{"pageNumber":"1614","pageRowStart":"40325","pageSize":"25","recordCount":68937,"records":[{"id":27135,"text":"wri944225 - 1995 - Selected characteristics of stormflow and base flow affected by land use and cover in the Chickahominy River basin, Virginia, 1989-91","interactions":[],"lastModifiedDate":"2012-02-02T00:08:25","indexId":"wri944225","displayToPublicDate":"1995-10-01T00:00:00","publicationYear":"1995","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":"94-4225","title":"Selected characteristics of stormflow and base flow affected by land use and cover in the Chickahominy River basin, Virginia, 1989-91","docAbstract":"The Chickahominy River is the principal source of raw-water supply managed by the Department of Public Utilities, City of Newport News. Selected characteristics of stormflow and base flow, and major land use and cover factors that affect the distribution, movement, and quality of water of the nontidal Chickahominy River were monitored at three continuous-record stations and two partial-record stations. The stations are located in areas that drain urban, residential, and rural land uses.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri944225","usgsCitation":"Focazio, M., and Cooper, R., 1995, Selected characteristics of stormflow and base flow affected by land use and cover in the Chickahominy River basin, Virginia, 1989-91: U.S. Geological Survey Water-Resources Investigations Report 94-4225, iv, 37 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944225.","productDescription":"iv, 37 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":157966,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4225/report-thumb.jpg"},{"id":56007,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4225/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa790","contributors":{"authors":[{"text":"Focazio, M. J.","contributorId":62997,"corporation":false,"usgs":true,"family":"Focazio","given":"M. J.","affiliations":[],"preferred":false,"id":197616,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooper, R.E.","contributorId":94700,"corporation":false,"usgs":true,"family":"Cooper","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":197617,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28614,"text":"wri944221 - 1995 - Water-quality assessment of the upper Snake River Basin, Idaho and western Wyoming — Environmental setting, 1980-92","interactions":[],"lastModifiedDate":"2021-12-16T20:48:16.613157","indexId":"wri944221","displayToPublicDate":"1995-10-01T00:00:00","publicationYear":"1995","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":"94-4221","title":"Water-quality assessment of the upper Snake River Basin, Idaho and western Wyoming — Environmental setting, 1980-92","docAbstract":"The 35,800-square-mile upper Snake River \nBasin is one of 20 areas studied as part of the \nNational Water-Quality Assessment (NAWQA) \nProgram of the U.S. Geological Survey. Objectives of NAWQA are to study ground- and \nsurface-water quality, biology, and their relations \nto land-use activities. Major land and water uses \nthat affect water quality in the basin are irrigated \nagriculture, grazing, aquaculture, food processing, \nand wastewater treatment. Data summarized in \nthis report are used in companion reports to help \ndefine the relations among land use, water use, \nwater quality, and biological conditions.\nThe upper Snake River Basin is located in \nsoutheastern Idaho and northwestern Wyoming \nand includes small parts of Nevada and Utah. Total \npopulation in the basin was about 425,000 in 1990. \nMajor urban areas are Idaho Falls, Pocatello, \nRexburg, and Twin Falls, Idaho, which make up \n10, 11,3, and 6 percent of the total population, \nrespectively. Climate in the basin is mostly \nsemiarid and mean annual precipitation ranges \nfrom 8 to more than 60 inches. The eastern Snake \nRiver Plain is the major geologic feature in the \nbasin and is delineated mostly by Quaternary and \nTertiary basalt flows. It is about 55 to 62 miles \nwide and 320 miles long and bisects the basin in a \nnortheast-southwest direction.\nThe Snake River is the dominant surface-water \nfeature and flows about 453 miles from the \nsouthern border of Yellowstone National Park in \nWyoming to King Hill, Idaho, where it leaves the \nbasin. The Snake River flows through five reservoirs that provide a total storage capacity of more \nthan 4 million acre-feet. Gravity-flow diversions\nare predominant in the upper part of the basin and \ntotaled 8.8 million.acre-feet in 1980. Pumped \ndiversions occur mainly in the lower part of the \nbasin and totaled 408,500 acre-feet in 1980.\nThe Snake River Plain aquifer is the predominant ground-water feature in the upper Snake \nRiver Basin and underlies the eastern Snake River \nPlain. The upper 500 feet of the aquifer may store \n200 to 300 million acre-feet of water. Ground-water resources that supply agricultural lands are \nsustained by recharge from surface-water irrigation, precipitation, and tributary inflow. Major \nground-water discharges are at springs and seeps \nor from ground-water pumpage for irrigation.\nWater use in the basin is dominated by irrigated agriculture, which is the largest consumptive \nwater use in the basin. Major crops in the basin \ninclude potatoes, wheat, sugar beets, hay, and \nbarley. Most irrigation needs are supplied from \nsurface-water sources through a series of canals \nand laterals. In 1990, about 2.5 million acres were \nirrigated with more than 14.2 million acre-feet of \nsurface and ground water. About 21 percent of the \nbasin is agricultural land and 50 percent is \nrangeland.\nIdaho leads the Nation in trout production \nfor commercial sale. Combined mean annual \ndischarges from 12 aquacultural facilities in the \nbasin (1985-90) were about 787,000 acre-feet. \nThese facilities are clustered in a reach of the \nSnake River between Milner Dam and King Hill \nwhere ground-water discharge is from many seeps \nand springs that provide sufficient quantities of \ngood-quality water. Other facilities that release \neffluent to the Snake River include 13 municipal \nwastewater treatment plants and 3 industrial facilities.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944221","usgsCitation":"Maupin, M.A., 1995, Water-quality assessment of the upper Snake River Basin, Idaho and western Wyoming — Environmental setting, 1980-92: U.S. Geological Survey Water-Resources Investigations Report 94-4221, iv, 35 p., https://doi.org/10.3133/wri944221.","productDescription":"iv, 35 p.","numberOfPages":"39","temporalStart":"1980-01-01","temporalEnd":"1992-12-31","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":393017,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48088.htm"},{"id":57437,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4221/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158959,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4221/report-thumb.jpg"}],"country":"United States","state":"Idaho, Wyoming","otherGeospatial":"upper Snake River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.3167,\n              41.4833\n            ],\n            [\n              -109.9167,\n              41.4833\n            ],\n            [\n              -109.9167,\n              44.6667\n            ],\n            [\n              -115.3167,\n              44.6667\n            ],\n            [\n              -115.3167,\n              41.4833\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ae32","contributors":{"authors":[{"text":"Maupin, Molly A. 0000-0002-2695-5505 mamaupin@usgs.gov","orcid":"https://orcid.org/0000-0002-2695-5505","contributorId":951,"corporation":false,"usgs":true,"family":"Maupin","given":"Molly","email":"mamaupin@usgs.gov","middleInitial":"A.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true},{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"preferred":true,"id":200119,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28586,"text":"wri944066 - 1995 - Effects of combined-sewer overflows and urban runoff on the water quality of Fall Creek, Indianapolis, Indiana","interactions":[],"lastModifiedDate":"2016-06-01T12:26:07","indexId":"wri944066","displayToPublicDate":"1995-10-01T00:00:00","publicationYear":"1995","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":"94-4066","title":"Effects of combined-sewer overflows and urban runoff on the water quality of Fall Creek, Indianapolis, Indiana","docAbstract":"<p>In 1986, the U.S. Geological Survey and the Indianapolis Department of Public Works began a study to evaluate the effects of combined-sewer overflows and urban runoff discharging to Fall Geek on the White River. This report describes the effects of combined-sewer overflows and urban runoff on the water quality of Fall Creek during summer 1987 by comparing the water quality during base flow with that during storm runoff and by comparing water quality in the urbanized area with that in the less urbanized area upstream from the combined-sewer overflows. Data were collected at three streamflow-gaging stations located upstream from, downstream from, and in the middle of 27 combined-sewer overflows on Fall Creek. The most downstream station also was immediately downstream from the discharge of filter backwash from a water-treatment plant for public supply.</p>\n<p>Specific conductance and concentrations of major ions and dissolved solids in base flow increased downstream in response to surface-water withdrawn for public supply, ground-water inflow, and the discharge of filter backwash. Concentrations of dissolved oxygen were least in the reach of Fall Creek in the middle of the combined- sewer overflows where black sludge deposits covered the stream bottom. Concentrations of nitrate plus nitrite and ammonia steadily increased downstream, whereas concentrations of organic nitrogen, phosphorus, and orthophosphate only increased at the most downstream station. Nearly all concentrations of chromium, copper, lead, nickel, and zinc at the upstream and middle stations were less than the detection limit of 10 micrograms per liter. Detectable concentrations of these metals and high concentrations of suspended solids in base-flow samples at the most downstream station were caused by the discharges from the water-treatment plant.</p>\n<p>Concentrations of dissolved oxygen measured at the station in the middle of the combined-sewer overflows were less than the Indiana minimum ambient water-quality standard of 4.0 milligrams per liter during all storms. Concentrations of ammonia, oxygen demand, copper, lead, zinc, and fecal coliform bacteria at the stations downstream from the combined-sewer overflows were much higher in storm runoff than in base flow. Increased concentrations of oxygen demand in runoff probably were caused by combined-sewer overflows, urban runoff, and the resuspension of organic material deposited on the streambed. Some of the increased concentrations of lead, zinc, and probably copper can be attributed to the discharge and resuspension of filter backwash</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/wri944066","collaboration":"Indianapolis Department of Public Works","usgsCitation":"Martin, J., 1995, Effects of combined-sewer overflows and urban runoff on the water quality of Fall Creek, Indianapolis, Indiana: U.S. Geological Survey Water-Resources Investigations Report 94-4066, vi, 92 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944066.","productDescription":"vi, 92 p. :ill., maps ;28 cm.","startPage":"1","endPage":"92","numberOfPages":"98","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":122875,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4066/report-thumb.jpg"},{"id":57414,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4066/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Indiana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.2265396118164,\n              39.742306320384046\n            ],\n            [\n              -86.2265396118164,\n              39.89946489938474\n            ],\n            [\n              -85.9518814086914,\n              39.89946489938474\n            ],\n            [\n              -85.9518814086914,\n              39.742306320384046\n            ],\n            [\n              -86.2265396118164,\n              39.742306320384046\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db684562","contributors":{"authors":[{"text":"Martin, Jeffrey D.","contributorId":40609,"corporation":false,"usgs":true,"family":"Martin","given":"Jeffrey D.","affiliations":[],"preferred":false,"id":200071,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26764,"text":"wri954012 - 1995 - A computer program (MACPUMP) for interactive aquifer-test analysis","interactions":[],"lastModifiedDate":"2019-12-07T11:17:19","indexId":"wri954012","displayToPublicDate":"1995-10-01T00:00:00","publicationYear":"1995","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":"95-4012","title":"A computer program (MACPUMP) for interactive aquifer-test analysis","docAbstract":"This report introduces MACPUMP (Version 1.0), an aquifer-test-analysis package for use with Macintosh4 computers. The report outlines the input- data format, describes the solutions encoded in the program, explains the menu-items, and offers a tutorial illustrating the use of the program. The package reads list-directed aquifer-test data from a file, plots the data to the screen, generates and plots type curves for several different test conditions, and allows mouse-controlled curve matching. MACPUMP features pull-down menus, a simple text viewer for displaying data-files, and optional on-line help windows. This version includes the analytical solutions for nonleaky and leaky confined aquifers, using both type curves and straight-line methods, and for the analysis of single-well slug tests using type curves. An executable version of the code and sample input data sets are included on an accompanying floppy disk.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri954012","usgsCitation":"Day-Lewis, F., Person, M., and Konikow, L.F., 1995, A computer program (MACPUMP) for interactive aquifer-test analysis: U.S. Geological Survey Water-Resources Investigations Report 95-4012, iv, 32 p. , https://doi.org/10.3133/wri954012.","productDescription":"iv, 32 p. ","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":366927,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4012/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158231,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4012/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b0d45","contributors":{"authors":[{"text":"Day-Lewis, F. D. 0000-0003-3526-886X","orcid":"https://orcid.org/0000-0003-3526-886X","contributorId":35773,"corporation":false,"usgs":true,"family":"Day-Lewis","given":"F. D.","affiliations":[],"preferred":false,"id":196960,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Person, M.A.","contributorId":91108,"corporation":false,"usgs":true,"family":"Person","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":196962,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Konikow, Leonard F. 0000-0002-0940-3856 lkonikow@usgs.gov","orcid":"https://orcid.org/0000-0002-0940-3856","contributorId":158,"corporation":false,"usgs":true,"family":"Konikow","given":"Leonard","email":"lkonikow@usgs.gov","middleInitial":"F.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":196961,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":31759,"text":"ofr95182 - 1995 - Water-level altitudes 1995, water-level changes 1977-95 and 1994-95, and compaction 1973-94 in the Chicot and Evangeline aquifers, Houston-Galveston region, Texas","interactions":[],"lastModifiedDate":"2016-08-15T12:55:05","indexId":"ofr95182","displayToPublicDate":"1995-10-01T00:00:00","publicationYear":"1995","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":"95-182","title":"Water-level altitudes 1995, water-level changes 1977-95 and 1994-95, and compaction 1973-94 in the Chicot and Evangeline aquifers, Houston-Galveston region, Texas","docAbstract":"<p>This report is one in an annual series of reports that depicts altitudes of water levels and water-level changes since 1977 and compaction since 1973 in the Chicot and Evangeline aquifers in the Houston-Galveston region, Texas.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95182","usgsCitation":"Kasmarek, M.C., Coplin, L., and Santos, H.X., 1995, Water-level altitudes 1995, water-level changes 1977-95 and 1994-95, and compaction 1973-94 in the Chicot and Evangeline aquifers, Houston-Galveston region, Texas: U.S. Geological Survey Open-File Report 95-182, 8 Sheets, https://doi.org/10.3133/ofr95182.","productDescription":"8 Sheets","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":160180,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":59968,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0182/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59969,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0182/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59970,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0182/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59971,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0182/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59972,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0182/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59973,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0182/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59974,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0182/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59975,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0182/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49efe4b07f02db5edb32","contributors":{"authors":[{"text":"Kasmarek, Mark C. 0000-0003-2808-2506 mckasmar@usgs.gov","orcid":"https://orcid.org/0000-0003-2808-2506","contributorId":1968,"corporation":false,"usgs":true,"family":"Kasmarek","given":"Mark","email":"mckasmar@usgs.gov","middleInitial":"C.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":206886,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coplin, L.S.","contributorId":49366,"corporation":false,"usgs":true,"family":"Coplin","given":"L.S.","affiliations":[],"preferred":false,"id":206884,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Santos, Horacio X.","contributorId":97159,"corporation":false,"usgs":true,"family":"Santos","given":"Horacio","email":"","middleInitial":"X.","affiliations":[],"preferred":false,"id":206885,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":31758,"text":"ofr95119 - 1995 - Altitude and configuration of the potentiometric surface in part of lower Providence Township, Montgomery County, Pennsylvania, May and June 1994","interactions":[],"lastModifiedDate":"2017-06-21T10:54:44","indexId":"ofr95119","displayToPublicDate":"1995-10-01T00:00:00","publicationYear":"1995","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":"95-119","title":"Altitude and configuration of the potentiometric surface in part of lower Providence Township, Montgomery County, Pennsylvania, May and June 1994","docAbstract":"A map showing ground-water levels in part of Lower Providence Township, Montgomery County, Pennsylvania, was constructed from water levels measured in 62 wells from May and June 1994. Observed water-level altitudes range from 60 feet above sea level near the Betzwood Picnic Area to 187 feet above sea level near the intersection of Egypt Road and Rittenhouse Road in Lower Providence Township.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95119","usgsCitation":"McManus, B., 1995, Altitude and configuration of the potentiometric surface in part of lower Providence Township, Montgomery County, Pennsylvania, May and June 1994: U.S. Geological Survey Open-File Report 95-119, 1 over-size sheet, scale 1:24,000 (1 inch = 2,000 feet)., https://doi.org/10.3133/ofr95119.","productDescription":"1 over-size sheet, scale 1:24,000 (1 inch = 2,000 feet).","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":19548,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0119/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160403,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686a29","contributors":{"authors":[{"text":"McManus, B. C.","contributorId":45731,"corporation":false,"usgs":true,"family":"McManus","given":"B. C.","affiliations":[],"preferred":false,"id":206883,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31760,"text":"ofr95183 - 1995 - Water-level altitudes 1995 and water-level changes 1990-95 and 1994-95 in the Chicot and Evangeline aquifers, Fort Bend County and adjacent areas, Texas","interactions":[],"lastModifiedDate":"2016-08-15T16:12:30","indexId":"ofr95183","displayToPublicDate":"1995-10-01T00:00:00","publicationYear":"1995","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":"95-183","title":"Water-level altitudes 1995 and water-level changes 1990-95 and 1994-95 in the Chicot and Evangeline aquifers, Fort Bend County and adjacent areas, Texas","docAbstract":"<p>This report is one in an annual series of reports that depicts altitudes of water levels and water-level changes since 1990 in the Chicot and Evangeline aquifers in Fort Bend Subsidence District, presents the approximate altitude of water levels (figs. 1, 4), January-February 1995, and approximate changes in water levels (figs. 2, 3, 5, 6), 1990-95 and 1994-95, in each of the aquifers. &nbsp;The most recent previously published water-level altitude maps for the aquifers are by Locke (1993), and the most recent previously published water-level change maps for the aquifers are by Coplin and Santos (1994). The earliest water-level altitude maps and the earliest water-level change maps for the Chicot aquifer are by Wesselman (1972). &nbsp;The first maps of water-level altitudes and water-level changes for the Chicot and Evangeline aquifers are by Locke (1990).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95183","usgsCitation":"Coplin, L., Kasmarek, M.C., Santos, H.X., and Noble, J.E., 1995, Water-level altitudes 1995 and water-level changes 1990-95 and 1994-95 in the Chicot and Evangeline aquifers, Fort Bend County and adjacent areas, Texas: U.S. Geological Survey Open-File Report 95-183, 6 Sheets: 21.87 x 17.32 inches or smaller, https://doi.org/10.3133/ofr95183.","productDescription":"6 Sheets: 21.87 x 17.32 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":59976,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0183/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59977,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0183/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59978,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0183/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59979,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0183/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59980,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0183/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59981,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0183/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160181,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr95183.PNG"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49efe4b07f02db5edb95","contributors":{"authors":[{"text":"Coplin, L.S.","contributorId":49366,"corporation":false,"usgs":true,"family":"Coplin","given":"L.S.","affiliations":[],"preferred":false,"id":206888,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kasmarek, Mark C. 0000-0003-2808-2506 mckasmar@usgs.gov","orcid":"https://orcid.org/0000-0003-2808-2506","contributorId":1968,"corporation":false,"usgs":true,"family":"Kasmarek","given":"Mark","email":"mckasmar@usgs.gov","middleInitial":"C.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":206890,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Santos, Horacio X.","contributorId":97159,"corporation":false,"usgs":true,"family":"Santos","given":"Horacio","email":"","middleInitial":"X.","affiliations":[],"preferred":false,"id":206889,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Noble, J. E.","contributorId":6476,"corporation":false,"usgs":true,"family":"Noble","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":206887,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":29939,"text":"wri954030 - 1995 - Geologic framework and hydrogeologic characteristics of the Edwards Aquifer recharge zone, Bexar County, Texas","interactions":[],"lastModifiedDate":"2016-08-16T14:44:15","indexId":"wri954030","displayToPublicDate":"1995-10-01T00:00:00","publicationYear":"1995","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":"95-4030","title":"Geologic framework and hydrogeologic characteristics of the Edwards Aquifer recharge zone, Bexar County, Texas","docAbstract":"<p>In Bexar County, residential and commercial development on the Edwards aquifer recharge zone is increasing. The aquifer possibly can be contaminated by spills, leakage of hazardous materials, or runoff from the rapidly developing urban areas that surround, or are built on, the intensely faulted and fractured, karstic limestone outcrops characteristic of the recharge zone. Furthermore, some of the hydrogeologic subdivisions that compose the Edwards aquifer have greater effective porosity than others. The areas where the most porous subdivisions crop out might provide efficient avenues for contaminants to enter the aquifer.</p>\n<p>The Edwards aquifer recharge zone has relatively large permeability resulting, in part, from the development or redistribution of secondary porosity. Lithology, stratigraphy, diagenesis, and karstification account for the effective porosity and permeability in the Edwards aquifer outcrop. Karst features that greatly enhance effective porosity in the outcrop area include sinkholes and caves.</p>\n<p>Hydrogeologic subdivision VI, the Kirschberg evaporite member, appears to be the most porous and permeable subdivision within the Kainer Formation. Hydrogeologic subdivision HI, the leached and collapsed members, undivided, is the most porous and permeable subdivision within the Person Formation. Hydrogeologic subdivision II, the cyclic and marine members, undivided, is moderately permeable, with both fabric- and not-fabric-selective porosity.</p>\n<p>The faults in northern Bexar County are part of the Balcones fault zone. Although most of the faults in this area trend northeast, a smaller set of cross-faults trend northwest. Generally, the faults are en echelon and normal, with the downthrown blocks typically toward the coast.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri954030","collaboration":"Prepared in cooperation with the San Antonio Water System","usgsCitation":"Stein, W., and Ozuna, G., 1995, Geologic framework and hydrogeologic characteristics of the Edwards Aquifer recharge zone, Bexar County, Texas: U.S. Geological Survey Water-Resources Investigations Report 95-4030, iii, 8 p., https://doi.org/10.3133/wri954030.","productDescription":"iii, 8 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science 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W.G.","contributorId":67931,"corporation":false,"usgs":true,"family":"Stein","given":"W.G.","email":"","affiliations":[],"preferred":false,"id":202392,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ozuna, G. B.","contributorId":25205,"corporation":false,"usgs":true,"family":"Ozuna","given":"G. B.","affiliations":[],"preferred":false,"id":202391,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28762,"text":"wri904112 - 1995 - Water withdrawals in the Black Warrior-Tombigbee basin in Alabama, 1985-87","interactions":[],"lastModifiedDate":"2022-09-19T18:44:07.844563","indexId":"wri904112","displayToPublicDate":"1995-10-01T00:00:00","publicationYear":"1995","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":"90-4112","title":"Water withdrawals in the Black Warrior-Tombigbee basin in Alabama, 1985-87","docAbstract":"Public-supply, industrial, and power generation water withdrawals were inventoried for the Black Warrior-Tombigbee basin in Alabama for 1987. A water source capacity analysis was done for each facility to assess the risk of the future water demand exceeding the capacity of the current source. Approximately 96 percent of all water withdrawn in the study area was surface water. Surface water accounted for 88 percent of withdrawals by public suppliers and 99 percent of withdrawals by self- supplied industries.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri904112","usgsCitation":"Mooty, W., 1995, Water withdrawals in the Black Warrior-Tombigbee basin in Alabama, 1985-87: U.S. Geological Survey Water-Resources Investigations Report 90-4112, v, 41 p., https://doi.org/10.3133/wri904112.","productDescription":"v, 41 p.","costCenters":[],"links":[{"id":57631,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4112/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118917,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4112/report-thumb.jpg"},{"id":406993,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47374.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alabama","otherGeospatial":"Black Warrior-Tombigbee basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.3333,\n              32.55\n            ],\n            [\n              -86.15,\n              32.55\n            ],\n            [\n              -86.15,\n              34.4333\n            ],\n            [\n              -88.3333,\n              34.4333\n            ],\n            [\n              -88.3333,\n              32.55\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ae3c","contributors":{"authors":[{"text":"Mooty, W. S.","contributorId":55837,"corporation":false,"usgs":true,"family":"Mooty","given":"W. S.","affiliations":[],"preferred":false,"id":200355,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29029,"text":"wri944212 - 1995 - Hydrogeology, ground-water quality, and source of ground water causing water-quality changes in the Davis well field at Memphis, Tennessee","interactions":[],"lastModifiedDate":"2016-02-03T09:59:08","indexId":"wri944212","displayToPublicDate":"1995-10-01T00:00:00","publicationYear":"1995","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":"94-4212","title":"Hydrogeology, ground-water quality, and source of ground water causing water-quality changes in the Davis well field at Memphis, Tennessee","docAbstract":"<p>An investigation was conducted by the U.S. Geological Survey from 1992 to 1994 to collect and interpret hydrogeologic and water-quality data to determine the source of ground water causing water-quality changes in water from wells screened in the Memphis aquifer in the Davis well field at Memphis, Tennessee. Water-quality changes in aquifers used for water supply are of concern because these changes can indicate a potential for contamination of the aquifers by downward leakage from near-surface sources.</p>\n<p>The water-quality changes at the Davis well field were detected by Memphis Light, Gas and Water Division, which has periodically sampled and analyzed water from many of the 14 production wells since the well field began operation in 1971. Memphis Light, Gas and Water Division analyzed the water samples primarily for hardness, alkalinity, chloride, ulfate, and iron. Results of the e analy es and results of more recent (1992) analyse of water samples by the U.S. Geological Survey indicate that the quality of water from eight of the production wells has changed since the well field began operation. For example, from 1972 to 1991, hardness of water from one well has increased from 90 to 292 milligrams per liter (224 percent).</p>\n<p>The confining unit, which separates the fluvial deposits aquifer from the Memphis aquifer in the area of the well field, is relatively thick and contains many clay layers. However, a test hole drilled for one of five shallow wells installed in the alluvial aquifer in the Mississippi Alluvial Plain just west of the well field indicated that the confining unit separating the alluvial aquifer from the Memphis aquifer locally is absent. Differences in hydrauLic head between the alluvial and fluvial deposits aquifers and the Memphis aquifer favor downward leakage of ground water. Thus, the absence of the confining unit beneath the Mississippi Alluvial Plain just west of the well field provides a direct pathway for water in the alluvial aquifer to enter the Memphis aquifer.</p>\n<p>Comparison of selected water-quality properties and major inorganic and trace element constituent concentrations in samples from the alluvial, fluvial deposits, and Memphis aquifers indicates that the source of ground water causing waterquality changes at the Davis well field is the alluvial aquifer west of the well field . The presence of tritium and chlorofluorocarbons in water from wells screened in the Memphis aquifer in the western part of the well field indicates that relatively young (post-1940) water from the alluvial aquifer has entered the Memphis aquifer.</p>\n<p>NETPATH geochemical model code was used to mix waters from the alluvial aquifer with water from the Memphis aquifer using chloride as a conservative tracer. The resulting models indicated that a mixture containing 3 percent alluvial aquifer water mixed with 97 percent unaffected Memphis aquifer water would produce the chloride concentration measured in water from the Memphis aquifer well most affected by water-quality changes. NETPATH also was used to calculate mixing percentages of alluvial and Memphis aquifer Abstract waters based on changes in the concentrations of selected dissolved major inorganic and trace element constituents that define the dominant reactions that occur during mixing. These models indicated that a mixture containing 18 percent alluvial aquifer water and 82 percent unaffected Memphis aquifer water would produce the major constituent and trace element concentrations measured in water from the Memphis aquifer well most affected by water-quality changes. However, these model simulations predicted higher dissolved methane concentrations than were measured in water samples from the Memphis aquifer wells.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Memphis, TN","doi":"10.3133/wri944212","collaboration":"Prepared in cooperation with the City of Memphis, Memphis Light, Gas, and Water Division, and the University of Memphis","usgsCitation":"Parks, W., Mirecki, J.E., and Kingsbury, J.A., 1995, Hydrogeology, ground-water quality, and source of ground water causing water-quality changes in the Davis well field at Memphis, Tennessee: U.S. Geological Survey Water-Resources Investigations Report 94-4212, v, 58 p., https://doi.org/10.3133/wri944212.","productDescription":"v, 58 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":316464,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4212/report.pdf"},{"id":158882,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4212/report-thumb.jpg"}],"country":"United States","state":"Tennessee","county":"Shelby County","city":"Memphis","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.1603317260742,\n              34.99597251289618\n            ],\n            [\n              -90.1603317260742,\n              35.036743220175275\n            ],\n            [\n              -90.08857727050781,\n              35.036743220175275\n            ],\n            [\n              -90.08857727050781,\n              34.99597251289618\n            ],\n            [\n              -90.1603317260742,\n              34.99597251289618\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db6842e9","contributors":{"authors":[{"text":"Parks, William S.","contributorId":25304,"corporation":false,"usgs":true,"family":"Parks","given":"William S.","affiliations":[],"preferred":false,"id":200822,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mirecki, June E.","contributorId":93577,"corporation":false,"usgs":true,"family":"Mirecki","given":"June","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":200821,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kingsbury, James A. 0000-0003-4985-275X jakingsb@usgs.gov","orcid":"https://orcid.org/0000-0003-4985-275X","contributorId":883,"corporation":false,"usgs":true,"family":"Kingsbury","given":"James","email":"jakingsb@usgs.gov","middleInitial":"A.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":581,"text":"Tennessee Water Science Center","active":true,"usgs":true},{"id":24708,"text":"Lower Mississippi-Gulf Water Science Center","active":true,"usgs":true}],"preferred":true,"id":200820,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30303,"text":"wri944194 - 1995 - Water quality of storm runoff and comparison of procedures for estimating storm-runoff loads, volume, event-mean concentrations, and the mean load for a storm for selected properties and constituents for Colorado Springs, southeastern Colorado, 1992","interactions":[],"lastModifiedDate":"2022-11-23T22:10:06.419017","indexId":"wri944194","displayToPublicDate":"1995-10-01T00:00:00","publicationYear":"1995","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":"94-4194","title":"Water quality of storm runoff and comparison of procedures for estimating storm-runoff loads, volume, event-mean concentrations, and the mean load for a storm for selected properties and constituents for Colorado Springs, southeastern Colorado, 1992","docAbstract":"The U.S. Environmental Protection Agency requires that municipalities that have a population of 100,000 or greater obtain National Pollutant Discharge Elimination System permits to characterize the quality of their storm runoff. In 1992, the U.S. Geological Survey, in cooperation with the Colorado Springs City Engineering Division, began a study to characterize the water quality of storm runoff and to evaluate procedures for the estimation of storm-runoff loads, volume and event-mean concentrations for selected properties and constituents.  Precipitation, streamflow, and water-quality data were collected during 1992 at five sites in Colorado Springs. Thirty-five samples were collected, seven at each of the five sites. At each site, three samples were collected for permitting purposes; two of the samples were collected during rainfall runoff, and one sample was collected during snowmelt runoff. Four additional samples were collected at each site to obtain a large enough sample size to estimate storm-runoff loads, volume, and event-mean concentrations for selected properties and constituents using linear-regression procedures developed using data from the Nationwide Urban Runoff Program (NURP). Storm-water samples were analyzed for as many as 186 properties and constituents. The constituents measured include total-recoverable metals, vola-tile-organic compounds, acid-base/neutral organic compounds, and pesticides.  Storm runoff sampled had large concentrations of chemical oxygen demand and 5-day biochemical oxygen demand. Chemical oxygen demand ranged from 100 to 830 milligrams per liter, and 5.-day biochemical oxygen demand ranged from 14 to 260 milligrams per liter. Total-organic carbon concentrations ranged from 18 to 240 milligrams per liter. The total-recoverable metals lead and zinc had the largest concentrations of the total-recoverable metals analyzed. Concentrations of lead ranged from 23 to 350 micrograms per liter, and concentrations of zinc ranged from 110 to 1,400 micrograms per liter.  The data for 30 storms representing rainfall runoff from 5 drainage basins were used to develop single-storm local-regression models. The response variables, storm-runoff loads, volume, and event-mean concentrations were modeled using explanatory variables for climatic, physical, and land-use characteristics. The r2 for models that use ordinary least-squares regression ranged from 0.57 to 0.86 for storm-runoff loads and volume and from 0.25 to 0.63 for storm-runoff event-mean concentrations. Except for cadmium, standard errors of estimate ranged from 43 to 115 percent for storm- runoff loads and volume and from 35 to 66 percent for storm-runoff event-mean concentrations. Eleven of the 30 concentrations collected during rainfall runoff for total-recoverable cadmium were censored (less than) concentrations. Ordinary least-squares regression should not be used with censored data; however, censored data can be included with uncensored data using tobit regression. Standard errors of estimate for storm-runoff load and event-mean concentration for total-recoverable cadmium, computed using tobit regression, are 247 and 171 percent.  Estimates from single-storm regional-regression models, developed from the Nationwide Urban Runoff Program data base, were compared with observed storm-runoff loads, volume, and event-mean concentrations determined from samples collected in the study area. Single-storm regional-regression models tended to overestimate storm-runoff loads, volume, and event-mean con-centrations. Therefore, single-storm local- and regional-regression models were combined using model-adjustment procedures to take advantage of the strengths of both models while minimizing the deficiencies of each model.  Procedures were used to develop single-stormregression equations that were adjusted using local data and estimates from single-storm regional-regression equations. Single-storm regression models developed using model- adjustment proce","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944194","usgsCitation":"Von Guerard, P., and Weiss, W.B., 1995, Water quality of storm runoff and comparison of procedures for estimating storm-runoff loads, volume, event-mean concentrations, and the mean load for a storm for selected properties and constituents for Colorado Springs, southeastern Colorado, 1992: U.S. Geological Survey Water-Resources Investigations Report 94-4194, iv, 68 p., https://doi.org/10.3133/wri944194.","productDescription":"iv, 68 p.","costCenters":[],"links":[{"id":409620,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48067.htm","linkFileType":{"id":5,"text":"html"}},{"id":59095,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4194/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159776,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4194/report-thumb.jpg"}],"country":"United States","state":"Colorado","city":"Colorado Springs","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -104.69843282718571,\n              38.88682699005443\n            ],\n            [\n              -104.93694788093742,\n              38.88682699005443\n            ],\n            [\n              -104.93694788093742,\n              38.73893775339917\n            ],\n            [\n              -104.69843282718571,\n              38.73893775339917\n            ],\n            [\n              -104.69843282718571,\n              38.88682699005443\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ae7f","contributors":{"authors":[{"text":"Von Guerard, Paul","contributorId":40620,"corporation":false,"usgs":true,"family":"Von Guerard","given":"Paul","affiliations":[],"preferred":false,"id":203020,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weiss, W. B.","contributorId":57506,"corporation":false,"usgs":true,"family":"Weiss","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":203021,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30240,"text":"wri944082 - 1995 - Geohydrology and ground-water quality of east King County, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:55","indexId":"wri944082","displayToPublicDate":"1995-10-01T00:00:00","publicationYear":"1995","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":"94-4082","title":"Geohydrology and ground-water quality of east King County, Washington","docAbstract":"East King County is a 250-square-mile area east of Seattle underlain by as much as 1,200 feet of unconsolidated deposits of glacial and nonglacial origin. A surficial geology map and 12 geohydrologic sections were constructed and used to delineate 10 geohydrologic units, 4 of which are major aquifers. Annual precipitation over the study area averages 57 inches, of which 31 inches, or 413,000 acre-feet, enter the ground-water system as recharge. Some 98,500 acre-feet of ground water is estimated to discharge to surface water bodies each year, 9,540 acre-feet is discharged through springs, and 4,270 acre-feet is withdrawn from wells. The chemical quality of the ground water in east King County is typical of that in other areas of western Washington. The median dissolved-solids concen- tration of 124 samples analyzed was 115 milligrams per liter, and 95 percent of the water samples were classified as soft or moderately hard. The median nitrate concentration was 0.07 milligrams per liter, and no widespread nitrate contamination was apparent.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-File Reports Section, [distributor],","doi":"10.3133/wri944082","usgsCitation":"Turney, G.L., Kahle, S.C., and Dion, N.P., 1995, Geohydrology and ground-water quality of east King County, Washington: U.S. Geological Survey Water-Resources Investigations Report 94-4082, v, 123 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/wri944082.","productDescription":"v, 123 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":119485,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4082/report-thumb.jpg"},{"id":59012,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4082/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59013,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4082/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59014,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4082/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59015,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4082/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59016,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4082/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59017,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4082/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8d0c","contributors":{"authors":[{"text":"Turney, G. L.","contributorId":95070,"corporation":false,"usgs":true,"family":"Turney","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":202918,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kahle, S. C.","contributorId":46992,"corporation":false,"usgs":true,"family":"Kahle","given":"S.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":202917,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dion, N. P.","contributorId":33302,"corporation":false,"usgs":true,"family":"Dion","given":"N.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":202916,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30390,"text":"wri944072 - 1995 - Subsurface recharge to the Tesuque aquifer system from selected drainage basins along the western side of the Sangre de Cristo Mountains near Santa Fe, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:09:07","indexId":"wri944072","displayToPublicDate":"1995-10-01T00:00:00","publicationYear":"1995","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":"94-4072","title":"Subsurface recharge to the Tesuque aquifer system from selected drainage basins along the western side of the Sangre de Cristo Mountains near Santa Fe, New Mexico","docAbstract":"Water budgets developed for basins of five streams draining the western side of the Sangre de Cristo Mountains in northern New Mexico indicate that subsurface inflow along the mountain front is recharging the Tesuque aquifer system of the Espanola Basin. Approximately 14,700 acre-feet of water per year, or 12.7 percent of average annual precipitation over the mountains, is calculated to leave the mountain block and enter the basin as subsurface recharge from the drainage basins of the Rio Nambe, Rio en Medio, Tesuque Creek, Little Tesuque Creek, and Santa Fe River. About 5,520 acre- feet per year, or about 12 percent of average annual precipitation, is calculated to enter from the Rio Nambe drainage basin; about 1,710 acre- feet per year, or about 15 percent of average annual precipitation, is calculated to enter from the Rio en Medio drainage basin; about 1,530 acre- feet, or about 10 percent of average annual precipi- tation, is calculated to enter from the Tesuque Creek drainage basin; about 1,790 acre-feet, or about 19 percent of average annual precipitation, is calculated to enter from the Little Tesuque Creek drainage basin; and about 4,170 acre-feet per year, or about 12 percent average annual precipitation, is calculated to enter from the Santa Fe River drainage basin. Calculated subsurface recharge values were used to define maximum fluxes permitted along the specified-flux boundary defining the mountain front of the Sangre De Cristo Mountains in a numerical computer model of the Tesuque aquifer system near Santa Fe, New Mexico.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri944072","usgsCitation":"Wasiolek, M., 1995, Subsurface recharge to the Tesuque aquifer system from selected drainage basins along the western side of the Sangre de Cristo Mountains near Santa Fe, New Mexico: U.S. Geological Survey Water-Resources Investigations Report 94-4072, vi, 57 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944072.","productDescription":"vi, 57 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":160949,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4072/report-thumb.jpg"},{"id":59166,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4072/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db6999dc","contributors":{"authors":[{"text":"Wasiolek, Maryann","contributorId":57901,"corporation":false,"usgs":true,"family":"Wasiolek","given":"Maryann","email":"","affiliations":[],"preferred":false,"id":203171,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20329,"text":"ofr95329 - 1995 - Pesticide movement in soils; a comparison of no-tillage and conventional tillage in the Beaver Creek watershed in West Tennessee","interactions":[],"lastModifiedDate":"2026-04-09T14:28:11.583442","indexId":"ofr95329","displayToPublicDate":"1995-10-01T00:00:00","publicationYear":"1995","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":"95-329","title":"Pesticide movement in soils; a comparison of no-tillage and conventional tillage in the Beaver Creek watershed in West Tennessee","docAbstract":"<p>In 1993, a study of pesticide movement and degradation in soils was intiated in the Beaver Creek watershed, which consists of about 95,000 acres and includes some of the Nation's most highly erodible soils. Resource-management agencies in this locality have recommended conservation tillage or \"no-tillage\" as a best management practices to control soil erosion. The pesticide aldicarb was selected for this study because it is both highly mobile and extremely toxic. Horizontal movement of aldicarb and its metabolites was negligible. Vertical movement of aldicarb and its metabolites was limited to the top 2.5 feet of soil. Most of the aldicarb residue (over 85 percent) remaining in the soil after 148 days was detected in the top 0.5 foot of soil. No significant differences in the movement or degradation of aldicarb and its metabolites were observed between the no-tilled and conventionally tilled fields. No-till practices did not increase the downward movement of aldicarb in the test areas. No-tillage has proven to be an effective best management practice for soil-loss reduction in many studies throughout the United States.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95329","usgsCitation":"Olsen, L., 1995, Pesticide movement in soils; a comparison of no-tillage and conventional tillage in the Beaver Creek watershed in West Tennessee: U.S. Geological Survey Open-File Report 95-329, 1 folded sheet :ill. ;22 x 36 cm. folded to 22 x 9 cm., https://doi.org/10.3133/ofr95329.","productDescription":"8 p.","costCenters":[],"links":[{"id":152550,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1135,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/ofr_95-329/index.html","linkFileType":{"id":5,"text":"html"}}],"country":"United 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,{"id":70205177,"text":"70205177 - 1995 - Carbon sequestration in an aggrading forest ecosystem in the Southeastern USA","interactions":[],"lastModifiedDate":"2019-09-19T10:20:37","indexId":"70205177","displayToPublicDate":"1995-09-30T10:18:15","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3420,"text":"Soil Science Society of America Journal","active":true,"publicationSubtype":{"id":10}},"title":"Carbon sequestration in an aggrading forest ecosystem in the Southeastern USA","docAbstract":"<p><span>An analysis of C pools at the Panola Mountain Research Watershed (PMRW) near Atlanta, GA, indicates that aggrading forests in the U.S. Southeast are an important regional C sink. The forests in this area were cut in the early 1800s and the land was cultivated until the early 1900s, when farming was abandoned and forest regeneration began. Cultivation resulted in extensive erosion, which depleted soil C pools. The rate of soil C sequestration during the 70-yr period of forest regeneration was estimated to be between 0.34 (standard error [SE] = 0.12) and 0.79 (SE = 0.19) Mg C ha</span><sup>−1</sup><span>&nbsp;yr</span><sup>−1</sup><span>. There is a large potential for continued C accumulation in the soil at PMRW based on the difference between current measured soil C pools of 82 Mg C ha</span><sup>−1</sup><span>&nbsp;at PMRW and 122 Mg C ha</span><sup>−1</sup><span>&nbsp;at the nearby “undisturbed” Fernbank Forest in Atlanta, GA. The rate of C sequestration in biomass at PMRW was 1.47 Mg C ha</span><sup>−1</sup><span>&nbsp;yr</span><sup>−1</sup><span>&nbsp;for the regeneration period, bringing the ecosystem total to between 1.81 and 2.26 Mg C ha</span><sup>−1</sup><span>&nbsp;yr</span><sup>−1</sup><span>. Carbon sequestration in temperate forest ecosystems partially mitigates the effects of increased atmospheric loading of CO</span><sub>2</sub><span>.</span></p>","language":"English","publisher":"ACSESS","doi":"10.2136/sssaj1995.03615995005900050036x","usgsCitation":"Huntington, T.G., 1995, Carbon sequestration in an aggrading forest ecosystem in the Southeastern USA: Soil Science Society of America Journal, v. 59, no. 5, p. 1459-1467, https://doi.org/10.2136/sssaj1995.03615995005900050036x.","productDescription":"9 p.","startPage":"1459","endPage":"1467","costCenters":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"links":[{"id":367213,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Georgia","city":"Atlanta","otherGeospatial":"Panola Mountain Research Watershed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.19424057006836,\n              33.60804305794581\n            ],\n            [\n              -84.19424057006836,\n              33.65149408962454\n            ],\n            [\n              -84.12694931030273,\n              33.65149408962454\n            ],\n            [\n              -84.12694931030273,\n              33.60804305794581\n            ],\n            [\n              -84.19424057006836,\n              33.60804305794581\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"59","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Huntington, Thomas G. 0000-0002-9427-3530 thunting@usgs.gov","orcid":"https://orcid.org/0000-0002-9427-3530","contributorId":117440,"corporation":false,"usgs":true,"family":"Huntington","given":"Thomas","email":"thunting@usgs.gov","middleInitial":"G.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":770225,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70205393,"text":"70205393 - 1995 - Loblolly-Shortleaf Pine:  Assessment of air pollutant loadings in Stewart and Marion Counties and their relationship to Southern Pine Beetle Infestations","interactions":[],"lastModifiedDate":"2019-09-19T10:47:47","indexId":"70205393","displayToPublicDate":"1995-09-17T10:24:24","publicationYear":"1995","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"title":"Loblolly-Shortleaf Pine:  Assessment of air pollutant loadings in Stewart and Marion Counties and their relationship to Southern Pine Beetle Infestations","docAbstract":"<p>No abstract available</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Georgia's forests: 1994 health update","largerWorkSubtype":{"id":2,"text":"State or Local Government Series"},"language":"English","publisher":"Georgia Forestry Commission","usgsCitation":"Huntington, T.G., 1995, Loblolly-Shortleaf Pine:  Assessment of air pollutant loadings in Stewart and Marion Counties and their relationship to Southern Pine Beetle Infestations, chap. <i>of</i> Georgia's forests: 1994 health update, p. 14-27.","productDescription":"14 p.","startPage":"14","endPage":"27","costCenters":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"links":[{"id":367472,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Georgia","county":"Marion County, Stewart County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -85.16876220703125,\n              31.784216884487385\n            ],\n            [\n              -84.2706298828125,\n              31.784216884487385\n            ],\n            [\n              -84.2706298828125,\n              32.57459172113418\n            ],\n            [\n              -85.16876220703125,\n              32.57459172113418\n            ],\n            [\n              -85.16876220703125,\n              31.784216884487385\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Huntington, Thomas G. 0000-0002-9427-3530 thunting@usgs.gov","orcid":"https://orcid.org/0000-0002-9427-3530","contributorId":117440,"corporation":false,"usgs":true,"family":"Huntington","given":"Thomas","email":"thunting@usgs.gov","middleInitial":"G.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":771038,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70069190,"text":"70069190 - 1995 - Soil-solution chemistry in a low-elevation spruce-fir ecosystem, Howland, Maine","interactions":[],"lastModifiedDate":"2014-01-13T15:53:09","indexId":"70069190","displayToPublicDate":"1995-09-01T15:37:39","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3728,"text":"Water, Air, & Soil Pollution","onlineIssn":"1573-2932","printIssn":"0049-6979","active":true,"publicationSubtype":{"id":10}},"title":"Soil-solution chemistry in a low-elevation spruce-fir ecosystem, Howland, Maine","docAbstract":"Soil solutions were collected monthly by tension and zero-tension lysimeters in a low-elevation red spruce stand in east-central Maine from May 1987 through December 1992. Soil solutions collected by Oa tension lysimeters had higher concentrations of most constituents than the Oa zero-tension lysimeters. In Oa horizon soil solutions growing season concentrations for SO<sub>4</sub>, Ca, and Mg averaged 57, 43, and 30 μmol L<sup>−1</sup> in tension lysimeters, and 43, 28, and 19 μmol L<sup>−1</sup> in zero-tension lysimeters, respectively. Because tension lysimeters remove water held by the soil at tensions up to 10 kPa, solutions are assumed to have more time to react with the soil compared to freely draining solutions collected by zero-tension lysimeters. Solutions collected in the Bs horizon by both types of collectors were similar which was attributed to the frequency of time periods when the water table was above the Bs lysimeters. Concentrations of SO<sub>4</sub> and NO<sub>3</sub> at this site were lower than concentrations reported for most other eastern U.S. spruce-fir sites, but base cation concentrations fell in the same range. Aluminum concentrations in this study were also lower than reported for other sites in the eastern U.S. and Ca/Al ratios did not suggest inhibition of Ca uptake by roots. Concentrations of SO<sub>4</sub>, Ca, K, and Cl decreased significantly in both the Oa and Bs horizons over the 56-month sampling period, which could reflect decreasing deposition rates for sulfur and base cations, climatic influences, or natural variation. A longer record of measured fluxes will be needed to adequately define temporal trends in solution chemistry and their causes.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Water, Air, and Soil Pollution","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Kluwer Academic Publishers","doi":"10.1007/BF00479593","usgsCitation":"Fernandez, I.J., Lawrence, G.B., and Son, Y., 1995, Soil-solution chemistry in a low-elevation spruce-fir ecosystem, Howland, Maine: Water, Air, & Soil Pollution, v. 84, no. 1-2, p. 129-145, https://doi.org/10.1007/BF00479593.","productDescription":"17 p.","startPage":"129","endPage":"145","numberOfPages":"17","costCenters":[],"links":[{"id":280925,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":280922,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00479593"}],"country":"United States","state":"Maine","city":"Howland","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -68.8055,45.0946 ], [ -68.8055,45.3553 ], [ -68.5152,45.3553 ], [ -68.5152,45.0946 ], [ -68.8055,45.0946 ] ] ] } } ] }","volume":"84","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd7332e4b0b29085108c99","contributors":{"authors":[{"text":"Fernandez, Ivan J.","contributorId":80174,"corporation":false,"usgs":true,"family":"Fernandez","given":"Ivan","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":488234,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lawrence, Gregory B. 0000-0002-8035-2350 glawrenc@usgs.gov","orcid":"https://orcid.org/0000-0002-8035-2350","contributorId":867,"corporation":false,"usgs":true,"family":"Lawrence","given":"Gregory","email":"glawrenc@usgs.gov","middleInitial":"B.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":488232,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Son, Yowhan","contributorId":47287,"corporation":false,"usgs":true,"family":"Son","given":"Yowhan","email":"","affiliations":[],"preferred":false,"id":488233,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70169119,"text":"70169119 - 1995 - Herbicides and metabolites in surface and ground water in the midwestern United States","interactions":[],"lastModifiedDate":"2016-03-21T08:58:36","indexId":"70169119","displayToPublicDate":"1995-09-01T10:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Herbicides and metabolites in surface and ground water in the midwestern United States","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of 209th Chemical Society Meeting","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"209th Chemical Society Meeting","conferenceDate":"April 2-7, 1995","conferenceLocation":"Anaheim, CA","language":"English","publisher":"Chemical Society","usgsCitation":"Goolsby, D.A., Thurman, E., Kolpin, D., and Meyer, M.T., 1995, Herbicides and metabolites in surface and ground water in the midwestern United States, <i>in</i> Proceedings of 209th Chemical Society Meeting, v. 35, no. 1, Anaheim, CA, April 2-7, 1995.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":319045,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","volume":"35","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f11b57e4b0f59b85ddc436","contributors":{"authors":[{"text":"Goolsby, D. A.","contributorId":50508,"corporation":false,"usgs":true,"family":"Goolsby","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":623062,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thurman, E.M.","contributorId":102864,"corporation":false,"usgs":true,"family":"Thurman","given":"E.M.","affiliations":[],"preferred":false,"id":623063,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kolpin, D.W.","contributorId":87565,"corporation":false,"usgs":true,"family":"Kolpin","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":623064,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Meyer, M. T.","contributorId":92279,"corporation":false,"usgs":true,"family":"Meyer","given":"M.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":623065,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":20267,"text":"ofr95153 - 1995 - Records of wells and chemical analyses of ground water in Charles Mix and Douglas counties, South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:07:40","indexId":"ofr95153","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1995","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":"95-153","title":"Records of wells and chemical analyses of ground water in Charles Mix and Douglas counties, South Dakota","docAbstract":"The U.S. Geological Survey, in cooperation with the South Dakota Department of Environmental and Natural Resources, maintains a data base of information on water resources in the State of South Dakota. The ground-water site data for Charles Mix and Douglas Counties are presented in two tables, with the data organized by county and location. The chemical data for ground-water sites also are located in a table organized by geologic unit and location.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95153","usgsCitation":"Neitzert, K.M., 1995, Records of wells and chemical analyses of ground water in Charles Mix and Douglas counties, South Dakota: U.S. Geological Survey Open-File Report 95-153, iii, 129 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr95153.","productDescription":"iii, 129 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":152283,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0153/report-thumb.jpg"},{"id":49802,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0153/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b695","contributors":{"authors":[{"text":"Neitzert, Kathleen M. kmneitze@usgs.gov","contributorId":1833,"corporation":false,"usgs":true,"family":"Neitzert","given":"Kathleen","email":"kmneitze@usgs.gov","middleInitial":"M.","affiliations":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":182355,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18748,"text":"ofr95286 - 1995 - Effects of two contrasting agricultural land uses on shallow groundwater quality in the San Joaquin Valley, California; design and preliminary interpretation","interactions":[],"lastModifiedDate":"2021-01-27T17:23:33.088008","indexId":"ofr95286","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1995","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":"95-286","title":"Effects of two contrasting agricultural land uses on shallow groundwater quality in the San Joaquin Valley, California; design and preliminary interpretation","docAbstract":"<p>From 1992 through 1994, the San Joaquin-Tulare Basins Study team of the USGS National Water Quality Assessment program investigated the occurrence and distribution of water quality constituents in shallow groundwater underlying two areas of different agricultural land uses: almond orchards and vineyards. The study was restricted to the alluvial fans of the eastern San Joaquin Valley, the area of most groundwater use in the valley. A geographic information system (GIS) was used to delineate the distribution of the two target land uses, to evaluate ancillary data, and to select candidate wells that fit prescribed criteria. Twenty domestic water supply wells were sampled in each of the two areas. In addition, pairs of observation wells were installed and sampled at five of the sites in each area to evaluate whether the water quality in the domestic wells reflects that of the shallow groundwater underlying the target land use. A preliminary evaluation of the results shows that nitrate concentrations in the shallow groundwater are significantly higher in the almond orchard areas than in the vineyard area (p=0.005). In contrast, concentrations of 1,2-dibromo-3-chloropropane (DBCP) were higher in the vineyard area than in the almond orchard area (p=0.032). The most frequently detected pesticides in groundwater underlying both areas were simazine, atrazine, and desethylatrazine (an atrazine degradation product). These observations are explained, in part, by differences in chemical application and hydrogeologic factors.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr95286","usgsCitation":"Dubrovsky, N., Burow, K.R., and Gronberg, J., 1995, Effects of two contrasting agricultural land uses on shallow groundwater quality in the San Joaquin Valley, California; design and preliminary interpretation: U.S. Geological Survey Open-File Report 95-286, v, 8 p., https://doi.org/10.3133/ofr95286.","productDescription":"v, 8 p.","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":150975,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0286/report-thumb.jpg"},{"id":382691,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0286/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"San Joaquin Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.70678710937499,\n              34.79576153473033\n            ],\n            [\n              -117.05932617187499,\n              34.79576153473033\n            ],\n            [\n              -117.05932617187499,\n              37.54457732085582\n            ],\n            [\n              -120.70678710937499,\n              37.54457732085582\n            ],\n            [\n              -120.70678710937499,\n              34.79576153473033\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db610028","contributors":{"authors":[{"text":"Dubrovsky, N. M.","contributorId":48199,"corporation":false,"usgs":true,"family":"Dubrovsky","given":"N. M.","affiliations":[],"preferred":false,"id":179670,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burow, Karen R. 0000-0001-6006-6667 krburow@usgs.gov","orcid":"https://orcid.org/0000-0001-6006-6667","contributorId":1504,"corporation":false,"usgs":true,"family":"Burow","given":"Karen","email":"krburow@usgs.gov","middleInitial":"R.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":179668,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gronberg, Jo Ann M.","contributorId":18342,"corporation":false,"usgs":true,"family":"Gronberg","given":"Jo Ann M.","affiliations":[],"preferred":false,"id":179669,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":20772,"text":"ofr94317 - 1995 - Selected hydrologic data from Fortymile Wash in the Yucca Mountain area, Nevada, water year 1992","interactions":[],"lastModifiedDate":"2012-02-02T00:07:35","indexId":"ofr94317","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1995","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":"94-317","title":"Selected hydrologic data from Fortymile Wash in the Yucca Mountain area, Nevada, water year 1992","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94317","usgsCitation":"Savard, C.S., 1995, Selected hydrologic data from Fortymile Wash in the Yucca Mountain area, Nevada, water year 1992: U.S. Geological Survey Open-File Report 94-317, iv, 38 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr94317.","productDescription":"iv, 38 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":152513,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0317/report-thumb.jpg"},{"id":50322,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0317/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8c41","contributors":{"authors":[{"text":"Savard, Charles S. cssavard@usgs.gov","contributorId":3538,"corporation":false,"usgs":true,"family":"Savard","given":"Charles","email":"cssavard@usgs.gov","middleInitial":"S.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":183225,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20560,"text":"ofr94514 - 1995 - Using chloride and chlorine-36 as soil-water tracers to estimate deep percolation at selected locations on the U.S. Department of Energy Hanford site, Washington","interactions":[],"lastModifiedDate":"2020-10-08T16:50:11.069117","indexId":"ofr94514","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1995","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":"94-514","title":"Using chloride and chlorine-36 as soil-water tracers to estimate deep percolation at selected locations on the U.S. Department of Energy Hanford site, Washington","docAbstract":"Long-term average deep-percolation rates of water from precipitation on the U.S. Department of Energy Hanford Site in semiarid south-central Washington, as estimated by a chloride mass-balance method, range from 0.008 to 0.30 mm/yr (millimeters per year) at nine locations covered by a variety of fine-grain soils and vegetated with sagebrush and other deep-rooted plants plus sparse shallow-rooted grasses. Deep-percolation rates estimated using a chlorine-36 bomb-pulse method at three of the nine locations range from 2.1 to 3.4 mm/yr. Because the mass-balance method may underestimate percolation rates and the bomb-pulse method probably overestimates percolation rates, estimates by the two methods probably bracket actual rates. These estimates, as well as estimates by previous investigators who used different methods, are a small fraction of mean annual precipitation, which ranges from about 160 to 210 mm/yr at the different test locations. Estimates by the mass-balance method at four locations in an area that is vegetated only with sparse shallow-rooted grasses range from 0.39 to 2.0 mm/yr. Chlorine-36 data at one location in this area were sufficient only to determine that the upper limit of deep percolation is more than 5.1 mm/yr. Although estimates for locations in this area are larger than the estimates for locations with deep-rooted plants, they are at the lower end of the range of estimates for this area made by previous investigators.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr94514","usgsCitation":"Prych, E.A., 1995, Using chloride and chlorine-36 as soil-water tracers to estimate deep percolation at selected locations on the U.S. Department of Energy Hanford site, Washington: U.S. Geological Survey Open-File Report 94-514, viii, 125 p., https://doi.org/10.3133/ofr94514.","productDescription":"viii, 125 p.","costCenters":[],"links":[{"id":152768,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0514/report-thumb.jpg"},{"id":379242,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0514/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.28319931030273,\n              46.35699885440808\n            ],\n            [\n              -119.26620483398438,\n              46.35699885440808\n            ],\n            [\n              -119.26620483398438,\n              46.37547772047758\n            ],\n            [\n              -119.28319931030273,\n              46.37547772047758\n            ],\n            [\n              -119.28319931030273,\n              46.35699885440808\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d4e4b07f02db5dd0da","contributors":{"authors":[{"text":"Prych, Edmund A.","contributorId":38139,"corporation":false,"usgs":true,"family":"Prych","given":"Edmund","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":182843,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":17837,"text":"ofr95126 - 1995 - Water-related scientific activities of the U.S. Geological Survey in Nevada, fiscal years 1993-94","interactions":[],"lastModifiedDate":"2012-02-02T00:07:13","indexId":"ofr95126","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1995","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":"95-126","title":"Water-related scientific activities of the U.S. Geological Survey in Nevada, fiscal years 1993-94","docAbstract":"The U.S. Geological Survey has been collecting water-resources data in Nevada since 1890. Most of the projects that constitute the current Nevada District program can be classified as either basic- data acquisition (about 25 percent) or hydrologic interpretation (about 75 percent). About 39 percent of the activities are supported by cooperative agreements with State and local agencies. Technical projects supported by other Federal agencies make up about 32 percent of the program, and the re- maining 29 percent consists of USGS data collection, interpretive projects, and research. Water con- ditions in most of Nevada during fiscal years 1993 and 1994 continued to be dry, a continuation of drought conditions since late 1986. The major water-resource issues in Nevada include: water allocation in the Truckee River and Carson River Basins; water-supply needs of Las Vegas and the Reno/Sparks area, including water-importation plans; hydrologic effects of weapons testing at the Nevada Test Site; assessment of potential long-term effects of the proposed Yucca Mountain Nuclear Waste Repository; and drought. Future water-resources issues in Nevada are likely to center on water supply for, and environmental effects of, the rapidly growing population centers at Las Vegas, Reno, and Elko; impacts of operations at the Nevada Test Site; management of interstate rivers such as the Truckee, Carson, Walker, and Colorado Rivers; hydrologic and environmental impacts at heavily mined areas; and water-quality management in the Lake Tahoe Basin.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-file Reports Section [distributor],","doi":"10.3133/ofr95126","usgsCitation":"Foglesong, M.T., 1995, Water-related scientific activities of the U.S. Geological Survey in Nevada, fiscal years 1993-94: U.S. Geological Survey Open-File Report 95-126, vii, 69 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr95126.","productDescription":"vii, 69 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":149512,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0126/report-thumb.jpg"},{"id":47075,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0126/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa04a","contributors":{"authors":[{"text":"Foglesong, M. Teresa (compiler)","contributorId":55451,"corporation":false,"usgs":true,"family":"Foglesong","given":"M.","suffix":"(compiler)","email":"","middleInitial":"Teresa","affiliations":[],"preferred":false,"id":178054,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":17235,"text":"ofr95143 - 1995 - Hydrogeologic data for the northern Rocky Mountains intermontane basins, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:07:15","indexId":"ofr95143","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1995","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":"95-143","title":"Hydrogeologic data for the northern Rocky Mountains intermontane basins, Montana","docAbstract":"The U.S. Geological Survey began a Regional Aquifer- System Analysis of the Northern Rocky Mountains Intermontane Basins of western Montana and central and central and northern Idaho in 1990 to establish a regional framework of information for aquifers in 54 intermontane basins in an area of about 77,500 square miles. Selected hydrogeologic data have been used as part of this analysis to define the hydro- logic systems. Records of 1,376 wells completed in 31 of the 34 intermontane basins in the Montana part of the study area are tabulated in this report. Data consist of location, alttiude of land surface, date well constructed, geologic unit, depth of well, diameter of casing, type of finish, top of open interval, primary use of water, water level, date water level measured, discharge, specific capacity, source of discharge data, type of log available, date water-quality parameters measured, specific conductance, pH, and temperature. Hydrographs for selected wells also are included. Locations of wells and basins are shown on the accompanying plate.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr95143","usgsCitation":"Dutton, D., Lawlor, S.M., Briar, D., and Tresch, R., 1995, Hydrogeologic data for the northern Rocky Mountains intermontane basins, Montana: U.S. Geological Survey Open-File Report 95-143, iv, 94 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr95143.","productDescription":"iv, 94 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":149311,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0143/report-thumb.jpg"},{"id":46384,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0143/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4fe4b07f02db628a0a","contributors":{"authors":[{"text":"Dutton, DeAnn M. ddutton@usgs.gov","contributorId":20762,"corporation":false,"usgs":true,"family":"Dutton","given":"DeAnn M.","email":"ddutton@usgs.gov","affiliations":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"preferred":false,"id":175539,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lawlor, Sean M. 0000-0001-5988-7548 slawlor@usgs.gov","orcid":"https://orcid.org/0000-0001-5988-7548","contributorId":1895,"corporation":false,"usgs":true,"family":"Lawlor","given":"Sean","email":"slawlor@usgs.gov","middleInitial":"M.","affiliations":[{"id":685,"text":"Wyoming-Montana Water Science Center","active":false,"usgs":true}],"preferred":true,"id":175538,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Briar, D.W.","contributorId":58287,"corporation":false,"usgs":true,"family":"Briar","given":"D.W.","affiliations":[],"preferred":false,"id":175541,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tresch, R.E.","contributorId":30646,"corporation":false,"usgs":true,"family":"Tresch","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":175540,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":17853,"text":"ofr95138 - 1995 - Water-resources activities in Utah by the U.S. Geological Survey, October 1, 1992, to September 30, 1993","interactions":[],"lastModifiedDate":"2017-08-31T13:37:39","indexId":"ofr95138","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1995","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":"95-138","title":"Water-resources activities in Utah by the U.S. Geological Survey, October 1, 1992, to September 30, 1993","docAbstract":"This report contains summaries of the progress of water-resources studies in Utah by the U.S. Geological Survey (USGS), Water Resources Division, Utah District, from October 1, 1992, to September 30, 1993. The program in Utah during this period consisted of 21 projects; a discussion of each project is presented in the main body of the report. The USGS was established by an act of Congress on March 3, 1879, to provide a permanent Federal agency to conduct the systematic and scientific classifi- cation of the public lands, and examination of the geologic structure, mineral resources, and products of national domain. An integral part of that original mission includes publishing and dissemi- nating the earth-science information needed to understand, to plan the use of, and to manage the Nation's energy, land, mineral, and water resources.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr95138","usgsCitation":"1995, Water-resources activities in Utah by the U.S. Geological Survey, October 1, 1992, to September 30, 1993: U.S. Geological Survey Open-File Report 95-138, vi, 37 p., https://doi.org/10.3133/ofr95138.","productDescription":"vi, 37 p.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":149930,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0138/report-thumb.jpg"},{"id":47091,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0138/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4dfa","contributors":{"compilers":[{"text":"Hardy, Ellen E.","contributorId":79122,"corporation":false,"usgs":true,"family":"Hardy","given":"Ellen","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":709175,"contributorType":{"id":3,"text":"Compilers"},"rank":1},{"text":"Dragos, Stefanie L.","contributorId":107301,"corporation":false,"usgs":true,"family":"Dragos","given":"Stefanie","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":709176,"contributorType":{"id":3,"text":"Compilers"},"rank":2}]}}
]}