{"pageNumber":"1725","pageRowStart":"43100","pageSize":"25","recordCount":68937,"records":[{"id":70017868,"text":"70017868 - 1993 - Petrology and isotopic composition of Quaternary basanites dredged from the Bering Sea continental margin near Navarin Basin","interactions":[],"lastModifiedDate":"2023-09-21T16:20:46.35207","indexId":"70017868","displayToPublicDate":"1993-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1168,"text":"Canadian Journal of Earth Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Petrology and isotopic composition of Quaternary basanites dredged from the Bering Sea continental margin near Navarin Basin","docAbstract":"<p><span>Quaternary basanites were recovered from shallow water depth from the continental margin of the Bering Sea (58°39.0′N, 177°12.9′W) near Navarin Basin. The basanites are highly vesicular flow rock and hyaloclastites similar to other alkalic volcanic rocks erupted repeatedly during the late Cenozoic on islands in the Bering Sea region and in mainland Alaska. K–Ar ages for the basanites indicate at least two episodes of volcanism at about 1.1 and 0.4 Ma. Similar alkalic volcanism occurred sporadically at geographically widely separated centers in the Bering Sea region for at least the past 6 Ma. Chemically, these alkalic lavas are intraplate basalts similar to those erupted from oceanic islands and in some continental settings. Trace-element data indicate these alkalic lavas have been generated by small, but variable, amounts of partial melting of a meta-somatized lherzolite source. The relatively primitive compositions (MgO &gt; 9%), presence of mantle-derived xenoliths in some alkalic lavas, and presence of forsteritic olivine with low CaO and high NiO suggest that magma rose rapidly from greath depth without spending time in large, long-lived magma chambers. Although lavas from different volcanic centers in the Bering Sea region are similar with respect to major elements and many trace-element ratios, isotopic compositions indicate heterogeneities in the source. The Navarin basanites have higher&nbsp;</span><sup>87</sup><span>Sr/</span><sup>86</sup><span>Sr and lower&nbsp;</span><sup>143</sup><span>Nd/</span><sup>144</sup><span>Nd values than any other lavas so far reported from this region. The&nbsp;</span><sup>207</sup><span>Pb/</span><sup>204</sup><span>Pb isotopic ratios indicate involvement of a crustal component, which may have resulted from metasomatism associated with subduction-related magmatic activity during the Early Eocene in this region. Although some volcanic episodes appear to have occurred roughly synchronously at geographically widely separated centers, no large-scale regional extension nor presence of large mantle plumes are indicated. Instead, alkalic volcanism apparently resulted from upwelling and decompressional melting of small isolated mantle diapirs in response to local lithospheric attenuation associated with jostling of blocks during adjustment to regional stresses.</span></p>","language":"English","publisher":"Canadian Science Publishing","doi":"10.1139/e93-081","issn":"00084077","usgsCitation":"Davis, A.S., Gunn, S., Gray, L., Marlow, M.S., and Wong, F.L., 1993, Petrology and isotopic composition of Quaternary basanites dredged from the Bering Sea continental margin near Navarin Basin: Canadian Journal of Earth Sciences, v. 30, no. 5, p. 975-984, https://doi.org/10.1139/e93-081.","productDescription":"10 p.","startPage":"975","endPage":"984","costCenters":[],"links":[{"id":228586,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Russia, United States","state":"Alaska","otherGeospatial":"Bering Sea, Navarin Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -161.02644563755487,\n              64.01937447302842\n            ],\n            [\n              -185.30270672550836,\n              64.01937447302842\n            ],\n            [\n              -185.30270672550836,\n              53.06258501763452\n            ],\n            [\n              -161.02644563755487,\n              53.06258501763452\n            ],\n            [\n              -161.02644563755487,\n              64.01937447302842\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"30","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7823e4b0c8380cd78649","contributors":{"authors":[{"text":"Davis, A. S.","contributorId":41424,"corporation":false,"usgs":true,"family":"Davis","given":"A.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":377796,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gunn, S.H.","contributorId":65236,"corporation":false,"usgs":true,"family":"Gunn","given":"S.H.","email":"","affiliations":[],"preferred":false,"id":377797,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gray, L.-B.","contributorId":10171,"corporation":false,"usgs":true,"family":"Gray","given":"L.-B.","email":"","affiliations":[],"preferred":false,"id":377795,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Marlow, M. S.","contributorId":76743,"corporation":false,"usgs":true,"family":"Marlow","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":377798,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wong, F. L.","contributorId":87515,"corporation":false,"usgs":true,"family":"Wong","given":"F.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":377799,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70017870,"text":"70017870 - 1993 - Dynamic behavior of Kilauea Volcano and its relation to hydrothermal systems and geothermal energy","interactions":[],"lastModifiedDate":"2012-03-12T17:19:55","indexId":"70017870","displayToPublicDate":"1993-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Dynamic behavior of Kilauea Volcano and its relation to hydrothermal systems and geothermal energy","docAbstract":"Exploitation of hydrothermal systems on active basaltic volcanoes poses some unique questions about the role of volcanism and hydrothermal system evolution. Volcanic activity creates and maintains hydrothermal systems while earthquakes create permeable fractures that, at least temporarily, enhance circulation. Magma and water, possibly hydrothermal water, can interact violently to produce explosive eruptions. Finally, we speculate on whether volcanic behavior can be affected by high rates of heat extraction.","largerWorkTitle":"Transactions - Geothermal Resources Council","conferenceTitle":"Proceedings of the 1993 Annual Meeting on Utilities and Geothermal: An Emerging Partnership","conferenceDate":"10 October 1993 through 13 October 1993","conferenceLocation":"Burlingame, CA, USA","language":"English","publisher":"Publ by Geothermal Resources Council","publisherLocation":"Davis, CA, United States","issn":"01935933","isbn":"0934412715","usgsCitation":"Kauhikaua, J., and Moore, R.B., 1993, Dynamic behavior of Kilauea Volcano and its relation to hydrothermal systems and geothermal energy, <i>in</i> Transactions - Geothermal Resources Council, v. 17, Burlingame, CA, USA, 10 October 1993 through 13 October 1993, p. 129-133.","startPage":"129","endPage":"133","numberOfPages":"5","costCenters":[],"links":[{"id":228631,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0423e4b0c8380cd507e2","contributors":{"editors":[{"text":"Anon","contributorId":128316,"corporation":true,"usgs":false,"organization":"Anon","id":536384,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Kauhikaua, Jim","contributorId":11354,"corporation":false,"usgs":true,"family":"Kauhikaua","given":"Jim","email":"","affiliations":[],"preferred":false,"id":377803,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, R. B.","contributorId":98720,"corporation":false,"usgs":true,"family":"Moore","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":377804,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70017878,"text":"70017878 - 1993 - Bridge-scour analysis using the water surface profile (WSPRO) model","interactions":[],"lastModifiedDate":"2012-03-12T17:19:55","indexId":"70017878","displayToPublicDate":"1993-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Bridge-scour analysis using the water surface profile (WSPRO) model","docAbstract":"A program was developed to extract hydraulic information required for bridge-scour computations, from the Water-Surface Profile computation model (WSPRO). The program is written in compiled BASIC and is menu driven. Using only ground points, the program can compute average ground elevation, cross-sectional area below a specified datum, or create a Drawing Exchange Format (DXF) fie of cross section. Using both ground points ad hydraulic information form the equal-conveyance tubes computed by WSPRO, the program can compute hydraulic parameters at a user-specified station or in a user-specified subsection of the cross section. The program can identify the maximum velocity in a cross section and the velocity and depth at a user-specified station. The program also can identify the maximum velocity in the cross section and the average velocity, average depth, average ground elevation, width perpendicular to the flow, cross-sectional area of flow, and discharge in a subsection of the cross section. This program does not include any help or suggestions as to what data should be extracted; therefore, the used must understand the scour equations and associated variables to the able to extract the proper information from the WSPRO output.","largerWorkTitle":"Proceedings - National Conference on Hydraulic Engineering","conferenceTitle":"Proceedings of the National Conference on Hydraulic Engineering","conferenceDate":"25 July 1993 through 30 July 1993","conferenceLocation":"San Francisco, CA, USA","language":"English","publisher":"Publ by ASCE","publisherLocation":"New York, NY, United States","isbn":"0872629201","usgsCitation":"Mueller, D.S., 1993, Bridge-scour analysis using the water surface profile (WSPRO) model, <i>in</i> Proceedings - National Conference on Hydraulic Engineering, no. pt 2, San Francisco, CA, USA, 25 July 1993 through 30 July 1993, p. 1714-1719.","startPage":"1714","endPage":"1719","numberOfPages":"6","costCenters":[],"links":[{"id":228729,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"pt 2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f27ae4b0c8380cd4b1cf","contributors":{"editors":[{"text":"Shen Hsieh WenSu S.T.Wen Feng","contributorId":128306,"corporation":true,"usgs":false,"organization":"Shen Hsieh WenSu S.T.Wen Feng","id":536385,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Mueller, David S. dmueller@usgs.gov","contributorId":1499,"corporation":false,"usgs":true,"family":"Mueller","given":"David","email":"dmueller@usgs.gov","middleInitial":"S.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":true,"id":377821,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70017895,"text":"70017895 - 1993 - Late Quaternary paleoceanography of the Pervenets Canyon area of the Bering Sea: Evidence from the diatom flora","interactions":[],"lastModifiedDate":"2023-09-26T16:11:49.844985","indexId":"70017895","displayToPublicDate":"1993-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1388,"text":"Diatom Research","active":true,"publicationSubtype":{"id":10}},"title":"Late Quaternary paleoceanography of the Pervenets Canyon area of the Bering Sea: Evidence from the diatom flora","docAbstract":"<p><span>Sediments from three gravity cores from an east-west shelf-to-slope transect along the axis of Pervenets Canyon in the northern Navarin basin, Bering Sea were analyzed for diatoms. The diatom floras present in the cores were divided into four assemblages following Sancetta (1981). The Bering Basin (deep water open ocean) and Sea Ice (ice cover at least six months per year) Assemblages were dominant in each core. The taxa that comprise the Bering Shelf Assemblage (continental shelf) indicate that downslope transport plays only a minor part in the development of the thanatocenoses. The presence (up to 10% of the total valve count) of the Productivity Assemblage, which consists mainly of poorly silicified, easily dissolved taxa, indicates that nutrient flux is relatively high in the region. Several taxa can be used as proxy indicators for specific water masses.&nbsp;</span><i>Neodenticula seminae</i><span>&nbsp;(Simonsen &amp; Kanaya) Akiba &amp; Yanagisawa is indicative of Holocene open marine (deep water) conditions.&nbsp;</span><i>Nitzschia cylindra</i><span>&nbsp;(Grunow) Hasle and&nbsp;</span><i>N. grunowii</i><span>&nbsp;Hasle are both associated with sea ice and are thought to indicate late Pleistocene conditions. The relative downcore abundance of these taxa was used to approximate the Pleistocene- Holocene boundary (recognized in Core 80–65 at a depth of about 75 cm).</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/0269249X.1993.9705247","usgsCitation":"Starratt, S.W., 1993, Late Quaternary paleoceanography of the Pervenets Canyon area of the Bering Sea: Evidence from the diatom flora: Diatom Research, v. 8, no. 1, p. 159-170, https://doi.org/10.1080/0269249X.1993.9705247.","productDescription":"12 p.","startPage":"159","endPage":"170","numberOfPages":"12","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":228955,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4531e4b0c8380cd670ed","contributors":{"authors":[{"text":"Starratt, Scott W. 0000-0001-9405-1746 sstarrat@usgs.gov","orcid":"https://orcid.org/0000-0001-9405-1746","contributorId":2891,"corporation":false,"usgs":true,"family":"Starratt","given":"Scott","email":"sstarrat@usgs.gov","middleInitial":"W.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":377857,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70017901,"text":"70017901 - 1993 - Application of headspace analysis to the study of sorption of hydrophobic organic chemicals to  α-Al<sub>2</sub>O<sub>3</sub>","interactions":[],"lastModifiedDate":"2015-05-25T11:23:22","indexId":"70017901","displayToPublicDate":"1993-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Application of headspace analysis to the study of sorption of hydrophobic organic chemicals to  α-Al<sub>2</sub>O<sub>3</sub>","docAbstract":"<p>The sorption of hydrophobic organic chemicals (HOCs) to ??-Al2O3 was investigated with a headspace analysis method. The semiautomated headspace analyzer gave rapid, precise, and accurate results for a homologous series alkylbenzenes even at low percentages of solute mass sorbed (3-50%). Sorption experiments carried out with benzene alone indicated weak interactions with well-characterized aluminum oxide, and a solids concentration effect was observed. When the sorption coefficients for benzene alone obtained by headspace analysis were extrapolated up to the solids concentrations typically used in batch sorption experiments, the measured sorption coefficients agreed with reported sorption coefficients for HOCs and sediments of low fractional organic carbon content. Sorbed concentrations increased exponentially with aqueous concentration in isotherms with mixtures of alkylbenzenes, indicating solute-solute interactions at the mineral surface. Sorption was, however, greater than predicted for partitioning of a solute between its pure liquid phase and water, indicating additional influences of the surface and/or the structured liquid near the mineral surface. ?? 1993 American Chemical Society.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/es00042a016","issn":"0013936X","usgsCitation":"Pelinger, J.A., Eisenreich, S.J., and Capel, P.D., 1993, Application of headspace analysis to the study of sorption of hydrophobic organic chemicals to  α-Al<sub>2</sub>O<sub>3</sub>: Environmental Science & Technology, v. 27, no. 5, p. 928-937, https://doi.org/10.1021/es00042a016.","productDescription":"10 p.","startPage":"928","endPage":"937","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":229046,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"5","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059eca3e4b0c8380cd493cd","contributors":{"authors":[{"text":"Pelinger, Judith A.","contributorId":69738,"corporation":false,"usgs":true,"family":"Pelinger","given":"Judith","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":377878,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eisenreich, Steven J.","contributorId":66001,"corporation":false,"usgs":false,"family":"Eisenreich","given":"Steven","email":"","middleInitial":"J.","affiliations":[{"id":6626,"text":"University of Minnesota","active":true,"usgs":false}],"preferred":false,"id":377877,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Capel, Paul D. 0000-0003-1620-5185 capel@usgs.gov","orcid":"https://orcid.org/0000-0003-1620-5185","contributorId":1002,"corporation":false,"usgs":true,"family":"Capel","given":"Paul","email":"capel@usgs.gov","middleInitial":"D.","affiliations":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"preferred":true,"id":377879,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70018399,"text":"70018399 - 1993 - Gas buildup in Lake Nyos, Cameroon: The recharge process and its consequences","interactions":[],"lastModifiedDate":"2023-02-14T12:22:37.076498","indexId":"70018399","displayToPublicDate":"1993-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":835,"text":"Applied Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Gas buildup in Lake Nyos, Cameroon: The recharge process and its consequences","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-gulliver text-s\"><div id=\"ab1\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id11\"><p>The gases dissolved in Lake Nyos, Cameroon, were quantified recently (December 1989 and September 1990) by two independent techniques:<span>&nbsp;</span><i>in-situ</i><span>&nbsp;</span>measurements using a newly designed probe and laboratory analyses of samples collected in pre-evacuated stainless steel cylinders. The highest concentrations of CO<sub>2</sub><span>&nbsp;</span>and CH<sub>4</sub><span>&nbsp;</span>were 0.30 mol/kg and 1.7 mmol/kg, respectively, measured in cylinders collected 1 m above lake bottom. Probe measurements of<span>&nbsp;</span><i>in-situ</i><span>&nbsp;</span>gas pressure at three different stations showed that horizontal variations in total dissolved gas were negligible. Total dissolved-gas pressure near the lake bottom is 1.06 MPa (10.5 atm), 50% as high as the hydrostatic pressure of 2.1 MPa (21 atm). Comparing the CO<sub>2</sub><span>&nbsp;</span>profile constructed from the 1990 data to one obtained in May 1987 shows that CO<sub>2</sub><span>&nbsp;</span>concentrations have increased at depths to below 150 m. Based on these profiles, the average rate of CO<sub>2</sub><span>&nbsp;</span>input to bottom waters was 2.6 × 10<sup>8</sup><span>&nbsp;</span>mol/a. Increased deep-water temperatures require an average heat flow of 0.32 MW into the hypolimnion over the same time period. The transport rates of CO<sub>2</sub>, heat, and major ions into the hypolimnion suggest that a low-temperature reservoir of free CO<sub>2</sub><span>&nbsp;</span>exists a short distance below lake bottom and that convective cycling of lake water through the sediments is involved in transporting the CO<sub>2</sub><span>&nbsp;</span>into the lake from the underlying diatreme. Increased CH<sub>4</sub><span>&nbsp;</span>concentrations at all depths below the oxycline and a high<sup>14</sup>C content (41% modern) in the CH<sub>4</sub><span>&nbsp;</span>4 m above lake bottom show that much of the CH<sub>4</sub><span>&nbsp;</span>is biologically produced within the lake. The CH<sub>4</sub><span>&nbsp;</span>production rate may vary with time, but if the CO<sub>2</sub><span>&nbsp;</span>recharge rate remains constant, CO<sub>2</sub><span>&nbsp;</span>saturation of the entire hypolimnion below 50 m depth would require ∼140a, given present-day concentrations.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0883-2927(93)90036-G","issn":"08832927","usgsCitation":"Evans, W.C., Kling, G., Tuttle, M.L., Tanyileke, G., and White, L.D., 1993, Gas buildup in Lake Nyos, Cameroon: The recharge process and its consequences: Applied Geochemistry, v. 8, no. 3, p. 207-221, https://doi.org/10.1016/0883-2927(93)90036-G.","productDescription":"15 p.","startPage":"207","endPage":"221","numberOfPages":"15","costCenters":[],"links":[{"id":480335,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/2027.42/30812>","text":"External Repository"},{"id":227510,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Cameroon","otherGeospatial":"Lake Nyos","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              10.28576250671452,\n              6.448942928703474\n            ],\n            [\n              10.28576250671452,\n              6.423707894002149\n            ],\n            [\n              10.31218713674616,\n              6.423707894002149\n            ],\n            [\n              10.31218713674616,\n              6.448942928703474\n            ],\n            [\n              10.28576250671452,\n              6.448942928703474\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"8","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a14c1e4b0c8380cd54b52","contributors":{"authors":[{"text":"Evans, William C.","contributorId":104903,"corporation":false,"usgs":true,"family":"Evans","given":"William","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":379439,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kling, G.W.","contributorId":22368,"corporation":false,"usgs":true,"family":"Kling","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":379436,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tuttle, M. L.","contributorId":71992,"corporation":false,"usgs":true,"family":"Tuttle","given":"M.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":379438,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tanyileke, G.","contributorId":35882,"corporation":false,"usgs":true,"family":"Tanyileke","given":"G.","email":"","affiliations":[],"preferred":false,"id":379437,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"White, L. D.","contributorId":14330,"corporation":false,"usgs":true,"family":"White","given":"L.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":379435,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70017496,"text":"70017496 - 1993 - Crude oil in a shallow sand and gravel aquifer—I. Hydrogeology and inorganic geochemistry","interactions":[],"lastModifiedDate":"2019-03-06T06:48:45","indexId":"70017496","displayToPublicDate":"1993-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":835,"text":"Applied Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Crude oil in a shallow sand and gravel aquifer—I. Hydrogeology and inorganic geochemistry","docAbstract":"<div>Changes in the distribution of inorganic solutes in a shallow ground water contaminated by crude oil document a series of geochemical reactions initiated by biodegradation of the oil. Upgradient of an oil body floating on the water table, oxidation of oil to carbonic acid dissolves carbonate minerals in the aquifer matrix. In this oxidized zone pH is depressed &sim;1 pH unit, and the concentrations of Ca, Mg and HCO<sub><span>3</span></sub><span>&minus;</span>&nbsp;increase to more than twice that of the native ground water. In the anoxic zone beneath the oil body concentrations of dissolved SiO<sub><span>2</span></sub>, Sr, K, Fe and Mn increase significantly. Here, Fe is mobilized by microbial reduction, pH is buffered by the carbonate system, and silicates weather via hydrolysis and organic-acid-enhanced dissolution. Farther down-gradient the ground water is reoxygenated and Fe precipitates from solution, possibly as iron hydroxide or iron carbonates, while SiO<span><sub>2</sub>&nbsp;</span>precipitates as amorphous silica. Other solutes, such as Mg, are transported more conservatively down-gradient where contaminated and native ground water mix.</div>\n<div>The observed changes in inorganic aqueous chemistry document changes in water-mineral interactions caused by the presence of an organic contaminant. These organic-initiated interactions are likely present in many contaminated aquifers and may be analogous to interactions occurring in other organic-rich natural waters.</div>","language":"English","publisher":"Elsevier","doi":"10.1016/0883-2927(93)90012-6","issn":"08832927","usgsCitation":"Bennett, P., Siegel, D., Baedecker, M., and Hult, M.F., 1993, Crude oil in a shallow sand and gravel aquifer—I. Hydrogeology and inorganic geochemistry: Applied Geochemistry, v. 8, no. 6, p. 529-549, https://doi.org/10.1016/0883-2927(93)90012-6.","productDescription":"21 p.","startPage":"529","endPage":"549","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":228326,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"Bagley Outwash plain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.11688232421875,\n              47.522765270504436\n            ],\n            [\n              -95.11688232421875,\n              47.56610235225701\n            ],\n            [\n              -95.02590179443358,\n              47.56610235225701\n            ],\n            [\n              -95.02590179443358,\n              47.522765270504436\n            ],\n            [\n              -95.11688232421875,\n              47.522765270504436\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"8","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fccae4b0c8380cd4e435","contributors":{"authors":[{"text":"Bennett, P.C.","contributorId":24357,"corporation":false,"usgs":true,"family":"Bennett","given":"P.C.","email":"","affiliations":[],"preferred":false,"id":376655,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Siegel, D.E.","contributorId":107983,"corporation":false,"usgs":true,"family":"Siegel","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":376658,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baedecker, M.J.","contributorId":42702,"corporation":false,"usgs":true,"family":"Baedecker","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":376657,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hult, M. F.","contributorId":29817,"corporation":false,"usgs":true,"family":"Hult","given":"M.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":376656,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1008467,"text":"1008467 - 1993 - Population structure, body mass, activity, and orientation of an aquatic snake (<i>Seminatrix pygaea</i>) during a drought","interactions":[],"lastModifiedDate":"2016-01-12T13:06:39","indexId":"1008467","displayToPublicDate":"1993-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1176,"text":"Canadian Journal of Zoology","active":true,"publicationSubtype":{"id":10}},"title":"Population structure, body mass, activity, and orientation of an aquatic snake (<i>Seminatrix pygaea</i>) during a drought","docAbstract":"<p><span>The snout &ndash; vent length, tail length, weight, sex, activity, and orientation of a population of swamp snakes (</span><i>Seminatrix pygaea</i><span>) in north &ndash; central Florida were recorded from 1985 through 1990. A small temporary pond was monitored for 1343 days, using a drift fence &ndash; pitfall trap sampling regime. I captured 123 different snakes, plus 45 recaptures. Juveniles comprised 89% of the snakes at the pond. Females were generally longer and weighed more than males, although regression analysis showed no differences between the sexes in the relationship of length versus wet body mass. Males had longer tails than females. The sex ratio of snakes with a snout &ndash; vent length of more than 150&ensp;mm was 1:1. Activity occurred throughout the year but peaked during summer. Hydroperiod and weather conditions did not appear to influence snake activity. During the latter years of the study, a regional drought that began in the mid-1980s became quite severe. However, drought had little direct effect on overland migration or body condition but caused snakes to leave or to shorten the amount of time they spent within the pond basin. Snakes immigrated and emigrated nonrandomly; orientation was directed to and from the nearest large water body. Certain temporary ponds may comprise developmental habitat for&nbsp;</span><i>Seminatrix pygaea</i><span>. The dynamic wet &ndash; dry climatic cycles in southeastern North America may lead to the formation of metapopulations in some aquatic snakes.</span></p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/z93-177","usgsCitation":"Dodd, C., 1993, Population structure, body mass, activity, and orientation of an aquatic snake (<i>Seminatrix pygaea</i>) during a drought: Canadian Journal of Zoology, v. 71, no. 7, p. 1281-1288, https://doi.org/10.1139/z93-177.","productDescription":"8 p.","startPage":"1281","endPage":"1288","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":275,"text":"Florida Integrated Science Center","active":false,"usgs":true}],"links":[{"id":131017,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"71","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db683de2","contributors":{"authors":[{"text":"Dodd, C.K. Jr.","contributorId":86286,"corporation":false,"usgs":true,"family":"Dodd","given":"C.K.","suffix":"Jr.","affiliations":[],"preferred":false,"id":317873,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1001141,"text":"1001141 - 1993 - Least tern and piping plover nesting at sand pits in Nebraska","interactions":[],"lastModifiedDate":"2012-02-02T00:04:44","indexId":"1001141","displayToPublicDate":"1993-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1272,"text":"Colonial Waterbirds","printIssn":"07386028","active":false,"publicationSubtype":{"id":10}},"title":"Least tern and piping plover nesting at sand pits in Nebraska","docAbstract":"Endangered Least Terns (Sterna antillarum) and threatened Piping Plovers (Charadrius melodus) nest at commercial sand and gravel mining operations (sand pits) along the Platte River system in Nebraska. Sandbar habitat has been disappearing since the early 1900's along the Platte River system, but numbers of sand pits have increased. We hypothesized that birds would more fully utilize sand pits where suitable sandbar habitat was limited. We inventoried sand pits and censused terns and plovers on both habitats along the Loup River, part of the North Loup River, and most of the Platte River during 1988-1991. Using aircraft, we also quantified features of suitable sand pits present on the central Platte in 1988 and lower Platte in 1990, and related features to abundance and presence of birds. We found 225 sand pits of which 78 were suitable and 187 were unsuitable for nesting. Along the central Platte, where sandbar habitat is severely degraded, birds nested at 81% of the suitable sand pits (N = 32) at least once during 1988-1991, and most birds (61-94%) nested on sand pits. Along the lower Platte, where both sandbar and sand pit habitat are plentiful, birds nested at 60% of the suitable sand pits (N = 35) at least once during 1988-1991, and most birds (60-86%) nested on sandbars. Numbers of terns and plovers were more weakly correlated with features of sand pits on the central Platte than on the lower Platte. Least Terns and Piping Plovers seem to use more of the suitable sand pit habitat on the central Platte than on the lower Platte. Sand pits probably have influenced the birds' distribution by providing alternative nesting habitat along rivers where suitable sandbars are rare or absent.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Colonial Waterbirds","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Sidle, J.G., and Kirsch, E., 1993, Least tern and piping plover nesting at sand pits in Nebraska: Colonial Waterbirds, v. 16, no. 2, p. 139-148.","productDescription":"p. 139-148","startPage":"139","endPage":"148","numberOfPages":"9","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":133715,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adfd7","contributors":{"authors":[{"text":"Sidle, John G.","contributorId":77099,"corporation":false,"usgs":true,"family":"Sidle","given":"John","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":310576,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kirsch, E.M.","contributorId":87486,"corporation":false,"usgs":true,"family":"Kirsch","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":310577,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1001191,"text":"1001191 - 1993 - Duck nest success on Conservation Reserve Program land in the prairie pothole region","interactions":[],"lastModifiedDate":"2017-12-29T12:45:04","indexId":"1001191","displayToPublicDate":"1993-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2456,"text":"Journal of Soil and Water Conservation","active":true,"publicationSubtype":{"id":10}},"title":"Duck nest success on Conservation Reserve Program land in the prairie pothole region","docAbstract":"<p><span>Habitat fragmentation from intensified farming has concentrated nesting waterfowl and their predators in the remaining, relatively small untitled habitats of the prairie pothole region in the United States. The areas of land that have been enrolled in the Conservation Reserve Program (CRP) in this area could help disperse these concentrations and reduce losses to predators. The presence of CRP land may influence decisions about intensive management of public lands devoted to waterfowl production. During 1989–1991, waterfowl nest success on CRP fields in areas of high wetland density in the prairie pothole region was 23.1 percent compared to 8.2 percent on similar covers on federal waterfowl production areas. CRP fields thus provided more secure nesting cover for upland-nesting ducks than waterfowl production areas. However, nest success and use of the fields by ducks varied greatly. CRP fields are abundant and of a wide variety of age classes and sizes. These characteristics make CRP fields well suited as study sites for determining the effects of cover area, distance to water, and cover age on nest success of ducks.</span></p>","language":"English","publisher":"Soil and Water Conservation Society","usgsCitation":"Kantrud, H., 1993, Duck nest success on Conservation Reserve Program land in the prairie pothole region: Journal of Soil and Water Conservation, v. 48, no. 3, p. 238-242.","productDescription":"5 p.","startPage":"238","endPage":"242","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":130618,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":11012,"rank":200,"type":{"id":15,"text":"Index Page"},"url":"https://www.jswconline.org/content/48/3/238.abstract"}],"volume":"48","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5ee4b07f02db633c28","contributors":{"authors":[{"text":"Kantrud, H.A.","contributorId":28553,"corporation":false,"usgs":true,"family":"Kantrud","given":"H.A.","email":"","affiliations":[],"preferred":false,"id":310693,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27778,"text":"wri914135 - 1992 - Effects of dried wastewater-treatment sludge application on ground-water quality in South Dade County, Florida","interactions":[],"lastModifiedDate":"2021-10-13T14:57:32.301863","indexId":"wri914135","displayToPublicDate":"2021-10-13T11:00:00","publicationYear":"1992","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":"91-4135","title":"Effects of dried wastewater-treatment sludge application on ground-water quality in South Dade County, Florida","docAbstract":"<p>Four test fields in the south Dade agricultural area were studied to determine the effects of sludge application on ground-water quality. Two fields had been cultivated for 10 years or more, and two had not been farmed for at least 10 years. The fields were representative of the area's two soil types (Rockdale and Perrine marl) and two major crop types (row crops and groves). Before the application of sludge, wells upgradient of, within, and downgradient of each field were sampled for possible sludge contaminants at the end of wet and dry seasons. Municipal wastewater treatment sludge from the Dade County Water and Sewe Authority Department was then applied to the fields at varying application rates. The wells at each field were sampled over a 2-year period under different hydrologic conditions for possible sludge-related constituents (specific conductance, pH, alkalinity, nitrogen, phosphorus, total organic carbon, copper, iron, magnesium, manganese, potassium, zinc, arsenic, cadmium, chloride, chromium, lead, mercury, nickel, and sodium). Comparisons were made between water quality in the vicinity of the test fields and Florida Department of Environmental Regulation primary and secondary drinking-water regulations, an between water quality upgradient of, beneath, and downgradient of the fields. Comparisons between presludge and postsludge water quality did not indicate any improvement because of retention of agrichemicals by the sludge nor did they indicate any deterioration because of leaching from the sludge. Comparisons of water quality upgradient of the fields to water quality beneath and downgradient of the fields also did not indicate any changes related to sludge. Florida Department of Environmental Regulation primary and secondary drinking-water regulations wer exceeded at the Rockdale maximum-application field by mercury (9.5 ug/L (micrograms per liter)), and the Perrine marl maximum-application field by manganese (60 ug/L) and lead (85 ug/L), and at the Perrine marl row-crop field by mercury (5.2 ug/L). All other exceedances were either in presludge or upgradient samples, or they were for constituents or properties, such as iron and color, which typically exceed standards in native ground water. Acid-extractable and base-neutral compounds, volatile organic compounds, chlorophenoxy herbicides, organophosphorus insecticides, and organochlorine compounds were analyzed for one shallow well at each field twice annually. Those compounds that equaled or exceeded the detection limit after sludge was applied included benzene (0.3 and 1.2 ug/L), chloroform (0.2 and 0.3 ug/L), bis(2-Ethylhexyl)phthalate (29 and 42 ug/L), methylene chloride (14 ug/L), tolulene (0.2, 0.4, 0.5, 1.3, and 4.4 ug/L), 1, 1,1-trichloroethana (0.6 ug/L), trichloroethylene (0.3 ug/L), 2.4-D (0.01 ug/L), and xylene (0.3 ug/L). It ws not possible to ascertain the origin of these compounds because they are available from sources other than sludge.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri914135","collaboration":"Prepared in cooperation with the South Dade Soil and Water Conservation District, Florida Department of Environmental Regulation, and the Dade County Water and Sewer Authority Department","usgsCitation":"Howie, B., 1992, Effects of dried wastewater-treatment sludge application on ground-water quality in South Dade County, Florida: U.S. Geological Survey Water-Resources Investigations Report 91-4135, v, 48 p., https://doi.org/10.3133/wri914135.","productDescription":"v, 48 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":124925,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4135/report-thumb.jpg"},{"id":56621,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4135/wri914135.pdf","text":"Report","size":"5.86 MB","linkFileType":{"id":1,"text":"pdf"}}],"contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2fe4b07f02db615cbb","contributors":{"authors":[{"text":"Howie, Barbara","contributorId":54248,"corporation":false,"usgs":true,"family":"Howie","given":"Barbara","email":"","affiliations":[],"preferred":false,"id":198674,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28739,"text":"wri914175 - 1992 - Hydrogeology and Migration of Septic-Tank Effluent in the Surficial Aquifer System in the Northern Midlands Area, Palm Beach County, Florida","interactions":[],"lastModifiedDate":"2021-10-13T14:56:41.022893","indexId":"wri914175","displayToPublicDate":"2021-10-13T11:00:00","publicationYear":"1992","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":"91-4175","displayTitle":"Hydrogeology and Migration of Septic-Tank Effluent in the Surficial Aquifer System in the Northern Midlands Area, Palm Beach County, Florida","title":"Hydrogeology and Migration of Septic-Tank Effluent in the Surficial Aquifer System in the Northern Midlands Area, Palm Beach County, Florida","docAbstract":"The northern Midlands area in Palm Beach County is an area of expected residential growth, but its flat topography, poor drainage, and near-surface marl layers retard rainfall infiltration and cause frequent flooding. Public water supplies and sewer services are not planned for the area, thus, residents must rely on domestic wells and septic tanks. The water table in the northern Midlands area is seldom more than 5 feet below land surface, and regional ground-water flows are east, southwest, and south from the north-central part of the area where ground-water levels are highest. Ground-water quality in the western part of the area and in the Loxahatchee Slough is greatly influenced by residual seawater emplaced during the Pleistocene Epoch. Chloride and dissolved-solids concentrations of ground water in the surficial aquifer system in these areas often exceed secondary drinking-water standards. Residual seawater has been more effectively flushed from the more permeable sediments elsewhere in the eastern and southwestern parts of the study area. Test at three septic-tank sites showed traces of effluent in ground water (38-92 feet from the septic tank outlets) and that near-surface marl layers greatly impede the downward migration of the effluent in the surficial aquifer system throughout the northern midlands.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri914175","collaboration":"Prepared in cooperation with Palm Beach County","usgsCitation":"Miller, W.L., 1992, Hydrogeology and Migration of Septic-Tank Effluent in the Surficial Aquifer System in the Northern Midlands Area, Palm Beach County, Florida: U.S. Geological Survey Water-Resources Investigations Report 91-4175, v, 69 p., https://doi.org/10.3133/wri914175.","productDescription":"v, 69 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":57591,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4175/wri914175.pdf","text":"Report","size":"7.40 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":124924,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4175/report-thumb.jpg"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.41666666666667,26.666666666666668 ], [ -80.41666666666667,27 ], [ -80,27 ], [ -80,26.666666666666668 ], [ -80.41666666666667,26.666666666666668 ] ] ] } } ] }","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db62786e","contributors":{"authors":[{"text":"Miller, Wesley L.","contributorId":91859,"corporation":false,"usgs":true,"family":"Miller","given":"Wesley","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":200318,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30038,"text":"wri914200 - 1992 - Effects of horizontal velocity variations on ultrasonic velocity measurements in open channels","interactions":[],"lastModifiedDate":"2021-10-14T12:05:42.329754","indexId":"wri914200","displayToPublicDate":"2021-10-13T11:00:00","publicationYear":"1992","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":"91-4200","displayTitle":"Effects of Horizontal Velocity Variations on Ultrasonic Velocity Measurements in Open Channels","title":"Effects of horizontal velocity variations on ultrasonic velocity measurements in open channels","docAbstract":"Use of an ultrasonic velocity meter to determine discharge in open channels involves measuring the velocity in a line between transducers in the stream and relating that velocity to the average velocity in the stream. The standard method of calculating average velocity in the channel assumes that the velocity profile in the channel can be represented by the one-dimensional von Karman universal velocity profile. However, the velocity profile can be described by a two-dimensional equation that accounts for the horizontal velocity variations induced by the channel sides.\r\n\r\nAn equation to calculate average velocity accounts for the two-dimensional variations in velocity within a stream. The use of this new equation to calculate average velocity was compared to the standard method in theoretical trapezoidal cross sections and in the L-31N and Snapper Creek Extension Canals near Miami, Florida. These comparisons indicate that the two-dimensional variations have the most significant effect in narrow, deep channels. Also, the two-dimensional effects may be significant in some field situations and need to be considered when determining average velocity and discharge with an ultrasonic velocity meter.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri914200","usgsCitation":"Swain, E., 1992, Effects of horizontal velocity variations on ultrasonic velocity measurements in open channels: U.S. Geological Survey Water-Resources Investigations Report 91-4200, v, 15 p., https://doi.org/10.3133/wri914200.","productDescription":"v, 15 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":58841,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4200/report.pdf","text":"Report","size":"2.09 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":122633,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4200/report-thumb.jpg"}],"contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611ea9","contributors":{"authors":[{"text":"Swain, E.D. 0000-0001-7168-708X","orcid":"https://orcid.org/0000-0001-7168-708X","contributorId":29007,"corporation":false,"usgs":true,"family":"Swain","given":"E.D.","affiliations":[],"preferred":false,"id":202576,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":54660,"text":"wdrMDDE922 - 1992 - Water resources data Maryland and Delaware, water year 1992, Volume 2: Ground-water data","interactions":[],"lastModifiedDate":"2021-01-22T19:41:14.391145","indexId":"wdrMDDE922","displayToPublicDate":"2021-01-22T14:50:00","publicationYear":"1992","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":"MD-DE-92-2","displayTitle":"Water Resources Data Maryland and Delaware, Water Year 1992, Volume 2. Ground-Water Data","title":"Water resources data Maryland and Delaware, water year 1992, Volume 2: Ground-water data","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMDDE922","usgsCitation":"James, R., and Smigaj, M., 1992, Water resources data Maryland and Delaware, water year 1992, Volume 2: Ground-water data: U.S. Geological Survey Water Data Report MD-DE-92-2, 585 p., https://doi.org/10.3133/wdrMDDE922.","productDescription":"585 p.","costCenters":[{"id":41514,"text":"Maryland-Delaware-District of Columbia  Water Science Center","active":true,"usgs":true}],"links":[{"id":381981,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1992/md-de-92-2/wdrMDDE922.pdf","text":"Report","size":"21.8 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Water Data Report 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,{"id":54659,"text":"wdrMDDE921 - 1992 - Water resources data Maryland and Delaware, water year 1992, Volume 1. Surface-water data","interactions":[],"lastModifiedDate":"2021-01-22T19:40:46.994517","indexId":"wdrMDDE921","displayToPublicDate":"2021-01-22T14:50:00","publicationYear":"1992","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":"MD-DE-92-1","displayTitle":"Water Resources Data Maryland and Delaware, Water Year 1992, Volume 1. Surface-Water Data","title":"Water resources data Maryland and Delaware, water year 1992, Volume 1. Surface-water data","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMDDE921","usgsCitation":"James, R., Simmons, R., Strain, B., and Hornlein, J., 1992, Water resources data Maryland and Delaware, water year 1992, Volume 1. 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 \"}}]}","contact":"<p><a href=\"https://pubs.er.usgs.gov/contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb70f","contributors":{"authors":[{"text":"James, R.W.","contributorId":70434,"corporation":false,"usgs":true,"family":"James","given":"R.W.","affiliations":[],"preferred":false,"id":251069,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simmons, R.H.","contributorId":19982,"corporation":false,"usgs":true,"family":"Simmons","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":251068,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Strain, B.F.","contributorId":76388,"corporation":false,"usgs":true,"family":"Strain","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":251070,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hornlein, J.F.","contributorId":102554,"corporation":false,"usgs":true,"family":"Hornlein","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":251071,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70208304,"text":"70208304 - 1992 - Food preferences of spring-migrating blue-winged teal in southwestern Louisiana","interactions":[],"lastModifiedDate":"2020-02-04T18:19:57","indexId":"70208304","displayToPublicDate":"2020-02-03T12:58:20","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3139,"text":"Proceedings of the Annual Conference of the Southeastern Association of Fish and Wildlife Agencies","active":true,"publicationSubtype":{"id":10}},"title":"Food preferences of spring-migrating blue-winged teal in southwestern Louisiana","docAbstract":"<p><span>We studied effects of pair status, molt intensity, and year on food selection by migrating male blue-winged teal (Anas discors) in southwestern Louisiana during springs 1990 and 1991. Diets consisted primarily of animal foods; but plant material, consisting mostly of seeds, comprised as much as 44%. There was no difference in animal food consumption by paired and unpaired males; however, the proportion of animal material in the male diet was greater in 1990 than in 1991. Animal food consumption was not positively correlated with mean molt intensity. Food preferences of paired and unpaired males were similar in both years. Animal foods, especially benthos and organisms associated with vegetative substrates, were preferred to seeds and freeswimming invertebrates. We recommend that habitat management for spring-migrating blue-winged teal focus on production of invertebrates, especially long-lived forms such as dragonflies, hemipterans (except water boatmen), midges, and other dipterans.</span></p>","language":"English","publisher":"SEAFWA","usgsCitation":"Manley, S.W., Hohman, W., Moore, J., and Richard, D., 1992, Food preferences of spring-migrating blue-winged teal in southwestern Louisiana: Proceedings of the Annual Conference of the Southeastern Association of Fish and Wildlife Agencies, p. 46-56.","productDescription":"11 p.","startPage":"46","endPage":"56","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":371990,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":371962,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.seafwa.org/publications/proceedings/?id=25072"}],"country":"United States","state":"Louisiana ","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.6474609375,\n              29.430029404571762\n            ],\n            [\n              -91.7138671875,\n              29.430029404571762\n            ],\n            [\n              -91.7138671875,\n              31.22219703210317\n            ],\n            [\n              -93.6474609375,\n              31.22219703210317\n            ],\n            [\n              -93.6474609375,\n              29.430029404571762\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Manley, Scott W.","contributorId":111335,"corporation":false,"usgs":true,"family":"Manley","given":"Scott","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":781330,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hohman, W.L.","contributorId":82638,"corporation":false,"usgs":true,"family":"Hohman","given":"W.L.","affiliations":[],"preferred":false,"id":781331,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moore, J.L.","contributorId":29100,"corporation":false,"usgs":true,"family":"Moore","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":781332,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Richard, David","contributorId":222208,"corporation":false,"usgs":false,"family":"Richard","given":"David","affiliations":[],"preferred":false,"id":781503,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70211062,"text":"70211062 - 1992 - A theoretical model for the flux of radon from rock to ground water","interactions":[],"lastModifiedDate":"2020-07-14T14:53:48.388553","indexId":"70211062","displayToPublicDate":"2020-01-01T09:51:36","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1727,"text":"GSA Special Papers","active":true,"publicationSubtype":{"id":10}},"title":"A theoretical model for the flux of radon from rock to ground water","docAbstract":"<p>A model is derived to predict the abundance of <sup>222</sup>Rn in ground water in contact with a rock of known uranium content. The model assumes that secular equilibrium is attained in the rock-water system as a whole, but is independent of any microscopic geometric properties of the system. The key variables in the model are bulk properties such as porosity, uranium content of the rock, emanating efficiency, and rock density, all of which are measurable. Thus, the model is simplified by the averaging effects of a macroscopic view of the system. Although less rigorous than other models presented in the literature, it is more generally applicable to natural systems because it does not rely on microscopic properties of the system, which are impossible to quantify. Application of the model to crystalline aquifers in the eastern United States shows that bulk emanation rates of radon are generally less than about 30%. </p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/SPE271-p73","usgsCitation":"Wanty, R.B., Lawrence, E.P., and Gundersen, L.C., 1992, A theoretical model for the flux of radon from rock to ground water: GSA Special Papers, v. 271, 6 p., https://doi.org/10.1130/SPE271-p73.","productDescription":"6 p.","costCenters":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":376319,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"271","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Wanty, Richard B. 0000-0002-2063-6423 rwanty@usgs.gov","orcid":"https://orcid.org/0000-0002-2063-6423","contributorId":443,"corporation":false,"usgs":true,"family":"Wanty","given":"Richard","email":"rwanty@usgs.gov","middleInitial":"B.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":792638,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lawrence, Errol P.","contributorId":228974,"corporation":false,"usgs":false,"family":"Lawrence","given":"Errol","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":792639,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gundersen, Linda C. lgundersen@usgs.gov","contributorId":238,"corporation":false,"usgs":true,"family":"Gundersen","given":"Linda","email":"lgundersen@usgs.gov","middleInitial":"C.","affiliations":[{"id":501,"text":"Office of Science Quality and Integrity","active":true,"usgs":true}],"preferred":true,"id":792640,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70179661,"text":"70179661 - 1992 - Tracing watershed weathering reactions with 13C","interactions":[],"lastModifiedDate":"2017-01-12T09:36:34","indexId":"70179661","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Tracing watershed weathering reactions with 13C","docAbstract":"<p>No abstract available.</p>","largerWorkTitle":"Proceedings of the 7th International Symposium on Water-Rock Interaction: WRI-7","conferenceTitle":"Proceedings of the 7th International Symposium on Water-Rock Interaction: WRI-7","conferenceDate":"July 13-18, 1992","conferenceLocation":"Park City, UT","language":"English","publisher":"A.A. Balkema","publisherLocation":"Rotterdam, Netherlands","usgsCitation":"Kendall, C., Mast, M., and Rice, K.C., 1992, Tracing watershed weathering reactions with 13C, <i>in</i> Proceedings of the 7th International Symposium on Water-Rock Interaction: WRI-7, Park City, UT, July 13-18, 1992, p. 569-572.","productDescription":"4 p.","startPage":"569","endPage":"572","costCenters":[],"links":[{"id":333065,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5878a4b7e4b04df303d95873","contributors":{"authors":[{"text":"Kendall, Carol 0000-0002-0247-3405 ckendall@usgs.gov","orcid":"https://orcid.org/0000-0002-0247-3405","contributorId":1462,"corporation":false,"usgs":true,"family":"Kendall","given":"Carol","email":"ckendall@usgs.gov","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":658114,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mast, M.A.","contributorId":67871,"corporation":false,"usgs":true,"family":"Mast","given":"M.A.","affiliations":[],"preferred":false,"id":658115,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rice, Karen C. 0000-0002-9356-5443 kcrice@usgs.gov","orcid":"https://orcid.org/0000-0002-9356-5443","contributorId":1998,"corporation":false,"usgs":true,"family":"Rice","given":"Karen","email":"kcrice@usgs.gov","middleInitial":"C.","affiliations":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"preferred":false,"id":658116,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70179971,"text":"70179971 - 1992 - Ground-water conditions in Utah, spring of 1992","interactions":[],"lastModifiedDate":"2017-01-20T15:16:45","indexId":"70179971","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":110,"text":"Cooperative Investigations Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"32","title":"Ground-water conditions in Utah, spring of 1992","docAbstract":"<p>This is the twenty-ninth in a series of annual reports that describe ground-water conditions in Utah. Reports in this series, published cooperatively by the U.S. Geological Survey and the Utah Division of Water Resources, provide data to enable interested parties to keep abreast of changing ground-water conditions.</p><p>This report, like the others in the series, contains information on well construction, ground-water withdrawal from wells, water-level changes, related changes in precipitation and streamflow, and chemical quality of water. Supplementary data, such as maps showing water-level contours, are included in reports of this series only for those years or areas for which applicable data are available and are important to a discussion of changing ground-water conditions.</p><p>This report includes individual discussions of selected major areas of ground-water development in the State for the calendar year 1991. Water-level fluctuations and selected related data, however, are described from the spring of 1987 to the spring of 1992. Most of the data used in this report were collected by the U.S. Geological Survey in cooperation with the Division of Water Rights and Division of Water Resources, Utah Department of Natural Resources.</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Resources","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the State of Utah, Division of Water Resources and Division of Water Rights","usgsCitation":"Batty, D., Herbert, L.R., Sory, J., Hanson, K.M., Eads, J.P., Smith, G.J., Danner, M., Drumiler, M., Garrett, R., Gerner, S., Slaugh, B., Swenson, R., Howells, J., Christiansen, H., and Thomas, B., 1992, Ground-water conditions in Utah, spring of 1992: Cooperative Investigations Report 32, ix, 91 p.","productDescription":"ix, 91 p","numberOfPages":"104","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333626,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333624,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-173"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5883303be4b0d0023163781c","contributors":{"authors":[{"text":"Batty, D.M.","contributorId":178513,"corporation":false,"usgs":false,"family":"Batty","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":659369,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Herbert, L. R.","contributorId":39865,"corporation":false,"usgs":true,"family":"Herbert","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":659370,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sory, J.D.","contributorId":178510,"corporation":false,"usgs":false,"family":"Sory","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":659371,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hanson, Karen M. khanson@usgs.gov","contributorId":936,"corporation":false,"usgs":true,"family":"Hanson","given":"Karen","email":"khanson@usgs.gov","middleInitial":"M.","affiliations":[{"id":423,"text":"National Geospatial Program","active":true,"usgs":true}],"preferred":true,"id":659372,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Eads, James P.","contributorId":178506,"corporation":false,"usgs":false,"family":"Eads","given":"James","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":659373,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Smith, G. J.","contributorId":80767,"corporation":false,"usgs":true,"family":"Smith","given":"G.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":659374,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Danner, M.R.","contributorId":178514,"corporation":false,"usgs":false,"family":"Danner","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":659375,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Drumiler, M.M.","contributorId":178512,"corporation":false,"usgs":false,"family":"Drumiler","given":"M.M.","affiliations":[],"preferred":false,"id":659376,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Garrett, R. B.","contributorId":35810,"corporation":false,"usgs":true,"family":"Garrett","given":"R. B.","affiliations":[],"preferred":false,"id":659377,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Gerner, S.J.","contributorId":16083,"corporation":false,"usgs":true,"family":"Gerner","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":659378,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Slaugh, B.A.","contributorId":178515,"corporation":false,"usgs":false,"family":"Slaugh","given":"B.A.","affiliations":[],"preferred":false,"id":659379,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Swenson, R.L.","contributorId":178508,"corporation":false,"usgs":false,"family":"Swenson","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":659380,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Howells, J.H.","contributorId":178516,"corporation":false,"usgs":false,"family":"Howells","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":659381,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Christiansen, H.K.","contributorId":178517,"corporation":false,"usgs":false,"family":"Christiansen","given":"H.K.","email":"","affiliations":[],"preferred":false,"id":659382,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Thomas, B.K.","contributorId":177516,"corporation":false,"usgs":false,"family":"Thomas","given":"B.K.","email":"","affiliations":[],"preferred":false,"id":659383,"contributorType":{"id":1,"text":"Authors"},"rank":15}]}}
,{"id":70179418,"text":"70179418 - 1992 - Toxicity of agricultural subsurface drainwater from the San Joaquin Valley, California to juvenile chinook salmon and striped bass","interactions":[],"lastModifiedDate":"2018-09-25T11:40:55","indexId":"70179418","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Toxicity of agricultural subsurface drainwater from the San Joaquin Valley, California to juvenile chinook salmon and striped bass","docAbstract":"<p><span>Juvenile chinook salmon </span><i>Oncorhynchus tshawytscha</i><span> (40-50 mm total length, TL) and striped bass </span><i>Morone saxatilis</i><span> (30-40 mm TL) were exposed to serial dilutions (100, 50, 25, and 12.5%) of agricultural subsurface drainwater (WWD), reconstituted drainwater (RWWD), and reconstituted seawater (IO). Agricultural subsurface drainwater contained naturally elevated concentrations of major ions (such as sodium and sulfate) and trace elements (especially boron and selenium), RWWD contained concentrations of major ions that mimicked those in WWD but trace elements were not elevated, and IO contained concentrations of total dissolved salt that were similar to those in WWD and RWWD but chloride replaced sulfate as the dominant anion. After 28 d of static exposure, over 75% of the chinook salmon in 100% WWD had died, whereas none had died in other dilutions and water types. Growth of chinook salmon in WWD and RWWD, but not in IO, exhibited dilution responses. All striped bass died in 100% WWD within 23 d, whereas 19 of 20 striped bass had died in 100% RWWD after 28 d. In contrast, none died in 100% IO. Growth of striped bass was impaired only in WWD. Fish in WWD accumulated as much as 200 μg/g (dry-weight basis) of boron, whereas fish in control water accumulated less than 3.1 μg/g. Although potentially toxic concentrations of selenium occurred in WWD (geometric means, 158-218 μg/L), chinook salmon and striped bass exposed to this water type accumulated 5.7 μg Se/g or less. These findings indicate that WWD was toxic to chinook salmon and striped bass. Judging from available data, the toxicity of WWD was due primarily to high concentrations of major ions present in atypical ratios, to high concentrations of sulfate, or to both. High concentrations of boron and selenium also may have contributed to the toxicity of WWD, but their effects were not clearly delineated.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1992)121<0078:TOASDF>2.3.CO;2","usgsCitation":"Saiki, M.K., Jennings, M.R., and Wiedmeyer, R.H., 1992, Toxicity of agricultural subsurface drainwater from the San Joaquin Valley, California to juvenile chinook salmon and striped bass: Transactions of the American Fisheries Society, v. 121, no. 1, p. 78-93, https://doi.org/10.1577/1548-8659(1992)121<0078:TOASDF>2.3.CO;2.","productDescription":"16 p.","startPage":"78","endPage":"93","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":332721,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Joaquin Valley","volume":"121","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5868d226e4b0cd2dabe7c80b","contributors":{"authors":[{"text":"Saiki, Michael K.","contributorId":54671,"corporation":false,"usgs":true,"family":"Saiki","given":"Michael","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":657183,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jennings, Mark R.","contributorId":31345,"corporation":false,"usgs":true,"family":"Jennings","given":"Mark","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":657184,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wiedmeyer, Raymond H.","contributorId":176717,"corporation":false,"usgs":false,"family":"Wiedmeyer","given":"Raymond","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":657185,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70179380,"text":"70179380 - 1992 - Toxicity of trace element and salinity mixtures to striped bass (<i>Morone saxatilis</i>) and <i>Daphnia magna</i>","interactions":[],"lastModifiedDate":"2016-12-30T10:44:47","indexId":"70179380","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Toxicity of trace element and salinity mixtures to striped bass (<i>Morone saxatilis</i>) and <i>Daphnia magna</i>","docAbstract":"<p>Acute toxicity tests with reconstituted water were conducted to investigate the relationship between water hardness, salinity, and a mixture of trace elements found in irrigation drain waters entering Stillwater Wildlife Management Area (SWMA), near Fallon, Nevada. The SWMA has been the site of many fish kills in recent years, and previous toxicity studies indicated that one drain water, Pintail Bay, was acutely toxic to organisms acclimated or cultured in fresh water or salt water. This toxicity could reflect both the ionic composition of this saline water and the presence of trace elements. The lowest water salinity tested with<i> Daphnia magna</i> was near the upper salinity tolerance of these organisms; therefore, we were unable to differentiate between the toxic effects of ion composition and those of trace elements. In toxicity tests conducted with striped bass (<i>Morone saxatilis</i>), we found that the extent to which salinity was lethal to striped bass depended on the ion composition of that salinity. Survival of striped bass increased as hardness increased. In addition, a trace element mixture was toxic to striped bass, even though the concentrations of individual elements were below expected acutely lethal concentrations. Although salinity is an important water quality characteristic, the ionic composition of the water must be considered when one assesses the hazard of irrigation drain waters to aquatic organisms.</p>","language":"English","publisher":"Wiley","doi":"10.1002/etc.5620110409","usgsCitation":"Dwyer, F., Burch, S., Ingersoll, C., and Hunn, J.B., 1992, Toxicity of trace element and salinity mixtures to striped bass (<i>Morone saxatilis</i>) and <i>Daphnia magna</i>: Environmental Toxicology and Chemistry, v. 11, no. 4, p. 513-520, https://doi.org/10.1002/etc.5620110409.","productDescription":"8 p.","startPage":"513","endPage":"520","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":332658,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Stillwater Wildlife Management Area ","volume":"11","issue":"4","noUsgsAuthors":false,"publicationDate":"1992-04-01","publicationStatus":"PW","scienceBaseUri":"58662f1ee4b0cd2dabe7c4ed","contributors":{"authors":[{"text":"Dwyer, F.J.","contributorId":107818,"corporation":false,"usgs":true,"family":"Dwyer","given":"F.J.","email":"","affiliations":[],"preferred":false,"id":656993,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burch, S.A.","contributorId":177775,"corporation":false,"usgs":false,"family":"Burch","given":"S.A.","email":"","affiliations":[{"id":6987,"text":"U.S. Fish and Wildlife Sevice","active":true,"usgs":false}],"preferred":false,"id":656994,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ingersoll, C.G. 0000-0003-4531-5949","orcid":"https://orcid.org/0000-0003-4531-5949","contributorId":56338,"corporation":false,"usgs":true,"family":"Ingersoll","given":"C.G.","affiliations":[],"preferred":false,"id":656995,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hunn, J. B.","contributorId":15133,"corporation":false,"usgs":true,"family":"Hunn","given":"J.","middleInitial":"B.","affiliations":[],"preferred":false,"id":656996,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70179100,"text":"70179100 - 1992 - Seepage study of the Bear River including Cutler Reservoir in Cache Valley, Utah and Idaho","interactions":[],"lastModifiedDate":"2016-12-30T10:00:15","indexId":"70179100","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"105","title":"Seepage study of the Bear River including Cutler Reservoir in Cache Valley, Utah and Idaho","docAbstract":"<p>A study was made during 1990 on selected reaches of the Bear River including Cutler Reservoir in Cache Valley, Utah and Idaho, to detem1ine gains or losses of flow from seepage in those reaches. The study showed a net gain of 23.5 cubic feet per second in the Riverdale, Idaho, to Smithfield, Utah, section of the Bear River. The upstream reach of this section of the river had a gain of 13.7 cubic feet per second, the middle reach had a gain of 2.1 cubic feet per second, and the downstream reach had a gain of 7.7 cubic feet per second. The Cutler Reservoir section of the Bear River (Smithfield to Wheelan, Utah) had a net gain of 79.0 cubic feet per second.</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United State Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Herbert, L.R., and Thomas, B., 1992, Seepage study of the Bear River including Cutler Reservoir in Cache Valley, Utah and Idaho: Technical Publication 105, iv, 18.","productDescription":"iv, 18","numberOfPages":"24","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":332203,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":332201,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-6-540"},{"id":332202,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w92000ai.pdf"}],"country":"United States","state":"daho, Utah","otherGeospatial":"Bear River, Cache Valley, Cutler Reservoir","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.181396484375,\n              41.41801503608024\n            ],\n            [\n              -112.181396484375,\n              42.52879629320373\n            ],\n            [\n              -111.719970703125,\n              42.52879629320373\n            ],\n            [\n              -111.719970703125,\n              41.41801503608024\n            ],\n            [\n              -112.181396484375,\n              41.41801503608024\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58550b8de4b02bdf681568d5","contributors":{"authors":[{"text":"Herbert, L. R.","contributorId":39865,"corporation":false,"usgs":true,"family":"Herbert","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":656039,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, B.K.","contributorId":177516,"corporation":false,"usgs":false,"family":"Thomas","given":"B.K.","email":"","affiliations":[],"preferred":false,"id":656040,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70179099,"text":"70179099 - 1992 - Seepage study of the Timpanogos, Wasatch, Sagebrush and Spring Creek, Upper Charleston, and Lower Charleston Canals, Wasatch County, Utah.","interactions":[],"lastModifiedDate":"2018-03-23T16:06:33","indexId":"70179099","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"104","title":"Seepage study of the Timpanogos, Wasatch, Sagebrush and Spring Creek, Upper Charleston, and Lower Charleston Canals, Wasatch County, Utah.","docAbstract":"<p style=\"text-align: left;\" data-mce-style=\"text-align: left;\">A seepage study was made during 1989 on selected reaches of the Timpanogos, Wasatch, Sagebrush and Spring Creek, Upper Charleston, and Lower Charleston Canals in Wasatch County, Utah, to determine gains or losses in discharge. Fluctuations in discharge were adjusted using information from water-stage recorders operated at selected locations during each set· of measurements. The investigation showed a net loss of about 14.9 cubic feet per second in the Timpanogos Canal: the upstream reach gained about 2.0 cubic feet per second, the two middle reaches together lost about 14.1 cubic feet per second, and the downstream reach lost about 2.8 cubic feet per second. The Wasatch Canal showed a net loss of about 8.2 cubic feet per second: the upstream reach lost about 3.7 cubic feet per second, the middle reach showed no gain or loss, and the downstream reach lost about 4.5 cubic feet per second. The Sagebrush and Spring Creek Canal showed a net loss of about 0.5 cubic foot per second: the upstream reach gained about 0.6 cubic foot per second, the middle reach showed no gain or loss, and the downstream reach lost about 1.1 cubic feet per second. The Upper Charleston Canal showed a net gain of about 4.0 cubic feet per second: the upstream reach gained about 5.0 cubic feet per second, and the down-stream reach lost about 1.0 cubic foot per second. The Lower Charleston Canal showed a net gain of about 1.8 cubic feet per second: the upstream reach gained about 2.2 cubic feet per second, and the downstream reach lost about 0.4 cubic foot per second.</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United State Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Herbert, L.R., Burden, C.B., and Thomas, B., 1992, Seepage study of the Timpanogos, Wasatch, Sagebrush and Spring Creek, Upper Charleston, and Lower Charleston Canals, Wasatch County, Utah.: Technical Publication 104, iv, 44 p.","productDescription":"iv, 44 p.","numberOfPages":"48","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":332200,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":332198,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-6-530"},{"id":332199,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/y920/y920000b.pdf"}],"country":"United States","state":"Utah","county":"Wasatch County","otherGeospatial":"Timpanogos, Wasatch, Sagebrush and Spring Creek, Upper Charleston, and Lower Charleston Canals","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.6,\n              40.4\n            ],\n            [\n              -111.6,\n              40.6\n            ],\n            [\n              -111.4,\n              40.6\n            ],\n            [\n              -111.4,\n              40.4\n            ],\n            [\n              -111.6,\n              40.4\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58550b8de4b02bdf681568d7","contributors":{"authors":[{"text":"Herbert, L. R.","contributorId":39865,"corporation":false,"usgs":true,"family":"Herbert","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":656036,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burden, Carole B. cburden@usgs.gov","contributorId":852,"corporation":false,"usgs":true,"family":"Burden","given":"Carole","email":"cburden@usgs.gov","middleInitial":"B.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":656037,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, B.K.","contributorId":177516,"corporation":false,"usgs":false,"family":"Thomas","given":"B.K.","email":"","affiliations":[],"preferred":false,"id":656038,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70176563,"text":"70176563 - 1992 - Geomorphic response to the 1989-90 eruptions of Redoubt Volcano, Alaska","interactions":[],"lastModifiedDate":"2017-04-19T14:20:37","indexId":"70176563","displayToPublicDate":"2016-04-05T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Geomorphic response to the 1989-90 eruptions of Redoubt Volcano, Alaska","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"1992 American Water Resources Association Annual Conference","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"American Water Resources Association Annual Conference","conferenceDate":"April 9-10, 1992","conferenceLocation":"Fairbanks, AK","language":"English","publisher":"American Water Resources Association","publisherLocation":"Middleburg, VA","usgsCitation":"Dorava, J., 1992, Geomorphic response to the 1989-90 eruptions of Redoubt Volcano, Alaska, <i>in</i> 1992 American Water Resources Association Annual Conference, Fairbanks, AK, April 9-10, 1992, p. 87-88.","productDescription":"2 p.","startPage":"87","endPage":"88","numberOfPages":"2","costCenters":[{"id":121,"text":"Alaska Volcano Observatory","active":false,"usgs":true}],"links":[{"id":328814,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":" Aleutian Range, at the head of the Chigmit Mountains subrange in Lake Clark National Park and Preserve","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -153.0010986328125,\n              60.356847344793586\n            ],\n            [\n              -153.0010986328125,\n              60.568077898122155\n            ],\n            [\n              -152.49298095703125,\n              60.568077898122155\n            ],\n            [\n              -152.49298095703125,\n              60.356847344793586\n            ],\n            [\n              -153.0010986328125,\n              60.356847344793586\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57feb5d7e4b0824b2d155132","contributors":{"authors":[{"text":"Dorava, J.M.","contributorId":68756,"corporation":false,"usgs":true,"family":"Dorava","given":"J.M.","affiliations":[],"preferred":false,"id":649206,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70176455,"text":"70176455 - 1992 - Sonar monitoring of gravel-transport processes at a stream-gaging station in a disturbed watershed [abs.]","interactions":[],"lastModifiedDate":"2016-09-14T15:07:03","indexId":"70176455","displayToPublicDate":"2016-04-04T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Sonar monitoring of gravel-transport processes at a stream-gaging station in a disturbed watershed [abs.]","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings 1992 International Association for Hydrological Sciences Meeting, Erosion and Sediment Transport Monitoring Programs in River Basins, Oslo, Norway","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"International Association of Hydrological Sciences Press","publisherLocation":"Wallingford, Oxfordshire OX10 8BB, UK","collaboration":"Norwegian Water Resources and Energy Administration and the International Commission on Continental Erosion of the International Association of Hydrological Sciences; co-sponsored by UNESCO, WMO, the Norwegian Geophysical Union, and the Norwegian National Committee for Hydrology","usgsCitation":"Dinehart, R., 1992, Sonar monitoring of gravel-transport processes at a stream-gaging station in a disturbed watershed [abs.], chap. <i>of</i> Proceedings 1992 International Association for Hydrological Sciences Meeting, Erosion and Sediment Transport Monitoring Programs in River Basins, Oslo, Norway, p. 71-76.","productDescription":"6 p.","startPage":"71","endPage":"76","numberOfPages":"6","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":328650,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57da74b9e4b090824ffb7e97","contributors":{"authors":[{"text":"Dinehart, R.L.","contributorId":54610,"corporation":false,"usgs":true,"family":"Dinehart","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":648811,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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