{"pageNumber":"4578","pageRowStart":"114425","pageSize":"25","recordCount":166008,"records":[{"id":70013178,"text":"70013178 - 1984 - Determination of total tin in geological materials by electrothermal atomic-absorption spectrophotometry using a tungsten-impregnated graphite furnace","interactions":[],"lastModifiedDate":"2025-08-13T16:58:08.291175","indexId":"70013178","displayToPublicDate":"2001-11-26T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3517,"text":"Talanta","active":true,"publicationSubtype":{"id":10}},"title":"Determination of total tin in geological materials by electrothermal atomic-absorption spectrophotometry using a tungsten-impregnated graphite furnace","docAbstract":"<p><span>An electrothermal atomic-absorption spectrophotometric method is described for the determination of total tin in geological materials, with use of a tungsten-impregnated graphite furnace. The sample is decomposed by fusion with lithium metaborate and the melt is dissolved in 10% hydrochloric acid. Tin is then extracted into trioctylphosphine oxide-methyl isobutyl ketone prior to atomization. Impregnation of the furnace with a sodium tungstate solution increases the sensitivity of the determination and improves the precision of the results. The limits of determination are 0.5–20 ppm of tin in the sample. Higher tin values can be determined by dilution of the extract. Replicate analyses of eighteen geological reference samples with diverse matrices gave relative standard deviations ranging from 2.0 to 10.8% with an average of 4.6%. Average tin values for reference samples were in general agreement with, but more precise than, those reported by others. Apparent recoveries of tin added to various samples ranged from 95 to 111% with an average of 102%.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0039-9140(84)80014-4","issn":"00399140","usgsCitation":"Zhou, L., Chao, T.T., and Meier, A.L., 1984, Determination of total tin in geological materials by electrothermal atomic-absorption spectrophotometry using a tungsten-impregnated graphite furnace: Talanta, v. 31, no. 1, p. 73-76, https://doi.org/10.1016/0039-9140(84)80014-4.","productDescription":"4 p.","startPage":"73","endPage":"76","costCenters":[],"links":[{"id":220410,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ffe0e4b0c8380cd4f444","contributors":{"authors":[{"text":"Zhou, L.","contributorId":68455,"corporation":false,"usgs":true,"family":"Zhou","given":"L.","email":"","affiliations":[],"preferred":false,"id":365478,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chao, T. T.","contributorId":31900,"corporation":false,"usgs":true,"family":"Chao","given":"T.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":365477,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meier, A. L.","contributorId":81480,"corporation":false,"usgs":true,"family":"Meier","given":"A.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":365479,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10301,"text":"ofr84704 - 1984 - Streamflow and basin characteristics at selected sites in Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:06:29","indexId":"ofr84704","displayToPublicDate":"1997-04-01T00:00:00","publicationYear":"1984","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":"84-704","title":"Streamflow and basin characteristics at selected sites in Kentucky","docAbstract":"Common basin and streamflow characteristics for sites in Kentucky are presented. Basin characteristics include quantified drainage basin parameters and statistics on areal rainfall. Streamflow characteristics include tables for mean, high and low flow frequencies and partial duration discharge. The data listed in this report are for continuous and low-flow partial-record sites. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84704","usgsCitation":"Melcher, N., and Ruhl, K., 1984, Streamflow and basin characteristics at selected sites in Kentucky: U.S. Geological Survey Open-File Report 84-704, v, 80 p. :ill., maps (some folded) ;28 cm., https://doi.org/10.3133/ofr84704.","productDescription":"v, 80 p. :ill., maps (some folded) ;28 cm.","costCenters":[],"links":[{"id":144092,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0704/report-thumb.jpg"},{"id":38159,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0704/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db626eda","contributors":{"authors":[{"text":"Melcher, N.B.","contributorId":71554,"corporation":false,"usgs":true,"family":"Melcher","given":"N.B.","email":"","affiliations":[],"preferred":false,"id":161163,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ruhl, K.J.","contributorId":35322,"corporation":false,"usgs":true,"family":"Ruhl","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":161162,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60252,"text":"mf1246L - 1984 - Maps showing distribution of pH, copper, zinc, fluoride, uranium, molybdenum, arsenic, and sulfate in water, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-10-25T19:02:48.751765","indexId":"mf1246L","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1246","chapter":"L","title":"Maps showing distribution of pH, copper, zinc, fluoride, uranium, molybdenum, arsenic, and sulfate in water, Richfield 1° x 2° quadrangle, Utah","docAbstract":"<p>These maps show the regional distribution of copper, zinc, arsenic, molybdenum, uranium, fluoride, sulfate, and pH in surface and ground water from the Richfield 1° x 2° quadrangle. This study supplements (Miller and others, 1984a-j) the regional drainage geochemical study done for the Richfield quadrangle under the U.S. Geological Survey’s Conterminuous United States Mineral Assessment Program (CUSMAP). Regional sampling was designed to define broad geochemical patterns and trends which can be used, along with geologic and geophysical data, to assess the mineral resource potential of the Richfield quadrangle. Analytical data used in compiling this report were published previously (McHugh and others, 1981).</p>\n<br/>\n<p>The Richfield quadrangle in west-central Utah covers the eastern part of the Pioche-Marysvale igneous and mineral belt that extends from the vicinity of Pioche in southeastern Nevada, east-northeastward for 250 km into central Utah. The western two-thirds of the Richfield quadrangle is in the Basin and Range Province, and the eastern third in the High Plateaus of Utah subprovince of the Colorado Plateau.</p>\n<br/>\n<p>Bedrock in the northern part of the Richfield quadrangle consists predominantly of latest Precambrian and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrane into a series of north-trending fault blocks; the uplifted mountain areas were deeply eroded and the resulting debris deposited in the adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed during igneous activity in the middle and late Cenozoic time.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver CO","doi":"10.3133/mf1246L","usgsCitation":"McHugh, J.B., Miller, W.R., and Ficklin, W.H., 1984, Maps showing distribution of pH, copper, zinc, fluoride, uranium, molybdenum, arsenic, and sulfate in water, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1246, 1 Plate: 40.89 x 32.77 inches, https://doi.org/10.3133/mf1246L.","productDescription":"1 Plate: 40.89 x 32.77 inches","costCenters":[],"links":[{"id":182629,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1246l.jpg"},{"id":283659,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1246-L/plate-1.pdf"},{"id":390899,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6856.htm"}],"scale":"500000","country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db60578b","contributors":{"authors":[{"text":"McHugh, J. B.","contributorId":79462,"corporation":false,"usgs":true,"family":"McHugh","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":263391,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, W. R.","contributorId":92239,"corporation":false,"usgs":true,"family":"Miller","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263393,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ficklin, W. H.","contributorId":89517,"corporation":false,"usgs":true,"family":"Ficklin","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":263392,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":4270,"text":"cir895G - 1984 - Digital line graph attribute coding standards","interactions":[],"lastModifiedDate":"2012-05-24T01:02:39","indexId":"cir895G","displayToPublicDate":"1994-01-01T01:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"895","chapter":"G","title":"Digital line graph attribute coding standards","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir895G","collaboration":"replaced by Data Users Guides 1-7","usgsCitation":"Allder, W.R., Sziede, A., McEwen, R., and Beck, F., 1984, Digital line graph attribute coding standards: U.S. Geological Survey Circular 895, vi, 31 p. ;26 cm., https://doi.org/10.3133/cir895G.","productDescription":"vi, 31 p. ;26 cm.","costCenters":[],"links":[{"id":92269,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1984/0895g/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138674,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1984/0895g/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65acd1","contributors":{"authors":[{"text":"Allder, William R.","contributorId":98709,"corporation":false,"usgs":true,"family":"Allder","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":148659,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sziede, A.J.","contributorId":57441,"corporation":false,"usgs":true,"family":"Sziede","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":148658,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McEwen, R.B.","contributorId":6043,"corporation":false,"usgs":true,"family":"McEwen","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":148656,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Beck, F.J.","contributorId":13219,"corporation":false,"usgs":true,"family":"Beck","given":"F.J.","email":"","affiliations":[],"preferred":false,"id":148657,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":4215,"text":"cir895C - 1984 - Digital line graphs from 1:24,000-scale maps","interactions":[],"lastModifiedDate":"2012-05-24T01:02:39","indexId":"cir895C","displayToPublicDate":"1994-01-01T01:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"895","chapter":"C","title":"Digital line graphs from 1:24,000-scale maps","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir895C","collaboration":"replaced by Data Users Guides 1","usgsCitation":"Allder, W.R., and Elassal, A.A., 1984, Digital line graphs from 1:24,000-scale maps: U.S. Geological Survey Circular 895, vi, 79 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir895C.","productDescription":"vi, 79 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":118232,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1984/0895c/report-thumb.jpg"},{"id":31329,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1984/0895c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d466","contributors":{"authors":[{"text":"Allder, William R.","contributorId":98709,"corporation":false,"usgs":true,"family":"Allder","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":148425,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elassal, Atef A.","contributorId":105699,"corporation":false,"usgs":true,"family":"Elassal","given":"Atef","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":148426,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7454,"text":"ofr84772 - 1984 - Primer on improving the state of earthquake hazards mitigation and preparedness","interactions":[],"lastModifiedDate":"2012-02-02T00:06:11","indexId":"ofr84772","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-772","title":"Primer on improving the state of earthquake hazards mitigation and preparedness","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84772","usgsCitation":"Gori, P.L., 1984, Primer on improving the state of earthquake hazards mitigation and preparedness: U.S. Geological Survey Open-File Report 84-772, ii, 222 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84772.","productDescription":"ii, 222 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":142159,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0772/report-thumb.jpg"},{"id":34865,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0772/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668e77","contributors":{"authors":[{"text":"Gori, P. L.","contributorId":87138,"corporation":false,"usgs":true,"family":"Gori","given":"P.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":155692,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30519,"text":"wri844147 - 1984 - Erosion, channel change, and sediment transport in the Big Lost River, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:08:57","indexId":"wri844147","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4147","title":"Erosion, channel change, and sediment transport in the Big Lost River, Idaho","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844147","usgsCitation":"Williams, R., and Krupkin, P., 1984, Erosion, channel change, and sediment transport in the Big Lost River, Idaho: U.S. Geological Survey Water-Resources Investigations Report 84-4147, 87 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844147.","productDescription":"87 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":126544,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4147/report-thumb.jpg"},{"id":59299,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4147/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdefc","contributors":{"authors":[{"text":"Williams, R.P.","contributorId":92285,"corporation":false,"usgs":true,"family":"Williams","given":"R.P.","email":"","affiliations":[],"preferred":false,"id":203389,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krupkin, P.J.","contributorId":101708,"corporation":false,"usgs":true,"family":"Krupkin","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":203390,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29152,"text":"wri834177 - 1984 - Georgia irrigation, 1970-1980 : a decade of growth","interactions":[],"lastModifiedDate":"2017-01-24T09:20:21","indexId":"wri834177","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"83-4177","title":"Georgia irrigation, 1970-1980 : a decade of growth","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834177","usgsCitation":"Pierce, R.R., Barber, N.L., and Stiles, H., 1984, Georgia irrigation, 1970-1980 : a decade of growth: U.S. Geological Survey Water-Resources Investigations Report 83-4177, vi, 29 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/wri834177.","productDescription":"vi, 29 p. :ill. 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,{"id":3759,"text":"cir850E - 1984 - Some chemical effects of the Mount St. Helens eruption on selected streams in the State of Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:05:32","indexId":"cir850E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"850","chapter":"E","title":"Some chemical effects of the Mount St. Helens eruption on selected streams in the State of Washington","docAbstract":"During several periods of volcanic-ash eruption at Mount St. Helens, Wash., (March 30, May 25-26, May 30-June 2, and June 12-13, 1980) strong winds from the north occurred at high altitudes. As a result, the volcanic ash fell some 50 miles to the south in the Bull Run watershed, the principal water-supply source for the metropolitan area of Portland, Oreg. Water samples collected from three stream sites within the watershed were compared with samples collected during the same season in previous years. No detectable changes were noted in chemical characteristics. Precipitation samples collected immediately after the June 12-13 ash fall ranged in specific conductance from 20 to 41 micromhos per centimeter at 25C and in pH from 4.0 to 4.3 pH units. Stream samples collected during the May-June period ranged in specific conductance from 18 to 28 micromhos per centimeter at 25C and in pH from 6.7 to 7.5 pH units. Volcanic-ash samples were collected and analyzed for particle size, chemical composition, and weight. Significant differences in particle size of ash were found in samples from two separate eruptions. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir850E","usgsCitation":"Klein, J.M., 1984, Some chemical effects of the Mount St. Helens eruption on selected streams in the State of Washington: U.S. Geological Survey Circular 850, vi, 26 p. :ill. ;26 cm., https://doi.org/10.3133/cir850E.","productDescription":"vi, 26 p. :ill. ;26 cm.","costCenters":[],"links":[{"id":123349,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1984/0850e/report-thumb.jpg"},{"id":30822,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1984/0850e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdc98","contributors":{"authors":[{"text":"Klein, John M.","contributorId":27036,"corporation":false,"usgs":true,"family":"Klein","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":147548,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25622,"text":"wri844073 - 1984 - Leaching study of oil shale in Kentucky: With a section on hydrologic reconnaissance of the oil shale outcrop in Kentucky","interactions":[],"lastModifiedDate":"2021-01-27T19:54:28.722464","indexId":"wri844073","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4073","title":"Leaching study of oil shale in Kentucky: With a section on hydrologic reconnaissance of the oil shale outcrop in Kentucky","docAbstract":"Oil shales in Kentucky are rocks of predominantly Devonian age. The most prominant are the Ohio, Chattanooga, and New Albany Shales. A leaching study was done on six fresh oil shale samples and one retorted oil shale sample. Leaching reagents were distilled water, 0.0005 N sulfuric acid, and 0.05 N sulfuric acid. The concentration of constituents in the leachates were highly variable. The concentration of sodium, manganese, and zinc in the retorted shale leachate was several orders of magnitude higher than those of the leachates of fresh shale samples. The major oil shale outcrop covers approximately 1,000 square miles in a horseshoe pattern from Vanceburg, Lewis County , in the east, to Louisville, Jefferson County, in the west. The Kentucky, Red, and Licking Rivers cross the outcrop belt, the Rolling Fork River flows along the strike of the shale in the southwest part of the outcrop, and the Ohio River flows past the outcrop at the ends of the horseshoe. Oil shale does not appear to significantly alter the water quality of these streams. Oil shale is not an aquifer, but seeps and springs found in the shale indicate that water moves through it. Ground water quality is highly variable. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri844073","usgsCitation":"Leung, S.S., Leist, D., Davis, R.W., and Cordiviola, S., 1984, Leaching study of oil shale in Kentucky: With a section on hydrologic reconnaissance of the oil shale outcrop in Kentucky: U.S. Geological Survey Water-Resources Investigations Report 84-4073, Report: viii, 68 p.; 1 Plate: 26.54 x 26.30 inches, https://doi.org/10.3133/wri844073.","productDescription":"Report: viii, 68 p.; 1 Plate: 26.54 x 26.30 inches","costCenters":[],"links":[{"id":382723,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4073/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":382722,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4073/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157257,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4073/report-thumb.jpg"}],"country":"United 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,{"id":9332,"text":"ofr84767 - 1984 - Fossils and time; selected books on paleontology, evolution and Earth history for elementary through college students and amateur paleontologists","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr84767","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-767","title":"Fossils and time; selected books on paleontology, evolution and Earth history for elementary through college students and amateur paleontologists","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84767","usgsCitation":"Hanley, J.H., 1984, Fossils and time; selected books on paleontology, evolution and Earth history for elementary through college students and amateur paleontologists: U.S. Geological Survey Open-File Report 84-767, i, 52 p. ;28 cm., https://doi.org/10.3133/ofr84767.","productDescription":"i, 52 p. ;28 cm.","costCenters":[],"links":[{"id":142389,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0767/report-thumb.jpg"},{"id":37053,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0767/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ce4b07f02db6a93c6","contributors":{"authors":[{"text":"Hanley, J. H. (compiler)","contributorId":19551,"corporation":false,"usgs":true,"family":"Hanley","given":"J.","suffix":"(compiler)","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":159492,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26282,"text":"wri834167 - 1984 - Sediment transport by irrigation return flows in four small drains within the DID-18 drainage of the Sulphur Creek basin, Yakima County, Washington, April 1979 to October 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:08:29","indexId":"wri834167","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"83-4167","title":"Sediment transport by irrigation return flows in four small drains within the DID-18 drainage of the Sulphur Creek basin, Yakima County, Washington, April 1979 to October 1981","docAbstract":"Suspended sediment, water discharges, and water temperatures were monitored in four small drains in the DID-18 basin of the Sulphur Creek basin, a tributary to the Yakima River, Washington. Water outflow, inflow, and miscellaneous sites were also monitored. The information was used to evaluate the effectiveness of management practices in reducing sediment loads in irrigated areas. This study was one of seven Model Implementation Plan projects selected by the U.S. Soil Conservation Service and the U.S. Environmental Protection Agency to demonstrate the effectiveness of institutional and administrative implementation of management plans. Sediment discharges from the four basins could not be correlated with changes in management practices, because Imhoff Cone readings collected for the study showed no statistical differences between the three irrigation seasons. However, one drain acted as a sink for sediment where more lands were sprinkler irrigated; this drain had a smaller proportion of row crops than did the other three drains. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834167","usgsCitation":"Boucher, P.R., 1984, Sediment transport by irrigation return flows in four small drains within the DID-18 drainage of the Sulphur Creek basin, Yakima County, Washington, April 1979 to October 1981: U.S. Geological Survey Water-Resources Investigations Report 83-4167, v, 149 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834167.","productDescription":"v, 149 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158223,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4167/report-thumb.jpg"},{"id":55090,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4167/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbef9","contributors":{"authors":[{"text":"Boucher, P. R.","contributorId":108088,"corporation":false,"usgs":true,"family":"Boucher","given":"P.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":196110,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10440,"text":"ofr84649 - 1984 - Preliminary analysis of geophysical logs from drill hole UE-25p#1, Yucca Mountain, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:27","indexId":"ofr84649","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-649","title":"Preliminary analysis of geophysical logs from drill hole UE-25p#1, Yucca Mountain, Nye County, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84649","usgsCitation":"Muller, D.C., and Kibler, J.E., 1984, Preliminary analysis of geophysical logs from drill hole UE-25p#1, Yucca Mountain, Nye County, Nevada: U.S. Geological Survey Open-File Report 84-649, ii, 17 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr84649.","productDescription":"ii, 17 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":143116,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0649/report-thumb.jpg"},{"id":38309,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0649/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38310,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0649/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38311,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0649/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a87a3","contributors":{"authors":[{"text":"Muller, D. C.","contributorId":75936,"corporation":false,"usgs":true,"family":"Muller","given":"D.","middleInitial":"C.","affiliations":[],"preferred":false,"id":161405,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kibler, J. E.","contributorId":49358,"corporation":false,"usgs":true,"family":"Kibler","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":161404,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9834,"text":"ofr84608 - 1984 - Availability of hydrologic data in San Juan County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:06:17","indexId":"ofr84608","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-608","title":"Availability of hydrologic data in San Juan County, New Mexico","docAbstract":"San Juan County, in the northwestern corner of New Mexico, uses surface water from the San Juan, Animas, and La Plata Rivers as a principal source of water for the county, but the water in these streams is fully appropriated. Ground water is present in San Juan County in several bedrock formations and in the alluvium of the river valleys. This report describes the hydrologic data that have been collected in San Juan County, presents examples of the data, shows the locations of the data-collection sites, and indicates where more complete records may be obtained. This data base should be helpful in assessing the quantity, quality, and availability of the county 's water resources. Information collected at 1,877 water wells, 39 streamflow-gaging stations, and 172 springs is presented. The collection sites and geology are shown on a base map with a scale of 1 inch = 2 miles. (USGS).","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84608","usgsCitation":"Klausing, R., and Welder, G.E., 1984, Availability of hydrologic data in San Juan County, New Mexico: U.S. Geological Survey Open-File Report 84-608, iv, 116 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84608.","productDescription":"iv, 116 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":142848,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0608/report-thumb.jpg"},{"id":37618,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0608/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37619,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0608/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d561","contributors":{"authors":[{"text":"Klausing, R.L.","contributorId":73205,"corporation":false,"usgs":true,"family":"Klausing","given":"R.L.","affiliations":[],"preferred":false,"id":160381,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Welder, G. E.","contributorId":100814,"corporation":false,"usgs":true,"family":"Welder","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":160382,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7460,"text":"ofr84760 - 1984 - Proceedings of the Geologic and Hydrologic Hazards Training Program","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr84760","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-760","title":"Proceedings of the Geologic and Hydrologic Hazards Training Program","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84760","usgsCitation":"Williams, M., 1984, Proceedings of the Geologic and Hydrologic Hazards Training Program: U.S. Geological Survey Open-File Report 84-760, iv, 1128 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84760.","productDescription":"iv, 1128 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":142095,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0760/report-thumb.jpg"},{"id":34881,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0760/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34879,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0760/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34880,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0760/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db6604a7","contributors":{"authors":[{"text":"Williams, M.E.","contributorId":11613,"corporation":false,"usgs":true,"family":"Williams","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":155714,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29589,"text":"wri834237 - 1984 - Water levels and water-level changes in the Prairie du Chien-Jordan and Mount Simon-Hinckley aquifers, Twin Cities metropolitan area, Minnesota, 1971-80","interactions":[],"lastModifiedDate":"2018-04-02T10:23:19","indexId":"wri834237","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"83-4237","title":"Water levels and water-level changes in the Prairie du Chien-Jordan and Mount Simon-Hinckley aquifers, Twin Cities metropolitan area, Minnesota, 1971-80","docAbstract":"<p>The ground-water system in the Twin Cities Metropolitan Area includes five aquifers; two of these aquifers the Prairie du Chien-Jordan and the Mount Simon-Hinckley supply about 80 percent and 10 percent, respectively, of the ground water pumped for public supply. Water levels and changes in water levels in these two aquifers differ greatly in the Twin Cities Metropolitan Area. The Mississippi, Minnesota, and St. Croix Rivers are in hydraulic connection with and influence the pattern of flow in the upper aquifer, the Prairie du Chien-Jordan. Water generally flows toward these streams from water-level highs northeast, northwest, and south of Minneapolis and St. Paul. Consequently, heavy pumping has caused only localized cones of depression in the potentiometric surface of this aquifer. In contrast, the Mount Simon-Hinckley, which has only a slight hydraulic connection to the streams, is greatly influenced by pumping. Pumping in the urban centers of Minneapolis and St. Paul has caused a large cone of depression in the Mount Simon-Hinckley potentiometric surface. During 1971, the measurable cone was centered in eastcentral Hennepin County, was about 25 miles in diameter, and was as much as 150 feet deep at its center.</p>\n<p>Between 1971 and 1980, average water levels in the Prairie du Chien-Jordan aquifer changed less than 5 feet in most of the study area, but rose or declined as much as 25 feet locally in response to pumpage and recharge. During this period, seasonal declines of water levels from winter to summer lessened, and the area where these declines exceeded 10 feet decreased.</p>\n<p>In contrast, between 1971 and 1980, average water levels in the Mount Simon-Hinckley aquifer rose as much as 60 feet in the center of the cone of depression in response to decreased pumping. Also, the measurable cone of depression contracted from about 25 miles to about 15 miles in diameter. However, because of increased summer pumping due to below-average precipitation during 1980, seasonal water levels declined much more and over a wider area during 1980 than in 1971.</p>\n<p>Water-level data suggest that (1) little variation in annual pumpage between 1971 and 1980 from the Prairie du Chien-Jordan aquifer produced generally stable water levels in that aquifer, (2) decreased annual pumpage from the Mount Simon-Hinckley aquifer from 1971 to 1980 caused water levels in that aquifer to rise, and (3) a greater seasonal component of pumpage from the Mount Simon-Hinckley aquifer than from the Prairie du Chien-Jordan produced larger and more widespread seasonal water-level declines in the Mount Simon-Hinckley than in the Prairie du Chien-Jordan, particularly during dry years.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri834237","collaboration":"Prepared in cooperation with the Metropolitan Council of the Twin Cities and Minnesota Department of Natural Resources","usgsCitation":"Schoenberg, M., 1984, Water levels and water-level changes in the Prairie du Chien-Jordan and Mount Simon-Hinckley aquifers, Twin Cities metropolitan area, Minnesota, 1971-80: U.S. Geological Survey Water-Resources Investigations Report 83-4237, Document: iv, 23 p.; 2 Plates: 34.56 x 30.51 inches and 34.60 x 30.78 inches, https://doi.org/10.3133/wri834237.","productDescription":"Document: iv, 23 p.; 2 Plates: 34.56 x 30.51 inches and 34.60 x 30.78 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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:{\"name\":\"Anoka\",\"state\":\"MN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9e31","contributors":{"authors":[{"text":"Schoenberg, Michael","contributorId":22802,"corporation":false,"usgs":true,"family":"Schoenberg","given":"Michael","affiliations":[],"preferred":false,"id":201771,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11356,"text":"ofr82365 - 1984 - Techniques for estimating flood hydrographs for ungaged urban watersheds","interactions":[],"lastModifiedDate":"2012-02-02T00:06:24","indexId":"ofr82365","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"82-365","title":"Techniques for estimating flood hydrographs for ungaged urban watersheds","docAbstract":"The Clark Method, modified slightly was used to develop a synthetic, dimensionless hydrograph which can be used to estimate flood hydrographs for ungaged urban watersheds. Application of the technique results in a typical (average) flood hydrograph for a given peak discharge. Input necessary to apply the technique is an estimate of basin lagtime and the recurrence interval peak discharge. Equations for this purpose were obtained from a recent nationwide study on flood frequency in urban watersheds. A regression equation was developed which relates flood volumes to drainage area size, basin lagtime, and peak discharge. This equation is useful where storage of floodwater may be a part of design of flood prevention. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82365","usgsCitation":"Stricker, V., and Sauer, V., 1984, Techniques for estimating flood hydrographs for ungaged urban watersheds: U.S. Geological Survey Open-File Report 82-365, v, 22 p. :ill. ;28 cm., https://doi.org/10.3133/ofr82365.","productDescription":"v, 22 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":143466,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0365/report-thumb.jpg"},{"id":39183,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0365/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685ed5","contributors":{"authors":[{"text":"Stricker, V.A.","contributorId":78703,"corporation":false,"usgs":true,"family":"Stricker","given":"V.A.","email":"","affiliations":[],"preferred":false,"id":162991,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sauer, V.B.","contributorId":39380,"corporation":false,"usgs":true,"family":"Sauer","given":"V.B.","email":"","affiliations":[],"preferred":false,"id":162990,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4691,"text":"twri03A10 - 1984 - Discharge ratings at gaging stations","interactions":[],"lastModifiedDate":"2012-02-02T00:05:31","indexId":"twri03A10","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"03-A10","title":"Discharge ratings at gaging stations","docAbstract":"A discharge rating is the relation of the discharge at a gaging station to stage and sometimes also to other variables. This chapter of 'Techniques of Water-Resources Investigations' describes the procedures commonly used to develop simple ratings where discharge is related only to stage and the most frequently encountered types of complex ratings where additional factors such as rate of change in stage, water-surface slope, or index velocity are used. Fundamental techniques of logarithmic plotting and the applications of simple storage routing to rating development are demonstrated. Computer applications, especially for handheld programmable calculators, and data handling are stressed.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/twri03A10","issn":"0565-596X","usgsCitation":"Kennedy, E., 1984, Discharge ratings at gaging stations: U.S. Geological Survey Techniques of Water-Resources Investigations 03-A10, xi, 59 p. :ill. ;26 cm., https://doi.org/10.3133/twri03A10.","productDescription":"xi, 59 p. :ill. ;26 cm.","costCenters":[],"links":[{"id":139176,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":251,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri3-a10/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64a9d2","contributors":{"authors":[{"text":"Kennedy, E.J.","contributorId":87529,"corporation":false,"usgs":true,"family":"Kennedy","given":"E.J.","email":"","affiliations":[],"preferred":false,"id":149628,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25471,"text":"wri844124 - 1984 - Effects of storm-water runoff on water quality of the Edwards Aquifer near Austin, Texas","interactions":[],"lastModifiedDate":"2016-08-09T14:16:38","indexId":"wri844124","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4124","title":"Effects of storm-water runoff on water quality of the Edwards Aquifer near Austin, Texas","docAbstract":"<p>Analyses of samples collected from Barton Springs at approximately weekly Intervals and from Barton Creek and five wells in the Austin area during selected storm-runoff periods generally show that recharge during storm runoff resulted in significant temporal and area! variations in the quality of ground water in the recharge zone of the Edwards aquifer. Recharge during storm runoff resulted in significant increases of bacterial densities in the ground water. Densities of fecal coliform bacteria in samples collected from Barton Springs, the major point of ground-water discharge, ranged from less than 1 colony per 100 milliliters during dry weather in November 1981 and January and August 1982 to 6,100 colonies per 100 milliliters during a storm in May 1982. Densities of fecal streptococcal bacteria ranged from 1 colony per 100 miniliters during dry weather in December 1981 to 11,000 colonies per 100 miniliters during a storm in May 1982.</p>\n<p>Recharge during storm runoff resulted in significant decreases in the specific conductance and the concentration of total nitrate nitrogen in the ground water. Specific-conductance values of samples from Barton Springs ranged from 438 micromhos per centimeter at 25&deg; Celsius after a storm in October 1981 to 682 micromhos after a relatively long period of deficient rainfall in September 1982. The specific-conductance values and, thus, the mineralization of the ground water in the recharge zone generally were inversely related to the quantity of recharge. Nitrate nitrogen was the most prevalent form of nitrogen in the ground water. Concentrations of total nitrate nitrogen in samples from Barton Springs ranged from 0.51 milligram per liter after a storm in October 1981 to 1.6 milligrams per liter during dry weather in February and September 1982.</p>\n<p>Although the values of these and other properties or constituents in ground water varied temporally and areally, available data indicate that the values of most of the major and minor elements in ground water in the recharge zone of the Edwards aquifer were significantly less than the primary maximum or secondary maximum contaminant levels set by the U.S. Environmental Protection Agency for public water systems.</p>\n<p>Bacteriological data for Barton Springs and selected wells indicate that the ground water in the aquifer is susceptible to bacterial pollution, especially during storm runoff. The water may require disinfection if used for drinking or culinary purposes.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri844124","usgsCitation":"Andrews, F.L., Schertz, T.L., Slade, R.M., and Rawson, J., 1984, Effects of storm-water runoff on water quality of the Edwards Aquifer near Austin, Texas: U.S. Geological Survey Water-Resources Investigations Report 84-4124, Report: v, 50 p.; 2 Plates: 9.98 x 13.18 inches and 10.33 x 13.20 inches, https://doi.org/10.3133/wri844124.","productDescription":"Report: v, 50 p.; 2 Plates: 9.98 x 13.18 inches and 10.33 x 13.20 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":54197,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4124/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54198,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4124/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54199,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4124/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123331,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4124/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db610ace","contributors":{"authors":[{"text":"Andrews, Freeman L.","contributorId":91486,"corporation":false,"usgs":true,"family":"Andrews","given":"Freeman","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":193822,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schertz, Terry L. tschertz@usgs.gov","contributorId":188,"corporation":false,"usgs":true,"family":"Schertz","given":"Terry","email":"tschertz@usgs.gov","middleInitial":"L.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":645095,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Slade, Raymond M. Jr.","contributorId":46487,"corporation":false,"usgs":true,"family":"Slade","given":"Raymond","suffix":"Jr.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":645096,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rawson, Jack","contributorId":18345,"corporation":false,"usgs":true,"family":"Rawson","given":"Jack","affiliations":[],"preferred":false,"id":645097,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":11086,"text":"ofr84708 - 1984 - State hydrologic unit maps","interactions":[{"subject":{"id":11086,"text":"ofr84708 - 1984 - State hydrologic unit maps","indexId":"ofr84708","publicationYear":"1984","noYear":false,"title":"State hydrologic unit maps"},"predicate":"SUPERSEDED_BY","object":{"id":2672,"text":"wsp2294 - 1987 - Hydrologic unit maps","indexId":"wsp2294","publicationYear":"1987","noYear":false,"title":"Hydrologic unit maps"},"id":1}],"supersededBy":{"id":2672,"text":"wsp2294 - 1987 - Hydrologic unit maps","indexId":"wsp2294","publicationYear":"1987","noYear":false,"title":"Hydrologic unit maps"},"lastModifiedDate":"2012-02-02T00:06:26","indexId":"ofr84708","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-708","title":"State hydrologic unit maps","docAbstract":"A set of maps depicting approved boundaries of, and numerical codes for, river-basin units of the United States has been developed by the U.S. Geological Survey. These ' State Hydrologic Unit Maps ' are four-color maps that present information on drainage, culture, hydrography, and hydrologic boundaries and codes: (1) the 21 major water-resources regions and the 222 subregions designated by the U.S. Water Resources Council; (2) the 352 accounting units of the U.S. Geological Survey 's National Water Data Network; and (3) the 2,149 cataloging units of the U.S. Geological Survey 's Catalog of Information on Water Data. The maps are plotted on the Geological Survey State base-map series at a scale of 1:500,000 and, except for Alaska, depict hydrologic unit boundaries for all drainage basins greater than 700 mi squared (1,813 km squared). A complete list of all the hydrologic units, along with their drainage areas, their names, and the names of the States or outlying areas in which they reside, is contained in the report. These maps and associated codes provide a standardized base for use by water-resources organizations in locating, storing, retrieving, and exchanging hydrologic data. The Hydrologic Unit Codes shown on the maps have been approved as a Federal Information Processing Standard for use by the Federal establishment. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84708","usgsCitation":"Seaber, P., Kapinos, F., and Knapp, G., 1984, State hydrologic unit maps: U.S. Geological Survey Open-File Report 84-708, 175 p. :ill., maps (some col.) ;28 cm., https://doi.org/10.3133/ofr84708.","productDescription":"175 p. :ill., maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":143264,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0708/report-thumb.jpg"},{"id":38845,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0708/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478ee4b07f02db489d17","contributors":{"authors":[{"text":"Seaber, P. R.","contributorId":53802,"corporation":false,"usgs":true,"family":"Seaber","given":"P. R.","affiliations":[],"preferred":false,"id":162508,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kapinos, F.P.","contributorId":73591,"corporation":false,"usgs":true,"family":"Kapinos","given":"F.P.","email":"","affiliations":[],"preferred":false,"id":162509,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Knapp, G.L.","contributorId":108116,"corporation":false,"usgs":true,"family":"Knapp","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":162510,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":29630,"text":"wri844151 - 1984 - Analysis of characteristics of simulated flows from small surface-mined and undisturbed Appalachian watersheds in the Tug Fork basin of Kentucky, Virginia, and West Virginia","interactions":[],"lastModifiedDate":"2023-01-04T19:56:58.574112","indexId":"wri844151","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4151","title":"Analysis of characteristics of simulated flows from small surface-mined and undisturbed Appalachian watersheds in the Tug Fork basin of Kentucky, Virginia, and West Virginia","docAbstract":"<p>Hydrologic and climatologic data were collected at 10 small, mined and unmined watersheds in the Tug Fork basin of Kentucky, Virginia, and West Virginia. These data included continuous records of discharge, precipitation, and air temperature. Daily records of sediment concentrations and sediment discharges were also obtained and periodic observations of water-quality data taken. A compilation of all these data is presented. The observed climatic and hydrologic data from these basins were used to calibrate the U.S. Geological Survey Precipitation-Runoff Modeling System for each watershed. The calibrated models of each basin were then used with a set of nearby, long-term climatic data to simulate a long record of stream-flow. A 68-year record of daily streamflow and 57 years of annual peaks were simulated for each site. These simulated records were analyzed to obtain flood-frequency curves, flow-duration curves, mean-annual discharges, and the 7-day, 10-year low flow for each site. The flow characteristics computed from the simulated records of discharge were analyzed graphically and statistically by regression analysis to investigate the degree of relationship and to define the relationship between mining and runoff. For this sample of small basins, peak flows, discharges for 10- and 50-percent flow durations, and mean-annual flows are directly related to percent of drainage area disturbed (measured from aerial photos) and drainage area. Percent of drainage area disturbed is generally a more statistically significant estimator of discharge than drainage area, particularly for peak flows of higher recurrence intervals.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844151","usgsCitation":"Scott, A.G., 1984, Analysis of characteristics of simulated flows from small surface-mined and undisturbed Appalachian watersheds in the Tug Fork basin of Kentucky, Virginia, and West Virginia: U.S. Geological Survey Water-Resources Investigations Report 84-4151, v, 169 p., https://doi.org/10.3133/wri844151.","productDescription":"v, 169 p.","costCenters":[],"links":[{"id":411369,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36024.htm","linkFileType":{"id":5,"text":"html"}},{"id":58450,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4151/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123615,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4151/report-thumb.jpg"}],"country":"United States","state":"Kentucky, Virginia, West Virginia","otherGeospatial":"Tug Fork basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -81.3,\n              38.144\n            ],\n            [\n              -82.667,\n              38.144\n            ],\n            [\n              -82.667,\n              37.115\n            ],\n            [\n              -81.3,\n              37.115\n            ],\n            [\n              -81.3,\n              38.144\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad0e4b07f02db680c60","contributors":{"authors":[{"text":"Scott, A. G.","contributorId":36552,"corporation":false,"usgs":true,"family":"Scott","given":"A.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":201847,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43703,"text":"ofr8439 - 1984 - Land use  and land cover and associated maps for Forsyth, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:10:10","indexId":"ofr8439","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-39","title":"Land use  and land cover and associated maps for Forsyth, Montana","language":"ENGLISH","doi":"10.3133/ofr8439","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Land use  and land cover and associated maps for Forsyth, Montana: U.S. Geological Survey Open-File Report 84-39, maps :photocopy ;45 x 67 cm., https://doi.org/10.3133/ofr8439.","productDescription":"maps :photocopy ;45 x 67 cm.","costCenters":[],"links":[{"id":162617,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b30e4b07f02db6b40d8","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":531316,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13236,"text":"ofr84881 - 1984 - Flight testing the Aerial Profiling of Terrain System","interactions":[],"lastModifiedDate":"2019-11-01T09:38:11","indexId":"ofr84881","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-881","title":"Flight testing the Aerial Profiling of Terrain System","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr84881","usgsCitation":"Cyran, E.J., and Chapman, W.H., 1984, Flight testing the Aerial Profiling of Terrain System: U.S. Geological Survey Open-File Report 84-881, 18 p. , https://doi.org/10.3133/ofr84881.","productDescription":"18 p. ","costCenters":[],"links":[{"id":145879,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0881/report-thumb.jpg"},{"id":368868,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0881/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5ef286","contributors":{"authors":[{"text":"Cyran, Edward J.","contributorId":75156,"corporation":false,"usgs":true,"family":"Cyran","given":"Edward","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":167450,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chapman, William H.","contributorId":25163,"corporation":false,"usgs":true,"family":"Chapman","given":"William","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":167449,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}