{"pageNumber":"518","pageRowStart":"12925","pageSize":"25","recordCount":16449,"records":[{"id":29863,"text":"wri854244 - 1985 - Estimation of evaporation from Ned Wilson Lake, Flat Tops Wilderness Area, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:59","indexId":"wri854244","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4244","title":"Estimation of evaporation from Ned Wilson Lake, Flat Tops Wilderness Area, Colorado","docAbstract":"As part of an effort to define the hydrology and water quality of Ned Wilson Lake, evaporation rates were estimated for the summer periods of 1983 and 1984. Mass-transfer and energy-budget techniques and the Morton model were used to estimate evaporation using data collected at the lake and data collected at a meteorological station 0.1 mile from the lake. The estimate of evaporation for July 29 through September 27, 1983, using the mass-transfer technique, was 9.50 inches; the estimate using the energy-budget technique was 8.10 inches; the estimate using the Morton model was 9.90 inches. The evaporation estimate for July 18 through September 25, 1984, using the mass-transfer technique was 8.71 inches; the estimate using the energy-budget technique was 7.88 inches; the estimate using the Moron model was 10.49 inches. These estimates will provide values to be used in future analyses of the interaction of lake and groundwater; however, refinement of data collection will be necessary to determine specifically the rate of evaporation. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854244","usgsCitation":"Spahr, N., and Turk, J., 1985, Estimation of evaporation from Ned Wilson Lake, Flat Tops Wilderness Area, Colorado: U.S. Geological Survey Water-Resources Investigations Report 85-4244, iv, 13 p. :ill., map ;28 cm., https://doi.org/10.3133/wri854244.","productDescription":"iv, 13 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":126593,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4244/report-thumb.jpg"},{"id":58674,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4244/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fba16","contributors":{"authors":[{"text":"Spahr, N.E.","contributorId":79476,"corporation":false,"usgs":true,"family":"Spahr","given":"N.E.","email":"","affiliations":[],"preferred":false,"id":202259,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Turk, J.T.","contributorId":94259,"corporation":false,"usgs":true,"family":"Turk","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":202260,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16702,"text":"ofr83943 - 1985 - Ground-water data, Green River basin, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:07:05","indexId":"ofr83943","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"83-943","title":"Ground-water data, Green River basin, Wyoming","docAbstract":"Hydrologic and geologic data collected by the U.S. Geological Survey as part of energy-related projects in the Green River basin of Wyoming are compiled from the files of the Geological Survey and the Wyoming State Engineer as of 1977. The data include well and spring location, well depth, casing diameter, type of lifts, type of power, use of water, rock type of producing zone, owner, and discharge for more than 1,600 sites. Analyses for common chemical constituents, trace elements, and radioactive chemicals are tabulated as well as water temperature and specific conductance measurement data. Lithologic logs of more than 300 wells, test holes, and measured sections constitute much of this report. County maps at a scale of 1:500 ,000 show the locations. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83943","usgsCitation":"Zimmerman, E.A., and Collier, K.R., 1985, Ground-water data, Green River basin, Wyoming: U.S. Geological Survey Open-File Report 83-943, v, 511 p. :maps ;28 cm., https://doi.org/10.3133/ofr83943.","productDescription":"v, 511 p. :maps ;28 cm.","costCenters":[],"links":[{"id":148944,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0943/report-thumb.jpg"},{"id":45774,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0943/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cefe","contributors":{"authors":[{"text":"Zimmerman, Everett Alfred","contributorId":18729,"corporation":false,"usgs":true,"family":"Zimmerman","given":"Everett","email":"","middleInitial":"Alfred","affiliations":[],"preferred":false,"id":173319,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Collier, K. R.","contributorId":36152,"corporation":false,"usgs":true,"family":"Collier","given":"K.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":173320,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26417,"text":"wri854014 - 1985 - Hydrologic description of the Tamarack Wildlife area and vicinity, Logan County, Colorado, and simulated effects of possible water-management activities","interactions":[],"lastModifiedDate":"2012-02-02T00:08:33","indexId":"wri854014","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4014","title":"Hydrologic description of the Tamarack Wildlife area and vicinity, Logan County, Colorado, and simulated effects of possible water-management activities","docAbstract":"The stream-aquifer system of the Tamarack Wildlife Area and vicinity in Logan County, Colorado, is described using analyses of water level, water temperature, and specific conductance data. Correlation analysis indicated that water levels in the flood plain relate better to those in the river than those in the upgradient valley meadow. Water table surfaces showed that water moves parallel to the river with a small gradient toward the river. Water temperature data for the river had a large annual fluctuation. The temperature of well water from 0 feet below land surface had no fluctuation. The temperature of sloughs and shallow groundwater had intermediate fluctuations. Specific conductance data ranged from 264 microsiemens/cm at 25 C in sandhill wells to 1,540 microsiemens in the river. A groundwater flow model and simplified slough-temperature model showed that additional groundwater pumpage or lower river stage caused by upstream diversions would decrease groundwater inflow to the slough, with a corresponding water temperature decrease. A simulated artificial recharge project would increase groundwater inflow to the slough and increase water temperature in the slough. The simulation of a plan to pump groundwater to create wildlife-habitat ponds indicated that this would cause stream depletions each month, except during the nonpumping period, June through August. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854014","usgsCitation":"Burns, A., 1985, Hydrologic description of the Tamarack Wildlife area and vicinity, Logan County, Colorado, and simulated effects of possible water-management activities: U.S. Geological Survey Water-Resources Investigations Report 85-4014, v, 42 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854014.","productDescription":"v, 42 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124076,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4014/report-thumb.jpg"},{"id":55211,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4014/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55212,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4014/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db607059","contributors":{"authors":[{"text":"Burns, A.W.","contributorId":65498,"corporation":false,"usgs":true,"family":"Burns","given":"A.W.","email":"","affiliations":[],"preferred":false,"id":196350,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19594,"text":"ofr85327 - 1985 - Background hydrologic information in potential lignite mining areas in north-central Mississippi, August 1984","interactions":[],"lastModifiedDate":"2012-02-02T00:07:29","indexId":"ofr85327","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-327","title":"Background hydrologic information in potential lignite mining areas in north-central Mississippi, August 1984","docAbstract":"The U.S. Geological Survey, in cooperation with the Mississippi Department of Natural Resources, Bureau of Geology, is conducting a hydrologic data collection program in potential lignite-producing areas in Mississippi. During the last two weeks of August 1984, hydrologic data were collected at 15 stream sites that drain potential lignite mining areas in Lafayette, Calhoun, and Yalobusha Counties. Main channel widths ranged from approximately 60 feet at three streams (Coon Creek near Toccopula, Muckaloon Creek near Tula, and Hurricane Creek near Velma) to approximately 120 feet at two streams (Potlockney Creek near Tula, and Savannah Creek near Bruce). Maximum water depths ranged from less than 1.0 foot at most streams to over 5.0 feet at sites on Potlockney Creek near Tula and McGill Creek near Sarepta. Stream discharge ranged from 0.32 cubic feet per second in Persimmon Creek near Bruce to 18.5 cubic feet per second in Puskus Creek near Etta. The specific conductance of stream water ranged from 25 to 160 microsiemens and dissolved solids concentrations ranged from 22 to 91 mg/L (milligrams per liter). Most major ion concentrations were less than 10 mg/L with the exception of calcium (11 mg/L), sodium (12 mg/L) and sulfate (18 mg/L) in the water of Persimmon Creek near Bruce. Dissolved oxygen concentrations were greater than 5.0 mg/L at all but one site. Turbidity values were generally less than 50 units. Nitrate plus nitrite concentrations were equal to or less than 0.10 mg/L in all streams except in Potlockney Creek near Tula where the concentration was 0.11 mg/L. Copper and selenium concentrations in the water at all sampling sites ranged from below the detection limits (1 microgram/g) to 4 micrograms/g (micrograms per gram) and mercury concentrations in bottom material samples ranged from less than 0.01 microgram/g to 0.15 microgram/g. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nOpen-File Services Section, Western Distribution Branch, U.S. Geological Survey [distributor],","doi":"10.3133/ofr85327","usgsCitation":"Kalkhoff, S., 1985, Background hydrologic information in potential lignite mining areas in north-central Mississippi, August 1984: U.S. Geological Survey Open-File Report 85-327, iv, 18 p. :ill. ;29 cm., https://doi.org/10.3133/ofr85327.","productDescription":"iv, 18 p. :ill. ;29 cm.","costCenters":[],"links":[{"id":151969,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0327/report-thumb.jpg"},{"id":49062,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0327/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6496b9","contributors":{"authors":[{"text":"Kalkhoff, S. J.","contributorId":28967,"corporation":false,"usgs":true,"family":"Kalkhoff","given":"S. J.","affiliations":[],"preferred":false,"id":181181,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27856,"text":"wri854032 - 1985 - Evaluation of the Mission, Santee, and Tijuana hydrologic subareas for reclaimed-water use, San Diego County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:35","indexId":"wri854032","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4032","title":"Evaluation of the Mission, Santee, and Tijuana hydrologic subareas for reclaimed-water use, San Diego County, California","docAbstract":"A study was made to determine the suitability of three small hydrologic subareas in San Diego County, California, for reuse of treated municipal wastewater (reclaimed water). Groundwater quality has been impacted by agricultural water use, changes in natural recharge patterns, seawater intrusion, and groundwater movement from surrounding marine sediments. Groundwater levels near land surface may limit artificial recharge of reclaimed water or may require pumping of groundwater from the aquifer prior to recharge with reclaimed water. Reclaimed water may be used for irrigated water in upland areas. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854032","usgsCitation":"Izbicki, J., 1985, Evaluation of the Mission, Santee, and Tijuana hydrologic subareas for reclaimed-water use, San Diego County, California: U.S. Geological Survey Water-Resources Investigations Report 85-4032, viii, 99 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854032.","productDescription":"viii, 99 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":120066,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4032/report-thumb.jpg"},{"id":56676,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4032/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56677,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4032/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56678,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4032/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56679,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4032/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56680,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4032/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa66a","contributors":{"authors":[{"text":"Izbicki, J. A. 0000-0003-0816-4408","orcid":"https://orcid.org/0000-0003-0816-4408","contributorId":28244,"corporation":false,"usgs":true,"family":"Izbicki","given":"J. A.","affiliations":[],"preferred":false,"id":198792,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27486,"text":"wri844131 - 1985 - Ground-water quality in the Santa Rita, Buellton, and Los Olivos hydrologic subareas of the Santa Ynez River basin, Santa Barbara County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:35","indexId":"wri844131","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4131","title":"Ground-water quality in the Santa Rita, Buellton, and Los Olivos hydrologic subareas of the Santa Ynez River basin, Santa Barbara County, California","docAbstract":"Groundwater quality in the upper Santa Ynez River Valley in Santa Barbara County has degraded due to both natural and anthropogenic causes. The semiarid climate and uneven distribution of rainfall has limited freshwater recharge and caused salt buildup in water supplies. Tertiary rocks supply mineralized water. Agricultural activities (irrigation return flow containing fertilizers and pesticides, cultivation, feedlot waste disposal) are a primary cause of water quality degradation. Urban development, which also causes water quality degradation (introduced contaminants, wastewater disposal, septic system discharge, and land fill disposal of waste), has imposed stricter requirements on water supply quality. A well network was designed to monitor changes in groundwater quality related to anthropogenic activities. Information from this network may aid in efficient management of the groundwater basins as public water supplies, centered around three basic goals. First is to increase freshwater recharge to the basins by conjunctive surface/groundwater use and surface-spreading techniques. Second is to optimize groundwater discharge by efficient timing and spacing of pumping. Third is to control and reduce sources of groundwater contamination by regulating wastewater quality and distribution and, preferably, by exporting wastewaters from the basin. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844131","usgsCitation":"Hamlin, S.N., 1985, Ground-water quality in the Santa Rita, Buellton, and Los Olivos hydrologic subareas of the Santa Ynez River basin, Santa Barbara County, California: U.S. Geological Survey Water-Resources Investigations Report 84-4131, v, 75 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844131.","productDescription":"v, 75 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124174,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4131/report-thumb.jpg"},{"id":56337,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4131/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db66721c","contributors":{"authors":[{"text":"Hamlin, S. N.","contributorId":46560,"corporation":false,"usgs":true,"family":"Hamlin","given":"S.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":198200,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26992,"text":"wri854066 - 1985 - Identification and characterization of hydrologic properties of fractured tuff using hydraulic and tracer tests — Test well USW H-4, Yucca Mountain, Nye County, Nevada","interactions":[],"lastModifiedDate":"2022-01-20T20:17:47.456542","indexId":"wri854066","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4066","title":"Identification and characterization of hydrologic properties of fractured tuff using hydraulic and tracer tests — Test well USW H-4, Yucca Mountain, Nye County, Nevada","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854066","usgsCitation":"Erickson, J., and Waddell, R.K., 1985, Identification and characterization of hydrologic properties of fractured tuff using hydraulic and tracer tests — Test well USW H-4, Yucca Mountain, Nye County, Nevada: U.S. Geological Survey Water-Resources Investigations Report 85-4066, Report: iv, 30 p.; 1 Plate: 20.14 × 26.46 inches, https://doi.org/10.3133/wri854066.","productDescription":"Report: iv, 30 p.; 1 Plate: 20.14 × 26.46 inches","costCenters":[],"links":[{"id":394611,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36246.htm"},{"id":55878,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4066/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55879,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4066/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121854,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4066/report-thumb.jpg"}],"country":"United States","state":"Nevada","county":"Nye County","otherGeospatial":"test well USW H-4, Yucca Mountain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.467,\n              36.833\n            ],\n            [\n              -116.443,\n              36.833\n            ],\n            [\n              -116.443,\n              36.85\n            ],\n            [\n              -116.467,\n              36.85\n            ],\n            [\n              -116.467,\n              36.833\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faafb","contributors":{"authors":[{"text":"Erickson, J.R.","contributorId":66689,"corporation":false,"usgs":true,"family":"Erickson","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":197371,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waddell, R. K.","contributorId":25560,"corporation":false,"usgs":true,"family":"Waddell","given":"R.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":197370,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30650,"text":"wri854226 - 1985 - Hydrology and water-quality monitoring considerations, Jackpile uranium mine, northwestern New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:09:01","indexId":"wri854226","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4226","title":"Hydrology and water-quality monitoring considerations, Jackpile uranium mine, northwestern New Mexico","docAbstract":"The Jackpile Uranium Mine, which is on the Pueblo of Laguna in northwestern New Mexico, was operated from 1953 to 1980. The mine and facilities have affected 3,141 acres of land, and about 2,656 acres were yet to be reclaimed by late 1980. The intended use of the restored land is stock grazing. Fractured Dakota Sandstone and Mancos Shale of Cretaceous age overlie the Jackpile sandstone and a 200-ft-thick tight mudstone unit of the Brushy Basin Member underlies the Jackpile. The hydraulic conductivity of the Jackpile sandstone probably is about 0.3 ft/day. The small storage coefficients determined from three aquifer tests indicate that the Jackpile sandstone is a confined hydrologic system throughout much of the mine area. Sediment from the Rio Paguate has nearly filled the Paguate Reservoir near Laguna since its construction in 1940. The mean concentrations of uranium, Ra-226, and other trace elements generally were less than permissible limits established in national drinking water regulations or New Mexico State groundwater regulations. No individual surface water samples collected upstream from the mine contained concentrations of Ra-226 in excess of the permissible limits. Ra-226 concentrations in many individual samples collected from the Rio Paguate from near the mouth of the Rio Moquino to the sampling sites along the downstream reach of the Rio Paguate, however, exceeded the recommended permissible concentration of Ra-226 for public drinking water supplies. Concentrations in surface water apparently are changed by groundwater inflow near the confluence of the two streams. The altitude of the water tables in the backfill of the pits will be controlled partly by the water level in the Rio Paguate. Other factors controlling the altitudes of the water tables are the recharge rate to the backfill and the hydraulic conductivities of the backfill, alluvium, Jackpile sandstone, and mudstone unit of the Brushy Basin Member. After reclamation, most of the shallow groundwater probably will discharge to the natural stream channels draining the mine area. Groundwater quality may be monitored as: (1) ' Limited monitoring, ' in which only the change in water quality is determined as the groundwater flows from the mine; or (2) ' thorough monitoring, ' in which specific sources of possible contaminants are described. (Author 's Abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854226","usgsCitation":"Zehner, H., 1985, Hydrology and water-quality monitoring considerations, Jackpile uranium mine, northwestern New Mexico: U.S. Geological Survey Water-Resources Investigations Report 85-4226, vi, 61 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854226.","productDescription":"vi, 61 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123499,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4226/report-thumb.jpg"},{"id":59422,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4226/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59423,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4226/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e78b","contributors":{"authors":[{"text":"Zehner, H.H.","contributorId":105322,"corporation":false,"usgs":true,"family":"Zehner","given":"H.H.","email":"","affiliations":[],"preferred":false,"id":203604,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44511,"text":"wri834261 - 1985 - Hydrology of Lake Carroll, Hillsborough County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:10:14","indexId":"wri834261","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"83-4261","title":"Hydrology of Lake Carroll, Hillsborough County, Florida","docAbstract":"Lakeshore property around Lake Carroll has undergone extensive residential development since 1960. This development increased the lake shoreline, altered surface water flow to and from the lake, and may have affected lake-stage characteristics. Some areas of the lake were dredged to provide fill material for lakefront property. Water-balance analyses for 1952-60, a predevelopment period, and 1961-80, a period of residential development, indicate that both net surface water flow to the lake and downward leakage from the lake to the Floridan aquifer were greater after 1960. These changes were due more to changes in the regional climate and related changes in ground-water levels than to changes associated with residential development. Results of water quality analyses in 1980-81 are within State limits for surface waters used for recreation and wildlife propagation. (USGS)","language":"ENGLISH","doi":"10.3133/wri834261","usgsCitation":"Henderson, S., Hayes, R., and Stoker, Y., 1985, Hydrology of Lake Carroll, Hillsborough County, Florida: U.S. Geological Survey Water-Resources Investigations Report 83-4261, 4 maps on 1 sheet : col. ; 41 x 37 cm. and smaller, on sheet 80 x 112 cm., https://doi.org/10.3133/wri834261.","productDescription":"4 maps on 1 sheet : col. ; 41 x 37 cm. and smaller, on sheet 80 x 112 cm.","costCenters":[],"links":[{"id":170404,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81893,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4261/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db6048ba","contributors":{"authors":[{"text":"Henderson, S.E.","contributorId":70806,"corporation":false,"usgs":true,"family":"Henderson","given":"S.E.","email":"","affiliations":[],"preferred":false,"id":229910,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hayes, R.D.","contributorId":19197,"corporation":false,"usgs":true,"family":"Hayes","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":229909,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stoker, Y.E.","contributorId":13253,"corporation":false,"usgs":true,"family":"Stoker","given":"Y.E.","email":"","affiliations":[],"preferred":false,"id":229908,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":28879,"text":"wri854197 - 1985 - Evaluation of the effects of coal-mine reclamation on water quality in Big Four Hollow near Lake Hope, southeastern Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:08:53","indexId":"wri854197","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4197","title":"Evaluation of the effects of coal-mine reclamation on water quality in Big Four Hollow near Lake Hope, southeastern Ohio","docAbstract":"A subsurface clay dike and mine-entrance hydraulic seals were constructed from July 1979 through May 1980 by the Ohio Department if Natural Resources, Division of Reclamation to reduce acidic mine drainage from abandoned drift-mine complex 88 into Big Four Hollow Creek. Big Four Hollow Creek flows into Sandy Run--the major tributary to Lake Hope. A data-collection program was established in 1979 by the U.S. Geological Survey to evaluate effects of drift-mine sealing on surface-water systems of the Big Four Hollow Creek and Sandy Run area just below the mine.\r\n\r\nData collected by private consultants from 1970 through 1971 near the mouth of Big Four Hollow Creek (U.S. Geological Survey station 03201700) show that pH ranged from 2.7 to 4.8, with a median of 3.1. The calculated iron load was 50 pounds per day.\r\n\r\nData collecetd near the mouth of Big Four Hollow Creek (station 03201700) from 1971 through 1979 (before dike construction) show the daily pH ranged from 2.1 to 6.7; the median was 3.6. The daily specific conduction ranged from 72 to 3,500 microsiements per centimeter at 25? Celsius and averaged 770. The estimated loads of chemical constituents were: Sulfate, 1,100 pounds per day: iron, 54 pounds per day: and manganese, 12 pounds per day.\r\n\r\nAll postconstruction data collected at station 03201700 through the end of the project, May 1980 through June 30, 1983, show that the daily pH ranged from 2.4 to 7.7, with a median of 3.7. Daily specific conductance ranged from 87 to 3,200 microsiemens per centimeter and averaged 1,200. The estimated loads of chemical constituents for this period were: Sulfate, 1,000 pounds per day: iron, 44 pounds per day: and manganese, 16 pounds per day.\r\n\r\nStandard nonparametric statistical tests were performed on the data collected before and after reclamation. Differences at the 95-percent confidence level were found in the before- and after-reclamation data sets for specific conductance, aluminum, and manganese at station 03201700. Data collected during the first 6 months after reclamation indicated moderate improvement in water quality only because no highly mineralized water was leaking from the closed mine. Later, perhaps in Sepember 1980 increased hydraulic head behind the clay dike caused the mine water to seep out and degrade the stream-water quality.\r\n\r\nIn order to investigate leakages, dye was injected into two wells that penetrated the closed mine complex 88. One injection revealed that the dye moved to a discharge point at a nearby mine entrance known to be connected to complex 88. No discharge of dye was detected as a result of dye injection into the other well during the project.\r\n\r\nAcidic mine water continues to seep from the closed mine complex 88. A definitive evaluation of the effects of reclamation on the area's water quality cannot be made until the hydrologic system stabilizes.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854197","usgsCitation":"Nichols, V., 1985, Evaluation of the effects of coal-mine reclamation on water quality in Big Four Hollow near Lake Hope, southeastern Ohio: U.S. Geological Survey Water-Resources Investigations Report 85-4197, vi, 215 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854197.","productDescription":"vi, 215 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123882,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4197/report-thumb.jpg"},{"id":57754,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4197/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa447","contributors":{"authors":[{"text":"Nichols, V.E.","contributorId":97930,"corporation":false,"usgs":true,"family":"Nichols","given":"V.E.","email":"","affiliations":[],"preferred":false,"id":200551,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44496,"text":"wri844215 - 1985 - Potentiometric surfaces of November 1982 and declines in the potentiometric surfaces between the period prior to development and November 1982 for the coastal plain aquifers of South Carolina","interactions":[],"lastModifiedDate":"2017-01-24T10:06:01","indexId":"wri844215","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4215","title":"Potentiometric surfaces of November 1982 and declines in the potentiometric surfaces between the period prior to development and November 1982 for the coastal plain aquifers of South Carolina","docAbstract":"Characteristics of the Coastal Plains aquifer of South Carolina are being studied as a part of the Regional Aquifer Systems Analysis program of the U.S. Geological Survey. A framework has been developed to best represent the hydrology of the State by dividing the aquifers into a system of five aquifers. This framework includes a surficial aquifer consisting of coastal terrace deposits, a limestone and stratigraphically equivalent sand aquifer of Eocene age, and three sand aquifers of Cretaceous age. (USGS)","language":"ENGLISH","doi":"10.3133/wri844215","usgsCitation":"Aucott, W.R., and Speiran, G.K., 1985, Potentiometric surfaces of November 1982 and declines in the potentiometric surfaces between the period prior to development and November 1982 for the coastal plain aquifers of South Carolina: U.S. Geological Survey Water-Resources Investigations Report 84-4215, 7 maps : col. ; 36 x 46 cm., on sheets 66 x 79 cm., folded in envelope 32 x 24 cm., https://doi.org/10.3133/wri844215.","productDescription":"7 maps : col. ; 36 x 46 cm., on sheets 66 x 79 cm., folded in envelope 32 x 24 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science 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,{"id":12386,"text":"ofr85191 - 1985 - Ground-water data from the San Miguel River basin, southwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:40","indexId":"ofr85191","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-191","title":"Ground-water data from the San Miguel River basin, southwestern Colorado","docAbstract":"Hydrologic data were collected from 36 wells and 80 springs in the San Miguel River basin from 1977 to 1979. Depth to water was measured for 22 wells and discharges were measured for 53 springs. Chemical analyses for water samples collected from 23 wells and 25 springs indicated larger dissolved solids concentrations in bedrock water samples than in alluvial water samples. Drillers ' records obtained from the Colorado State Engineer 's Office for 86 wells indicate generally larger yields from wells completed in alluvium than in bedrock. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85191","usgsCitation":"Ackerman, D.J., and Brooks, T., 1985, Ground-water data from the San Miguel River basin, southwestern Colorado: U.S. Geological Survey Open-File Report 85-191, v, 19 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr85191.","productDescription":"v, 19 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":145676,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0191/report-thumb.jpg"},{"id":40621,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1985/0191/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40622,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0191/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cf35","contributors":{"authors":[{"text":"Ackerman, D. J.","contributorId":53380,"corporation":false,"usgs":true,"family":"Ackerman","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":166047,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brooks, T.D.","contributorId":47373,"corporation":false,"usgs":true,"family":"Brooks","given":"T.D.","email":"","affiliations":[],"preferred":false,"id":166046,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":47716,"text":"wri854112 - 1985 - Maps of the Bonsall area of the San Luis Rey River valley, San Diego County, California, showing geology, hydrology, and ground-water quality","interactions":[],"lastModifiedDate":"2015-09-24T15:20:56","indexId":"wri854112","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4112","title":"Maps of the Bonsall area of the San Luis Rey River valley, San Diego County, California, showing geology, hydrology, and ground-water quality","docAbstract":"<p>In November 1984, 84 wells and 1 spring in the Bonsall area of the San Luis Rey River valley were inventoried by U.S. Geological Survey personnel. Depth to water in 38 wells ranged from 1.3 to 38 ft and 23 wells had depths to water less than 10 feet. Dissolved solids concentration of water from 29 wells and 1 spring sampled in autumn 1983 and spring 1984 ranged from 574 to 2,370 mgs/L. Groundwater with a dissolved solids concentration less than 1,000 mgs/L was generally restricted to the eastern part of the aquifer. The total volume of alluvial fill in the Bonsall area is 113,000 acre-feet; the amount of groundwater storage available in the alluvial aquifer is 18,000 acre-feet. The alluvial aquifer is, in part, surrounded and underlain by colluvium and weathered crystalline rock that add some additional groundwater storage capacity to the system. Data in this report are presented on five maps showing well locations , thickness of alluvial fill, water level contours in November 1983 and hydrographs of selected wells, groundwater quality in spring 1960 and graphs showing changes in dissolved solids concentrations of water from selected wells with time, and groundwater quality in spring 1984. This report is part of a larger cooperative project between the Rainbow Municipal Irrigation District and the U.S. Geological Survey. The purpose of the larger project is to develop an appropriate groundwater management plan for the Bonsall area of the San Luis Rey River valley. (USGS)</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854112","usgsCitation":"Izbicki, J., 1985, Maps of the Bonsall area of the San Luis Rey River valley, San Diego County, California, showing geology, hydrology, and ground-water quality: U.S. Geological Survey Water-Resources Investigations Report 85-4112, 5 Plates: 27.66 x 29.98 inches or smaller, https://doi.org/10.3133/wri854112.","productDescription":"5 Plates: 27.66 x 29.98 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308562,"rank":301,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4112/plate-2.pdf","text":"Plate 2","size":"17,543 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":84625,"rank":300,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4112/plate-1.pdf","text":"Plate 1","size":"16,080 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":169426,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4112/report-thumb.jpg"},{"id":308563,"rank":302,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4112/plate-3.pdf","text":"Plate 3","size":"16,194 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":308564,"rank":303,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4112/plate-4.pdf","text":"Plate 4","size":"17,766 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":308565,"rank":304,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4112/plate-5.pdf","text":"Plate 5","size":"15,405 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"San Diego County","otherGeospatial":"San Luis Rey River Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.32437133789061,\n              33.10879798900969\n            ],\n            [\n              -117.32437133789061,\n              33.415967956844625\n            ],\n            [\n              -116.96113586425781,\n              33.415967956844625\n            ],\n            [\n              -116.96113586425781,\n              33.10879798900969\n            ],\n            [\n              -117.32437133789061,\n              33.10879798900969\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fc199","contributors":{"authors":[{"text":"Izbicki, John A. 0000-0003-0816-4408 jaizbick@usgs.gov","orcid":"https://orcid.org/0000-0003-0816-4408","contributorId":1375,"corporation":false,"usgs":true,"family":"Izbicki","given":"John A.","email":"jaizbick@usgs.gov","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":236066,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12374,"text":"ofr85346 - 1985 - Water-resources activities of the U.S. Geological Survey in Texas; fiscal years 1982-84","interactions":[],"lastModifiedDate":"2016-08-12T13:45:36","indexId":"ofr85346","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-346","title":"Water-resources activities of the U.S. Geological Survey in Texas; fiscal years 1982-84","docAbstract":"<p>The U.S. Geological Survey (USGS) was established by an act of Congress on March 3, 1879, to provide a permanent Federal agency to conduct the systematic and scientific classification of the public lands, and examination of the geological structure, mineral resources, and products of national domain. An integral part of that original mission includes publishing and disseminating the earth-science information needed to understand, to plan the use of, and to manage the Nation's energy, land, mineral, and water resources.</p>\n<p>Since 1879, the research and fact-finding role of the USGS has grown and been modified to meet the changing needs of the Nation it serves. As part of that evolution, the USGS has become the Federal Government's largest earth-science research agency, the Nation's largest civilian mapmaking agency, the primary source of data on the Nation's surface- and ground-water resources, and the employer of the largest number of professional earth scientists. Today's programs serve a diversity of needs and users. Programs include:</p>\n<ul>\n<li>Conducting detailed assessments of the energy and mineral potential of the Nation's land and offshore areas.</li>\n<li>Investigating and issuing warnings of earthquakes, volcanic eruptions, landslides, and other geologic and hydrologic hazards.</li>\n<li>Conducting research on the geologic structure of the Nation.</li>\n<li>Studying the geologic features, structure, processes, and history of the other planets of our solar system.</li>\n<li>Conducting topographic surveys of the Nation and preparing topographic and thematic maps and related cartographic products.</li>\n<li>Developing and producing digital cartographic data bases and products.</li>\n<li>Collecting data on a routine basis to determine the quantity, quality, and use of surface and ground water.</li>\n<li>Conducting water-resources appraisals in order to describe the consequences of alternative plans for developing land and water resources.</li>\n<li>Conducting research in hydraulics and hydrology and coordinating all Federal water-data acquisition.</li>\n<li>Using remotely sensed data to develop new cartographic, geologic, and hydrologic research techniques for natural resources planning and management.</li>\n<li>Providing earth-science information through an extensive publications program and a network of public access points.</li>\n</ul>\n<p>Along with its continuing commitment to meet the growing and changing earthscience information needs of the Nation, the USGS remains dedicated to its original mission to collect, analyze, interpret, publish, and disseminate information about the natural resources of the Nation providing \"earth science in the public service.\"</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr85346","usgsCitation":"Grozier, R., and Land, L.F., 1985, Water-resources activities of the U.S. Geological Survey in Texas; fiscal years 1982-84: U.S. Geological Survey Open-File Report 85-346, iv, 60 p., https://doi.org/10.3133/ofr85346.","productDescription":"iv, 60 p.","numberOfPages":"64","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":145861,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0346/report-thumb.jpg"},{"id":40611,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0346/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9a1e","contributors":{"authors":[{"text":"Grozier, R.U.","contributorId":105704,"corporation":false,"usgs":true,"family":"Grozier","given":"R.U.","affiliations":[],"preferred":false,"id":166024,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Land, L. F.","contributorId":17253,"corporation":false,"usgs":true,"family":"Land","given":"L.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":166023,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":12372,"text":"ofr85422 - 1985 - Water-resources activities of the U.S. Geological Survey in South Dakota; fiscal year 1984","interactions":[],"lastModifiedDate":"2012-02-02T00:06:39","indexId":"ofr85422","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-422","title":"Water-resources activities of the U.S. Geological Survey in South Dakota; fiscal year 1984","docAbstract":"Project descriptions, water-resources summaries, and lists of hydrologic-data stations are presented to show the status of the U.S. Geological survey water-resources studies in South Dakota. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85422","usgsCitation":"LeRoux, E.F., and Decker, E., 1985, Water-resources activities of the U.S. Geological Survey in South Dakota; fiscal year 1984: U.S. Geological Survey Open-File Report 85-422, iii, 62 p. :ill. ;28 cm., https://doi.org/10.3133/ofr85422.","productDescription":"iii, 62 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":145859,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0422/report-thumb.jpg"},{"id":40608,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0422/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4f8d","contributors":{"authors":[{"text":"LeRoux, E. F.","contributorId":29795,"corporation":false,"usgs":true,"family":"LeRoux","given":"E.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":166020,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Decker, E.M.","contributorId":43345,"corporation":false,"usgs":true,"family":"Decker","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":166021,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68090,"text":"ha684 - 1985 - Hydrologic reconnaissance of the Kolob, Alton, and Kaiparowits Plateau coal fields, south-central Utah","interactions":[{"subject":{"id":10703,"text":"ofr8471 - 1984 - Hydrologic reconnaissance of the Kolob, Alton, and Kaiparowits Plateau coal fields, south-central Utah","indexId":"ofr8471","publicationYear":"1984","noYear":false,"title":"Hydrologic reconnaissance of the Kolob, Alton, and Kaiparowits Plateau coal fields, south-central Utah"},"predicate":"SUPERSEDED_BY","object":{"id":68090,"text":"ha684 - 1985 - Hydrologic reconnaissance of the Kolob, Alton, and Kaiparowits Plateau coal fields, south-central Utah","indexId":"ha684","publicationYear":"1985","noYear":false,"title":"Hydrologic reconnaissance of the Kolob, Alton, and Kaiparowits Plateau coal fields, south-central Utah"},"id":1}],"lastModifiedDate":"2022-12-27T21:46:48.280079","indexId":"ha684","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"684","title":"Hydrologic reconnaissance of the Kolob, Alton, and Kaiparowits Plateau coal fields, south-central Utah","docAbstract":"<p><span>The study area in south-central Utah (fig. 1) is noted for its large coal reserves in the Alton, Kolob, and Kaiparowits Plateau coal fields. The area also is noted for its scenic beauty and general scarcity of water. Although there has been very little development of the coal resources through 1983, there is a potential for large-scale development with both surface- and underground-mining methods. Mining of coal could have significant effects on the quantity and quality of the water resources. The purpose of this atlas is to define the surface- and ground-water resources of the area and to identify the potential effects on these resources by coal mining.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha684","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Plantz, G.G., 1985, Hydrologic reconnaissance of the Kolob, Alton, and Kaiparowits Plateau coal fields, south-central Utah: U.S. Geological Survey Hydrologic Atlas 684, 2 Plates: 34.0 x 42.5 inches and 34.0 x 40.0 inches, https://doi.org/10.3133/ha684.","productDescription":"2 Plates: 34.0 x 42.5 inches and 34.0 x 40.0 inches","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":186226,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":411087,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16082.htm","linkFileType":{"id":5,"text":"html"}},{"id":91830,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/684/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}},{"id":91829,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/684/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Utah","otherGeospatial":"Alton coal field, Kaiparowits Plateau coal field, Kolob coal field","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.25,\n              37\n            ],\n            [\n              -110.9,\n              37\n            ],\n            [\n              -110.9,\n              38\n            ],\n            [\n              -113.25,\n              38\n            ],\n            [\n              -113.25,\n              37\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db605524","contributors":{"authors":[{"text":"Plantz, Gerald G.","contributorId":96149,"corporation":false,"usgs":true,"family":"Plantz","given":"Gerald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":277624,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13219,"text":"ofr85645 - 1985 - Annual water-resources review, White Sands Missile Range, New Mexico, 1984","interactions":[],"lastModifiedDate":"2012-02-02T00:06:48","indexId":"ofr85645","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-645","title":"Annual water-resources review, White Sands Missile Range, New Mexico, 1984","docAbstract":"Hydrologic data were collected at White Sands Missile Range in 1984. The total groundwater withdrawal in 1984 was 685,275,000 gallons. The Post Headquarters well field produced 650,821,000 gallons in 1984. Six new wells were drilled at White Sands Missile Range in 1984. Nineteen water samples were collected for major chemical-constituent, trace-element, or radiochemical analysis in 1984. Depth-to-water measurements in the Post Headquarters supply wells showed seasonal fluctuations as well as continued long-term declines. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85645","usgsCitation":"Cruz, R.R., 1985, Annual water-resources review, White Sands Missile Range, New Mexico, 1984: U.S. Geological Survey Open-File Report 85-645, iv, 25 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr85645.","productDescription":"iv, 25 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":146112,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0645/report-thumb.jpg"},{"id":41600,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0645/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b743","contributors":{"authors":[{"text":"Cruz, R. R.","contributorId":97496,"corporation":false,"usgs":true,"family":"Cruz","given":"R.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":167424,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26394,"text":"wri844318 - 1985 - The hydrologic bench-mark program; a standard to evaluate time-series trends in selected water-quality constituents for streams in Georgia","interactions":[],"lastModifiedDate":"2017-01-24T10:13:42","indexId":"wri844318","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4318","title":"The hydrologic bench-mark program; a standard to evaluate time-series trends in selected water-quality constituents for streams in Georgia","docAbstract":"Significant temporal trends in monthly pH, specific conductance, total alkalinity, hardness, total nitrite-plus-nitrite nitrogen, and total phosphorus measurements at five stream sites in Georgia were identified using a rank correlation technique, the seasonal Kendall test and slope estimator. These sites include a U.S. Geological Survey Hydrologic Bench-Mark site, Falling Creek near Juliette, and four periodic water-quality monitoring sites. Comparison of raw data trends with streamflow-residual trends and, where applicable, with chemical-discharge trends (instantaneous fluxes) shws that some of these trends are responses to factors other than changing streamflow. Percentages of forested, agricultural, and urban cover with each basin did not change much during the periods of water-quality record, and therefore these non-flow-related trends are not obviously related to changes in land cover or land use. Flow-residual water-quality trends at the Hydrologic Bench-Mark site and at the Chattooga River site probably indicate basin reponses to changes in the chemical quality of atmospheric deposition. These two basins are predominantly forested and have received little recent human use. Observed trends at the other three sites probably indicate basin responses to various land uses and water uses associated with agricultural and urban land or to changes in specific uses. 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,{"id":13241,"text":"ofr85423 - 1985 - January 1985 water levels, and data related to water-level changes, western and south-central Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:06:56","indexId":"ofr85423","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-423","title":"January 1985 water levels, and data related to water-level changes, western and south-central Kansas","docAbstract":"Hydrologic data related to water level measurements made in approximately 1,350 observation wells in western and south-central Kansas are shown in this report. The measurements were made in mid-winter when pumping was minimal and water levels had recovered, for the most part, form the effects of pumping during the previous irrigation season. Annual hydrologic data are provided for relating water level changes from a ' base-reference year ' (predevelopment year), a year of abnormally high rainfall and minimum pumpage (1966 or 1974), and each of 7 consecutive years of measurement (1979-85). The ' base-reference year ' is designated as 1940 for the southwestern area, 1944 for the south-central area, and 1950 for the northwestern, west-central, and Equus Beds areas. Data also are provided for relating the average annual water level changes, saturated thickness of the deposits, and percentage changes in saturated thickness. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85423","usgsCitation":"Dague, B., 1985, January 1985 water levels, and data related to water-level changes, western and south-central Kansas: U.S. Geological Survey Open-File Report 85-423, iv, 162 p. :maps ;28 cm., https://doi.org/10.3133/ofr85423.","productDescription":"iv, 162 p. :maps ;28 cm.","costCenters":[],"links":[{"id":146921,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0423/report-thumb.jpg"},{"id":41626,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0423/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc4c7","contributors":{"authors":[{"text":"Dague, B.J.","contributorId":45723,"corporation":false,"usgs":true,"family":"Dague","given":"B.J.","affiliations":[],"preferred":false,"id":167457,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13301,"text":"ofr85476 - 1985 - Hydrologic and micrometeorologic data from an unsaturated zone study at a low-level radioactive waste burial site near Barnwell, South Carolina","interactions":[],"lastModifiedDate":"2016-12-14T14:15:13","indexId":"ofr85476","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-476","title":"Hydrologic and micrometeorologic data from an unsaturated zone study at a low-level radioactive waste burial site near Barnwell, South Carolina","docAbstract":"Two years of selected hydrologic and micrometeorologic data collected at a low-level radioactive waste burial site near Barnwell, South Carolina are available on magnetic tape in card-image format. Hydrologic data include daily measurements of soil-moisture tension, soil-moisture specific conductance, and soil temperature at four monitoring site locations. Micrometeorlogic data include hourly measurements for the following parameters: dry- and wet-bulb temperatures, soil temperatures, soil heat flux, wind speeds and direction, incoming and reflected short-wave solar radiation, incoming and emitted long-wave radiation, net radiation and precipitation. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85476","usgsCitation":"Dennehy, K., and McMahon, P., 1985, Hydrologic and micrometeorologic data from an unsaturated zone study at a low-level radioactive waste burial site near Barnwell, South Carolina: U.S. Geological Survey Open-File Report 85-476, iv, 32 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr85476.","productDescription":"iv, 32 p. :ill., map ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":147370,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0476/report-thumb.jpg"},{"id":41720,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0476/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South Carolina","county":"Barnwell","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-81.2198,33.4393],[-81.2148,33.3902],[-81.2215,33.2295],[-81.2176,33.2209],[-81.224,33.1581],[-81.2119,33.1476],[-81.2069,33.1344],[-81.1943,33.1231],[-81.2304,33.1176],[-81.2442,33.1189],[-81.2589,33.1134],[-81.2836,33.1083],[-81.3652,33.1081],[-81.4354,33.1297],[-81.4519,33.1346],[-81.5123,33.1503],[-81.5419,33.1579],[-81.5708,33.1332],[-81.6142,33.0953],[-81.6187,33.0952],[-81.6241,33.0946],[-81.6268,33.0941],[-81.6323,33.0928],[-81.6362,33.0924],[-81.6395,33.0923],[-81.6428,33.0928],[-81.6466,33.0937],[-81.6494,33.0949],[-81.6532,33.0973],[-81.6536,33.0977],[-81.6569,33.1009],[-81.6611,33.1041],[-81.6621,33.1046],[-81.667,33.1072],[-81.6752,33.1099],[-81.6851,33.1135],[-81.6961,33.1161],[-81.6993,33.1166],[-81.7016,33.117],[-81.7025,33.1172],[-81.7053,33.1183],[-81.7076,33.1188],[-81.7098,33.1207],[-81.7126,33.1224],[-81.7162,33.1243],[-81.7189,33.1252],[-81.7211,33.1257],[-81.7236,33.1278],[-81.7263,33.13],[-81.7297,33.1332],[-81.7352,33.1368],[-81.7407,33.1409],[-81.7428,33.1424],[-81.7479,33.1463],[-81.7545,33.1517],[-81.759,33.1557],[-81.7622,33.1599],[-81.7648,33.1649],[-81.767,33.1708],[-81.7673,33.1716],[-81.7691,33.1758],[-81.7701,33.1777],[-81.7701,33.1795],[-81.7689,33.1808],[-81.7674,33.1817],[-81.7669,33.183],[-81.7669,33.1839],[-81.7673,33.1864],[-81.7662,33.1877],[-81.7655,33.1881],[-81.7636,33.1894],[-81.762,33.1903],[-81.7615,33.1907],[-81.7609,33.1913],[-81.7588,33.1931],[-81.7577,33.1949],[-81.7573,33.1972],[-81.7575,33.1982],[-81.5165,33.3824],[-81.373,33.4907],[-81.3399,33.4831],[-81.3251,33.485],[-81.3047,33.48],[-81.2738,33.4637],[-81.2463,33.4442],[-81.2198,33.4393]]]},\"properties\":{\"name\":\"Barnwell\",\"state\":\"SC\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6117f3","contributors":{"authors":[{"text":"Dennehy, K.F.","contributorId":41841,"corporation":false,"usgs":true,"family":"Dennehy","given":"K.F.","affiliations":[],"preferred":false,"id":167568,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McMahon, P.B. 0000-0001-7452-2379","orcid":"https://orcid.org/0000-0001-7452-2379","contributorId":10762,"corporation":false,"usgs":true,"family":"McMahon","given":"P.B.","affiliations":[],"preferred":false,"id":167567,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":12368,"text":"ofr85181 - 1985 - Water-resources activities of the U.S. Geological Survey in Nebraska, 1984","interactions":[],"lastModifiedDate":"2012-02-02T00:06:40","indexId":"ofr85181","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-181","title":"Water-resources activities of the U.S. Geological Survey in Nebraska, 1984","docAbstract":"The State of Nebraska has a greater abundance of water than most of the surrounding States. The major water issues in the State concern the management of these water resources in regard to their availability areally across the State and temporally over the changing seasons and cycles of weather. Management also concerns the protection of the supply of water from deterioration through contamination. The U.S. Geological Survey (USGS) in Nebraska began providing data to allow for better management of the State 's water near the end of the 19th Century. Since then the USGS activities have continued and have included the monitoring of hydrologic conditions, detailed studies to describe the hydrology of specific areas, and studies to add to the basic scientific knowledge of hydrology. Projects in all these areas continue. The work has been supported through Federal funding, through support from other Federal agencies, and through cooperative programs with many State and local agencies. This report summarizes these activities which are ongoing in the State of Nebraska. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85181","usgsCitation":"McKinney, J., 1985, Water-resources activities of the U.S. Geological Survey in Nebraska, 1984: U.S. Geological Survey Open-File Report 85-181, vi, 33 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr85181.","productDescription":"vi, 33 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":145819,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0181/report-thumb.jpg"},{"id":40604,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0181/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9e87","contributors":{"authors":[{"text":"McKinney, J.E.","contributorId":31774,"corporation":false,"usgs":true,"family":"McKinney","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":166016,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30273,"text":"wri844121 - 1985 - Compilation of water resources development and hydrologic data of Saipan, Mariana Islands","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri844121","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4121","title":"Compilation of water resources development and hydrologic data of Saipan, Mariana Islands","docAbstract":"Saipan is the largest island of the Northern Mariana Islands, a chain of 14 islands north of Guam. Saipan comprises one third of the land area of the islands. No long-term rainfall record is available at any location, but some rainfall records are for periods up to 16 years, some of which began in 1901. Average annual rainfall for the island is 81 inches, with the southern end receiving about 10 inches less annually than the rest of the island. The amount of rainfall which runs off in northeast Saipan ranges from 23 to 64 percent and averages about 40 percent. Runoff on the rest of the island is from springs or occurs only during heavy rainfall. Surface-water development appears impractical. Ground water is the main source of water for the island and production was almost 4 million gallons per day in 1982. However, chloride concentration in ground water exceeds 1,000 milligrams per liter in many locations. The average chloride concentration of the domestic water stays near the maximum permissible level (600 milligrams per liter). This report summarizes the history of the water-resources development and presents all available hydrologic data, including rainfall records since 1901, streamflow records since 1968, and drilling logs, pumping tests, chemical analyses, and production figures from 180 testholes and wells drilled on Saipan. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844121","usgsCitation":"Van der Brug, O., 1985, Compilation of water resources development and hydrologic data of Saipan, Mariana Islands: U.S. Geological Survey Water-Resources Investigations Report 84-4121, x, 578 p. :ill. ;28 cm., https://doi.org/10.3133/wri844121.","productDescription":"x, 578 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":123890,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4121/report-thumb.jpg"},{"id":59056,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4121/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8408","contributors":{"authors":[{"text":"Van der Brug, Otto","contributorId":37347,"corporation":false,"usgs":true,"family":"Van der Brug","given":"Otto","email":"","affiliations":[],"preferred":false,"id":202968,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29198,"text":"wri854220 - 1985 - Dissolved constituents including selenium in waters in the vicinity of Kesterson National Wildlife Refuge and the west grassland, Fresno and Merced Counties, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:50","indexId":"wri854220","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4220","title":"Dissolved constituents including selenium in waters in the vicinity of Kesterson National Wildlife Refuge and the west grassland, Fresno and Merced Counties, California","docAbstract":"Analyses were made for dissolved constituents including selenium (Se) in waters associated with subsurface agricultural drainage from the western San Joaquin Valley of California. In the vicinity of Kesterson National Wildlife Refuge and the Grassland wetlands area Se was found to be mobilized in water. As a consequence of this mobility and bioaccumulation in the aquatic food chain, Se occurred in waterfowl at levels toxic enough to cause deformities and deaths. Se concentrations in sumps that collect subsurface agricultural drainage water and inflows to drains sampled, ultimately leading into Kesterson National Wildlife Refuge and the Grassland, ranged from 84 to 4200 microgram/L (ug/L) Se. Levels of Se were reduced in the San Luis Drain flowing into Kesterson National Wildlife Refute to approximately 300 ug/L Se and in three of the drains sampled flowing into the Grassland to approximately 50 ug/L Se. Serious effects on water fowl habitat were caused by both these levels. Se contents of algal mats and salt crusts from evaporation ponds of the San Luis Drain contained up to parts per million Se. Total ecosystem assessment of Se may be necessary for the evaluation of the toxicity of Se to the environment. No other trace element reported exceeded the various criteria for water at the level of magnitude of Se. Other dissolved constituents and the isotopic ratios of oxygen and hydrogen were analyzed to elucidate water types, reaction states of the aqueous solution with respect to minerals, and the origin of mixed waters. These data will be used later to evaluate the geologic source of Se. Methods used for collection and analysis are described and documented. Hydrologic effects were found to be complex. Preliminary indications from wells are also given. A historical sequence is adhered to and other data from the study area which serve as a guide to the toxicity of Se are included. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854220","usgsCitation":"Presser, T.S., and Barnes, I., 1985, Dissolved constituents including selenium in waters in the vicinity of Kesterson National Wildlife Refuge and the west grassland, Fresno and Merced Counties, California: U.S. Geological Survey Water-Resources Investigations Report 85-4220, vi, 73 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854220.","productDescription":"vi, 73 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123319,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4220/report-thumb.jpg"},{"id":58059,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4220/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a281","contributors":{"authors":[{"text":"Presser, T. S.","contributorId":93875,"corporation":false,"usgs":true,"family":"Presser","given":"T.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":201130,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, Ivan","contributorId":56619,"corporation":false,"usgs":true,"family":"Barnes","given":"Ivan","email":"","affiliations":[],"preferred":false,"id":201129,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25972,"text":"wri854089 - 1985 - The geohydrologic system and probable effects of mining in the Sand Creek-Hanks lignite area, western Williams County, North Dakota","interactions":[],"lastModifiedDate":"2025-01-10T21:13:04.701978","indexId":"wri854089","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4089","title":"The geohydrologic system and probable effects of mining in the Sand Creek-Hanks lignite area, western Williams County, North Dakota","docAbstract":"<p>The investigation was undertaken to define the geohydrology of the Sand Creek-Hanks area and to project probable hydrologic effects of lignite mining on the area. </p><p>Aquifers occur in sandstone beds in the Fox Hills Sandstone and the Hell Creek Formation of Cretaceous age and in sandstone lenses and lignite beds in the Tongue River and Sentinel Butte Members of the Fort Union Formation of Tertiary age.</p><p>The top of the Fox Hills aquifer ranges from about 1,200 to 2,000 feet below land surface. Yields of wells completed in the aquifer could be as much as 60 gallons per minute. Water in the Fox Hills aquifer is a sodium bicarbonate type and generally</p><p>Depths to the top of the Hell Creek aquifer range from about 900 to 1,600 feet. Well yields range from less than 10 to 40 gallons per minute. Water in the aquifer is a sodium bicarbonate type and generally contains between 1,000 and 2,200 milligrams per liter dissolved solids. </p><p>Depths to aquifers in the Tongue River and Sentinel Butte Members of Fort Union Formation range from near land surface to about 1,000 feet below land surface. Wells completed in the aquifers may yield as much as 40 gallons per minute of sodium bicarbonate or a sodium sulfate type water that contains about 800 to 4,100 milligrams per liter dissolved solids.</p><p>Glacial drift covers most of the study area. The drift thickness ranges from a veneer to about 380 feet. Well yields range from a few gallons per minute to 900 gallons per minute. Dissolved-solids concentrations in water from the glacial drift generally range from 477 to 2,050 milligrams per liter. </p><p>Mining of lignite will destroy all aquifers in and above the mined lignite and will expose overburden to oxidation. Leaching will cause an increase in dissolved solids in ground water immediately beneath the mines and possibly will cause some increase in the dissolved solids in low flows in area streams.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854089","usgsCitation":"Armstrong, C.A., 1985, The geohydrologic system and probable effects of mining in the Sand Creek-Hanks lignite area, western Williams County, North Dakota: U.S. Geological Survey Water-Resources Investigations Report 85-4089, Report: v, 36 p.; 3 Plates: 15.07 × 14.51 inches or smaller, https://doi.org/10.3133/wri854089.","productDescription":"Report: v, 36 p.; 3 Plates: 15.07 × 14.51 inches or smaller","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":158268,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4089/report-thumb.jpg"},{"id":54722,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4089/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54719,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4089/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54720,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4089/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54721,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4089/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":410644,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_49201.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"North Dakota","county":"Williams County","otherGeospatial":"Sand Creek-Hanks lignite area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -103.6,\n              48\n            ],\n            [\n              -103.6,\n              48.667\n            ],\n            [\n              -104.0417,\n              48.667\n            ],\n            [\n              -104.0417,\n              48\n            ],\n            [\n              -103.6,\n              48\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65da1b","contributors":{"authors":[{"text":"Armstrong, C. A.","contributorId":66231,"corporation":false,"usgs":true,"family":"Armstrong","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":195566,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12360,"text":"ofr85415 - 1985 - Water resources activities in Louisiana district, fiscal year 1985","interactions":[],"lastModifiedDate":"2012-02-02T00:06:32","indexId":"ofr85415","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-415","title":"Water resources activities in Louisiana district, fiscal year 1985","docAbstract":"Water resources activities of the U.S. Geological Survey (USGS) in Louisiana consist of collecting water resources data and conducting interpretive hydrologic investigations and research. The water resources data and the results of the interpretive investigations are published or released by either the USGS or by cooperating agencies. The USGS water resources activities in Louisiana for the 1985 fiscal year (October 1, 1984 to September 30, 1985) are described, including data collection and dissemination, water resources appraisals (interpretive studies) and research. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85415","usgsCitation":"Herbert, R., and Ellsworth, E., 1985, Water resources activities in Louisiana district, fiscal year 1985: U.S. Geological Survey Open-File Report 85-415, iv, 64 p. :maps ;28 cm., https://doi.org/10.3133/ofr85415.","productDescription":"iv, 64 p. :maps ;28 cm.","costCenters":[],"links":[{"id":143749,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0415/report-thumb.jpg"},{"id":40596,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0415/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48d7e4b07f02db5492ba","contributors":{"authors":[{"text":"Herbert, R.A.","contributorId":59449,"corporation":false,"usgs":true,"family":"Herbert","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":166004,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ellsworth, E.A.","contributorId":88739,"corporation":false,"usgs":true,"family":"Ellsworth","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":166005,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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