{"pageNumber":"4955","pageRowStart":"123850","pageSize":"25","recordCount":184617,"records":[{"id":44480,"text":"wri844360 - 1985 - Ground-water levels in the Columbia River basalt and overlying materials, spring 1983, southeastern Washington","interactions":[],"lastModifiedDate":"2022-05-19T18:40:18.783766","indexId":"wri844360","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4360","title":"Ground-water levels in the Columbia River basalt and overlying materials, spring 1983, southeastern Washington","docAbstract":"A 2 1/2-year study of the Columbia Plateau in Washington was begun in March 1982 to define spatial and temporal variations in dissolved sodium in aquifers of the Columbia River Basalt Group and to relate these variations to the groundwater system and its geologic framework. This report is part of that study and describes groundwater level contours for four major geohydrologic units in southeastern Washington, constructed from water-level data collected from approximately 1,100 wells during the spring of 1983, data from U.S. Geological Survey studies in the area, and other indirect methods. Configuration of the groundwater level contours is controlled by: (1) extent of a geohydrologic unit and geologic structure, (2) recharge from precipitation and surface water bodies, (3) rivers, lakes, and coulees that drain the groundwater system, and (4) hydraulic conductivities of each unit. Upgradient flexures of water level contours north of Connel, Washington, show effects of prolonged irrigation while downgradient flexures in an area south of Potholes Reservoir, in the vicinity of the East Low Irrigation Canal, show the effects of increased man-induced recharge. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844360","usgsCitation":"Bauer, H.H., Vaccaro, J.J., and Lane, R.C., 1985, Ground-water levels in the Columbia River basalt and overlying materials, spring 1983, southeastern Washington: U.S. Geological Survey Water-Resources Investigations Report 84-4360, 4 Plates: 44.10 × 29.00 inches or smaller, https://doi.org/10.3133/wri844360.","productDescription":"4 Plates: 44.10 × 29.00 inches or smaller","costCenters":[],"links":[{"id":134642,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":400826,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36191.htm"},{"id":81838,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4360/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81837,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4360/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81836,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4360/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81835,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4360/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","country":"United States","state":"Washington","otherGeospatial":"Columbia River basalt","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121,\n 45.603\n ],\n [\n -116.903,\n 45.603\n ],\n [\n -116.903,\n 48.2440\n ],\n [\n -121,\n 48.2440\n ],\n [\n -121,\n 45.603\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a384e","contributors":{"authors":[{"text":"Bauer, H. H.","contributorId":85142,"corporation":false,"usgs":true,"family":"Bauer","given":"H.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":229850,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vaccaro, John J. jvaccaro@usgs.gov","contributorId":5848,"corporation":false,"usgs":true,"family":"Vaccaro","given":"John","email":"jvaccaro@usgs.gov","middleInitial":"J.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":229848,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lane, R. C.","contributorId":6421,"corporation":false,"usgs":true,"family":"Lane","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":229849,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":25820,"text":"wri844330 - 1985 - Water quality and streamflow data for the West Fork Trinity River in Fort Worth, Texas","interactions":[],"lastModifiedDate":"2021-11-24T23:02:29.862557","indexId":"wri844330","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4330","title":"Water quality and streamflow data for the West Fork Trinity River in Fort Worth, Texas","docAbstract":"Water-quality data were collected on a 13.6-mile reach of the West Fork Trinity River in Fort Worth, Texas to test a dynamic Lagrangian model. Flow was steady. Loads of dissolved constituents varied with time at the beginning of the study reach and in the reach, primarily because of photosynthesis. River quality was fairly good despite low dissolved oxygen measured in the headwaters and the significant sewage load from the tributaries. Diel and longitudinal trends were defined by sampling at fixed sites and by following dyed parcels of water. Nitrification, deoxygenation, reaeration, and photosynthesis affected the dissolved oxygen balance. Independent estimates of some of the rate coefficients were 0.1 to 0.2, 0.8, and 0 to 3.6 , all per day, for deoxygenation, nitrification, and reaeration, respectively. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844330","usgsCitation":"McCutcheon, S.C., 1985, Water quality and streamflow data for the West Fork Trinity River in Fort Worth, Texas: U.S. Geological Survey Water-Resources Investigations Report 84-4330, ix, 101 p., https://doi.org/10.3133/wri844330.","productDescription":"ix, 101 p.","costCenters":[],"links":[{"id":392127,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36168.htm"},{"id":54571,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4330/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158051,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4330/report-thumb.jpg"}],"country":"United States","state":"Texas","city":"Fort Worth","otherGeospatial":"West Fork Trinity River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -97.32032775878906,\n 32.7428148750609\n ],\n [\n -97.17269897460938,\n 32.7428148750609\n ],\n [\n -97.17269897460938,\n 32.7907379828099\n ],\n [\n -97.32032775878906,\n 32.7907379828099\n ],\n [\n -97.32032775878906,\n 32.7428148750609\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2be4b07f02db6130ce","contributors":{"authors":[{"text":"McCutcheon, S. C.","contributorId":44190,"corporation":false,"usgs":true,"family":"McCutcheon","given":"S.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":195203,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25807,"text":"wri854126 - 1985 - Types, features, and occurrence of sinkholes in the karst of west-central Florida","interactions":[],"lastModifiedDate":"2021-11-04T21:10:48.510868","indexId":"wri854126","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"85-4126","title":"Types, features, and occurrence of sinkholes in the karst of west-central Florida","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854126","usgsCitation":"Sinclair, W., Stewart, J.W., Knutilla, R., Gilboy, A.E., and Miller, R.L., 1985, Types, features, and occurrence of sinkholes in the karst of west-central Florida: U.S. Geological Survey Water-Resources Investigations Report 85-4126, vi, 81 p., https://doi.org/10.3133/wri854126.","productDescription":"vi, 81 p.","costCenters":[],"links":[{"id":391401,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36290.htm"},{"id":158407,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4126/report-thumb.jpg"},{"id":54558,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4126/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.95,\n 26.767\n ],\n [\n -81.25,\n 26.767\n ],\n [\n -81.25,\n 29.1\n ],\n [\n -82.95,\n 29.1\n ],\n [\n -82.95,\n 26.767\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a48e4b07f02db6236b9","contributors":{"authors":[{"text":"Sinclair, W. C.","contributorId":65855,"corporation":false,"usgs":true,"family":"Sinclair","given":"W. C.","affiliations":[],"preferred":false,"id":195158,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stewart, J. W.","contributorId":72774,"corporation":false,"usgs":true,"family":"Stewart","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":195159,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Knutilla, R. L.","contributorId":65451,"corporation":false,"usgs":true,"family":"Knutilla","given":"R. L.","affiliations":[],"preferred":false,"id":195157,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gilboy, A. E.","contributorId":34173,"corporation":false,"usgs":true,"family":"Gilboy","given":"A.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":195155,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Miller, R. L.","contributorId":54178,"corporation":false,"usgs":true,"family":"Miller","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":195156,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":25598,"text":"wri854166 - 1985 - Hydrologic effects of ground- and surface-water withdrawals in the Milford area, Elkhart and Kosciusko counties, Indiana","interactions":[],"lastModifiedDate":"2016-06-01T10:15:07","indexId":"wri854166","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"85-4166","title":"Hydrologic effects of ground- and surface-water withdrawals in the Milford area, Elkhart and Kosciusko counties, Indiana","docAbstract":"

Agricultural irrigation in northern Indiana has increased rapidly since 1975 and might double by the year 2000. A 16.5 square-mile area in north-central Indiana was studied to determine possible effects of increased irrigation on local water supply. In 1982, an average of 2 inches of water was used to irrigate 975 acres of sandy soil overlying highly transmissive outwash deposits. Irrigational pumpage was 75 percent of the summer water use but was less than potential irrigational pumpage because (1) only one-third of the suitable land was irrigated, and (2) precipitation was near normal for the year.

\n

A three-dimensional digital flow model, calibrated with data collected in 1982, was used to simulate four hypothetical pumping plans representing various irrigational schemes and possible rainfall conditions: (1) 1982 acreage irrigated and 1982 (above normal) precipitation; (2) 1982 acreage irrigated and below-normal precipitation; (3) maximum acreage irrigated and normal precipitation; and (4) maximum acreage irrigated and below-normal precipitation. A fifth pumping plan was used to simulate maximum year-round water use. Plan 5 was not designed to simulate irrigational development but rather a maximum rate of withdrawal sustainable year-round until steady-state is reached.

\n

Of the four pumping plans that simulated irrigational pumpage, plan 4 had the greatest effect on ground- and surface-water supply. Compared with 1982 pumpage, this plan represented a thirteenfold increase in the volume of water pumped for irrigation from wells and from Turkey Creek, a stream bordering the area of study. The model predicted a potentiometric decline of as much as 20.7 feet over an 8-acre area of the aquifer. This decline was one-fourth of the available drawdown and would not dewater the source aquifer. Streamflow in Turkey Creek would be reduced 39 percent by simulated ground-water and surface-water pumpage but remaining flow would still be twice the 7-day, 10-year low flow. However, the model predicted that flow in two smaller streams would be reduced to zero.

\n

The rate of pumping used in plan 5 was nearly 4 times the pumping rate in 1982. Potentiometric decline for plan 5 was as much as 40 percent of available drawdown, and predicted streamflow reduction would cause flow in Turkey Creek to decrease below the 7-day, 10-year low flow.

\n

Results of plans 1, 2, 3, and 4 indicate that the outwash system provides adequate water for current (1982) needs and substantial growth for irrigation. However, maximum irrigational development might cause temporary, local competition for water in several parts of the area. Plan 5 indicates .that water use could increase substantially before effects of pumping would prevail year-round.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/wri854166","collaboration":"Indiana Department of Natural Resources","usgsCitation":"Lindgren, H., Peters, J.G., Cohen, D., and Crompton, E., 1985, Hydrologic effects of ground- and surface-water withdrawals in the Milford area, Elkhart and Kosciusko counties, Indiana: U.S. Geological Survey Water-Resources Investigations Report 85-4166, vi, 75 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854166.","productDescription":"vi, 75 p. :ill., maps ;28 cm.","startPage":"1","endPage":"75","numberOfPages":"81","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":54342,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4166/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":126873,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4166/report-thumb.jpg"}],"country":"United States","state":"Indiana","county":"Elkhart, Kosciusko","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-85.7874,41.7615],[-85.7591,41.7613],[-85.6606,41.7608],[-85.6589,41.699],[-85.6575,41.6122],[-85.6554,41.5251],[-85.6542,41.4733],[-85.6552,41.4384],[-85.6538,41.3521],[-85.6527,41.2949],[-85.6518,41.2668],[-85.6522,41.1787],[-85.6876,41.179],[-85.6856,41.0896],[-85.6849,41.0465],[-85.9457,41.0424],[-86.017,41.0414],[-86.0179,41.0863],[-86.0758,41.0851],[-86.0777,41.1736],[-86.0539,41.1735],[-86.0574,41.3033],[-86.059,41.4336],[-86.059,41.4367],[-86.0594,41.4644],[-86.0593,41.474],[-86.0593,41.479],[-86.0592,41.4935],[-86.0598,41.4999],[-86.0624,41.7619],[-85.932,41.7623],[-85.7874,41.7615]]]},\"properties\":{\"name\":\"Elkhart\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db607040","contributors":{"authors":[{"text":"Lindgren, H.A.","contributorId":85627,"corporation":false,"usgs":true,"family":"Lindgren","given":"H.A.","email":"","affiliations":[],"preferred":false,"id":194358,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peters, J. G.","contributorId":56216,"corporation":false,"usgs":true,"family":"Peters","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":194356,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cohen, D.A.","contributorId":17628,"corporation":false,"usgs":true,"family":"Cohen","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":194355,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Crompton, E. J.","contributorId":70412,"corporation":false,"usgs":true,"family":"Crompton","given":"E. J.","affiliations":[],"preferred":false,"id":194357,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":25413,"text":"wri844314 - 1985 - Chemical and isotopic characteristics of brines from three oil- and gas-producing sandstones in eastern Ohio, with applications to the geochemical tracing of brine sources","interactions":[],"lastModifiedDate":"2022-02-14T21:24:14.271237","indexId":"wri844314","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4314","title":"Chemical and isotopic characteristics of brines from three oil- and gas-producing sandstones in eastern Ohio, with applications to the geochemical tracing of brine sources","docAbstract":"Chemical and isotopic characteristics of selected inorganic constituents are reported for brines from the Berea Sandstone of Mississippian age, the Clinton sandstone, Albion Sandstone of Silurian age, and the Rose Run formation of Cambrian and Ordovician age in 24 counties in eastern Ohio. Ionic concentrations of dissolved constituents in brines from these formations generally fall in the following ranges (in millimoles per kilogram of brine): Na, Cl > 1,000; 100 < Ca, Mg < 1,000; 1 < K, Br, Sr, Li, Fe, SO4 < 100; Mn, Zn, Al, I, HCO3, SiO2 < 1. Mean ionic concentrations of Ca, Mg, Na, Cl, K, SO4 and Br, and mean values of density and dissolved solids are significantly different at the 95-percent confidence level in each formation. Only potassium has a unique concentration range in each formation. Selected concentration ratios are identified as potential indicators for geochemical tracing of brines having some history of dilution. The k:Na ratios work best for identifying the source formation of an unidentified brine. Isotopic characteristics of hydrogen and oxygen indicate a meteoric origin for the water matrix of the brines. Sulfur isotopes may have utility for differentiating brines from oxidizing ground water.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri844314","collaboration":"Prepared in cooperation with the Ohio Department of Natural Resources, Division of Oil and Gas","usgsCitation":"Breen, K.J., Angelo, C.G., Masters, R.W., and Sedam, A.C., 1985, Chemical and isotopic characteristics of brines from three oil- and gas-producing sandstones in eastern Ohio, with applications to the geochemical tracing of brine sources (Version 1.1): U.S. Geological Survey Water-Resources Investigations Report 84-4314, v, 58 p., https://doi.org/10.3133/wri844314.","productDescription":"v, 58 p.","costCenters":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"links":[{"id":395945,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36155.htm"},{"id":277993,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/1984/4314/"},{"id":123971,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4314/report-thumb.jpg"}],"country":"United States","state":"Ohio","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -83.083,\n 38.667\n ],\n [\n -80.517,\n 38.667\n ],\n [\n -80.517,\n 41.978\n ],\n [\n -83.083,\n 41.978\n ],\n [\n -83.083,\n 38.667\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"Version 1.1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e4858","contributors":{"authors":[{"text":"Breen, K. J.","contributorId":44176,"corporation":false,"usgs":true,"family":"Breen","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":193582,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Angelo, Clifford G.","contributorId":48596,"corporation":false,"usgs":true,"family":"Angelo","given":"Clifford","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":193583,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Masters, Robert W.","contributorId":32195,"corporation":false,"usgs":true,"family":"Masters","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":193581,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sedam, Alan C.","contributorId":9300,"corporation":false,"usgs":true,"family":"Sedam","given":"Alan","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":193580,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":25444,"text":"wri854111 - 1985 - Development and testing of highway storm-sewer flow measurement and recording system","interactions":[],"lastModifiedDate":"2012-02-02T00:08:17","indexId":"wri854111","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"85-4111","title":"Development and testing of highway storm-sewer flow measurement and recording system","docAbstract":"A comprehensive study and development of measuring instruments and techniques for measuring all components of flow in a storm-sewer drainage system was undertaken by the U.S. Geological Survey under the sponsorship of the Federal Highway Administration. The study involved laboratory and field calibration and testing of measuring flumes, pipe insert meters, weirs, electromagnetic velocity meters as well as the development and calibration of pneumatic-bubbler pressure transducer head measuring systems. Tracer-dilution and acoustic flow meter measurements were used in field verification tests. A single micrologger was used to record data from all the above instruments as well as from a tipping-bucket rain gage and also to activate on command the electromagnetic velocity meter and tracer-dilution systems. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey, WRD,","doi":"10.3133/wri854111","usgsCitation":"Kilpatrick, F.A., Kaehrle, W., Hardee, J., Cordes, E.H., and Landers, M.N., 1985, Development and testing of highway storm-sewer flow measurement and recording system: U.S. Geological Survey Water-Resources Investigations Report 85-4111, xiii, 98 p. :ill. ;28 cm., https://doi.org/10.3133/wri854111.","productDescription":"xiii, 98 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":118776,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4111/report-thumb.jpg"},{"id":54179,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4111/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686725","contributors":{"authors":[{"text":"Kilpatrick, F. A.","contributorId":22319,"corporation":false,"usgs":true,"family":"Kilpatrick","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":193719,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kaehrle, W.R.","contributorId":17650,"corporation":false,"usgs":true,"family":"Kaehrle","given":"W.R.","affiliations":[],"preferred":false,"id":193718,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hardee, Jack","contributorId":99554,"corporation":false,"usgs":true,"family":"Hardee","given":"Jack","email":"","affiliations":[],"preferred":false,"id":193722,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cordes, E. H.","contributorId":49002,"corporation":false,"usgs":true,"family":"Cordes","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":193720,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Landers, M. N.","contributorId":63428,"corporation":false,"usgs":true,"family":"Landers","given":"M.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":193721,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":25508,"text":"wri844145 - 1985 - Fishery survey and related limnological conditions of Williams Lake, Hubbard County, Minnesota","interactions":[],"lastModifiedDate":"2018-04-02T11:36:14","indexId":"wri844145","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4145","title":"Fishery survey and related limnological conditions of Williams Lake, Hubbard County, Minnesota","docAbstract":"

Bluegill (Lepomis macrochirus), pumpkinseed sunfish (Lepomis gibbosus), largemouth bass (Micropterus salmoides), yellow perch (Perca flavescens) rock bass (Amploplites rupestris), black crappie (Pomozis nigromaculatus), and northern pike (Esox lucius) were found in Williams Lake, Hubbard County, Minnesota, during a fishery survey of the lake in late August 1982. The most abundant fish were the bluegills. These fish live in the large littoral zone of the lake; this zone underlies 55% of the surface area of the lake. The most ubiquitous benthic invertebrate in the littoral zone (amphipods) and the most abundant benthic invertebrate (chironomid larvae) were major food sources for the bluegill. Other organisms found in the stomach contents of fish collected in this survey were zooplankton, gastropods, Diptera larvae, odonates, terrestrial insects, and other fish. Daphnia were the only zooplankters of a diverse plankton community that were found in stomach contents. The abundance of fish other than bluegill was typical for a system in which northern pike is the major predator.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lakewood, CO","doi":"10.3133/wri844145","usgsCitation":"Taylor, W., LaBaugh, J.W., Freeberg, M., and Dowling, D., 1985, Fishery survey and related limnological conditions of Williams Lake, Hubbard County, Minnesota: U.S. Geological Survey Water-Resources Investigations Report 84-4145, iv, 25 p., https://doi.org/10.3133/wri844145.","productDescription":"iv, 25 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":123645,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4145/report-thumb.jpg"},{"id":54225,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4145/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","county":"Hubbard County","otherGeospatial":"Williams Lake","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-95.1817,47.4124],[-94.6911,47.4106],[-94.6711,47.4103],[-94.6708,47.3225],[-94.6628,47.3221],[-94.6624,47.1498],[-94.6623,47.1429],[-94.664,46.9771],[-94.6554,46.9772],[-94.6597,46.8041],[-94.7856,46.8058],[-94.8752,46.8063],[-95.1643,46.8072],[-95.1646,46.9789],[-95.1713,46.9788],[-95.1724,47.049],[-95.1696,47.1496],[-95.1694,47.3238],[-95.1827,47.3241],[-95.1817,47.4124]]]},\"properties\":{\"name\":\"Hubbard\",\"state\":\"MN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5ef339","contributors":{"authors":[{"text":"Taylor, W.W.","contributorId":61002,"corporation":false,"usgs":true,"family":"Taylor","given":"W.W.","email":"","affiliations":[],"preferred":false,"id":193984,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LaBaugh, J. W.","contributorId":23484,"corporation":false,"usgs":true,"family":"LaBaugh","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":193983,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Freeberg, M.H.","contributorId":71209,"corporation":false,"usgs":true,"family":"Freeberg","given":"M.H.","email":"","affiliations":[],"preferred":false,"id":193985,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dowling, D.C.","contributorId":84796,"corporation":false,"usgs":true,"family":"Dowling","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":193986,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":25515,"text":"wri844304 - 1985 - Geochemical controls on dissolved sodium in basalt aquifers of the Columbia Plateau, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:20","indexId":"wri844304","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4304","title":"Geochemical controls on dissolved sodium in basalt aquifers of the Columbia Plateau, Washington","docAbstract":"Miocene basaltic aquifers of the Columbia Plateau are the principal source of water for agricultural, domestic, and municipal use in Washington State. Irrigation with groundwaters with relatively high sodium concentrations has been cause for concern in recent years, because of the tendency of such waters to reduce soil permeability. Chemical reactions involving groundwater and the basalts are the primary mechanisms responsible for the input of sodium to groundwater in the plateau. This conclusion is supported by the sequence of secondary alteration products found and by progressive changes in groundwater chemistry with depth and position along regional flow paths. Upgradient and shallow groundwaters have low sodium concentrations and sodium-adsorption ratios (SAR's), and are predominantly calcium sodium bicarbonate waters. Groundwaters from deeper and downgradient locations have higher sodium concentrations and SAR 's and are predominantly sodium bicarbonate water. Volcanic glass and cryptocrystalline matrix are the major sources of groundwater sodium, and are dissolved by a combination of silicate hydrolysis and dissolution by carbonic acid. Magnesium, iron, and calcium are removed from solution by the formation of an iron magnesium smectite, calcite , and amorphous iron oxyhydroxide. The addition of sodium, silicon, and potassium by dissolution of basalt exceeds their removal by the precipitation of secondary minerals, and their concentrations increase in the initial stages of this process. In later stages, these continued increases produce a water saturated with clinoptilolite and silica phases, and these begin to precipitate. While the timing of these processes is unclear, the mineralogy of secondary alteration and estimated cooling rates of the basalt flows suggest that observed alteration products formed primarily at low temperature, under conditions similar to those existing at the present time. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844304","usgsCitation":"Hearn, P., Steinkampf, W., Bortleson, G.C., and Drost, B., 1985, Geochemical controls on dissolved sodium in basalt aquifers of the Columbia Plateau, Washington: U.S. Geological Survey Water-Resources Investigations Report 84-4304, v, 38 p. :ill., maps (one col.) ;28 cm., https://doi.org/10.3133/wri844304.","productDescription":"v, 38 p. :ill., maps (one col.) ;28 cm.","costCenters":[],"links":[{"id":123433,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4304/report-thumb.jpg"},{"id":54231,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4304/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54232,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4304/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae499","contributors":{"authors":[{"text":"Hearn, P.P.","contributorId":18380,"corporation":false,"usgs":true,"family":"Hearn","given":"P.P.","affiliations":[],"preferred":false,"id":194007,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steinkampf, W.C.","contributorId":8137,"corporation":false,"usgs":true,"family":"Steinkampf","given":"W.C.","affiliations":[],"preferred":false,"id":194006,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bortleson, Gilbert C.","contributorId":57472,"corporation":false,"usgs":true,"family":"Bortleson","given":"Gilbert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":194009,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Drost, B. W.","contributorId":38526,"corporation":false,"usgs":true,"family":"Drost","given":"B. W.","affiliations":[],"preferred":false,"id":194008,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":42093,"text":"ofr85752 - 1985 - Aeromagnetic map of the Clan Alpine Mountains, west-central Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:11:10","indexId":"ofr85752","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-752","title":"Aeromagnetic map of the Clan Alpine Mountains, west-central Nevada","language":"ENGLISH","doi":"10.3133/ofr85752","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1985, Aeromagnetic map of the Clan Alpine Mountains, west-central Nevada: U.S. Geological Survey Open-File Report 85-752, 2 maps :photocopy ;44 x 75 cm., on sheets 70 x 92 cm., https://doi.org/10.3133/ofr85752.","productDescription":"2 maps :photocopy ;44 x 75 cm., on sheets 70 x 92 cm.","costCenters":[],"links":[{"id":176104,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79836,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1985/0752/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79837,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1985/0752/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696ef2","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":530826,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":47695,"text":"wri854184 - 1985 - Maps showing ground-water conditions in the Cottonwood Creek area, Shasta and Tehama counties, California, 1983-84","interactions":[],"lastModifiedDate":"2012-02-02T00:10:25","indexId":"wri854184","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"85-4184","title":"Maps showing ground-water conditions in the Cottonwood Creek area, Shasta and Tehama counties, California, 1983-84","language":"ENGLISH","doi":"10.3133/wri854184","usgsCitation":"Evenson, K.D., and Kinsey, W., 1985, Maps showing ground-water conditions in the Cottonwood Creek area, Shasta and Tehama counties, California, 1983-84: U.S. Geological Survey Water-Resources Investigations Report 85-4184, 3 maps on 1 sheet ; 27 x 59 cm. and smaller, sheet 114 x 91 cm., folded in envelope 30 x 23 cm., https://doi.org/10.3133/wri854184.","productDescription":"3 maps on 1 sheet ; 27 x 59 cm. and smaller, sheet 114 x 91 cm., folded in envelope 30 x 23 cm.","costCenters":[],"links":[{"id":169737,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":84605,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4184/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605974","contributors":{"authors":[{"text":"Evenson, Kristin D.","contributorId":42943,"corporation":false,"usgs":true,"family":"Evenson","given":"Kristin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":236032,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kinsey, W.B.","contributorId":33985,"corporation":false,"usgs":true,"family":"Kinsey","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":236031,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2745,"text":"wsp2256A - 1985 - Distribution and transport of trace substances in the Schuylkill River basin from Berne to Philadelphia, Pennsylvania","interactions":[{"subject":{"id":48805,"text":"ofr83265 - 1983 - Distribution and transport of trace substances in the Schuylkill River Basin from Berne to Philadelphia, Pennsylvania","indexId":"ofr83265","publicationYear":"1983","noYear":false,"title":"Distribution and transport of trace substances in the Schuylkill River Basin from Berne to Philadelphia, Pennsylvania"},"predicate":"SUPERSEDED_BY","object":{"id":2745,"text":"wsp2256A - 1985 - Distribution and transport of trace substances in the Schuylkill River basin from Berne to Philadelphia, Pennsylvania","indexId":"wsp2256A","publicationYear":"1985","noYear":false,"chapter":"A","title":"Distribution and transport of trace substances in the Schuylkill River basin from Berne to Philadelphia, Pennsylvania"},"id":1}],"lastModifiedDate":"2017-06-09T08:37:03","indexId":"wsp2256A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2256","chapter":"A","title":"Distribution and transport of trace substances in the Schuylkill River basin from Berne to Philadelphia, Pennsylvania","docAbstract":"During the period from October 1978 to March 1981, the U.S. Geological Survey assessed the river quality of the Schuylkill River basin in Pennsylvania from the headwaters to the Fairmount Dam at Philadelphia (river mile 8.4). The assessment focused on the distribution and transport of trace metals and organic substances (trace substances). Trace metals included were arsenic, beryllium, cadmium, copper, lead, mercury, nickel, and zinc; trace organic substances included organochlorine insecticides and polychlorinated biphenyls. \r\n\r\nIn general, concentrations of trace substances in the streambed sediments were greater in the main stem of the Schuylkill River than in its tributaries and exceeded the background concentrations in the study area. Concentrations of most trace metals in the sediments were lowest in the Berne area (river mile 95) and highest in the urban-industrial area of Reading (river mile 76). Concentrations generally decreased from Reading downstream to Philadelphia (river mile 10.2). Concentrations of the organochlorine insecticides chlordane, DDT and its metabolites, and dieldrin generally increased gradually from Berne to Philadelphia. Average concentrations of trace metals in the main stem of the Schuylkill River in the sediment-sized fraction, less than 0.063 millimeters, were: zinc, 603 ?g/g (micrograms per gram); lead, 284 ?g/g; copper, 252 ?g/g; nickel, 119 ?g/g; chromium, 96 ?g/g; beryllium, 8.2 ?g/g; arsenic, 0.64 ?g/g; and mercury, 0.002 ?g/g. Average concentrations of trace organic substances in sediments of the main stem of the river were: polychlorinated biphenyls, 152 ?g/kg (micrograms per kilogram); chlordane, 24 ?g/kg; DDT and its metabolites, 18 ?g/kg; and dieldrin, 1.8 ?g/kg. \r\n\r\nThe average annual transport of trace substances by the river was computed for chromium, copper, lead, nickel, and zinc. Concentrations of other trace substances in the sediment-water mixtures were generally undetectable. Of the trace metals, average annual transport of zinc was the greatest, and that of nickel was the least. Transport of trace metals in the river is closely associated with and related to suspended-sediment transport. About 71 percent of the average annual total metal transport is particulate material. \r\n\r\nYields, in tons per square mile per year, of copper, lead, zinc, and total organic carbon in the Schuylkill River basin were compared with yields in the Chattahoochee River basin (Georgia). The comparison indicates that yields, by constituent, were of the same order of magnitude. Both basins lie in the Piedmont province, and both have about the same percentage of urban land use.\r\n\r\nThe frequency of occurrence of concentrations of copper, lead, and zinc in the sediment-water mixture at Manayunk in Philadelphia were compared with domestic water-supply criteria of the U.S. Environmental Protection Agency. 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Four closely spaced boreholes were drilled through approximately 20 meters of till into schist bedrock near Mirror Lake, West Thornton, New Hampshire. The site was selected for borehole geophysical research because it is included in a detailed groundwater study where the effects of flow in fractures on flow in overlying drift deposits is being studied. Three of the boreholes are approximately 100 meters in depth, and the fourth is approximately 230 meters in depth. All four boreholes were logged with caliper, acoustic, gamma, single-point-resistivity, and acoustic televiewer logs. Fracture sets dipping approximately 45 degrees to the east were detected in all four boreholes. Two sets of deeper fractures were detected near the bottom of the deepest borehole. Acoustic waveform logs were obtained in all boreholes using three different source frequencies, 34, 15, and 5 kilohertz, for future comparison with surface to borehole seismic data.

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