Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMDDE851","usgsCitation":"James, R., Simmons, R., and Strain, B., 1986, Water resources data Maryland and Delaware, water year 1985: U.S. Geological Survey Water Data Report MD-DE-85-1, 287 p., https://doi.org/10.3133/wdrMDDE851.","productDescription":"287 p.","costCenters":[{"id":41514,"text":"Maryland-Delaware-District of Columbia Water Science Center","active":true,"usgs":true}],"links":[{"id":174926,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1985/md-de-85-1/wdrMDDE851_coverthb.jpg"},{"id":381949,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1985/md-de-85-1/wdrMDDE851.pdf","text":"Report","size":"13.3 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Water Data Report MD-DE-85-1"}],"country":"United States","state":"Delaware, 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\"}}]}","contact":"","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fce38","contributors":{"authors":[{"text":"James, R.W.","contributorId":70434,"corporation":false,"usgs":true,"family":"James","given":"R.W.","affiliations":[],"preferred":false,"id":257156,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simmons, R.H.","contributorId":19982,"corporation":false,"usgs":true,"family":"Simmons","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":257155,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Strain, B.F.","contributorId":76388,"corporation":false,"usgs":true,"family":"Strain","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":257157,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70179994,"text":"70179994 - 1986 - Developing a state water plan: Ground-water conditions in Utah, spring of 1986","interactions":[],"lastModifiedDate":"2017-01-20T17:41:59","indexId":"70179994","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":110,"text":"Cooperative Investigations Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"26","title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1986","docAbstract":"This is the twenty-third in a series of annual reports that describe ground-water conditions in Utah. Reports in this series, published cooperatively by the U.S. Geological Survey and the Utah Division of Water Resources, provide data to enable interested parties to keep abreast of changing ground-water conditions.
This report, like the others in the series, contains information on well construction, ground-water withdrawals from wells, water-level changes, and related changes in precipitation and streamflow. Supplementary data such as graphs showing chemical quality of water and maps showing water-level contours are included in reports of this series only for those years or areas for which applicable data are available and are important to a discussion of changing ground-water conditions.
This report includes individual discussions of selected major areas of ground-water development in the State for the calendar year 1985. Water-level fluctuations, however, are described from the spring of 1985 to the spring of 1986. Much of the data used in this report were collected by the U.S. Geological Survey in cooperation with the Division of Water Rights, Utah Department of Natural Resources.
","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Resources","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the State of Utah","usgsCitation":"Mason, J.L., Smith, G.J., Roark, D.M., Lambert, P.M., Jensen, V., Wilberg, D.E., Burden, C.B., Garrett, R., Emett, D.C., Duncanson, S., Sandberg, G.W., Puchta, R.W., and Herbert, L.R., 1986, Developing a state water plan: Ground-water conditions in Utah, spring of 1986: Cooperative Investigations Report 26, vii, 83 p.","productDescription":"vii, 83 p.","numberOfPages":"92","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333654,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333653,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-179"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5883303be4b0d00231637828","contributors":{"authors":[{"text":"Mason, James L.","contributorId":14397,"corporation":false,"usgs":true,"family":"Mason","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":659589,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, G. J.","contributorId":80767,"corporation":false,"usgs":true,"family":"Smith","given":"G.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":659590,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Roark, D. Michael mroark@usgs.gov","contributorId":127806,"corporation":false,"usgs":true,"family":"Roark","given":"D.","email":"mroark@usgs.gov","middleInitial":"Michael","affiliations":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"preferred":true,"id":659591,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lambert, Patrick M. 0000-0001-6808-2303 plambert@usgs.gov","orcid":"https://orcid.org/0000-0001-6808-2303","contributorId":349,"corporation":false,"usgs":true,"family":"Lambert","given":"Patrick","email":"plambert@usgs.gov","middleInitial":"M.","affiliations":[{"id":38131,"text":"WMA - Office of Planning and Programming","active":true,"usgs":true}],"preferred":true,"id":659592,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Jensen, V.L.","contributorId":99034,"corporation":false,"usgs":true,"family":"Jensen","given":"V.L.","email":"","affiliations":[],"preferred":false,"id":659593,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Wilberg, Dale E.","contributorId":101275,"corporation":false,"usgs":true,"family":"Wilberg","given":"Dale","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":659594,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Burden, Carole B. cburden@usgs.gov","contributorId":852,"corporation":false,"usgs":true,"family":"Burden","given":"Carole","email":"cburden@usgs.gov","middleInitial":"B.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":659595,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Garrett, R. B.","contributorId":35810,"corporation":false,"usgs":true,"family":"Garrett","given":"R. B.","affiliations":[],"preferred":false,"id":659596,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Emett, D. C.","contributorId":21213,"corporation":false,"usgs":true,"family":"Emett","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":659597,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Duncanson, Susan","contributorId":178538,"corporation":false,"usgs":false,"family":"Duncanson","given":"Susan","email":"","affiliations":[],"preferred":false,"id":659598,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Sandberg, G. W.","contributorId":55426,"corporation":false,"usgs":true,"family":"Sandberg","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659599,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Puchta, R. W","contributorId":177482,"corporation":false,"usgs":false,"family":"Puchta","given":"R.","email":"","middleInitial":"W","affiliations":[],"preferred":false,"id":659600,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Herbert, L. R.","contributorId":39865,"corporation":false,"usgs":true,"family":"Herbert","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":659601,"contributorType":{"id":1,"text":"Authors"},"rank":13}]}} ,{"id":70178916,"text":"70178916 - 1986 - Program for monitoring the chemical quality of ground water in Utah – Summary of data collected through 1984","interactions":[],"lastModifiedDate":"2016-12-12T11:33:48","indexId":"70178916","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"88","title":"Program for monitoring the chemical quality of ground water in Utah – Summary of data collected through 1984","docAbstract":"The U.S. Geological Survey formally started a program for monitoring ground-water quality in Utah during 1957 in cooperation with the State of Utah. Most observation wells in the monitoring network are privately owned. Initially, the network consisted of fewer than 50 wells; by 1984, however, it had expanded to include more than 200 wells. Chemical analyses are available for water from some of the wells from as early as 1927, long before those wells were formally added to the network. The monitoring program was initiated to detect any changes in chemical quality that might be associated with the withdrawal of water from wells.
Dissolved-solids concentrations in water samples collected from the observation wells through 1984 ranged from 92 to 19,000 milligrams per liter. An observation well in the Uinta Basin yielded the sample with the smallest dissolved-solids concentration, and another well in the Uinta Basin yielded the sample with the largest dissolved-solids concentration. There was a progressive increase in salinity of water produced by several of the observation wells in Pahvant Valley and in the Milford and Beryl-Enterprise areas. The increases in salinity occurred during 1950-84, coinciding with the decline of water levels due to pumping for irrigation. Water-quality changes related either to ground-water withdrawals or ground-water recharge also were detected in several other areas, including Curlew Valley, Cedar City Valley, Northern Utah Valley, the lower Bear River valley, and the Sevier Desert.
Water produced from wells in Goshen Valley and the upper Fremont River valley had short term increases in chloride, sulfate, and dissolved-solids concentrations, indicating possible local contamination of the ground water. Also, since the late 1950's, dissolved-solids concentrations have increased in water produced by a well completed in the principal aquifer in Salt Lake Valley downgradient from areas where extensive use has been made of road salt.
","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Price, D., and Arnow, T., 1986, Program for monitoring the chemical quality of ground water in Utah – Summary of data collected through 1984: Technical Publication 88, vi, 119 p.","productDescription":"vi, 119 p.","numberOfPages":"126","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":331906,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331904,"rank":1,"type":{"id":15,"text":"Index 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"584fc564e4b00645734c53a5","contributors":{"authors":[{"text":"Price, Don","contributorId":30608,"corporation":false,"usgs":true,"family":"Price","given":"Don","email":"","affiliations":[],"preferred":false,"id":655516,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Arnow, Ted","contributorId":84733,"corporation":false,"usgs":true,"family":"Arnow","given":"Ted","affiliations":[],"preferred":false,"id":655517,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70178906,"text":"70178906 - 1986 - Ground-water conditions in the Kaiparowits Plateau area, Utah and Arizona, with emphasis on the Navajo Sandstone","interactions":[],"lastModifiedDate":"2016-12-12T11:10:13","indexId":"70178906","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"81","title":"Ground-water conditions in the Kaiparowits Plateau area, Utah and Arizona, with emphasis on the Navajo Sandstone","docAbstract":"This report presents results of investigation of ground-water conditions in the Kaiparowits Plateau area of south-central Utah and north-central Arizona (fig. 1). The area is under investigation for development of its large quantities of energy resources, primarily coal. Production and transportation of those energy resources would require attendant development of water resources. The purpose of this study was to determine the availability and quality of ground water in major aquifers in the area - namely aquifers in the Entrada, Navajo, and Wingate Sandstones; emphasis was on the Navajo Sandstone. The study was made by the U.S. Geological Survey in cooperation with the Utah Department of Natural Resources, Division of Water Rights. Field work was done intermittently during July through October 1979, and October 1980 through October 1981.
","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"PreIared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Blanchard, P.J., 1986, Ground-water conditions in the Kaiparowits Plateau area, Utah and Arizona, with emphasis on the Navajo Sandstone: Technical Publication 81, vi, 87 p.","productDescription":"vi, 87 p.","numberOfPages":"95","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":331890,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331887,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-6-100"},{"id":331888,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w92000a6.pdf"}],"country":"United States","state":"Arizona, Utah","county":"Coconino County, Garfield County, Kane County","otherGeospatial":"Kaiparowits Plateau","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.4947509765625,\n 36.9806150652861\n ],\n [\n -111.368408203125,\n 37.055177106660814\n ],\n [\n -111.22558593749999,\n 37.05956083025126\n ],\n [\n -111.15966796875,\n 37.125286284966805\n ],\n [\n -111.0498046875,\n 37.12090636165327\n ],\n [\n -110.91796875,\n 37.16469418870222\n ],\n [\n -110.8740234375,\n 37.243448378654115\n ],\n [\n -110.8575439453125,\n 37.304644804751106\n ],\n [\n -110.885009765625,\n 37.35705927979369\n ],\n [\n -110.81359863281249,\n 37.322120359451766\n ],\n [\n -110.76416015625,\n 37.35269280367274\n ],\n [\n -110.8245849609375,\n 37.431250501793585\n ],\n [\n -110.972900390625,\n 37.714244967649265\n ],\n [\n -111.1102294921875,\n 37.92686760148135\n ],\n [\n -111.24206542968749,\n 38.229550455326134\n ],\n [\n -111.500244140625,\n 38.30718056188316\n ],\n [\n -112.0550537109375,\n 38.09133660751176\n ],\n [\n -112.2967529296875,\n 37.80978395301097\n ],\n [\n -112.47802734375,\n 37.640334898059486\n ],\n [\n -112.5604248046875,\n 37.41816326969145\n ],\n [\n -112.3297119140625,\n 36.901587303978474\n ],\n [\n -112.1978759765625,\n 36.74328605437939\n ],\n [\n -111.884765625,\n 36.686041276581925\n ],\n [\n -111.6265869140625,\n 36.74768773190056\n ],\n [\n -111.4727783203125,\n 36.88840804313823\n ],\n [\n -111.4947509765625,\n 36.9806150652861\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"584fc564e4b00645734c53a7","contributors":{"authors":[{"text":"Blanchard, Paul J.","contributorId":24388,"corporation":false,"usgs":true,"family":"Blanchard","given":"Paul","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":655476,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70176447,"text":"70176447 - 1986 - A history of paleoflood hydrology in the United States","interactions":[],"lastModifiedDate":"2016-09-14T12:29:05","indexId":"70176447","displayToPublicDate":"2016-03-23T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3879,"text":"Eos, Earth and Space Science News","active":true,"publicationSubtype":{"id":10}},"title":"A history of paleoflood hydrology in the United States","docAbstract":"The origins of paleoflood hydrology in the United States can be traced back to the beginning of the 19th century, when windgaps and watergaps in the Applachians were believed to have been eroded by extraordinary floods as large lakes that were ponded behind the ridges rapidly drained. Sediment evidence for extraordinary floods was evoked several decades later when glacial sediments in New England were interpreted as deposits from the great Biblical deluge, and estimates of the depth and velocity of the great flood were attempted. The popularization of the glacial origins of drift by Agassiz by 1840 resulted in strong beliefs in uniformitarianism and waning interests in paleoflood investigations. The documentation of the origins of the channeled scablands in eastern Washington by catastrophic glacial outbreak floods, begun by Bretz in the early 1920s, led to renewed interest in paleoflood hydrology. Subsequent efforts to reconstruct hydraulic variables of past floods used conventional open channel flow equations applied to other enormous Pleistocene floods. The elevation of sediments was used as a paleostage estimator in the 1880s, and botanical techniques for estimating paleoflood frequency and magnitude were well documented by the mid-1960s. Since 1970, an exponential expansion has occurred in the recognition and use of paleoflood hydrology in the United States.
","language":"English","publisher":"American Geophysical Union","publisherLocation":"Washington, D.C.","doi":"10.1029/EO067i017p00425-02","usgsCitation":"Costa, J.E., 1986, A history of paleoflood hydrology in the United States: Eos, Earth and Space Science News, v. 67, no. 17, p. 425-430, https://doi.org/10.1029/EO067i017p00425-02.","productDescription":"4 p.","startPage":"425","endPage":"430","numberOfPages":"4","temporalStart":"1800-01-01","temporalEnd":"1970-12-31","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":328641,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"67","issue":"17","noUsgsAuthors":false,"publicationDate":"2011-06-03","publicationStatus":"PW","scienceBaseUri":"57da74ade4b090824ffb7e0b","contributors":{"authors":[{"text":"Costa, John E.","contributorId":105743,"corporation":false,"usgs":true,"family":"Costa","given":"John","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":648798,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70174615,"text":"70174615 - 1986 - Metabolism of reduced methylated sulfur compounds in anaerobic sediments and by a pure culture of an estuarine methanogen","interactions":[],"lastModifiedDate":"2023-01-26T18:10:44.374029","indexId":"70174615","displayToPublicDate":"2016-01-13T06:45:00","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":850,"text":"Applied and Environmental Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Metabolism of reduced methylated sulfur compounds in anaerobic sediments and by a pure culture of an estuarine methanogen","docAbstract":"Addition of dimethylsulfide (DMS), dimethyldisulfide (DMDS), or methane thiol (MSH) to a diversity of anoxic aquatic sediments (e.g., fresh water, estuarine, alkaline/hypersaline) stimulated methane production. The yield of methane recovered from DMS was often 52 to 63%, although high concentrations of DMS (as well as MSH and DMDS) inhibited methanogenesis in some types of sediments. Production of methane from these reduced methylated sulfur compounds was blocked by 2-bromoethanesulfonic acid. Sulfate did not influence the metabolism of millimolar levels of DMS, DMDS, or MSH added to sediments. However, when DMS was added at ∼2-μM levels as [14C]DMS, metabolism by sediments resulted in a 14CH4/14CO2 ratio of only 0.06. Addition of molybdate increased the ratio to 1.8, while 2-bromoethanesulfonic acid decreased it to 0, but did not block 14CO2 production. These results indicate the methanogens and sulfate reducers compete for DMS when it is present at low concentrations; however, at high concentrations, DMS is a “noncompetitive” substrate for methanogens. Metabolism of DMS by sediments resulted in the appearance of MSH as a transient intermediate. A pure culture of an obligately methylotrophic estuarine methanogen was isolated which was capable of growth on DMS. Metabolism of DMS by the culture also resulted in the transient appearance of MSH, but the organism could grow on neither MSH nor DMDS. The culture metabolized [14C]-DMS to yield a 14CH4/14CO2 ratio of ∼2.8. Reduced methylated sulfur compounds represent a new class of substrates for methanogens and may be potential precursors of methane in a variety of aquatic habitats.
\nCrossbred coho salmon Oncorhynchus kisutch were produced from all possible crosses among three stocks. The relative susceptibility of the progeny to infection by the myxosporean parasite Ceratomyxa shasta was determined by exposure of juvenile fish to Willamette River water that contained the infective stage of the parasite. Susceptibility of coho salmon native to the Columbia River basin to the disease ceratomyxosis was relatively low whereas that of coho salmon from remote locations was relatively high. Susceptibility of crossbred progeny nearly always was intermediate between the susceptibilities of fish from the parental stocks.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1986)115<492:SOPFCA>2.0.CO;2","usgsCitation":"Hemmingsen, A., McIntyre, J., and Fryer, J.L., 1986, Susceptibility of progeny from crosses among three stocks of coho salmon to infection by Ceratomyxa shasta: Transactions of the American Fisheries Society, v. 115, no. 3, p. 492-495, https://doi.org/10.1577/1548-8659(1986)115<492:SOPFCA>2.0.CO;2.","productDescription":"4 p.","startPage":"492","endPage":"495","numberOfPages":"4","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314306,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"115","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5698d4d2e4b0fbd3f7fa4c65","contributors":{"authors":[{"text":"Hemmingsen, A.R.","contributorId":84313,"corporation":false,"usgs":true,"family":"Hemmingsen","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":588664,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McIntyre, J.D.","contributorId":27006,"corporation":false,"usgs":true,"family":"McIntyre","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":588665,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fryer, J. L.","contributorId":21900,"corporation":false,"usgs":true,"family":"Fryer","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":588666,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70157450,"text":"70157450 - 1986 - Hydrogeology and ground-water use and quality, Brown County, Wisconsin","interactions":[],"lastModifiedDate":"2018-01-08T19:27:03","indexId":"70157450","displayToPublicDate":"2015-04-06T04:30:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5596,"text":"Wisconsin Geological & Natural History Survey Information Circular","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"57","title":"Hydrogeology and ground-water use and quality, Brown County, Wisconsin","docAbstract":"The Paleozoic rock of Brown County includes formations of Cambrian, Ordovician, and Silurian age. These formations are eastward-dipping sedimentary rock that rest on Precambrian crystalline rock and are overlain by Pleistocene deposits. The units that are the principal sources of ground water were grouped into three aquifers (upper, St. Peter, and Elk Mound), and the less permeable units are grouped into three confining units (Maquoketa-Sinnipee, St. Lawrence, and Precambrian). The geologic and hydraulic characteristics of the aquifers and confining units are estimated from logs of more than 1,000 Brown County wells, from results of a packer test, and from published values.
\nRecharge to the water table, which was estimated at five monitored sites, ranges from 1 to 6 inches a year; most recharge is contributed by spring snowmelt and rainfall. A cone of depression caused by pumping the deeper aquifers in the Green Bay metropolitan area induces flow from the upper aquifer to the underlying st. Peter aquifer throughout most of the county. Several reaches of Duck Creek and the Suamico River also contribute water to the aquifers. A
\nbout 13 million gallons per day of ground water was pumped in Brown County during 1979, 63 percent of which was from wells open to both the St. Peter and Elk Mound aquifers. Municipal and industrial water users pumped 9.44 million gallons per day or 72 percent of the ground water withdrawn in 1979.
\nMost ground :water in the county is a calcium magnesium bicarbonate type. However, water from wells sampled in an area between the Fox River and Silurian escarpment have elevated levels of sodium (44 milligrams per liter) and sulfate (226 milligrams per liter). Water from wells that tap rocks older than Silurian dolomite contains high concentrations of strontium (more than 2.4 milligrams per liter) and fluoride (more than 0.85 milligrams per liter).
\nA three-dimensional digital model was used to simulate flow in the ground-water system. Model results indicate that sources of ground water pumped from wells tapping the St. Peter and Elk Mound aquifers in Brown County, 1979, include 4.8 million gallons per day of underflow, most of which enters the county across the west border; 1.9 million gallons per day of flow from vertical leakage within the county; and 1.5 million gallons per day from storage. The model is most sensitive to the horizontal hydraulic conductivity of the upper aquifer. Vertical hydraulic conductivity of the confining units and recharge rates to the water-table aquifer are the least well-defined model parameters.
","language":"English","publisher":"Wisconsin Geological & Natural History Survey","collaboration":"In cooperation with the University of Wisconsin-Extension, Geological and Natural History Survey","usgsCitation":"Krohelski, J.T., and Brown, B., 1986, Hydrogeology and ground-water use and quality, Brown County, Wisconsin: Wisconsin Geological & Natural History Survey Information Circular 57, v, 42 p.","productDescription":"v, 42 p.","numberOfPages":"49","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308459,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":350385,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://wgnhs.uwex.edu/pubs/download_ic57/"}],"country":"United States","state":"Wisconsin","county":"Brown County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-87.9887,44.6778],[-87.9888,44.6728],[-87.9901,44.6719],[-87.9907,44.6719],[-87.9914,44.6719],[-87.9932,44.6751],[-87.9939,44.6751],[-87.9952,44.6751],[-87.9958,44.6747],[-87.9971,44.6719],[-87.9991,44.672],[-88.0029,44.6738],[-88.0061,44.6743],[-88.0067,44.6739],[-88.0074,44.6734],[-88.008,44.673],[-88.0074,44.6716],[-88.0062,44.6702],[-88.0005,44.6679],[-87.9998,44.6674],[-87.9998,44.6665],[-88.0005,44.6651],[-88.0012,44.6647],[-88.0018,44.6647],[-88.0075,44.6679],[-88.0082,44.6679],[-88.0088,44.6675],[-88.0082,44.6638],[-88.009,44.6575],[-88.0099,44.6461],[-88.0106,44.6456],[-88.0112,44.6456],[-88.0144,44.6466],[-88.0151,44.6466],[-88.0151,44.6457],[-88.0145,44.6429],[-88.0145,44.642],[-88.0191,44.6352],[-88.0185,44.6343],[-88.0153,44.6338],[-88.0147,44.6334],[-88.0117,44.6251],[-88.0074,44.6141],[-88.0068,44.6132],[-88.0004,44.6118],[-87.9941,44.6067],[-87.9816,44.5947],[-87.9797,44.5933],[-87.979,44.5924],[-87.9798,44.5878],[-87.9805,44.5828],[-87.9818,44.5824],[-87.983,44.5892],[-87.9848,44.591],[-87.9861,44.5943],[-87.9898,44.6002],[-88.0012,44.6077],[-88.0082,44.61],[-88.0088,44.61],[-88.0101,44.61],[-88.0107,44.6105],[-88.0107,44.6119],[-88.0136,44.6228],[-88.0149,44.6238],[-88.0155,44.6247],[-88.0162,44.6247],[-88.0168,44.6247],[-88.0175,44.6234],[-88.0182,44.6188],[-88.0178,44.6092],[-88.0187,44.5974],[-88.0188,44.5946],[-88.0207,44.5937],[-88.0214,44.5924],[-88.0214,44.5901],[-88.019,44.585],[-88.0204,44.5782],[-88.0191,44.5782],[-88.0185,44.5759],[-88.0173,44.5745],[-88.0179,44.5732],[-88.0192,44.5723],[-88.0211,44.5737],[-88.0217,44.5755],[-88.0237,44.5755],[-88.0269,44.5746],[-88.0365,44.577],[-88.039,44.5766],[-88.0462,44.5726],[-88.0468,44.5717],[-88.0475,44.5694],[-88.0476,44.5658],[-88.0451,44.5644],[-88.0425,44.5639],[-88.0406,44.5648],[-88.0399,44.5675],[-88.0386,44.5684],[-88.0335,44.5665],[-88.0284,44.5637],[-88.0259,44.5614],[-88.0234,44.56],[-88.0234,44.5591],[-88.0247,44.5582],[-88.0266,44.5573],[-88.0286,44.5569],[-88.0337,44.5583],[-88.0349,44.5583],[-88.0356,44.5574],[-88.0356,44.5565],[-88.0287,44.5514],[-88.0255,44.5495],[-88.0249,44.5486],[-88.0249,44.5477],[-88.0249,44.5463],[-88.0218,44.5445],[-88.0212,44.5436],[-88.0212,44.5427],[-88.0218,44.5422],[-88.027,44.5391],[-88.0264,44.5386],[-88.0245,44.5386],[-88.0226,44.5386],[-88.02,44.5399],[-88.018,44.5435],[-88.0167,44.544],[-88.0154,44.5435],[-88.0142,44.5417],[-88.0116,44.5407],[-88.0046,44.5393],[-87.9925,44.5337],[-87.9811,44.5303],[-87.9664,44.5284],[-87.9504,44.5277],[-87.9401,44.529],[-87.9343,44.5316],[-87.931,44.5348],[-87.927,44.5416],[-87.9244,44.5429],[-87.9171,44.5529],[-87.9105,44.5605],[-87.9079,44.5628],[-87.9053,44.5664],[-87.9052,44.5682],[-87.9045,44.571],[-87.9031,44.575],[-87.905,44.5755],[-87.9095,44.576],[-87.914,44.5743],[-87.916,44.5743],[-87.9172,44.5752],[-87.9172,44.5761],[-87.9094,44.5797],[-87.9036,44.5819],[-87.8964,44.5864],[-87.8918,44.5918],[-87.886,44.5963],[-87.8839,44.6026],[-87.8813,44.6049],[-87.8741,44.6085],[-87.8695,44.6139],[-87.861,44.6188],[-87.8585,44.6192],[-87.8565,44.6187],[-87.8527,44.6178],[-87.8495,44.6173],[-87.8463,44.6177],[-87.8262,44.6284],[-87.8177,44.6338],[-87.8131,44.636],[-87.806,44.6373],[-87.7919,44.638],[-87.7823,44.6374],[-87.7732,44.6396],[-87.7706,44.6414],[-87.7654,44.645],[-87.7628,44.6477],[-87.7643,44.5888],[-87.7646,44.5017],[-87.7655,44.4146],[-87.7665,44.3271],[-87.8879,44.3277],[-87.888,44.2402],[-87.9238,44.2402],[-88.0099,44.2407],[-88.0431,44.2411],[-88.1317,44.2411],[-88.163,44.2414],[-88.193,44.2421],[-88.1919,44.3288],[-88.1921,44.3871],[-88.1921,44.4167],[-88.1918,44.5016],[-88.1908,44.5864],[-88.2203,44.5858],[-88.2453,44.5846],[-88.2446,44.6239],[-88.2432,44.664],[-88.2528,44.6641],[-88.2525,44.6846],[-88.2435,44.6845],[-88.2287,44.6844],[-88.2289,44.6725],[-88.1833,44.6734],[-88.1312,44.677],[-88.0092,44.6775],[-87.9887,44.6778]]]},\"properties\":{\"name\":\"Brown\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5603cd44e4b03bc34f544b0e","contributors":{"authors":[{"text":"Krohelski, J. T.","contributorId":59046,"corporation":false,"usgs":true,"family":"Krohelski","given":"J.","email":"","middleInitial":"T.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":573205,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, B.A.","contributorId":147913,"corporation":false,"usgs":false,"family":"Brown","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":573206,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70046142,"text":"70046142 - 1986 - Geohydrology of the Vamoosa-Ada aquifer east-central Oklahoma with a section on chemical quality of water","interactions":[{"subject":{"id":8675,"text":"ofr77487 - 1977 - Hydrologic data for the Vamoosa Aquifer, east-central Oklahoma","indexId":"ofr77487","publicationYear":"1977","noYear":false,"title":"Hydrologic data for the Vamoosa Aquifer, east-central Oklahoma"},"predicate":"SUPERSEDED_BY","object":{"id":70046142,"text":"70046142 - 1986 - Geohydrology of the Vamoosa-Ada aquifer east-central Oklahoma with a section on chemical quality of water","indexId":"70046142","publicationYear":"1986","noYear":false,"title":"Geohydrology of the Vamoosa-Ada aquifer east-central Oklahoma with a section on chemical quality of water"},"id":1}],"lastModifiedDate":"2023-09-20T00:19:18.616106","indexId":"70046142","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":244,"text":"Circular","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"87","title":"Geohydrology of the Vamoosa-Ada aquifer east-central Oklahoma with a section on chemical quality of water","docAbstract":"The Vamoosa-Ada aquifer, which underlies an area of about 2,320 mi2, consists principally of the Vamoosa Formation and the overlying Ada Group of Pennsylvanian age. Rocks comprising the aquifer were deposited in a nearshore environment ranging from marine on the west to nonmarine on the east. Because of changes in depositional environments with time and from place to place, the aquifer is a complex sequence of fine- to very fine-grained sandstone, siltstone, shale, and conglomerate, with interbedded very thin limestone. The aggregate thickness of water-bearing sandstones is greatest south of the Cimarron River, where it reaches a maximum of 550 ft in the vicinity of Seminole. North of the Cimarron River, the average aggregate thickness of the sandstones is about 100 ft, but locally it may be as much as 200 ft. Transmissivity values derived from seven aquifer tests made for this study range from 70 to 490 ft2 per day; values decrease from south to north with decreasing sandstone thickness. Hydraulic-conductivity values range from 2 to 4 ft per day. Storage coefficients for the confined part of the aquifer, as determined from four aquifer tests made during 1944, have an average value of 0.0002. The average storage coefficient for the unconfined part of the aquifer is estimated at 0.12, based on an analysis of geophysical logs and grain-size data. The specific capacity of wells tested is generally less than 1 gallon per minute per foot of drawdown. An approximate hydrologic budget for the aquifer for 1975 gives values, in acre-feet per year, of 93,000 for recharge, 233,000 for runoff, and 2,003,000 for evapotranspiration. The total of these values is almost equal to the average annual precipitation of 2,330,000 acre-ft per year. The estimated amount of water containing a maximum of 1,500 milligrams per liter of dissolved solids stored in the aquifer is estimated at 60 million acre-ft. Of this amount, an estimated 36 million acre-ft is available for use. The quality of water in the Vamoosa-Ada aquifer generally is suitable for municipal, domestic, and stock use. Of 55 water samples analyzed in the laboratory, about 75 percent were of the sodium bicarbonate or sodium calcium bicarbonate type; the remainder were of the sodium sulfate, calcium sulfate, sodium chloride, or indeterminate types. Laboratory and on-site chemical-quality data indicate that mineralization of both ground and surface waters is greater than normal in some areas. Water samples from 7 wells and 12 stream sites had concentrations of bromide exceeding 1 milligram per liter; the only known source of bromide in the area is brine associated with petroleum production.","language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Reston, VA","collaboration":"Prepared by the United States Geological Survey in cooperation with the Oklahoma Geological Survey","usgsCitation":"D’Lugosz, J.J., McClaflin, R.G., and Marcher, M.V., 1986, Geohydrology of the Vamoosa-Ada aquifer east-central Oklahoma with a section on chemical quality of water: Circular 87, vi, 42 p.; Maps: 3 Sheets: 40 x 44 inches.","productDescription":"vi, 42 p.; Maps: 3 Sheets: 40 x 44 inches","numberOfPages":"48","costCenters":[{"id":634,"text":"Water Resources Program","active":false,"usgs":true}],"links":[{"id":272929,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.ou.edu/ogs/publications/circulars/circularssearch"},{"id":272933,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70046142.png"}],"country":"United States","state":"Oklahoma","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,33.62 ], [ -103.0,37.0 ], [ -94.43,37.0 ], [ -94.43,33.62 ], [ -103.0,33.62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51a5d1e9e4b0605bc571efbc","contributors":{"authors":[{"text":"D’Lugosz, Joseph J.","contributorId":71172,"corporation":false,"usgs":true,"family":"D’Lugosz","given":"Joseph","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":479029,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McClaflin, Roger G.","contributorId":50157,"corporation":false,"usgs":true,"family":"McClaflin","given":"Roger","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":479028,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Marcher, Melvin V.","contributorId":11590,"corporation":false,"usgs":true,"family":"Marcher","given":"Melvin","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":479027,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70044044,"text":"70044044 - 1986 - Ground-water conditions in the Lake Powell area, Utah","interactions":[{"subject":{"id":48910,"text":"ofr8593 - 1986 - Ground-water conditions in the Lake Powell area, Utah","indexId":"ofr8593","publicationYear":"1986","noYear":false,"title":"Ground-water conditions in the Lake Powell area, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70044044,"text":"70044044 - 1986 - Ground-water conditions in the Lake Powell area, Utah","indexId":"70044044","publicationYear":"1986","noYear":false,"title":"Ground-water conditions in the Lake Powell area, Utah"},"id":1}],"lastModifiedDate":"2016-12-17T10:58:15","indexId":"70044044","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"84","title":"Ground-water conditions in the Lake Powell area, Utah","docAbstract":"The Lake Powell area comprises about 2,450 square miles in south-central Utah. It is subdivided into three geographical areas by the Colorado and San Juan Rivers. The Henry Mountains area is north of the Colorado River, the Navajo Mountain area is south of the San Juan River, and the third area is between the Colorado and San Juan Rivers.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with The Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Blanchard, P.J., 1986, Ground-water conditions in the Lake Powell area, Utah: Technical Publication 84, vi, 64 p.","productDescription":"vi, 64 p.","numberOfPages":"70","costCenters":[{"id":610,"text":"Utah Water Science 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37.00035919622158\n ]\n ]\n ]\n }\n }\n ]\n}","publicComments":"This report supersedes open-file report 85-93.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"512c960fe4b0855fde6697bd","contributors":{"authors":[{"text":"Blanchard, Paul J.","contributorId":24388,"corporation":false,"usgs":true,"family":"Blanchard","given":"Paul","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":474688,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70044030,"text":"70044030 - 1986 - Water resources of the Park City area, Utah, with emphasis on ground water","interactions":[{"subject":{"id":14181,"text":"ofr85638 - 1985 - Water resources of the Park City area, Utah, with emphasis on ground water","indexId":"ofr85638","publicationYear":"1985","noYear":false,"title":"Water resources of the Park City area, Utah, with emphasis on ground water"},"predicate":"SUPERSEDED_BY","object":{"id":70044030,"text":"70044030 - 1986 - Water resources of the Park City area, Utah, with emphasis on ground water","indexId":"70044030","publicationYear":"1986","noYear":false,"title":"Water resources of the Park City area, Utah, with emphasis on ground water"},"id":1}],"lastModifiedDate":"2016-12-13T09:32:51","indexId":"70044030","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"85","title":"Water resources of the Park City area, Utah, with emphasis on ground water","docAbstract":"The Park City area is a rapidly growing residential and recreational area about 30 miles east of Sal t Lake City (fig. 1). The area of study is about 140 square miles in which the principle industries are agriculture, skiing, and other recreational activities. The area once was a major lead- and silver-mining district, but no mines were active in 1984. A resumption in mining activity, however, could take place with an increase in the price of metals.
The population of the Park City area is expected to increase rapidly in the near future; and the provision of an adequate water supply for the growing population, while avoiding harmful affects of development, is a major concern for local municipalities, developers, and the Utah Division of Water Rights. In addition, agricultural interests in and below the area are concerned about the effects of increased ground-water withdrawals on streamflow, which is fully appropriated by downstream users. The area also contains the proposed site for the Jordanelle dam, a part of the Bonneville unit of the central Utah Project. The damsite is near an historic mining area; and mining companies are concerned that if mining is resumed, the reservoir may create some additional dewatering problems in the mines.
","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources, Division of Water Rights","usgsCitation":"Holmes, W.F., Thompson, K.R., and Enright, M., 1986, Water resources of the Park City area, Utah, with emphasis on ground water: Technical Publication 85, vi, 82 p.","productDescription":"vi, 82 p.","numberOfPages":"90","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":268267,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268266,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w92000aa.pdf"},{"id":332012,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-6-170"}],"country":"United States","state":"Utah","city":"Park City","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.8792724609375,\n 40.44694705960048\n ],\n [\n -111.8792724609375,\n 41.025499378313754\n ],\n [\n -111.1376953125,\n 41.025499378313754\n ],\n [\n -111.1376953125,\n 40.44694705960048\n ],\n [\n -111.8792724609375,\n 40.44694705960048\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"512c9623e4b0855fde669820","contributors":{"authors":[{"text":"Holmes, Walter F.","contributorId":31737,"corporation":false,"usgs":true,"family":"Holmes","given":"Walter","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":474673,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, Kendall R.","contributorId":100854,"corporation":false,"usgs":true,"family":"Thompson","given":"Kendall","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":474675,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Enright, Michael","contributorId":99979,"corporation":false,"usgs":true,"family":"Enright","given":"Michael","email":"","affiliations":[],"preferred":false,"id":474674,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70043186,"text":"70043186 - 1986 - Bedrock aquifers of eastern San Juan County, Utah","interactions":[{"subject":{"id":12494,"text":"ofr85568 - 1985 - Bedrock aquifers of eastern San Juan County, Utah","indexId":"ofr85568","publicationYear":"1985","noYear":false,"title":"Bedrock aquifers of eastern San Juan County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043186,"text":"70043186 - 1986 - Bedrock aquifers of eastern San Juan County, Utah","indexId":"70043186","publicationYear":"1986","noYear":false,"title":"Bedrock aquifers of eastern San Juan County, Utah"},"id":1}],"lastModifiedDate":"2016-12-13T09:44:27","indexId":"70043186","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"86","title":"Bedrock aquifers of eastern San Juan County, Utah","docAbstract":"This study is one of a series of studies appraising the waterbearing properties of the Navajo Sandstone and associated formations in southern Utah. The stu<¥ area is al:x>dy area is about 4,600 square miles, extending from the Utah-Arizona State line northward to the San Juan-Grand County line and westward from the Utah-Colorado State line to the longitude of about 109°50'.
Some of the water-yielding formations are grouped into aquifer systems. The C aquifer is comprised of the DeChelly Sandstone Member of the Cutler Formation. The P aquifer is comprised of the Cedar Mesa Member of the Cutler Formation and the undifferentiated Cutler Formation. The N aquifer is comprised of the sedimentary section that includes the Wingate Sandstone, Kayenta Formation, Navajo Sandstone, Carmel Formation, and Entrada sandstone. The M aquifer is comprised of the Bluff Sandstone Member and other sandstone units of the Morrison Formation. The D aquifer is comprised of the Burro Canyon Formation and Dakota Sandstone. Discharge from the ground-water reservoir to the San Juan River between gaging stations at Four Corners and Mexican Hat is about 66 cubic feet per second.
The N aquifer is the main aquifer in the study area. Recharge by infiltration of precipitation is estimated to be 25,000 acre-feet per year. A major ground-water divide exists under the broad area east of Monticello. The thickness of the N aquifer, where the sedimentary section is fully preserved and saturated, generally is 750 to 1,250 feet. Hydraulic conductivity values obtained from aquifer tests range from 0.02 to 0.34 foot per day. The total volume of water in transient storage is about 11 million acre-feet. Well discharge somewhat exceeded 2,340 acre-feet during 1981. Discharge to the San Juan River from the N aquifer is estimated to be 6.9 cubic feet per second. Water quality ranges from a calcium bicarbonate to sodium chloride type water
","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the Unites States Geological Survey in cooperation with the Utah Department of Natural Resources and Energy Division of Water Rights","usgsCitation":"Avery, C., 1986, Bedrock aquifers of eastern San Juan County, Utah: Technical Publication 86, viii, 114 p.","productDescription":"viii, 114 p.","numberOfPages":"125","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267104,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":332013,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-6-200"},{"id":332014,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w92000ab.pdf"}],"country":"United States","state":"Utah","county":"San Juan County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.918212890625,\n 37.00255267215955\n ],\n [\n -109.918212890625,\n 38.74123075381228\n ],\n [\n -109.0447998046875,\n 38.74123075381228\n ],\n [\n -109.0447998046875,\n 37.00255267215955\n ],\n [\n -109.918212890625,\n 37.00255267215955\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5114dafce4b0ca7af0743b0c","contributors":{"authors":[{"text":"Avery, Charles","contributorId":70739,"corporation":false,"usgs":true,"family":"Avery","given":"Charles","affiliations":[],"preferred":false,"id":473124,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70044324,"text":"70044324 - 1986 - Effects of brine on the chemical quality of water in parts of Creek, Lincoln, Okfuskee, Payne, Pottawatomie, and Seminole Counties, Oklahoma","interactions":[{"subject":{"id":20205,"text":"ofr84445 - 1984 - Effects of brine on the chemical quality of water in parts of Creek, Lincoln, Okfuskee, Payne, Pottawatomie, and Seminole counties, Oklahoma","indexId":"ofr84445","publicationYear":"1984","noYear":false,"title":"Effects of brine on the chemical quality of water in parts of Creek, Lincoln, Okfuskee, Payne, Pottawatomie, and Seminole counties, Oklahoma"},"predicate":"SUPERSEDED_BY","object":{"id":70044324,"text":"70044324 - 1986 - Effects of brine on the chemical quality of water in parts of Creek, Lincoln, Okfuskee, Payne, Pottawatomie, and Seminole Counties, Oklahoma","indexId":"70044324","publicationYear":"1986","noYear":false,"title":"Effects of brine on the chemical quality of water in parts of Creek, Lincoln, Okfuskee, Payne, Pottawatomie, and Seminole Counties, Oklahoma"},"id":1}],"lastModifiedDate":"2013-03-02T14:44:35","indexId":"70044324","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":244,"text":"Circular","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"89","title":"Effects of brine on the chemical quality of water in parts of Creek, Lincoln, Okfuskee, Payne, Pottawatomie, and Seminole Counties, Oklahoma","docAbstract":"A study of water-quality degradation due to brine contamination was made in an area of ~1,700 mi2 in east-central Oklahoma. The study area coincides in part with the outcrop of the Vamoosa-Ada aquifer of Pennsylvanian age.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","collaboration":"Prepared by the United States Geological Survey in cooperation with the Oklahoma Geological Survey","usgsCitation":"Morton, R.B., 1986, Effects of brine on the chemical quality of water in parts of Creek, Lincoln, Okfuskee, Payne, Pottawatomie, and Seminole Counties, Oklahoma: Circular 89, iii, 38 p.; Map: 1 Sheet.","productDescription":"iii, 38 p.; Map: 1 Sheet","startPage":"i","endPage":"38","numberOfPages":"42","costCenters":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"links":[{"id":268663,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268661,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/circular89mm.pdf"},{"id":268662,"type":{"id":17,"text":"Plate"},"url":"https://www.ogs.ou.edu/pubsscanned/CircularsPlates/C89P1.pdf"}],"country":"United States","state":"Oklahoma","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,33.62 ], [ -103.0,37.0 ], [ -94.43,37.0 ], [ -94.43,33.62 ], [ -103.0,33.62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51332d74e4b0c316aaf0681d","contributors":{"authors":[{"text":"Morton, Robert B.","contributorId":50899,"corporation":false,"usgs":true,"family":"Morton","given":"Robert","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":475292,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70038342,"text":"70038342 - 1986 - Water resources inventory of Connecticut Part 9: Farmington River basin","interactions":[],"lastModifiedDate":"2015-11-30T10:06:57","indexId":"70038342","displayToPublicDate":"2012-05-01T10:47:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":108,"text":"Connecticut Water Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"29","title":"Water resources inventory of Connecticut Part 9: Farmington River basin","docAbstract":"The Farmington River basin covers 435 square miles in north-central Connecticut upstream from Tariffville and downstream of the Massachusetts state line. Most water in the basin is derived from precipitation, which averages 48 inches (366 billion gallons) per year. An additional 67 billion gallons of water per year enters the basin from Massachusetts in the West Branch of the Farmington River, Hubbard River, Valley Brook and some smaller streams. Of the total 433 billion gallons, 174 billion gallons returns to the atmosphere through evaporation and transpiration. 239 billion gallons flows out of the study area in the Farmington River at Tariffville, and 20 billion gallons is diverted for Hartford water supply. Variations in streamflow at 23 continuous-record gaging stations are summarized in standardized graphs and tables that can be used to estimate streamflow characteristics at other sites. For example, mean flow and low-flow characteristics such as the 7-day annual minimum flow for 2-year and 10-year recurrence intervals, have been determined for many partial-record stations from the data for the 23 continuous-record stations. Of the 31 principal lakes, ponds, and reservoirs in the basin, eight have usable storage capacities of more than 1 billion gallons. Two of the largest, Colebrook River Lake and Barkhamsted Reservoir, have more than 30 billion gallons usable storage. Floods have occurred in the area in every month of the year. The greatest known flood on the Farmington River was in August 1955, which had a peak flow of 140,000 cubic feet per second at Collinsville. Since then, three major floodcontrol reservoirs have been constructed to reduce the hazards of high streamflow. The major aquifers underlying the basin are composed of unconsolidated materials (stratified drift and till) and bedrock (sedimentary, igneous, and metamorphic). Stratified drift overlies till and bedrock in valleys and lowlands; it averages about 90 feet in thickness, and is capable of large sustained yields of water to individual wells. Based on hydrologic characteristics and available recharge, sixteen stratified-drift areas are selected as the most favorable for large-scale development. Potential yields can be estimated by several methods. Small water supplies can be obtained from all aquifers. Wells in bedrock yield at least one to two gallons per minute at most sites. The probability of adequate yields for domestic supply is greater from sedimentary than from crystalline bedrock and is also greater from stratified-drift overburden than from till. The quality of water from all sources in the basin is good except where adversely affected by swamp drainage, aquifer composition or human activities. The water is generally low in dissolved-solids concentration and is soft to moderately hard. Surface water is less mineralized than ground water, especially during high-flow conditions when it is primarily direct runoff. Samples of water collected from 20 streams during high flow had 34 mg/L median dissolved-solids concentration and 16 mg/L median hardness. Samples collected from the same sites at low flow had 52 mg/L median dissolved solids and 28 mg/L median hardness. In contrast, water from wells had 112 mg/L median dissolved-solids concentration and 60 mg/L median hardness. Iron and manganese occur in objectionable concentrations ~n a few parts of the basin where streams drain swamps and aquifers are rich in iron- and manganese-bearing minerals. Five percent of streams at high flow, 21 percent at low flow, and 7 percent of ground-water samples contained iron in sufficient concentration to cause stains on plumbing fixtures and laundry. Human activities have modified the quality of water in parts of the basin. The high bacterial content of the Pequabuck River. and the high nitrate and chloride concentrations in some ground-water samples, are evidence of man’s influence. The quantity and quality of water in the basin’s streams and aquifers are satisfactory for a wide variety of uses. and, with suitable treatment, may be used for most purposes. The total amount of water used by 21 principal public supplies within the basin was 29 billion gallons in 1970. About 70 percent of this was used for domestic and commercial purposes, and nearly 30 percent was used by industry. Analyses of water from these systems show good quality.
","language":"English","publisher":"Connecticut Department of Environmental Protection","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Connecticut Department of Environmental Protection","usgsCitation":"Handman, E.H., Haeni, F.P., and Thomas, M.P., 1986, Water resources inventory of Connecticut Part 9: Farmington River basin: Connecticut Water Resources Bulletin 29, Report: viii, 91 p.; 4 Plates: 38.67 x 42.36 inches and smaller.","productDescription":"Report: viii, 91 p.; 4 Plates: 38.67 x 42.36 inches and smaller","numberOfPages":"101","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":286022,"rank":6,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70038342.jpg"},{"id":311385,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70038342/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":286018,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038342/plate-a.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":286021,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038342/plate-d.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":286019,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038342/plate-b.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":286020,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038342/plate-c.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","country":"United States","state":"Connecticut","otherGeospatial":"Farmington River Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -73.30215454101562,\n 41.53839396783225\n ],\n [\n -73.30215454101562,\n 42.04317376494972\n ],\n [\n -72.68280029296875,\n 42.04317376494972\n ],\n [\n -72.68280029296875,\n 41.53839396783225\n ],\n [\n -73.30215454101562,\n 41.53839396783225\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bcb7fe4b08c986b32d69f","contributors":{"authors":[{"text":"Handman, Elinor H.","contributorId":31748,"corporation":false,"usgs":true,"family":"Handman","given":"Elinor","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":463911,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haeni, F. Peter","contributorId":41479,"corporation":false,"usgs":true,"family":"Haeni","given":"F.","email":"","middleInitial":"Peter","affiliations":[],"preferred":false,"id":463912,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, Mendall P.","contributorId":104314,"corporation":false,"usgs":true,"family":"Thomas","given":"Mendall","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":463913,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70006870,"text":"70006870 - 1986 - Effect of injected rotenone on the production and composition of urine from the rainbow trout (Salmo gairdneri)","interactions":[],"lastModifiedDate":"2012-07-14T01:01:39","indexId":"70006870","displayToPublicDate":"2012-01-01T14:40:38","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":874,"text":"Aquatic Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Effect of injected rotenone on the production and composition of urine from the rainbow trout (Salmo gairdneri)","docAbstract":"Renal function was evaluated in adult rainbow trout (Salmo gairdneri) dosed i.a. with rotenone at 225 and 275 μg/kg. The chemical composition of urine samples and urine flow rates collected over a 5-h pretreatment period were compared with hourly urine samples collected over a 5-h posttreatment period. Significant increases in osmolality and in concentrations of sodium, potassium, chloride, glucose, and total protein were observed in the urine of treated fish. Urine solute concentrations reached maximum values within 1 to 3 h after treatment and decreased thereafter, indicating that the effects were reversible. Concentrations of sodium and chloride were highly correlated in 2-h posttreatment urine samples at the low (r = 0.922) and high (r = 0.981) rotenone treatments. Urine flow rates were reduced in trout at each dose of rotenone but the decrease in volume of urine voided was not dose-dependent. In a separate study, [14C]polyethylene glycol was used as a filtration marker to determine the effect of rotenone treatment (225 &mu:g/kg) on urine flow rate, glomerular filtration rate, and renal water reabsorption. We showed that posttreatment urine flow rates were reduced partly by reduced glomerular filtration and partly by increased water reabsorption. Transient increases in plasma osmolality and hematocrit also were observed 0.5 h after rotenone treatment.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Aquatic Toxicology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0166-445X(86)90014-7","collaboration":"Abstract has subscript/superscript to be fixed","usgsCitation":"Erickson, D., and Gingerich, W., 1986, Effect of injected rotenone on the production and composition of urine from the rainbow trout (Salmo gairdneri): Aquatic Toxicology, v. 9, no. 4-5, p. 263-274, https://doi.org/10.1016/0166-445X(86)90014-7.","productDescription":"12 p.","startPage":"263","endPage":"274","numberOfPages":"12","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":258894,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":258873,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0166-445X(86)90014-7","linkFileType":{"id":5,"text":"html"}}],"volume":"9","issue":"4-5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a05eee4b0c8380cd51028","contributors":{"authors":[{"text":"Erickson, D.A.","contributorId":96942,"corporation":false,"usgs":true,"family":"Erickson","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":355383,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gingerich, W.H.","contributorId":83481,"corporation":false,"usgs":true,"family":"Gingerich","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":355382,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70006493,"text":"70006493 - 1986 - Liquid chromatography of hydrocarbonaeous quaternary amines on cyclodextrin bonded silica","interactions":[],"lastModifiedDate":"2024-04-16T23:08:30.505957","indexId":"70006493","displayToPublicDate":"2012-01-01T14:11:57","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2213,"text":"Journal of Chromatography","active":true,"publicationSubtype":{"id":10}},"title":"Liquid chromatography of hydrocarbonaeous quaternary amines on cyclodextrin bonded silica","docAbstract":"Mixtures of n-alkylbenzyldimethylammonium chloride (ABDAC) were resolved into homologous components by high-performance liquid chromatography (HPLC) with a cyclodextrin-bonded silica stationary phase. With a few exceptions, results from this study are similar to those obtained from traditional reversed-phase HPLC. It was found that the presence of electrolytes in aqueous mobile phases is not a critical factor in determining the success of HPLC separation. Under normal HPLC conditions, a mobile phase consisting of either methanol—water (50:50) or acetonitrile—water (30:70) was employed for obtaining adequate resolution of the quaternary ammonium mixtures. Although the percent organic modifier—water profiles were similar to those in previous studies with these compounds, resolution (R) and selectivity (α) parameters were found to be quite susceptible to changes in the mobile phase solvent composition. The retention behavior of the cationic analytes in the homologous series is consistent with the hydrophobic-interaction concept proposed for the retention mechanism via dominant inclusion complex formation. Several electolytes were chosen for a study of the counter ion effect on the chromatographic characteristics of ABDAC components. Among the electrolytes examined, the perchlorate ion was found most likely to act as an ion-pairing counter ion for ammonium cations in the HPLC system studied. A correlation study established linear relationships between the chain length of ABDAC and the logarithmic capacity factor (k′). The analytical utility of the HPLC method was demonstrated by the analysis of various unknown mixtures.
","language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/S0021-9673(01)86948-X","usgsCitation":"Abidi, S.L., 1986, Liquid chromatography of hydrocarbonaeous quaternary amines on cyclodextrin bonded silica: Journal of Chromatography, v. 362, no. 1, p. 33-46, https://doi.org/10.1016/S0021-9673(01)86948-X.","productDescription":"14 p.","startPage":"33","endPage":"46","numberOfPages":"14","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":259538,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"362","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a47fce4b0c8380cd67b30","contributors":{"authors":[{"text":"Abidi, S. L.","contributorId":19898,"corporation":false,"usgs":true,"family":"Abidi","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":354612,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70039038,"text":"70039038 - 1986 - United States Geological Survey Yearbook, fiscal year 1985","interactions":[],"lastModifiedDate":"2017-03-08T16:22:17","indexId":"70039038","displayToPublicDate":"2012-01-01T12:35:55","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":392,"text":"Yearbook","active":false,"publicationSubtype":{"id":6}},"title":"United States Geological Survey Yearbook, fiscal year 1985","docAbstract":"The fiscal year 1985 Yearbook summarizes the activities of the U.S. Geological Survey in response to its scientific and regulatory missions.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039038","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1986, United States Geological Survey Yearbook, fiscal year 1985: Yearbook, vi, 143 p., https://doi.org/10.3133/70039038.","productDescription":"vi, 143 p.","costCenters":[],"links":[{"id":261281,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039038/report.pdf","text":"Report","size":"51.64 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":261282,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039038/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbc94e4b08c986b328d07","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":535207,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70006829,"text":"70006829 - 1986 - Persistence of rotenone in ponds at different temperatures","interactions":[],"lastModifiedDate":"2012-07-07T01:01:38","indexId":"70006829","displayToPublicDate":"2012-01-01T11:31:00","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Persistence of rotenone in ponds at different temperatures","docAbstract":"Two ponds were treated with liquid rotenone (5% rotenone), one with 3 mg/L at 24°C and the other with 2 mg/L at 0°C (concentrations of active rotenone were 0.15 and 0.10 mg/L, respectively). Water samples were collected and analyzed by high-performance liquid chromatography. The concentration of rotenone declined to 0.02 mg/L in 48 h in warm water and in 11 d in cold water. The half-life of rotenone was calculated at 13.9 h in warm water and 83.9 h in cold water.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"North American Journal of Fisheries Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor & Francis","publisherLocation":"Philadelphia, PA","doi":"10.1577/1548-8659(1986)6<129:PORIPA>2.0.CO;2","collaboration":"Abstract has subscript/superscript to be fixed","usgsCitation":"Gilderhus, P., Allen, J.L., and Dawson, V.K., 1986, Persistence of rotenone in ponds at different temperatures: North American Journal of Fisheries Management, v. 6, no. 1, p. 129-130, https://doi.org/10.1577/1548-8659(1986)6<129:PORIPA>2.0.CO;2.","productDescription":"2 p.","startPage":"129","endPage":"130","numberOfPages":"2","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":258238,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":258228,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/1548-8659(1986)6<129:PORIPA>2.0.CO;2","linkFileType":{"id":5,"text":"html"}}],"volume":"6","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a76f0e4b0c8380cd783a3","contributors":{"authors":[{"text":"Gilderhus, P.A.","contributorId":60156,"corporation":false,"usgs":true,"family":"Gilderhus","given":"P.A.","affiliations":[],"preferred":false,"id":355311,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allen, J. L.","contributorId":49295,"corporation":false,"usgs":true,"family":"Allen","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":355310,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dawson, V. K.","contributorId":48900,"corporation":false,"usgs":true,"family":"Dawson","given":"V.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":355309,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70006558,"text":"70006558 - 1986 - Dynamics of alewives in Lake Ontario following a mass mortality","interactions":[],"lastModifiedDate":"2012-11-16T10:34:47","indexId":"70006558","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Dynamics of alewives in Lake Ontario following a mass mortality","docAbstract":"The U.S. Fish and Wildlife Service and the New York Department of Environmental Conservation assessed the population of alewives Alosa pseudoharengus in U.S. waters of Lake Ontario during 1976–1982 with bottom trawls. Alewives were abundant in 1976 but a die-off greatly reduced their numbers during the winter of 1976–1977. The population quickly recovered, however, adult abundance increasing nearly sevenfold during 1978–1981. In spring 1981 the bottom population in southern Lake Ontario was estimated to be 5.25 × 109 fish weighing 128,500 t. Estimated average alewife biomass per hectare during 1978–1982 far exceeded the estimates for either Lake Michigan during 1967–1982 or western Lake Huron during 1973–1982. Recruitment of age-II fish to the population was affected by abundance of adults in two ways: (1) the number of yearlings produced was directly related to adult abundance at low population levels but inversely related at high population levels; and (2) survival of yearlings to age II was inversely related to adult abundance. Growth in 1977 was exceptional, leaving a wide, unmistakable band on scales of the previously slow-growing adults. This wide growth zone served as a marker to identify survivors of the 1976–1977 die-off and to show that each year after 1978 a successively larger proportion of survivors was failing to grow in length or to form an annulus (54% in 1979, 96% in 1980, and 100% in 1981). There was no marker on scales of alewives recruited after the die-off, but the apparent age composition of our catches strongly suggested that most of them also failed to grow in 1981.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the American Fisheries Society","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor & Francis","publisherLocation":"Philadelphia, PA","doi":"10.1577/1548-8659(1986)115<1:DOAILO>2.0.CO;2","collaboration":"Abstract has subscript/superscript to be fixed","usgsCitation":"O’Gorman, R., and Schneider, C.P., 1986, Dynamics of alewives in Lake Ontario following a mass mortality: Transactions of the American Fisheries Society, v. 115, no. 1, p. 1-14, https://doi.org/10.1577/1548-8659(1986)115<1:DOAILO>2.0.CO;2.","productDescription":"14 p.","startPage":"1","endPage":"14","numberOfPages":"13","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":263223,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":263222,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/1548-8659(1986)115<1:DOAILO>2.0.CO;2"}],"otherGeospatial":"Lake Ontario","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.9363,43.1696 ], [ -79.9363,44.3608 ], [ -76.0002,44.3608 ], [ -76.0002,43.1696 ], [ -79.9363,43.1696 ] ] ] } } ] }","volume":"115","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50a76e95e4b0e93eb366ee73","contributors":{"authors":[{"text":"O’Gorman, Robert rogorman@usgs.gov","contributorId":3451,"corporation":false,"usgs":true,"family":"O’Gorman","given":"Robert","email":"rogorman@usgs.gov","affiliations":[],"preferred":true,"id":354760,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schneider, Clifford P.","contributorId":45251,"corporation":false,"usgs":true,"family":"Schneider","given":"Clifford","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":354761,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5223556,"text":"5223556 - 1986 - [Book review] Status and conservation of the world's seabirds, edited by J.P. Croxall, P.G.H. Evans, and R.W. Schreiber","interactions":[],"lastModifiedDate":"2023-11-19T15:15:47.12692","indexId":"5223556","displayToPublicDate":"2010-06-16T12:19:01","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1272,"text":"Colonial Waterbirds","printIssn":"07386028","active":false,"publicationSubtype":{"id":10}},"title":"[Book review] Status and conservation of the world's seabirds, edited by J.P. Croxall, P.G.H. Evans, and R.W. Schreiber","docAbstract":"No abstract available.
","language":"English","publisher":"Waterbird Society","doi":"10.2307/1521158","usgsCitation":"Clapp, R.B., 1986, [Book review] Status and conservation of the world's seabirds, edited by J.P. Croxall, P.G.H. Evans, and R.W. Schreiber: Colonial Waterbirds, v. 9, no. 1, p. 128-131, https://doi.org/10.2307/1521158.","productDescription":"4 p.","startPage":"128","endPage":"131","numberOfPages":"4","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201886,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47b9e4b07f02db4a246b","contributors":{"authors":[{"text":"Clapp, R. B.","contributorId":9371,"corporation":false,"usgs":true,"family":"Clapp","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":338975,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5222091,"text":"5222091 - 1986 - Trace elements in sediments, water, and American coots (Fulica americana) at a coal-fired power plant in Texas, 1979-1982","interactions":[],"lastModifiedDate":"2023-10-31T01:01:33.646792","indexId":"5222091","displayToPublicDate":"2010-06-16T12:19:01","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1103,"text":"Bulletin of Environmental Contamination and Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Trace elements in sediments, water, and American coots (Fulica americana) at a coal-fired power plant in Texas, 1979-1982","docAbstract":"No abstract available.
","language":"English","publisher":"Springer","doi":"10.1007/BF01623523","usgsCitation":"White, D.H., King, K.A., Mitchell, C.A., and Mulhern, B., 1986, Trace elements in sediments, water, and American coots (Fulica americana) at a coal-fired power plant in Texas, 1979-1982: Bulletin of Environmental Contamination and Toxicology, v. 36, no. 3, p. 376-383, https://doi.org/10.1007/BF01623523.","productDescription":"8 p.","startPage":"376","endPage":"383","numberOfPages":"8","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":199364,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"36","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627e22","contributors":{"authors":[{"text":"White, Donald H.","contributorId":97868,"corporation":false,"usgs":true,"family":"White","given":"Donald","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":335481,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, Kirk A.","contributorId":9203,"corporation":false,"usgs":true,"family":"King","given":"Kirk","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":335479,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mitchell, C. A.","contributorId":54543,"corporation":false,"usgs":true,"family":"Mitchell","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":335480,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mulhern, B.M.","contributorId":98683,"corporation":false,"usgs":true,"family":"Mulhern","given":"B.M.","email":"","affiliations":[],"preferred":false,"id":335482,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ]}