{"pageNumber":"1279","pageRowStart":"31950","pageSize":"25","recordCount":46734,"records":[{"id":27199,"text":"wri964101 - 1996 - Nutrient sources and analysis of nutrient water-quality data, Apalachicola-Chattahoochee-Flint River basin, Georgia, Alabama, and Florida, 1972-90","interactions":[],"lastModifiedDate":"2023-01-11T22:26:31.883944","indexId":"wri964101","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-4101","title":"Nutrient sources and analysis of nutrient water-quality data, Apalachicola-Chattahoochee-Flint River basin, Georgia, Alabama, and Florida, 1972-90","docAbstract":"<p>In 1991, the U.S. Geological Survey began full-scale implementation of the National Water-Quality Assessment (NAWQA) program. One of the initial tasks of the NAWQA program is to compile and evaluate existing data from individual study units. Available nutrient data from 1972 through 1990 water years were used to estimate nutrient sources to the Apalachicola–Chattahoochee–Flint (ACF) River basin and describe the presence, distribution, and transport of nutrients in surface and ground waters.</p><p>In 1990, about 2,500 tons of nitrogen and 1,100 tons of phosphorus were discharged as point-source loads by 127 municipal wastewater-treatment facilities&nbsp;(WWTF). Nonpoint-source inputs, an unknown percentage of which entered the hydrologic system, included about 120,000 tons of nitrogen and 28,000 tons of phosphorus from animal manure; 82,000 tons of nitrogen and 20,000 tons of phosphorus&nbsp;applied as fertilizer; and 24,000 tons of nitrogen from atmospheric deposition. Estimates of nutrient input to the ACF River basin were not made for natural sources and for the following anthropogenic sources: industrial-wastewater effluent; storm drains; sanitary and combined sewer outflows; and runoff from agricultural, urban, and suburban areas. Nutrient outflow from the Apalachicola River into Apalachicola Bay, Fla., was about 13 percent of estimated&nbsp;nitrogen sources and about 3 percent of estimated&nbsp;total-phosphorus sources in the ACF River basin.</p><p>For 1972–90, nutrient concentrations in surface water were high enough to warrant concerns about accelerated eutrophication based on total-phosphorus concentrations and to warrant concerns intermittently about toxicity to fish based on dissolved-ammonia concentrations downstream of wastewater-treatment outfalls from Metropolitan Atlanta and LaGrange, Ga. Many improvements to the water quality of the Chattahoochee&nbsp;and Flint Rivers in the 1980’s and early 1990’s can be directly attributed to improvements in WWTF, legislation directed at decreasing point-source loads of phosphorus, and changes in locations of wastewater-treatment outfalls. However, limited data indicate that nonpoint-source inputs increased upstream of Atlanta and in the Chipola River watershed.</p><p>Significant increases in nutrient concentrations, loads, and yields occurred from upstream to downstream of the metropolitan areas of Atlanta, Ga.; Columbus, Ga., and Phenix City, Ala.; and Albany, Ga. The highest mean-annual yields estimated in the ACF River basin for total nitrogen (2.9 tons per square mile (tons/mi<sup>2</sup>)), total-inorganic nitrogen (2.0 tons/mi<sup>2</sup>), dissolved ammonia (1.1 tons/mi<sup>2</sup>), and total phosphorus (0.75 tons/mi<sup>2</sup>) were downstream of Atlanta.</p><p>Most significant trends in nutrient-concentration data from 1980–90 in the Chattahoochee River and the Middle and Lower Flint River basins were increasing, except dissolved ammonia which decreased at several sampling sites in reaches downstream of Atlanta, Columbus and Phenix City, and Albany. At sampling sites on the Chattahoochee and Flint Rivers downstream of Atlanta and Albany, decreasing trends in dissolved-ammonia concentration and increasing trends in dissolved-nitrate concentration were the result&nbsp;of improved wastewater treatment at WWTF. Dissolved-ammonia concentrations decreased and dissolved-nitrate concentrations increased along river reaches downstream of wastewater-treatment facility outfalls for Atlanta and Albany because of nitrification&nbsp;of ammonia to nitrate. Increasing trends in total-phosphorus concentrations are an accurate representation of data for the period 1980–90. However, legislated restrictions on the use of phosphate detergents and improvements to WWTF in the late 1980’s and early 1990’s, resulted in substantial&nbsp;reductions of phosphorus concentrations in&nbsp;wastewater effluent and in rivers at many locations in the 1990’s.</p><p>Reservoirs affect nutrient transport because of uptake by phytoplankton and aquatic plants, denitrification,and accumulation of phosphorus associated with sediment in reservoirs. Yields of total-inorganic nitrogen, dissolved ammonia, dissolved nitrate, and total phosphorus decreased between sampling sites upstream and downstream of four reservoirs on the Chattahoochee River. The only exception was the yield of dissolved ammonia increased slightly from upstream to downstream of Lake Sidney Lanier. Much of the nutrient load in the Chattahoochee River downstream of Atlanta is utilized by algae or settles out primarily in West Point Lake, and to a lesser extent, in Lake Harding and Walter F. George Reservoir.&nbsp;In general, the Flint River arm of Lake Seminole had significantly higher concentrations of nutrients than the Chattahoochee River arm of Lake Seminole, which may be the result of the large percentage&nbsp;of the Middle and Lower Chattahoochee River in backwater from reservoirs, the absence of reservoirs on the Flint River downstream of Albany until Lake Seminole, and nonpoint-source inputs of nutrients from intensively farmed areas in the Lower Flint River basin. Decreases in dissolved-ammonia, dissolved-nitrate, and total-phosphorus concentrations in reservoirs and backwater along the Chattahoochee&nbsp;River from West Point Lake to Lake Seminole during summer months are related to the seasonality of phytoplankton production.</p><p>The Chipola River had the highest yields of dissolved nitrate (1.2 tons/mi<sup>2</sup>) estimated in the ACF River basin. Estimated loads of dissolved nitrate increased fairly steadily from 500 to 1,500 tons per year from 1972–90. These factors strongly suggest an agricultural nonpoint source of elevated dissolved-nitrate concentrations from increased irrigated agriculture and fertilizer applications in the Chipola River watershed.</p><p>Analyses of nutrients in ground water within the ACF River basin for 1972–90 water years were restricted because of limited available data. The distribution of nitrate concentrations in the ACF River basin for 1972–90 water years included 10 percent of wells and 6 percent of springs with concentrations that probably have elevated nitrate concentrations (3.1 to 10 milligrams per liter (mg/L)), and 1 percent of wells with median nitrate concentrations exceeding the maximum contaminant level of 10 mg/L. Dissolved-nitrate concentrations were significantly lower in the Providence aquifer than in the Floridan aquifer system and the crystalline-rock aquifers. Dissolved-nitrate concentrations in wells used for public supply were significantly lower than in wells used for domestic use or unused wells.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri964101","usgsCitation":"Frick, E.A., Buell, G.R., and Hopkins, E.H., 1996, Nutrient sources and analysis of nutrient water-quality data, Apalachicola-Chattahoochee-Flint River basin, Georgia, Alabama, and Florida, 1972-90: U.S. Geological Survey Water-Resources Investigations Report 96-4101, ix, 120 p., https://doi.org/10.3133/wri964101.","productDescription":"ix, 120 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":121496,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_96_4101.jpg"},{"id":411753,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48459.htm","linkFileType":{"id":5,"text":"html"}},{"id":2141,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri96-4101/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alabama, Florida, Georgia","otherGeospatial":"Apalachicola-Chattahoochee-Flint River basin","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"properties\":{},\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-84.869384765625,29.878755346037977],[-84.9847412109375,29.673735421779128],[-85.2044677734375,29.73099249532227],[-85.4241943359375,30.012030680358613],[-85.49011230468749,30.552800413453546],[-85.49560546875,32.16166284018013],[-85.27587890625,33.5963189611327],[-84.72656249999999,34.17090836352573],[-83.924560546875,34.6241677899049],[-83.64990234375,34.89494244739732],[-83.34228515625,34.56990638085636],[-83.583984375,33.8521697014074],[-84.375,33.22030778968541],[-83.73779296875,31.96148355726853],[-84.05639648437499,30.911651004518244],[-84.5068359375,30.64736425824319],[-84.869384765625,29.878755346037977]]]}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696749","contributors":{"authors":[{"text":"Frick, Elizabeth A.","contributorId":98714,"corporation":false,"usgs":true,"family":"Frick","given":"Elizabeth","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":197723,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buell, Gary R. grbuell@usgs.gov","contributorId":3107,"corporation":false,"usgs":true,"family":"Buell","given":"Gary","email":"grbuell@usgs.gov","middleInitial":"R.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":197721,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hopkins, Evelyn H.","contributorId":59025,"corporation":false,"usgs":true,"family":"Hopkins","given":"Evelyn","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":197722,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30305,"text":"wri964061 - 1996 - Hydrogeology and simulation of ground-water flow, Picatinny Arsenal and vicinity, Morris County, New Jersey","interactions":[],"lastModifiedDate":"2019-12-07T09:48:02","indexId":"wri964061","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-4061","title":"Hydrogeology and simulation of ground-water flow, Picatinny Arsenal and vicinity, Morris County, New Jersey","docAbstract":"Ground-water flow in glacial sediments and bedrock at Picatinny Arsenal, N.J., was simulated by use of a three-dimensional finite-difference ground- water-flow model. The modeled area includes a 4.3-square-mile area that extends from Picatinny Lake to the Rockaway River. Most of the study area is bounded by the natural hydrologic boundaries of the ground-water system. eophysical logs, lithologic logs, particle-size data, and core data from selected wells and surface geophysical data were analyzed to define the hydrogeologic framework. Hydrogeologic sections and thickness maps define six permeable and three low-permeability layers that are represented in the model as aquifers and confining units, respectively. Hydrologic data incorporated in the model include a rate of recharge from precipitation of 22 inches per year, estimated from long-term precipitation records and estimates of evapotranspiration. Additional recharge from infiltration along valleys was estimated from measured discharge of springs along the adjacent valley walls and from estimates of runoff from upland drainage that flows to the valley floor. Horizontal and vertical hydraulic conductivities of permeable and low-permeability layers were estimated from examination of aquifer-test data, gamma-ray logs, borehole cuttings, and previously published data. Horizontal hydraulic conductivities in glacial sediments range from 10 to 380 feet per day. Vertical hydraulic conductivities of the low-permeability layers range from 0.01 to 0.7 feet per day. The model was calibrated by simulating steady-state conditions during 1989-93 and by closely matching simulated and measured ground-water levels, vertical ground-water-head differences, and streamflow gain and loss. Simulated steady-state potentiometric- surface maps produced for the six permeable layers indicate that ground water in the unconfined material within Picatinny Arsenal flows predominantly toward the center of the valley, where it discharges to Green Pond Brook. Beneath the upper confining unit, ground water flows southwestward, down the valley. Between First Street and Farley Avenue, the upper confining unit pinches out near the valley walls, resulting in a major input of water to, and causing a local potentiometric high in, the underlying aquifer layers. Ground-water-flow directions southwest of the southern arsenal boundary are predominantly to the Rockaway River.","language":"English","publisher":"U.S. Geological Survey ","publisherLocation":"Reston, VA","doi":"10.3133/wri964061","usgsCitation":"Voronin, L., and Rice, D., 1996, Hydrogeology and simulation of ground-water flow, Picatinny Arsenal and vicinity, Morris County, New Jersey: U.S. Geological Survey Water-Resources Investigations Report 96-4061, vi, 64 p., https://doi.org/10.3133/wri964061.","productDescription":"vi, 64 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":123662,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4061/report-thumb.jpg"},{"id":59097,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1996/4061/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59098,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4061/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Jersey","county":"Morris 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L. M.","contributorId":93486,"corporation":false,"usgs":true,"family":"Voronin","given":"L. M.","affiliations":[],"preferred":false,"id":203026,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rice, D.E.","contributorId":44188,"corporation":false,"usgs":true,"family":"Rice","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":203025,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29337,"text":"wri964038C - 1996 - Benthic invertebrates of benchmark streams in agricultural areas of eastern Wisconsin — Western Lake Michigan drainages","interactions":[],"lastModifiedDate":"2022-01-21T21:01:57.760672","indexId":"wri964038C","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-4038","chapter":"C","title":"Benthic invertebrates of benchmark streams in agricultural areas of eastern Wisconsin — Western Lake Michigan drainages","docAbstract":"<p>This study describes the benthic invertebrate communities of 20 benchmark streams in agricultural areas of eastern Wisconsin. Streams with minimal adverse effects from human activity were selected from four agricultural areas with differing surficial deposits and bedrock types (relatively homogeneous units, or RHU's). Most aquatic invertebrate orders were well represented in the 20 benchmark stream samples; 217 species and 151 genera within 56 families were identified. Diptera was the best represented order (96 species), followed by Trichoptera (42 species) and Ephemeroptera (26 species). Diptera were the most abundant organisms in terms of numbers of individuals in the sample (28 percent of the total) followed by Trichoptera (25 percent) and Ephemeroptera (13 percent). Nine species of freshwater mussels were found, but only in 5 of the 20 benchmark streams.</p>\n<p>Community measures were calculated for the following: total number of individuals; number of species; number of families; Margalef's diversity index; percent dominant family; percent Ephemeroptera-Plecoptera-Trichoptera (EPT); ratio of EPT to Chironomidae; percent shredders; ratio of scrapers to collectors-gatherers-filterers; Hilsenhoff's Biotic Index; Hilsenhoff's family level biotic index; and mean tolerance value. The S AS statistical software package was used for calculations of variance and correlations, normality checks, and principal components analysis of these measures and to find relations between benthic-invertebrate data and environmental-setting, habitat, and water-quality data.</p>\n<p>Coefficients of variation within the RHU's were as great or greater than those for all 20 streams for most measures and RHU's. The specific taxa assemblages present at the sites did not show distinct differences between RHU's or similarities within the RHU's. The covariance and the Kruskal-Wallis tests showed that the benthic invertebrate measures were not related to RHU. These results all indicate that the combined effect of the RHU variables (bedrock geology, texture of surficial deposits, and land use/land cover) were not elemental in describing invertebrate communities in the study-area streams.</p>\n<p>A principal components analysis (PCA) was done on the 20 benchmark streams which used the invertebrate population measures as variables. A three-dimensional ordination plot of these components revealed that 18 of the 20 streams could be divided into three groups relative to stream size, available habitat, and water quality. The three classifications of streams include large, warmer streams with slight pollution; deep, mixed-water streams with minimal pollution; and small, cold, pristine headwater streams. The two streams not defined by the three PCA groupings were not suitable to represent benchmark conditions. One site lacked suitable quality habitat or sufficient nutrients to support a healthy population of invertebrates, causing low measures of diversity. The other site appeared to be affected by sedimentation and low flows.</p>\n<p>The classification groupings did not show any significant relations to percentage agricultural land use. Percentage of agricultural land use varied greatly within each group and the means for each group were similar. All streams in this study had some level of protection from agricultural practices in their basins. Although the intensity of agriculture is known to be a factor causing deterioration of invertebrate populations in past studies, the finding in this study indicated that the level of protection the stream received and other factors such as environmental setting and habitat could be more important to benthic invertebrates than the percentage of agriculture in the basin.</p>\n<p>Information gathered from these benchmark streams can be used as a regional reference for comparison with other streams in agricultural areas, based on communities of aquatic biota, habitat, and water quality.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri964038C","usgsCitation":"Rheaume, S.J., Lenz, B.N., and Scudder, B.C., 1996, Benthic invertebrates of benchmark streams in agricultural areas of eastern Wisconsin — Western Lake Michigan drainages: U.S. Geological Survey Water-Resources Investigations Report 96-4038, vi, 39 p., https://doi.org/10.3133/wri964038C.","productDescription":"vi, 39 p.","numberOfPages":"46","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":394722,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48405.htm"},{"id":58180,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4038c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119051,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4038c/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","otherGeospatial":"Lake Michigan","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.483642578125,\n              43.1090040242731\n            ],\n            [\n              -89.483642578125,\n              45.46783598133375\n            ],\n            [\n              -86.737060546875,\n              45.46783598133375\n            ],\n            [\n              -86.737060546875,\n              43.1090040242731\n            ],\n            [\n              -89.483642578125,\n              43.1090040242731\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b4bb","contributors":{"authors":[{"text":"Rheaume, S. J.","contributorId":70804,"corporation":false,"usgs":true,"family":"Rheaume","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":201366,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lenz, B. N.","contributorId":106164,"corporation":false,"usgs":true,"family":"Lenz","given":"B.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":201368,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Scudder, B. C.","contributorId":71588,"corporation":false,"usgs":true,"family":"Scudder","given":"B.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":201367,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26472,"text":"wri964050 - 1996 - Ground-water hydrology, historical water use, and simulated ground-water flow in Cretaceous-age Coastal Plain aquifers near Charleston and Florence, South Carolina","interactions":[],"lastModifiedDate":"2019-12-30T12:53:36","indexId":"wri964050","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-4050","title":"Ground-water hydrology, historical water use, and simulated ground-water flow in Cretaceous-age Coastal Plain aquifers near Charleston and Florence, South Carolina","docAbstract":"A quasi-three-dimensional, transient, digital, ground-water flow model representing the Coastal Plain aquifers of South Carolina, has been constructed to assist in defining the ground- water-flow system of Cretaceous aquifers near Charleston and Florence, S.C. Both cities are near the centers of large (greater than 150 feet) potentiometric declines in the Middendorf aquifer. In 1989, the diameter of the depressions was approximately 40 miles at Charleston and 15 miles at Florence. The potentiometric decline occurred between predevelopment (1926) and 1982 near Florence, and between predevelopment (1879) and 1989 near Charleston. The city of Charleston does not withdraw water from these aquifers; however, some of the small communities in the area use these aquifers for a potable water supply. The model simulates flow in and between four aquifer systems. The model has a variable-cell-size grid, and spans the Coastal Plain from the Savannah River in the southwest to the Cape Fear Arch in the northeast, and from the Fall Line in the northwest to approximately 30 miles offshore to the southeast. Model-grid cell size is 1 by 1 mile in a 48 by 48 mile area centered in Charleston, and in a 36 by 48 mile area centered in Florence. The model cell size gradually increases to a maximum of 4 by 4 miles outside the two study areas. The entire grid consists of 115 by 127 cells and covers an area of 39,936 square miles. The model was calibrated to historical water-level data. The calibration relied on three techniques: (1) matching simulated and observed potentiometric map surfaces, (2) statistical comparison of observed and simulated heads, and (3) comparison of observed and simulated well hydrographs. Systematic changes in model parameters showed that simulated heads are most sensitive to changes in aquifer transmissivity. Eight predictive ground-water-use scenarios were simulated for the Mount Pleasant area, which presently (1993) uses the Middendorf aquifer as a sole-source of potable water. These simulations use various combinations of spatial distribution, and injection of treated wastewater effluent for existing and future Middendorf aquifer wells.","language":"English","publisher":"U.S. Geological Survey ","doi":"10.3133/wri964050","usgsCitation":"Campbell, B.G., and van Heeswijk, M., 1996, Ground-water hydrology, historical water use, and simulated ground-water flow in Cretaceous-age Coastal Plain aquifers near Charleston and Florence, South Carolina: U.S. Geological Survey Water-Resources Investigations Report 96-4050, viii, 100 p. , https://doi.org/10.3133/wri964050.","productDescription":"viii, 100 p. ","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":55291,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4050/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124971,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4050/report-thumb.jpg"}],"country":"United States","state":"South Carolina","city":"Charleston, Florence","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.18920898437499,\n              32.59310597426537\n            ],\n            [\n              -79.65087890624999,\n              32.59310597426537\n            ],\n            [\n              -79.65087890624999,\n              33.03169299978312\n            ],\n            [\n              -80.18920898437499,\n              33.03169299978312\n            ],\n            [\n              -80.18920898437499,\n              32.59310597426537\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.013427734375,\n              34.043556504127444\n            ],\n            [\n              -79.6014404296875,\n              34.043556504127444\n            ],\n            [\n              -79.6014404296875,\n              34.334364487026306\n            ],\n            [\n              -80.013427734375,\n              34.334364487026306\n            ],\n            [\n              -80.013427734375,\n              34.043556504127444\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b10cb","contributors":{"authors":[{"text":"Campbell, B. G.","contributorId":68764,"corporation":false,"usgs":true,"family":"Campbell","given":"B.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":196453,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"van Heeswijk, Marijke heeswijk@usgs.gov","contributorId":1537,"corporation":false,"usgs":true,"family":"van Heeswijk","given":"Marijke","email":"heeswijk@usgs.gov","affiliations":[],"preferred":true,"id":196452,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30515,"text":"wri964148 - 1996 - Evaluation of quality assurance/quality control data collected by the U.S. Geological Survey for water-quality activities at the Idaho National Engineering Laboratory, Idaho, 1989 through 1993","interactions":[],"lastModifiedDate":"2022-01-11T20:58:51.986624","indexId":"wri964148","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-4148","title":"Evaluation of quality assurance/quality control data collected by the U.S. Geological Survey for water-quality activities at the Idaho National Engineering Laboratory, Idaho, 1989 through 1993","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri964148","usgsCitation":"Williams, L.M., 1996, Evaluation of quality assurance/quality control data collected by the U.S. Geological Survey for water-quality activities at the Idaho National Engineering Laboratory, Idaho, 1989 through 1993: U.S. Geological Survey Water-Resources Investigations Report 96-4148, ix, 116 p., https://doi.org/10.3133/wri964148.","productDescription":"ix, 116 p.","costCenters":[],"links":[{"id":394214,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48494.htm"},{"id":59297,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4148/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119679,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4148/report-thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Idaho National Engineering Laboratory","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.3042,\n              43.2167\n            ],\n            [\n              -112.5,\n              43.2167\n            ],\n            [\n              -112.5,\n              43.9333\n            ],\n            [\n              -113.3042,\n              43.9333\n            ],\n            [\n              -113.3042,\n              43.2167\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fabeb","contributors":{"authors":[{"text":"Williams, L. M.","contributorId":63045,"corporation":false,"usgs":true,"family":"Williams","given":"L.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":203383,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44736,"text":"wri944198 - 1996 - Atlas of ground-water resources in Puerto Rico and the U.S. Virgin Islands","interactions":[],"lastModifiedDate":"2016-05-13T14:29:39","indexId":"wri944198","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"94-4198","title":"Atlas of ground-water resources in Puerto Rico and the U.S. Virgin Islands","docAbstract":"<p>This atlas presents an overview of the ground-water resources of the main island of Puerto Rico; two of its larger offshore islands, Isla de Culebra and Isla de Vieques; and the three principal islands of the U.S. Virgin Islands, St. Thomas, St. John, and St. Croix. The atlas presents the most important ground-water information available for these islands, and is written for water managers and the general public. It describes, through the use of maps, graphs, and hydrogeologic sections, the most important aspects of the geohydrology, ground-water flow system, and groundwater withdrawals for the principal aquifers in these islands. Most of the information presented in the atlas is from published reports, although unpublished data from ongoing studies by the U.S. Geological Survey were used to prepare parts of the atlas. This report provides a useful compilation of information concerning major aquifers in Puerto Rico and the U.S. Virgin Islands and provides a first step in gaining a general knowledge of these aquifers. More detailed information is available from the primary sources referenced in the report. The atlas contains an introductory section and 15 sections describing the ground-water resources of 12 regions within the 7 ground-water areas of the main island of Puerto Rico, Isla de Culebra and Isla de Vieques (described in a single section of the atlas), and the U.S. Virgin Islands (St. Thomas and St. John are described in one section of the atlas and St. Croix in another), and a concluding section describing present and potential problems related to the development of ground-water resources. Information presented in each of 15 descriptive sections of the atlas include the (1) location and major geographic features of the area covered by that section, (2) population and estimated (4) hydrogeology of the area, (5) ground-water levels and movements, and (6) a description of soil permeabilities.</p>","language":"ENGLISH","doi":"10.3133/wri944198","usgsCitation":"1996, Atlas of ground-water resources in Puerto Rico and the U.S. Virgin Islands: U.S. Geological Survey Water-Resources Investigations Report 94-4198, viii, 151 p. : ill. (some col.), maps (some col.) ; 28 x 44 cm., https://doi.org/10.3133/wri944198.","productDescription":"viii, 151 p. : ill. (some col.), maps (some col.) ; 28 x 44 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":168107,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4198/report-thumb.jpg"},{"id":3871,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pr.water.usgs.gov/public/online_pubs/wri94_4198/index.html","linkFileType":{"id":5,"text":"html"}},{"id":82038,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4198/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dee4b07f02db5e2a08","contributors":{"editors":[{"text":"Veve, Thalia D.","contributorId":37806,"corporation":false,"usgs":true,"family":"Veve","given":"Thalia","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":629288,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Taggart, Bruce E. btaggart@usgs.gov","contributorId":144,"corporation":false,"usgs":true,"family":"Taggart","given":"Bruce","email":"btaggart@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":629289,"contributorType":{"id":2,"text":"Editors"},"rank":2}]}}
,{"id":24871,"text":"ofr96676 - 1996 - Preliminary geologic map of the Mesquite quadrangle, Clark and Lincoln Counties, Nevada, and Mohave County, Arizona","interactions":[],"lastModifiedDate":"2022-09-12T19:49:59.31575","indexId":"ofr96676","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-676","title":"Preliminary geologic map of the Mesquite quadrangle, Clark and Lincoln Counties, Nevada, and Mohave County, Arizona","docAbstract":"Original geologic data mapped by the author in 1995 and 1996 with emphasis on structures in Miocene basin-fill deposits of the Muddy Creek Formation that may control availability and quality of groundwater.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96676","usgsCitation":"Williams, V., 1996, Preliminary geologic map of the Mesquite quadrangle, Clark and Lincoln Counties, Nevada, and Mohave County, Arizona (Version 1.1): U.S. Geological Survey Open-File Report 96-676, Report: 11 p.: HTML Document, https://doi.org/10.3133/ofr96676.","productDescription":"Report: 11 p.: HTML Document","costCenters":[],"links":[{"id":406551,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22972.htm","linkFileType":{"id":5,"text":"html"}},{"id":53863,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0676/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157563,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0676/report-thumb.jpg"},{"id":1870,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1996/ofr-96-0676/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Arizona, Nevada","county":"Clark County, Lincoln County, Mohave County","otherGeospatial":"Mesquite quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.125,\n              36.75\n            ],\n            [\n              -114,\n              36.75\n            ],\n            [\n              -114,\n              36.875\n            ],\n            [\n              -114.125,\n              36.875\n            ],\n            [\n              -114.125,\n              36.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b100","contributors":{"authors":[{"text":"Williams, Van S.","contributorId":38583,"corporation":false,"usgs":true,"family":"Williams","given":"Van S.","affiliations":[],"preferred":false,"id":192717,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24704,"text":"ofr96660 - 1996 - Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1994 through September 1996","interactions":[],"lastModifiedDate":"2012-02-02T00:08:23","indexId":"ofr96660","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-660","title":"Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1994 through September 1996","docAbstract":"This report describes the status of ground-water resources at U.S. Navy Support Facility, Diego Garcia. Data presented are from January 1994 through September 1996, with a focus on data from July through September 1996 (third quarter of 1996). A complete database of ground-water withdrawals and chloride-concentration records since 1985 is maintained by the U.S. Geological Survey. Total rainfall for the period July through September 1996 was 8.94 inches, which is 60 percent less than the mean rainfall of 22.23 inches for the period July through September. July and August are part of the annual dry season, while September is the start of the annual wet season. Ground-water withdrawal during July through September 1996 averaged 1,038,300 gallons per day. Withdrawal for the same 3 months in 1995 averaged 888,500 gallons per day. Ground-water withdrawals have steadily increased since about April 1995. At the end of September 1996, the chloride concentration of water from the elevated tanks at Cantonment and Air Operations were 68 and 150 milligrams per liter, respectively. The chloride concentration from all five production areas increased throughout the third quarter of 1996, and started the upward trend in about April 1995. Chloride concentration of ground water in monitoring wells at Cantonment and Air Operations also increased throughout the third quarter of 1996, with the largest increases from water in the deepest monitoring wells. Chloride concentrations have not been at this level since the dry season of 1994. A fuel-pipeline leak at Air Operations in May 1991 decreased total islandwide withdrawals by 15 percent. This lost pumping capacity is being offset by increased pumpage at Cantonment. Six wells do not contribute to the water supply because they are being used to hydraulically divert fuel migration away from water-supply wells by a program of ground-water withdrawal and injection.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr96660","issn":"0094-9140","usgsCitation":"Torikai, J., 1996, Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1994 through September 1996: U.S. Geological Survey Open-File Report 96-660, v, 43 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr96660.","productDescription":"v, 43 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":157561,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0660/report-thumb.jpg"},{"id":53737,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0660/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e486fe4b07f02db50ce10","contributors":{"authors":[{"text":"Torikai, J.D.","contributorId":93926,"corporation":false,"usgs":true,"family":"Torikai","given":"J.D.","affiliations":[],"preferred":false,"id":192407,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22331,"text":"ofr96598 - 1996 - Ground-water data for the Warm Springs Indian Reservation and contiguous areas, north-central Oregon","interactions":[],"lastModifiedDate":"2022-02-02T21:41:42.587875","indexId":"ofr96598","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-598","title":"Ground-water data for the Warm Springs Indian Reservation and contiguous areas, north-central Oregon","docAbstract":"<p>This report presents well data that were collected and compiled during 1985-86 by the U.S. Geological Survey and used to determine the amount of ground water discharging to the Deschutes River on and near the Warm Springs Indian Reservation. The report contains well-construction data from 171 wells, information from drillers' logs for 66 wells, water-level data for 29 wells, and a map showing well locations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/ofr96598","issn":"0094-9140","usgsCitation":"Anderson, D.B., 1996, Ground-water data for the Warm Springs Indian Reservation and contiguous areas, north-central Oregon: U.S. Geological Survey Open-File Report 96-598, Report: iv, 66 p.; 1 Plate: 16.93 x 15.54 inches, https://doi.org/10.3133/ofr96598.","productDescription":"Report: iv, 66 p.; 1 Plate: 16.93 x 15.54 inches","numberOfPages":"73","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":51739,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0598/plate-1.pdf","text":"Plate 1","size":"1.92 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,{"id":24655,"text":"ofr96662A - 1996 - Total dissolved gas, barometric pressure, and water temperature data, lower Columbia River, Oregon and Washington, 1996","interactions":[],"lastModifiedDate":"2017-02-07T10:01:37","indexId":"ofr96662A","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-662","chapter":"A","title":"Total dissolved gas, barometric pressure, and water temperature data, lower Columbia River, Oregon and Washington, 1996","docAbstract":"<p>Increased levels of total dissolved gas pressure can cause gas-bubble trauma in fish downstream from dams on the Columbia River. In cooperation with the U.S. Army Corps of Engineers, the U.S. Geological Survey collected data on total dissolved gas pressure, barometric pressure, water temperature, and dissolved oxygen pressure at 11 stations on the lower Columbia River from the John Day forebay (river mile 215.6) to Wauna Mill (river mile 41.9) from March to September 1996. Methods of data collection, review, and processing are described in this report. Summaries of daily minimum, maximum, and mean hourly values are presented for total dissolved gas pressure, barometric pressure, and water temperature. Hourly values for these parameters are presented graphically. Dissolved oxygen data are not presented in this report because the quality-control data show that the data have poor precision and high bias. Suggested changes to monitoring procedures for future studies include (1) improved calibration procedures for total dissolved gas and dissolved oxygen to better define accuracy at elevated levels of supersaturation and (2) equipping dissolved oxygen sensors with stirrers because river velocities at the shoreline monitoring stations probably cannot maintain an adequate flow of water across the membrane surface of the dissolved oxygen sensor.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/ofr96662A","issn":"0094-9140","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers","usgsCitation":"Tanner, D.Q., Harrison, H.E., and McKenzie, S.W., 1996, Total dissolved gas, barometric pressure, and water temperature data, lower Columbia River, Oregon and Washington, 1996: U.S. Geological Survey Open-File Report 96-662, vi, 85 p., https://doi.org/10.3133/ofr96662A.","productDescription":"vi, 85 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E.","contributorId":8485,"corporation":false,"usgs":true,"family":"Harrison","given":"Howard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":192330,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McKenzie, Stuart W.","contributorId":27841,"corporation":false,"usgs":true,"family":"McKenzie","given":"Stuart","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":192331,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":22400,"text":"ofr96458 - 1996 - Quality of Wisconsin stormwater, 1989-94","interactions":[],"lastModifiedDate":"2015-10-15T14:41:53","indexId":"ofr96458","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-458","title":"Quality of Wisconsin stormwater, 1989-94","docAbstract":"<p>Water-quality data were compiled from four urban stormwater monitoring projects conducted in Wisconsin between 1989 and 1994. These projects included monitoring in both storm-sewer pipes and urban streams. A total of 147 constitu ents were analyzed for in stormwater sampled from 10 storm-sewer pipes and four urban streams. Land uses represented by the storm-sewer watersheds included residential, commercial, industrial, and mixed. For about one-half the con stituents, at least 10 percent of the event mean con centrations exceeded the laboratory's minimum reporting limit. Detection frequencies were greater than 75 percent for many of the heavy metals and polycyclic aromatic hydrocarbons in both the storm sewer and stream samples, whereas detec tion frequencies were about 20 percent or greater for many of the pesticides in both types of sam ples. Stormwater concentrations for conventional constituents, such as suspended solids, chloride, total phosphorus, and fecal coliform bacteria were greater than minimum reporting limits almost 100 percent of the time. Concentrations of many of the constituents were high enough to say that stormwater in the storm sewers and urban streams might be contrib uting to the degradation of the streams. In this report, constituents defined as potential contami nants are those for which the laboratory minimum report limit was exceeded for at least 10 percent of the sampled storm events, and for which at least one event mean concentration exceeded an estab lished water-quality standard. Storm-sewer sam ples had event mean concentrations of lead, copper, zinc, cadmium, and silver that frequently exceeded Wisconsin's acute toxicity criteria for cold water fisheries. Wisconsin's human cancer criteria was exceeded almost 100 percent of the time for polycyclic aromatic hydrocarbons in stormwater samples from storm sewers and streams. Maximum concentrations of diazinon found in storm sewers exceeded recommended levels of diazinon. Storm-sewer samples also exceeded Wisconsin's ground-water enforcement standards for pesticides, PCB's, phthalates, and chloride. Defined by criteria in this report, poten tial contaminants included five metals (lead, zinc, copper, silver, and cadmium), nine polycyclic aro matic hydrocarbons, Bis(2-ethylhexyl)phthalate, four pesticides (DDT, atrazine, alachlor, and 2,4 D), suspended solids, chlorides, total phosphorus, BOD 5-day, and bacteria. Wisconsin stormwater quality was similar to stormwater quality monitored in other states. Nearly one-half of median concentrations of con stituents in Wisconsin stormwater were within 30 percent of the medians from other states. The clos est agreement was seen for biochemical oxygen demand, total phosphorus, and total recoverable zinc. Similarities in stormwater quality for the storm sewer and urban streams indicated the storm sewers were a major source of water to the streams during storm events. Concentrations of potential contaminants in urban streams increased dramati cally during storm events as compared to baseflow concentrations.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96458","issn":"0094-9140","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Bannerman, R.T., Legg, A.D., and Greb, S.R., 1996, Quality of Wisconsin stormwater, 1989-94: U.S. Geological Survey Open-File Report 96-458, iv, 26 p., https://doi.org/10.3133/ofr96458.","productDescription":"iv, 26 p.","numberOfPages":"30","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbd40","contributors":{"authors":[{"text":"Bannerman, Roger T. 0000-0001-9221-2905 rbannerman@usgs.gov","orcid":"https://orcid.org/0000-0001-9221-2905","contributorId":5560,"corporation":false,"usgs":true,"family":"Bannerman","given":"Roger","email":"rbannerman@usgs.gov","middleInitial":"T.","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":true,"id":188178,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Legg, Andrew D.","contributorId":6091,"corporation":false,"usgs":true,"family":"Legg","given":"Andrew","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":188179,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Greb, Steven R.","contributorId":29010,"corporation":false,"usgs":false,"family":"Greb","given":"Steven","email":"","middleInitial":"R.","affiliations":[{"id":6913,"text":"Wisconsin Department of Natural Resources","active":true,"usgs":false}],"preferred":false,"id":188180,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":23631,"text":"ofr96553 - 1996 - Selected ground-water data for Yucca Mountain region, southern Nevada and eastern California, through December 1995","interactions":[],"lastModifiedDate":"2012-02-02T00:08:01","indexId":"ofr96553","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-553","title":"Selected ground-water data for Yucca Mountain region, southern Nevada and eastern California, through December 1995","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nInformation Services [distributor],","doi":"10.3133/ofr96553","issn":"0094-9140","usgsCitation":"La Camera, R., Westenburg, C., and Locke, G., 1996, Selected ground-water data for Yucca Mountain region, southern Nevada and eastern California, through December 1995: U.S. Geological Survey Open-File Report 96-553, iv, 75 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr96553.","productDescription":"iv, 75 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":154876,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0553/report-thumb.jpg"},{"id":52908,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0553/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f96c7","contributors":{"authors":[{"text":"La Camera, R.J.","contributorId":83932,"corporation":false,"usgs":true,"family":"La Camera","given":"R.J.","affiliations":[],"preferred":false,"id":190452,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Westenburg, C.L.","contributorId":102511,"corporation":false,"usgs":true,"family":"Westenburg","given":"C.L.","affiliations":[],"preferred":false,"id":190453,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Locke, G.L.","contributorId":59065,"corporation":false,"usgs":true,"family":"Locke","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":190451,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":24865,"text":"ofr96650 - 1996 - Locations and monitoring well completion logs of wells surveyed by U.S. Geological Survey at Air Force Plant 4 and Naval Air Station, Joint Reserve Base, Carswell Field, Fort Worth area, Texas","interactions":[],"lastModifiedDate":"2016-08-22T15:27:02","indexId":"ofr96650","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-650","title":"Locations and monitoring well completion logs of wells surveyed by U.S. Geological Survey at Air Force Plant 4 and Naval Air Station, Joint Reserve Base, Carswell Field, Fort Worth area, Texas","docAbstract":"<p>Completion logs are presented for 16 monitoring wells installed by the U.S. Geological Survey at Air Force Plant 4 and Naval Air Station, Joint Reserve Base, Carswell Field, in the Fort Worth area, Texas. Natural gamma-ray logs are presented for selected monitoring wells. Also included are survey data for eight wells installed by Geo-Marine, Inc.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96650","issn":"0094-9140","usgsCitation":"Williams, M., and Kuniansky, E., 1996, Locations and monitoring well completion logs of wells surveyed by U.S. Geological Survey at Air Force Plant 4 and Naval Air Station, Joint Reserve Base, Carswell Field, Fort Worth area, Texas: U.S. Geological Survey Open-File Report 96-650, 79 p., https://doi.org/10.3133/ofr96650.","productDescription":"79 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":156216,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0650/report-thumb.jpg"},{"id":53860,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0650/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63bf9a","contributors":{"authors":[{"text":"Williams, M.D.","contributorId":79507,"corporation":false,"usgs":true,"family":"Williams","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":192705,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kuniansky, E. L.","contributorId":82342,"corporation":false,"usgs":true,"family":"Kuniansky","given":"E. L.","affiliations":[],"preferred":false,"id":192706,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21714,"text":"ofr96614 - 1996 - Data from synoptic water-quality studies on the Colorado River in the Grand Canyon, Arizona, November 1990 and June 1991","interactions":[],"lastModifiedDate":"2018-02-15T12:53:33","indexId":"ofr96614","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-614","title":"Data from synoptic water-quality studies on the Colorado River in the Grand Canyon, Arizona, November 1990 and June 1991","docAbstract":"Two water-quality synoptic studies were made on the Colorado River in the Grand Canyon, Arizona. Field measurements and the collection of water samples for laboratory analysis were made at 10 mainstem and 6 tributary sites every 6 hours for a 48-hour period on November 5-6, 1990, and again on June 18-20, 1991. Field\r\nmeasurements included discharge, alkalinity, water temperature, light penetration, pH, specific conductance, and dissolved oxygen. Water samples were collected for the laboratory analysis of major and minor ions (calcium, magnesium, sodium, potassium, strontium, chloride, sulfate, silica as SiO2), trace elements (aluminum, arsenic, boron, barium, beryllium, cadmium, cobalt, chromium, copper, iron, lead, lithium, manganese, molybdenum, nickel, selenium, thallium, uranium, vanadium and zinc), and nutrients (phosphate, nitrate, ammonium, nitrite, total\r\ndissolved nitrogen, total dissolved phosphorus and dissolved organic carbon). Biological measurements included drift (benthic invertebrates and detrital material), and benthic invertebrates from the river bottom.","language":"ENGLISH","publisher":"U.S. Geological Survey ;","doi":"10.3133/ofr96614","issn":"0566-8174","usgsCitation":"Taylor, H.E., Peart, D., Antweiler, R.C., Brinton, T., Campbell, W.L., Barbarino, J., Roth, D., Hart, R.J., and Averett, R., 1996, Data from synoptic water-quality studies on the Colorado River in the Grand Canyon, Arizona, November 1990 and June 1991: U.S. Geological Survey Open-File Report 96-614, iv, 176 p. :ill. ; 28 cm., https://doi.org/10.3133/ofr96614.","productDescription":"iv, 176 p. :ill. ; 28 cm.","temporalStart":"1990-11-01","temporalEnd":"1991-06-30","costCenters":[],"links":[{"id":8225,"rank":9999,"type":{"id":18,"text":"Project Site"},"url":"https://wwwbrr.cr.usgs.gov/projects/SW_inorganic/","linkFileType":{"id":5,"text":"html"}},{"id":154546,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0614/report-thumb.jpg"},{"id":8224,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://wwwbrr.cr.usgs.gov/projects/SW_inorganic/download/Synoptic.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":51241,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0614/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c87f","contributors":{"authors":[{"text":"Taylor, Howard E. hetaylor@usgs.gov","contributorId":1551,"corporation":false,"usgs":true,"family":"Taylor","given":"Howard","email":"hetaylor@usgs.gov","middleInitial":"E.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":185377,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peart, D.B.","contributorId":45304,"corporation":false,"usgs":true,"family":"Peart","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":185379,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Antweiler, Ronald C. 0000-0001-5652-6034 antweil@usgs.gov","orcid":"https://orcid.org/0000-0001-5652-6034","contributorId":1481,"corporation":false,"usgs":true,"family":"Antweiler","given":"Ronald","email":"antweil@usgs.gov","middleInitial":"C.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":185381,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brinton, T.I.","contributorId":93922,"corporation":false,"usgs":true,"family":"Brinton","given":"T.I.","affiliations":[],"preferred":false,"id":185383,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Campbell, W. L.","contributorId":46939,"corporation":false,"usgs":true,"family":"Campbell","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":185380,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Barbarino, J.R.","contributorId":94336,"corporation":false,"usgs":true,"family":"Barbarino","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":185384,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Roth, D.A.","contributorId":100864,"corporation":false,"usgs":true,"family":"Roth","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":185385,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Hart, R. J.","contributorId":62607,"corporation":false,"usgs":true,"family":"Hart","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":185382,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Averett, R. C.","contributorId":35709,"corporation":false,"usgs":true,"family":"Averett","given":"R. C.","affiliations":[],"preferred":false,"id":185378,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":24280,"text":"ofr96664A - 1996 - Water-level data for the Albuquerque Basin, New Mexico, period of record through September 30, 1995","interactions":[],"lastModifiedDate":"2012-02-02T00:08:00","indexId":"ofr96664A","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-664","chapter":"A","title":"Water-level data for the Albuquerque Basin, New Mexico, period of record through September 30, 1995","docAbstract":"The Albuquerque Basin, located in central New Mexico, is about \r\n100 miles long and 25 to 40 miles wide. The basin is defined as \r\nthe extent of Cenozoic deposits that encompass the structural Rio \r\nGrande Rift within the basin. Drinking-water supplies throughout \r\nthe Albuquerque Basin are currently (1996) obtained solely from \r\nground-water resources. The population of the basin grew from \r\n419,000 in 1980 to 563,600 in 1990, a 34-percent increase, and \r\nresulted in increases in water demand and ground-water pumpage. \r\nBetween April 1982 and September 1983, a network of wells was \r\nestablished to monitor changes in ground-water levels throughout \r\nthe Albuquerque Basin. Water-level data were collected at 74 \r\nwells and piezometers for the period of record through September \r\n30, 1995, in the Albuquerque Basin.  Water-level data are \r\ncurrently (1996) collected annually at sites 11 and 39; \r\nsemiannually at sites 1-10; quarterly at sites 12, 13, 26, 36-38, \r\n40, 43, 49-51, 64-67, 69, and 71-74; and monthly at sites 14-25, \r\n33-35, 41, 52-63, and 68.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr96664A","issn":"0094-9140","usgsCitation":"Rankin, D.R., 1996, Water-level data for the Albuquerque Basin, New Mexico, period of record through September 30, 1995: U.S. Geological Survey Open-File Report 96-664, v, 28 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr96664A.","productDescription":"v, 28 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":155041,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0664a/report-thumb.jpg"},{"id":53401,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0664a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa4c1","contributors":{"authors":[{"text":"Rankin, Dale R.","contributorId":50924,"corporation":false,"usgs":true,"family":"Rankin","given":"Dale","email":"","middleInitial":"R.","affiliations":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"preferred":false,"id":191622,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25434,"text":"wri964138 - 1996 - Detailed study of selenium and other constituents in water, bottom sediment, soil, alfalfa, and biota associated with irrigation drainage in the Uncompahgre Project area and in the Grand Valley, west-central Colorado, 1991-93","interactions":[],"lastModifiedDate":"2025-01-08T14:26:25.607745","indexId":"wri964138","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-4138","title":"Detailed study of selenium and other constituents in water, bottom sediment, soil, alfalfa, and biota associated with irrigation drainage in the Uncompahgre Project area and in the Grand Valley, west-central Colorado, 1991-93","docAbstract":"<p>In 1985, the U.S. Department of the Interior began a program to study the effects of irrigation drainage in the Western United States. These studies were done to determine whether irrigation drainage was causing problems related to human health, water quality, and fish and wildlife resources. Results of a study in 1991-93 of irrigation drainage associated with the Uncompahgre Project area, located in the lower Gunnison River Basin, and of the Grand Valley, located along the Colorado River, are described in this report. The focus of the report is on the sources, distribution, movement, and fate of selenium in the hydrologic and biological systems and the effects on biota. Generally, other trace- constituent concentrations in water and biota were not elevated or were not at levels of concern. </p><p>Soils in the Uncompahgre Project area that primarily were derived from Mancos Shale contained the highest concentrations of total and watrer-extractable selenium. Only 5 of 128 alfalfa samples had selenium concentrations that exceeded a recommended dietary limit for livestock. Selenium data for soil and alfalfa indicate that irrigation might be mobilizing and redistributing selenium in the Uncompahgre Project area. </p><p>Distribution of dissolved selenium in ground water is affected by the aqueous geochemical environment of the shallow ground- water system. Selenium concentrations were as high as 1,300 micrograms per liter in water from shallow wells. The highest concentrations of dissolved selenium were in water from wells completed in alluvium overlying the Mancos Shale of Cretaceous age; selenium concentrations were lower in water from wells completed in Mancos Shale residuum. Selenium in the study area could be mobilized by oxidation of reduced selenium, desorption from aquifer sediments, ion exchange, and dissolution. Infiltration of irrigation water and, perhaps nitrate, provide oxidizing conditions for mobilization of selenium from alluvium and shale residuum and for transport to streams and irrigation drains that are tributary to the Gunnison, Uncompahgre, and Colorado Rivers. </p><p>Selenium concentrations in about 64 percent of water samples collected from the lower Gunnison River and about 50 percent of samples from the Colorado River near the Colorado-Utah State line exceeded the U.S. Environmental Protection Agency criterion of 5 micrograms per liter for protection of aquatic life. Almost all selenium concentrations in samples collected during the nonirrigation season from Mancos Shale areas exceeded the aquatic-life criterion. The maximum selenium concentrations in surface-water samples were 600 micrograms per liter in the Uncompahgre Project area and 380 micrograms per liter in the Grand Valley. </p><p>Irrigation drainage from the Uncompahgre Project and the Grand Valley might account for as much as 75 percent of the selenium load in the Colorado River near the Colorado-Utah State line. The primary source areas of selenium were the eastern side of the Uncompahgre Project and the western one-half of the Grand Valley, where there is extensive irrigation on soils derived from Mancos Shale. The largest mean selenium loads from tributary drainages were 14.0 pounds per day from Loutsenhizer Arroyo in the Uncompahgre Project and 12.8 pounds per day from Reed Wash in the Grand Valley. Positive correlations between selenium loads and dissolved-solids loads could indicate that salinity-control projects designed to decrease dissolved-solids loads also could decrease selenium loads from the irrigated areas. Selenium concentrations in irrigation drainage in the Grand Valley were much higher than concentrations predicted by simple evaporative concentration of irrigation source water. Selenium probably is removed from pond water by chemical and biological processes and incorporated into bottom sediment. The maximum selenium concentration in bottom sediment was 47 micrograms per gram from a pond on the eastern side of the Uncompahgre Project.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri964138","usgsCitation":"Butler, D.L., Wright, W.G., Stewart, K.C., Osmundson, B.C., Krueger, R.P., and Crabtree, D., 1996, Detailed study of selenium and other constituents in water, bottom sediment, soil, alfalfa, and biota associated with irrigation drainage in the Uncompahgre Project area and in the Grand Valley, west-central Colorado, 1991-93: U.S. Geological Survey Water-Resources Investigations Report 96-4138, ix, 136 p., https://doi.org/10.3133/wri964138.","productDescription":"ix, 136 p.","costCenters":[],"links":[{"id":123072,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4138/report-thumb.jpg"},{"id":54166,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4138/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":465849,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48486.htm","text":"Grand Valley area","linkFileType":{"id":5,"text":"html"}},{"id":465850,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48487.htm","text":"Uncompahgre area","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48b1e4b07f02db530813","contributors":{"authors":[{"text":"Butler, D. L.","contributorId":36967,"corporation":false,"usgs":true,"family":"Butler","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":193676,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wright, W. G.","contributorId":19582,"corporation":false,"usgs":true,"family":"Wright","given":"W.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":193675,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stewart, K. C.","contributorId":46519,"corporation":false,"usgs":true,"family":"Stewart","given":"K.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":193677,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Osmundson, B. C.","contributorId":15655,"corporation":false,"usgs":true,"family":"Osmundson","given":"B.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":193674,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Krueger, R. P.","contributorId":8890,"corporation":false,"usgs":true,"family":"Krueger","given":"R.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":193672,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Crabtree, D.W.","contributorId":10070,"corporation":false,"usgs":true,"family":"Crabtree","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":193673,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":23809,"text":"ofr96648 - 1996 - Ground-water levels in Wyoming, January 1986 through September 1995","interactions":[],"lastModifiedDate":"2012-02-02T00:08:16","indexId":"ofr96648","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-648","title":"Ground-water levels in Wyoming, January 1986 through September 1995","docAbstract":"Water levels were measured in a network of 81 observation wells in Wyoming as of September 1995.  The wells are located mainly in areas where ground water is used in large quantities for irrigation or municipal purposes.  Water-level data were collected at 74 of the 81  observation wells by Wyoming State Engineer personnel; data at theremaining 7 wells were collected by the U.S. Geological Survey.  This report contains hydrographs for 81 observation wells showing water-level fluctuations from January 1986 through September 1995.  Included in the report are maps showing location of the observation wells and tableslisting observation-well depths, use of water, principal geologic source, records available, and highest and lowest water levels for the period ofrecord.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr96648","issn":"0094-9140","usgsCitation":"Mason, J.P., and Green, S.L., 1996, Ground-water levels in Wyoming, January 1986 through September 1995: U.S. Geological Survey Open-File Report 96-648, iv, 119 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr96648.","productDescription":"iv, 119 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":156814,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0648/report-thumb.jpg"},{"id":53023,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0648/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667928","contributors":{"authors":[{"text":"Mason, J. P.","contributorId":27491,"corporation":false,"usgs":true,"family":"Mason","given":"J.","middleInitial":"P.","affiliations":[],"preferred":false,"id":190769,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Green, S. L.","contributorId":83525,"corporation":false,"usgs":true,"family":"Green","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":190770,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21757,"text":"ofr96601 - 1996 - Earthquake data report, January 1996","interactions":[],"lastModifiedDate":"2012-02-02T00:07:52","indexId":"ofr96601","displayToPublicDate":"1997-06-01T00:00:00","publicationYear":"1996","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":"96-601","title":"Earthquake data report, January 1996","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr96601","issn":"0566-8174","usgsCitation":"National Earthquake Information Center, 1996, Earthquake data report, January 1996: U.S. Geological Survey Open-File Report 96-601, 6 computer disks ;5 1/4 in., https://doi.org/10.3133/ofr96601.","productDescription":"6 computer disks ;5 1/4 in.","costCenters":[],"links":[{"id":154691,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62a805","contributors":{"authors":[{"text":"National Earthquake Information Center","contributorId":128066,"corporation":true,"usgs":false,"organization":"National Earthquake Information Center","id":529072,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22090,"text":"ofr9683 - 1996 - R/V Cape Henlopen, May 24-30, 1994, CH94-12: Archive of the USGS QMIPS sidescan sonar and navigation field data collected along Little Egg Inlet, New Jersey","interactions":[],"lastModifiedDate":"2022-06-13T20:20:42.128002","indexId":"ofr9683","displayToPublicDate":"1997-06-01T00:00:00","publicationYear":"1996","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":"96-83","title":"R/V Cape Henlopen, May 24-30, 1994, CH94-12: Archive of the USGS QMIPS sidescan sonar and navigation field data collected along Little Egg Inlet, New Jersey","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr9683","usgsCitation":"Paskevich, V., 1996, R/V Cape Henlopen, May 24-30, 1994, CH94-12: Archive of the USGS QMIPS sidescan sonar and navigation field data collected along Little Egg Inlet, New Jersey: U.S. Geological Survey Open-File Report 96-83, 2 CD-ROMs, https://doi.org/10.3133/ofr9683.","productDescription":"2 CD-ROMs","costCenters":[],"links":[{"id":153795,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":402123,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13252.htm","linkFileType":{"id":5,"text":"html"}},{"id":333307,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0083/ofr9683_2.zip","text":"Disc 2","linkFileType":{"id":6,"text":"zip"}},{"id":333306,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0083/ofr9683_1.zip","text":"Disc 1","linkFileType":{"id":6,"text":"zip"}}],"country":"United States","state":"New Jersey","otherGeospatial":"Little Egg Inlet","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.28543090820312,\n              39.377833529911555\n            ],\n            [\n              -74.15496826171874,\n              39.377833529911555\n            ],\n            [\n              -74.15496826171874,\n              39.52099229357195\n            ],\n            [\n              -74.28543090820312,\n              39.52099229357195\n            ],\n            [\n              -74.28543090820312,\n              39.377833529911555\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649fde","contributors":{"authors":[{"text":"Paskevich, V.F.","contributorId":96285,"corporation":false,"usgs":true,"family":"Paskevich","given":"V.F.","email":"","affiliations":[],"preferred":false,"id":187025,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24418,"text":"ofr96653 - 1996 - Active-, inactive-, and abandoned-mine information and selected geochemical data for the State of Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:08:14","indexId":"ofr96653","displayToPublicDate":"1997-06-01T00:00:00","publicationYear":"1996","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":"96-653","title":"Active-, inactive-, and abandoned-mine information and selected geochemical data for the State of Utah","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr96653","issn":"0094-9140","usgsCitation":"Ryder, J.L., 1996, Active-, inactive-, and abandoned-mine information and selected geochemical data for the State of Utah: U.S. Geological Survey Open-File Report 96-653, 1 computer disk ;3 1/2 in., https://doi.org/10.3133/ofr96653.","productDescription":"1 computer disk ;3 1/2 in.","costCenters":[],"links":[{"id":157104,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1762,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1996/ofr-96-0653/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a3386","contributors":{"authors":[{"text":"Ryder, Jean L.","contributorId":80709,"corporation":false,"usgs":true,"family":"Ryder","given":"Jean","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":191886,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22680,"text":"ofr96377 - 1996 - Digital geologic map of McAlester-Texarkana quadrangles, southeastern Oklahoma","interactions":[],"lastModifiedDate":"2023-08-29T19:10:22.109131","indexId":"ofr96377","displayToPublicDate":"1997-06-01T00:00:00","publicationYear":"1996","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":"96-377","title":"Digital geologic map of McAlester-Texarkana quadrangles, southeastern Oklahoma","docAbstract":"This data set consists of digital data and accompanying documentation of the surficial geology of the 1:250,000-scale McAlester and Texarkana quadrangles, Oklahoma. The original data are from the Geologic Map, sheet 1 of 4, included in Oklahoma Geological Survey publication, Reconnaissance of the water resources of the McAlester and Texarkana quadrangles, southeastern Oklahoma, Hydrologic Atlas 9, Marcher and Bergman, 1983. The geology was compiled by M.V. Marcher and D.L. Bergman, 1971, and revised by R.O. Fay, 1978.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96377","usgsCitation":"Cederstrand, J., 1996, Digital geologic map of McAlester-Texarkana quadrangles, southeastern Oklahoma: U.S. Geological Survey Open-File Report 96-377, 3 computer disks, https://doi.org/10.3133/ofr96377.","productDescription":"3 computer disks","costCenters":[],"links":[{"id":1436,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://ok.water.usgs.gov/gis/geology/","linkFileType":{"id":5,"text":"html"}},{"id":420254,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_40015.htm","linkFileType":{"id":5,"text":"html"}},{"id":154604,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Oklahoma","otherGeospatial":"McAlester-Texarkana quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -96,\n              35\n            ],\n            [\n              -96,\n              33.618\n            ],\n            [\n              -94.435,\n              33.618\n            ],\n            [\n              -94.435,\n              35\n            ],\n            [\n              -96,\n              35\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d450","contributors":{"authors":[{"text":"Cederstrand, J. R.","contributorId":91523,"corporation":false,"usgs":true,"family":"Cederstrand","given":"J. R.","affiliations":[],"preferred":false,"id":188682,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21762,"text":"ofr96317 - 1996 - Effectiveness of highway-drainage systems in preventing contamination of ground water by road salt, Route 25, southeastern Massachusetts; description of study area, data collection programs, and methodology","interactions":[],"lastModifiedDate":"2012-02-02T00:07:52","indexId":"ofr96317","displayToPublicDate":"1997-06-01T00:00:00","publicationYear":"1996","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":"96-317","title":"Effectiveness of highway-drainage systems in preventing contamination of ground water by road salt, Route 25, southeastern Massachusetts; description of study area, data collection programs, and methodology","docAbstract":"Four test sites along a 7-mile section of Route 25 in southeastern Massachusetts, each representing a specific highway-drainage system, were instrumented to determine the effectiveness of the drainage systems in preventing contamination of ground water by road salt. One of the systems discharges highway runoff onsite through local drainpipes. The other systems use trunkline drainpipes through which runoff from highway surfaces, shoulders, and median strips is diverted and discharged into either a local stream or a coastal waterway. Route 25 was completed and opened to traffic in the summer of 1987. Road salt was first applied to the highway in the winter of 1987-88. The study area is on a thick outwash plain composed primarily of sand and gravel. Water-table depths range from 15 to 60 feet below land surface at the four test sites. Ground-water flow is in a general southerly direction, approximately perpendicular to the highway. Streamflow in the study area is controlled primarily by ground-water discharge. Background concentrations of dissolved chloride, sodium, and calcium-the primary constituents of road salt-are similar in ground water and surface water and range from 5 to 20, 5 to 10, and 1 to 5 milligrams per liter, respectively. Data-collection programs were developed for monitoring the application of road salt to the highway, the quantity of road-salt water entering the ground water, diverted through the highway-drainage systems, and entering a local stream. The Massachusetts Highway Department monitored road salt applied to the highway and reported these data to the U.S. Geological Survey. The U.S. Geological Survey designed and operated the ground-water, highway- drainage, and surface-water data-collection programs. A road-salt budget will be calculated for each test site so that the effectiveness of the different highway-drainage systems in preventing contamination of ground water by road salt can be determined.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr96317","issn":"0566-8174","usgsCitation":"Church, P.E., Armstrong, D., Granato, G., Stone, V., Smith, K., and Provencher, P., 1996, Effectiveness of highway-drainage systems in preventing contamination of ground water by road salt, Route 25, southeastern Massachusetts; description of study area, data collection programs, and methodology: U.S. Geological Survey Open-File Report 96-317, vi, 72 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr96317.","productDescription":"vi, 72 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":154712,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0317/report-thumb.jpg"},{"id":51260,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0317/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db6253e8","contributors":{"authors":[{"text":"Church, P. E.","contributorId":39406,"corporation":false,"usgs":true,"family":"Church","given":"P.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":185577,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Armstrong, D.S.","contributorId":81517,"corporation":false,"usgs":true,"family":"Armstrong","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":185582,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Granato, G.E.","contributorId":61457,"corporation":false,"usgs":true,"family":"Granato","given":"G.E.","affiliations":[],"preferred":false,"id":185581,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stone, V.J.","contributorId":41025,"corporation":false,"usgs":true,"family":"Stone","given":"V.J.","email":"","affiliations":[],"preferred":false,"id":185578,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Smith, K.P.","contributorId":54231,"corporation":false,"usgs":true,"family":"Smith","given":"K.P.","email":"","affiliations":[],"preferred":false,"id":185580,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Provencher, P.L.","contributorId":51778,"corporation":false,"usgs":true,"family":"Provencher","given":"P.L.","email":"","affiliations":[],"preferred":false,"id":185579,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":24419,"text":"ofr96710 - 1996 - Active-, inactive-, and abandoned-mine information and selected geochemical data for the State of Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:14","indexId":"ofr96710","displayToPublicDate":"1997-06-01T00:00:00","publicationYear":"1996","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":"96-710","title":"Active-, inactive-, and abandoned-mine information and selected geochemical data for the State of Washington","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr96710","issn":"0094-9140","usgsCitation":"Ryder, J.L., 1996, Active-, inactive-, and abandoned-mine information and selected geochemical data for the State of Washington (Diskette version.): U.S. Geological Survey Open-File Report 96-710, 1 computer disk ;3 1/2 in., https://doi.org/10.3133/ofr96710.","productDescription":"1 computer disk ;3 1/2 in.","costCenters":[],"links":[{"id":156964,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Diskette version.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a338b","contributors":{"authors":[{"text":"Ryder, J. L.","contributorId":30997,"corporation":false,"usgs":true,"family":"Ryder","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":191887,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22749,"text":"ofr96352 - 1996 - Statistical summaries of ground-water level data collected in the Suwannee River Water Management District, 1948 to 1994","interactions":[],"lastModifiedDate":"2012-02-02T00:08:05","indexId":"ofr96352","displayToPublicDate":"1997-06-01T00:00:00","publicationYear":"1996","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":"96-352","title":"Statistical summaries of ground-water level data collected in the Suwannee River Water Management District, 1948 to 1994","docAbstract":"Since 1948, ground-water level data have beensystematically collected from selected wells in theSuwannee River Water Management District (SRWMD) by the U.S. Geological Survey (USGS),the SRWMD, and other agencies. Records of waterlevels in the SRWMD (fig. 1), collected by the USGS  and SRWMD through 1990, and by the SRWMD from 1990 to 1994, have been published for many  years in the USGS annual report series &quot;Water  Resources Data for Florida.&quot; However, no systematic  statistical summaries of water levels in the SRWMD  have been previously published.  The need for such statistical summary data forevaluations of drought severity, ground-water supplyavailability, and minimum water levels for regulatory  purposes increases daily as demands for ground-water usage increase. Also, much of the base flow of  the Suwannee River is dependent upon ground water.  As the population and demand for ground water for  drinking water and irrigation purposes increase, the  ability to quickly and easily predict trends in ground-water availability will become paramount. In  response to this need, the USGS, in cooperation with  the SRWMD, compiled this report. Ground-water sta tistics for 136 sites are presented as well as figures  showing water levels that were measured in wells  from 1948 through September 1994.  In 1994, the SRWMD and the USGS began a long- term program of cooperative studies designed tobetter understand minimum and maximum streamflows and ground-water levels in the SRWMD. Minimum and maximum flows and levels are needed  by the district to manage the surface- and ground-water resources of the SRWMD and to maintain or  improve the various ecosystems. Data evaluation was  a necessary first step in the long- term SRWMD  ground-water investigations program, because basic  statistics for ground-water levels are not included in  the USGS annual data reports such as &quot;Water Resources Data for Florida, Water Year 1994&quot; (Fran klin and others, 1995). Statistics included in this  report were generated using the USGS computer pro gram ADAPS (Automatic Data Processing System)  to characterize normal ground-water levels and depar tures from normal. The report has been organized so that the statisti cal analyses of water levels in the wells are presentedfollowing this introductory material, a description ofthe hydrogeology in the study area, and a description  of the statistics used to present the water-level data.  Specifically, the report presents statistical analyses  for each well, as appropriate, in the following manner: Description of the well.Hydrographs of ground-water levels for the period of record, for the last 10 years of record,  and for the last 5 years of record.  Graphs of maximum, minimum, and mean of monthly mean ground-water levels for wells with  5 or more years of record.Frequency hydrographs (25, 50, and 75 percent)  of monthly mean ground-water levels for wells  with 5 or more years of record. Water-level data and statistical plots are grouped  by county and sorted within the county by ascendingsite identification number. Well locations are plottedon county maps preceding the well descriptions andhydrographs.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr96352","issn":"0094-9140","usgsCitation":"Collins, J., and Freeman, L., 1996, Statistical summaries of ground-water level data collected in the Suwannee River Water Management District, 1948 to 1994: U.S. Geological Survey Open-File Report 96-352, vi, 351 p. :chiefly ill., maps ;28 cm., https://doi.org/10.3133/ofr96352.","productDescription":"vi, 351 p. :chiefly ill., maps ;28 cm.","costCenters":[],"links":[{"id":155596,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0352/report-thumb.jpg"},{"id":52189,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0352/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa540","contributors":{"authors":[{"text":"Collins, J.J.","contributorId":67844,"corporation":false,"usgs":true,"family":"Collins","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":188811,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Freeman, L.D.","contributorId":85220,"corporation":false,"usgs":true,"family":"Freeman","given":"L.D.","email":"","affiliations":[],"preferred":false,"id":188812,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":22683,"text":"ofr96380 - 1996 - Digital geologic map of Tulsa quadrangle, northeastern Oklahoma","interactions":[],"lastModifiedDate":"2024-11-05T16:52:24.253226","indexId":"ofr96380","displayToPublicDate":"1997-06-01T00:00:00","publicationYear":"1996","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":"96-380","title":"Digital geologic map of Tulsa quadrangle, northeastern Oklahoma","docAbstract":"This data set consists of digital data and accompanying documentation of the surficial geology of the 1:250,000-scale Tulsa quadrangle, Oklahoma. The original data are from the Geologic Map, sheet 1 of 4, included in the Oklahoma Geological Survey publication, 'Reconnaissance of the water resources of the Tulsa quadrangle, northeastern Oklahoma', Hydrologic Atlas 2, Marcher and Bingham, 1971. The geology was compiled by M.V. Marcher, in 1969.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96380","issn":"0094-9140","usgsCitation":"Cederstrand, J., 1996, Digital geologic map of Tulsa quadrangle, northeastern Oklahoma: U.S. Geological Survey Open-File Report 96-380, 1 CD-ROM, https://doi.org/10.3133/ofr96380.","productDescription":"1 CD-ROM","costCenters":[],"links":[{"id":154624,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":463701,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0380/ofr96380.zip","linkFileType":{"id":6,"text":"zip"}},{"id":400187,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_40022.htm"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Tulsa quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96,\n              36\n            ],\n            [\n              -94.533,\n              36\n            ],\n            [\n              -94.533,\n              37\n            ],\n            [\n              -96,\n              37\n            ],\n            [\n              -96,\n              36\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67f431","contributors":{"authors":[{"text":"Cederstrand, J. R.","contributorId":91523,"corporation":false,"usgs":true,"family":"Cederstrand","given":"J. R.","affiliations":[],"preferred":false,"id":188685,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}