{"pageNumber":"2059","pageRowStart":"51450","pageSize":"25","recordCount":68919,"records":[{"id":1971,"text":"wsp2252 - 1984 - Use of the routing procedure to study dye and gas transport in the West Fork Trinity River, Texas","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp2252","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2252","title":"Use of the routing procedure to study dye and gas transport in the West Fork Trinity River, Texas","docAbstract":"Rhodamine-WT dye, ethylene, and propane were injected at three sites along a 21.6-kilometer reach of the West Fork Trinity River below Fort Worth, Texas. Complete dye concentration versus time curves and peak gas concentrations were measured at three cross sections below each injection. The peak dye concentrations were located and samples were collected at about three-hour intervals for as many as six additional cross sections. These data were analyzed to determine the longitudinal dispersion coefficients as well as the gas desorption coefficients using both standard techniques and a numerical routing procedure. \r\n\r\nThe routing procedure, using a Lagrangian transport model to minimize numerical dispersion, provided better estimates of the dispersion coefficient than did the method of moments. At a steady flow of about 0.76 m2/s, the dispersion coefficient varied from about 0.7 m2/s in a reach contained within a single deep pool to about 2.0 m2/s in a reach containing riffles and small pools. \r\n\r\nThe bulk desorption coefficients computed using the routing procedure and the standard peak method were essentially the same. The liquid film coefficient could also be obtained using the routing procedure. Both the bulk desorption coefficient and the liquid film coefficient were much smaller in the pooled reach than in the reaches containing riffles.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2252","usgsCitation":"Jobson, H.E., and Rathbun, R.E., 1984, Use of the routing procedure to study dye and gas transport in the West Fork Trinity River, Texas: U.S. Geological Survey Water Supply Paper 2252, iv, 21 p. :ill. ;28 cm., https://doi.org/10.3133/wsp2252.","productDescription":"iv, 21 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":138297,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2252/report-thumb.jpg"},{"id":27347,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2252/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa28e","contributors":{"authors":[{"text":"Jobson, Harvey E.","contributorId":27032,"corporation":false,"usgs":true,"family":"Jobson","given":"Harvey","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":144455,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rathbun, R. E.","contributorId":61796,"corporation":false,"usgs":true,"family":"Rathbun","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":144456,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":57307,"text":"wdrCO831 - 1984 - Water Resources Data, Colorado Water Year 1983, Volume 1. Missouri River Basin, Arkansas River Basin, and Rio Grande Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:12:05","indexId":"wdrCO831","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CO-83-1","title":"Water Resources Data, Colorado Water Year 1983, Volume 1. Missouri River Basin, Arkansas River Basin, and Rio Grande Basin","language":"ENGLISH","doi":"10.3133/wdrCO831","usgsCitation":"Ugland, R., Steinheimer, J., Blattner, J., and Steger, R., 1984, Water Resources Data, Colorado Water Year 1983, Volume 1. Missouri River Basin, Arkansas River Basin, and Rio Grande Basin: U.S. Geological Survey Water Data Report CO-83-1, 379 p., 6 fig., 6 tab., https://doi.org/10.3133/wdrCO831.","productDescription":"379 p., 6 fig., 6 tab.","costCenters":[],"links":[{"id":180943,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1983/co-83-1/report-thumb.jpg"},{"id":88257,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1983/co-83-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fc01e","contributors":{"authors":[{"text":"Ugland, R.C.","contributorId":14044,"corporation":false,"usgs":true,"family":"Ugland","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":256655,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steinheimer, J.T.","contributorId":81121,"corporation":false,"usgs":true,"family":"Steinheimer","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":256658,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blattner, J.L.","contributorId":44541,"corporation":false,"usgs":true,"family":"Blattner","given":"J.L.","affiliations":[],"preferred":false,"id":256656,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Steger, R.D.","contributorId":78008,"corporation":false,"usgs":true,"family":"Steger","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":256657,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":25728,"text":"wri844011 - 1984 - Quality and quantity of runoff and atmospheric deposition in urban areas of Salt Lake County, Utah, 1980-81","interactions":[],"lastModifiedDate":"2025-07-21T17:33:27.68156","indexId":"wri844011","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":"84-4011","title":"Quality and quantity of runoff and atmospheric deposition in urban areas of Salt Lake County, Utah, 1980-81","docAbstract":"Water of good quality from mountain streams is degraded as it moves through urban areas to the Jordan River in Salt Lake County, Utah. The impact of urban runoff and atmospheric deposition on the quality of water in those streams and in storm conduits and canals functioning as storm drains was evaluated using data collected during 1980-81. Atmospheric-wetfall loads for an average storm were as much as 10 pounds per acre for total solids, but the dissolved trace metals were generally present in insignificant quantities. Wetfall-deposition loads generally were greater than storm-runoff loads, indicating that a large quantity of the wetfall load remained as soil deposits. Acid rain fell in more than one-half of the storms sampled, most commonly in September and October. Dustfall concentrations reflected the composition of local soils, particularly with regard to iron, manganese, and chromium; but concentrations of cadmium, copper, lead, zinc, and chloride were considerably enriched. Monthly loads of dryfall solids reached a maximum of 62 pounds per acre in the Little Cottonwood Creek urban basin, but were of the same magnitude as total storm loads for a heavy rainfall. Urban runoff represented about 38 percent of the discharge in three canals. The water in the canals was poorer in quality than the water in the mountain streams. The impact of the canal discharges to the streams is slight, however, owing to their ' relatively small amounts. ' Concentrations of sediment, suspended solids, suspended trace metals, phosphorus, and oxygen-demanding substances were much greater during storm runoff than under base-flow conditions. This report contains data for basin and storm characteristics and water-quality information for atmospheric deposition and urban runoff. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844011","collaboration":"Prepared In cooperation with the Salt Lake County Division of Flood Control and Water Quality","usgsCitation":"Christensen, R., Stephens, D.W., Pyper, G., McCormack, H., and Weigel, J.F., 1984, Quality and quantity of runoff and atmospheric deposition in urban areas of Salt Lake County, Utah, 1980-81: U.S. Geological Survey Water-Resources Investigations Report 84-4011, Report: viii, 223 p.; 1 Plate: 25.97 x 20.67 inches, https://doi.org/10.3133/wri844011.","productDescription":"Report: viii, 223 p.; 1 Plate: 25.97 x 20.67 inches","costCenters":[],"links":[{"id":54490,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4011/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157121,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4011/report-thumb.jpg"},{"id":492652,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4011/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","county":"Salt Lake County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"id\":\"47\",\"properties\":{\"name\":\"Utah\",\"nation\":\"USA  \"},\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-111.046551,41.251716],[-111.046723,40.997959],[-110.750727,40.996847],[-110.715026,40.996347],[-110.539819,40.996346],[-110.500718,40.994746],[-110.375714,40.994947],[-110.250709,40.996089],[-110.237848,40.995427],[-110.125709,40.99655],[-110.121639,40.997101],[-110.048476,40.997555],[-110.006495,40.997815],[-110.000708,40.997352],[-109.999838,40.99733],[-109.97553,40.997912],[-109.855299,40.997614],[-109.854302,40.997661],[-109.715409,40.998191],[-109.713877,40.998266],[-109.676421,40.998395],[-109.534926,40.998143],[-109.500694,40.999127],[-109.250735,41.001009],[-109.231985,41.002059],[-109.173682,41.000859],[-109.050076,41.000659],[-109.048455,40.826081],[-109.049088,40.714562],[-109.048373,40.662602],[-109.048249,40.653601],[-109.048044,40.619231],[-109.050074,40.540358],[-109.049955,40.539901],[-109.050698,40.499963],[-109.050314,40.495092],[-109.050946,40.444368],[-109.050969,40.222662],[-109.050973,40.180849],[-109.050944,40.180712],[-109.050813,40.059579],[-109.050873,40.058915],[-109.050615,39.87497],[-109.05104,39.660472],[-109.051363,39.497674],[-109.050765,39.366677],[-109.051512,39.126095],[-109.052436,38.999985],[-109.053292,38.942878],[-109.053233,38.942467],[-109.053797,38.905284],[-109.053943,38.904414],[-109.054189,38.874984],[-109.057388,38.795456],[-109.059541,38.719888],[-109.060253,38.599328],[-109.059962,38.499987],[-109.060062,38.275489],[-109.054648,38.244921],[-109.041762,38.16469],[-109.041837,38.153022],[-109.04282,37.999301],[-109.042819,37.997068],[-109.043121,37.97426],[-109.041058,37.907236],[-109.041653,37.88117],[-109.041844,37.872788],[-109.041723,37.842051],[-109.041754,37.835826],[-109.041461,37.800105],[-109.042098,37.74999],[-109.041636,37.74021],[-109.04176,37.713182],[-109.041732,37.711214],[-109.042269,37.666067],[-109.042089,37.623795],[-109.042131,37.617662],[-109.041806,37.604171],[-109.041865,37.530726],[-109.041915,37.530653],[-109.043137,37.499992],[-109.043464,37.484711],[-109.04581,37.374993],[-109.046039,37.249993],[-109.045584,37.249351],[-109.045487,37.210844],[-109.045978,37.201831],[-109.045995,37.177279],[-109.045156,37.112064],[-109.045203,37.111958],[-109.045173,37.109464],[-109.045189,37.096271],[-109.044995,37.086429],[-109.045058,37.074661],[-109.045166,37.072742],[-109.045223,36.999084],[-109.181196,36.999271],[-109.233848,36.999266],[-109.246917,36.999346],[-109.26339,36.999263],[-109.268213,36.999242],[-109.270097,36.999266],[-109.378039,36.999135],[-109.381226,36.999148],[-109.495338,36.999105],[-109.625668,36.998308],[-109.875673,36.998504],[-110.000677,36.997968],[-110.000876,36.998502],[-110.021778,36.998602],[-110.47019,36.997997],[-110.490908,37.003566],[-110.50069,37.00426],[-110.599512,37.003448],[-110.625605,37.003416],[-110.62569,37.003721],[-110.75069,37.003197],[-111.066496,37.002389],[-111.133718,37.000779],[-111.254853,37.001077],[-111.278286,37.000465],[-111.405517,37.001497],[-111.405869,37.001481],[-111.412784,37.001478],[-112.35769,37.001025],[-112.368946,37.001125],[-112.534545,37.000684],[-112.538593,37.000674],[-112.540368,37.000669],[-112.545094,37.000734],[-112.558974,37.000692],[-112.609787,37.000753],[-112.899366,37.000319],[-112.966471,37.000219],[-113.965907,36.999976],[-113.965907,37.000025],[-114.0506,37.000396],[-114.051749,37.088434],[-114.051822,37.090976],[-114.052827,37.103961],[-114.051867,37.134292],[-114.052179,37.14711],[-114.051673,37.172368],[-114.051405,37.233854],[-114.051974,37.283848],[-114.051974,37.284511],[-114.0518,37.293044],[-114.0518,37.293548],[-114.051927,37.370459],[-114.051927,37.370734],[-114.051765,37.418083],[-114.052448,37.43144],[-114.052701,37.492014],[-114.052685,37.502513],[-114.052718,37.517264],[-114.052689,37.517859],[-114.052962,37.592783],[-114.052472,37.604776],[-114.051728,37.745997],[-114.051785,37.746249],[-114.05167,37.746958],[-114.051109,37.756276],[-114.049919,37.765586],[-114.048473,37.809861],[-114.049677,37.823645],[-114.049928,37.852508],[-114.049658,37.881368],[-114.050423,37.999961],[-114.049903,38.148601],[-114.050138,38.24996],[-114.049417,38.2647],[-114.05012,38.404536],[-114.050091,38.404673],[-114.050485,38.499955],[-114.049834,38.543784],[-114.049862,38.547764],[-114.050154,38.57292],[-114.049883,38.677365],[-114.049749,38.72921],[-114.049168,38.749951],[-114.049465,38.874949],[-114.048521,38.876197],[-114.048054,38.878693],[-114.049104,39.005509],[-114.047079,39.499943],[-114.047728,39.542742],[-114.047273,39.759413],[-114.047783,39.79416],[-114.047214,39.821024],[-114.047134,39.906037],[-114.046555,39.996899],[-114.046835,40.030131],[-114.046386,40.097896],[-114.046741,40.104231],[-114.046683,40.116931],[-114.046153,40.231971],[-114.046178,40.398313],[-114.045826,40.424823],[-114.045218,40.430282],[-114.045518,40.494474],[-114.045577,40.495801],[-114.045281,40.506586],[-114.043505,40.726292],[-114.043831,40.758666],[-114.043803,40.759205],[-114.043176,40.771675],[-114.042145,40.999926],[-114.041447,41.207752],[-114.042553,41.210923],[-114.041396,41.219958],[-114.040231,41.49169],[-114.040942,41.499921],[-114.040437,41.615377],[-114.039968,41.62492],[-114.039901,41.753781],[-114.041152,41.850595],[-114.041107,41.850573],[-114.039648,41.884816],[-114.041723,41.99372],[-113.993903,41.992698],[-113.893261,41.988057],[-113.822163,41.988479],[-113.796082,41.989104],[-113.76453,41.989459],[-113.500837,41.992799],[-113.496548,41.993305],[-113.431563,41.993799],[-113.40223,41.994161],[-113.396497,41.99425],[-113.357611,41.993859],[-113.340072,41.994747],[-113.250829,41.99561],[-113.249159,41.996203],[-113.000821,41.998223],[-113.00082,41.998223],[-112.979218,41.998263],[-112.909587,41.998791],[-112.882367,41.998922],[-112.880619,41.998921],[-112.833125,41.999345],[-112.833084,41.999305],[-112.788542,41.999681],[-112.709375,42.000309],[-112.648019,42.000307],[-112.450814,42.000953],[-112.450567,42.001092],[-112.38617,42.001126],[-112.264936,42.000991],[-112.239107,42.001217],[-112.192976,42.001167],[-112.173352,41.996568],[-112.163956,41.996708],[-112.109532,41.997598],[-112.01218,41.99835],[-111.915837,41.998519],[-111.915622,41.998496],[-111.876491,41.998528],[-111.750778,41.99933],[-111.507264,41.999518],[-111.471381,41.999739],[-111.425535,42.00084],[-111.420898,42.000793],[-111.415873,42.000748],[-111.046689,42.001567],[-111.045818,41.579845],[-111.045789,41.565571],[-111.046264,41.377731],[-111.0466,41.360692],[-111.046551,41.251716]]]}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db655310","contributors":{"authors":[{"text":"Christensen, R.C.","contributorId":56670,"corporation":false,"usgs":true,"family":"Christensen","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":194819,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stephens, D. W.","contributorId":68335,"corporation":false,"usgs":true,"family":"Stephens","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":194820,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pyper, G. E.","contributorId":35337,"corporation":false,"usgs":true,"family":"Pyper","given":"G. E.","affiliations":[],"preferred":false,"id":194818,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McCormack, H.F.","contributorId":93453,"corporation":false,"usgs":true,"family":"McCormack","given":"H.F.","email":"","affiliations":[],"preferred":false,"id":194822,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Weigel, J. F.","contributorId":74394,"corporation":false,"usgs":true,"family":"Weigel","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":194821,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":59053,"text":"mf1710 - 1984 - Bathymetric map of Lydonia Canyon, U.S. Atlantic Outer Continental Shelf","interactions":[],"lastModifiedDate":"2016-08-22T09:47:44","indexId":"mf1710","displayToPublicDate":"1994-01-01T00:00:00","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":"1710","title":"Bathymetric map of Lydonia Canyon, U.S. Atlantic Outer Continental Shelf","docAbstract":"<p>Lydonia Canyon is one of several large submarine canyons that indent the eastern U.S. Continental Shelf along the southern flank of Georges Bank (Index map). &nbsp;This bathymetric map of the upper part of Lydonia Canyon (water depths shallower than about 2,00 m) was prepared as part of a study of the physical oceanography and geology of Lydonia Canyon (Butman and others, 1983; Twichell, 1983). &nbsp;An accurate map of the canyon at a scale of at least 1:50,000 was needed for placement of current-meter morrings, for location of hydrographic and sediment sampling stations, and for interpretation of current-meter and geologic data. The map covers the area from 40&deg;10'N. to&nbsp;40&deg;40'N. and from 67&deg;28'W. to 67&deg;50'W.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1710","usgsCitation":"Butman, B., and Moody, J.A., 1984, Bathymetric map of Lydonia Canyon, U.S. Atlantic Outer Continental Shelf: U.S. Geological Survey Miscellaneous Field Studies Map 1710, 2 Plates: 32.92 x 49.35 inches and 27.74 x 49.69 inches, https://doi.org/10.3133/mf1710.","productDescription":"2 Plates: 32.92 x 49.35 inches and 27.74 x 49.69 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183530,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1710.PNG"},{"id":327161,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1710/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":327162,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1710/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Atlantic Outer Continental Shelf, Lydonia Canyon","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -67.83333333333333,40.166666666666664 ], [ -67.83333333333333,40.666666666666664 ], [ -67.5,40.666666666666664 ], [ -67.5,40.166666666666664 ], [ -67.83333333333333,40.166666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640923","contributors":{"authors":[{"text":"Butman, Bradford 0000-0002-4174-2073 bbutman@usgs.gov","orcid":"https://orcid.org/0000-0002-4174-2073","contributorId":943,"corporation":false,"usgs":true,"family":"Butman","given":"Bradford","email":"bbutman@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":261334,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moody, John A. 0000-0003-2609-364X jamoody@usgs.gov","orcid":"https://orcid.org/0000-0003-2609-364X","contributorId":771,"corporation":false,"usgs":true,"family":"Moody","given":"John","email":"jamoody@usgs.gov","middleInitial":"A.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":261335,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26338,"text":"wri844017 - 1984 - Source, movement, and effects of nitrogen and phosphorus in three ponds in the headwaters of Hop Brook, Marlborough, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:08:27","indexId":"wri844017","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":"84-4017","title":"Source, movement, and effects of nitrogen and phosphorus in three ponds in the headwaters of Hop Brook, Marlborough, Massachusetts","docAbstract":"The headwaters of Hop Brook near Marlborough, Massachusetts, contain a series of three in-line ponds--Hager Pond, Brist Millpond, and Carding Millpond--which receive over half of their surface-water inflow as effluent from the Marlborough Easterly Wastewater Treatment Plant. These ponds have a history of summer algal blooms and fish kills. Water entering these ponds contains quantities of nitrogen and phosphorus far higher than the levels known to promote excessive growth of aquatic vegetation. As the water moves through the three ponds, nitrogen levels decrease. Although some nitrogen is lost to the atmosphere by denitrification, the bulk of the nitrogen probably is retained in the pond sediments. There is a net decrease in phosphorus in the water leaving Carding Millpond compared to the water entering Hager Pond. However, during most sampling periods, the phosphorus concentration of water leaving Carding Millpond is still above the level known to cause excessive growth of aquatic vegetation in lakes. During certain summer periods, there appears to be release of some phosphorus from the sediments in Carding and Grist Millponds. No improvement in water quality of the three ponds can be expected until the concentrations of nutrients entering Hager Pond are reduced to levels that will not support excessive growth of aquatic vegetation. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844017","usgsCitation":"Briggs, J.C., and Silvey, W.D., 1984, Source, movement, and effects of nitrogen and phosphorus in three ponds in the headwaters of Hop Brook, Marlborough, Massachusetts: U.S. Geological Survey Water-Resources Investigations Report 84-4017, iv, 55 p. :ill., map ;28 cm., https://doi.org/10.3133/wri844017.","productDescription":"iv, 55 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":2022,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri844017/","linkFileType":{"id":5,"text":"html"}},{"id":158017,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7758","contributors":{"authors":[{"text":"Briggs, John C.","contributorId":24349,"corporation":false,"usgs":true,"family":"Briggs","given":"John","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":196205,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Silvey, William D.","contributorId":74036,"corporation":false,"usgs":true,"family":"Silvey","given":"William","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":196206,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":12510,"text":"ofr84714 - 1984 - Water-quality data for selected wells on or near the Idaho National Engineering Laboratory, 1949 through 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:06:51","indexId":"ofr84714","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":"84-714","title":"Water-quality data for selected wells on or near the Idaho National Engineering Laboratory, 1949 through 1982","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84714","usgsCitation":"Bagby, J., White, L., and Jensen, R.G., 1984, Water-quality data for selected wells on or near the Idaho National Engineering Laboratory, 1949 through 1982: U.S. Geological Survey Open-File Report 84-714, vii, 797 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84714.","productDescription":"vii, 797 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":147245,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0714/report-thumb.jpg"},{"id":40756,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0714/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fac9d","contributors":{"authors":[{"text":"Bagby, J.C.","contributorId":51288,"corporation":false,"usgs":true,"family":"Bagby","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":166251,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, L.J.","contributorId":67080,"corporation":false,"usgs":true,"family":"White","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":166253,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jensen, R. G.","contributorId":63799,"corporation":false,"usgs":true,"family":"Jensen","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":166252,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":38647,"text":"pp1151D - 1984 - Stratigraphy and structure of the western Kentucky fluorspar district","interactions":[],"lastModifiedDate":"2012-02-02T00:09:58","indexId":"pp1151D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1151","chapter":"D","title":"Stratigraphy and structure of the western Kentucky fluorspar district","docAbstract":"The western Kentucky fluorspar district is part of the larger Illinois-Kentucky fluorspar district, the largest producer of fluorspar in the United States. This report is based largely on data gathered from 1960 to 1974 during the U.S. Geological Survey-Kentucky Geological Survey cooperative geologic mapping program of Kentucky. It deals chiefly with the stratigraphy and structure of the district and, to a lesser extent, with the fluorspar-zinc-lead-barite deposits. \r\n\r\nSedimentary rocks exposed in the district range in age from Early Mississippian (Osagean) to Quaternary. Most rocks exposed at the surface are Mississippian in age; two-thirds are marine fossiliferous limestones, and the remainder are shales, siltstones, and sandstones. Osagean deep-water marine silty limestone and chert are present at the surface in the southwestern corner of the district. Meramecian marine limestone is exposed at the surface in about half the area. Chesterian marine and fluvial to fluviodeltaic clastic sedimentary rocks and marine limestone underlie about one-third of the area. The total sequence of Mississippian rocks is about 3,000 ft thick. \r\n\r\nPennsylvanian rocks are dominantly fluvial clastic sedimentary rocks that change upward into younger fluviodeltaic strata. Pennsylvanian strata of Morrowan and Atokan age are locally thicker than 600 ft along the eastern and southeastern margin and in the major grabens of the district where they have been preserved from erosion. \r\n\r\nCretaceous and Tertiary sediments of the Mississippi embayment truncate Paleozoic formations in and near the southwestern corner of the district and are preserved mostly as erosional outliers. The deposits are Gulfian nonmarine gravels, sands, and clays as much as 170 ft thick and upper Pliocene fluvial continental deposits as thick as 45 ft. Pleistocene loess deposits mantle the upland surface of the district, and Quaternary fluvial and fluviolacustrine deposits are common and widespread along the Ohio and Cumberland Rivers and their major tributaries. \r\n\r\nMany mafic dikes and a few mafic sills are present. The mafic rocks are mostly altered mica peridotites or lamprophyres that are composed of carbonate minerals, serpentine, chlorite, and biotite and contain some hornblende, pyroxene, and olivine. Most of the dikes are in a north-north west-trending belt 6 to 8 mi wide and strike N. 20 0 -30 0 W. The dikes dip from 80 0 to 90 0 and are commonly 5 to 10 ft wide. Radioisotopic study indicates that the dikes are Early Permian in age. \r\n\r\nThe district is just southeast of the intersection of the east-trending Rough Creek-Shawneetown and northeast-trending New Madrid fault systems. The district's principal structural features are a northwest-trending domal anticline, the Tolu Arch, and a series of steeply dipping to nearly vertical normal faults and fault zones that trend dominantly northeastward and divide the area into elongated northeast-trending grabens and horsts. Formation of these grabens and horsts was one of the major tectonic events in the district. Vertical displacement may be as much as 3,000 ft but commonly ranges from a few feet to a few hundred feet; no substantial horizontal movement is believed to have taken place. Many cross faults having only a few feet of displacement trend northwestward and are occupied at places by mafic dikes. Faulting was mostly post-Early Permian to pre-middle Cretaceous in age. \r\n\r\nMany theories have been advanced to explain the structural history of the district. A generally acceptable overall hypothesis that would account for all the structural complexities, however, is still lacking. Useful structural data, such as the structural differences between the grabens and the horsts, have been obtained, however, from the recently completed geologic mapping. Mapping also has more clearly shown the alinement of the Tolu Arch, the belt of dikes, and an unusually deep graben (the Griffith Bluff graben); this alinement suggests that possibl","language":"ENGLISH","doi":"10.3133/pp1151D","usgsCitation":"Trace, R.D., and Amos, D., 1984, Stratigraphy and structure of the western Kentucky fluorspar district: U.S. Geological Survey Professional Paper 1151, p. D1-D41; 1 plate in pocket, https://doi.org/10.3133/pp1151D.","productDescription":"p. D1-D41; 1 plate in pocket","costCenters":[],"links":[{"id":119900,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1151d/report-thumb.jpg"},{"id":65478,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1151d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65479,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1151d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a7fee","contributors":{"authors":[{"text":"Trace, R. D.","contributorId":47004,"corporation":false,"usgs":true,"family":"Trace","given":"R.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":220215,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Amos, D.H.","contributorId":75600,"corporation":false,"usgs":true,"family":"Amos","given":"D.H.","email":"","affiliations":[],"preferred":false,"id":220216,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21883,"text":"ofr84303 - 1984 - Ice free valleys, Victoria Land, Antarctica; topographic map, 1962","interactions":[],"lastModifiedDate":"2012-02-02T00:07:44","indexId":"ofr84303","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":"84-303","title":"Ice free valleys, Victoria Land, Antarctica; topographic map, 1962","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr84303","issn":"0566-8174","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Ice free valleys, Victoria Land, Antarctica; topographic map, 1962: U.S. Geological Survey Open-File Report 84-303, 1 map on 2 sheets ;83 x 94 cm., sheets 65 x 101 cm., https://doi.org/10.3133/ofr84303.","productDescription":"1 map on 2 sheets ;83 x 94 cm., sheets 65 x 101 cm.","costCenters":[],"links":[{"id":153060,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":51371,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0303/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":51372,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0303/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb967","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":529078,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15469,"text":"ofr84818 - 1984 - Land subsidence in the Santa Clara Valley, California as of 1980","interactions":[{"subject":{"id":15469,"text":"ofr84818 - 1984 - Land subsidence in the Santa Clara Valley, California as of 1980","indexId":"ofr84818","publicationYear":"1984","noYear":false,"title":"Land subsidence in the Santa Clara Valley, California as of 1980"},"predicate":"SUPERSEDED_BY","object":{"id":38874,"text":"pp497F - 1988 - Land subsidence in the Santa Clara Valley, California, as of 1982","indexId":"pp497F","publicationYear":"1988","noYear":false,"chapter":"F","title":"Land subsidence in the Santa Clara Valley, California, as of 1982"},"id":1}],"supersededBy":{"id":38874,"text":"pp497F - 1988 - Land subsidence in the Santa Clara Valley, California, as of 1982","indexId":"pp497F","publicationYear":"1988","noYear":false,"title":"Land subsidence in the Santa Clara Valley, California, as of 1982"},"lastModifiedDate":"2019-08-29T10:12:02","indexId":"ofr84818","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":"84-818","title":"Land subsidence in the Santa Clara Valley, California as of 1980","docAbstract":"From 1916 to 1966 in the San Jose area of Santa Clara Valley, California, deficient rainfall and runoff was accompanied by a fourfold increase in groundwater withdrawals. In response the artesian head declined 180-240 ft. The land surface subsided 12.7 ft in San Jose, due to compaction of the fine-grained compressible beds. The subsidence resulted in flooding of lands, and the compaction of the sediments caused compressional failure of many well casings. From 1967 to 1975, the artesian head recovered 70 to 100 feet due to a fivefold increase in surface water imports, favorable local water supply, decreased withdrawal, and increased recharge. In 1960, the Geological Survey installed extensometers in core holes 1,000 ft deep in San Jose and Sunnyvale. Measurements of compaction of the confined aquifer system obtained from these extensometers demonstrate the marked decrease in rate of compaction in response to the major head recovery since 1967. In San Jose the rate decreased from about 1 ft/yr in 1961 to 0.1 ft/yr in 1973. The subsidence has been stopped by raising the artesian head in the aquifers until it equaled or exceeded the maximum pore pressures in the fine-grained beds. However, the subsidence will recommence if the artesian head is drawn down appreciably below the levels of 1971-73. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr84818","usgsCitation":"Poland, J.F., and Ireland, R.L., 1984, Land subsidence in the Santa Clara Valley, California as of 1980: U.S. Geological Survey Open-File Report 84-818, vi, 93 p. , https://doi.org/10.3133/ofr84818.","productDescription":"vi, 93 p. ","costCenters":[],"links":[{"id":147961,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0818/report-thumb.jpg"},{"id":367074,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0818/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Santa Clara Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.420654296875,\n              36.97183825093165\n            ],\n            [\n              -121.40991210937499,\n              36.97183825093165\n            ],\n            [\n              -121.40991210937499,\n              37.58811876638322\n            ],\n            [\n              -122.420654296875,\n              37.58811876638322\n            ],\n            [\n              -122.420654296875,\n              36.97183825093165\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae9aa","contributors":{"authors":[{"text":"Poland, J. F.","contributorId":64223,"corporation":false,"usgs":true,"family":"Poland","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":171181,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ireland, R. L.","contributorId":89893,"corporation":false,"usgs":true,"family":"Ireland","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":171182,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":19592,"text":"ofr836 - 1984 - Engineering geology studies in the National Petroleum Reserve, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:07:29","indexId":"ofr836","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":"83-6","title":"Engineering geology studies in the National Petroleum Reserve, Alaska","docAbstract":"Engineering geology studies were conducted in direct support of the exploration program in the National Petroleum Reserve, Alaska. The studies included laboratory and field tests and observations to address design and construction problems of airfields, roads, drill pads and foundations, and to evaluate their actual performance. Permafrost containing large amounts of near surface ground ice as wedges, masses, and intergranular ice, required that all construction activity not disturb the thermal regime of the ground surface, which could lead to thaw of permafrost and ground subsidence. Summer activity, therefore was not allowable, yet the winter climate was so harsh that winter work was slow and inefficient. To allow summer operations at well sites planned for all year activity, it was necessary to adapt existing techniques for arctic construction and to devise new ones. \r\n\r\nThe design and construction of facilities at the deep exploration wells at Inigok, Tunalik, and Lisburne posed the greatest challenge. These sites, requiring a year or more to drill, could only be attempted if continuous access to drilling and logistic supplies could be assured throughout the year, including the possibility of bringing in another drill rig, in the event of a blowout. Thus all-seasons airstrips were required at these wells. Sufficient quantities of local gravel were not readily available at the Inigok and Tunalik sites to construct the airstrips with the required 6 feet or more of gravel to prevent the underlying permafrost from thawing. Therefore, insulation was used to maintain the subbase of local sands in a continuously frozen state, which in turn was overlain by 15 inches of gravel or sandy gravel. Tests at the U.S. Army Waterways Experimental Station defined the minimum thickness of gravel required above the insulation to provide the desired bearing capacity for the C-130 type aircraft without crushing the insulation. \r\n\r\nField testing also included the evaluation of another design option, using military landing mat underlain by insulation. Temperature recording devices were installed beneath the landing mat test sections, insulated runways, roads, drill pads, and reserve pits, to monitor the actual conditions and confirm the design assumptions. Investigations of thaw-settlement, erosion, and revegetation of all areas affected by construction were also conducted in anticipation of abandoning the sites, or, upgrading the facilities in the event the design life was extended.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr836","usgsCitation":"Kachadoorian, R., and Crory, F., 1984, Engineering geology studies in the National Petroleum Reserve, Alaska: U.S. Geological Survey Open-File Report 83-6, i, 37 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr836.","productDescription":"i, 37 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":151952,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0006/report-thumb.jpg"},{"id":49061,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0006/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db60271a","contributors":{"authors":[{"text":"Kachadoorian, Reuben","contributorId":24336,"corporation":false,"usgs":true,"family":"Kachadoorian","given":"Reuben","email":"","affiliations":[],"preferred":false,"id":181177,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crory, F.E.","contributorId":45734,"corporation":false,"usgs":true,"family":"Crory","given":"F.E.","email":"","affiliations":[],"preferred":false,"id":181178,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":45824,"text":"ofr84589 - 1984 - Linear features determined from Landsat imagery in the Texas and Oklahoma panhandles","interactions":[],"lastModifiedDate":"2012-02-02T00:04:59","indexId":"ofr84589","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":"84-589","title":"Linear features determined from Landsat imagery in the Texas and Oklahoma panhandles","docAbstract":"A map (scale 1:500,000) shows the linear features determined from Landsat imagery in the Texas and Oklahoma panhandles. The linear features, sometimes called linear trends or lineaments, are not identified as to type or origin. Most probably represent fractures or fracture zones, which may affect the movement of water or other fluids through rocks. The linear features are classified as to length--less than 30 mi/mg and more than 30 mi/mg. (USGS)","language":"ENGLISH","doi":"10.3133/ofr84589","usgsCitation":"Cooley, M.E., 1984, Linear features determined from Landsat imagery in the Texas and Oklahoma panhandles: U.S. Geological Survey Open-File Report 84-589, 1 map :photocopy ;80 x 56 cm., on sheet 98 x 83 cm., https://doi.org/10.3133/ofr84589.","productDescription":"1 map :photocopy ;80 x 56 cm., on sheet 98 x 83 cm.","costCenters":[],"links":[{"id":135881,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":82801,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0589/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4bd1","contributors":{"authors":[{"text":"Cooley, M. E.","contributorId":89868,"corporation":false,"usgs":true,"family":"Cooley","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":232081,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27819,"text":"wri844006 - 1984 - Hydrogeology of the Verna well-field area and management alternatives for improving yield and quality of water, Sarasota County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:43","indexId":"wri844006","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":"84-4006","title":"Hydrogeology of the Verna well-field area and management alternatives for improving yield and quality of water, Sarasota County, Florida","docAbstract":"About 8 million gallons of water are pumped daily from the 3-square-mile Verna well field to supply the city of Sarasota. Pumping has resulted in water-level declines and changes in water quality. Drawdowns of at least 30 feet have occurred in the producing zone at the well-field boundaries. Sulfate concentrations in the pumped water have increased from about 200 milligrams per liter in 1966 to about 400 milligrams per liter in 1982 in the western part of the well field. In the eastern part, sulfate concentrations have increased from about 300 to 350 milligrams per liter during this period. The increases roughly coincide with increases in pumping rates. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844006","usgsCitation":"Hutchinson, C.B., 1984, Hydrogeology of the Verna well-field area and management alternatives for improving yield and quality of water, Sarasota County, Florida: U.S. Geological Survey Water-Resources Investigations Report 84-4006, v, 53 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844006.","productDescription":"v, 53 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124123,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4006/report-thumb.jpg"},{"id":56655,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4006/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ee4b07f02db615028","contributors":{"authors":[{"text":"Hutchinson, C. B.","contributorId":94655,"corporation":false,"usgs":true,"family":"Hutchinson","given":"C.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":198734,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25645,"text":"wri834122E - 1984 - Map showing outcrops of thick, dominantly argillaceous sedimentary and metasedimentary rocks, Basin and Range province, Utah","interactions":[],"lastModifiedDate":"2022-01-05T19:42:12.264942","indexId":"wri834122E","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":"83-4122","chapter":"E","title":"Map showing outcrops of thick, dominantly argillaceous sedimentary and metasedimentary rocks, Basin and Range province, Utah","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834122E","usgsCitation":"Johnson, W., 1984, Map showing outcrops of thick, dominantly argillaceous sedimentary and metasedimentary rocks, Basin and Range province, Utah: U.S. Geological Survey Water-Resources Investigations Report 83-4122, Report: 10 p.; 1 Plate: 24.93 × 46.49 inches, https://doi.org/10.3133/wri834122E.","productDescription":"Report: 10 p.; 1 Plate: 24.93 × 46.49 inches","costCenters":[],"links":[{"id":393925,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35785.htm"},{"id":54409,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4122e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54408,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4122e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121724,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4122e/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Basin and Range province","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.042,\n              37\n            ],\n            [\n              -111.29,\n              37\n            ],\n            [\n              -111.29,\n              42\n            ],\n            [\n              -114.042,\n              42\n            ],\n            [\n              -114.042,\n              37\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b14e4b07f02db6a47c4","contributors":{"authors":[{"text":"Johnson, W. D.","contributorId":16865,"corporation":false,"usgs":true,"family":"Johnson","given":"W. D.","affiliations":[],"preferred":false,"id":194504,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25635,"text":"wri834119D - 1984 - Map showing outcrops of granitic rocks, Basin and Range Province, Nevada","interactions":[],"lastModifiedDate":"2020-03-27T14:54:31","indexId":"wri834119D","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":"83-4119","chapter":"D","title":"Map showing outcrops of granitic rocks, Basin and Range Province, Nevada","docAbstract":"<p>This map report is one of a series of geologic and hydrologic maps covering all or parts of States within the Basin and Range province of the western United States. The map reports contain information on subjects that characterize the geohydrology of the province, including the ground-water hydrology, ground-water quality, surface distribution of selected rock types, tectonic conditions, areal geophysics, Pleistocene lakes and marshes, and mineral and energy resources. This work is a part of the U.S. Geological Survey's program for geologic and hydrologic evaluation of the Basin and Range province to identify potentially suitable regions for further study relative to isolation of high-level nuclear waste (Bedinger, Sargent, and Reed, 1984).</p><p>Data for this report were taken largely from Spengler and others (1979), supplemented by data from individual geologic maps and reports, following the project guidelines as defined in Sargent and Bedinger (1984). As used in this report, granitic rocks include granodiorite, quartz monzonite, and granite, and locally associated mafic rocks such as diorite and gabbro. In the Snake Range and Ruby Mountains, Stewart (1980) has recognized large areas as metamorphic core complexes, and in these complexes some plutonic masses may not extend to great depth because of lateral displacement along low-angle faults subsequent to intrusion.</p><p>The Description of Map Units includes the sources of data, the geologic, and if available, the radiometric age, lithologic character, type of intrusive body and relation to rock units, where known, for the granitic rocks within outlined and numbered areas in each county of the study area. The radiometric ages of the rock units are only those which are available and do not necessarily represent the entire age range of the geologic units.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834119D","usgsCitation":"Sargent, K.A., and Roggensack, K., 1984, Map showing outcrops of granitic rocks, Basin and Range Province, Nevada: U.S. Geological Survey Water-Resources Investigations Report 83-4119, Report: 36 p.; 2 Plates: 44.34 x 34.69 inches and 43.46 x 37.84 inches, https://doi.org/10.3133/wri834119D.","productDescription":"Report: 36 p.; 2 Plates: 44.34 x 34.69 inches and 43.46 x 37.84 inches","costCenters":[],"links":[{"id":118874,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4119d/report-thumb.jpg"},{"id":54388,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4119d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":373628,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4119d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":373629,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4119d/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","datum":"National Geodetic Vertical Datum of 1929","country":"United States","state":"Nevada","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.0146484375,\n              35.02099970111467\n            ],\n            [\n              -114.027099609375,\n              35.02099970111467\n            ],\n            [\n              -114.027099609375,\n              42.00032514831621\n            ],\n            [\n              -120.0146484375,\n              42.00032514831621\n            ],\n            [\n              -120.0146484375,\n              35.02099970111467\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a37e6","contributors":{"authors":[{"text":"Sargent, K. A.","contributorId":58630,"corporation":false,"usgs":true,"family":"Sargent","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":194486,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roggensack, Kurt","contributorId":35771,"corporation":false,"usgs":true,"family":"Roggensack","given":"Kurt","email":"","affiliations":[],"preferred":false,"id":194485,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25628,"text":"wri834119F - 1984 - Map showing outcrops of basaltic rocks of early Quaternary and Tertiary age, Basin and Range Province, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:08:21","indexId":"wri834119F","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":"83-4119","chapter":"F","title":"Map showing outcrops of basaltic rocks of early Quaternary and Tertiary age, Basin and Range Province, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834119F","usgsCitation":"Roggensack, K., and Sargent, K.A., 1984, Map showing outcrops of basaltic rocks of early Quaternary and Tertiary age, Basin and Range Province, Nevada: U.S. Geological Survey Water-Resources Investigations Report 83-4119, 20 p. :maps ;28 cm., https://doi.org/10.3133/wri834119F.","productDescription":"20 p. :maps ;28 cm.","costCenters":[],"links":[{"id":118868,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4119f/report-thumb.jpg"},{"id":54374,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4119f/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54375,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4119f/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54376,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4119f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a374e","contributors":{"authors":[{"text":"Roggensack, Kurt","contributorId":35771,"corporation":false,"usgs":true,"family":"Roggensack","given":"Kurt","email":"","affiliations":[],"preferred":false,"id":194471,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sargent, K. A.","contributorId":58630,"corporation":false,"usgs":true,"family":"Sargent","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":194472,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":18112,"text":"ofr8463 - 1984 - Geohydrologic data for test well USW G-4, Yucca Mountain area, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:07:16","indexId":"ofr8463","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":"84-63","title":"Geohydrologic data for test well USW G-4, Yucca Mountain area, Nye County, Nevada","docAbstract":"Data are presented on drilling operations, lithology, borehole geophysics, hydrologic monitoring, core analysis, water chemistry, pumping tests, and packer-injection tests for test well USW G-4. The well is one of a series of test wells drilled in and near the southwestern part of the Nevada Test Site, Nye County, Nevada, in cooperation with the U.S. Department of Energy. These test wells are part of the Nevada Nuclear Waste Storage Investigations to identify suitable sites for underground storage of high-level radioactive wastes. Test well USW G-4 was drilled to a total depth of 915 meters through volcanic rocks, consisting mostly of ash-flow tuff. Depth of water in the well during and after drilling and testing ranged from 538 to 544 meters below land surface, at approximate altitude of 728 meters above sea level. Drawdown in the well was about 3 meters after test pumping more than 5,000 minutes at a rate of 16 liters per second. A borehold-flow survey indicated that almost all water withdrawn from the well was contributed by the zone between a depth of about 865 and 915 meters below land surface. Analysis of a composite water sample collected after well completion showed the water to contain 216 milligrams per liter of dissolved solids, with relatively large concentrations of silica, sodium, and bicarbonate. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8463","usgsCitation":"Bentley, C., 1984, Geohydrologic data for test well USW G-4, Yucca Mountain area, Nye County, Nevada: U.S. Geological Survey Open-File Report 84-63, v, 67 p. :ill. ;28 cm., https://doi.org/10.3133/ofr8463.","productDescription":"v, 67 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":149312,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0063/report-thumb.jpg"},{"id":47467,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0063/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8f1c","contributors":{"authors":[{"text":"Bentley, C.B.","contributorId":28223,"corporation":false,"usgs":true,"family":"Bentley","given":"C.B.","email":"","affiliations":[],"preferred":false,"id":178569,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":45715,"text":"pp1292AB - 1984 - Geology, geochemistry, and age of Archean and Early Proterozoic rocks in the Marenisco-Watersmeet area, northern Michigan; and Geologic interpretation of gravity data, Marenisco-Watersmeet area, northern Michigan","interactions":[],"lastModifiedDate":"2022-06-10T19:47:05.247792","indexId":"pp1292AB","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1292","chapter":"A,B","title":"Geology, geochemistry, and age of Archean and Early Proterozoic rocks in the Marenisco-Watersmeet area, northern Michigan; and Geologic interpretation of gravity data, Marenisco-Watersmeet area, northern Michigan","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1292AB","usgsCitation":"Sims, P., Peterman, Z.E., Prinz, W.C., Benedict, F.C., and Klasner, J.S., 1984, Geology, geochemistry, and age of Archean and Early Proterozoic rocks in the Marenisco-Watersmeet area, northern Michigan; and Geologic interpretation of gravity data, Marenisco-Watersmeet area, northern Michigan: U.S. Geological Survey Professional Paper 1292, 68 p., https://doi.org/10.3133/pp1292AB.","productDescription":"68 p.","costCenters":[],"links":[{"id":82299,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1292a-b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":135174,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1292a-b/report-thumb.jpg"},{"id":402068,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4789.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Michigan","otherGeospatial":"Marenisco-Watersmeet area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.75,\n              46.25\n            ],\n            [\n              -89.0339,\n              46.25\n            ],\n            [\n              -89.0339,\n              46.5\n            ],\n            [\n              -89.75,\n              46.5\n            ],\n            [\n              -89.75,\n              46.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c697","contributors":{"authors":[{"text":"Sims, P.K.","contributorId":30191,"corporation":false,"usgs":true,"family":"Sims","given":"P.K.","email":"","affiliations":[],"preferred":false,"id":231896,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterman, Z. E.","contributorId":63781,"corporation":false,"usgs":true,"family":"Peterman","given":"Z.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":231897,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Prinz, W. C.","contributorId":82670,"corporation":false,"usgs":true,"family":"Prinz","given":"W.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":231899,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Benedict, F. C.","contributorId":97068,"corporation":false,"usgs":true,"family":"Benedict","given":"F.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":231900,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Klasner, J. S.","contributorId":66228,"corporation":false,"usgs":true,"family":"Klasner","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":231898,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":27781,"text":"wri844139 - 1984 - Determination of reaeration coefficients for Ohio streams","interactions":[],"lastModifiedDate":"2012-02-02T00:08:26","indexId":"wri844139","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":"84-4139","title":"Determination of reaeration coefficients for Ohio streams","docAbstract":"The hydrocarbon-gas tracer technique was used to determine reaeration coefficients on 30 reaches of Ohio streams. The studies were done from September 1979 through August 1982 to determine the reaeration coefficients for the individual reaches and to develop general equation that could be used to estimate the coefficients. \r\n\r\nMultiple linear regression was used to determine relationships among the reaeration coefficients and physical stream characteristics. Four special equation based on the general equation were developed from various combinations of discharge, slope, width, depth, measured velocity, and estimated velocity. The standard errors of estimate for these equations ranged from 37 to 47 percent. The variables that resulted in the lowest standard error of estimate were discharge, slope, width, depth, and measured velocity. The most significant variables were depth and velocity.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844139","usgsCitation":"Hren, J., 1984, Determination of reaeration coefficients for Ohio streams: U.S. Geological Survey Water-Resources Investigations Report 84-4139, iii, 12 p. :map ;28 cm., https://doi.org/10.3133/wri844139.","productDescription":"iii, 12 p. :map ;28 cm.","costCenters":[],"links":[{"id":123885,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4139/report-thumb.jpg"},{"id":56624,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4139/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6676a0","contributors":{"authors":[{"text":"Hren, Janet","contributorId":69554,"corporation":false,"usgs":true,"family":"Hren","given":"Janet","email":"","affiliations":[],"preferred":false,"id":198677,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27783,"text":"wri844117 - 1984 - A statistical approach to evaluate the relation of coal mining, land reclamation, and surface-water quality in Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:08:35","indexId":"wri844117","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":"84-4117","title":"A statistical approach to evaluate the relation of coal mining, land reclamation, and surface-water quality in Ohio","docAbstract":"Base-flow data from 779 sites in Ohio 's coal region were analyzed statistically to relate land use to selected water-quality characteristics. Sites were classified into five categories: unmined (100 percent unmined land), abandoned (50 percent or more abandoned surface mines), reclaimed (50 percent or more reclaimed surface mines), deep-mined (50 percent or more underground mines), and mixed (all others). Specific conductance , pH, alkalinity, acidity, sulfate, dissolved iron, total iron, and total manganese in streams draining basins in the coal region were the eight characteristics selected for analysis. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844117","usgsCitation":"Hren, J., Wilson, K.S., and Helsel, D., 1984, A statistical approach to evaluate the relation of coal mining, land reclamation, and surface-water quality in Ohio: U.S. Geological Survey Water-Resources Investigations Report 84-4117, iv, 325 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844117.","productDescription":"iv, 325 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124255,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4117/report-thumb.jpg"},{"id":56626,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4117/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a62d6","contributors":{"authors":[{"text":"Hren, Janet","contributorId":69554,"corporation":false,"usgs":true,"family":"Hren","given":"Janet","email":"","affiliations":[],"preferred":false,"id":198681,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, K. S.","contributorId":41042,"corporation":false,"usgs":true,"family":"Wilson","given":"K.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":198679,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Helsel, D.R.","contributorId":57448,"corporation":false,"usgs":false,"family":"Helsel","given":"D.R.","email":"","affiliations":[{"id":7242,"text":"Wisconsin Department of Natural Resources, Madison, WI, USA","active":true,"usgs":false}],"preferred":false,"id":198680,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":47190,"text":"ofr8452 - 1984 - Flow characteristics of the Snake River and water budget for the Snake River plain, Idaho and eastern Oregon","interactions":[{"subject":{"id":47190,"text":"ofr8452 - 1984 - Flow characteristics of the Snake River and water budget for the Snake River plain, Idaho and eastern Oregon","indexId":"ofr8452","publicationYear":"1984","noYear":false,"title":"Flow characteristics of the Snake River and water budget for the Snake River plain, Idaho and eastern Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":68263,"text":"ha680 - 1986 - Flow characteristics of the Snake River and water budget for the Snake River Plain, Idaho and eastern Oregon","indexId":"ha680","publicationYear":"1986","noYear":false,"title":"Flow characteristics of the Snake River and water budget for the Snake River Plain, Idaho and eastern Oregon"},"id":1}],"supersededBy":{"id":68263,"text":"ha680 - 1986 - Flow characteristics of the Snake River and water budget for the Snake River Plain, Idaho and eastern Oregon","indexId":"ha680","publicationYear":"1986","noYear":false,"title":"Flow characteristics of the Snake River and water budget for the Snake River Plain, Idaho and eastern Oregon"},"lastModifiedDate":"2022-04-27T18:12:32.179177","indexId":"ofr8452","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":"84-52","title":"Flow characteristics of the Snake River and water budget for the Snake River plain, Idaho and eastern Oregon","docAbstract":"<p>This report is one in a series resulting from the U.S. Geological Survey's Snake River Plain Rasa (Regional Aquifer System Analysis) study that was initiation in October 1979.&nbsp;</p><p>Purposes of the RASA study were to (1) refine knowledge of the regional ground-water flow system, (2) determine effects of conjunctive use of ground water and surface water, and (3) describe water chemistry. This purpose of this report is to describe flow characteristics of the Snake River and tributaries and to develop a water budget for the Snake River Plain. Data and interpretation in this report will be used in development of ground-water flow models.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8452","usgsCitation":"Kjelstrom, L., 1984, Flow characteristics of the Snake River and water budget for the Snake River plain, Idaho and eastern Oregon: U.S. Geological Survey Open-File Report 84-52, 2 Plates: 50.67 x 38.09 inches and 41.32 x 30.24 inches, https://doi.org/10.3133/ofr8452.","productDescription":"2 Plates: 50.67 x 38.09 inches and 41.32 x 30.24 inches","costCenters":[],"links":[{"id":399778,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0052/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":399777,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0052/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":135235,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0052/report-thumb.jpg"}],"scale":"500000","country":"United States","state":"Idaho, Oregon","otherGeospatial":"Snake River plain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.1142578125,\n              44.5278427984555\n            ],\n            [\n              -117.46582031249999,\n              44.276671273775186\n            ],\n            [\n              -117.57568359374999,\n              43.77109381775651\n            ],\n            [\n              -116.8505859375,\n              43.27720532212024\n            ],\n            [\n              -116.4111328125,\n              42.924251753870685\n            ],\n            [\n              -115.29052734375,\n              42.4234565179383\n            ],\n            [\n              -114.2578125,\n              42.342305278572816\n            ],\n            [\n              -112.8955078125,\n              42.61779143282346\n            ],\n            [\n              -112.4560546875,\n              43.197167282501276\n            ],\n            [\n              -111.7529296875,\n              43.644025847699496\n            ],\n            [\n              -111.4892578125,\n              44.213709909702054\n            ],\n            [\n              -111.4892578125,\n              44.32384807250689\n            ],\n            [\n              -111.884765625,\n              44.74673324024678\n            ],\n            [\n              -112.52197265625,\n              44.62175409623324\n            ],\n            [\n              -112.8515625,\n              44.276671273775186\n            ],\n            [\n              -113.64257812499999,\n              43.51668853502906\n            ],\n            [\n              -114.12597656249999,\n              43.51668853502906\n            ],\n            [\n              -114.9169921875,\n              43.56447158721811\n            ],\n            [\n              -115.3564453125,\n              43.59630591596548\n            ],\n            [\n              -115.90576171874999,\n              43.67581809328341\n            ],\n            [\n              -116.1474609375,\n              44.10336537791152\n            ],\n            [\n              -116.03759765625,\n              44.37098696297173\n            ],\n            [\n              -116.3232421875,\n              44.824708282300236\n            ],\n            [\n              -116.71874999999999,\n              44.74673324024678\n            ],\n            [\n              -117.1142578125,\n              44.5278427984555\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5defef","contributors":{"authors":[{"text":"Kjelstrom, L.C.","contributorId":89104,"corporation":false,"usgs":true,"family":"Kjelstrom","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":234796,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57499,"text":"wdrMN832 - 1984 - Water Resources Data for Minnesota, Water Year 1983. Volume 2, Upper Mississippi and Missouri River Basins","interactions":[],"lastModifiedDate":"2012-02-02T00:11:50","indexId":"wdrMN832","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MN-83-2","title":"Water Resources Data for Minnesota, Water Year 1983. Volume 2, Upper Mississippi and Missouri River Basins","language":"ENGLISH","doi":"10.3133/wdrMN832","usgsCitation":"Gunard, K., Hess, J., Zirbel, J., and Cornelius, C., 1984, Water Resources Data for Minnesota, Water Year 1983. Volume 2, Upper Mississippi and Missouri River Basins: U.S. Geological Survey Water Data Report MN-83-2, 447 p., https://doi.org/10.3133/wdrMN832.","productDescription":"447 p.","costCenters":[],"links":[{"id":175120,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1983/mn-83-2/report-thumb.jpg"},{"id":88268,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1983/mn-83-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcddd","contributors":{"authors":[{"text":"Gunard, K.T.","contributorId":103733,"corporation":false,"usgs":true,"family":"Gunard","given":"K.T.","affiliations":[],"preferred":false,"id":257175,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hess, J.H.","contributorId":100465,"corporation":false,"usgs":true,"family":"Hess","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":257174,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zirbel, J.L.","contributorId":70837,"corporation":false,"usgs":true,"family":"Zirbel","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":257173,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cornelius, C.E.","contributorId":106190,"corporation":false,"usgs":true,"family":"Cornelius","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":257176,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":18885,"text":"ofr843 - 1984 - Analytical results for 102 water samples from sites draining the Buffalo Peaks Wilderness Study Area, Lake, Park, and Chaffee counties, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:07:25","indexId":"ofr843","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":"84-3","title":"Analytical results for 102 water samples from sites draining the Buffalo Peaks Wilderness Study Area, Lake, Park, and Chaffee counties, Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr843","usgsCitation":"Ficklin, W.H., Nowland, G., and Dover, R., 1984, Analytical results for 102 water samples from sites draining the Buffalo Peaks Wilderness Study Area, Lake, Park, and Chaffee counties, Colorado: U.S. Geological Survey Open-File Report 84-3, 11 p. :map ;28 cm., https://doi.org/10.3133/ofr843.","productDescription":"11 p. :map ;28 cm.","costCenters":[],"links":[{"id":150812,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0003/report-thumb.jpg"},{"id":48281,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0003/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48282,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0003/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acae4b07f02db67ccaf","contributors":{"authors":[{"text":"Ficklin, W. H.","contributorId":89517,"corporation":false,"usgs":true,"family":"Ficklin","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":179919,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nowland, G.A.","contributorId":67538,"corporation":false,"usgs":true,"family":"Nowland","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":179918,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dover, R.A.","contributorId":65100,"corporation":false,"usgs":true,"family":"Dover","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":179917,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":45713,"text":"pp1273D - 1984 - Apparent water resistivity, porosity, and water temperature of the Madison Limestone and underlying rocks in parts of Montana, Nebraska, North Dakota, South Dakota, and Wyoming","interactions":[{"subject":{"id":41885,"text":"ofr81629 - 1981 - Apparent water resistivity, porosity, and ground-water temperature of the Madison limestone and underlying rocks in parts of Montana, Nebraska, North Dakota, South Dakota, and Wyoming","indexId":"ofr81629","publicationYear":"1981","noYear":false,"title":"Apparent water resistivity, porosity, and ground-water temperature of the Madison limestone and underlying rocks in parts of Montana, Nebraska, North Dakota, South Dakota, and Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":45713,"text":"pp1273D - 1984 - Apparent water resistivity, porosity, and water temperature of the Madison Limestone and underlying rocks in parts of Montana, Nebraska, North Dakota, South Dakota, and Wyoming","indexId":"pp1273D","publicationYear":"1984","noYear":false,"chapter":"D","title":"Apparent water resistivity, porosity, and water temperature of the Madison Limestone and underlying rocks in parts of Montana, Nebraska, North Dakota, South Dakota, and Wyoming"},"id":1}],"lastModifiedDate":"2012-02-02T00:04:56","indexId":"pp1273D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1273","chapter":"D","title":"Apparent water resistivity, porosity, and water temperature of the Madison Limestone and underlying rocks in parts of Montana, Nebraska, North Dakota, South Dakota, and Wyoming","language":"ENGLISH","doi":"10.3133/pp1273D","usgsCitation":"MacCary, L., 1984, Apparent water resistivity, porosity, and water temperature of the Madison Limestone and underlying rocks in parts of Montana, Nebraska, North Dakota, South Dakota, and Wyoming: U.S. Geological Survey Professional Paper 1273, p. D1-D14; 20 plates in pocket, https://doi.org/10.3133/pp1273D.","productDescription":"p. D1-D14; 20 plates in pocket","costCenters":[],"links":[{"id":104590,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4784.htm","linkFileType":{"id":5,"text":"html"},"description":"4784"},{"id":120232,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1273d/report-thumb.jpg"},{"id":82276,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1273d/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82277,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1273d/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82278,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1273d/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82279,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1273d/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82280,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1273d/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82281,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1273d/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82282,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1273d/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82283,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1273d/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82284,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1273d/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82285,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1273d/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82286,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1273d/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82287,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1273d/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82288,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1273d/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82289,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1273d/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82290,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1273d/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82291,"rank":415,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1273d/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82292,"rank":416,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1273d/plate-17.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82293,"rank":417,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1273d/plate-18.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82294,"rank":418,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1273d/plate-19.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82295,"rank":419,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1273d/plate-20.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82296,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1273d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67acd0","contributors":{"authors":[{"text":"MacCary, L.M.","contributorId":13200,"corporation":false,"usgs":true,"family":"MacCary","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":231892,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11438,"text":"ofr8472 - 1984 - The concept of electron activity and its relation to redox potentials in aqueous geochemical systems","interactions":[],"lastModifiedDate":"2012-02-02T00:06:33","indexId":"ofr8472","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":"84-72","title":"The concept of electron activity and its relation to redox potentials in aqueous geochemical systems","docAbstract":"The definition of a formal thermodynamic activity of electrons in redox reactions appears in the literature of the 1920's. The concept of pe as -log (electron activity) was introduced by Jorgensen in 1945 and popularized in the geochemical literature by Sillen, who considered pe and pH as master variables in geochemical reactions. The physical significance of the concept of electron activity was challenged as early as 1928. However, only in the last two decades have sufficient thermodynamic data become available to examine this question quantitatively. The chemical nature of hydrated electrons differs greatly from that of hydrated protons, and thermodynamic data show that hydrated electrons cannot exist at physically meaningful equilibrium concentrations under natural conditions. This has important consequences for the understanding of redox processes in natural waters. These are: (1) the analogy between pe and pH as master variables is generally carried much further than is justified; (2) a thermodynamically meaningful value of redox potential cannot be assigned to disequilibrium systems; (3) the most useful approach to the study of redox characteristics is the analysis and study of multiple redox couples in the system; and (4) for all practical purposes, thermodynamically defined redox potentials do not exist (and thus cannot be measured) in natural waters. The overall implication for natural systems is that, in terms of redox reactions, each case must be considered on an individual and detailed basis. Field studies would appear to be a mandatory part of any site-specific study; conclusions regarding redox processes cannot be based solely on electrode measurements or thermodynamic stability calculations. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8472","usgsCitation":"Thorstenson, D., 1984, The concept of electron activity and its relation to redox potentials in aqueous geochemical systems: U.S. Geological Survey Open-File Report 84-72, iii, 66 p. :ill. ;28 cm., https://doi.org/10.3133/ofr8472.","productDescription":"iii, 66 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":144902,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0072/report-thumb.jpg"},{"id":39287,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0072/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6493b1","contributors":{"authors":[{"text":"Thorstenson, D.C.","contributorId":47377,"corporation":false,"usgs":true,"family":"Thorstenson","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":163141,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19604,"text":"ofr83768 - 1984 - Investigations and research in Nevada by the Water Resources Division, U.S. Geological Survey, 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:07:36","indexId":"ofr83768","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":"83-768","title":"Investigations and research in Nevada by the Water Resources Division, U.S. Geological Survey, 1982","docAbstract":"The Water Resources Division, U.S. Geological Survey, is charged with (1) maintaining a hydrologic network in Nevada that provides information on the status of the State 's water resources and (2) engaging in technical water-resources investigations that have a high degree of transferability. To meet these broad objectives, 26 projects were active during fiscal year 1982, in cooperation with 36 Federal, State, and local agencies. Total funds were $3,319,455, of which State and local cooperative funding amounted to $741,500 and Federal funding (comprised of Geological Survey Federal and cooperative program plus funds from six other Federal agencies) amounted to $2,577,955 for the fiscal year. Projects other than continuing programs for collection of hydrologic data included the following topics of study: geothermal resources, areal ground-water resources and ground-water modeling, waste disposal , paleohydrology, acid mine drainage, the unsaturated zone, stream and reservoir sedimentation, river-quality modeling, flood hazards, and remote sensing in hydrology. In total, 26 reports and symposium abstracts were published or in press during fiscal year 1982. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83768","usgsCitation":"Katzer, T., Moosburner, O., and Nichols, W.D., 1984, Investigations and research in Nevada by the Water Resources Division, U.S. Geological Survey, 1982: U.S. Geological Survey Open-File Report 83-768, v, 40 p. :ill. ;28 cm., https://doi.org/10.3133/ofr83768.","productDescription":"v, 40 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":152696,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0768/report-thumb.jpg"},{"id":49072,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0768/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6675a1","contributors":{"authors":[{"text":"Katzer, Terry","contributorId":103679,"corporation":false,"usgs":true,"family":"Katzer","given":"Terry","email":"","affiliations":[],"preferred":false,"id":181200,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moosburner, Otto","contributorId":41822,"corporation":false,"usgs":true,"family":"Moosburner","given":"Otto","email":"","affiliations":[],"preferred":false,"id":181198,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nichols, W. D.","contributorId":73220,"corporation":false,"usgs":true,"family":"Nichols","given":"W.","middleInitial":"D.","affiliations":[],"preferred":false,"id":181199,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}