{"pageNumber":"1286","pageRowStart":"32125","pageSize":"25","recordCount":46734,"records":[{"id":26347,"text":"wri964080 - 1996 - Estimated water use and general hydrologic conditions for Oregon, 1985 and 1990","interactions":[],"lastModifiedDate":"2017-02-07T08:39:09","indexId":"wri964080","displayToPublicDate":"1997-02-01T00:00:00","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":"96-4080","title":"Estimated water use and general hydrologic conditions for Oregon, 1985 and 1990","docAbstract":"Water-use information is vital to planners, engineers, and hydrologists in water resources. This report is a compilation of water-use information for Oregon for calendar years 1985 and 1990. The report presents water-use data by geographic region for several categories of use, including public supply, domestic, commercial, industrial, mining, thermoelectric power, hydroelectric power, live-stock, irrigation, reservoir evaporation, and wastewater treatment. Hydroelectric power is the only instream use discussed; all other uses are considered offstream. The Appendix presents 1985 and 1990 data by region and by drainage basin for the previously mentioned categories of use. The Cascade Range divides Oregon into two distinct climatic zones. The area west of the Cascade Range has an average annual precipitation that ranges from 40 to 200 inches, and precipitation in the area east of the Cascade Range ranges from 10 to 20 inches. The differences in precipitation and geology have an effect on the sources, uses, and amounts of water withdrawn. Most of the large public-supply systems west of the Cascade Range rely on surface water, whereas many of the large public-supply systems east of the Cascade Range use on wells or springs. Irrigators west of the Cascade Range rely primarily on nearby surface- water sources; however, irrigators east of the Cascade Range use primarily surface water that commonly is delivered from distant sources through irrigation ditches. A variety of methods was used to estimate water-use information. Most withdrawals for public-water suppliers were metered; however, irrigation withdrawals usually were estimated by using information on crops, climate, application efficiencies, and conveyance losses. The accuracy of the estimated total withdrawal values for public supply was estimated to be within 4 percent of the values that would be obtained if all public-supply withdrawals were metered. Total withdrawals for irrigation were estimated to be within 40 percent of metered irrigation withdrawals. The estimates-of-error are presented to show the relative, rather than absolute, accuracy of the data for each water-use category. A total of 8,400 million gallons of water per day was withdrawn in Oregon during 1990, about 1,900 million gallons per day more than the 6,500 million gallons per day withdrawn in 1985. Whereas actual water use increased in 1990, the major differences between 1985 and 1990 were attributed to the inclusion of offstream fish hatcheries, the use of different crop coefficients to estimate irrigation, and the availability of more detailed information in the 1990 estimates. Surface-water withdrawals accounted for 92 percent of the total withdrawals in 1990; irrigation was the largest category of water use, accounting for 82 percent of the total withdrawals.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/wri964080","usgsCitation":"Broad, T., and Collins, C.A., 1996, Estimated water use and general hydrologic conditions for Oregon, 1985 and 1990: U.S. Geological Survey Water-Resources Investigations Report 96-4080, vi, 154 p. :ill., maps ;28 cm. [PGS - 166 p.], https://doi.org/10.3133/wri964080.","productDescription":"vi, 154 p. :ill., maps ;28 cm. [PGS - 166 p.]","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":123473,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4080/report-thumb.jpg"},{"id":55143,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4080/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a0d0","contributors":{"authors":[{"text":"Broad, T.M.","contributorId":6478,"corporation":false,"usgs":true,"family":"Broad","given":"T.M.","affiliations":[],"preferred":false,"id":196224,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Collins, C. A.","contributorId":43731,"corporation":false,"usgs":true,"family":"Collins","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":196225,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26685,"text":"wri954269 - 1996 - Water quality of surficial aquifers in the Georgia-Florida Coastal Plain","interactions":[],"lastModifiedDate":"2022-12-19T20:30:26.795536","indexId":"wri954269","displayToPublicDate":"1997-02-01T00:00:00","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":"95-4269","title":"Water quality of surficial aquifers in the Georgia-Florida Coastal Plain","docAbstract":"The National Water Quality Assessment Program of the U.S. Geological Survey established the Georgia-Florida Coastal Plain study unit in 1991. The ground-water study-unit survey was conducted in 1993 to provide a broad over-view of water quality in surficial aquifers. Three land resource provinces were included in the Georgia-Florida Coastal Plain study-unit survey: the Central Florida Ridge, the Coastal Flatwoods, and the Southern Coastal Plain. The U.S. Geological Survey sampled 37 wells in surficial aquifers, 18 in the Coastal Flatwoods and 19 in the Southern Coastal Plain. The Florida Department of Environmental Protection sampled 27 wells tapping surficial aquifers in the Central Florida Ridge as part of the background ground-water quality monitoring network from 1985 through 1989. The data were used to characterize water quality in surficial aquifers of the Central Florida Ridge. Results of the study-unit survey indicated that dissolved solids concentrations in ground water were mostly less than 100 mg/L (milligrams per liter). Higher medians of pH, specific conductance, and concentrations of calcium, bicarbonate, and dissolved solids were measured in samples from the Central Florida Ridge compared to the Southern Coastal Plain and Coastal Flatwoods, probably because of a greater percentage of carbonate minerals in aquifer materials. The U.S. Environmental Protection Agency secondary maximum contaminant level for iron of 300 ug/L (micrograms per liter) in drinking water was exceeded in 15 of 45 samples. Concentrations of nitrate as nitrogen were less than 3.0 mg/L in most samples (74 percent), indicating little or no influence from human activity. Only five samples (9 percent) had concentrations above 10 mg/L, the U.S. Environmental Protection Agency maximum contaminant level for nitrate concentration in drinking water. Significantly lower median concentrations of nitrate were measured in samples from polyvinyl chloride monitoring wells with diameters less than 6 inches than in large diameter, uncased, or iron-cased wells. The median nitrate concentration was 0.05 mg/L in water from monitoring wells, 1.0 mg/L in samples from iron cased wells, and 2.0 mg/L in samples from uncased wells. Concentrations of volatile organic compounds were mostly less than the detection levels and exceeded 1 ug/L in only four samples. Compounds detected at concentrations greater than 1 ug/L were: tetrachloroethane (8.77 ug/L), toluene (23 ug/L) and chloromethane (21 ug/L). Atrazine, desethyl-atrazine, and metolachlor were the only pesticides detected; concentrations were less than 0.02 ug/L, except for metolachlor (2.5 ug/L). Detection of organic compounds in surficial aquifer may be associated with specific activities or sources near the well. Concentrations of radon exceeded the U.S. Environmental Protection Agency proposed maximum contaminant level of 300 picocuries per liter (pCi/L) in 33 samples from wells on the Coastal Flatwoods and the Southern Coastal Plain. Concentrations as high as 13,000 pCi/L were detected in northern Florida. Although uranium concentrations were less than 1 ug/L in all but one sample (1.3 ug/L) from the Southern Coastal Plain, elevated radon concentrations indicate that uranium is present in aquifer material. Uranium is most likely sorbed to iron oxides and clays in subsurface materials. Tritium concentrations indicated that ground water was recharged by precipitation during the past 40 years. Higher concentrations of tritium in ground water were found in the northern part of the study area and may be related to Savannah River Nuclear Facility.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri954269","usgsCitation":"Crandall, C.A., and Berndt, M.P., 1996, Water quality of surficial aquifers in the Georgia-Florida Coastal Plain: U.S. Geological Survey Water-Resources Investigations Report 95-4269, vi, 28 p., https://doi.org/10.3133/wri954269.","productDescription":"vi, 28 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":158849,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":410731,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48342.htm"},{"id":2042,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri954269","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Florida, Georgia","otherGeospatial":"Georgia-Florida Coastal Plain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -85,\n              33.2333\n            ],\n            [\n              -85,\n              27.6833\n            ],\n            [\n              -80.45,\n              27.6833\n            ],\n            [\n              -80.45,\n              33.2333\n            ],\n            [\n              -85,\n              33.2333\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478ee4b07f02db489e2b","contributors":{"authors":[{"text":"Crandall, C. A.","contributorId":93943,"corporation":false,"usgs":true,"family":"Crandall","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":196827,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berndt, M. P.","contributorId":74761,"corporation":false,"usgs":true,"family":"Berndt","given":"M.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":196826,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27987,"text":"wri964009 - 1996 - Ground-water levels in aquifers used for residential supply, Campton Township, Kane County, Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:08:42","indexId":"wri964009","displayToPublicDate":"1997-02-01T00:00:00","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":"96-4009","title":"Ground-water levels in aquifers used for residential supply, Campton Township, Kane County, Illinois","docAbstract":"The U.S. Geological Survey, in cooperation with the Campton Township Board of Trustees, measured water levels in the aquifers used for residential supply in Campton Township, Kane County, Illinois. Aquifers used for residential supply are the shallow and deep aquifers in the glacial drift, composed of unconsolidated sand and gravels; the Alexandrian-Maquoketa aquifer, composed of dolomite and shale of the Alexandrian Series and the Maquoketa Group; the Galena-Platteville aquifer, composed of dolomite of the Platteville and Galena Groups; and the Ancell aquifer, composed of sandstones of the Glenwood Formation and the St. Peter Sanstone. Water-level altitudes in the shallow drift aquifers generally follow surface topography. Analysis of water-level data does not clearly indicate overutilization of these aquifers. Water-level altitudes in the deep drift aquifers decrease from west to east. Comparison of historical depth to water measurements with current (1995) measurements indicates large decreases in water levels in some areas. The deep drift aquifers may be overutilized at these locations. Water-level altitudes in the Alexandrian-Maquoketa aquifer generally decrease from west to east. The potentiometric surface of the aquifer follows the bedrock-surface topography in some locations. Localized low water-level altitudes and large decreases in water levels indicate the Alexandrian-Maquoketa aquifer is overutilized in several areas. Water-level altitudes in the wells finished in the Galena- Platteville aquifer vary by more than 300 feet. Large decreases in water levels in wells finished in the Galena-Platteville aquifer indicate the Galena-Platteville and Alexandrian-Maquoketa aquifers are overutilized in the northern part of the township. Water-level altitudes in the wells finished in the Ancell aquifer are also highly variable. There is no indication that the Ancell aquifer is overutilized.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/wri964009","usgsCitation":"Kay, R.T., and Kraske, K.A., 1996, Ground-water levels in aquifers used for residential supply, Campton Township, Kane County, Illinois: U.S. Geological Survey Water-Resources Investigations Report 96-4009, iv, 29, [7] p. :ill., maps ;28 cm. [PGS - 37 p.], https://doi.org/10.3133/wri964009.","productDescription":"iv, 29, [7] p. :ill., maps ;28 cm. [PGS - 37 p.]","costCenters":[],"links":[{"id":2213,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://il.water.usgs.gov/pubsearch/reports.cgi/view?series=WRIR&number=96-4009","linkFileType":{"id":5,"text":"html"}},{"id":123539,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4009/report-thumb.jpg"},{"id":56810,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4009/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696dfe","contributors":{"authors":[{"text":"Kay, Robert T. 0000-0002-6281-8997 rtkay@usgs.gov","orcid":"https://orcid.org/0000-0002-6281-8997","contributorId":1122,"corporation":false,"usgs":true,"family":"Kay","given":"Robert","email":"rtkay@usgs.gov","middleInitial":"T.","affiliations":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"preferred":true,"id":199017,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kraske, Kurt A.","contributorId":82746,"corporation":false,"usgs":true,"family":"Kraske","given":"Kurt","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":199018,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28252,"text":"wri964014 - 1996 - Determination of the 100-year flood plain on Upper Three Runs and selected tributaries, and the Savannah River at the Savannah River site, South Carolina, 1995","interactions":[],"lastModifiedDate":"2019-12-30T12:50:59","indexId":"wri964014","displayToPublicDate":"1997-02-01T00:00:00","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":"96-4014","title":"Determination of the 100-year flood plain on Upper Three Runs and selected tributaries, and the Savannah River at the Savannah River site, South Carolina, 1995","docAbstract":"The 100-year flood plain was determined for Upper Three Runs, its tributaries, and the part of the Savannah River that borders the Savannah River Site. The results are provided in tabular and graphical formats. The 100-year flood-plain maps and flood profiles provide water-resource managers of the Savannah River Site with a technical basis for making flood-plain management decisions that could minimize future flood problems and provide a basis for designing and constructing drainage structures along roadways. A hydrologic analysis was made to estimate the 100-year recurrence- interval flow for Upper Three Runs and its tributaries. The analysis showed that the well-drained, sandy soils in the head waters of Upper Three Runs reduce the high flows in the stream; therefore, the South Carolina upper Coastal Plain regional-rural-regression equation does not apply for Upper Three Runs. Conse- quently, a relation was established for 100-year recurrence-interval flow and drainage area using streamflow data from U.S. Geological Survey gaging stations on Upper Three Runs. This relation was used to compute 100-year recurrence-interval flows at selected points along the stream. The regional regression equations were applicable for the tributaries to Upper Three Runs, because the soil types in the drainage basins of the tributaries resemble those normally occurring in upper Coastal Plain basins. This was verified by analysis of the flood-frequency data collected from U.S. Geological Survey gaging station 02197342 on Fourmile Branch. Cross sections were surveyed throughout each reach, and other pertinent data such as flow resistance and land-use were col- lected. The surveyed cross sections and computed 100-year recurrence-interval flows were used in a step-backwater model to compute the 100-year flood profile for Upper Three Runs and its tributaries. The profiles were used to delineate the 100-year flood plain on topographic maps. The Savannah River forms the southwestern border of the Savannah River Site. Data from previously published reports were used to delineate the 100-year flood plain for the Savannah River from the downstream site boundary at the mouth of Lower Three Runs at river mile 125 to the upstream site boundary at river mile 163.","language":"English","publisher":"U.S. Geological Survey ","doi":"10.3133/wri964014","usgsCitation":"Lanier, T.H., 1996, Determination of the 100-year flood plain on Upper Three Runs and selected tributaries, and the Savannah River at the Savannah River site, South Carolina, 1995: U.S. Geological Survey Water-Resources Investigations Report 96-4014, Report: v, 65 p.; 3 Plates: 41.59 x 34.10 inches or smaller, https://doi.org/10.3133/wri964014.","productDescription":"Report: v, 65 p.; 3 Plates: 41.59 x 34.10 inches or smaller","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":57079,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1996/4014/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57080,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1996/4014/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57078,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1996/4014/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57081,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4014/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123837,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4014/report-thumb.jpg"}],"country":"United States","state":"South Carolina","city":"Aiken","otherGeospatial":"Savannah River, Upper Three 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H.","contributorId":41469,"corporation":false,"usgs":true,"family":"Lanier","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":199472,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29819,"text":"wri964017 - 1996 - Transport of agricultural chemicals in surface flow, tileflow, and streamflow of Walnut Creek Watershed near Ames, Iowa, April 1991-September 1993","interactions":[],"lastModifiedDate":"2022-12-16T21:20:07.302723","indexId":"wri964017","displayToPublicDate":"1997-02-01T00:00:00","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":"96-4017","title":"Transport of agricultural chemicals in surface flow, tileflow, and streamflow of Walnut Creek Watershed near Ames, Iowa, April 1991-September 1993","docAbstract":"<p>The U.S. Geological Survey, in cooperation with the National Soil Tilth Laboratory of the U.S. Department of Agriculture, Agricultural Research Service, conducted a study as part of the multi-scale, inter-agency Management Systems Evaluation Area (MSEA) program to evaluate the effects of agricultural management (farming) systems on water quality. Data on surface flow, tileflow, and streamflow in the Walnut Creek watershed just south of Ames, Iowa, were collected during April 1991-September 1993 at five sites with drainage areas ranging from 366 to 5,130 hectares. Precipitation, flow discharge, and concentration, loads, and yields of nitrate as nitrogen, atrazine, and metolachlor were analyzed to relate the transport of agricultural chemicals to major water-flow processes and to examine flow and transport differences among three subwatersheds.</p>\n<p>Antecedent conditions and basin-characteristic differences had significant effects on the flow response from the subwatersheds. Monthly streamflow-to-precipitation ratios were greater than 1.0, as a result of snowmelt, and negative when streamflow was lost to the ground-water system in the downstream subwatershed. Dry antecedent conditions resulted in ratios less than 0.3 (July 1992), whereas wet antecedent conditions resulted in ratios from 0.7 to almost 1.0 (July 1993) during months with similar large rainfall amounts.</p>\n<p>Most of the streamflow from the upland subwatersheds came from tileflow. Surface flow (surface runoff, interflow, and return flow) was highly variable and intermittent, usually lasting for only a few days after a storm, although it could be the dominant source of flow when stormflow was large. Tileflow was less variable and much more persistent, ceasing only after prolonged dry periods.</p>\n<p>Large quantities of nitrate as nitrogen were transported in Walnut Creek, with concentrations often greater than the Maximum Contaminant Level of 10 milligrams per liter established by the U.S. Environmental Protection Agency for finished drinking water. In the upland subwatersheds, ground-water flow from the tiles appears to have been the primary means of transport to the streams. Concentrations in tileflow and streamflow generally were 4 to 16 milligrams per liter, with the lower concentrations often the result of dilution by surface runoff. Loss ratios, chemical yields expressed as a percentage of average application rates of nitrate as nitrogen for October 1992-September 1993, were about 10 percent for surface flow and more than 100 percent for tileflow from the 366-hectare basin and were more than 200 percent for streamflow from the downstream subwatershed.</p>\n<p>Concentrations of atrazine and metolachlor in streamflow, typically, were less than the Maximum Contaminant Level of 3.0 micrograms per liter, but were as high as 59 and 80 micrograms per liter, respectively, during stormflow.&nbsp;Concentrations as high as 170 micrograms per liter occurred in tileflow, but these were related to surface flow through surface inlets. The transport of herbicides was extremely variable, with most of the loads occurring during stormflow. Atrazine appeared more susceptible to transport losses to streamflow than did metolachlor. Loss ratios for streamflow from the subwatersheds for April-September periods were 0.3 to 20 percent for atrazine and 0.1 to 2.9 percent for metolachlor.</p>\n<p>Chemical loss ratios indicated differences in the transport characteristics of the three subwatersheds. The downstream subwatershed, which has steeper terrain, a more-developed natural drainage system, and fewer tiles than the two upland subwatersheds, had the largest loss rates for all three chemicals 206 percent for nitrate as nitrogen (October 1992-September 1993) and 20 percent for atrazine and 2.9 percent for metolachlor (April-September 1993). For May-July 1993, when most of the herbicides were transported, the downstream subwatershed also had the largest cumulative unit discharge and the largest streamflow-to-precipitation ratios.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City, IA","doi":"10.3133/wri964017","collaboration":"Prepared in cooperation with the U.S. Department of Agriculture, Agricultural Research Service, National Soil Tilth Laboratory","usgsCitation":"Soenksen, P.J., 1996, Transport of agricultural chemicals in surface flow, tileflow, and streamflow of Walnut Creek Watershed near Ames, Iowa, April 1991-September 1993: U.S. Geological Survey Water-Resources Investigations Report 96-4017, iv, 41 p., https://doi.org/10.3133/wri964017.","productDescription":"iv, 41 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":410648,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48384.htm","linkFileType":{"id":5,"text":"html"}},{"id":159088,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4017/report-thumb.jpg"},{"id":58622,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4017/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Iowa","otherGeospatial":"Walnut Creek watershed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.75,\n              41.9167\n            ],\n            [\n              -93.75,\n              42\n            ],\n            [\n              -93.5667,\n              42\n            ],\n            [\n              -93.5667,\n              41.9167\n            ],\n            [\n              -93.75,\n              41.9167\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ce4b07f02db626be8","contributors":{"authors":[{"text":"Soenksen, P. J.","contributorId":71575,"corporation":false,"usgs":true,"family":"Soenksen","given":"P.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":202183,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27115,"text":"wri964038B - 1996 - Habitat characteristics of benchmark streams in agricultural areas of eastern Wisconsin","interactions":[],"lastModifiedDate":"2015-10-22T15:06:10","indexId":"wri964038B","displayToPublicDate":"1997-02-01T00:00:00","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":"B","title":"Habitat characteristics of benchmark streams in agricultural areas of eastern Wisconsin","docAbstract":"<p>Stream habitat characteristics were measured at twenty sites in agricultural areas of eastern Wisconsin by the U.S. Geological Survey in May and June, 1993 as part of the National Water-Quality Assessment Program Western Lake Michigan Drainages study unit. These \"benchmark\" stream sites were selected for study to represent standards of reference for comparison to other streams in similar physical settings that appear to be more detrimentally affected by agriculture. The agricultural benchmark streams were selected from four physical settings, or relatively homogeneous units (RHU's), that differ in bedrock type and texture of surficial deposits. Habitat characteristics at streams in these four physical settings are described and compared to each other, and a habitat classification scheme was used to rank the quality of habitat in these streams. Additional aquatic information was collected along with the habitat data: water-quality data and population surveys of fish, invertebrates, and algae. Habitat data were collected at three levels: drainage basin, stream segment between major tributaries (length from 1 to 14 km), and stream reach (approximately 150m). Results of statistical analyses show that, in general, most correlations are among basin-level habitat characteristics. Few correlations were observed among reach- and basin-level characteristics. Principal components analysis (PCA) on basin-level data resulted in principal components that reflect RHU, land use or latitude, and basin size. Groupings of habitat characteristics at the reach level are less clearly attributed to some outside environmental factor. Streams that have undergone habitat restoration for fisheries group closely together on PCA ordination plots. Less than half of the habitat characteristics were found to be significantly different between one RHU and the other three. Characteristics that differed between RHU's were mainly at the basin level but also included some reach-level characteristics. Stream-habitat characteristics were classified according to the Michigan Department of Environmental Quality, Great Lakes Environmental Assessment Section (GLEAS) Procedure 51. No relation was found between GLEAS scores and RHU or the percentage of agricultural land in the drainage basins above the benchmark-stream sites. GLEAS scores were varied in each RHU. Streams with high GLEAS scores (rated good or excellent) can be considered benchmark or reference streams as far as habitat is concerned. Of the 20 streams sampled, 16 met this criterion.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri964038B","usgsCitation":"Fitzpatrick, F., Peterson, E.M., and Stewart, J., 1996, Habitat characteristics of benchmark streams in agricultural areas of eastern Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 96-4038, vi, 35 p., https://doi.org/10.3133/wri964038B.","productDescription":"vi, 35 p.","numberOfPages":"40","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":119872,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4038b/report-thumb.jpg"},{"id":55973,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4038b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"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}","publicComments":"\\National Water-Quality Assessment Program: Western Lake Michigan Drainages","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649771","contributors":{"authors":[{"text":"Fitzpatrick, F. A. 0000-0002-9748-7075","orcid":"https://orcid.org/0000-0002-9748-7075","contributorId":61446,"corporation":false,"usgs":true,"family":"Fitzpatrick","given":"F. A.","affiliations":[],"preferred":false,"id":197575,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, E. M.","contributorId":70805,"corporation":false,"usgs":true,"family":"Peterson","given":"E.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":197577,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stewart, J.S.","contributorId":65890,"corporation":false,"usgs":true,"family":"Stewart","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":197576,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":21888,"text":"ofr96481 - 1996 - Index of stations: Surface-water data-collection network of Texas, September 1995","interactions":[],"lastModifiedDate":"2022-12-13T19:18:53.365147","indexId":"ofr96481","displayToPublicDate":"1997-02-01T00:00:00","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":"96-481","title":"Index of stations: Surface-water data-collection network of Texas, September 1995","docAbstract":"<p>As of September 30, 1995, the surface-water data-collection network of Texas (table 1) included 305 continuous-recording streamflow stations (D), 28 gageheight record only stations (G), 23 crest-stage partialrecord stations (C), 42 flood-hydrograph partial-record stations (H), 33 low-flow partial-record stations (L), 19 continuous-recording temperature and conductivity stations (M2), 5 continuous-recording temperature, conductivity, and dissolved oxygen stations (M3), 17 continuous-recording temperature, conductivity, dissolved oxygen, and pH stations (M4), 6 daily chemicalquality stations (Q), 143 periodic chemical-quality stations (Qp), 20 reservoir/lake surveys for water quality (Qs), and 64 continuous or daily reservoir-content stations (R). Plate 1 identifies the major river basins in Texas and shows the location of the stations listed in table 1.</p>\n<p>Table 1 shows the station number and name, latitude and longitude, type of station, and the office responsible for the collection of the data and the record. An 8-digit permanent numerical designation for all gaging stations has been adopted on a nationwide basis; stations are numbered and listed in downstream order. In the downstream direction along the main stem, all stations on a tributary entering between two main-stem stations are listed between them. A similar order is followed in listing stations by first rank, second rank, and other ranks of tributaries. The rank of any tributary with respect to the stream to which it is an immediate&nbsp;tributary is indicated by an indention in the table. Each indention represents one rank. This downstream order and system of indention shows which gaging stations are on tributaries between any two stations on a main stem and the rank of the tributary on which each gaging station is situated.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96481","usgsCitation":"1996, Index of stations: Surface-water data-collection network of Texas, September 1995: U.S. Geological Survey Open-File Report 96-481, Report: iii, 17 p.; 1 Plate: 35.92 x 36.56 inches, https://doi.org/10.3133/ofr96481.","productDescription":"Report: iii, 17 p.; 1 Plate: 35.92 x 36.56 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":51376,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0481/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"},{"id":410376,"rank":4,"type":{"id":36,"text":"NGMDB Index 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,{"id":24564,"text":"ofr95723 - 1996 - Bibliography of glacier studies by the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2012-02-02T00:08:00","indexId":"ofr95723","displayToPublicDate":"1997-01-10T00:00:00","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":"95-723","title":"Bibliography of glacier studies by the U.S. Geological Survey","docAbstract":"Reports on glaciers written by U.S. Geological Survey members between 1896 and early 1996 are listed. The reports contain information about glacier and had at least one USGS author or was dependent on USGS data or projects. Extensive glacier studies have been done by the USGS in North America, Greenland, Iceland, as well as in Antarctica.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95723","issn":"0094-9140","usgsCitation":"Snyder, E., 1996, Bibliography of glacier studies by the U.S. Geological Survey: U.S. Geological Survey Open-File Report 95-723, 35 p. :ill. ;28 cm., https://doi.org/10.3133/ofr95723.","productDescription":"35 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":155125,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0723/report-thumb.jpg"},{"id":53612,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0723/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cee4b07f02db545a08","contributors":{"authors":[{"text":"Snyder, E.F.","contributorId":18787,"corporation":false,"usgs":true,"family":"Snyder","given":"E.F.","email":"","affiliations":[],"preferred":false,"id":192164,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23400,"text":"ofr96382 - 1996 - Hydrologic data for Long Valley Caldera, Mono County, California, 1987-93","interactions":[],"lastModifiedDate":"2019-06-06T13:08:28","indexId":"ofr96382","displayToPublicDate":"1997-01-10T00:00:00","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":"96-382","title":"Hydrologic data for Long Valley Caldera, Mono County, California, 1987-93","docAbstract":"Hydrologic data were collected during 1987-93 as part of the U.S. Geological Survey's long-term Volcanic Hazards Monitoring Program of the Long Valley Caldera, Mono County, California. The data are presented in graphs or tables. Data collected for the Long Valley Hydrologic Advisory Committee monitoring program also are presented. Hydrologic data collected include continuous record of ground-water levels in 6 wells, instantaneous measurement of ground-water levels in 55 wells, continuous record of discharge at 2 streams and 5 springs, instantaneous discharge measurements at 4 streams and 2 springs, ground-water temperature profiles of 3 thermal wells, continuous record of water temperature in 1 stream and 5 springs, vent gas temperatures at 2 fumaroles, and chemical and isotopic analyses of water samples collected at 13 ground-water and 6 surface-water sites. Precipitation amounts at three sites also are included.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr96382","issn":"0094-9140","usgsCitation":"Howle, J., and Farrar, C.D., 1996, Hydrologic data for Long Valley Caldera, Mono County, California, 1987-93: U.S. Geological Survey Open-File Report 96-382, vii, 286 p. :ill., maps ;28 cm. +1 computer disk (3 1/2 in.), https://doi.org/10.3133/ofr96382.","productDescription":"vii, 286 p. :ill., maps ;28 cm. +1 computer disk (3 1/2 in.)","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":156126,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0382/report-thumb.jpg"},{"id":52702,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0382/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60edb2","contributors":{"authors":[{"text":"Howle, J. F. 0000-0003-0491-6203","orcid":"https://orcid.org/0000-0003-0491-6203","contributorId":66294,"corporation":false,"usgs":true,"family":"Howle","given":"J. F.","affiliations":[],"preferred":false,"id":190044,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Farrar, C. D.","contributorId":71978,"corporation":false,"usgs":true,"family":"Farrar","given":"C.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":190045,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24590,"text":"ofr96217 - 1996 - Urban land-use study plan for the National Water-Quality Assessment Program","interactions":[],"lastModifiedDate":"2012-02-02T00:08:06","indexId":"ofr96217","displayToPublicDate":"1997-01-10T00:00:00","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":"96-217","title":"Urban land-use study plan for the National Water-Quality Assessment Program","docAbstract":"This study plan is for Urban Land-Use Studies initiated as part of the U.S. Geological Survey's National Water-Quality Assessment (NAWQA) Program. There are two Urban Land-Use Study objectives: (1) Define the water quality in recharge areas of shallow aquifers underlying areas of new residential and commercial land use in large metropolitan areas, and (2) determine which natural and human factors most strongly affect the occurrence of contaminants in these shallow aquifers. To meet objective 1, each NAWQA Study Unit will install and collect water samples from at least 30 randomly located monitoring wells in a metropolitan area. To meet objective 2, aquifer characteristics and land-use information will be documented. This includes particle-size analysis of each major lithologic unit both in the unsaturated zone and in the aquifer near the water table. The percentage of organic carbon also will be determined for each lithologic unit. Geographic information system coverages will be created that document existing land use around the wells. These data will aid NAWQA personnel in relating natural and human factors to the occurrence of contaminants. Water samples for age dating also will be collected from all monitoring wells, but the samples will be stored until the occurrence of contaminants has been determined. Age-date analysis will be done only on those samples that have no detectable concentrations of anthropogenic contaminants.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr96217","issn":"0094-9140","usgsCitation":"Squillace, P.J., and Price, C.V., 1996, Urban land-use study plan for the National Water-Quality Assessment Program: U.S. Geological Survey Open-File Report 96-217, v, 19 p. :map ;28 cm., https://doi.org/10.3133/ofr96217.","productDescription":"v, 19 p. :map ;28 cm.","costCenters":[],"links":[{"id":1628,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr96-217","linkFileType":{"id":5,"text":"html"}},{"id":155732,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0217/report-thumb.jpg"},{"id":53639,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0217/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db60527c","contributors":{"authors":[{"text":"Squillace, P. J.","contributorId":8878,"corporation":false,"usgs":true,"family":"Squillace","given":"P.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":192212,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Price, C. V.","contributorId":19190,"corporation":false,"usgs":true,"family":"Price","given":"C.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":192213,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21582,"text":"ofr96525 - 1996 - Analytical methods manual for the Mineral Resource Surveys Program, U.S. Geological Survey","interactions":[],"lastModifiedDate":"2021-05-27T15:22:46.792702","indexId":"ofr96525","displayToPublicDate":"1997-01-10T00:00:00","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":"96-525","title":"Analytical methods manual for the Mineral Resource Surveys Program, U.S. Geological Survey","docAbstract":"<p>The analytical methods validated by the Mineral Resource Surveys Program, Geologic Division, is the subject of this manual. This edition replaces the methods portion of Open-File Report 90-668 published in 1990. Newer methods may be used which have been approved by the quality assurance (QA) project and are on file with the QA coordinator.</p><p>This manual is intended primarily for use by laboratory scientists; this manual can also assist laboratory users to evaluate the data they receive. The analytical methods are written in a step by step approach so that they may be used as a training tool and provide detailed documentation of the procedures for quality assurance. A \"Catalog of Services\" is available for customer (submitter) use with brief listings of:</p><p><ul><li>the element(s)/species determined,<br></li><li>method of determination,<br></li><li>reference to cite,<br></li><li>contact person,<br></li><li>summary of the technique,<br></li><li>and analyte concentration range.</li></ul></p><p>For a copy please contact the Branch office at (303) 236-1800 or fax (303) 236-3200. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96525","usgsCitation":"1996, Analytical methods manual for the Mineral Resource Surveys Program, U.S. Geological Survey: U.S. Geological Survey Open-File Report 96-525, xi, 248 p., https://doi.org/10.3133/ofr96525.","productDescription":"xi, 248 p.","costCenters":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true}],"links":[{"id":51165,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0525/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153451,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0525/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67f7df","contributors":{"editors":[{"text":"Arbogast, Belinda F.","contributorId":89124,"corporation":false,"usgs":true,"family":"Arbogast","given":"Belinda","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":726007,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":22456,"text":"ofr96220 - 1996 - Water-quality data and estimated loads of selected constituents in five tributaries to the Chesapeake Bay at the Fall Line, Virginia, July 1993 through June 1995","interactions":[],"lastModifiedDate":"2012-02-02T00:08:01","indexId":"ofr96220","displayToPublicDate":"1997-01-10T00:00:00","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":"96-220","title":"Water-quality data and estimated loads of selected constituents in five tributaries to the Chesapeake Bay at the Fall Line, Virginia, July 1993 through June 1995","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nInformation Services [distributor],","doi":"10.3133/ofr96220","issn":"0094-9140","usgsCitation":"Belval, D., and Campbell, J., 1996, Water-quality data and estimated loads of selected constituents in five tributaries to the Chesapeake Bay at the Fall Line, Virginia, July 1993 through June 1995: U.S. Geological Survey Open-File Report 96-220, v, 79 p. :ill. ;28 cm., https://doi.org/10.3133/ofr96220.","productDescription":"v, 79 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":155084,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0220/report-thumb.jpg"},{"id":51980,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0220/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c1ae","contributors":{"authors":[{"text":"Belval, D.L.","contributorId":52186,"corporation":false,"usgs":true,"family":"Belval","given":"D.L.","affiliations":[],"preferred":false,"id":188286,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, J.P.","contributorId":80310,"corporation":false,"usgs":true,"family":"Campbell","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":188287,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68103,"text":"ha739 - 1996 - Susceptibility of ground water to surface and shallow sources of contamination in Mississippi","interactions":[],"lastModifiedDate":"2016-08-23T09:26:13","indexId":"ha739","displayToPublicDate":"1997-01-10T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"739","title":"Susceptibility of ground water to surface and shallow sources of contamination in Mississippi","docAbstract":"<p>Ground water, because of its extensive use in agriculture, industry, and public-water supply, is one of Mississippi's most important natural resources. &nbsp;Ground water is the source for about 80 percent of the total freshwater used by the State's population (Solley and others, 1993). &nbsp;About 2,600 Mgal/d of freshwater is withdrawn from aquifers in Mississippi (D.E. Burt, Jr., U.S. Geological Survey, oral commun., 1995). &nbsp;Wells capable of yielding 200 gal/min of water with quality suitable for most uses can be developed nearly anywhere in the State (Bednar, 1988). &nbsp;The U.S. Geological Survey (USGS), in cooperation with the Mississippi Department of Environmental Quality, Office of Pollution Control, and the Mississippi Department of Agriculture and Commerce, Bureau of Plant Industry, conducted an investigation to evaluate the susceptibility of ground water to contamination from surgace and shallow sources in Mississippi. &nbsp;A geographic information system (GIS) was used to develop and analyze statewide spatial data layers that contain geologic, hydrologic, physiographic, and cultural information.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha739","isbn":"0607861126","usgsCitation":"O'Hara, C., 1996, Susceptibility of ground water to surface and shallow sources of 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688064","contributors":{"authors":[{"text":"O'Hara, Charles G.","contributorId":83911,"corporation":false,"usgs":true,"family":"O'Hara","given":"Charles G.","affiliations":[],"preferred":false,"id":277651,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67960,"text":"ha738A - 1996 - Geologic history and hydrogeologic units of intermontane basins of the northern Rocky Mountains, Montana and Idaho","interactions":[],"lastModifiedDate":"2015-10-28T11:10:58","indexId":"ha738A","displayToPublicDate":"1997-01-10T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"738","chapter":"A","title":"Geologic history and hydrogeologic units of intermontane basins of the northern Rocky Mountains, Montana and Idaho","docAbstract":"<p>The Regional Aquifer-System Analysis (RASA) program is a series of studies by the U.S. Geological Survey (USGS) to analyze regional ground-water systems that compose a major portion of the Nation&rsquo;s water supply (Sun, 1986). The Northern Rocky Mountains Intermontane Basins is one of the study regions in this national program. The main objectives of the RASA studies are to: (1) describe the ground-water systems as they exist today, (2) analyze the known changes that have led to the system's present condition, (3) combine results of previous studies in a regional analysis, where possible, and (4) provide means by which effects of future ground-water development can be estimated.<br />The purpose of this study, which began in 1990, was to increase understanding of the hydrogeology of the intermontane basins of the Northern Rocky Mountains area. This report is Chapter Cofa three-part series and describes the quality of ground-water and surface water in the study area. Chapter A (T&uuml;ck and others, 1996) describes the geologic history and generalized hydrogeologic units. Chapter B (Briar and others, 1996) describes the general distribution of ground-watcrlcwels in basin-fill deposits,<br />Water-quality data illustrated in this report represent the distribution of concentrations and composition of dissolved solids in ground-water and surface water in the intermontane areas. The chemistry of ground and surface water in the intermontane areas is influenced by the chemical and physical nature of the rocks in the basin deposits of the valleys and surrounding bedrock in the mountains.</p>","language":"ENGLISH","doi":"10.3133/ha738A","isbn":"0607861428","usgsCitation":"Tuck, L., Briar, D.W., and Clark, D.W., 1996, Geologic history and hydrogeologic units of intermontane basins of the northern Rocky Mountains, Montana and Idaho: U.S. Geological Survey Hydrologic Atlas 738, 1 map :col. ;86 x 64 cm., on sheet 109 x 94 cm., folded in envelope 30 x 24 cm. +1 data sheet (76 x 101 cm.), https://doi.org/10.3133/ha738A.","productDescription":"1 map :col. ;86 x 64 cm., on sheet 109 x 94 cm., folded in envelope 30 x 24 cm. +1 data sheet (76 x 101 cm.)","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":265404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/738a/plate-1.pdf"},{"id":265405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/738a/plate-2.pdf"},{"id":265403,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ha/738a/report.pdf"},{"id":185557,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/738a/report-thumb.jpg"}],"scale":"750000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115,44 ], [ -115,49 ], [ -111,49 ], [ -111,44 ], [ -115,44 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a551b","contributors":{"authors":[{"text":"Tuck, L.K.","contributorId":54247,"corporation":false,"usgs":true,"family":"Tuck","given":"L.K.","email":"","affiliations":[],"preferred":false,"id":277399,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Briar, David W. dbriar@usgs.gov","contributorId":4034,"corporation":false,"usgs":true,"family":"Briar","given":"David","email":"dbriar@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":277398,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clark, David W.","contributorId":77146,"corporation":false,"usgs":true,"family":"Clark","given":"David","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":277400,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":24175,"text":"ofr95736 - 1996 - Geohydrology and potential for upward movement of saline water in the Cocoa well field, East Orange County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:05","indexId":"ofr95736","displayToPublicDate":"1997-01-10T00:00:00","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":"95-736","title":"Geohydrology and potential for upward movement of saline water in the Cocoa well field, East Orange County, Florida","docAbstract":"The Floridan aquifer system, an approximately 2,000-foot thick sequence of Eocene-age limestone and dolomite, is the main source of water supply in central Florida. Hydraulic conductivity is different in strata of different lithology and is the basis for separating the aquifer system into the Upper Floridan aquifer, a middle semi- confining unit, and the Lower Floridan aquifer. The coastal city of Cocoa withdraws about 26 million gallons of water per day from the Upper Floridan aquifer from a well field in east Orange County, about 25 miles inland. About 60 million gallons per day are withdrawn from the Upper Floridan aquifer and 56 million gallons per day from the Lower Floridan aquifer in the Orlando area, about 15 miles west of the Cocoa well field. Wells drilled in the Cocoa well field from 1955-61 yielded water with chloride concentrations ranging from 25-55 milligrams per liter. Soon after the wells were put in service, chloride concentrations increased; therefore, new wells were drilled further inland. Chloride concen- trations in water from many of the new wells also have increased. Possible sources of saline water are lateral movement of relict seawater in the Upper Floridan aquifer from the east, regional upconing of saline water from the Lower Floridan aquifer or underlying older rocks, or localized upward movement of saline water through fractures. Several test wells were drilled to provide information about chloride concentration changes with depth and to monitor changes with time, including a multi-zone well drilled in 1965 (well C) and two wells drilled in the 1990's (wells R and S). Chloride concentrations have increased in the zone pumped by the supply wells (the upper 500 feet of the aquifer) and in the 1,351-1,357-foot deep zone of well C, but not in the two intervening zones. This indicates that the source of saline water is located laterally, rather than vertically, from the pumped zone in the area of well C. The potential for upward movement of saline water depends on the direction of the vertical hydraulic gradient and on the vertical hydraulic conductivity of the aquifer. A series of aquifer tests was run in 1993-94 and existing water-level and water-quality data were analyzed to evaluate the potential for upward movement of saline water in the well field. The transmissivity of the upper 500 feet of the aquifer is about 100,000 feet squared per day (the horizontal hydraulic conductivity is about 200 feet per day) and the storage coefficient is about 2x10 -4. Horizontal hydraulic conductivities determined from slug tests of the three deepest zones of well C ranged from 20-50 feet per day. Vertical hydraulic conductivities probably do not exceed 0.05 feet per day. The vertical hydraulic gradient is determined by comparing water levels in the various zones, but because of density differences, unadjusted water levels in the deepest zone investigated cannot be directly compared to water levels in the overlying freshwater zones. The difference between environmental-water heads (adjusted for density differences) in the saline-water zone of well C and the overlying freshwater zone were calculated from measured water levels for the period 1966 to 1994. During most of this time period, the gradient was downward, indicating that saline water did not move upward. Upconing of saline water probably is not taking place in the center and western part of the well field, based on the low vertical hydraulic conductivity values estimated for the middle semi-confining unit, the generally downward vertical hydraulic gradient, and the constant chloride concentrations in the intermediate zones of well C. However, there is no information about the extent of the zone of low vertical hydraulic conductivity gradient in the eastern part of the well field. Thus, increased chloride concentrations in supply wells in the eastern part of the well field could be caused either by lateral movement of saline water from the east, or by upwar","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr95736","issn":"0094-9140","usgsCitation":"Phelps, G.G., and Schiffer, D., 1996, Geohydrology and potential for upward movement of saline water in the Cocoa well field, East Orange County, Florida: U.S. Geological Survey Open-File Report 95-736, vi, 38 p. :ill. ;28 cm., https://doi.org/10.3133/ofr95736.","productDescription":"vi, 38 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":1579,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr95736/","linkFileType":{"id":5,"text":"html"}},{"id":155483,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8cbb","contributors":{"authors":[{"text":"Phelps, G. G.","contributorId":82346,"corporation":false,"usgs":true,"family":"Phelps","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":191449,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schiffer, D. M.","contributorId":102103,"corporation":false,"usgs":true,"family":"Schiffer","given":"D. M.","affiliations":[],"preferred":false,"id":191450,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":22891,"text":"ofr96432 - 1996 - Water-quality, bed-sediment, and biological data (October 1994 through September 1995) and statistical summaries of data for streams in the upper Clark Fork basin, Montana","interactions":[],"lastModifiedDate":"2019-12-05T16:27:58","indexId":"ofr96432","displayToPublicDate":"1997-01-10T00:00:00","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":"96-432","title":"Water-quality, bed-sediment, and biological data (October 1994 through September 1995) and statistical summaries of data for streams in the upper Clark Fork basin, Montana","docAbstract":"Water, bed sediment, and biota were sampled in streams from Butte to below Missoula as part of a program to characterize aquatic resources in the upper Clark Fork basin of western Montana. Sampling stations were located on the Clark Fork and major tributaries. Water-quality data were obtained periodically at 16 stations during October 1994 through September 1995 (water year 1995). Data for twelve bed-sediment and eleven biological stations were obtained in August 1995. The primary constituents analyzed were trace elements associated with mine tailings from historical mining and smelting activities. Water-quality data include concentrations of major ions, trace element, and suspended sediment in stream samples collected periodically during water year 1995. Daily values of streamflow, suspended- sediment concentrations in the fine-grained and bulk fractions. Biological data include trace- element concentrations in whole-body tissue of aquatic benthic insects. Quality-assurance data are reported for analytical results of water, bed sediment, and biota. Statistical summaries of water-quality, bed-sediment, and biological data are provided for the period of record at each station since 1985.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr96432","issn":"0094-9140","usgsCitation":"Dodge, K.A., Hornberger, M.I., and Axtmann, E., 1996, Water-quality, bed-sediment, and biological data (October 1994 through September 1995) and statistical summaries of data for streams in the upper Clark Fork basin, Montana: U.S. Geological Survey Open-File Report 96-432, iv, 109 p., https://doi.org/10.3133/ofr96432.","productDescription":"iv, 109 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683411","contributors":{"authors":[{"text":"Dodge, K. A.","contributorId":40615,"corporation":false,"usgs":true,"family":"Dodge","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":189080,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hornberger, Michelle I. 0000-0002-7787-3446","orcid":"https://orcid.org/0000-0002-7787-3446","contributorId":23574,"corporation":false,"usgs":true,"family":"Hornberger","given":"Michelle","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":189078,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Axtmann, E.V.","contributorId":30652,"corporation":false,"usgs":true,"family":"Axtmann","given":"E.V.","email":"","affiliations":[],"preferred":false,"id":189079,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":24247,"text":"ofr96428 - 1996 - Drilling, construction, and caliper-log data for well 3-3505-25, North Lower Anahulu exploratory well, Oahu, Hawaii","interactions":[],"lastModifiedDate":"2017-08-30T17:12:07","indexId":"ofr96428","displayToPublicDate":"1997-01-10T00:00:00","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":"96-428","title":"Drilling, construction, and caliper-log data for well 3-3505-25, North Lower Anahulu exploratory well, Oahu, Hawaii","docAbstract":"The North Lower Anahulu exploratory well (State well number 3-3505-25) was drilled about 1.4 miles east-northeast of the town of Haleiwa. The well was drilled on agricultural land in the Kawailoa ground-water area. The well was drilled from an elevation of about 232 feet above mean sea level and penetrates about 22 feet into a basalt aquifer. Well-construction data, logs of drilling notes, geologic descriptions for the samples, and caliper-log data are presented for the well. The well is one of 12 exploratory wells drilled in the north-central Oahu area between July, 1993 and May, 1994 in cooperation with the Honolulu Board of Water Supply.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Honolulu, HI","doi":"10.3133/ofr96428","issn":"0094-9140","collaboration":"Prepared in cooperatih with the City and County of Honolulu Board of Water Supply","usgsCitation":"Presley, T., and Oki, D., 1996, Drilling, construction, and caliper-log data for well 3-3505-25, North Lower Anahulu exploratory well, Oahu, Hawaii: U.S. Geological Survey Open-File Report 96-428, 10 p., https://doi.org/10.3133/ofr96428.","productDescription":"10 p.","costCenters":[],"links":[{"id":157019,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0428/report-thumb.jpg"},{"id":53377,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0428/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5ee4b07f02db633eb2","contributors":{"authors":[{"text":"Presley, T.K.","contributorId":61858,"corporation":false,"usgs":true,"family":"Presley","given":"T.K.","email":"","affiliations":[],"preferred":false,"id":191560,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oki, D.S.","contributorId":75184,"corporation":false,"usgs":true,"family":"Oki","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":191561,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21777,"text":"ofr9679 - 1996 - Explanation of fields used in the Alaska Resource Data File of mines, prospects, and mineral occurrences in Alaska","interactions":[],"lastModifiedDate":"2017-01-30T08:24:37","indexId":"ofr9679","displayToPublicDate":"1997-01-10T00:00:00","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":"96-79","title":"Explanation of fields used in the Alaska Resource Data File of mines, prospects, and mineral occurrences in Alaska","docAbstract":"<p>Descriptions of mines, prospects, and mineral occurrences in the Alaska Resource Data File (ARDF) are published for individual U.S. Geological Survey 1:250,000 scale quadrangles in Alaska (see accompanying map) and are available for downloading from USGS World Wide Web site: <a href=\"http://www-rnrs-ak.wr.usgs.gov/ardf\" data-mce-href=\"http://www-rnrs-ak.wr.usgs.gov/ardf\">http://www-rnrs-ak.wr.usgs.gov/ardf</a>.</p><p>These descriptions are divided into a number of fields which describe features of each mine, prospect, or mineral occurrence. These descriptions were complied from published literature and from unpublished reports and data from industry, the U.S. Bureau of Mines, and the U.S. Geological Survey and other sources. Compilation of this database is an ongoing process and each report is essentially a progress report. The authors of the individual quadrangle reports would appreciate any corrections or additional information that users may be able to contribute.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr9679","issn":"0566-8174","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1996, Explanation of fields used in the Alaska Resource Data File of mines, prospects, and mineral occurrences in Alaska: U.S. Geological Survey Open-File Report 96-79, 4 p., https://doi.org/10.3133/ofr9679.","productDescription":"4 p.","numberOfPages":"4","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":154768,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0079/report-thumb.jpg"},{"id":51277,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0079/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8def","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529074,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24135,"text":"ofr96246 - 1996 - Selected well and ground-water chemistry data for the Boise River Valley, southwestern Idaho, 1990-95","interactions":[],"lastModifiedDate":"2013-11-15T13:42:04","indexId":"ofr96246","displayToPublicDate":"1997-01-10T00:00:00","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":"96-246","title":"Selected well and ground-water chemistry data for the Boise River Valley, southwestern Idaho, 1990-95","docAbstract":"Water samples were collected from 903 wells in the Boise River Valley, Idaho, from January 1990 through December 1995. Selected well information and analyses of 1,357 water samples are presented. Analyses include physical properties ad concentrations of nutrients, bacteria, major ions, selected trace elements, radon-222, volatile organic compounds, and pesticides.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96246","usgsCitation":"Parliman, D., Boyle, L., and Nicholls, S., 1996, Selected well and ground-water chemistry data for the Boise River Valley, southwestern Idaho, 1990-95: U.S. Geological Survey Open-File Report 96-246, iii, 199 p., https://doi.org/10.3133/ofr96246.","productDescription":"iii, 199 p.","numberOfPages":"197","temporalStart":"1990-01-01","temporalEnd":"1995-12-30","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":157284,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0246/report-thumb.jpg"},{"id":53287,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0246/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"10000","projection":"Albers Equal-Area projection","country":"United States","state":"Idaho","otherGeospatial":"Boise River Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.75,43.5 ], [ -116.75,43.75 ], [ -116.0,43.75 ], [ -116.0,43.5 ], [ -116.75,43.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3acb","contributors":{"authors":[{"text":"Parliman, D. J.","contributorId":64220,"corporation":false,"usgs":true,"family":"Parliman","given":"D. J.","affiliations":[],"preferred":false,"id":191382,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boyle, Linda","contributorId":25600,"corporation":false,"usgs":true,"family":"Boyle","given":"Linda","email":"","affiliations":[],"preferred":false,"id":191381,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nicholls, Sabrina","contributorId":106532,"corporation":false,"usgs":true,"family":"Nicholls","given":"Sabrina","email":"","affiliations":[],"preferred":false,"id":191383,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":24140,"text":"ofr96281 - 1996 - MAPIT; an improved method for mapping digital sidescan sonar data using the Woods Hole Image Processing System (WHIPS) software","interactions":[],"lastModifiedDate":"2012-02-02T00:08:02","indexId":"ofr96281","displayToPublicDate":"1997-01-10T00:00:00","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":"96-281","title":"MAPIT; an improved method for mapping digital sidescan sonar data using the Woods Hole Image Processing System (WHIPS) software","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr96281","issn":"0094-9140","usgsCitation":"Paskevich, V., 1996, MAPIT; an improved method for mapping digital sidescan sonar data using the Woods Hole Image Processing System (WHIPS) software: U.S. Geological Survey Open-File Report 96-281, ii, 73 p.  :ill. (some col.) ;28 cm., https://doi.org/10.3133/ofr96281.","productDescription":"ii, 73 p.  :ill. (some col.) ;28 cm.","costCenters":[],"links":[{"id":155834,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0281/report-thumb.jpg"},{"id":53289,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0281/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648b64","contributors":{"authors":[{"text":"Paskevich, V.F.","contributorId":96285,"corporation":false,"usgs":true,"family":"Paskevich","given":"V.F.","email":"","affiliations":[],"preferred":false,"id":191388,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24209,"text":"ofr96414 - 1996 - Snow-depth and water-equivalent data for the Fairbanks area, Alaska, spring 1995","interactions":[],"lastModifiedDate":"2012-02-02T00:08:04","indexId":"ofr96414","displayToPublicDate":"1997-01-10T00:00:00","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":"96-414","title":"Snow-depth and water-equivalent data for the Fairbanks area, Alaska, spring 1995","docAbstract":"Snow depths at 34 sites and snow-water equivalents at 13 sites in the Fairbanks area were monitored during the 1995 snowmelt period (March 30 to April 26) in the spring of 1995. The U.S. Geological Survey conducted this study in cooperation with the Fairbanks International Airport, the University of Alaska Fairbanks, the Alaska Department of Natural Resources-Division of Mining and Water Management, the U.S Army, Alaska, and the U.S. Army Corps of Engineers-Alaska District. These data were collected to provide information about potential recharge of the ground-and surface-water systems during the snowmelt period in the Fairbanks area. This information is needed by companion geohydrologic studies of areas with known or suspected contaminants in the subsurface. Data-collection sites selected had open, boggy, wooded, or brushy vegetation cover and had different slope aspects. The deepest snow at any site, 27.1 inches, was recorded on April 1, 1995; the shallowest snow measured that day was 19.1 inches. The snow-water equivalents at these two sites were 5.9 inches and 4.5 inches, respectively. Snow depths and water equivalents were comparatively greater at open and bog sites than at wooded or brushy sites. Snow depths and water equivalents at all sites decreased throughout the measuring period. The decrease was more rapid at open and boggy sites than at wooded and brushy sites. Snow had completely disappeared from all sites by April 26, 1995.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr96414","issn":"0094-9140","usgsCitation":"Plumb, E., and Lilly, M.R., 1996, Snow-depth and water-equivalent data for the Fairbanks area, Alaska, spring 1995: U.S. Geological Survey Open-File Report 96-414, 16 p.  :ill., maps ;28 cm., https://doi.org/10.3133/ofr96414.","productDescription":"16 p.  :ill., maps ;28 cm.","costCenters":[],"links":[{"id":155522,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0414/report-thumb.jpg"},{"id":53348,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0414/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f0e4b07f02db5edef0","contributors":{"authors":[{"text":"Plumb, E.W.","contributorId":95508,"corporation":false,"usgs":true,"family":"Plumb","given":"E.W.","email":"","affiliations":[],"preferred":false,"id":191491,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lilly, M. R.","contributorId":38594,"corporation":false,"usgs":true,"family":"Lilly","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":191490,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24683,"text":"ofr96224 - 1996 - Sublake geologic structure from high-resolution seismic-reflection data from four sinkhole lakes in the Lake Wales Ridge, central Florida","interactions":[],"lastModifiedDate":"2022-09-23T20:05:03.542062","indexId":"ofr96224","displayToPublicDate":"1997-01-10T00:00:00","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":"96-224","title":"Sublake geologic structure from high-resolution seismic-reflection data from four sinkhole lakes in the Lake Wales Ridge, central Florida","docAbstract":"Seismic-reflection profiles from Lake Wales, Blue Lake, Lake Letta, and Lake Apthorp located along the Lake Wales Ridge in central Florida provide local detail within the regional hydrogeologic framework as described by litho- and hydrostratigraphic cross sections. Lakes located with the mantled karst region have long been considered to be sinkhole lakes, originating from subsidence activity. High-resolution seismic- reflection data confirm this origin for these four lakes. The geologic framework of the Lake Wales Ridge has proven to be a suitable geologic setting for continuous high-resolution seismic-reflection profiling in lakes; however, the nature of the lake-bottom sediments largely controls the quality of the seismic data. In lakes with significant organic-rich bottom deposits, interpretable record was limited to areas where organic deposits were minimal. In lakes with clean, sandy bottoms, the seismic-reflection methods were highly successful in obtaining data that can be correlated with sublake subsidence features. These techniques are useful in examining sublake geology and providing a better understanding of how confining units are affected by subsidence in a region where their continuity is of significant importance to local lake hydrology. Although local geologic control around each lake generally corresponds to the regional geologic framework, local deviations from regional geologic trends occur in sublake areas affected by subsidence activity. Each of the four lakes examined represents a unique set of geologic controls and provides some degree of structural evidence of subsidence activity. Sublake geologic structures identified include: (1) marginal lake sediments dipping into bathymetric lows, (2) lateral discontinuity of confining units including sags and breaches, (3) the disruption and reworking of overlying unconsolidated siliciclastic sediments as they subside into the underlying irregular limestone surface, and (4) sublake regions where confining units appear to remain intact and unaffected by nearby subsidence activity. Each lake likely is underlain by several piping features rather than one large subsidence feature.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96224","usgsCitation":"Tihansky, A., Arthur, J.D., and DeWitt, D., 1996, Sublake geologic structure from high-resolution seismic-reflection data from four sinkhole lakes in the Lake Wales Ridge, central Florida: U.S. Geological Survey Open-File Report 96-224, vi, 72 p., https://doi.org/10.3133/ofr96224.","productDescription":"vi, 72 p.","costCenters":[],"links":[{"id":407287,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18595.htm","linkFileType":{"id":5,"text":"html"}},{"id":157915,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0224/report-thumb.jpg"},{"id":53706,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0224/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","otherGeospatial":"Lake Wales Ridge","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.064,\n              27.034\n            ],\n            [\n              -80.843,\n              27.034\n            ],\n            [\n              -80.843,\n              28.349\n            ],\n            [\n              -82.064,\n              28.349\n            ],\n            [\n              -82.064,\n              27.034\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699c1f","contributors":{"authors":[{"text":"Tihansky, A. B. 0000-0003-1681-1601","orcid":"https://orcid.org/0000-0003-1681-1601","contributorId":77956,"corporation":false,"usgs":true,"family":"Tihansky","given":"A. B.","affiliations":[],"preferred":false,"id":192381,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Arthur, J. D.","contributorId":67924,"corporation":false,"usgs":true,"family":"Arthur","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":192380,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"DeWitt, D.W.","contributorId":55044,"corporation":false,"usgs":true,"family":"DeWitt","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":192379,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":24243,"text":"ofr96424 - 1996 - Drilling and construction data for well 3-3406-13, Kaamooloa exploratory well, Oahu, Hawaii","interactions":[],"lastModifiedDate":"2012-02-02T00:08:09","indexId":"ofr96424","displayToPublicDate":"1997-01-10T00:00:00","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":"96-424","title":"Drilling and construction data for well 3-3406-13, Kaamooloa exploratory well, Oahu, Hawaii","docAbstract":"An exploratory well (Hawaii State well number 3-3406-13) was drilled about 1.6 miles south of the town of Haleiwa. The well is located on agricultural land within the Waialua ground-water area. The well penetrates about 20 feet into a basalt aquifer to an elevation of -10 feet. Well construction information and logs of drilling notes and geologic descriptions for the samples are presented for the well. The well is one of 12 exploratory wells drilled in the north-central Oahu area between July 1993 and May 1994 in cooperation with the Honolulu Board of Water Supply.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr96424","issn":"0094-9140","usgsCitation":"Presley, T., and Oki, D., 1996, Drilling and construction data for well 3-3406-13, Kaamooloa exploratory well, Oahu, Hawaii: U.S. Geological Survey Open-File Report 96-424, iii, 8 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr96424.","productDescription":"iii, 8 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":156591,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0424/report-thumb.jpg"},{"id":53373,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0424/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635b72","contributors":{"authors":[{"text":"Presley, T.K.","contributorId":61858,"corporation":false,"usgs":true,"family":"Presley","given":"T.K.","email":"","affiliations":[],"preferred":false,"id":191552,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oki, D.S.","contributorId":75184,"corporation":false,"usgs":true,"family":"Oki","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":191553,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24245,"text":"ofr96422 - 1996 - Drilling, construction, and aquifer-test data from wells 3-3307-20 and -21, Thompson Corner exploratory wells I and II, Oahu, Hawaii","interactions":[],"lastModifiedDate":"2012-02-02T00:08:12","indexId":"ofr96422","displayToPublicDate":"1997-01-10T00:00:00","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":"96-422","title":"Drilling, construction, and aquifer-test data from wells 3-3307-20 and -21, Thompson Corner exploratory wells I and II, Oahu, Hawaii","docAbstract":"The Thompson Corner exploratory wells I and II (State well numbers 3-3307-20 and -21) were drilled near Thompson Corner, about 2.2 miles south-southwest of the town of Haleiwa. The wells are located on agricultural land in the Waialua ground-water area. The wells are about 50 feet apart and penetrate about 90 feet into the ground water. Aquifer tests were conducted using well 3-3307-20 as a pumping well and well 3-3307-21 as an observation well. Well-construction data, logs of drilling notes, geologic descriptions for the samples, and aquifer-test data are presented for the wells. The wells are two of twelve exploratory wells drilled in the north-central Oahu area between July 1993 and May 1994 in cooperation with the Honolulu Board of Water Supply.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr96422","issn":"0094-9140","usgsCitation":"Presley, T., and Oki, D., 1996, Drilling, construction, and aquifer-test data from wells 3-3307-20 and -21, Thompson Corner exploratory wells I and II, Oahu, Hawaii: U.S. Geological Survey Open-File Report 96-422, iii, 24 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr96422.","productDescription":"iii, 24 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":157011,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0422/report-thumb.jpg"},{"id":53375,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0422/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c01c","contributors":{"authors":[{"text":"Presley, T.K.","contributorId":61858,"corporation":false,"usgs":true,"family":"Presley","given":"T.K.","email":"","affiliations":[],"preferred":false,"id":191556,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oki, D.S.","contributorId":75184,"corporation":false,"usgs":true,"family":"Oki","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":191557,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24869,"text":"ofr96366 - 1996 - Nutrient, sediment, and pesticide data collected at four small agricultural basins in the Beaver Creek watershed, West Tennessee, 1990-1995","interactions":[],"lastModifiedDate":"2012-02-02T00:08:24","indexId":"ofr96366","displayToPublicDate":"1997-01-10T00:00:00","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":"96-366","title":"Nutrient, sediment, and pesticide data collected at four small agricultural basins in the Beaver Creek watershed, West Tennessee, 1990-1995","docAbstract":"In 1989, the U.S. Geological Survey began a cooperative study with the Tennessee Department of Agriculture to assess the impact of agricultural activities on water quality in the Beaver Creek watershed in West Tennessee. Quantification of the transport of nutrients, sediment, and pesticides from agricultural fields was one of the objectives of the study. This report presents nutrient, sediment, and pesticide data collected during selected storm events from 1990 through 1995 at four relatively small, agricultural basins (28 to 422 acres) in the Beaver Creek watershed. Approximately 3,000 water samples (500 to 1,000 at each site) were analyzed for nitrogen and phosphorus species. Total nitrogen (N) concentrations ranged from 0.2 to 41.2 milligrams per liter (mg/L). Median concentrations for samples from each site ranged from 2.0 to 2.7 mg/L for total nitrogen, 1.2 to 1.9 mg/L for organic nitrogen, 0.05 to 0.14 mg/L for ammonia (measured as N), and 0.2 to 0.8 mg/L for nitrate plus nitrite (measured as N). Total phosphorus (P) concentrations ranged from 0.03 to 16.0 mg/L. Median concentrations for samples from each site ranged from 0.80 to 1.2 mg/L for total phosphorus and 0.15 to 0.72 for orthophosphate (measured as P). Approximately 6,000 water samples (1,300 to 1,800 at each site) were analyzed for suspended sediment. Suspended-sediment concentrations ranged from 8.0 to 98,353 mg/L. Concentrations exceeded 1,000 mg/L in 33 percent of the samples collected and exceeded 10,000 mg/L in 6 percent of the samples. Median concentrations ranged from 347 to 713 mg/L at the four sites. Several herbicides and insecticides were detected in water samples. Maximum concentrations detected were 37 micrograms per liter for metolachlor, 3.2 for trifluralin, 150 for fluometuron, and 430 for aldicarb. Aldicarb metabolites were also detected in several samples. The maximum aldicarb sulfoxide and aldicarb sulfone concentrations detected were 68.4 and 14.3 micrograms per liter, respectively.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr96366","issn":"0094-9140","usgsCitation":"Williams, S.D., and Harris, R.M., 1996, Nutrient, sediment, and pesticide data collected at four small agricultural basins in the Beaver Creek watershed, West Tennessee, 1990-1995: U.S. Geological Survey Open-File Report 96-366, iv, 115 p. :ill. ;28 cm., https://doi.org/10.3133/ofr96366.","productDescription":"iv, 115 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":1868,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr96-366","linkFileType":{"id":5,"text":"html"}},{"id":157552,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696753","contributors":{"authors":[{"text":"Williams, Shannon D. swilliam@usgs.gov","contributorId":4133,"corporation":false,"usgs":true,"family":"Williams","given":"Shannon","email":"swilliam@usgs.gov","middleInitial":"D.","affiliations":[{"id":24708,"text":"Lower Mississippi-Gulf Water Science Center","active":true,"usgs":true}],"preferred":true,"id":192712,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harris, Robin M.","contributorId":59838,"corporation":false,"usgs":true,"family":"Harris","given":"Robin","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":192713,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}