{"pageNumber":"1883","pageRowStart":"47050","pageSize":"25","recordCount":68927,"records":[{"id":13697,"text":"ofr87700 - 1988 - Water-quality and sediment-chemistry data of drain water and evaporation ponds from Tulare Lake Drainage District, Kings County, California March 1985 to March 1986","interactions":[],"lastModifiedDate":"2012-02-02T00:06:57","indexId":"ofr87700","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-700","title":"Water-quality and sediment-chemistry data of drain water and evaporation ponds from Tulare Lake Drainage District, Kings County, California March 1985 to March 1986","docAbstract":"Trace element and major ion concentrations were measured in water samples collected monthly between March 1985 and March 1986 at the MD-1 pumping station at the Tulare Lake Drainage District evaporation ponds, Kings County, California. Samples were analyzed for selected pesticides several times during the year. Salinity, as measured by specific conductance, ranged from 11,500 to 37,600 microsiemens/centimeter; total recoverable boron ranged from 4,000 to 16,000 micrg/L; and total recoverable molybdenum ranged from 630 to 2,600 microg/L. Median concentrations of total arsenic and total selenium were 97 and 2 microg/L. Atrazine, prometone, propazine, and simazine were the only pesticides detected in water samples collected at the MD-1 pumping station. Major ions, trace elements, and selected pesticides also were analyzed in water and bottom-sediment samples from five of the southern evaporation ponds at Tulare Lake Drainage District. Water enters the ponds from the MD-1 pumping station at pond 1 and flows through the system terminating at pond 10. The water samples increased in specific conductance (21,700 to 90,200 microsiemens/centimeter) and concentrations of total arsenic (110 to 420 microg/L), total recoverable boron (12,000 to 80,000 microg/L) and total recoverable molybdenum (1,200 to 5,500 microg/L) going from pond 1 to pond 10, respectively. Pesticides were not detected in water from any of the ponds sampled. Median concentrations of total arsenic and total selenium in the bottom sediments were 4.0 and 0.9 microg/g, respectively. The only pesticides detected in bottom sediment samples from the evaporation ponds were DDD and DDE, with maximum concentration of 0.8 microg/kilogram. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87700","usgsCitation":"Fujii, R., 1988, Water-quality and sediment-chemistry data of drain water and evaporation ponds from Tulare Lake Drainage District, Kings County, California March 1985 to March 1986: U.S. Geological Survey Open-File Report 87-700, iv, 19 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr87700.","productDescription":"iv, 19 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":146818,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0700/report-thumb.jpg"},{"id":42251,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0700/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cde4b07f02db544bc9","contributors":{"authors":[{"text":"Fujii, Roger rfujii@usgs.gov","contributorId":553,"corporation":false,"usgs":true,"family":"Fujii","given":"Roger","email":"rfujii@usgs.gov","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":168252,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16302,"text":"ofr88466 - 1988 - Inventory of interbasin water transfers in Minnesota","interactions":[],"lastModifiedDate":"2018-04-02T11:47:01","indexId":"ofr88466","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"88-466","title":"Inventory of interbasin water transfers in Minnesota","docAbstract":"<p>Water transfer data were collected by the U.S. Geological Survey , in cooperation with the Minnesota Department of Natural Resources, from the 13 hydrologic subregions in Minnesota. About 30,000 acre-ft of water is exported annually from eight of these subregions. Interbasin transfer of water is classified according to type of water conveyance in Minnesota. This information is needed by water-system managers and planners to develop water budgets for major river basins, to examine the extent of existing interbasin transfers, and to evaluate the feasibility of transferring water to meet regional water demands.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr88466","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources","usgsCitation":"Trotta, L.C., 1988, Inventory of interbasin water transfers in Minnesota: U.S. Geological Survey Open-File Report 88-466, iii, 15 p., https://doi.org/10.3133/ofr88466.","productDescription":"iii, 15 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":45232,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0466/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148739,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0466/report-thumb.jpg"}],"country":"United 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,{"id":16301,"text":"ofr8740 - 1988 - Aggregation of Minnesota water-use data and transfer of data to the National Water-Use Data System; Procedures and programs","interactions":[],"lastModifiedDate":"2018-04-02T11:46:34","indexId":"ofr8740","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-40","title":"Aggregation of Minnesota water-use data and transfer of data to the National Water-Use Data System; Procedures and programs","docAbstract":"<p>The Minnesota Water-Use Data System stores data on the quantity of withdrawals and discharge in Minnesota. To transfer these data into the U.S. Geological Survey 's National Water-Use Data System properly, certain procedures must be followed. Uniform data categorization and entry allows comparison of water use from State to State. The data in the National Water-Use Data System are aggregated by county and by watershed (hydrologic unit). This report documents the data aggregation and transfer process as developed by the Minnesota Department of Natural Resources, the Minnesota State Planning Agency/Planning Information Center, and the U.S. Geological Survey as part of the National Water-Use Information Program.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr8740","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources and the Minnesota State Planning Agency","usgsCitation":"Trotta, L.C., 1988, Aggregation of Minnesota water-use data and transfer of data to the National Water-Use Data System; Procedures and programs: U.S. Geological Survey Open-File Report 87-40, iv, 71 p., https://doi.org/10.3133/ofr8740.","productDescription":"iv, 71 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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,{"id":13678,"text":"ofr88346 - 1988 - National Research Program of the Water Resources Division, U.S. Geological Survey, fiscal year 1987","interactions":[],"lastModifiedDate":"2018-11-08T10:20:22","indexId":"ofr88346","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"88-346","title":"National Research Program of the Water Resources Division, U.S. Geological Survey, fiscal year 1987","docAbstract":"<p>The National Research Program (NRP) of the U.S. Geological Survey's Water Resources Division (WRD) had its beginnings in the late 1950's when \"core research\" was added as a line item to the Congressional budget. Since that time, the NRP has grown to encompass a broad spectrum of scientific investigations. The sciences of hydrology, mathematics, chemistry, physics, biology, geology, and engineering are used to gain a fundamental understanding of the processes that affect the availability, movement, and quality of the Nation's water resources. The knowledge gained and methods developed have great value to WRD's operational program. Results of the investigations conducted by the NRP are applicable not only to the solution of current water problems, but also to future issues, anticipated or unanticipated, that may affect the Nation's water resources.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr88346","usgsCitation":"1988, National Research Program of the Water Resources Division, U.S. Geological Survey, fiscal year 1987: U.S. Geological Survey Open-File Report 88-346, iii, 231 p., https://doi.org/10.3133/ofr88346.","productDescription":"iii, 231 p.","costCenters":[],"links":[{"id":147560,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0346/report-thumb.jpg"},{"id":359315,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0346/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698769","contributors":{"compilers":[{"text":"Friedman, Linda C.","contributorId":98702,"corporation":false,"usgs":true,"family":"Friedman","given":"Linda C.","affiliations":[],"preferred":false,"id":725472,"contributorType":{"id":3,"text":"Compilers"},"rank":1},{"text":"Donato, Christine N.","contributorId":43791,"corporation":false,"usgs":true,"family":"Donato","given":"Christine","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":725473,"contributorType":{"id":3,"text":"Compilers"},"rank":2}]}}
,{"id":13669,"text":"ofr88475 - 1988 - Models, data available, and data requirements for estimating the effects of injecting saltwater into disposal wells in the greater Altamont-Bluebell oil and gas field, northern Uinta Basin, Utah","interactions":[],"lastModifiedDate":"2017-08-31T16:05:21","indexId":"ofr88475","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"88-475","title":"Models, data available, and data requirements for estimating the effects of injecting saltwater into disposal wells in the greater Altamont-Bluebell oil and gas field, northern Uinta Basin, Utah","docAbstract":"<p>Permits for disposing of salty oil-production water have been issued for 19 wells in the Greater Altamont-Bluebell field. During 1986 more than 500 million gallons of production water were injected into the Duchesne River, Uinta, and Green River Formations through 18 of these wells. The physical and chemical effects of injecting this water into aquifers containing potable water are poorly understood. Interfingering and the structural configuration of these formations add complexity to the description of the geometry and hydrogeology of the ground-water system.</p><p>A preliminary assessment of the problem indicates that numerical modeling may offer a method of determining the effects of injection. Modeling possibilities include variable-density, three-dimensional flow, sectionaltransport, and areal-transport models. Data needed to develop these models can be derived from a synthesis of geologic, hydrologic, and hydrochemical data already available in the files of State and Federal agencies, oil companies, and private companies. Results from each modeling phase would contribute information for implementing the following phase. The result will be a better understanding of how water moves naturally through the groundwater system, the extent of alterations of both vertical and horizontal flow near the disposal wells, and an overall concept of the effects of deep injection on near-surface aquifers. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr88475","collaboration":"Prepared in cooperation with the Utah Division of Oil, Gas, And Mining","usgsCitation":"Freethey, G.W., 1988, Models, data available, and data requirements for estimating the effects of injecting saltwater into disposal wells in the greater Altamont-Bluebell oil and gas field, northern Uinta Basin, Utah: U.S. Geological Survey Open-File Report 88-475, iv, 30 p., https://doi.org/10.3133/ofr88475.","productDescription":"iv, 30 p.","numberOfPages":"34","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":42220,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0475/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147794,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0475/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Altamont-Bluebell oil and gas field, Uinta Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db6996ba","contributors":{"authors":[{"text":"Freethey, Geoffrey W.","contributorId":25570,"corporation":false,"usgs":true,"family":"Freethey","given":"Geoffrey","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":168204,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12646,"text":"ofr87573 - 1988 - Character and evolution of the ground-water flow system in the central part of the western San Joaquin Valley, California","interactions":[{"subject":{"id":12646,"text":"ofr87573 - 1988 - Character and evolution of the ground-water flow system in the central part of the western San Joaquin Valley, California","indexId":"ofr87573","publicationYear":"1988","noYear":false,"title":"Character and evolution of the ground-water flow system in the central part of the western San Joaquin Valley, California"},"predicate":"SUPERSEDED_BY","object":{"id":1007,"text":"wsp2348 - 1990 - Character and evolution of the ground-water flow system in the central part of the western San Joaquin Valley, California","indexId":"wsp2348","publicationYear":"1990","noYear":false,"title":"Character and evolution of the ground-water flow system in the central part of the western San Joaquin Valley, California"},"id":1}],"supersededBy":{"id":1007,"text":"wsp2348 - 1990 - Character and evolution of the ground-water flow system in the central part of the western San Joaquin Valley, California","indexId":"wsp2348","publicationYear":"1990","noYear":false,"title":"Character and evolution of the ground-water flow system in the central part of the western San Joaquin Valley, California"},"lastModifiedDate":"2019-03-08T12:24:51","indexId":"ofr87573","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-573","title":"Character and evolution of the ground-water flow system in the central part of the western San Joaquin Valley, California","docAbstract":"<p>The occurrence of selenium in agricultural drain water derived from the western San Joaquin Valley, California, has focused concern on the ground-water flow system of the western valley. In this investigation, previous work and recently collected texture and water-level data are used to evaluate the character and evolution of the regional ground-water flow system in the central part of the western valley, with particular emphasis on the deposits overlying the Corcoran Clay Member of the Tulare Formation.</p><p>The Corcoran Clay Member, where present, divides the flow system into an upper semiconfined zone and a lower con-fined zone. Above the Corcoran, three hydrogeologic units can be recognized: Coast Range alluvium, Sierran sand, and flood-basin deposits. These units differ in texture, hydrologic properties, and oxidation state.</p><p>The development of irrigated agriculture in the central part of the western valley has significantly altered the flow system. Percolation of irrigation water past crop roots has caused a rise in the altitude of the water table in midfan and distal-fan areas. Pumpage of ground water from wells has caused a lowering of the water table beneath parts of the fanheads and a lowering of the potentiometric surface of the confined zone over much of the western valley. The combination of percolation and pumpage has resulted in development of a large downward hydraulic head gradient in the semi-confined zone and has created a groundwater divide along the western margin of the valley. Surface-water deliveries from the California Aqueduct have allowed a decrease in pumpage and a consequent recovery in hydraulic head throughout the system.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87573","usgsCitation":"Belitz, K., 1988, Character and evolution of the ground-water flow system in the central part of the western San Joaquin Valley, California: U.S. Geological Survey Open-File Report 87-573, iv, 34 p., https://doi.org/10.3133/ofr87573.","productDescription":"iv, 34 p.","costCenters":[],"links":[{"id":361896,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0573/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143778,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0573/report-thumb.jpg"}],"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              -120.75,\n              36\n            ],\n            [\n              -119.75,\n              36\n            ],\n            [\n              -119.75,\n              37\n            ],\n            [\n              -120.75,\n              37\n            ],\n            [\n              -120.75,\n              36\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e5546","contributors":{"authors":[{"text":"Belitz, Kenneth 0000-0003-4481-2345 kbelitz@usgs.gov","orcid":"https://orcid.org/0000-0003-4481-2345","contributorId":442,"corporation":false,"usgs":true,"family":"Belitz","given":"Kenneth","email":"kbelitz@usgs.gov","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":166476,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19479,"text":"ofr88704 - 1988 - Ground-water data for Michigan 1987","interactions":[],"lastModifiedDate":"2012-02-02T00:07:29","indexId":"ofr88704","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"88-704","title":"Ground-water data for Michigan 1987","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88704","usgsCitation":"Huffman, G., and Whited, C., 1988, Ground-water data for Michigan 1987: U.S. Geological Survey Open-File Report 88-704, v, 56 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr88704.","productDescription":"v, 56 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":151859,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0704/report-thumb.jpg"},{"id":48949,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0704/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cf80","contributors":{"authors":[{"text":"Huffman, G.C.","contributorId":44150,"corporation":false,"usgs":true,"family":"Huffman","given":"G.C.","email":"","affiliations":[],"preferred":false,"id":180980,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Whited, C.R.","contributorId":49387,"corporation":false,"usgs":true,"family":"Whited","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":180981,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":12667,"text":"ofr87679 - 1988 - Geophysical logs and hydrologic data for eight wells in the Coyote Spring Valley area, Clark and Lincoln counties, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:32","indexId":"ofr87679","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-679","title":"Geophysical logs and hydrologic data for eight wells in the Coyote Spring Valley area, Clark and Lincoln counties, Nevada","docAbstract":"Geophysical logs, drilling operations, pump-test data, and water quality determinations are presented for eight wells in the Coyote Spring Valley area of southeastern Nevada. The wells are in an area where thick units of Paleozoic carbonate rock are overlain by Tertiary semiconsolidated basin-fill deposits and Quaternary alluvial deposits. Data collected by the U.S. Geological Survey were augmented with data from previous investigations; however, complete sets of logs and other data are not available for all eight wells. Geophysical data presented included natural-gamma, neutron, gamma-gamma density, caliper, temperature, acoustic, single-point resistance, long- and short-natural resistivity, and spontaneous-potential logs. Drilling penetration rates, lithologic columns, and well construction are also summarized and presented. Measurements of drawdown and recovery during and after constant-discharge pumping periods are also included. Also presented are results of chemical and physical analyses for major-ion chemistry, trace constituents, stable and radioactive isotopes, temperature, pH, specific conductance, and dissolved oxygen. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87679","usgsCitation":"Berger, D., Kilroy, K., and Schaefer, D.H., 1988, Geophysical logs and hydrologic data for eight wells in the Coyote Spring Valley area, Clark and Lincoln counties, Nevada: U.S. Geological Survey Open-File Report 87-679, vii, 58 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr87679.","productDescription":"vii, 58 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":143704,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0679/report-thumb.jpg"},{"id":41075,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0679/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8602","contributors":{"authors":[{"text":"Berger, D.L.","contributorId":106904,"corporation":false,"usgs":true,"family":"Berger","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":166514,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kilroy, K. C.","contributorId":49795,"corporation":false,"usgs":true,"family":"Kilroy","given":"K. C.","affiliations":[],"preferred":false,"id":166512,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schaefer, D. H.","contributorId":84763,"corporation":false,"usgs":true,"family":"Schaefer","given":"D.","middleInitial":"H.","affiliations":[],"preferred":false,"id":166513,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":57627,"text":"wdrFL874 - 1988 - Water resources data for Florida, water year 1987. Volume 4. Northwest Florida","interactions":[],"lastModifiedDate":"2025-02-10T14:54:39.791891","indexId":"wdrFL874","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"FL-87-4","title":"Water resources data for Florida, water year 1987. Volume 4. Northwest Florida","docAbstract":"<p>Water resources data for the 1987 water year in Florida consists of continuous or daily discharge for 320 streams, periodic discharge for 38 streams, miscellaneous discharge for 29 streams, continuous or daily stage for 94 streams, periodic stage for 48 streams, peak discharge for 76 streams and peak stage for 69 streams; continuous or daily elevations for 80 lakes, periodic elevations for 74 lakes; ground-water levels for 477 wells, periodic ground-water levels for 562 wells, and miscellaneous water-level measurements for 2886 wells; quality-of-water data for 223 surface-water sites and 900 wells.</p><p>The data for northwest Florida include continuous or daily discharge for 49 streams, periodic discharge for 4 streams, miscellaneous discharge for 6 streams, continuous or daily stage for 9 streams, peak discharge for 30 streams, and peak stage for 30 streams; continuous elevations for 5 lakes and periodic elevations for 4 lakes; continuous ground-water levels for 16 wells, and periodic ground-water levels for 70 wells; quality of water for 22 surface-water sites and 20 wells.</p><p>These data represent the National Water Data System records collected by the U.S. Geological Survey and cooperating local, state and federal agencies in Florida.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrFL874","collaboration":"Prepared in cooperation with the State of Florida and with other agencies","usgsCitation":"Meadows, P., Martin, J., and Mixson, P., 1988, Water resources data for Florida, water year 1987. Volume 4. Northwest Florida: U.S. Geological Survey Water Data Report FL-87-4, xiv, 265 p., https://doi.org/10.3133/wdrFL874.","productDescription":"xiv, 265 p.","costCenters":[],"links":[{"id":181421,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1987/fl-87-4/report-thumb.jpg"},{"id":481811,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1987/fl-87-4/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","otherGeospatial":"Northwest 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,{"id":17204,"text":"ofr88323 - 1988 - Ground-water data for Georgia, 1987","interactions":[],"lastModifiedDate":"2024-12-17T19:39:52.774728","indexId":"ofr88323","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"88-323","title":"Ground-water data for Georgia, 1987","docAbstract":"This report was prepared in cooperation with the State of Georgia;  Chatham County; Glynn County; the cities of Brunswick and Valdosta; and  the Albany Water, Gas, and Light Commission. This report is the culmination of a concerted effort by dedicated  personnel of the U.S. Geological Survey who collected, compiled, analyzed, verified, and organized the data, and who edited and assembled the report. In addition to the authors, who had primary responsibility for assuring that the information contained herein is accurate, complete, and adheres to Geological Survey policy and established guidelines, the following individuals contributed significantly to the collection, processing, and tabulation of the data:","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Doraville, GA","doi":"10.3133/ofr88323","collaboration":"Prepared in cooperation with the Georgia Department OF Natural Resources Environmental Protection Division and the Georgia Geologic Survey","usgsCitation":"Joiner, C.N., Reynolds, M., Stayton, W., and Boucher, F., 1988, Ground-water data for Georgia, 1987: U.S. Geological Survey Open-File Report 88-323, xvi, 172 p., https://doi.org/10.3133/ofr88323.","productDescription":"xvi, 172 p.","additionalOnlineFiles":"N","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":279467,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0323/report.pdf"},{"id":149902,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0323/report-thumb.jpg"},{"id":465211,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17399.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Georgia","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85.61,30.36 ], [ -85.61,35.00 ], [ -80.75,35.00 ], [ -80.75,30.36 ], [ -85.61,30.36 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cfa3","contributors":{"authors":[{"text":"Joiner, C. N.","contributorId":17615,"corporation":false,"usgs":true,"family":"Joiner","given":"C.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":175389,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reynolds, M.S.","contributorId":35338,"corporation":false,"usgs":true,"family":"Reynolds","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":175390,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stayton, W.L.","contributorId":65487,"corporation":false,"usgs":true,"family":"Stayton","given":"W.L.","affiliations":[],"preferred":false,"id":175392,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Boucher, F.G.","contributorId":53821,"corporation":false,"usgs":true,"family":"Boucher","given":"F.G.","email":"","affiliations":[],"preferred":false,"id":175391,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":12125,"text":"ofr88483 - 1988 - Index of surface-water stations in Texas, January 1988","interactions":[],"lastModifiedDate":"2016-08-12T15:23:07","indexId":"ofr88483","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"88-483","title":"Index of surface-water stations in Texas, January 1988","docAbstract":"<p>As of January 1, 1988, the surface-water data-collection network in Texas included 368 continuous streamflow, 12 continuous or daily reservoir-content, 38 gage height, 15 crest-stage partia 1-record, 4 periodic discharge through range, 32 floodhydrocjraph partial-record, 9 flood-profile partial-record, 36 low-flow partial-record 45 daily chemical-quality, 19 continuous-recording water-quality, 83 periodic biological, 19 lake surveys, 160 periodic organic and (or) nutrient, 3 periodic insecticide, 33 periodic pesticide, 20 automatic sampler, 137 periodic minor elements, 125 periodic chemical-quality, 74 periodic physica1-organic, 24 continuous-recording three- or four-parameter water-quality, 34 periodic sediment, 21 continuous-recording temperature, and 30 national stream-quality accounting network stations. Plate 1 shows the location of surface-water streamflow or reservoir-content and chemicalquality or sediment stations in Texas. Plate 2 shows the location of partial-record surface-water stations.</p>\n<p>This index shows the station number and name, latitude and longitude, type of data collected, and the office principally responsible for the data collection (table 1). An 8-digit permanent numerical designation for gaging stations has been adopted on a nationwide basis; stations are numbered and listed in downstream order. In the downstream direction along the main stem, all stations on a tributary entering above a main-stem station are listed before that station. A tributary entering between two main-stem stations is listed between them. A similar order is followed in listing stations on first rank, second rank, and other ranks of tributaries. To indicate the rank of any tributary on which a gaging station is situated and the stream to which it is an immediate tributary, each indention in the listing of gaging stations represent one rank. This downstream order and system of indention show which gaging stations are on tributaries between any two stations on a main stem and the rank of the tributary on which each gaging station is situated. On plates 1 and 2, the 8-digit station number is abbreviated because of space limitation.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr88483","usgsCitation":"1988, Index of surface-water stations in Texas, January 1988: U.S. Geological Survey Open-File Report 88-483, Report: iii, 17 p.; 2 Plates: 16.20 x 15.18 inches and 16.25 x 15.14 inches, https://doi.org/10.3133/ofr88483.","productDescription":"Report: iii, 17 p.; 2 Plates: 16.20 x 15.18 inches and 16.25 x 15.14 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f296b","contributors":{"compilers":[{"text":"Rawson, Jack","contributorId":18345,"corporation":false,"usgs":true,"family":"Rawson","given":"Jack","affiliations":[],"preferred":false,"id":645398,"contributorType":{"id":3,"text":"Compilers"},"rank":1},{"text":"Carrillo, E.R.","contributorId":77924,"corporation":false,"usgs":true,"family":"Carrillo","given":"E.R.","email":"","affiliations":[],"preferred":false,"id":645399,"contributorType":{"id":3,"text":"Compilers"},"rank":2},{"text":"Buckner, H.D.","contributorId":49783,"corporation":false,"usgs":true,"family":"Buckner","given":"H.D.","email":"","affiliations":[],"preferred":false,"id":645400,"contributorType":{"id":3,"text":"Compilers"},"rank":3}]}}
,{"id":13547,"text":"ofr8885 - 1988 - Evaluation of the state water-resources research institutes","interactions":[],"lastModifiedDate":"2012-02-02T00:06:49","indexId":"ofr8885","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"88-85","title":"Evaluation of the state water-resources research institutes","docAbstract":"Water resources research institutes, as authorized by the Water Resources Research Act of 1984 (Public Law 98-242), are located in each state and in the District of Columbia, Guam, Puerto Rico , and the Virgin Islands. Public Law 98-242 mandated an onsite evaluation of each of these institutes to determine whether ' . . .the quality and relevance of its water resources research and its effectiveness as an institution for planning, conducting, and arranging for research warrant its continued support in the national interest. ' The results of these evaluations, which were conducted between September 1985 and June 1987, are summarized. The evaluation teams found that all 54 institutes are meeting the basic objectives of the authorizing legislation in that they: (1) use the grant funds to support research that addresses water problems of state and regional concern; (2) provide opportunities for training of water scientists through student involvement on research projects; and (3) promote the application of research results through preparation of technical reports and contributions to the technical literature. The differences among institutes relate primarily to degrees of effectiveness, and most often are determined by the financial, political, and geographical contexts in which the institutes function and by the quality of their leadership. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8885","usgsCitation":"Ertel, M., 1988, Evaluation of the state water-resources research institutes: U.S. Geological Survey Open-File Report 88-85, iii, 28 p. ;28 cm., https://doi.org/10.3133/ofr8885.","productDescription":"iii, 28 p. ;28 cm.","costCenters":[],"links":[{"id":145975,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0085/report-thumb.jpg"},{"id":42029,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0085/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e09c0","contributors":{"authors":[{"text":"Ertel, M.O.","contributorId":71183,"corporation":false,"usgs":true,"family":"Ertel","given":"M.O.","email":"","affiliations":[],"preferred":false,"id":167986,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12693,"text":"ofr88719 - 1988 - Hydrologic data collection activities in the Solomon Gulch basin near Valdez, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:39","indexId":"ofr88719","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"88-719","title":"Hydrologic data collection activities in the Solomon Gulch basin near Valdez, Alaska","docAbstract":"In 1981, the Alaska Power Authority completed construction of a dam spillway at the north end of Solomon Lake near Valdez. Regulation and diversion from the dam since 1982 have significantly altered the natural flow characteristics of Solomon Gulch. In September 1986, the Geological Survey began data collection to determine mean daily discharge at four sites below Solomon Lake and thus document the effects of regulation and diversion of water on the flow at various points in the system. Periodic discharge measurements and continuous records of water stage were obtained at two of the sites, and daily discharge values were computed for all four sites. The report contains descriptions of the data collection sites and the discharge records for each site for September 1986 and water year 1987. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88719","usgsCitation":"Bigelow, B.B., 1988, Hydrologic data collection activities in the Solomon Gulch basin near Valdez, Alaska: U.S. Geological Survey Open-File Report 88-719, iv, 15 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr88719.","productDescription":"iv, 15 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":145556,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0719/report-thumb.jpg"},{"id":41105,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0719/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f808","contributors":{"authors":[{"text":"Bigelow, B. B.","contributorId":76317,"corporation":false,"usgs":true,"family":"Bigelow","given":"B.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":166555,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55126,"text":"wdrWY871 - 1988 - Water resources data, Wyoming, water year 1987","interactions":[],"lastModifiedDate":"2025-08-19T13:28:17.520867","indexId":"wdrWY871","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WY-87-1","title":"Water resources data, Wyoming, water year 1987","docAbstract":"<p>Water resources data for the 1987 water year for Wyoming consists of records of stage, discharge and water quality of streams; stage and contents of lakes and reservoirs; and water levels and water quality of ground water. This report contains discharge records for 172 gaging stations; stage and contents for 16 lakes and reservoirs; water quality for 67 gaging stations, and 52 ungaged stations; and water levels for 5 observation wells. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Wyoming.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWY871","usgsCitation":"Druse, S.A., Glass, W.R., McCollum, P.B., and Peterson, D.A., 1988, Water resources data, Wyoming, water year 1987: U.S. Geological Survey Water Data Report WY-87-1, ix, 396 p., https://doi.org/10.3133/wdrWY871.","productDescription":"ix, 396 p.","costCenters":[],"links":[{"id":174026,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1987/wy-87-1/report-thumb.jpg"},{"id":494265,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1987/wy-87-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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A.","contributorId":89934,"corporation":false,"usgs":true,"family":"Druse","given":"S.","middleInitial":"A.","affiliations":[],"preferred":false,"id":252713,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Glass, W. R.","contributorId":97535,"corporation":false,"usgs":true,"family":"Glass","given":"W.","middleInitial":"R.","affiliations":[],"preferred":false,"id":252714,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McCollum, P. B.","contributorId":27921,"corporation":false,"usgs":true,"family":"McCollum","given":"P.","middleInitial":"B.","affiliations":[],"preferred":false,"id":252712,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Peterson, D. A.","contributorId":6453,"corporation":false,"usgs":true,"family":"Peterson","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":252711,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":15547,"text":"ofr88322 - 1988 - Water-resources investigations in Tennessee; programs and activities of the U.S. Geological Survey, 1987-1988","interactions":[],"lastModifiedDate":"2012-02-02T00:07:07","indexId":"ofr88322","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"88-322","title":"Water-resources investigations in Tennessee; programs and activities of the U.S. Geological Survey, 1987-1988","docAbstract":"This report contains a summation of 44 projects which were active in the Tennessee District during 1987 and 1988. Given in each summary is the name of the project chief, the objective of the project, the progress or results of the study to date, and the name of the cooperator. Hydrologic data are the backbone of the investigations conducted by the U.S Geological Survey (USGS). The basic data programs conducted by the Tennessee District provide streamflow, quality of water, and groundwater levels information essential to the assessment and management of the State 's water resources. Long-term streamflow, quality of water, and groundwater levels network are operated as part of the Hydrologic Data Section. Field operations are about equally divided among field offices in Memphis, Nashville, and Knoxville. A staff of about 40 engineers, hydrologists, and hydrologic technicians labor in the operation of the long-term network as well as short-term efforts in support of areal investigations. The data collected as part of the networks are published in the series of annual data reports. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88322","usgsCitation":"Quinones, F., Balthrop, B., and Baker, E., 1988, Water-resources investigations in Tennessee; programs and activities of the U.S. Geological Survey, 1987-1988: U.S. Geological Survey Open-File Report 88-322, v, 63 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr88322.","productDescription":"v, 63 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":148391,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1005,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr88-322","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4e77","contributors":{"authors":[{"text":"Quinones, Ferdinand","contributorId":44138,"corporation":false,"usgs":true,"family":"Quinones","given":"Ferdinand","email":"","affiliations":[],"preferred":false,"id":171309,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Balthrop, B.H.","contributorId":42980,"corporation":false,"usgs":true,"family":"Balthrop","given":"B.H.","email":"","affiliations":[],"preferred":false,"id":171308,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baker, E.G.","contributorId":84382,"corporation":false,"usgs":true,"family":"Baker","given":"E.G.","email":"","affiliations":[],"preferred":false,"id":171310,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":15797,"text":"ofr88462 - 1988 - Report of the River Master of the Delaware River for the period December 1, 1986-November 30, 1987, with a section on water quality","interactions":[],"lastModifiedDate":"2012-02-02T00:07:12","indexId":"ofr88462","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"88-462","title":"Report of the River Master of the Delaware River for the period December 1, 1986-November 30, 1987, with a section on water quality","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88462","usgsCitation":"Sauer, S.P., Harkness, W.E., Krejmas, B.E., and White, K.E., 1988, Report of the River Master of the Delaware River for the period December 1, 1986-November 30, 1987, with a section on water quality: U.S. Geological Survey Open-File Report 88-462, v, 86 p. ill. (1 col.), map ;28 cm., https://doi.org/10.3133/ofr88462.","productDescription":"v, 86 p. ill. (1 col.), map ;28 cm.","costCenters":[],"links":[{"id":149787,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0462/report-thumb.jpg"},{"id":44824,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0462/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5ee4b07f02db633b4c","contributors":{"authors":[{"text":"Sauer, Stanley P.","contributorId":38966,"corporation":false,"usgs":true,"family":"Sauer","given":"Stanley","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":171739,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harkness, William E.","contributorId":43797,"corporation":false,"usgs":true,"family":"Harkness","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":171740,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krejmas, Bruce E.","contributorId":102501,"corporation":false,"usgs":true,"family":"Krejmas","given":"Bruce","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":171742,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"White, K. E.","contributorId":65873,"corporation":false,"usgs":true,"family":"White","given":"K.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":171741,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":12702,"text":"ofr88167 - 1988 - Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey","interactions":[{"subject":{"id":12702,"text":"ofr88167 - 1988 - Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey","indexId":"ofr88167","publicationYear":"1988","noYear":false,"title":"Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey"},"predicate":"SUPERSEDED_BY","object":{"id":18174,"text":"ofr91500 - 1991 - Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey","indexId":"ofr91500","publicationYear":"1991","noYear":false,"title":"Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey"},"id":1}],"supersededBy":{"id":18174,"text":"ofr91500 - 1991 - Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey","indexId":"ofr91500","publicationYear":"1991","noYear":false,"title":"Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey"},"lastModifiedDate":"2012-02-02T00:06:32","indexId":"ofr88167","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"88-167","title":"Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey","docAbstract":"Codes for the unique identification of public and private organizations listed in computerized data systems are presented. These codes are used by the U.S. Geological Survey 's National Water Data Exchange (NAWDEX), National Water Data Storage and Retrieval System (WATSTORE), National Cartographic Information Center (NCIC), and Office of Water Data Coordination (OWDC). The format structure of the codes is discussed and instructions are given for requesting new books. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88167","usgsCitation":"Blackwell, C., 1988, Identification codes for organizations listed in computerized data systems of the U.S. Geological Survey: U.S. Geological Survey Open-File Report 88-167, vi, 334 p. (loose leafed) ;28 cm., https://doi.org/10.3133/ofr88167.","productDescription":"vi, 334 p. (loose leafed) ;28 cm.","costCenters":[],"links":[{"id":143795,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0167/report-thumb.jpg"},{"id":41115,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0167/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faa7d","contributors":{"authors":[{"text":"Blackwell, C.D.","contributorId":51747,"corporation":false,"usgs":true,"family":"Blackwell","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":166569,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25617,"text":"wri884165 - 1988 - Iodine-129 in the Snake River Plain aquifer at the Idaho National Engineering Laboratory, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:08:21","indexId":"wri884165","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4165","title":"Iodine-129 in the Snake River Plain aquifer at the Idaho National Engineering Laboratory, Idaho","docAbstract":"From 1953 to 1983, an estimated 0.01 to 0.136 Ci (curies)/year of iodine-129 were contained in wastewater generated by the ICPP (Idaho Chemical Processing Plant) at the Idaho National Engineering Laboratory. The wastewater was directly discharged to the Snake River Plain aquifer through a deep disposal well until February 9, 1984, when the well was replaced by an unlined infiltration pond; a second pond was put into use on October 17, 1985. For 1984-86, the annual amount of iodine-129 in wastewater discharged to the ponds ranged from 0.0064 to 0.039 Ci. In August 1986, iodine-129 concentrations in water from 35 wells near the ICPP ranged from less than the reporting level to 3.6 +or-0.4 pCi/L (picocuries/L). By comparison, in April 1977 the water from 20 wells contained a maximum of 27 +or-1 pCi/L of iodine-129; in 1981, the maximum concentration in water from 32 wells was 41 +or-2 pCi/L. The average concentrations of iodine-129 in water from 18 wells that were sampled in 1977, 1981 and 1986 were 4.0, 6.7 and 1.3 pCi/L, respectively. The marked decrease in the iodine-129 concentration from 1981 to 1986 is the result of three factors: (1) The amount of iodine-129 disposed annually; (2) a change from the routine use of the disposal well to the infiltration ponds; and (3) a dilution of the iodine-129 in the aquifer by recharge from the Big Lost River. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884165","usgsCitation":"Mann, L., Chew, E., Morton, J., and Randolph, R., 1988, Iodine-129 in the Snake River Plain aquifer at the Idaho National Engineering Laboratory, Idaho: U.S. Geological Survey Water-Resources Investigations Report 88-4165, iv, 27 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884165.","productDescription":"iv, 27 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124081,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4165/report-thumb.jpg"},{"id":54363,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4165/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6966ff","contributors":{"authors":[{"text":"Mann, L. J.","contributorId":39392,"corporation":false,"usgs":true,"family":"Mann","given":"L. J.","affiliations":[],"preferred":false,"id":194428,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chew, E.W.","contributorId":21818,"corporation":false,"usgs":true,"family":"Chew","given":"E.W.","email":"","affiliations":[],"preferred":false,"id":194426,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morton, J.S.","contributorId":14249,"corporation":false,"usgs":true,"family":"Morton","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":194425,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Randolph, R.B.","contributorId":38606,"corporation":false,"usgs":true,"family":"Randolph","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":194427,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":27106,"text":"wri874034 - 1988 - Hydrogeology, aquifer characteristics, and ground-water flow of the surficial aquifer system, Broward County, Florida","interactions":[],"lastModifiedDate":"2022-01-10T12:39:00.489015","indexId":"wri874034","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4034","title":"Hydrogeology, aquifer characteristics, and ground-water flow of the surficial aquifer system, Broward County, Florida","docAbstract":"The surficial aquifer system, in which an unconfined groundwater flow system exists, comprises the sediments from land surface to the intermediate confining unit (formerly called the Floridan aquiclude) in Broward County, Florida. These sediments have hydraulic conductivities that range more than seven orders of magnitude from about 0.001 ft/d to more than 10,000 ft/d. The sediments are grouped into (1) the Biscayne aquifer, (2) a semiconfining unit, (3) a gray limestone aquifer in west Broward County, and (4) basal sand or clayey sand. The system is about 160 ft thick in west Broward County and more than 350 ft thick in east Broward. Transmissivities, locally variable, show a clear areal trend from greater than 300,000 sq ft/day in southeast Broward County to less than 75,000 sq ft/day in the northwest part of the county. Very high transmissivity is associated with the Biscayne aquifer. Transmissivity of the gray limestone aquifer ranged from about 20,000 to 88,000 sq ft/day. Topography, water levels, geologic framework, and water quality in west Broward County suggest past and present groundwater movement is south or southeast. Drainage and urban development have greatly altered circulation patterns in east Broward County , eliminating the original coastal groundwater ridge, causing rapid surface runoff and short groundwater flow paths, and saltwater intrusion. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri874034","collaboration":"Prepared in cooperation with the South Florida Water Management District","usgsCitation":"Fish, J., 1988, Hydrogeology, aquifer characteristics, and ground-water flow of the surficial aquifer system, Broward County, Florida: U.S. Geological Survey Water-Resources Investigations Report 87-4034, vi, 92 p., https://doi.org/10.3133/wri874034.","productDescription":"vi, 92 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science 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href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db6148c9","contributors":{"authors":[{"text":"Fish, J.E.","contributorId":101658,"corporation":false,"usgs":true,"family":"Fish","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":197561,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57448,"text":"wdrMS871 - 1988 - Water resources data for Mississippi, water year 1987","interactions":[],"lastModifiedDate":"2025-08-28T13:41:03.782564","indexId":"wdrMS871","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MS-87-1","title":"Water resources data for Mississippi, water year 1987","docAbstract":"<p>Water resources data for the 1987 water year for Mississippi consist of records of stage, discharge, and water quality of streams; stage, and water quality of lakes and reservoirs; and water levels and water quality of ground-water wells. This report contains records of water discharge at 78 gaging stations; stage records for 18 of these gaging stations; stage only at 5 gaging stations; water quality for 11 stations, 3 precipitation quality stations, and 120 wells; and water levels for 498 observation wells. Also included are peak-discharge data for 56 crest-stage partial record stations, discharge data at 263 low-flow partial-record stations, and water quality data at 2 partial-record or miscellaneous sites. Locations of these sites are shown on Figures 4-6. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Mississippi. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMS871","collaboration":"Prepared in cooperation with the Mississippi Department of Natural Resources and with other State, county, municipal, and Federal agencies","usgsCitation":"Tharpe, E., Plunkett, M., Morris, F., and Oakley, W.T., 1988, Water resources data for Mississippi, water year 1987: U.S. Geological Survey Water Data Report MS-87-1, viii, 408 p., https://doi.org/10.3133/wdrMS871.","productDescription":"viii, 408 p.","costCenters":[],"links":[{"id":494987,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1987/ms-87-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174621,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1987/ms-87-1/report-thumb.jpg"}],"country":"United 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fccdf","contributors":{"authors":[{"text":"Tharpe, E.J.","contributorId":57534,"corporation":false,"usgs":true,"family":"Tharpe","given":"E.J.","email":"","affiliations":[],"preferred":false,"id":257044,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plunkett, M.L.","contributorId":82368,"corporation":false,"usgs":true,"family":"Plunkett","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":257046,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morris, F.","contributorId":17299,"corporation":false,"usgs":true,"family":"Morris","given":"F.","affiliations":[],"preferred":false,"id":257043,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Oakley, W. T.","contributorId":76331,"corporation":false,"usgs":true,"family":"Oakley","given":"W.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":257045,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":3627,"text":"cir1019 - 1988 - Review of the general geology and solid-phase geochemical studies in the vicinity of the Central Oklahoma aquifer","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"cir1019","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1019","title":"Review of the general geology and solid-phase geochemical studies in the vicinity of the Central Oklahoma aquifer","docAbstract":"The Central Oklahoma aquifer is the principal source of ground water for municipal, industrial, and rural use in central Oklahoma. Ground water in the aquifer is contained in consolidated sedimentary rocks consisting of the Admire, Council Grove, and Chase Groups, Wellington Formation, and Garber Sandstone and in the unconsolidated Quaternary alluvium and terrace deposits that occur along the major stream systems in the study area. The Garber Sandstone and the Wellington Formation comprise the main flow system and, as such, the aquifer is often referred to as the 'Garber-Wellington aquifer.' The consolidated sedimentary rocks consist of interbedded lenticular sandstone, shale, and siltstone beds deposited in similar deltaic environments in early Permian time. Arsenic, chromium, and selenium are found in the ground water of the Central Oklahoma aquifer in concentrations that, in places, exceed the primary drinking-water standards of the Environmental Protection Agency. Gross-alpha concentrations also exceed the primary standards in some wells, and uranium concentrations are uncommonly high in places. \r\n\r\nAs a prerequisite to a surface and subsurface solid-phase geochemical study, this report summarizes the general geology of the Central Oklahoma study area. Summaries of results from certain previously reported solid-phase geochemical studies that relate to the vicinity of the Central Oklahoma aquifer are also given; including a summary of the analytical results and distribution plots for arsenic, selenium, chromium, thorium, uranium, copper, and barium from the U.S. Department of Energy's National Uranium Resource Evaluation (NURE) Program.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/cir1019","usgsCitation":"Mosier, E.L., and Bullock, J., 1988, Review of the general geology and solid-phase geochemical studies in the vicinity of the Central Oklahoma aquifer: U.S. Geological Survey Circular 1019, iii, 18 p. :ill., maps ;28 cm., https://doi.org/10.3133/cir1019.","productDescription":"iii, 18 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":117413,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1988/1019/report-thumb.jpg"},{"id":30670,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1988/1019/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbe12","contributors":{"authors":[{"text":"Mosier, Elwin L.","contributorId":70374,"corporation":false,"usgs":true,"family":"Mosier","given":"Elwin","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":147284,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bullock, John H.","contributorId":43336,"corporation":false,"usgs":true,"family":"Bullock","given":"John H.","affiliations":[],"preferred":false,"id":147283,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27164,"text":"wri874260 - 1988 - Hydrogeology and flow of water in a sand and gravel aquifer contaminated by wood-preserving compounds, Pensacola, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:26","indexId":"wri874260","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4260","title":"Hydrogeology and flow of water in a sand and gravel aquifer contaminated by wood-preserving compounds, Pensacola, Florida","docAbstract":"The sand and gravel aquifer in southern Escambia County, Florida , is a typical surficial aquifer composed of quartz sands and gravels interbedded locally with silts and clays. Problems of groundwater contamination from leaking surface impoundments are common in surficial aquifers and are a subject of increasing concern and attention. A potentially widespread contamination problem involves organic chemicals from wood-preserving processes. Because creosote is the most extensively used industrial preservative in the United States, an abandoned wood-treatment plant near Pensacola was chosen for investigation. This report describes the hydrogeology and groundwater flow system of the sand and gravel aquifer near the plant. A three-dimensional simulation of groundwater flow in the aquifer was evaluated under steady-state conditions. The model was calibrated on the basis of observed water levels from January 1986. Calibration criteria included reproducing all water levels within the accuracy of the data (one-half contour interval in most cases). Sensitivity analysis showed that the simulations were most sensitive to recharge and vertical leakance of the confining units between layers 1 and 2, and relatively insensitive to changes in hydraulic conductivity and transmissivity and to other changes in vertical leakance. Applications of the results of the calibrated flow model in evaluation of solute transport may require further discretization of the contaminated area, including more sublayers, than were needed for calibration of the groundwater flow system itself. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874260","usgsCitation":"Franks, B., 1988, Hydrogeology and flow of water in a sand and gravel aquifer contaminated by wood-preserving compounds, Pensacola, Florida: U.S. Geological Survey Water-Resources Investigations Report 87-4260, v, 72 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874260.","productDescription":"v, 72 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123427,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4260/report-thumb.jpg"},{"id":56040,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4260/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ade66","contributors":{"authors":[{"text":"Franks, B.J.","contributorId":107739,"corporation":false,"usgs":true,"family":"Franks","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":197671,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4687,"text":"twri02D2 - 1988 - Application of seismic-refraction techniques to hydrologic studies","interactions":[{"subject":{"id":13950,"text":"ofr84746 - 1986 - Application of seismic-refraction techniques to hydrologic studies","indexId":"ofr84746","publicationYear":"1986","noYear":false,"title":"Application of seismic-refraction techniques to hydrologic studies"},"predicate":"SUPERSEDED_BY","object":{"id":4687,"text":"twri02D2 - 1988 - Application of seismic-refraction techniques to hydrologic studies","indexId":"twri02D2","publicationYear":"1988","noYear":false,"title":"Application of seismic-refraction techniques to hydrologic studies"},"id":1}],"lastModifiedDate":"2019-10-15T07:46:19","indexId":"twri02D2","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"02-D2","title":"Application of seismic-refraction techniques to hydrologic studies","docAbstract":"During the past 30 years, seismic-refraction methods have been used extensively in petroleum, mineral, and engineering investigations and to some extent for hydrologic applications.  Recent advances in equipment, sound sources, and computer interpretation techniques make seismic refraction a highly effective and economical means of obtaining subsurface data in hydrologic studies.  Aquifers that can be defined by one or more high-seismic-velocity surface, such as (1) alluvial or glacial deposits in consolidated rock valleys, (2) limestone or sandstone underlain by metamorphic or igneous rock, or (3) saturated unconsolidated deposits overlain by unsaturated unconsolidated deposits, are ideally suited for seismic-refraction methods.  These methods allow economical collection of subsurface data, provide the basis for more efficient collection of data by test drilling or aquifer tests, and result in improved hydrologic studies.  This manual briefly reviews the basics of seismic-refraction theory and principles.  It emphasizes the use of these techniques in hydrologic investigations and describes the planning, equipment, field procedures, and interpretation techniques needed for this type of study.  Further-more, examples of the use of seismic-refraction techniques in a wide variety of hydrologic studies are presented.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/twri02D2","issn":"0565-596X","usgsCitation":"Haeni, F., 1988, Application of seismic-refraction techniques to hydrologic studies: U.S. Geological Survey Techniques of Water-Resources Investigations 02-D2, x, 86 p. , https://doi.org/10.3133/twri02D2.","productDescription":"x, 86 p. ","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"links":[{"id":139165,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":247,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri2d2/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a89a","contributors":{"authors":[{"text":"Haeni, F.P.","contributorId":87105,"corporation":false,"usgs":true,"family":"Haeni","given":"F.P.","affiliations":[],"preferred":false,"id":149624,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27177,"text":"wri884040 - 1988 - Geohydrology of the Navajo sandstone in western Kane, southwestern Garfield, and southeastern Iron counties, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:08:26","indexId":"wri884040","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4040","title":"Geohydrology of the Navajo sandstone in western Kane, southwestern Garfield, and southeastern Iron counties, Utah","docAbstract":"The upper Navajo and Lamb Point aquifers in the Navajo Sandstone are the principal source of water for the city of Kanab, irrigation, stock, and for rural homes in the study area. Well logs and outcrop descriptions indicate the Navajo Sandstone consists of the Lamb Point Tongue and an unnamed upper member that are separated by the Tenney Canyon Tongue of the Kayenta Formation. The main Kayenta Formation underlies the Lamb Point Tongue. The Lamb Point Tongue and the upper member of the Navajo Sandstone are saturated and hydraulically connected through the Tenney Canyon Tongue. Available data indicate that precipitation percolates to the groundwater reservoir where the Navajo Sandstone crops out. Estimates of the rate of recharge at the outcrop range from 0.1 to as much as 2.8 in/yr. Water level data indicate that water moves from the upper member of the Navajo Sandstone, through the Tenney Canyon Tongue, and into the Lamb Point Tongue. Lateral flow is generally from the outcrop areas toward the incised canyons formed by tributaries of Kanab Creek and Johnson Wash. Direction and rate of groundwater movement and the location and character of the natural hydrologic boundaries in the northern part of the area where the Navajo Sandstone is buried cannot be determined conclusively without additional water level data. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884040","usgsCitation":"Freethey, G., 1988, Geohydrology of the Navajo sandstone in western Kane, southwestern Garfield, and southeastern Iron counties, Utah: U.S. Geological Survey Water-Resources Investigations Report 88-4040, v, 43 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884040.","productDescription":"v, 43 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118738,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4040/report-thumb.jpg"},{"id":56053,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4040/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56054,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4040/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56052,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4040/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8932","contributors":{"authors":[{"text":"Freethey, G. W.","contributorId":105714,"corporation":false,"usgs":true,"family":"Freethey","given":"G. W.","affiliations":[],"preferred":false,"id":197695,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27179,"text":"wri874279 - 1988 - Effects of fluctuating river-pool stages on ground-water levels in the adjacent alluvial aquifer in the lower Arkansas River, Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:08:26","indexId":"wri874279","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4279","title":"Effects of fluctuating river-pool stages on ground-water levels in the adjacent alluvial aquifer in the lower Arkansas River, Arkansas","docAbstract":"The U.S. Geological Survey conducted a study in cooperation with the U.S. Army Corps of Engineers to determine the effect of fluctuating the lower Arkansas River. A network of 41 wells was used to delineate 4 cross sections adjacent to river pools 2 and 5 of the McClellan-Kerr Arkansas River Navigation System to examine groundwater levels at various distances from the river. The hydraulic gradient of water levels in the alluvial aquifer along these cross sections indicates that the river is losing water to the adjacent aquifer. The effect on groundwater levels in the alluvial aquifer caused by pool-stage fluctuations was most pronounced at distances less than about 2 miles from the Arkansas River. At distances greater than about 2 miles, the changes in groundwater levels probably were the result of water levels rising in the aquifer since the heavy summer irrigation withdrawals have ceased. An equation useful for estimating the distribution of head change an aquifer in response to river-pool-stage changes, was applied to the study area to estimate the effect of a 1-foot rise in pool stage on water levels in the adjacent alluvial aquifer after equilibrium conditions have been established. The theoretical head change (rise) in the aquifer was estimated to range from 1-foot at the Arkansas River to 0.57 foot at a distance of 5 miles away from the river. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874279","usgsCitation":"Freiwald, D., and Grosz, G., 1988, Effects of fluctuating river-pool stages on ground-water levels in the adjacent alluvial aquifer in the lower Arkansas River, Arkansas: U.S. Geological Survey Water-Resources Investigations Report 87-4279, iv, 22 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874279.","productDescription":"iv, 22 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124180,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4279/report-thumb.jpg"},{"id":56055,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4279/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ce4b07f02db6140f1","contributors":{"authors":[{"text":"Freiwald, D.A.","contributorId":39000,"corporation":false,"usgs":true,"family":"Freiwald","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":197697,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grosz, G.D.","contributorId":90340,"corporation":false,"usgs":true,"family":"Grosz","given":"G.D.","email":"","affiliations":[],"preferred":false,"id":197698,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}