rainfall and high potential evapotranspiration, the principal sources of ground-water recharge are urban runoff, excess irrigation, canal seepage and surface-water flows during years of higher-than-normal rainfall. Withdrawals greatly exceed recharge and, in some area, ground-water levels have declines as much as 350 ft (Laney and other, 1978; Ross, 1978). In the study area, ground-water declines of more than 300 ft have occurred in Deer Valley and from Luke Air Force Base north to Beardsley. As a result, a large depression of the water table has developed west of Luke Air Force Base (fig. 2). Ground-water use has decreased in recent years because precipitation and surface-water supplies have been greater than normal. Increased precipitation also caused large quantities of runoff to be released into the normally dry Salt and Gila River channels. From February 1978 to June 1980, streamflow losses of at least 90,000 acre-ft occurred between Jointhead Dam near the east boundary of the study area and  Gillespie Dam several miles southwest of the west edge of the study area (Mann and Rhone, 1983). Consequently, ground-water declines in a large part of the basin have slowed, and ground-water levels in some sarea have risen significantly. In many areas along the Salt River and northeast of the confluence of the Salt and Agua Fria River, ground-water levels rose more than 25 ft between 1978 and 1984 (Reeter and Remick, 1986).","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884202","collaboration":"Prepared in cooperation with the Arizona Department of Water Resources, Salt River Project, and Arizona Municipal Water Users' Association","usgsCitation":"Brown, J.G., and Pool, D.R., 1989, Hydrogeology of the western part of the Salt River Valley area, Maricopa County, Arizona: U.S. Geological Survey Water-Resources Investigations Report 88-4202, 4 Plates: 45.81 x 39.54 inches and smaller, https://doi.org/10.3133/wri884202.","productDescription":"4 Plates: 45.81 x 39.54 inches and smaller","costCenters":[],"links":[{"id":171262,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri884202.PNG"},{"id":279489,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4202/plate-3.pdf"},{"id":279490,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4202/plate-4.pdf"},{"id":279487,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4202/plate-1.pdf"},{"id":279488,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4202/plate-2.pdf"}],"country":"United States","state":"Arizona","county":"Maricopa County","otherGeospatial":"Salt River Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.0,33.25 ], [ -113.0,34.0 ], [ -112.0,34.0 ], [ -112.0,33.25 ], [ -113.0,33.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db614b2d","contributors":{"authors":[{"text":"Brown, James G.","contributorId":81094,"corporation":false,"usgs":true,"family":"Brown","given":"James","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":230517,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pool, D. R.","contributorId":75581,"corporation":false,"usgs":true,"family":"Pool","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":230516,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29649,"text":"wri884138 - 1989 - Ground-water levels, water quality, and potential effects of toxic-substance spills or cessation of quarry dewatering near a municipal ground-water supply, southern Franklin County, Ohio","interactions":[],"lastModifiedDate":"2022-01-06T21:47:52.976112","indexId":"wri884138","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4138","title":"Ground-water levels, water quality, and potential effects of toxic-substance spills or cessation of quarry dewatering near a municipal ground-water supply, southern Franklin County, Ohio","docAbstract":"A newly completed municipal ground-water supply that produces from a sand and gravel aquifer in southern Franklin County, Ohio, may be susceptible to potential sources of pollution. Among these are spills of toxic substances that could enter recharge areas of the aquifer or be carried by surface drainage and subsequently enter the aquifer by induced infiltration. Ground water of degraded quality also is present in the vicinity of several landfills located upstream from the municipal supply.\r\n\r\nLocal dewatering by quarrying operations has created a ground-water divide which, at present, prevents direct movement of the degraded ground water to the municipal supply. In addition, the dewatering has held water levels at the largest landfills below the base of the landfill. Should the dewatering cease, concern would be raised regarding the rise of water levels at this landfills and transport of contaminants through the aquifer to the Scioto River and subsequently by the river to the well field.\r\n\r\nFrom June 1984 through July 1986, the U.S. Geological Survey, in cooperation with the City of Columbus, Ohio, investigated the relations among the ground-water supply and potential sources of contamination by means of an observation-well network and a program of measuring water levels and sampling for water quality. Sample collections included those made to determine the baseline levels of organic chemicals and metals, as well as periodic sampling and analysis for common constituents to evaluate any changes taking place in the system. Finally, a steady-state, three-dimensional numerical model was used to determine ground-water flow directions and average ground-water velocities to asses potential effects of toxic-substance spills. The model also was used to simulate changes in the ground-water flow system that could result if part or all of the quarry dewatering ceased.\r\n\r\nFew of the organic-chemical and metal constituents analyzed for were present at detectable levels. With respect to chemical analysis of water and soil materials reported in earlier studies, no new problem areas were discovered as a result of either the baseline or periodic samplings. Model simulations suggest that, under March 1986 conditions, a toxic-substance spill along the major highways in the northern two-thirds of the study area eventually could discharge into one of the two quarries being dewatered or into the Scioto River.\r\n\r\nA toxic-substance spill in the southern one-third of the study area ultimately may discharge into the Scioto River, Big Walnut Creek, or possibly into the municipal ground-water supply. Model simulations also indicate that concentrated landfill leachate probably would not reach the municipal ground-water supply under current or well-field pumping conditions if dewatering ceased at either or both of the quarries.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884138","usgsCitation":"Sedam, A., Eberts, S.M., and Bair, E., 1989, Ground-water levels, water quality, and potential effects of toxic-substance spills or cessation of quarry dewatering near a municipal ground-water supply, southern Franklin County, Ohio: U.S. Geological Survey Water-Resources Investigations Report 88-4138, vii, 111 p., https://doi.org/10.3133/wri884138.","productDescription":"vii, 111 p.","costCenters":[],"links":[{"id":58467,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4138/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124542,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4138/report-thumb.jpg"},{"id":393989,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47047.htm"}],"country":"United States","state":"Ohio","county":"Franklin County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.05,\n              39.8333\n            ],\n            [\n              -82.9583,\n              39.8333\n            ],\n            [\n              -82.9583,\n              39.925\n            ],\n            [\n              -83.05,\n              39.925\n            ],\n            [\n              -83.05,\n              39.8333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db66747d","contributors":{"authors":[{"text":"Sedam, A. C.","contributorId":32530,"corporation":false,"usgs":true,"family":"Sedam","given":"A. C.","affiliations":[],"preferred":false,"id":201886,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eberts, S. M.","contributorId":28276,"corporation":false,"usgs":true,"family":"Eberts","given":"S.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":201885,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bair, E. Scott","contributorId":73231,"corporation":false,"usgs":true,"family":"Bair","given":"E. Scott","affiliations":[],"preferred":false,"id":201887,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":27241,"text":"wri874269 - 1989 - Ground-water quality in Douglas County, western Nevada","interactions":[],"lastModifiedDate":"2019-08-20T10:36:46","indexId":"wri874269","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"87-4269","title":"Ground-water quality in Douglas County, western Nevada","docAbstract":"A 182% increase in population within the last 10 years in Douglas County, Nevada, has raised concerns by county officials as to the possible effects land development may have on groundwater quality. Most groundwater in Douglas County meets the State of Nevada drinking water standards. Of the 333 water samples used in this analysis, 6 equaled or were greater than the drinking water standards for sulfates, 44 for fluoride, 4 for dissolved solids, 5 for nitrate as nitrate, 12 for arsenic, 33 for iron, and 18 for manganese. Groundwater in the west-central, northern, and northeastern part of Carson Valley is influenced by geothermal water. Some areas in the county may have septic-tank effluent contaminating the groundwater. Temporal changes in most municipal wells showed no overall trend for dissolved-solids and nitrate concentrations spanning the years 1969-83. However, a municipal well in the Topaz Lake area has shown a general increases in the nitrate concentration from 1961 to 1984, but the concentration does not exceed the drinking-water standard. A future groundwater quality monitoring program in Douglas County would include periodic sampling of primary or heavily pumped wells, long-term trend wells, and supplemental wells. (Thacker-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri874269","usgsCitation":"Garcia, K.T., 1989, Ground-water quality in Douglas County, western Nevada: U.S. Geological Survey Water-Resources Investigations Report 87-4269, vii, 107 p. , https://doi.org/10.3133/wri874269.","productDescription":"vii, 107 p. ","costCenters":[],"links":[{"id":366713,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4269/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158743,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4269/report-thumb.jpg"}],"country":"United States","state":"Nevada","county":"Douglas County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-119.5461,39.0859],[-119.5272,39.0858],[-119.316,39.0841],[-119.3155,38.9902],[-119.3356,38.9895],[-119.3366,38.9818],[-119.349,38.9816],[-119.4023,38.9826],[-119.4022,38.9558],[-119.4176,38.9547],[-119.4182,38.9098],[-119.4192,38.8817],[-119.4381,38.8823],[-119.4374,38.8533],[-119.419,38.8531],[-119.4192,38.835],[-119.4193,38.8164],[-119.4122,38.8165],[-119.4126,38.8093],[-119.4019,38.8099],[-119.4013,38.7863],[-119.4026,38.7654],[-119.4085,38.7658],[-119.4077,38.7354],[-119.4075,38.73],[-119.3887,38.7303],[-119.3888,38.7348],[-119.3788,38.735],[-119.3611,38.7352],[-119.3505,38.7354],[-119.3502,38.7263],[-119.349,38.6788],[-119.349,38.6769],[-119.3488,38.6466],[-119.3299,38.6469],[-119.3306,38.5364],[-119.4492,38.6196],[-119.4543,38.6231],[-119.5498,38.6895],[-119.5523,38.6912],[-119.5771,38.7084],[-119.5977,38.7226],[-119.6088,38.7303],[-119.6166,38.7357],[-119.678,38.7781],[-119.7033,38.7953],[-119.7285,38.8132],[-119.743,38.8235],[-119.752,38.8297],[-119.7873,38.8541],[-119.7899,38.8554],[-119.8223,38.8775],[-119.8261,38.8802],[-119.8471,38.8948],[-119.9025,38.9332],[-119.9151,38.942],[-119.9194,38.945],[-119.9508,38.9664],[-120.0009,39.0005],[-120.0023,39.0677],[-120.0031,39.1116],[-119.949,39.1122],[-119.9419,39.1123],[-119.8974,39.1123],[-119.8631,39.1129],[-119.8358,39.113],[-119.7611,39.1144],[-119.7612,39.099],[-119.7517,39.0987],[-119.7525,39.0851],[-119.6232,39.086],[-119.6042,39.0859],[-119.5657,39.0861],[-119.5461,39.0859]]]},\"properties\":{\"name\":\"Douglas\",\"state\":\"NV\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db66723c","contributors":{"authors":[{"text":"Garcia, K. T.","contributorId":52613,"corporation":false,"usgs":true,"family":"Garcia","given":"K.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":197782,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25960,"text":"wri884222 - 1989 - Evaluation of a watershed model to simulate sediment transport in a small agricultural watershed in Indiana","interactions":[],"lastModifiedDate":"2016-05-09T10:36:58","indexId":"wri884222","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4222","title":"Evaluation of a watershed model to simulate sediment transport in a small agricultural watershed in Indiana","docAbstract":"<p>The streamflow and sediment components of the watershed model, ' Hydrologic Simulation Program-Fortran ', were evaluated using 2 years and 9 months of data from a 2.7-sq mi agricultural watershed in Indiana. Hydrographs of simulated sediment concentration generally have smaller peaks and longer recessions than do hydrographs of measured data. The attenuation of simulated peaks was partly caused by difficulties in designing a representative channel system. Simulated surface runoff during low-intensity rainfall was greater than measured surface runoff; this caused an overestimation of sediment concentration and discharge. Rainfalls of low intensity were mostly absorbed by the soil, but the model predicted that the amount of surface runoff from such storms would be large. The overly large volume of simulated surface runoff transported more sediment than actually occurred. The mean absolute error of mean sediment concentrations during storms is 45% of the measured average concentration. The error resulted from a combination of error in recording streamflow and rainfall, in simulating streamflows, and in simulating sedimentation processes. The largest percent errors are associated with simulated maximum streamflows and average sediment discharges. The root-mean-square errors are 93 and 102% of the measured maximum streamflow and average sediment discharges. 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,{"id":17633,"text":"ofr88318 - 1989 - Results of hydrologic research at a low-level radioactive-waste disposal site near Sheffield, Illinois","interactions":[{"subject":{"id":17633,"text":"ofr88318 - 1989 - Results of hydrologic research at a low-level radioactive-waste disposal site near Sheffield, Illinois","indexId":"ofr88318","publicationYear":"1989","noYear":false,"title":"Results of hydrologic research at a low-level radioactive-waste disposal site near Sheffield, Illinois"},"predicate":"SUPERSEDED_BY","object":{"id":2635,"text":"wsp2367 - 1991 - Results of hydrologic research at a low-level radioactive-waste disposal site near Sheffield, Illinois","indexId":"wsp2367","publicationYear":"1991","noYear":false,"title":"Results of hydrologic research at a low-level radioactive-waste disposal site near Sheffield, Illinois"},"id":1}],"supersededBy":{"id":2635,"text":"wsp2367 - 1991 - Results of hydrologic research at a low-level radioactive-waste disposal site near Sheffield, Illinois","indexId":"wsp2367","publicationYear":"1991","noYear":false,"title":"Results of hydrologic research at a low-level radioactive-waste disposal site near Sheffield, Illinois"},"lastModifiedDate":"2021-03-05T19:30:36.120435","indexId":"ofr88318","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-318","title":"Results of hydrologic research at a low-level radioactive-waste disposal site near Sheffield, Illinois","docAbstract":"<p>Ten years of hydrologic research have been conducted by the U.S. Geological Survey at a commercial low-level radioactive-waste disposal site near Sheffield, Illinois. Research included studies of microclimate, evapotranspiration, and tritium release by plants; runoff and land modification; water movement through a trench cover; water and tritium movement in the unsaturated zone; gases in the unsaturated zone; water and tritium movement in the saturated zone; and water chemistry. Implications specific to each research topic and those based on overlapping research topics are summarized as to their potential effect on the selection, characterization, design, operation, and decommissioning processes of future low-level radioactive-waste disposal sites. </p><p>Unconsolidated deposits at the site are diverse in lithologic character and are spatially and stratigraphically complex. Thickness of these Quaternary deposits ranges from 3 to 27 meters and averages 17 meters. The unconsolidated deposits overlay 140 meters of Pennsylvanian shale, mudstone, siltstone, and coal. </p><p>Approximately 90,500 cubic meters of waste were buried from August 1967 through August 1978, in 21 trenches that were constructed in glacial materials by using a cut-and-fill process. Trenches generally were constructed below grade and ranged from 11 to 180 meters long, 2.4 to 21 meters wide, and 2.4 to about 7.9 meters deep. </p><p>Research on microclimate and evapotranspiration at the site was conducted from July 1982 through June 1984. Continuous measurements were made of precipitation, incoming and reflected solar (shortwave) radiation, incoming and emitted terrestrial (longwave) radiation, horizontal windspeed and direction, wet- and dry-bulb air temperature, barometric pressure, soil-heat fluxes, and soil temperature. Soil-moisture content, for this research phase, was measured approximately biweekly. Evapotranspiration rates were estimated by using three techniques--energy budget, aerodynamic profile, and water budget. Although monthly totals for each method differed, estimated annual evapotranspiration averages ranged from 630 to 693 millimeters or about 70 percent of precipitation. </p><p>Tritium concentrations in leaf water from on-site plants were determined for 125 vegetation samples collected during the summers of 1982 through 1986. Concentrations varied significantly among some locations and plant types. Tritium concentrations ranged from the detection limit of 0 .2 to 1,330 nanocuries per liter, with alfalfa (Medicago sativa) having the highest concentrations, followed by brome grass (Bromus inermis), and then red clover (Trifoleum pratense); these variations in concentration are most likely a result of root depth. </p><p>Runoff and sediment transport were measured from July 1982 through December 1985 in four basins--three comprising almost two-thirds of the 8.1-hectare site and one comprising a 1.4-hectare undisturbed area. Volumes and equivalent weights of collapses were estimated from records of site surficial conditions from October 1978 through December 1985. Runoff showed a direct relation to degree of land modification; lowest mean yields were measured at the undisturbed area, and highest mean yields were measured from the basin composed wholly of trench and intertrench areas. Sediment yield measured onsite averaged 3.4 megagrams per hectare. A total of 315 collapse cavities, corresponding to a cumulative volume of about 500 cubic meters, were documented. Most collapses were recorded after periods of rainfall or snowmelt when soil moisture was near maximum. Almost two-thirds of the collapses, corresponding to 63 percent of the cumulative cavity volume, occurred during February through April. </p><p>Data for the study of water movement through a trench cover were collected from July 1982 through June 1934. Pressure-head data were collected at four different clusters at depths ranging from 50 to 1,850 millimeters within a selected trench cover. Soil-moisture content for this research phase was measured weekly with a gamma-attenuation moisture probe. The amount of water stored within the trench cover fluctuated in an annual cycle. Moisture contents were greatest in late March or early April, decreased steadily from late spring through the summer, reached a minimum in late August or early September, and then increased gradually from midfall through the winter. Depths of wetting-front movements were a function of initial soil-moisture content and total storm precipitation. Seepage to the trench was estimated by use of four different methods: the Darcy method, the zero-flux phase method, the surface-based water-budget method, and the ground-water based water-budget method. Estimates by the different methods differed considerably. </p><p>Investigation of the unsaturated zone at the site began in 1981 and is ongoing (1987). Water movement was measured along a generalized vertical section through four trenches. A 120-meter-long, 2-meter-diameter horizontal tunnel provided access below the trenches. The timing of water movement varied temporally and spatially. Vertical flow was inhibited at interfaces between lithologic units of contrasting hydraulic conductivities. Data also indicate that water movement through the sand of the Toulon Member of the Glasford Formation occurs along localized partially saturated to saturated flow paths. Average velocities of water movement through the extent of the unsaturated zone, as estimated by a saturation-tracking method, ranged from 0.04 to 0.34 meter per day. </p><p>Tritium concentrations in the unsaturated zone varied spatially reflecting the heterogeneity of wastes in the overlying trenches and local hydrogeologic conditions. Tritium concentrations at all lysimeter locations increased with time; however, the increases usually were of small magnitude. Tritium concentrations increased abruptly, from five to nine times previous concentrations, at only 3 of 14 locations. </p><p>Gas samples were collected from a network of soil-gas piezometers located in the undisturbed unsaturated zone near a waste trench at approximately 70-day intervals during 1984-86. Relative proportions of nitrogen, oxygen plus argon, carbon dioxide, methane, ethane, propane, butane, tritiated water vapor, carbon dioxide, and 222radon were converted to partial pressures, based on a mean atmospheric pressure of 98.6 kilopascals. Methane and 14 carbon dioxide were identified as originating in the waste and having mean partial pressures that generally decreased with horizontal distance from the trench and with vertical distance to the land surface. Partial-pressure gradients for other radioactive gases were not detected in the gas sampling network; definable gradients may occur much nearer to the waste source. </p><p>Ground-water flow has been studied at the site since 1976. The spatial, stratigraphic, and lithologic complexity of the unconsolidated deposits that compose the shallow aquifer result in the free water surface intersecting nine different lithologic units at the site. Saturated hydraulic conductivities of these units range from about 4x10-12 to 8x10-6 centimeters per second. Three ground-water basins were defined within the shallow aquifer, with flow generally from west to east. Ground-water velocities are highly variable. A tracer test conducted in a pebbly-sand unit resulted in velocities in the range of 640 to 770 meters per year. Estimated velocities for the other units ranged from 2 to 490 meters per year. </p><p>Tritium was detected in observation wells on-site in 1976 and off-site in 1982. Concentrations ranged from the analytical detection limit of 0.2 to over 300 nanocuries per liter. Seasonal variations in tritium concentrations were observed in most wells, and dilution caused by infiltrating rainfall was observed. </p><p>Water-chemistry research included the collection and analysis of precipitation, geologic materials, and unsaturated- and saturated-zone water, both on-site and off-site, and in all geologic units, during 1978 to 1984. Precipitation was a calcium-zinc-sulfate type water. Calcium and bicarbonate were the most abundant cation and anion, respectively, in the geologic materials. Mean dissolved organic carbon and tritium concentrations (45 milligrams per liter and 290 nanocuries per liter, respectively) were greater in samples from six lysimeters located directly below waste trenches and one located within a trench, than in samples from all other lysimeters (8.4 milligrams per liter and 17 nanocuries per liter, respectively). Water in the saturated zone was generally a magnesium-bicarbonate type. Tritium was the only radionuclide detected in the saturated zone.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr88318","usgsCitation":"1989, Results of hydrologic research at a low-level radioactive-waste disposal site near Sheffield, Illinois: U.S. Geological Survey Open-File Report 88-318, x, 114 p., https://doi.org/10.3133/ofr88318.","productDescription":"x, 114 p.","costCenters":[],"links":[{"id":149804,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0318/report-thumb.jpg"},{"id":384153,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0318/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Illinois","city":"Sheffield","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.76242065429688,\n              41.33660710626423\n            ],\n            [\n              -89.67727661132811,\n              41.33660710626423\n            ],\n            [\n              -89.67727661132811,\n              41.3675335097313\n            ],\n            [\n              -89.76242065429688,\n              41.3675335097313\n            ],\n            [\n              -89.76242065429688,\n              41.33660710626423\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db673fe8","contributors":{"editors":[{"text":"Ryan, Barbara J.","contributorId":53397,"corporation":false,"usgs":true,"family":"Ryan","given":"Barbara J.","affiliations":[],"preferred":false,"id":749494,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":14028,"text":"ofr8933 - 1989 - Bibliography of Oklahoma hydrology; reports prepared by the U.S. Geological Survey and principal cooperating agencies, 1901-88","interactions":[],"lastModifiedDate":"2012-02-02T00:06:53","indexId":"ofr8933","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-33","title":"Bibliography of Oklahoma hydrology; reports prepared by the U.S. Geological Survey and principal cooperating agencies, 1901-88","docAbstract":"Reports on the hydrology of Oklahoma have been issued by the U.S. Geological Survey since 1901. This bibliography lists reports on hydrology in Oklahoma prepared by the U.S. Geological Survey and the principal State cooperating agencies, the Oklahoma Geological Survey and the Oklahoma Water Resources Board. Of the nearly 350 reports issued from 1901 through 1988, about 200 have been concerned primarily with groundwater; the remainder have dealt with some aspect of surface water, water quality, or geology. The reports are listed by agency and report type, and are indexed both by author and subject. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8933","usgsCitation":"Havens, J.S., 1989, Bibliography of Oklahoma hydrology; reports prepared by the U.S. Geological Survey and principal cooperating agencies, 1901-88: U.S. Geological Survey Open-File Report 89-33, iv, 59 p. ;28 cm., https://doi.org/10.3133/ofr8933.","productDescription":"iv, 59 p. ;28 cm.","costCenters":[],"links":[{"id":147232,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0033/report-thumb.jpg"},{"id":42682,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0033/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62988d","contributors":{"authors":[{"text":"Havens, John S. (compiler)","contributorId":99996,"corporation":false,"usgs":true,"family":"Havens","given":"John","suffix":"(compiler)","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":168817,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57630,"text":"wdrFL882A - 1989 - Water resources data, Florida; Water year 1988; Volume 2A. South Florida surface water","interactions":[],"lastModifiedDate":"2025-06-10T13:23:54.555431","indexId":"wdrFL882A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"FL-88-2A","title":"Water resources data, Florida; Water year 1988; Volume 2A. South Florida surface water","docAbstract":"<p>Water resources data for the 1988 water year in Florida consists of continuous or daily discharge for 338 streams, periodic discharge for 34 streams, miscellaneous discharge for 28 streams, continuous or daily stage for 152 streams, periodic stage for 29 streams, peak discharge for 71 streams, continuous daily tide stage for 8 streams, and peak stage for 84 streams; continuous or daily elevations for 73 lakes, periodic elevations for 72 lakes; continuous ground-water levels for 490 wells, periodic ground-water levels for 1,620 wells, and miscellaneous water level measurements for 2,678 wells; quality of water data for 158 surface-water sites and 884 wells.</p><p>The data for South Florida include continuous or daily discharge for 65 streams, periodic discharge for 2 streams, peak discharge for 4 streams, continuous or daily stage for 82 streams, periodic stage for 16 streams, peak discharge for 2 streams, and peak stage for 12 streams; continuous elevations for 1 lake and periodic elevations for 5 lakes; continuous ground-water levels for 179 wells, periodic ground-water levels for 298 wells, and miscellaneous water-level measurements for 250 wells; quality-of-water for 6 surface-water sites and 558 wells.</p><p>This data represent the National Water Data System records collected by the U.S. Geological Survey and cooperation local, state and federal agencies in Florida.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrFL882A","collaboration":"Prepared in cooperation with the State of Florida and with other agencies","usgsCitation":"Haire, W., Price, E., Lietz, A., and Workman, E., 1989, Water resources data, Florida; Water year 1988; Volume 2A. 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