{"pageNumber":"523","pageRowStart":"13050","pageSize":"25","recordCount":16449,"records":[{"id":70012962,"text":"70012962 - 1985 - Errors and parameter estimation in precipitation-runoff modeling: 1. Theory","interactions":[],"lastModifiedDate":"2020-01-19T10:38:12","indexId":"70012962","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Errors and parameter estimation in precipitation-runoff modeling: 1. Theory","docAbstract":"<p><span>Errors in complex conceptual precipitation-runoff models may be analyzed by placing them into a statistical framework. This amounts to treating the errors as random variables and defining the probabilistic structure of the errors. By using such a framework, a large array of techniques, many of which have been presented in the statistical literature, becomes available to the modeler for quantifying and analyzing the various sources of error. A number of these techniques are reviewed in this paper, with special attention to the peculiarities of hydrologic models. Known methodologies for parameter estimation (calibration) are particularly applicable for obtaining physically meaningful estimates and for explaining how bias in runoff prediction caused by model error and input error may contribute to bias in parameter estimation.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR021i008p01195","usgsCitation":"Troutman, B.M., 1985, Errors and parameter estimation in precipitation-runoff modeling: 1. Theory: Water Resources Research, v. 21, no. 8, p. 1195-1213, https://doi.org/10.1029/WR021i008p01195.","productDescription":"19 p.","startPage":"1195","endPage":"1213","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":222047,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"8","noUsgsAuthors":false,"publicationDate":"2008-01-08","publicationStatus":"PW","scienceBaseUri":"505a0a49e4b0c8380cd522b2","contributors":{"authors":[{"text":"Troutman, Brent M.","contributorId":195329,"corporation":false,"usgs":false,"family":"Troutman","given":"Brent","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":364945,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012827,"text":"70012827 - 1985 - Palmer Drought Severity Index as a Measure of Hydrologic Drought","interactions":[],"lastModifiedDate":"2013-03-14T13:09:41","indexId":"70012827","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2529,"text":"Journal of the American Water Resources Association","active":true,"publicationSubtype":{"id":10}},"title":"Palmer Drought Severity Index as a Measure of Hydrologic Drought","docAbstract":"The Palmer Drought Severity Index (PDSI) for climatic divisions in New Jersey is compared to the occurrence within each climatic division of streamflows in their lower quartile for the month (streamflow index) and ground-water levels in their lower quartile for the month (ground-water index). These indices are found to have distinct properties. The PDSI values and groundwater index indicate more persistent subnormal conditions than the streamflow index for truncation levels yielding the same total duration of drought over a period. Overall, the three indices of drought can provide three very different characterizations of drought. Refs.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the American Water Resources Association","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wiley","doi":"10.1111/j.1752-1688.1985.tb05357.x","issn":"00431370","usgsCitation":"Alley, W., 1985, Palmer Drought Severity Index as a Measure of Hydrologic Drought: Journal of the American Water Resources Association, v. 21, no. 1, p. 105-114, https://doi.org/10.1111/j.1752-1688.1985.tb05357.x.","startPage":"105","endPage":"114","numberOfPages":"10","costCenters":[],"links":[{"id":221915,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269331,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1752-1688.1985.tb05357.x"}],"volume":"21","issue":"1","noUsgsAuthors":false,"publicationDate":"2007-06-08","publicationStatus":"PW","scienceBaseUri":"505a732ae4b0c8380cd76ed0","contributors":{"authors":[{"text":"Alley, William M.","contributorId":93030,"corporation":false,"usgs":true,"family":"Alley","given":"William M.","affiliations":[],"preferred":false,"id":364619,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012825,"text":"70012825 - 1985 - Statistical evaluation of an inductively coupled plasma atomic emission spectrometric method for routine water quality testing","interactions":[],"lastModifiedDate":"2020-01-19T11:01:35","indexId":"70012825","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":847,"text":"Applied Spectroscopy","active":true,"publicationSubtype":{"id":10}},"title":"Statistical evaluation of an inductively coupled plasma atomic emission spectrometric method for routine water quality testing","docAbstract":"In an interlaboratory test, inductively coupled plasma atomic emission spectrometry (ICP-AES) was compared with flame atomic absorption spectrometry and molecular absorption spectrophotometry for the determination of 17 major and trace elements in 100 filtered natural water samples. No unacceptable biases were detected. The analysis precision of ICP-AES was found to be equal to or better than alternative methods. Known-addition recovery experiments demonstrated that the ICP-AES determinations are accurate to between plus or minus 2 and plus or minus 10 percent; four-fifths of the tests yielded average recoveries of 95-105 percent, with an average relative standard deviation of about 5 percent.","language":"English","publisher":"Sage","doi":"10.1366/0003702854248458","issn":"00037028","usgsCitation":"Garbarino, J., Jones, B.E., and Stein, G., 1985, Statistical evaluation of an inductively coupled plasma atomic emission spectrometric method for routine water quality testing: Applied Spectroscopy, v. 39, no. 3, p. 535-541, https://doi.org/10.1366/0003702854248458.","productDescription":"7 p.","startPage":"535","endPage":"541","numberOfPages":"7","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":221913,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"3","noUsgsAuthors":false,"publicationDate":"1985-05-01","publicationStatus":"PW","scienceBaseUri":"505b9729e4b08c986b31b902","contributors":{"authors":[{"text":"Garbarino, J.R.","contributorId":76326,"corporation":false,"usgs":true,"family":"Garbarino","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":364615,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, B. E.","contributorId":70787,"corporation":false,"usgs":true,"family":"Jones","given":"B.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":364614,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stein, G.P.","contributorId":30363,"corporation":false,"usgs":true,"family":"Stein","given":"G.P.","email":"","affiliations":[],"preferred":false,"id":364613,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012805,"text":"70012805 - 1985 - Reduction of hexavalent chromium in water samples acidified for preservation","interactions":[],"lastModifiedDate":"2020-01-19T11:08:06","indexId":"70012805","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2262,"text":"Journal of Environmental Quality","active":true,"publicationSubtype":{"id":10}},"title":"Reduction of hexavalent chromium in water samples acidified for preservation","docAbstract":"<div class=\"article-section__content en main\"><p>Reduction of hexavalent chromium, Cr(VI), in water samples, preserved by standard techniques, was investigated. The standard preservation technique for water samples that are to be analyzed for Cr(VI) consists of filtration through a 0.45‐<i>µ</i>m membrane, acidification to a pH &lt; 2, and storage in plastic bottles. Batch experiments were conducted to evaluate the effect of H<sup>+</sup><span>&nbsp;</span>concentration, NO<sub>2</sub>, temperature, and dissolved organic carbon (DOC) on the reduction of Cr(VI) to Cr(III). The rate of reduction of Cr(VI) to Cr(III) increased with increasing NO<sub>2</sub>, DOC, H<sup>+</sup>, and temperature. Reduction of Cr(VI) by organic matter occurred in some samples even though the samples were unacidified. Reduction of Cr(VI) is inhibited to an extent by storing the sample at 4°C. Stability of Cr(VI) in water is variable and depends on the other constituents present in the sample. Water samples collected for the determination of Cr(VI) should be filtered (0.45‐<i>µ</i>m membrane), refrigerated, and analyzed as quickly as possible. Water samples should not be acidified. Measurement of total Cr in addition to Cr(VI) can serve as a check for Cr(VI) reduction. If total Cr is greater than Cr(VI), the possibility that Cr(VI) reduction has occurred needs to be considered.</p></div><div class=\"accordion article-accordion\"><h2><br data-mce-bogus=\"1\"></h2></div>","language":"English","publisher":"Wiley","doi":"10.2134/jeq1985.00472425001400030017x","issn":"00472425","usgsCitation":"Stollenwerk, K.G., and Grove, D., 1985, Reduction of hexavalent chromium in water samples acidified for preservation: Journal of Environmental Quality, v. 14, no. 3, p. 396-399, https://doi.org/10.2134/jeq1985.00472425001400030017x.","productDescription":"4 p.","startPage":"396","endPage":"399","numberOfPages":"4","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":222557,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e4a3dce4b0e8fec6cdb9e6","contributors":{"authors":[{"text":"Stollenwerk, Kenneth G. kgstolle@usgs.gov","contributorId":578,"corporation":false,"usgs":true,"family":"Stollenwerk","given":"Kenneth","email":"kgstolle@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":779763,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grove, D.B.","contributorId":56689,"corporation":false,"usgs":true,"family":"Grove","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":364578,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012795,"text":"70012795 - 1985 - Error bounds in cascading regressions","interactions":[],"lastModifiedDate":"2020-01-19T11:10:56","indexId":"70012795","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2554,"text":"Journal of the International Association for Mathematical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Error bounds in cascading regressions","docAbstract":"<p>Cascading regressions is a technique for predicting a value of a dependent variable when no paired measurements exist to perform a standard regression analysis. Biases in coefficients of a cascaded-regression line as well as error variance of points about the line are functions of the correlation coefficient between dependent and independent variables. Although this correlation cannot be computed because of the lack of paired data, bounds can be placed on errors through the required properties of the correlation coefficient. The potential meansquared error of a cascaded-regression prediction can be large, as illustrated through an example using geomorphologic data.&nbsp;</p>","language":"English","publisher":"Springer","doi":"10.1007/BF01034754","issn":"00205958","usgsCitation":"Karlinger, M., and Troutman, B., 1985, Error bounds in cascading regressions: Journal of the International Association for Mathematical Geology, v. 17, no. 3, p. 287-295, https://doi.org/10.1007/BF01034754.","productDescription":"9 p.","startPage":"287","endPage":"295","numberOfPages":"9","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":222440,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0a48e4b0c8380cd522ac","contributors":{"authors":[{"text":"Karlinger, M.R.","contributorId":95039,"corporation":false,"usgs":true,"family":"Karlinger","given":"M.R.","affiliations":[],"preferred":false,"id":364547,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Troutman, B.M.","contributorId":73638,"corporation":false,"usgs":true,"family":"Troutman","given":"B.M.","email":"","affiliations":[],"preferred":false,"id":364546,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70013018,"text":"70013018 - 1985 - Modeling the rate-controlled sorption of hexavalent chromium","interactions":[],"lastModifiedDate":"2020-01-19T10:48:54","indexId":"70013018","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Modeling the rate-controlled sorption of hexavalent chromium","docAbstract":"<p><span>Sorption of chromium VI on the iron-oxide- and hydroxide-coated surface of alluvial material was numerically simulated with rate-controlled reactions. Reaction kinetics and diffusional processes, in the form of film, pore, and particle diffusion, were simulated and compared with experimental results. The use of empirically calculated rate coefficients for diffusion through the reacting surface was found to simulate experimental data; pore or particle diffusion is believed to be a possible rate-controlling mechanism. The use of rate equations to predict conservative transport and rate- and local-equilibrium-controlled reactions was shown to be feasible.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR021i011p01703","usgsCitation":"Grove, D., and Stollenwerk, K.G., 1985, Modeling the rate-controlled sorption of hexavalent chromium: Water Resources Research, v. 21, no. 11, p. 1703-1709, https://doi.org/10.1029/WR021i011p01703.","productDescription":"7 p.","startPage":"1703","endPage":"1709","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":220671,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"11","noUsgsAuthors":false,"publicationDate":"2008-01-08","publicationStatus":"PW","scienceBaseUri":"505a4ad4e4b0c8380cd690ab","contributors":{"authors":[{"text":"Grove, D.B.","contributorId":56689,"corporation":false,"usgs":true,"family":"Grove","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":365086,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stollenwerk, Kenneth G. kgstolle@usgs.gov","contributorId":578,"corporation":false,"usgs":true,"family":"Stollenwerk","given":"Kenneth","email":"kgstolle@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":779757,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012937,"text":"70012937 - 1985 - WATER RESOURCES ACTIVITIES OF THE U. S. GEOLOGICAL SURVEY.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:07","indexId":"70012937","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3718,"text":"Water Resources Bulletin","printIssn":"0043-1370","active":true,"publicationSubtype":{"id":10}},"title":"WATER RESOURCES ACTIVITIES OF THE U. S. GEOLOGICAL SURVEY.","docAbstract":"The U. S. Geological Survey's (USGS) program of hydrologic data collection, investigations, and research provides information essential to water-resoures planning and management. The activities of the Water Resources Division (WRD) are in support of the Geological Survey's mission to provide geologic, topographic, and hydrologic information that contributes to the wise management of the Nation's natural resources and that promotes the health, safety, and well-being of the people.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Water Resources Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00431370","usgsCitation":"Peck, D.L., 1985, WATER RESOURCES ACTIVITIES OF THE U. S. GEOLOGICAL SURVEY.: Water Resources Bulletin, v. 21, no. 6, p. 901-907.","startPage":"901","endPage":"907","numberOfPages":"7","costCenters":[],"links":[{"id":222626,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc38fe4b08c986b32b24c","contributors":{"authors":[{"text":"Peck, Dallas L.","contributorId":60187,"corporation":false,"usgs":true,"family":"Peck","given":"Dallas","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":364883,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012732,"text":"70012732 - 1985 - Thermodynamic stability of CoOOH and its coprecipitation with manganese","interactions":[],"lastModifiedDate":"2020-01-19T10:59:36","indexId":"70012732","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Thermodynamic stability of CoOOH and its coprecipitation with manganese","docAbstract":"<p><span>A precipitate of cobalt oxyhydroxides formed by bubbling oxygen through a dilute solution of Co(NO</span><sub>3</sub><span>)</span><sub>2</sub><span>&nbsp;held at pH 9.0 and 25°C was aged for 23 months in contact with the original solution, with access to atmospheric oxygen. Co</span><sub>3</sub><span>O</span><sub>4</sub><span>&nbsp;and CoOOH were identified in the precipitate by X-ray diffraction. Chemical equilibria involving these solids were evaluated by measurements of solution pH and Co</span><sup>2+</sup><span>&nbsp;activities and by redox potential measurements and gave a&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>&amp;#x394;G</mtext><msub><mi></mi><mn>coOOH</mn></msub><msup><mi></mi><mn>0</mn></msup></math>\"><span class=\"MJX_Assistive_MathML\">ΔGcoOOH0</span></span></span><span>&nbsp;of&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-2-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>&amp;#x2212;92.3 &amp;#xB1; 0.5 kcal/mole</mtext></math>\"><span class=\"MJX_Assistive_MathML\">−92.3 ± 0.5 kcal/mole</span></span></span><span>. This value and other thermodynamic data show relative feasibility of hypothetical reaction steps and changes in reaction paths during automated coprecipitation titrations and subsequent aging of a precipitate that finally contained βMnOOH, MnO</span><sub>2</sub><span>&nbsp;(birnessite) and CoOOH.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(85)90173-5","issn":"00167037","usgsCitation":"Hem, J., Roberson, C.E., and Lind, C.J., 1985, Thermodynamic stability of CoOOH and its coprecipitation with manganese: Geochimica et Cosmochimica Acta, v. 49, no. 3, p. 801-810, https://doi.org/10.1016/0016-7037(85)90173-5.","productDescription":"10 p.","startPage":"801","endPage":"810","numberOfPages":"10","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":222322,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"49","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb27ce4b08c986b325826","contributors":{"authors":[{"text":"Hem, J.D.","contributorId":54576,"corporation":false,"usgs":true,"family":"Hem","given":"J.D.","affiliations":[],"preferred":false,"id":364382,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roberson, C. E.","contributorId":40190,"corporation":false,"usgs":true,"family":"Roberson","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":364381,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lind, Carol J.","contributorId":36110,"corporation":false,"usgs":true,"family":"Lind","given":"Carol","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":364380,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70013359,"text":"70013359 - 1985 - Hydrologic changes associated with the October 28, 1983, Idaho earthquake","interactions":[],"lastModifiedDate":"2012-03-12T17:18:38","indexId":"70013359","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3209,"text":"Pure and Applied Geophysics PAGEOPH","active":true,"publicationSubtype":{"id":10}},"title":"Hydrologic changes associated with the October 28, 1983, Idaho earthquake","docAbstract":"Significant hydrologic changes were observed after the magnitude 7.3 earthquake that occurred on October 28, 1983, in central Idaho. Groundwater levels rose by as much as 3 meters near the epicenter. Discharge in many streams and springs increased, in some instances by more than 100%. One warm spring ceased flowing for several days; the flow then resumed and peaked at about nine times its original rate. Available data show no significant changes in water quality following the earthquake. ?? 1985 Birkha??user Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Pure and Applied Geophysics PAGEOPH","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Birkha??user-Verlag","doi":"10.1007/BF00874599","issn":"00334553","usgsCitation":"Whitehead, R., Harper, R., and Sisco, H., 1985, Hydrologic changes associated with the October 28, 1983, Idaho earthquake: Pure and Applied Geophysics PAGEOPH, v. 122, no. 2-4, p. 280-293, https://doi.org/10.1007/BF00874599.","startPage":"280","endPage":"293","numberOfPages":"14","costCenters":[],"links":[{"id":205022,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00874599"},{"id":220249,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"122","issue":"2-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3577e4b0c8380cd5ff40","contributors":{"authors":[{"text":"Whitehead, R.L.","contributorId":34891,"corporation":false,"usgs":true,"family":"Whitehead","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":365895,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harper, R.W.","contributorId":36104,"corporation":false,"usgs":true,"family":"Harper","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":365896,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sisco, H.G.","contributorId":54185,"corporation":false,"usgs":true,"family":"Sisco","given":"H.G.","email":"","affiliations":[],"preferred":false,"id":365897,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012261,"text":"70012261 - 1985 - Unit hydrograph approximations assuming linear flow through topologically random channel networks","interactions":[],"lastModifiedDate":"2020-03-05T20:03:23","indexId":"70012261","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Unit hydrograph approximations assuming linear flow through topologically random channel networks","docAbstract":"<p><span>The instantaneous unit Hydrograph (IUH) of a drainage basin is derived in terms of fundamental basin characteristics (</span><i>Z</i><span>, α, β), where α parameterizes the link (channel segment) length distribution, and β is a vector of hydraulic parameters,<span>&nbsp;</span></span><i>Z</i><span><span>&nbsp;</span>is one of three basin topological properties,<span>&nbsp;</span></span><i>N</i><span>, (</span><i>N</i><span>,<span>&nbsp;</span></span><i>D</i><span>), or (</span><i>N</i><span>,<span>&nbsp;</span></span><i>M</i><span>), where<span>&nbsp;</span></span><i>N</i><span><span>&nbsp;</span>is magnitude (number of first-order streams),<span>&nbsp;</span></span><i>D</i><span><span>&nbsp;</span>is diameter (mainstream length), and<span>&nbsp;</span></span><i>M</i><span><span>&nbsp;</span>is order. The IUH is derived based on assumptions that the links are independent and identically distributed random variables and that the network is a member of a topologically random population. Linear routing schemes, including translation, diffusion, and general linear routing are used, and constant drainage density is assumed. By using (</span><i>N</i><span>, α, β) as the fundamental basin characteristics, asymptotic (for large<span>&nbsp;</span></span><i>N</i><span>) considerations lead to a Weibull probability density function for the IUH, with time to peak given by<span>&nbsp;</span></span><i>t<sub>p</sub></i><span><span>&nbsp;</span>= (2</span><i>N</i><span>)</span><sup>½</sup><span><span>&nbsp;</span>α</span><sup>*</sup><span>/β</span><sup>*</sup><span><span>&nbsp;</span>where α</span><sup>*</sup><span><span>&nbsp;</span>is mean link length, and β</span><sup>*</sup><span><span>&nbsp;</span>is a scalar hydraulic parameter (usually average celerity). This asymptotic IUH is identical for all linear routing schemes.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR021i005p00743","usgsCitation":"Troutman, B.M., and Karlinger, M.R., 1985, Unit hydrograph approximations assuming linear flow through topologically random channel networks: Water Resources Research, v. 21, no. 5, p. 743-754, https://doi.org/10.1029/WR021i005p00743.","productDescription":"12 p.","startPage":"743","endPage":"754","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":222125,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"5","noUsgsAuthors":false,"publicationDate":"2008-01-08","publicationStatus":"PW","scienceBaseUri":"505bbc88e4b08c986b328cb1","contributors":{"authors":[{"text":"Troutman, Brent M.","contributorId":195329,"corporation":false,"usgs":false,"family":"Troutman","given":"Brent","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":363118,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Karlinger, Michael R.","contributorId":10777,"corporation":false,"usgs":true,"family":"Karlinger","given":"Michael","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":363119,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70013336,"text":"70013336 - 1985 - U. S. G. S. MODULAR GROUND-WATER FLOW MODEL: DESIGNED TO BE UNDERSTOOD AND ADAPTED.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:39","indexId":"70013336","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"U. S. G. S. MODULAR GROUND-WATER FLOW MODEL: DESIGNED TO BE UNDERSTOOD AND ADAPTED.","docAbstract":"The paper discusses a carefully designed model program and its complementary complete description of all of the physical and mathematical concepts used in the model. The model program consists of a series of independent subroutines called modules. Modules are grouped by hydrologic function into 'packages. ' A report describing the model was written in three levels. At one level the hydrologic concepts on which the model is based are explained. The second level describes how the concepts were incorporated into the program. The third level describes specific modules in sufficient depth to permit modifications to the model.","conferenceTitle":"Hydraulics and Hydrology in the Small Computer Age, Proceedings of the Specialty Conference.","conferenceLocation":"Lake Buena Vista, FL, USA","language":"English","publisher":"ASCE","publisherLocation":"New York, NY, USA","isbn":"0872624749","usgsCitation":"McDonald, M.G., and Harbaugh, A.W., 1985, U. S. G. S. MODULAR GROUND-WATER FLOW MODEL: DESIGNED TO BE UNDERSTOOD AND ADAPTED., Hydraulics and Hydrology in the Small Computer Age, Proceedings of the Specialty Conference., Lake Buena Vista, FL, USA, p. 1225-1230.","startPage":"1225","endPage":"1230","numberOfPages":"6","costCenters":[],"links":[{"id":219909,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb9e5e4b08c986b327eb8","contributors":{"authors":[{"text":"McDonald, Michael G.","contributorId":47352,"corporation":false,"usgs":true,"family":"McDonald","given":"Michael","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":365838,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harbaugh, Arlen W. harbaugh@usgs.gov","contributorId":426,"corporation":false,"usgs":true,"family":"Harbaugh","given":"Arlen","email":"harbaugh@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":365837,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70013069,"text":"70013069 - 1985 - Assessment of long-term salinity changes in an irrigated stream-aquifer system","interactions":[],"lastModifiedDate":"2020-01-19T11:09:19","indexId":"70013069","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Assessment of long-term salinity changes in an irrigated stream-aquifer system","docAbstract":"<p><span>Changes in salinity in groundwater and surface water in the Arkansas River valley of southeastern Colorado are primarily related to irrigation practices. A solute transport model was applied to an 11-mile reach of the valley to compute salinity changes in response to spatially and temporally varying stresses. The model was calibrated in 1973 using detailed field measurements made during 1971 and 1972. In 1973 the calibrated model was used to predict that a gradual long-term increase in groundwater salinity of about 2–3% per year would occur if the observed irrigation practices continued. The study area was resampled during the winter of 1982 to help evaluate if any long-term changes in salinity are actually occurring. Nonparametric and parametric statistical tests were used to help assess the significance of observed changes in groundwater salinity. These tests indicate that a statistically significant increase in salinity occurred between the winters of 1971 and 1972 (the model calibration period). However, a comparison of the winter 1972 and winter 1982 data indicates that no significant net change in salinity has occurred during this 10-year period. An analysis of the few available historical data (1895, 1923, 1959–1961, and 1964) supports the hypothesis that groundwater salinity in this irrigated area has reached a long-term dynamic equilibrium in response to irrigation practices. The model predictions of long-term salinity increases were invalid probably because the calibration period occurred during a short-term annual trend of increasing salinity in the river (and hence in leaky irrigation canals and in applied irrigation water), which was not representative of the long-term trend.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR021i011p01611","usgsCitation":"Konikow, L.F., and Person, M., 1985, Assessment of long-term salinity changes in an irrigated stream-aquifer system: Water Resources Research, v. 21, no. 11, p. 1611-1624, https://doi.org/10.1029/WR021i011p01611.","productDescription":"14 p.","startPage":"1611","endPage":"1624","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":220405,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Arkansas River valley","volume":"21","issue":"11","noUsgsAuthors":false,"publicationDate":"2008-01-08","publicationStatus":"PW","scienceBaseUri":"5059e637e4b0c8380cd47268","contributors":{"authors":[{"text":"Konikow, Leonard F. 0000-0002-0940-3856 lkonikow@usgs.gov","orcid":"https://orcid.org/0000-0002-0940-3856","contributorId":158,"corporation":false,"usgs":true,"family":"Konikow","given":"Leonard","email":"lkonikow@usgs.gov","middleInitial":"F.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":365210,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Person, Mark","contributorId":55568,"corporation":false,"usgs":true,"family":"Person","given":"Mark","affiliations":[],"preferred":false,"id":365211,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012952,"text":"70012952 - 1985 - Overview of hydrologic-data collection by the US Geological Survey in Oklahoma.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:05","indexId":"70012952","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2944,"text":"Oklahoma Geology Notes","active":true,"publicationSubtype":{"id":10}},"title":"Overview of hydrologic-data collection by the US Geological Survey in Oklahoma.","docAbstract":"The US Geological Survey (USGS) collects hydrologic data from 1332 stream, lake, and ground-water sites in Oklahoma. Information on the quantity of water from a network of 123 streamflow stations, 30 lakes, 42 peak-flow stations, three low-flow stations, and on the quality of water from 40 stream locations is published each year in the USGS publication Water Resources Data for Oklahoma. Information on water levels from 1134 ground-water wells is currently published in cooperation with the State of Oklahoma in the USGS publication Ground-Water Levels in Observation Wells in Oklahoma. The data also are made available to the public as printouts from several computerized databases maintained by the USGS. -Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Oklahoma Geology Notes","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00301736","usgsCitation":"Hauth, L., 1985, Overview of hydrologic-data collection by the US Geological Survey in Oklahoma.: Oklahoma Geology Notes, v. 45, no. 4, p. 149-161.","startPage":"149","endPage":"161","numberOfPages":"13","costCenters":[],"links":[{"id":221861,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a720ee4b0c8380cd768d8","contributors":{"authors":[{"text":"Hauth, L.D.","contributorId":48551,"corporation":false,"usgs":true,"family":"Hauth","given":"L.D.","affiliations":[],"preferred":false,"id":364922,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70013064,"text":"70013064 - 1985 - Lacustrine-humate model for primary uranium ore deposits, Grants uranium region, New Mexico","interactions":[],"lastModifiedDate":"2023-01-12T17:04:16.864261","indexId":"70013064","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Lacustrine-humate model for primary uranium ore deposits, Grants uranium region, New Mexico","docAbstract":"<p>Two generations of uranium ore, primary and redistributed, occur in fluvial sandstones of the Upper Jurassic Morrison Formation in the San Juan basin; the two stages of ore formation can be related to the hydrologic history of the basin. Primary ore formed soon after Morrison deposition, in the Late Jurassic to Early Cretaceous, and a model, the lacustrine-humate model, is offered that views primary mineralization as a diagenetic event related to early pore fluid evolution. The basic premise is that the humate, a pore-filling organic material closely associated with primary ore, originated as humic acids dissolved in pore waters of greenish-gray lacustrine mudstones deposited in the mud-flat facies of the Brushy Basin Member and similar \"K\" shale beds in the Westwater Can on Member. During compaction associated with early burial, formation water expelled from lacustrine mudstone units carried these humic acids into adjacent sandstone beds where the organics precipitated, forming the humate deposits that concentrated uranium.</p><p>During the Tertiary, much later in the hydrologic history of the basin, when Jurassic sediments were largely compacted, oxygenated ground water flowed basinward from uplifted basin margins. This invasion of Morrison sandstone beds by oxidizing ground waters redistributed uranium from primary ores along redox boundaries, forming ore deposits that resemble roll-front-type uranium ores.</p>","language":"English","publisher":"American Association of Petroleum Geologists (AAPG)","doi":"10.1306/94885589-1704-11D7-8645000102C1865D","usgsCitation":"Turner-Peterson, C., 1985, Lacustrine-humate model for primary uranium ore deposits, Grants uranium region, New Mexico: American Association of Petroleum Geologists Bulletin, v. 69, no. 11, p. 1990-2020, https://doi.org/10.1306/94885589-1704-11D7-8645000102C1865D.","productDescription":"31 p.","startPage":"1990","endPage":"2020","numberOfPages":"31","costCenters":[],"links":[{"id":220347,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"Grants uranium region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -108.64038174995106,\n              36.04693775500846\n            ],\n            [\n              -108.64038174995106,\n              34.70563438153877\n            ],\n            [\n              -106.912022747075,\n              34.70563438153877\n            ],\n            [\n              -106.912022747075,\n              36.04693775500846\n            ],\n            [\n              -108.64038174995106,\n              36.04693775500846\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"69","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4130e4b0c8380cd6537f","contributors":{"authors":[{"text":"Turner-Peterson, C. E.","contributorId":53958,"corporation":false,"usgs":true,"family":"Turner-Peterson","given":"C. E.","affiliations":[],"preferred":false,"id":365203,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012979,"text":"70012979 - 1985 - Nitrogen and phosphorus speciation and flux in a large Florida river wetland System","interactions":[],"lastModifiedDate":"2018-02-12T18:11:13","indexId":"70012979","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Nitrogen and phosphorus speciation and flux in a large Florida river wetland System","docAbstract":"<p><span>Hydrologic measurements and analyses of various nitrogen and phosphorus species were made on the Apalachicola River system in northern Florida in 1979 and 1980. Annual outflows of total nitrogen (TN) and total phosphorus (TP) were not substantially different from annual inflows. However, there was significant net import of ammonia and soluble reactive phosphorus and net export of some particulate and organic species. The TN: TP ratio ranged from 12 to 15, but the specific ratio of dissolved inorganic nitrogen: soluble reactive phosphorus was much higher (up to 40) and increased in a downstream direction; this contributed to a phosphorus-limiting situation in Apalachicola estuary. Processes within the flood plain ecosystem accounted for much of the release of organic and particulate species and retention of inorganic species. This flood plain function is probably critical for maintaining a nutrient pool in the estuary which supports secondary productivity and a detrital-based food web.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR021i005p00724","usgsCitation":"Elder, J.F., 1985, Nitrogen and phosphorus speciation and flux in a large Florida river wetland System: Water Resources Research, v. 21, no. 5, p. 724-732, https://doi.org/10.1029/WR021i005p00724.","productDescription":"9 p.","startPage":"724","endPage":"732","costCenters":[],"links":[{"id":487159,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/wr021i005p00724","text":"Publisher Index Page"},{"id":220223,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Apalachicola river","volume":"21","issue":"5","noUsgsAuthors":false,"publicationDate":"2008-01-08","publicationStatus":"PW","scienceBaseUri":"505a66c5e4b0c8380cd72fa4","contributors":{"authors":[{"text":"Elder, John F.","contributorId":23919,"corporation":false,"usgs":true,"family":"Elder","given":"John","email":"","middleInitial":"F.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":364993,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70013054,"text":"70013054 - 1985 - Culturing Selenastrum capricornutum (Chlorophyta) in a synthetic algal nutrient medium with defined mineral particulates","interactions":[],"lastModifiedDate":"2020-01-19T11:03:40","indexId":"70013054","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1919,"text":"Hydrobiologia","onlineIssn":"1573-5117","printIssn":"0018-8158","active":true,"publicationSubtype":{"id":10}},"title":"Culturing Selenastrum capricornutum (Chlorophyta) in a synthetic algal nutrient medium with defined mineral particulates","docAbstract":"<p>Algal nutrient studies in chemically-defined media typically employ a synthetic chelator to prevent iron hydroxide precipitation. Micronutrient-particulate interactions may, however, significantly affect chemical speciation and hence biovailability of these nutrients in natural waters. A technique is described by which Selenastrum capricornutum Printz (Chlorophyta) may be cultured in a medium where trace metal speciation (except iron) is controlled, not by organic chelation, but by sorption onto titanium dioxide. Application of this culturing protocol in conjunction with results from sorption studies of nutrient ions on mineral particles provides a means of studying biological impacts of sorptive processes in aquatic environments.</p>","language":"English","publisher":"Springer","doi":"10.1007/BF00011393","issn":"00188158","usgsCitation":"Kuwabara, J.S., Davis, J., and Chang, C.C., 1985, Culturing Selenastrum capricornutum (Chlorophyta) in a synthetic algal nutrient medium with defined mineral particulates: Hydrobiologia, v. 124, no. 1, p. 23-271, https://doi.org/10.1007/BF00011393.","productDescription":"249 p.","startPage":"23","endPage":"271","numberOfPages":"249","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":220228,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"124","issue":"1","noUsgsAuthors":false,"publicationDate":"1985-05-01","publicationStatus":"PW","scienceBaseUri":"5059fd08e4b0c8380cd4e5cb","contributors":{"authors":[{"text":"Kuwabara, James S. 0000-0003-2502-1601 kuwabara@usgs.gov","orcid":"https://orcid.org/0000-0003-2502-1601","contributorId":3374,"corporation":false,"usgs":true,"family":"Kuwabara","given":"James","email":"kuwabara@usgs.gov","middleInitial":"S.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":779761,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, J.A.","contributorId":71694,"corporation":false,"usgs":true,"family":"Davis","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":365183,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chang, Cecily C.Y.","contributorId":68032,"corporation":false,"usgs":true,"family":"Chang","given":"Cecily","email":"","middleInitial":"C.Y.","affiliations":[],"preferred":false,"id":365182,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70013134,"text":"70013134 - 1985 - Phosphorus-zinc interactive effects on growth by Selenastrum capricornutum (chlorophyta)","interactions":[],"lastModifiedDate":"2020-03-09T19:25:42","indexId":"70013134","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","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":"Phosphorus-zinc interactive effects on growth by Selenastrum capricornutum (chlorophyta)","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/es00135a005","issn":"0013936X","usgsCitation":"Kuwabara, J., 1985, Phosphorus-zinc interactive effects on growth by Selenastrum capricornutum (chlorophyta): Environmental Science & Technology, v. 19, no. 5, p. 417-421, https://doi.org/10.1021/es00135a005.","productDescription":"5 p.","startPage":"417","endPage":"421","numberOfPages":"5","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":220352,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"5","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a78bfe4b0c8380cd78789","contributors":{"authors":[{"text":"Kuwabara, J.S.","contributorId":57905,"corporation":false,"usgs":true,"family":"Kuwabara","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":365370,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70013128,"text":"70013128 - 1985 - Migration of wood-preserving chemicals in contaminated groundwater in a sand aquifer at Pensacola, Florida","interactions":[],"lastModifiedDate":"2020-01-19T10:51:51","indexId":"70013128","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","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":"Migration of wood-preserving chemicals in contaminated groundwater in a sand aquifer at Pensacola, Florida","docAbstract":"Operation of a wood-preserving facility for nearly 80 years at Pensacola, FL, contaminated the near-surface groundwater with creosote and pentachlorophenol. The major source of aquifer contamination was unlined surface impoundments that were in direct hydraulic contact with the groundwater. Episodes of overtopping the impoundments and overland flow of treatment liquor and waste were also significant to the migration and contamination of the groundwater. Solutes contaminating the ground-water are mainly naphthalene and substituted phenols. Sorption did not influence retardation of solutes in transport in the groundwater. Phenol and the mono substituted methylphenols appear to be undergoing bio-transformation. Pentachlorophenol (PCP) was not found in significant concentrations in the groundwater possibly because the solubility of PCP is approximately 5 mg/L at pH 6, near the average acidity for the groundwater.","language":"English","publisher":"ACS","doi":"10.1021/es00140a012","issn":"0013936X","usgsCitation":"Goerlitz, D., Troutman, D., Godsy, E., and Franks, B., 1985, Migration of wood-preserving chemicals in contaminated groundwater in a sand aquifer at Pensacola, Florida: Environmental Science & Technology, v. 19, no. 10, p. 955-961, https://doi.org/10.1021/es00140a012.","productDescription":"7 p.","startPage":"955","endPage":"961","numberOfPages":"7","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":220234,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida ","city":"Pensacola ","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.099609375,\n              30.259067203213018\n            ],\n            [\n              -86.253662109375,\n              30.259067203213018\n            ],\n            [\n              -86.253662109375,\n              30.713503990354965\n            ],\n            [\n              -87.099609375,\n              30.713503990354965\n            ],\n            [\n              -87.099609375,\n              30.259067203213018\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"19","issue":"10","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a5713e4b0c8380cd6da32","contributors":{"authors":[{"text":"Goerlitz, D.F.","contributorId":8445,"corporation":false,"usgs":true,"family":"Goerlitz","given":"D.F.","affiliations":[],"preferred":false,"id":365356,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Troutman, D.E.","contributorId":66301,"corporation":false,"usgs":true,"family":"Troutman","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":365358,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Godsy, E.M.","contributorId":56685,"corporation":false,"usgs":true,"family":"Godsy","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":365357,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Franks, B.J.","contributorId":107739,"corporation":false,"usgs":true,"family":"Franks","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":365359,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70013123,"text":"70013123 - 1985 - Errors and parameter estimation in precipitation-runoff modeling: 2. Case study","interactions":[],"lastModifiedDate":"2020-01-19T10:38:48","indexId":"70013123","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Errors and parameter estimation in precipitation-runoff modeling: 2. Case study","docAbstract":"<p><span>A case study is presented which illustrates some of the error analysis, sensitivity analysis, and parameter estimation procedures reviewed in the first part of this paper. It is shown that those procedures, most of which come from statistical nonlinear regression theory, are invaluable in interpreting errors in precipitation-runoff modeling and in identifying appropriate calibration strategies.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR021i008p01214","usgsCitation":"Troutman, B.M., 1985, Errors and parameter estimation in precipitation-runoff modeling: 2. Case study: Water Resources Research, v. 21, no. 8, p. 1214-1222, https://doi.org/10.1029/WR021i008p01214.","productDescription":"9 p.","startPage":"1214","endPage":"1222","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":220178,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"8","noUsgsAuthors":false,"publicationDate":"2008-01-08","publicationStatus":"PW","scienceBaseUri":"505a0a4ae4b0c8380cd522b5","contributors":{"authors":[{"text":"Troutman, Brent M.","contributorId":195329,"corporation":false,"usgs":false,"family":"Troutman","given":"Brent","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":365346,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70013033,"text":"70013033 - 1985 - Geochemical investigations of polychlorinated dibenzo-p-dioxins in the subsurface environment at an abandoned wood-treatment facility","interactions":[],"lastModifiedDate":"2020-01-19T11:22:42","indexId":"70013033","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","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":"Geochemical investigations of polychlorinated dibenzo-p-dioxins in the subsurface environment at an abandoned wood-treatment facility","docAbstract":"<p>The discharge of effluents containing creosote and pentachlorophenol into two unlined surface impoundments at a wood-treatment facility in Pensacola, Florida, resulted in contamination of the underlying sand and gravel aquifer. These wastes contained significant amounts of chlorinated dioxins, such as isomers of hexa- and heptachlorodibenzo-p-dioxins and octachlorodibenzo-p-dioxin, probably derived from commercial pentachlorophenol. Geochemical investigations of pond sludge, groundwater and porous media from the unsaturated and saturated zones indicated that these geologic materials were contaminated by chlorinated dioxins. The fate and movement of these compounds in the subsurface environment were studied using the technique of GC-MS-MS. Chlorinated dioxins migrated both vertically and horizontally in the subsurface and were present at considerable distances from the source of contamination. Concentrations of chlorinated dioxins in groundwater were several orders of magnitude lower than in porous media from the unsaturated and saturated zones. Ratios of the various isomers remained relatively constant in highly contaminated areas. However, in less contaminated areas, isomer ratios changed dramatically; at certain locations, one hexachlorodibenzo-p-dioxin isomer predominated. The environmental significance of these compounds is discussed.</p>","language":"English","publisher":"Wiley","doi":"10.1002/etc.5620040507","issn":"07307268","usgsCitation":"Pereira, W.E., Rostad, C., and Sisak, M., 1985, Geochemical investigations of polychlorinated dibenzo-p-dioxins in the subsurface environment at an abandoned wood-treatment facility: Environmental Toxicology and Chemistry, v. 4, no. 5, p. 629-639, https://doi.org/10.1002/etc.5620040507.","productDescription":"11 p.","startPage":"629","endPage":"639","numberOfPages":"11","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":219952,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"5","noUsgsAuthors":false,"publicationDate":"1985-10-01","publicationStatus":"PW","scienceBaseUri":"505a1649e4b0c8380cd5510b","contributors":{"authors":[{"text":"Pereira, W. E.","contributorId":46981,"corporation":false,"usgs":true,"family":"Pereira","given":"W.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":365128,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rostad, C.E.","contributorId":50939,"corporation":false,"usgs":true,"family":"Rostad","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":365129,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sisak, M.E.","contributorId":24912,"corporation":false,"usgs":true,"family":"Sisak","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":365127,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70013215,"text":"70013215 - 1985 - STREAMFLOW LOSSES, CONSEQUENT FLOW THROUGH A THICK UNSATURATED ZONE, AND RECHARGE TO AN UNCONFINED AQUIFER.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:39","indexId":"70013215","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"STREAMFLOW LOSSES, CONSEQUENT FLOW THROUGH A THICK UNSATURATED ZONE, AND RECHARGE TO AN UNCONFINED AQUIFER.","docAbstract":"Two experiments were conducted in conjunction with a 23-day aquifer test made in south-central Arizona to determine (1) water loss from a natural channel and (2) flow through a 330-foot-thick unsaturated zone overlying an unconfined aquifer. The experiments provided control for the aquifer test plus results relative to arid land hydrology. The increases of soil moisture within the 330-foot-thick unsaturated zone and the consequent water-level rises show that recharge can occur quickly and that relatively large amounts of water can be recharged through thick sequences of unsaturated material.","conferenceTitle":"Development and Management Aspects of Irrigation and Drainage Systems.","conferenceLocation":"San Antonio, TX, USA","language":"English","publisher":"ASCE","publisherLocation":"New York, NY, USA","isbn":"0872624722","usgsCitation":"Marie, J., 1985, STREAMFLOW LOSSES, CONSEQUENT FLOW THROUGH A THICK UNSATURATED ZONE, AND RECHARGE TO AN UNCONFINED AQUIFER., Development and Management Aspects of Irrigation and Drainage Systems., San Antonio, TX, USA, p. 486-487.","startPage":"486","endPage":"487","numberOfPages":"2","costCenters":[],"links":[{"id":220022,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aaf97e4b0c8380cd87694","contributors":{"authors":[{"text":"Marie, J.R.","contributorId":63416,"corporation":false,"usgs":true,"family":"Marie","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":365561,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70013117,"text":"70013117 - 1985 - ANNIE - INTERACTIVE PROCESSING OF DATA BASES FOR HYDROLOGIC MODELS.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:38","indexId":"70013117","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"ANNIE - INTERACTIVE PROCESSING OF DATA BASES FOR HYDROLOGIC MODELS.","docAbstract":"ANNIE is a data storage and retrieval system that was developed to reduce the time and effort required to calibrate, verify, and apply watershed models that continuously simulate water quantity and quality. Watershed models have three categories of input: parameters to describe segments of a drainage area, linkage of the segments, and time-series data. Additional goals for ANNIE include the development of software that is easily implemented on minicomputers and some microcomputers and software that has no special requirements for interactive display terminals. Another goal is for the user interaction to be based on the experience of the user so that ANNIE is helpful to the inexperienced user and yet efficient and brief for the experienced user. Finally, the code should be designed so that additional hydrologic models can easily be added to ANNIE.","conferenceTitle":"International Conference on Interactive Information and Processing Systems for Meteorology, Oceanography, and Hydrology (Preprints of Papers).","conferenceLocation":"Los Angeles, CA, USA","language":"English","publisher":"American Meteorological Soc","publisherLocation":"Boston, MA, USA","usgsCitation":"Lumb, A.M., and Kittle, J.L., 1985, ANNIE - INTERACTIVE PROCESSING OF DATA BASES FOR HYDROLOGIC MODELS., International Conference on Interactive Information and Processing Systems for Meteorology, Oceanography, and Hydrology (Preprints of Papers)., Los Angeles, CA, USA, p. 91-93.","startPage":"91","endPage":"93","numberOfPages":"3","costCenters":[],"links":[{"id":220123,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e62ee4b0c8380cd47210","contributors":{"authors":[{"text":"Lumb, Alan M.","contributorId":47792,"corporation":false,"usgs":true,"family":"Lumb","given":"Alan","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":365334,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kittle, John L.","contributorId":90468,"corporation":false,"usgs":true,"family":"Kittle","given":"John","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":365335,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70013191,"text":"70013191 - 1985 - QUALITY ASSURANCE OF U. S. GEOLOGICAL SURVEY WATER-QUALITY FIELD MEASUREMENTS.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:29","indexId":"70013191","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"QUALITY ASSURANCE OF U. S. GEOLOGICAL SURVEY WATER-QUALITY FIELD MEASUREMENTS.","docAbstract":"Reference samples are submitted semiannually to field analysts for measurement of these parameters with the same techniques and instruments used in the field. Both the personnel and the instruments involved in making the determinations are recorded. When the data are complete, a report defining the quality of the analytical results is prepared and circulated to appropriate District, Regional, and National offices. Field data, in addition to their immediate use, are normally placed in a national data base and are available to all hydrologists. As a result, the quality of field measurements can have a profound effect on their investigations. The quality assurance program described is designed to insure that the field data of the Water Resources Division are highly accurate.","largerWorkTitle":"ASTM Special Technical Publication","conferenceTitle":"Quality Assurance for Environmental Measurements.","conferenceLocation":"Boulder, CO, USA","language":"English","publisher":"ASTM","publisherLocation":"Philadelphia, PA, USA","issn":"00660558","isbn":"0803102240","usgsCitation":"Erdmann, D.E., and Thomas, J., 1985, QUALITY ASSURANCE OF U. S. GEOLOGICAL SURVEY WATER-QUALITY FIELD MEASUREMENTS., <i>in</i> ASTM Special Technical Publication, Boulder, CO, USA, p. 110-115.","startPage":"110","endPage":"115","numberOfPages":"6","costCenters":[],"links":[{"id":220574,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a906de4b0c8380cd7fd1b","contributors":{"authors":[{"text":"Erdmann, D. E.","contributorId":30264,"corporation":false,"usgs":true,"family":"Erdmann","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":365510,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, J.D.","contributorId":76884,"corporation":false,"usgs":true,"family":"Thomas","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":365511,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70013148,"text":"70013148 - 1985 - Dissolution of alkaline earth sulfates in the presence of montmorillonite","interactions":[],"lastModifiedDate":"2020-01-19T10:49:50","indexId":"70013148","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3728,"text":"Water, Air, & Soil Pollution","onlineIssn":"1573-2932","printIssn":"0049-6979","active":true,"publicationSubtype":{"id":10}},"title":"Dissolution of alkaline earth sulfates in the presence of montmorillonite","docAbstract":"In a study of the effect of montmorillonite on the dissolution of BaSO4 (barite), SrSO4 (celestite), and 226Ra from U mill tailings, it was found that: (1) More of these substances dissolve in an aqueous system that contains montmorillonite than dissolve in a similar system without clay, due to the ion exchange properties of the clay; (2) Na-montmorillonite is more effective in aiding dissolution than is Ca-montmorillonite; (3) the amount of Ra that moves from mill tailings to an exchanger increases as solution sulfate activity decreases. Leaching experiments suggest that 226Ra from H2SO4-circuit U mill tailings from Edgemont, South Dakota, is not present as pure Ra sulfate or as an impurity in anhydrite or gypsum; it is less soluble, and probably occurs as a trace constituent in barite.","language":"English","publisher":"Springer","doi":"10.1007/BF00568389","issn":"00496979","usgsCitation":"Eberl, D.D., and Landa, E.R., 1985, Dissolution of alkaline earth sulfates in the presence of montmorillonite: Water, Air, & Soil Pollution, v. 25, no. 2, p. 207-214, https://doi.org/10.1007/BF00568389.","productDescription":"8 p.","startPage":"207","endPage":"214","numberOfPages":"8","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":220571,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a022de4b0c8380cd4ff13","contributors":{"authors":[{"text":"Eberl, D. D.","contributorId":66282,"corporation":false,"usgs":true,"family":"Eberl","given":"D.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":365404,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Landa, Edward R. erlanda@usgs.gov","contributorId":2112,"corporation":false,"usgs":true,"family":"Landa","given":"Edward","email":"erlanda@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":779758,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012263,"text":"70012263 - 1985 - Water-level changes in the Ogallala aquifer, northwestern Oklahoma.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:03","indexId":"70012263","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2944,"text":"Oklahoma Geology Notes","active":true,"publicationSubtype":{"id":10}},"title":"Water-level changes in the Ogallala aquifer, northwestern Oklahoma.","docAbstract":"The Ogallala aquifer, that part of the High Plains aquifer in Oklahoma, is part of a regional aquifer system that underlies parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming. In 1978 the US Geological Survey began a 5- year study of the High Plains regional aquifer system to provide hydrologic information for evaluation of the effects of long-term development of the aquifer and to develop a capability for predicting aquifer response to various ground-water-management alternatives (Weeks, 1978). -from Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Oklahoma Geology Notes","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00301736","usgsCitation":"Havens, J., 1985, Water-level changes in the Ogallala aquifer, northwestern Oklahoma.: Oklahoma Geology Notes, v. 45, no. 5, p. 205-210.","startPage":"205","endPage":"210","numberOfPages":"6","costCenters":[],"links":[{"id":222127,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bcd4de4b08c986b32dfac","contributors":{"authors":[{"text":"Havens, J.S.","contributorId":12043,"corporation":false,"usgs":true,"family":"Havens","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":363125,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}