{"pageNumber":"1876","pageRowStart":"46875","pageSize":"25","recordCount":68927,"records":[{"id":3186,"text":"wsp2325 - 1988 - National water summary 1986: Hydrologic events and ground-water quality","interactions":[],"lastModifiedDate":"2024-06-28T20:58:06.584628","indexId":"wsp2325","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2325","title":"National water summary 1986: Hydrologic events and ground-water quality","docAbstract":"<p>Ground water is one of the most important natural resources of the United States and degradation of its quality could have a major effect on the welfare of the Nation. Currently (1985), ground water is the source of drinking water for 53 percent of the Nation's population and for more than 97 percent of its rural population. It is the source of about 40 percent of the Nation's public water supply, 33 percent of water for irrigation, and 17 percent of freshwater for selfsupplied industries.</p><p>Ground water also is the source of about 40 percent of the average annual streamflow in the United States, although during long periods of little or no precipitation, ground-water discharges provide nearly all of the base streamflow. This hydraulic connection between aquifers and streams implies that if a persistent pollutant gets into an aquifer, it eventually could discharge into a stream.</p><p>Information presented in the 1986 National Water Summary clearly shows that the United States has very large amounts of potable ground water available for use. Although naturally occurring constituents, such as nitrate, and human-induced substances, such as synthetic organic chemicals, frequently are detected in ground water, their concentrations usually do not exceed existing Federal or State standards or guidelines for maximum concentrations in drinking water.</p><p>Troublesome contamination of ground water falls into two basic categories related to the source or sources of the contamination. Locally, high concentrations of a variety of toxic metals, organic chemicals, and petroleum products have been detected in ground water associated with point sources such as wastedisposal sites, storage-tank leaks, and hazardous chemical spills. These types of local problems commonly occur in densely populated urban areas and industrialized areas. Larger, multicounty areas also have been identified where contamination frequently is found in shallow wells. These areas generally are associated with broad-scale, or nonpoint, sources of contamination such as agricultural activities or highdensity domestic waste disposal (septic systems) in urban centers. At present, only a very small percentage of the total volume of potable ground water in the United States is contaminated from both point and nonpoint sources; however, available data, especially data about the occurrence of synthetic organic and toxic substances, generally are inadequate to determine the full extent of ground-water contamination in the Nation's aquifers or to define trends in groundwater quality. Most information about the occurrence of these substances has come from the study of individual sites or areas where contamination had already been detected or suspected.</p><p>Management and protection of ground water present a major challenge to the Nation. Current and projected costs of detection and cleanup of existing ground-water contamination are staggering and, even so, complete removal of pollutants from ground water in the vicinity of some waste sites might not be technically feasible. At all levels of government, the task of protecting the resource for its most beneficial uses is difficult and controversial.</p><p>Despite increasing awareness that some of the Nation's ground water is contaminated with a variety of toxic metals, synthetic organic chemicals, radionuclides, pesticides, and other contaminants that might present a long-term risk to human health, public policy towards ground-water protection is still in the formative stages. Despite increasing efforts devoted to ground-water protection by State and Federal regulatory and resource-management agencies, the extent of ground-water contamination is likely to appear to increase over the next few years because more agencies will be searching for evidence of contamination, and they will be using increasingly sensitive analytical procedures. Increased technology and expanded monitoring activities probably will detect the effects of past contamination and land uses on water quality. The significant time lag between a waterquality change in one part of an aquifer system and the effects of that change at a downgradient site, such as a well, results from the generally slow movement of ground water. This lag between cause and observed effect needs to be considered in evaluating the effectiveness of current and future ground-water policies and remedial measures.</p><p>Conclusive answers to questions about the location, extent, and severity of ground-water contamination, and about trends in ground-water quality, must await further collection and analysis of data from the Nation's aquifers. Generalizations, however, can be made, and the 1986 National Water Summary, which describes the natural quality of ground-water resources in each State and the major contamination problems that have been identified as of 1986, provides a national perspective of the ground-water-quality situation.</p><p>The 1986 <i>National Water Summary</i> follows the format of previous volumes. It contains three parts, and the contents of each of these parts are highlighted below.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2325","usgsCitation":"United States Geological Survey, 1988, National water summary 1986: Hydrologic events and ground-water quality: U.S. Geological Survey Water Supply Paper 2325, ix, 560 p., https://doi.org/10.3133/wsp2325.","productDescription":"ix, 560 p.","numberOfPages":"570","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true},{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true},{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true},{"id":583,"text":"Texas Water Science 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,{"id":27304,"text":"wri884055 - 1988 - Channel infiltration from floodflows along the Pawnee River and its tributaries, west-central Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:08:41","indexId":"wri884055","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":"88-4055","title":"Channel infiltration from floodflows along the Pawnee River and its tributaries, west-central Kansas","docAbstract":"Most of the streams is west-central Kansas are ephemeral. Natural recharge to the alluvial aquifers underlying these streams occurs during periods of storm runoff in the ephemeral channels. Proposed flood-retarding structures within the basin will alter the downstream runoff characteristics in these channels by reducing the peak flow and increasing the flow duration. Information concerning channel-infiltration rate, unsaturated and saturated flow, and lithology of the unsaturated zone as related to stream stage and duration was collected along the Pawnee River and its tributaries to determine the effects of the flood-retarding structures. The infiltration rate on ephemeral streams was determined at five sites within the Pawnee River Basin. Tests were conducted in channel infiltrometers constructed by isolating a section of channel with two plastic-lined wooden cofferdams. At two of the sites, perched groundwater mounds intersected the bottom of the channel and reduced the infiltration rate. At two other sites where the perched groundwater mounds did not reach the bottom of the channel, the infiltration rate was directly proportional to the stage. Comparison of infiltration from simulated controlled and uncontrolled floodflows at the five sites indicated an average increase of about 2% with the controlled floodflow. Cumulative infiltration for these simulations ranged from 0.5 to 14.8 acre-ft/mi of channel. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884055","usgsCitation":"Gillespie, J.B., and Perry, C.A., 1988, Channel infiltration from floodflows along the Pawnee River and its tributaries, west-central Kansas: U.S. Geological Survey Water-Resources Investigations Report 88-4055, v, 30 p. :ill., map ;28 cm., https://doi.org/10.3133/wri884055.","productDescription":"v, 30 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":122949,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4055/report-thumb.jpg"},{"id":56177,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4055/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dee4b07f02db5e30a8","contributors":{"authors":[{"text":"Gillespie, James B.","contributorId":72809,"corporation":false,"usgs":true,"family":"Gillespie","given":"James","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":197883,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Perry, C. A.","contributorId":106149,"corporation":false,"usgs":true,"family":"Perry","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":197884,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28999,"text":"wri884009 - 1988 - Fracture characterization and fracture-permeability estimation at the underground research laboratory in southeastern Manitoba, Canada","interactions":[],"lastModifiedDate":"2012-02-02T00:08:52","indexId":"wri884009","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":"88-4009","title":"Fracture characterization and fracture-permeability estimation at the underground research laboratory in southeastern Manitoba, Canada","docAbstract":"Various conventional geophysical well logs were obtained in conjunction with acoustic tube-wave amplitude and experimental heat-pulse flowmeter measurements in two deep boreholes in granitic rocks on the Canadian shield in southeastern Manitoba. The objective of this study is the development of measurement techniques and data processing methods for characterization of rock volumes that might be suitable for hosting a nuclear waste repository. One borehole, WRA1, intersected several major fracture zones, and was suitable for testing quantitative permeability estimation methods. The other borehole, URL13, appeared to intersect almost no permeable fractures; it was suitable for testing methods for the characterization of rocks of very small permeability and uniform thermo-mechanical properties in a potential repository horizon. Epithermal neutron , acoustic transit time, and single-point resistance logs provided useful, qualitative indications of fractures in the extensively fractured borehole, WRA1. A single-point log indicates both weathering and the degree of opening of a fracture-borehole intersection. All logs indicate the large intervals of mechanically and geochemically uniform, unfractured granite below depths of 300 m in the relatively unfractured borehole, URL13. Some indications of minor fracturing were identified in that borehole, with one possible fracture at a depth of about 914 m, producing a major acoustic waveform anomaly. Comparison of acoustic tube-wave attenuation with models of tube-wave attenuation in infinite fractures of given aperture provide permeability estimates ranging from equivalent single-fractured apertures of less than 0.01 mm to apertures of &gt; 0.5 mm. One possible fracture anomaly in borehole URL13 at a depth of about 914 m corresponds with a thin mafic dike on the core where unusually large acoustic contrast may have produced the observed waveform anomaly. No indications of naturally occurring flow existed in borehole URL13; however, flowmeter measurements indicated flow at &lt; 0.05 L/min from the upper fracture zones in borehole WRA1 to deeper fractures at depths below 800 m. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884009","usgsCitation":"Paillet, F.L., 1988, Fracture characterization and fracture-permeability estimation at the underground research laboratory in southeastern Manitoba, Canada: U.S. Geological Survey Water-Resources Investigations Report 88-4009, 42 p. :ill. ;28 cm., https://doi.org/10.3133/wri884009.","productDescription":"42 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":124154,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4009/report-thumb.jpg"},{"id":57866,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4009/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a9025","contributors":{"authors":[{"text":"Paillet, Frederick L.","contributorId":63820,"corporation":false,"usgs":true,"family":"Paillet","given":"Frederick","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":200762,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12905,"text":"ofr88497 - 1988 - History of suspended-sediment data collection and inventory of available data for the Tennessee and Cumberland River basins","interactions":[],"lastModifiedDate":"2012-02-02T00:06:48","indexId":"ofr88497","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":"88-497","title":"History of suspended-sediment data collection and inventory of available data for the Tennessee and Cumberland River basins","docAbstract":"In 1934 and 1935, the Tennessee Valley Authority established 51 daily record suspended-sediment stations on the Tennessee River and its major tributaries. Most of these stations were operated for 8 years. From 1962 to 1965, the Tennessee Valley Authority again collected daily sediment record at 10 of the original 49 stations. In addition to the data sets collected on the major rivers, the Tennessee Valley Authority has conducted several intensive studies of small watersheds throughout the Tennessee River basin. In the Cumberland River basin, daily sediment records have been collected primarily by the Survey. Daily stations have been operated for various periods on 17 basins ranging in size from 0.67 to 1,977 sq mi, with the earliest data of daily record being October 1953. All of these daily stations are located in the upper Cumberland River basin upstream of any major impoundments. Periodic sediment data have been collected by the Survey at 194 stations in the Tennessee River basin and at 106 stations in the Cumberland River basin, however; the number of samples/station is quite low. 86% of the periodic stations in the Tennessee River basin and 91% of the periodic stations in the Cumberland River basin have 30 samples or less. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88497","usgsCitation":"Carey, W.P., Brown, R.T., and Chatham, C.G., 1988, History of suspended-sediment data collection and inventory of available data for the Tennessee and Cumberland River basins: U.S. Geological Survey Open-File Report 88-497, iv, 51 p. ill., map ;28 cm., https://doi.org/10.3133/ofr88497.","productDescription":"iv, 51 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":146187,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":989,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr88-497","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bfe0","contributors":{"authors":[{"text":"Carey, William P.","contributorId":69556,"corporation":false,"usgs":true,"family":"Carey","given":"William","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":166927,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, Russell T.","contributorId":29825,"corporation":false,"usgs":true,"family":"Brown","given":"Russell","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":166926,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chatham, Carrie G.","contributorId":89906,"corporation":false,"usgs":true,"family":"Chatham","given":"Carrie","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":166928,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":18365,"text":"ofr8927 - 1988 - Ground-water chemical evolution and diagenetic processes in the Upper Floridan aquifer, southern South Carolina and northeastern Georgia","interactions":[{"subject":{"id":18365,"text":"ofr8927 - 1988 - Ground-water chemical evolution and diagenetic processes in the Upper Floridan aquifer, southern South Carolina and northeastern Georgia","indexId":"ofr8927","publicationYear":"1988","noYear":false,"title":"Ground-water chemical evolution and diagenetic processes in the Upper Floridan aquifer, southern South Carolina and northeastern Georgia"},"predicate":"SUPERSEDED_BY","object":{"id":1096,"text":"wsp2392 - 1993 - Ground-water chemical evolution and diagenetic processes in the upper Floridan Aquifer, southern South Carolina and northeastern Georgia","indexId":"wsp2392","publicationYear":"1993","noYear":false,"title":"Ground-water chemical evolution and diagenetic processes in the upper Floridan Aquifer, southern South Carolina and northeastern Georgia"},"id":1}],"supersededBy":{"id":1096,"text":"wsp2392 - 1993 - Ground-water chemical evolution and diagenetic processes in the upper Floridan Aquifer, southern South Carolina and northeastern Georgia","indexId":"wsp2392","publicationYear":"1993","noYear":false,"title":"Ground-water chemical evolution and diagenetic processes in the upper Floridan Aquifer, southern South Carolina and northeastern Georgia"},"lastModifiedDate":"2021-01-21T19:47:56.358806","indexId":"ofr8927","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":"89-27","title":"Ground-water chemical evolution and diagenetic processes in the Upper Floridan aquifer, southern South Carolina and northeastern Georgia","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr8927","usgsCitation":"Burt, R., 1988, Ground-water chemical evolution and diagenetic processes in the Upper Floridan aquifer, southern South Carolina and northeastern Georgia: U.S. Geological Survey Open-File Report 89-27, viii, 129 p., https://doi.org/10.3133/ofr8927.","productDescription":"viii, 129 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":382412,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0027/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151761,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0027/report-thumb.jpg"}],"country":"United States","state":"Florida, Georgia, South Carolina","otherGeospatial":"Upper Floridan Aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.29608154296874,\n              31.80756092262095\n            ],\n            [\n              -81.29608154296874,\n              33.06162236089505\n            ],\n            [\n              -80.07659912109375,\n              33.06162236089505\n            ],\n            [\n              -80.07659912109375,\n              31.80756092262095\n            ],\n            [\n              -81.29608154296874,\n              31.80756092262095\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d322","contributors":{"authors":[{"text":"Burt, R.A.","contributorId":40994,"corporation":false,"usgs":true,"family":"Burt","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":178988,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55715,"text":"wdrND871 - 1988 - Water resources data, North Dakota, water year 1987","interactions":[],"lastModifiedDate":"2020-12-07T18:37:37.325801","indexId":"wdrND871","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":"ND-87-1","title":"Water resources data, North Dakota, water year 1987","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrND871","usgsCitation":"Harkness, R., Haffield, N., and Ryan, G., 1988, Water resources data, North Dakota, water year 1987: U.S. Geological Survey Water Data Report ND-87-1, xi, 392 p., https://doi.org/10.3133/wdrND871.","productDescription":"xi, 392 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,{"id":28634,"text":"wri874251 - 1988 - Channel morphology of Cottonwood Creek near Cottonwood, California, from 1940 to 1985","interactions":[],"lastModifiedDate":"2012-02-02T00:08:39","indexId":"wri874251","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":"87-4251","title":"Channel morphology of Cottonwood Creek near Cottonwood, California, from 1940 to 1985","docAbstract":"Proposed construction of two dams on Cottonwood Creek California , has caused concern that resulting streamflow modification may alter downstream channel morphology. Baseline information on Cottonwood Creek channel characteristics from 1982-83 field surveys and 1940-84 aerial photographs indicates an alluvial channel that consists of a braided inner main channel within a broader flood channel, with no clear topographic break between the main and flood channels. The braided channel is subject to large and rapid position shifts in the flood channel, which meanders within the valley fill; however, the position of the flood channel has remained relatively stable since 1940. Mean slope of Cottonwood Creek is 0.0017 and that of South Fork Cottonwood Creek is 0.0020. Fluctuations of mean bed elevation appear to be random with no apparent long-term trend of aggradation or degradation. Mean bed-material size ranged from 3 to 82 millimeters. Low-flow channel sinuosity ranged from 1.04 to 1.47 from 1940 to 1984. Cumulative lateral migration for Cottonwood Creek decreased upstream, while for South Fork, it remained relatively constant. Net lateral migration was toward the right bank on Cottonwood Creek whereas no trend in net lateral migration is apparent for the South Fork. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874251","usgsCitation":"McCaffrey, W.F., Blodgett, J.C., and Thornton, J., 1988, Channel morphology of Cottonwood Creek near Cottonwood, California, from 1940 to 1985: U.S. Geological Survey Water-Resources Investigations Report 87-4251, iv, 33 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874251.","productDescription":"iv, 33 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122671,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4251/report-thumb.jpg"},{"id":57472,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4251/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e6003","contributors":{"authors":[{"text":"McCaffrey, W. F.","contributorId":18001,"corporation":false,"usgs":true,"family":"McCaffrey","given":"W.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":200147,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blodgett, J. C.","contributorId":32154,"corporation":false,"usgs":true,"family":"Blodgett","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":200148,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thornton, J.L.","contributorId":41460,"corporation":false,"usgs":true,"family":"Thornton","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":200149,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":29113,"text":"wri874255 - 1988 - Reconnaissance investigation of water quality, bottom sediment, and biota associated with irrigation drainage in the Kendrick Reclamation Project Area, Wyoming, 1986-87","interactions":[],"lastModifiedDate":"2012-02-02T00:08:53","indexId":"wri874255","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":"87-4255","title":"Reconnaissance investigation of water quality, bottom sediment, and biota associated with irrigation drainage in the Kendrick Reclamation Project Area, Wyoming, 1986-87","docAbstract":"A reconnaissance investigation of the Kendrick Reclamation Project in central Wyoming was conducted during 1986-87 to determine if irrigation drainage has caused or has the potential to cause harmful effects on human health, fish, and wildlife, or other water uses. The investigation of the Kendrick Reclamation Project is one of nine similar investigations being conducted in the western conterminous United States as part of the Department of the Interior 's Irrigation Drainage Program. Samples of surface water were collected at 10 sites and ground water at 5 sites. Surface-water analyses included trace elements, radiochemicals, and pesticides. Concentrations in the water generally were less than national standards for public water supplies, with the exception of selenium. The median concentration of dissolved selenium was 7.5 microgm/L in 24 samples of surface and groundwater. Of the 11 samples that contained dissolved- selenium concentrations greater than the national standard for public water supplies of 10 microgm/L, 10 of the samples were collected at sites on streams that are not used for public water supplies; the eleventh sample was collected from a shallow well. Dissolved-selenium concentrations ranged from less than 1 to 300 microgm/L. Concentrations of dissolved selenium in the North Platte River, which supplies drinking water for several municipalities, ranged from less than 1 to 4 microgm/L. The dissolved-selenium concentration and selenium discharge in the North Platte River increased in the downstream direction. The four principal tributaries that receive drainage from the Kendrick Reclamation Project contributed substantially to the increase in selenium concentration and discharge in the North Platte River. Bottom-sediment samples from the North Platte River contained selenium contents of 1.2 microgm/g or less. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874255","usgsCitation":"Peterson, D.A., Jones, W.E., and Morton, A., 1988, Reconnaissance investigation of water quality, bottom sediment, and biota associated with irrigation drainage in the Kendrick Reclamation Project Area, Wyoming, 1986-87: U.S. Geological Survey Water-Resources Investigations Report 87-4255, v, 57 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874255.","productDescription":"v, 57 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159643,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4255/report-thumb.jpg"},{"id":57981,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4255/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db626d2b","contributors":{"authors":[{"text":"Peterson, D. A.","contributorId":6453,"corporation":false,"usgs":true,"family":"Peterson","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200966,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, W. E.","contributorId":39021,"corporation":false,"usgs":true,"family":"Jones","given":"W.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":200967,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morton, A.G.","contributorId":55863,"corporation":false,"usgs":true,"family":"Morton","given":"A.G.","email":"","affiliations":[],"preferred":false,"id":200968,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26868,"text":"wri874264 - 1988 - Cost-effectiveness of the streamflow-gaging program in Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:28","indexId":"wri874264","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":"87-4264","title":"Cost-effectiveness of the streamflow-gaging program in Wyoming","docAbstract":"This report documents the results of a cost-effectiveness study of the streamflow-gaging program in Wyoming. Regression analysis or hydrologic flow-routing techniques were considered for 24 combinations of stations from a 139-station network operated in 1984 to investigate suitability of techniques for simulating streamflow records. Only one station was determined to have sufficient accuracy in the regression analysis to consider discontinuance of the gage. The evaluation of the gaging-station network, which included the use of associated uncertainty in streamflow records, is limited to the nonwinter operation of the 47 stations operated by the Riverton Field Office of the U.S. Geological Survey. The current (1987) travel routes and measurement frequencies require a budget of $264,000 and result in an average standard error in streamflow records of 13.2%. Changes in routes and station visits using the same budget, could optimally reduce the standard error by 1.6%. Budgets evaluated ranged from $235,000 to $400,000. A $235,000 budget increased the optimal average standard error/station from 11.6 to 15.5%, and a $400,000 budget could reduce it to 6.6%. For all budgets considered, lost record accounts for about 40% of the average standard error. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874264","usgsCitation":"Druse, S.A., and Wahl, K., 1988, Cost-effectiveness of the streamflow-gaging program in Wyoming: U.S. Geological Survey Water-Resources Investigations Report 87-4264, iv, 35 p. :ill., map ;28 cm., https://doi.org/10.3133/wri874264.","productDescription":"iv, 35 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":123772,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4264/report-thumb.jpg"},{"id":55758,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4264/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6837af","contributors":{"authors":[{"text":"Druse, S. A.","contributorId":89934,"corporation":false,"usgs":true,"family":"Druse","given":"S.","middleInitial":"A.","affiliations":[],"preferred":false,"id":197154,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wahl, K.L.","contributorId":19598,"corporation":false,"usgs":true,"family":"Wahl","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":197153,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28974,"text":"wri884063 - 1988 - Estimates of consumptive use and ground-water return flow using water budgets in Parker Valley, Arizona and California, 1981-84","interactions":[],"lastModifiedDate":"2012-02-02T00:08:35","indexId":"wri884063","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":"88-4063","title":"Estimates of consumptive use and ground-water return flow using water budgets in Parker Valley, Arizona and California, 1981-84","docAbstract":"Annual water budgets were used to estimate consumptive use by vegetation and groundwater return flow in Parker Valley, Arizona and California. Consumptive use by vegetation was estimated to be 482,800 acre-ft in 1981, 432,000 acre-ft in 1982, 413,500 acre-ft in 1983, and 420,900 acre-ft in 1984 on the Arizona side of the Colorado River, and 45,400 acre-ft in 1984 on the California side of the river. Groundwater return flow from the area north of Tyson Wash in Arizona was estimated to be 0 acre-ft in 1981, 1983, and 1984 and 1,900 acre-ft in 1982. Water budget estimates of consumptive use by vegetation were compared to estimates of evapotranspiration. Estimates of evapotranspiration were from 1% less to 9% higher than estimates of consumptive use by vegetation in the area north of Tyson Wash. The percentage differences in the two estimates were within the measurement errors of the two major measured components in the water budget regardless of differences in year-to-year conditions. Estimates of consumptive use of Colorado River water calculated as measured diversions minus return flows were consistently lower than estimates of consumptive use by vegetation. Estimates of consumptive use of Colorado River water were from 18 to 37% lower than estimates of consumptive use by vegetation variations in tributary inflow, river stage, and induced seepage from the river to replace groundwater transpired by phreatophytes are not accounted for in the calculation. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884063","usgsCitation":"Owen-Joyce, S.J., 1988, Estimates of consumptive use and ground-water return flow using water budgets in Parker Valley, Arizona and California, 1981-84: U.S. Geological Survey Water-Resources Investigations Report 88-4063, vi, 64 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884063.","productDescription":"vi, 64 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124214,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4063/report-thumb.jpg"},{"id":57847,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4063/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcb34","contributors":{"authors":[{"text":"Owen-Joyce, Sandra J. 0000-0002-4400-5618 sjowen@usgs.gov","orcid":"https://orcid.org/0000-0002-4400-5618","contributorId":5215,"corporation":false,"usgs":true,"family":"Owen-Joyce","given":"Sandra","email":"sjowen@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":200715,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12466,"text":"ofr88159 - 1988 - U.S. Geological Survey ground-water studies in California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:46","indexId":"ofr88159","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":"88-159","title":"U.S. Geological Survey ground-water studies in California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88159","usgsCitation":"Anttila, P., 1988, U.S. Geological Survey ground-water studies in California: U.S. Geological Survey Open-File Report 88-159, 2 p. :map ;28 cm., https://doi.org/10.3133/ofr88159.","productDescription":"2 p. :map ;28 cm.","costCenters":[],"links":[{"id":146351,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0159/report-thumb.jpg"},{"id":40722,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0159/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db612a6c","contributors":{"authors":[{"text":"Anttila, P.W.","contributorId":56231,"corporation":false,"usgs":true,"family":"Anttila","given":"P.W.","email":"","affiliations":[],"preferred":false,"id":166184,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18309,"text":"ofr88146 - 1988 - U.S. Geological Survey ground-water studies in Iowa","interactions":[],"lastModifiedDate":"2016-03-11T13:03:18","indexId":"ofr88146","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":"88-146","title":"U.S. Geological Survey ground-water studies in Iowa","docAbstract":"<p>Ground water is the primary source for most water uses in Iowa. Ground-water resources supply 81 percent of the water withdrawn in Iowa for non-power-generating uses. Ground water from five principal aquifer systems is the source of drinking water for approximately 82 percent of the State's population. These aquifers range from land surface to several thousand feet below land surface. Land use in Iowa is predominately agricultural; about 93 percent of the land is farmed. 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,{"id":12894,"text":"ofr88196 - 1988 - Water-resources activities in Ohio, 1988","interactions":[],"lastModifiedDate":"2012-02-02T00:06:54","indexId":"ofr88196","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":"88-196","title":"Water-resources activities in Ohio, 1988","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88196","usgsCitation":"Camp, L., 1988, Water-resources activities in Ohio, 1988: U.S. Geological Survey Open-File Report 88-196, 2 p. :map ;28 cm., https://doi.org/10.3133/ofr88196.","productDescription":"2 p. :map ;28 cm.","costCenters":[],"links":[{"id":147317,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0196/report-thumb.jpg"},{"id":41306,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0196/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4ca3","contributors":{"authors":[{"text":"Camp, L.D.","contributorId":99568,"corporation":false,"usgs":true,"family":"Camp","given":"L.D.","email":"","affiliations":[],"preferred":false,"id":166906,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21178,"text":"ofr88162 - 1988 - U.S. Geological Survey ground-water studies in Puerto Rico","interactions":[],"lastModifiedDate":"2012-02-02T00:07:49","indexId":"ofr88162","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":"88-162","title":"U.S. Geological Survey ground-water studies in Puerto Rico","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88162","usgsCitation":"Troester, J., 1988, U.S. Geological Survey ground-water studies in Puerto Rico: U.S. Geological Survey Open-File Report 88-162, 2 p. :ill. ;28 cm., https://doi.org/10.3133/ofr88162.","productDescription":"2 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":153747,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0162/report-thumb.jpg"},{"id":50770,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0162/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a5245","contributors":{"authors":[{"text":"Troester, J.W.","contributorId":90750,"corporation":false,"usgs":true,"family":"Troester","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":183979,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27505,"text":"wri884176 - 1988 - Geology of an area near Brentwood, Williamson County, Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:08:44","indexId":"wri884176","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":"88-4176","title":"Geology of an area near Brentwood, Williamson County, Tennessee","docAbstract":"The geology and structure of an area near Brentwood, Williamson County, Tennessee, were studied to define the potential aquifers and confining units that comprise the groundwater flow system of the area. Four different formations were identified. These formations are, in descending order, the Bigby-Cannon Limestone, the Hermitage Formation, the Carters Limestone, and the Lebanon Limestone. The Bigby-Cannon Limestone and the Hermitage Formation have been affected by recent erosion. Any variation of the Carters Limestone is controlled by pre-Carters erosion of the top of the Lebanon Limestone. The thickness of this formation ranges from 65 to 79 ft. A small scale anticline-syncline pair is evident. This structure is not a result of erosion and also occurs in the T-3 bentonite bed in the Carters Limestone. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884176","usgsCitation":"Hanchar, D., 1988, Geology of an area near Brentwood, Williamson County, Tennessee: U.S. Geological Survey Water-Resources Investigations Report 88-4176, iii, 24 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884176.","productDescription":"iii, 24 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":2144,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri884176/","linkFileType":{"id":5,"text":"html"}},{"id":124121,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_88_4176.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683ad6","contributors":{"authors":[{"text":"Hanchar, D. W.","contributorId":87986,"corporation":false,"usgs":true,"family":"Hanchar","given":"D. W.","affiliations":[],"preferred":false,"id":198227,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27714,"text":"wri884058 - 1988 - Calibration and standardization of geophysical well-logging equipment for hydrologic applications","interactions":[],"lastModifiedDate":"2012-02-02T00:08:38","indexId":"wri884058","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":"88-4058","title":"Calibration and standardization of geophysical well-logging equipment for hydrologic applications","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri884058","usgsCitation":"Hodges, R., 1988, Calibration and standardization of geophysical well-logging equipment for hydrologic applications: U.S. Geological Survey Water-Resources Investigations Report 88-4058, iv, 25 p. :ill. ;28 cm., https://doi.org/10.3133/wri884058.","productDescription":"iv, 25 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":119790,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4058/report-thumb.jpg"},{"id":56558,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4058/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f95bd","contributors":{"authors":[{"text":"Hodges, R.E.","contributorId":45350,"corporation":false,"usgs":true,"family":"Hodges","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":198577,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21450,"text":"ofr88314 - 1988 - National research program: Ground-water perspective","interactions":[],"lastModifiedDate":"2019-11-25T14:19:36","indexId":"ofr88314","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":"88-314","title":"National research program: Ground-water perspective","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr88314","usgsCitation":"Wolff, R.G., Stephens, J.C., and Friedman, L., 1988, National research program: Ground-water perspective: U.S. Geological Survey Open-File Report 88-314, 2 p. , https://doi.org/10.3133/ofr88314.","productDescription":"2 p. ","costCenters":[],"links":[{"id":369562,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0314/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153635,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0314/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698383","contributors":{"authors":[{"text":"Wolff, Roger G.","contributorId":19580,"corporation":false,"usgs":true,"family":"Wolff","given":"Roger","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":184448,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stephens, Jerry C.","contributorId":81493,"corporation":false,"usgs":true,"family":"Stephens","given":"Jerry","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":184449,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Friedman, Linda C.","contributorId":98702,"corporation":false,"usgs":true,"family":"Friedman","given":"Linda C.","affiliations":[],"preferred":false,"id":184450,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":57625,"text":"wdrFL873A - 1988 - Water resources data for Florida, water year 1987. Volume 3A. Southwest Florida-surface water","interactions":[],"lastModifiedDate":"2025-02-10T14:50:33.573549","indexId":"wdrFL873A","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-87-3A","title":"Water resources data for Florida, water year 1987. Volume 3A. Southwest Florida-surface water","docAbstract":"<p>Water resources data for the 1987 water year in Florida consist 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; continuous 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 southwest Florida include records of stage, discharge and water quality of streams; stage, contents, water quality of lakes and reservoirs, and water levels and water quality of ground-water wells. Volume 3A contains continuous or daily discharge for 61 streams, periodic discharge for 5 streams, miscellaneous discharge for 4 streams, continuous daily stage for 22 streams, periodic stage for 2 streams, peak discharge for 16 streams, continuous daily tide stage for 10 sites, continuous elevation for 22 lakes and periodic elevation for 16 lakes, and quality-of-water for 80 surface-water sites.</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/wdrFL873A","collaboration":"Prepared in cooperation with the State of Florida and with other agencies","usgsCitation":"Fletcher, W., White, R., Coston, V., and Todd, J., 1988, Water resources data for Florida, water year 1987. Volume 3A. 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,{"id":25706,"text":"wri884115 - 1988 - Phytoplankton populations in lakes in Loch Vale, Rocky Mountain National Park, Colorado: Sensitivity to acidic conditions and nitrate enrichment","interactions":[],"lastModifiedDate":"2020-11-09T17:40:24.076318","indexId":"wri884115","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":"88-4115","title":"Phytoplankton populations in lakes in Loch Vale, Rocky Mountain National Park, Colorado: Sensitivity to acidic conditions and nitrate enrichment","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri884115","usgsCitation":"McKnight, D.M., Miller, C., Smith, R., Baron, J., and Spaulding, S.A., 1988, Phytoplankton populations in lakes in Loch Vale, Rocky Mountain National Park, Colorado: Sensitivity to acidic conditions and nitrate enrichment: U.S. Geological Survey Water-Resources Investigations Report 88-4115, vi, 102 p., https://doi.org/10.3133/wri884115.","productDescription":"vi, 102 p.","costCenters":[{"id":40553,"text":"WMA - Office of the Chief Operating Officer","active":true,"usgs":true}],"links":[{"id":156914,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Rocky Mountain National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.6745719909668,\n              40.282144825334825\n            ],\n            [\n              -105.63457489013672,\n              40.282144825334825\n            ],\n            [\n              -105.63457489013672,\n              40.309247135103334\n            ],\n            [\n              -105.6745719909668,\n              40.309247135103334\n            ],\n            [\n              -105.6745719909668,\n              40.282144825334825\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68591d","contributors":{"authors":[{"text":"McKnight, Diane M.","contributorId":59773,"corporation":false,"usgs":false,"family":"McKnight","given":"Diane","email":"","middleInitial":"M.","affiliations":[{"id":16833,"text":"INSTAAR, University of Colorado","active":true,"usgs":false}],"preferred":false,"id":194739,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Christine","contributorId":21582,"corporation":false,"usgs":true,"family":"Miller","given":"Christine","affiliations":[],"preferred":false,"id":194740,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, Richard","contributorId":34172,"corporation":false,"usgs":true,"family":"Smith","given":"Richard","email":"","affiliations":[],"preferred":false,"id":194741,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Baron, Jill 0000-0002-5902-6251 jill_baron@usgs.gov","orcid":"https://orcid.org/0000-0002-5902-6251","contributorId":194124,"corporation":false,"usgs":true,"family":"Baron","given":"Jill","email":"jill_baron@usgs.gov","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":194742,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Spaulding, Sarah A. 0000-0002-9787-7743 sspaulding@usgs.gov","orcid":"https://orcid.org/0000-0002-9787-7743","contributorId":1157,"corporation":false,"usgs":true,"family":"Spaulding","given":"Sarah","email":"sspaulding@usgs.gov","middleInitial":"A.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":true,"id":194743,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":4705,"text":"twri06A1 - 1988 - A modular three-dimensional finite-difference ground-water flow model","interactions":[{"subject":{"id":20038,"text":"ofr83875 - 1984 - A modular three-dimensional finite-difference ground-water flow model","indexId":"ofr83875","publicationYear":"1984","noYear":false,"title":"A modular three-dimensional finite-difference ground-water flow model"},"predicate":"SUPERSEDED_BY","object":{"id":4705,"text":"twri06A1 - 1988 - A modular three-dimensional finite-difference ground-water flow model","indexId":"twri06A1","publicationYear":"1988","noYear":false,"title":"A modular three-dimensional finite-difference ground-water flow model"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:31","indexId":"twri06A1","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":"06-A1","title":"A modular three-dimensional finite-difference ground-water flow model","docAbstract":"This report presents a finite-difference model and its associated modular computer program. The model simulates flow in three dimensions. The report includes detailed explanations of physical and mathematical concepts on which the model is based and an explanation of how those concepts are incorporated in the modular structure of the computer program. The modular structure consists of a Main Program and a series of highly independent subroutines called 'modules.' The modules are grouped into 'packages.' Each package deals with a specific feature of the hydrologic system which is to be simulated, such as flow from rivers or flow into drains, or with a specific method of solving linear equations which describe the flow system, such as the Strongly Implicit Procedure or Slice-Successive Overrelaxation. \r\n\r\nThe division of the program into modules permits the user to examine specific hydrologic features of the model independently. This also facilita development of additional capabilities because new packages can be added to the program without modifying the existing packages. The input and output systems of the computer program are also designed to permit maximum flexibility. \r\n\r\nGround-water flow within the aquifer is simulated using a block-centered finite-difference approach. Layers can be simulated as confined, unconfined, or a combination of confined and unconfined. Flow associated with external stresses, such as wells, areal recharge, evapotranspiration, drains, and streams, can also be simulated. The finite-difference equations can be solved using either the Strongly Implicit Procedure or Slice-Successive Overrelaxation. \r\n\r\nThe program is written in FORTRAN 77 and will run without modification on most computers that have a FORTRAN 77 compiler. For each program ,module, this report includes a narrative description, a flow chart, a list of variables, and a module listing.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/twri06A1","issn":"0565-596X","usgsCitation":"McDonald, M.G., and Harbaugh, A.W., 1988, A modular three-dimensional finite-difference ground-water flow model: U.S. Geological Survey Techniques of Water-Resources Investigations 06-A1, 586 p. :ill. ;28 cm., https://doi.org/10.3133/twri06A1.","productDescription":"586 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":139143,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":295,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri6a1/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae07b","contributors":{"authors":[{"text":"McDonald, Michael G.","contributorId":47352,"corporation":false,"usgs":true,"family":"McDonald","given":"Michael","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":149652,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harbaugh, Arlen W. harbaugh@usgs.gov","contributorId":426,"corporation":false,"usgs":true,"family":"Harbaugh","given":"Arlen","email":"harbaugh@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":149651,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2394,"text":"wsp2333 - 1988 - Tritium migration from a low-level radioactive-waste disposal site near Chicago, Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:05:33","indexId":"wsp2333","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2333","title":"Tritium migration from a low-level radioactive-waste disposal site near Chicago, Illinois","docAbstract":"This paper describes the results of a study to determine the geologic and hydrologic factors that control migration of tritium from a closed, low-level radioactive-waste disposal site. The disposal site, which operated from 1943 to mid1949, contains waste generated by research activities at the world's first nuclear reactors. Tritium has migrated horizontally at least 1,300 feet northward in glacial drift and more than 650 feet in the underlying dolomite. Thin, gently sloping sand layers in an otherwise clayey glacial drift are major conduits for ground-water flow and tritium migration in a perched zone beneath the disposal site. Tritium concentrations in the drift beneath the disposal site exceed 100,000 nanocuries per liter. Regional horizontal joints in the dolomite are enlarged by solution and are the major conduits for ground-water flow and tritium migration in the dolomite. A weathered zone at the top of the dolomite also is a pathway for tritium migration. The maximum measured tritium concentration in the dolomite is 29.4 nanocuries per liter. Fluctuations of tritium concentration in the dolomite are the result of dilution by seasonal recharge from the drift.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2333","usgsCitation":"Nicholas, J., and Healy, R.W., 1988, Tritium migration from a low-level radioactive-waste disposal site near Chicago, Illinois: U.S. Geological Survey Water Supply Paper 2333, iv, 46 p. :ill., maps ;28 cm., https://doi.org/10.3133/wsp2333.","productDescription":"iv, 46 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":139189,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2333/report-thumb.jpg"},{"id":28371,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2333/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db624515","contributors":{"authors":[{"text":"Nicholas, J.R.","contributorId":26673,"corporation":false,"usgs":true,"family":"Nicholas","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":145129,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Healy, R. W.","contributorId":89872,"corporation":false,"usgs":true,"family":"Healy","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":145130,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25386,"text":"wri854127 - 1988 - Alternative sources of large seasonal ground-water supplies in the headwaters of the Susquehanna River basin, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:08:29","indexId":"wri854127","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":"85-4127","title":"Alternative sources of large seasonal ground-water supplies in the headwaters of the Susquehanna River basin, New York","docAbstract":"The northern divide of the Susquehanna River basin crosses 29 broad valleys that contain thick glacial deposits but are drained only by small headwater streams. Much groundwater could be withdrawn from sand and gravel deposits in these valleys with little immediate effect on streamflow. A digital model of the headwater reach of one typical valley suggests that pumping 10.8 million gal/day for 2 months every summer would lower the water table as much as 33 ft, cause the upper 1,900 ft of the stream draining the valley to go dry, and reduce streamflow downvalley by 1.2 million gal/day by the time pumping ceased. Saturated thickness of surficial sand and gravel exceeds 40 ft in about half the headwater valley reaches; the valley floor areas range from 0.2 to 9 sq mi. Seepage losses from small streams that carry runoff from adjacent till-covered uplands are a major source of recharge to aquifers in these valleys under natural conditions and would increase if the water table were lowered by seasonal withdrawals. Some aquifers beneath extensive clay layers in these and other valleys of the Susquehanna River basin may be partially independent of streams but not easily evaluated. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854127","usgsCitation":"Randall, A., Snavely, D.S., Holecek, T., and Waller, R., 1988, Alternative sources of large seasonal ground-water supplies in the headwaters of the Susquehanna River basin, New York: U.S. Geological Survey Water-Resources Investigations Report 85-4127, v, 121 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854127.","productDescription":"v, 121 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122814,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4127/report-thumb.jpg"},{"id":54120,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4127/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adde4b07f02db686aed","contributors":{"authors":[{"text":"Randall, A. D.","contributorId":81077,"corporation":false,"usgs":true,"family":"Randall","given":"A. D.","affiliations":[],"preferred":false,"id":193479,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snavely, D. S.","contributorId":103692,"corporation":false,"usgs":true,"family":"Snavely","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":193480,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Holecek, T.P.","contributorId":76358,"corporation":false,"usgs":true,"family":"Holecek","given":"T.P.","email":"","affiliations":[],"preferred":false,"id":193478,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Waller, R.M.","contributorId":13659,"corporation":false,"usgs":true,"family":"Waller","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":193477,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":57460,"text":"wdrMT871 - 1988 - Water resources data for Montana, water year 1987. Volume 1. Hudson Bay and Missouri River Basins","interactions":[],"lastModifiedDate":"2020-08-21T18:17:43.971056","indexId":"wdrMT871","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":"MT-87-1","title":"Water resources data for Montana, water year 1987. Volume 1. Hudson Bay and Missouri River Basins","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrMT871","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1988, Water resources data for Montana, water year 1987. Volume 1. 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