{"pageNumber":"4846","pageRowStart":"121125","pageSize":"25","recordCount":165626,"records":[{"id":70011607,"text":"70011607 - 1982 - Comparison of techniques for estimating annual lake evaporation using climatological data","interactions":[],"lastModifiedDate":"2020-09-02T17:36:22.506657","indexId":"70011607","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","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":"Comparison of techniques for estimating annual lake evaporation using climatological data","docAbstract":"<p><span>Mean annual evaporation estimates were determined for 30 lakes by use of a numerical model (Morton, 1979) and by use of an evaporation map prepared by the U.S. Weather Service (Kohler et al., 1959). These estimates were compared to the reported value of evaporation determined from measurements on each lake. Various lengths of observation and methods of measurement were used among the 30 lakes. The evaporation map provides annual evaporation estimates which are more consistent with observations than those determined by use of the numerical model. The map cannot provide monthly estimates, however, and is only available for the contiguous United States. The numerical model can provide monthly estimates for shallow lakes and is based on monthly observations of temperature, humidity, and sunshine duration.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR018i003p00630","usgsCitation":"Andersen, M., and Jobson, H., 1982, Comparison of techniques for estimating annual lake evaporation using climatological data: Water Resources Research, v. 18, no. 3, p. 630-636, https://doi.org/10.1029/WR018i003p00630.","productDescription":"7 p.","startPage":"630","endPage":"636","costCenters":[],"links":[{"id":220783,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"3","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"5059f894e4b0c8380cd4d1cd","contributors":{"authors":[{"text":"Andersen, M.E.","contributorId":39520,"corporation":false,"usgs":true,"family":"Andersen","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":361529,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jobson, H.E.","contributorId":44952,"corporation":false,"usgs":true,"family":"Jobson","given":"H.E.","affiliations":[],"preferred":false,"id":361530,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011587,"text":"70011587 - 1982 - Depositional setting and diagenetic evolution of some Tertiary unconventional reservoir rocks, Uinta Basin, Utah","interactions":[],"lastModifiedDate":"2023-01-10T17:56:03.888123","indexId":"70011587","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","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":"Depositional setting and diagenetic evolution of some Tertiary unconventional reservoir rocks, Uinta Basin, Utah","docAbstract":"<p>The Douglas Creek Member of the Tertiary Green River Formation underlies much of the Uinta basin, Utah, and contains large volumes of oil and gas trapped in a complex of fractured low-permeability sandstone reservoirs. In the southeastern part of the basin at Pariette Bench, the Eocene Douglas Creek Member is a thick sequence of fine-grained alluvial sandstone complexly intercalated with lacustrine claystone and carbonate rock. Sediments were deposited in a subsiding intermontane basin along the shallow fluctuating margin of ancient Lake Uinta. Although the Uinta basin has undergone postdepositional uplift and erosion, the deepest cored rocks at Pariette Bench have never been buried more than 9,800 ft (3,000 m).</p><p>The sandstones, dominantly lithic arkoses and feldspathic litharenites, were derived from source terranes south of the Uinta basin. Secondary silica and several generations of authigenic calcite [Ca<sub>1.8-1.9</sub>(Mg<sub>0.02-0.06</sub>Fe<sub>0.02-0.06</sub>)(CO<sub>3</sub>)<sub>2</sub>], dolomite [Ca<sub>1.3-1.4</sub>(Mg<sub>0.6-0.7</sub>Fe<sub>0.02-0.04</sub>)(CO<sub>3</sub>)<sub>2</sub>], and ankerite [Ca<sub>1.2-1.3</sub>(Mg<sub>0.2-0.3</sub>Fe<sub>0.4-0.6</sub>)(CO<sub>3</sub>)<sub>2</sub>] form a replacive cement in the sandstones. Commonly, syntaxial overgrowths of late iron-bearing carbonate occur on detrital grains and preexisting relicts of iron-free carbonate cement. In sandstone where carbonate has been partly dissolved, abundant authigenic illite, partly ordered mixed- ayer illite-smectite, and small amounts of chlorite partly to completely fill secondary pores. Isotopic composition of carbonate cement and grain-supported rock range from -0.39 to -6.18 ^pmil for ^dgr<sup>13</sup>C and -7.80 to -13.98 ^pmil for ^dgr<sup>18</sup>O, indicating that authigenic carbonate formed at low temperatures in the presence of meteoric waters by a process of solution-precipitation. Enrichment of carbon and oxygen in early diagenetic calcite and fossiliferous rock relative to late diagenetic ankerite indicates a trend toward lighter isotopic carbonate compositions with increasing diagenesis.</p><p>Kerogenous rocks at Pariette Bench are thermochemically immature and therefore are not the source of oil produced in the field. Hydrocarbons are compositionally similar to some of the oils produced from the Green River Formation in the Bluebell-Altamont field and are interpreted to have migrated from mature Green River source rocks through a network of open fractures. The occurrence of small amounts of hydrocarbon in secondary pores indicates that its emplacement postdated carbonate dissolution.</p>","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/03B5A98F-16D1-11D7-8645000102C1865D","usgsCitation":"Pitman, J.K., Fouch, T.D., and Goldhaber, M., 1982, Depositional setting and diagenetic evolution of some Tertiary unconventional reservoir rocks, Uinta Basin, Utah: American Association of Petroleum Geologists Bulletin, v. 66, no. 10, p. 1581-1596, https://doi.org/10.1306/03B5A98F-16D1-11D7-8645000102C1865D.","productDescription":"16 p.","startPage":"1581","endPage":"1596","numberOfPages":"16","costCenters":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":221598,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Uinta Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -111.0225857789739,\n              40.63348012338835\n            ],\n            [\n              -111.0225857789739,\n              39.27696875971418\n            ],\n            [\n              -108.75245518662385,\n              39.27696875971418\n            ],\n            [\n              -108.75245518662385,\n              40.63348012338835\n            ],\n            [\n              -111.0225857789739,\n              40.63348012338835\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"66","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fec8e4b0c8380cd4ef16","contributors":{"authors":[{"text":"Pitman, Janet K. 0000-0002-0441-779X jpitman@usgs.gov","orcid":"https://orcid.org/0000-0002-0441-779X","contributorId":767,"corporation":false,"usgs":true,"family":"Pitman","given":"Janet","email":"jpitman@usgs.gov","middleInitial":"K.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true},{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":361472,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fouch, T. D.","contributorId":68333,"corporation":false,"usgs":true,"family":"Fouch","given":"T.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":361471,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goldhaber, M. B. 0000-0002-1785-4243","orcid":"https://orcid.org/0000-0002-1785-4243","contributorId":103280,"corporation":false,"usgs":true,"family":"Goldhaber","given":"M. B.","affiliations":[],"preferred":false,"id":361473,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011586,"text":"70011586 - 1982 - Morphology, distribution, and development of submarine canyons on the United States Atlantic continental slope between Hudson and Baltimore Canyons","interactions":[],"lastModifiedDate":"2017-09-13T14:34:57","indexId":"70011586","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Morphology, distribution, and development of submarine canyons on the United States Atlantic continental slope between Hudson and Baltimore Canyons","docAbstract":"<p><span>The distribution and morphology of submarine canyons off the eastern United States between Hudson and Baltimore Canyons have been mapped by long-range sidescan sonar. In this area canyons are numerous, and their spacing correlates with overall slope gradient; they are absent where the gradient is less than 3°, are 2 to 10 km apart where the gradient is 3° to 5°, and are 1.5 to 4 km apart where the gradient exceeds 6°. Canyons range from straight to sinuous; those having sinuous axes indent the edge of the continental shelf and appear to be older than those that head on the upper slope and have straighter axes. A difference in canyon age would suggest that canyons are initiated on the continental slope and only with greater age erode headward to indent the shelf. Shallow gullies on the middle and upper slope parts of the canyon walls suggest that submarine erosion has been a major process in a recent phase of canyon development.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1982)10<408:MDADOS>2.0.CO;2","issn":"00917613","usgsCitation":"Twichell, D.C., and Roberts, D.G., 1982, Morphology, distribution, and development of submarine canyons on the United States Atlantic continental slope between Hudson and Baltimore Canyons: Geology, v. 10, no. 8, p. 408-412, https://doi.org/10.1130/0091-7613(1982)10<408:MDADOS>2.0.CO;2.","productDescription":"5 p.","startPage":"408","endPage":"412","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":221597,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Baltimore Canyon, Hudson Canyon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.1357421875,\n              37.55764242679524\n            ],\n            [\n              -74.1357421875,\n              39.5633531658293\n            ],\n            [\n              -70.7794189453125,\n              39.5633531658293\n            ],\n            [\n              -70.7794189453125,\n              37.55764242679524\n            ],\n            [\n              -74.1357421875,\n              37.55764242679524\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"10","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5e5de4b0c8380cd709b2","contributors":{"authors":[{"text":"Twichell, David C.","contributorId":37730,"corporation":false,"usgs":true,"family":"Twichell","given":"David","email":"","middleInitial":"C.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":361470,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roberts, David G.","contributorId":39937,"corporation":false,"usgs":false,"family":"Roberts","given":"David","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":361469,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011571,"text":"70011571 - 1982 - Exotic terranes of western California","interactions":[],"lastModifiedDate":"2012-03-12T17:18:31","indexId":"70011571","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Exotic terranes of western California","docAbstract":"Numerous distinct geological terranes compose the North American Cordillera1; there may be as many as 50 terranes in California alone2. Critical to deciphering the history of Cordilleran tectonic assembly is an understanding of the displacement history of individual terranes. It is therefore important to know: (1) whether a terrane has undergone significant motion with respect to the stable craton (that is, whether it is allochthonous or exotic); (2) if so, when relative motion started and stopped; (3) from where an individual terrane originated; and (4) the nature of interterrane movements. We consider here the problem of determining whether the now-juxtaposed Salinian and Stanley Mountain terranes of California became amalgamated at or near their present position with respect to cratonic North America, or if they collided at a considerable distance from their present positions and were later accreted to North America as a composite package. The palaeomagnetic data that we present indicate that the latter was the case. ?? 1982 Nature Publishing Group.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Nature","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1038/297215a0","issn":"00280836","usgsCitation":"McWilliams, M., and Howell, D.G., 1982, Exotic terranes of western California: Nature, v. 297, no. 5863, p. 215-217, https://doi.org/10.1038/297215a0.","startPage":"215","endPage":"217","numberOfPages":"3","costCenters":[],"links":[{"id":205110,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1038/297215a0"},{"id":221298,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"297","issue":"5863","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0db3e4b0c8380cd53155","contributors":{"authors":[{"text":"McWilliams, M.O.","contributorId":7840,"corporation":false,"usgs":true,"family":"McWilliams","given":"M.O.","email":"","affiliations":[],"preferred":false,"id":361425,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Howell, D. G.","contributorId":52546,"corporation":false,"usgs":true,"family":"Howell","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":361426,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1000279,"text":"1000279 - 1982 - Subcellular distribution of mercury in liver of lake trout (<i>Salvelinus namaycush</i>)","interactions":[],"lastModifiedDate":"2016-04-01T09:13:33","indexId":"1000279","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1606,"text":"Experientia","active":true,"publicationSubtype":{"id":10}},"title":"Subcellular distribution of mercury in liver of lake trout (<i>Salvelinus namaycush</i>)","docAbstract":"<p>Mercury was found primarily (80%) in the submicroscopic material (magnification x &lt; 7700) of environmentally exposed adult lake trout from Lake Michigan, USA.</p>","language":"English","publisher":"Springer","doi":"10.1007/BF01964098","usgsCitation":"Passino, D.M., and Kramer, J.M., 1982, Subcellular distribution of mercury in liver of lake trout (<i>Salvelinus namaycush</i>): Experientia, v. 38, no. 6, p. 689-690, https://doi.org/10.1007/BF01964098.","productDescription":"2 p.","startPage":"689","endPage":"690","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128919,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"38","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699c04","contributors":{"authors":[{"text":"Passino, D.R. May","contributorId":30573,"corporation":false,"usgs":true,"family":"Passino","given":"D.R.","email":"","middleInitial":"May","affiliations":[],"preferred":false,"id":308328,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kramer, J. Matsumoto","contributorId":103619,"corporation":false,"usgs":true,"family":"Kramer","given":"J.","email":"","middleInitial":"Matsumoto","affiliations":[],"preferred":false,"id":308329,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011830,"text":"70011830 - 1982 - Techniques for using iron crucibles in experimental igneous petrology.","interactions":[],"lastModifiedDate":"2013-02-14T09:53:10","indexId":"70011830","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":738,"text":"American Mineralogist","active":true,"publicationSubtype":{"id":10}},"title":"Techniques for using iron crucibles in experimental igneous petrology.","docAbstract":"Some iron crucibles contain impurities of Mn, Ti and other elements. Such impurities may alter the fO2 of the system and induce crucible-charge interactions. Pretreatment of impure iron crucibles in a CO2-CO atmosphere at 1050oC, under conditions slightly more reducing than Fe-Fe1-xO, minimizes undesirable changes in the bulk composition of the charge. -J.A.Z.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Mineralogist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Mineralogical Society of America","issn":"0003004X","usgsCitation":"Thornber, C., and Huebner, J., 1982, Techniques for using iron crucibles in experimental igneous petrology.: American Mineralogist, v. 67, no. 11-12, p. 1144-1154.","startPage":"1144","endPage":"1154","numberOfPages":"11","costCenters":[],"links":[{"id":221392,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267368,"type":{"id":11,"text":"Document"},"url":"https://www.minsocam.org/ammin/AM67/AM67_1144.pdf"}],"volume":"67","issue":"11-12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba439e4b08c986b3201ac","contributors":{"authors":[{"text":"Thornber, C.R.","contributorId":69302,"corporation":false,"usgs":true,"family":"Thornber","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":362060,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Huebner, J.S.","contributorId":41422,"corporation":false,"usgs":true,"family":"Huebner","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":362059,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011789,"text":"70011789 - 1982 - The solubilities of calcite, aragonite and vaterite in CO2-H2O solutions between 0 and 90°C, and an evaluation of the aqueous model for the system CaCO3-CO2-H2O","interactions":[],"lastModifiedDate":"2018-03-21T15:17:40","indexId":"70011789","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","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":"The solubilities of calcite, aragonite and vaterite in CO2-H2O solutions between 0 and 90°C, and an evaluation of the aqueous model for the system CaCO3-CO2-H2O","docAbstract":"<p>Calculations based on approximately 350 new measurements (Ca<sub><i>T</i></sub>-PCO<sub>2</sub>) of the solubilities of calcite, aragonite and vaterite in CO<sub>2</sub>-H<sub>2</sub>O solutions between 0 and 90&deg;C indicate the following values for the log of the equilibrium constants&nbsp;<i>K</i><sub><i>C</i></sub>,&nbsp;<i>K</i><sub><i>A</i></sub>, and&nbsp;<i>K</i><sub><i>V</i></sub>&nbsp;respectively, for the reaction CaCO<sub>3</sub>(s) = Ca<sup>2+</sup>&nbsp;+ CO<sup>2&minus;</sup><sub>3</sub>:&nbsp;</p>\n<p><span><img src=\"http://ars.els-cdn.com/content/image/1-s2.0-0016703782900564-si1.gif\" alt=\"\" title=\"\" width=\"519\" height=\"18\" data-inlimgeid=\"1-s2.0-0016703782900564-si1.gif\" data-loaded=\"true\" /></span><span><img src=\"http://ars.els-cdn.com/content/image/1-s2.0-0016703782900564-si2.gif\" alt=\"\" title=\"\" width=\"519\" height=\"18\" data-inlimgeid=\"1-s2.0-0016703782900564-si2.gif\" data-loaded=\"true\" /></span><span><img src=\"http://ars.els-cdn.com/content/image/1-s2.0-0016703782900564-si3.gif\" alt=\"\" title=\"\" width=\"519\" height=\"18\" data-inlimgeid=\"1-s2.0-0016703782900564-si3.gif\" data-loaded=\"true\" /></span>&nbsp;where&nbsp;<i>T</i>&nbsp;is in&nbsp;<sup>o</sup>K. At 25&deg;C the logarithms of the equilibrium constants are &minus;8.480 &plusmn; 0.020, &minus;8.336 &plusmn; 0.020 and &minus;7.913 &plusmn; 0.020 for calcite, aragonite and vaterite, respectively.</p>\n<p>The equilibrium constants are internally consistent with an aqueous model that includes the CaHCO<sup>+</sup><sub>3</sub>&nbsp;and CaCO<sup>0</sup><sub>3</sub>&nbsp;ion pairs, revised analytical expressions for CO<sub>2</sub>-H<sub>2</sub>O equilibria, and extended Debye-H&uuml;ckel individual ion activity coefficients. Using this aqueous model, the equilibrium constant of aragonite shows no PCO<sub>2</sub>-dependence if the CaHCO<sup>+</sup><sub>3</sub>&nbsp;association constant is&nbsp;<span><img src=\"http://ars.els-cdn.com/content/image/1-s2.0-0016703782900564-si4.gif\" alt=\"\" title=\"\" width=\"567\" height=\"22\" data-inlimgeid=\"1-s2.0-0016703782900564-si4.gif\" data-loaded=\"true\" /></span>between 0 and 90&deg;C, corresponding to the value&nbsp;<i>log</i><i>K</i><sub><i>Cahco</i><sup>+</sup><sub>3</sub></sub>&nbsp;= 1.11 &plusmn; 0.07 at 25&deg;C. The CaCO<sup>0</sup><sub>3</sub>association constant was measured potentiometrically to be&nbsp;<span><img src=\"http://ars.els-cdn.com/content/image/1-s2.0-0016703782900564-si5.gif\" alt=\"\" title=\"\" width=\"555\" height=\"21\" data-inlimgeid=\"1-s2.0-0016703782900564-si5.gif\" data-loaded=\"true\" /></span>&nbsp;between 5 and 80&deg;C, yielding&nbsp;<i>log</i><i>K</i><sub><i>CaCO</i><sup>0</sup><sub>3</sub></sub>&nbsp;= 3.22 &plusmn; 0.14 at 25&deg;C.</p>\n<p>The CO<sub>2</sub>-H<sub>2</sub>O equilibria have been critically evaluated and new empirical expressions for the temperature dependence of&nbsp;<i>K</i><sub><i>H</i></sub>,&nbsp;<i>K</i><sub>1</sub>&nbsp;and&nbsp;<i>K</i><sub>2</sub>&nbsp;are&nbsp;<span><img src=\"http://ars.els-cdn.com/content/image/1-s2.0-0016703782900564-si6.gif\" alt=\"\" title=\"\" width=\"622\" height=\"21\" data-inlimgeid=\"1-s2.0-0016703782900564-si6.gif\" data-loaded=\"true\" /></span>,&nbsp;<span><img src=\"http://ars.els-cdn.com/content/image/1-s2.0-0016703782900564-si7.gif\" alt=\"\" title=\"\" width=\"680\" height=\"21\" data-inlimgeid=\"1-s2.0-0016703782900564-si7.gif\" data-loaded=\"true\" /></span>and&nbsp;<i>log</i><i>K</i><sub>2</sub>&nbsp;= &minus;107.8871 &minus; 0.03252849<i>T</i>&nbsp;+ 5151.79/<i>T</i>&nbsp;+ 38.92561&nbsp;<i>log</i><i>T</i>&nbsp;&minus; 563713.9/<i>T</i><sup>2</sup>&nbsp;which may be used to at least 250&deg;C. These expressions hold for 1 atm. total pressure between 0 and 100&deg;C and follow the vapor pressure curve of water at higher temperatures.</p>\n<p>Extensive measurements of the pH of Ca-HCO<sub>3</sub>&nbsp;solutions at 25&deg;C and 0.956 atm PCO<sub>2</sub>&nbsp;using different compositions of the reference electrode filling solution show that measured differences in pH are closely approximated by differences in liquid-junction potential as calculated by the Henderson equation. Liquid-junction corrected pH measurements agree with the calculated pH within 0.003-0.011 pH.</p>\n<p>Earlier arguments suggesting that the CaHCO<sup>+</sup><sub>3</sub>&nbsp;ion pair should not be included in the CaCO<sub>3</sub>-CO<sub>2</sub>-H<sub>2</sub>O aqueous model were based on less accurate calcite solubility data. The CaHCO<sup>+</sup><sub>3</sub>&nbsp;ion pair must be included in the aqueous model to account for the observed PCO<sub>2</sub>-dependence of aragonite solubility between 317 ppm CO<sub>2</sub>&nbsp;and 100% CO<sub>2</sub>.</p>\n<p>Previous literature on the solubility of CaCO<sub>3</sub>&nbsp;polymorphs have been critically evaluated using the aqueous model and the results are compared.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geochimica et Cosmochimica Acta","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/0016-7037(82)90056-4","issn":"00167037","usgsCitation":"Plummer, N., and Busenberg, E., 1982, The solubilities of calcite, aragonite and vaterite in CO2-H2O solutions between 0 and 90°C, and an evaluation of the aqueous model for the system CaCO3-CO2-H2O: Geochimica et Cosmochimica Acta, v. 46, no. 6, p. 1011-1040, https://doi.org/10.1016/0016-7037(82)90056-4.","startPage":"1011","endPage":"1040","numberOfPages":"30","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":220722,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb03ee4b08c986b324d14","contributors":{"authors":[{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":361964,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Busenberg, Eurybiades ebusenbe@usgs.gov","contributorId":2271,"corporation":false,"usgs":true,"family":"Busenberg","given":"Eurybiades","email":"ebusenbe@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":361963,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70137336,"text":"70137336 - 1982 - Current-induced sediment movement in the deep Florida Straits: Observations","interactions":[],"lastModifiedDate":"2017-08-24T12:59:56","indexId":"70137336","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Current-induced sediment movement in the deep Florida Straits: Observations","docAbstract":"<p>No abstract available</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The dynamic environment of the ocean floor","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Lexington Books","publisherLocation":"Lexington, MA","usgsCitation":"Wimbush, M., Nemeth, L., and Birdsall, B., 1982, Current-induced sediment movement in the deep Florida Straits: Observations, chap. <i>of</i> The dynamic environment of the ocean floor, p. 77-94.","productDescription":"18 p.","startPage":"77","endPage":"94","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":297049,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Florida Straits","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.44091796875,\n              22.59372606392931\n            ],\n            [\n              -84.44091796875,\n              30.713503990354965\n            ],\n            [\n              -77.98095703125,\n              30.713503990354965\n            ],\n            [\n              -77.98095703125,\n              22.59372606392931\n            ],\n            [\n              -84.44091796875,\n              22.59372606392931\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54dd2b6ce4b08de9379b337e","contributors":{"editors":[{"text":"Fanning, Kent A.","contributorId":138529,"corporation":false,"usgs":false,"family":"Fanning","given":"Kent","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":537747,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Manheim, Frank T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":45294,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank T.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":537748,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Wimbush, Mark","contributorId":138530,"corporation":false,"usgs":false,"family":"Wimbush","given":"Mark","email":"","affiliations":[],"preferred":false,"id":537749,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nemeth, Laszlo","contributorId":138531,"corporation":false,"usgs":false,"family":"Nemeth","given":"Laszlo","email":"","affiliations":[],"preferred":false,"id":537750,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Birdsall, Barton","contributorId":138532,"corporation":false,"usgs":false,"family":"Birdsall","given":"Barton","email":"","affiliations":[{"id":104,"text":"Alabama Cooperative Fish & Wildlife Unit","active":false,"usgs":true}],"preferred":false,"id":537751,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011604,"text":"70011604 - 1982 - Regional thermal-inertia mapping from an experimental satellite","interactions":[],"lastModifiedDate":"2024-04-18T16:34:53.386785","indexId":"70011604","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Regional thermal-inertia mapping from an experimental satellite","docAbstract":"<p><span>A new experimental satellite has provided, for the first time, thermal data that should be useful in reconnaissance geologic exploration. Thermal inertia, a property of geologic materials, can be mapped from these data by applying an algorithm that has been developed using a new thermal model. A simple registration procedure was used on a pair of day and night images of the Powder River basin, Wyoming, to illustrate the method. Preliminary assessment of these satellite data suggests that they will be of significant use for resource exploration when used in conjunction with other geologic, geophysical, and geochemical data.</span></p>","language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/1.1441317","issn":"00168033","usgsCitation":"Watson, K., 1982, Regional thermal-inertia mapping from an experimental satellite: Geophysics, v. 47, no. 12, p. 1681-1687, https://doi.org/10.1190/1.1441317.","productDescription":"7 p.","startPage":"1681","endPage":"1687","numberOfPages":"7","costCenters":[],"links":[{"id":220780,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"47","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e4a58ee4b0e8fec6cdbe67","contributors":{"authors":[{"text":"Watson, K.","contributorId":39123,"corporation":false,"usgs":true,"family":"Watson","given":"K.","email":"","affiliations":[],"preferred":false,"id":361524,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011536,"text":"70011536 - 1982 - Application of automated image analysis to coal petrography","interactions":[],"lastModifiedDate":"2024-02-24T01:39:00.168408","indexId":"70011536","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2033,"text":"International Journal of Coal Geology","active":true,"publicationSubtype":{"id":10}},"title":"Application of automated image analysis to coal petrography","docAbstract":"<div id=\"preview-section-abstract\"><div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"aep-abstract-id5\" class=\"abstract author\"><div id=\"aep-abstract-sec-id6\"><p>The coal petrologist seeks to determine the petrographic characteristics of organic and inorganic coal constituents and their lateral and vertical variations within a single coal bed or different coal beds of a particular coal field. Definitive descriptions of coal characteristics and coal facies provide the basis for interpretation of depositional environments, diagenetic changes, and burial history and determination of the degree of coalification or metamorphism. Numerous coal core or columnar samples must be studied in detail in order to adequately describe and define coal microlithotypes, lithotypes, and lithologic facies and their variations. The large amount of petrographic information required can be obtained rapidly and quantitatively by use of an automated image-analysis system (AIAS).</p><p>An AIAS can be used to generate quantitative megascopic and microscopic modal analyses for the lithologic units of an entire columnar section of a coal bed. In our scheme for megascopic analysis, distinctive bands 2 mm or more thick are first demarcated by visual inspection. These bands consist of either nearly pure microlithotypes or lithotypes such as vitrite/vitrain or fusite/fusain, or assemblages of microlithotypes. Megascopic analysis with the aid of the AIAS is next performed to determine volume percentages of vitrite, inertite, minerals, and microlithotype mixtures in bands 0.5 to 2 mm thick. The microlithotype mixtures are analyzed microscopically by use of the AIAS to determine their modal composition in terms of maceral and optically observable mineral components. Megascopic and microscopic data are combined to describe the coal unit quantitatively in terms of (V) for vitrite, (E) for liptite, (I) for inertite or fusite, (M) for mineral components other than iron sulfide, (S) for iron sulfide, and (VEIM) for the composition of the mixed phases (X<sub><i>i</i></sub>)<span>&nbsp;</span><i>i</i><span>&nbsp;</span>= 1,2, etc. in terms of the maceral groups vitrinite V, exinite E, inertinite I, and optically observable mineral content M. The volume percentage of each component present is indicated by a subscript. For example, a lithologic unit was determined megascopically to have the composition (V)<sub>13</sub>(I)<sub>1</sub>(S)<sub>1</sub>(X<sub>1</sub>)<sub>83</sub>(X<sub>2</sub>)<sub>2</sub>. After microscopic analysis of the mixed phases, this composition was expressed as (V)<sub>13</sub>(I)<sub>1</sub>(S)<sub>1</sub>(V<sub>63</sub>E<sub>19</sub>I<sub>14</sub>M<sub>4</sub>)<sub>83</sub>(V<sub>67</sub>E<sub>11</sub>I<sub>13</sub>M<sub>9</sub>)<sub>2</sub>. Finally, these data were combined in a description of the bulk composition as V<sub>67</sub>E<sub>16</sub>I<sub>13</sub>M<sub>3</sub>S<sub>1</sub>. An AIAS can also analyze textural characteristics and can be used for quick and reliable determination of rank (reflectance).</p><p>Our AIAS is completely software based and incorporates a television (TV) camera that has optimum response characteristics in the range of reflectance less than 5%, making it particularly suitable for coal studies. Analysis of the digitized signal from the TV camera is controlled by a microprocessor having a resolution of 64 gray levels between full illumination and dark current. The processed image is reconverted for display on a TV monitor screen, on which selection of phases or features to be analyzed is readily controlled and edited by the operator through use of a lightpen.</p><p>We expect that automated image analysis, because it can rapidly provide a large amount of pertinent information, will play a major role in the advancement of coal petrography.</p></div></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0166-5162(82)90002-7","issn":"01665162","usgsCitation":"Chao, E.C., Minkin, J., and Thompson, C., 1982, Application of automated image analysis to coal petrography: International Journal of Coal Geology, v. 2, no. 2, p. 113-150, https://doi.org/10.1016/0166-5162(82)90002-7.","productDescription":"38 p.","startPage":"113","endPage":"150","numberOfPages":"38","costCenters":[],"links":[{"id":220777,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ec96e4b0c8380cd49376","contributors":{"authors":[{"text":"Chao, E. C. T.","contributorId":96713,"corporation":false,"usgs":true,"family":"Chao","given":"E.","email":"","middleInitial":"C. T.","affiliations":[],"preferred":false,"id":361350,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Minkin, J.A.","contributorId":38588,"corporation":false,"usgs":true,"family":"Minkin","given":"J.A.","affiliations":[],"preferred":false,"id":361349,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thompson, C.L.","contributorId":12189,"corporation":false,"usgs":true,"family":"Thompson","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":361348,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011694,"text":"70011694 - 1982 - Siderite concretions: indicators of early diagenesis in the Gammon shale (Cretaceous).","interactions":[],"lastModifiedDate":"2012-03-12T17:18:27","indexId":"70011694","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2450,"text":"Journal of Sedimentary Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Siderite concretions: indicators of early diagenesis in the Gammon shale (Cretaceous).","docAbstract":"The Gammon member of the Pierre shale of the northern Great Plains, USA, contains abundant siderite concretions. The relative depth and time of siderite precipitation can be inferred from the structure, mineralogy and isotopic composition of these concretions. Concretions that formed at shallow depths, early in the history of the sediment, contain a high percentage (75-85%) of carbonate, preserve uncompacted structures and have oxygen isotopic ratios similar to that of sea-water. In contrast, concretions that formed later and/or at greater depths have lower carbonate content and lower 18O/16O ratios. Concretions in rapidly deposited sediments formed at shallow depths (<10 m), and those in sediments that accumulated slowly formed at greater depths. These differences agree with the fossil evidence. Siderite did not form until nearly all the dissolved sulphur had been reduced and precipitated as pyrite; the excess organic matter produced methane at about the same time.-H.R.B.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Sedimentary Petrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00224472","usgsCitation":"Gautier, D.L., 1982, Siderite concretions: indicators of early diagenesis in the Gammon shale (Cretaceous).: Journal of Sedimentary Petrology, v. 52, no. 3, p. 859-871.","startPage":"859","endPage":"871","numberOfPages":"13","costCenters":[],"links":[{"id":221127,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"52","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8ef2e4b08c986b318c3e","contributors":{"authors":[{"text":"Gautier, D. L.","contributorId":69996,"corporation":false,"usgs":true,"family":"Gautier","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":361729,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011736,"text":"70011736 - 1982 - Storage, migration, and eruption of magma at Kilauea volcano, Hawaii, 1971-1972","interactions":[],"lastModifiedDate":"2012-03-12T17:18:32","indexId":"70011736","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"Storage, migration, and eruption of magma at Kilauea volcano, Hawaii, 1971-1972","docAbstract":"The magmatic plumbing system of Kilauea Volcano consists of a broad region of magma generation in the upper mantle, a steeply inclined zone through which magma rises to an intravolcano reservoir located about 2 to 6 km beneath the summit of the volcano, and a network of conduits that carry magma from this reservoir to sites of eruption within the caldera and along east and southwest rift zones. The functioning of most parts of this system was illustrated by activity during 1971 and 1972. When a 29-month-long eruption at Mauna Ulu on the east rift zone began to wane in 1971, the summit region of the volcano began to inflate rapidly; apparently, blockage of the feeder conduit to Mauna Ulu diverted a continuing supply of mantle-derived magma to prolonged storage in the summit reservoir. Rapid inflation of the summit area persisted at a nearly constant rate from June 1971 to February 1972, when a conduit to Mauna Ulu was reopened. The cadence of inflation was twice interrupted briefly, first by a 10-hour eruption in Kilauea Caldera on 14 August, and later by an eruption that began in the caldera and migrated 12 km down the southwest rift zone between 24 and 29 September. The 14 August and 24-29 September eruptions added about 107 m3 and 8 ?? 106 m3, respectively, of new lava to the surface of Kilauea. These volumes, combined with the volume increase represented by inflation of the volcanic edifice itself, account for an approximately 6 ?? 106 m3/month rate of growth between June 1971 and January 1972, essentially the same rate at which mantle-derived magma was supplied to Kilauea between 1952 and the end of the Mauna Ulu eruption in 1971. The August and September 1971 lavas are tholeiitic basalts of similar major-element chemical composition. The compositions can be reproduced by mixing various proportions of chemically distinct variants of lava that erupted during the preceding activity at Mauna Ulu. Thus, part of the magma rising from the mantle to feed the Mauna Ulu eruption may have been stored within the summit reservoir from 4 to 20 months before it was erupted in the summit caldera and along the southwest rift zone in August and September. The September 1971 activity was only the fourth eruption on the southwest rift zone during Kilauea's 200 years of recorded history, in contrast to more than 20 eruptions on the east rift zone. Order-of-magnitude differences in topographic and geophysical expression indicate greatly disparate eruption rates for far more than historic time and thus suggest a considerably larger dike swarm within the east rift zone than within the southwest rift zone. Characteristics of the historic eruptions on the southwest rift zone suggest that magma may be fed directly from active lava lakes in Kilauea Caldera or from shallow cupolas at the top of the summit magma reservoir, through fissures that propagate down rift from the caldera itself at the onset of eruption. Moreover, emplacement of this magma into the southwest rift zone may be possible only when compressive stress across the rift is reduced by some unknown critical amount owing either to seaward displacement of the terrane south-southeast of the rift zone or to a deflated condition of Mauna Loa Volcano adjacent to the northwest, or both. The former condition arises when the forceful emplacement of dikes into the east rift zone wedges the south flank of Kilauea seaward. Such controls on the potential for eruption along the southwest rift zone may be related to the topographic and geophysical constrasts between the two rift zones. ?? 1982.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03770273","usgsCitation":"Duffield, W.A., Christiansen, R., Koyanagi, R.Y., and Peterson, D.W., 1982, Storage, migration, and eruption of magma at Kilauea volcano, Hawaii, 1971-1972: Journal of Volcanology and Geothermal Research, v. 13, no. 3-4, p. 273-307.","startPage":"273","endPage":"307","numberOfPages":"35","costCenters":[],"links":[{"id":220720,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9874e4b08c986b31c045","contributors":{"authors":[{"text":"Duffield, W. A.","contributorId":71935,"corporation":false,"usgs":true,"family":"Duffield","given":"W.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":361840,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Christiansen, R.L. 0000-0002-8017-3918","orcid":"https://orcid.org/0000-0002-8017-3918","contributorId":25565,"corporation":false,"usgs":true,"family":"Christiansen","given":"R.L.","affiliations":[],"preferred":false,"id":361838,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Koyanagi, R. Y.","contributorId":35719,"corporation":false,"usgs":true,"family":"Koyanagi","given":"R.","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":361839,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Peterson, D. W.","contributorId":84326,"corporation":false,"usgs":true,"family":"Peterson","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":361841,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70011804,"text":"70011804 - 1982 - Unary and binary multisystems: Topologic classification of phase diagrams and relation to Euler's theorem on polyhedra","interactions":[],"lastModifiedDate":"2023-02-08T17:47:39.604216","indexId":"70011804","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":732,"text":"American Journal of Science","active":true,"publicationSubtype":{"id":10}},"title":"Unary and binary multisystems: Topologic classification of phase diagrams and relation to Euler's theorem on polyhedra","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Journal of Science","doi":"10.2475/ajs.282.3.286","usgsCitation":"Roseboom, E.H., and Zen, E., 1982, Unary and binary multisystems: Topologic classification of phase diagrams and relation to Euler's theorem on polyhedra: American Journal of Science, v. 282, no. 3, p. 286-310, https://doi.org/10.2475/ajs.282.3.286.","productDescription":"25 p.","startPage":"286","endPage":"310","numberOfPages":"25","costCenters":[],"links":[{"id":480264,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2475/ajs.282.3.286","text":"Publisher Index Page"},{"id":220997,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"282","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbc11e4b08c986b3289f8","contributors":{"authors":[{"text":"Roseboom, E. H. Jr.","contributorId":40730,"corporation":false,"usgs":true,"family":"Roseboom","given":"E.","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":361993,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zen, E-An","contributorId":47064,"corporation":false,"usgs":true,"family":"Zen","given":"E-An","email":"","affiliations":[],"preferred":false,"id":361994,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011346,"text":"70011346 - 1982 - Post-depositional alteration of titanomagnetite in a Miocene sandstone, south Texas (U.S.A.)","interactions":[],"lastModifiedDate":"2023-12-12T23:20:24.905181","indexId":"70011346","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Post-depositional alteration of titanomagnetite in a Miocene sandstone, south Texas (U.S.A.)","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"ab1\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id3\"><p>Petrographic and geochemical studies have yielded information on the time-space relationships of the post-depositional alteration of detrital titanomagnetite (Ti-mt) in fine- to medium-grained sandstone from unoriented core samples (taken below the water table at depths of 30–45 m) of the Miocene Catahoula Sandstone, south Texas. Aqueous sulfide introduced from sour gas reservoirs along a growth fault into part of the Catahoula shortly after deposition resulted in the replacement at the periphery of Ti-mt grains by iron disulfide (FeS<sub>2</sub>) minerals. Remnants of Ti-mt in cores of the partly sulfidized grains show no evidence of earlier hematitic oxidation. After sulfidization, part of the sandstone body was invaded by oxygenated groundwaters flowing down a shallowly inclined (1°) hydrologic gradient. The boundary between oxidized and reduced facies is clearly defined by the distribution of ferric and ferrous iron minerals, and the concentrations of Mo, U, and Se. In oxidized (light-red) strata that had not been previously subjected to sulfidic-reducing conditions but that are correlative with strata containing FeS<sub>2</sub><span>&nbsp;</span>minerals, Ti-mt has been partly to entirely replaced pseudomorphously by hematite to form martite. The absence of hematitic alteration of Ti-mt in the reduced facies is strong evidence that martite in the oxidized facies formed after deposition.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(82)90068-1","issn":"0012821X","usgsCitation":"Reynolds, R.L., 1982, Post-depositional alteration of titanomagnetite in a Miocene sandstone, south Texas (U.S.A.): Earth and Planetary Science Letters, v. 61, no. 2, p. 381-391, https://doi.org/10.1016/0012-821X(82)90068-1.","productDescription":"11 p.","startPage":"381","endPage":"391","numberOfPages":"11","costCenters":[],"links":[{"id":220899,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -100.72139192813091,\n              29.418408283078875\n            ],\n            [\n              -100.72139192813091,\n              25.837329072246007\n            ],\n            [\n              -96.50264192813093,\n              25.837329072246007\n            ],\n            [\n              -96.50264192813093,\n              29.418408283078875\n            ],\n            [\n              -100.72139192813091,\n              29.418408283078875\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"61","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7e5fe4b0c8380cd7a4d6","contributors":{"authors":[{"text":"Reynolds, R. L. 0000-0002-4572-2942","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":79885,"corporation":false,"usgs":true,"family":"Reynolds","given":"R.","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":360885,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011633,"text":"70011633 - 1982 - Modern shallow-water graded sand layers from storm surges, Bering Shelf: a mimic of Bouma sequences and turbidite systems","interactions":[],"lastModifiedDate":"2024-05-21T23:50:16.941879","indexId":"70011633","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2450,"text":"Journal of Sedimentary Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Modern shallow-water graded sand layers from storm surges, Bering Shelf: a mimic of Bouma sequences and turbidite systems","docAbstract":"<div><div id=\"12458278\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>A sequence of graded sand layers, interbedded with mud, extends offshore over 100 km from the Yukon Delta shoreline across the flat, shallow (&lt;20 m depth) epicontinental shelf of the northern Bering Sea, Alaska. Proximal graded sand beds on the delta-front platform near the shoreline are coarser (2-3phi ), thicker (10 to 20 cm), and contain more complete vertical sequences of sedimentary structures than distal beds. The inshore graded vertical sequence of structures from the base to the top of individual sand layers includes plane-parallel lamination (S<span>&nbsp;</span><sub>b</sub><span>&nbsp;</span>), cross lamination (S<span>&nbsp;</span><sub>c</sub><span>&nbsp;</span>), plane-parallel lamination (S<span>&nbsp;</span><sub>d</sub><span>&nbsp;</span>), and mud (S<span>&nbsp;</span><sub>e</sub><span>&nbsp;</span>) analogous to the Bouma T (sub a-e) turbidite sequence. Structures vary between interchannel platform deposits with complete S<span>&nbsp;</span><sub>b</sub><span>&nbsp;</span>-S<span>&nbsp;</span><sub>e</sub><span>&nbsp;</span>sequences and channel-floor sands that are all trough cross-laminated. Distally, storm-sand layers change to thin (1 to 5 cm) silt beds that contain flat and ripple-drift lamination (S (sub c-e,de) ), are commonly bioturbated, and are associated with shell and pebble lags from storm-wave reworking. The sequence of graded sands appears to be related to the major storm surges that occur every several years. The major storms increase the average 10-m water depth in southern Norton Sound as much as 5 m and cause fluctuations in pore pressure from wave cyclic loading that may liquefy the upper 2 to 3 m of sediment. Storm-associated bottom currents, possibly dominated by rapidly waning ebb flow, transport the liquefied inshore sand far offshore (&gt; 100 kin). Such shallow-water graded layers off lobate deltas may be distinguished from similar deep-water turbidites by: 1) the predominance of trough cross-lamination, perhaps resulting from wave oscillation effects, in the proximal part of the system, and 2) gradation to common shallow marine fossils, bioturbation, and storm lag layers in distal areas.</p></div></div>","language":"English","publisher":"SEPM","doi":"10.1306/212F7F9A-2B24-11D7-8648000102C1865D","issn":"00224472","usgsCitation":"Nelson, C., 1982, Modern shallow-water graded sand layers from storm surges, Bering Shelf: a mimic of Bouma sequences and turbidite systems: Journal of Sedimentary Petrology, v. 52, no. 2, p. 537-545, https://doi.org/10.1306/212F7F9A-2B24-11D7-8648000102C1865D.","productDescription":"9 p.","startPage":"537","endPage":"545","numberOfPages":"9","costCenters":[],"links":[{"id":221188,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"52","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5ca1e4b0c8380cd6fe37","contributors":{"authors":[{"text":"Nelson, C.H.","contributorId":88346,"corporation":false,"usgs":true,"family":"Nelson","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":361582,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010416,"text":"70010416 - 1982 - Gamma-emitting radionuclide measurements at the US geological survey national water quality laboratory, Denver, Colorado","interactions":[],"lastModifiedDate":"2012-03-12T17:18:17","indexId":"70010416","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2906,"text":"Nuclear Instruments and Methods","active":true,"publicationSubtype":{"id":10}},"title":"Gamma-emitting radionuclide measurements at the US geological survey national water quality laboratory, Denver, Colorado","docAbstract":"Like sediment samples from Scofield Resevior in Utah were analyzed for 210Pb by the gamma-ray spectrometric method. The top 10 cm of surface sediment yielded excess 210Pb activity (excluding in situ 226Ra supported 210Pb) of 1.05 pCi/g dry weight and decreased to 0.25 pCi/g at a depth of 25 cm. Based on these data, sedimentation rate was approximately 0.49 cm/y for a total of 30 cm of lake sediment and a lake history of approximately 60 y. An alternative method of 210Pb measurements using wet chemical procedures followed by beta counting gave equivalent results. ?? 1982.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Nuclear Instruments and Methods","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"0029554X","usgsCitation":"In, C.Y., and Ambats, E., 1982, Gamma-emitting radionuclide measurements at the US geological survey national water quality laboratory, Denver, Colorado: Nuclear Instruments and Methods, v. 193, no. 1-2, p. 197-201.","startPage":"197","endPage":"201","numberOfPages":"5","costCenters":[],"links":[{"id":219374,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"193","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a14b2e4b0c8380cd54b04","contributors":{"authors":[{"text":"In, Che Yang","contributorId":39934,"corporation":false,"usgs":true,"family":"In","given":"Che","email":"","middleInitial":"Yang","affiliations":[],"preferred":false,"id":358869,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ambats, E.","contributorId":23270,"corporation":false,"usgs":true,"family":"Ambats","given":"E.","email":"","affiliations":[],"preferred":false,"id":358868,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1013897,"text":"1013897 - 1982 - A review of pond zooplankton production and fertilization for the culture of larval and fingerling striped bass","interactions":[],"lastModifiedDate":"2023-08-09T14:55:10.472023","indexId":"1013897","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":853,"text":"Aquaculture","active":true,"publicationSubtype":{"id":10}},"title":"A review of pond zooplankton production and fertilization for the culture of larval and fingerling striped bass","docAbstract":"<div id=\"preview-section-abstract\"><div id=\"abstracts\" class=\"Abstracts u-font-gulliver text-s\"><div id=\"aep-abstract-id3\" class=\"abstract author\"><div id=\"aep-abstract-sec-id4\"><p>Successful culture of the planktivorous fry of warmwater fish species such as striped bass (<i>Morone saxatilis</i>) depends heavily upon the composition and density of zooplankton established in rearing ponds during the 4–6-week culture period. The paper reviews the growth, reproduction, and succession patterns of zooplankton in ponds, organic and inorganic pond fertilization, and predator—prey relationships as they relate to the culture of striped bass fingerlings. Based upon this information, a pond management strategy is proposed using combinations of organic and liquid inorganic fertilizers and crustacean zooplankton inoculation to develop and maintain the zooplankton forage base in striped bass rearing ponds.</p></div></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0044-8486(83)90106-0","usgsCitation":"Geiger, J.G., 1982, A review of pond zooplankton production and fertilization for the culture of larval and fingerling striped bass: Aquaculture, v. 35, no. 4, p. 353-369, https://doi.org/10.1016/0044-8486(83)90106-0.","productDescription":"17 p.","startPage":"353","endPage":"369","numberOfPages":"17","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132016,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"35","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8002","contributors":{"authors":[{"text":"Geiger, J. G.","contributorId":29340,"corporation":false,"usgs":true,"family":"Geiger","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":319411,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011558,"text":"70011558 - 1982 - Biostratigraphy and paleoenvironment of Miocene- Pliocene hemipelagic limestone: Kingshill Seaway, St. Croix, US Virgin Islands.","interactions":[],"lastModifiedDate":"2013-03-24T12:14:36","indexId":"70011558","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2294,"text":"Journal of Foraminiferal Research","active":true,"publicationSubtype":{"id":10}},"title":"Biostratigraphy and paleoenvironment of Miocene- Pliocene hemipelagic limestone: Kingshill Seaway, St. Croix, US Virgin Islands.","docAbstract":"The Kingshill Limestone and younger carbonate rocks constitute the central portion of St. Croix, forming the remains of an ancient seaway that was flanked by emergent highlands. The seaway has been filled with thick epipelagic sediments alternating with carbonate turbidites and ash falls and capped with shallow-water reefal and terrigenous debris. Planktonic foraminifera indicate that ages of these rocks range sequentially in a SW direction from the middle Miocene to lower Pliocene. Scanning electron micrographs illustrate 42 species and subspecies of pelagic foraminifera and 13 selected paleoenvironmentally significant aberrant forms.-from Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Foraminiferal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.2113/gsjfr.12.3.205","issn":"00961191","usgsCitation":"Lidz, B.H., 1982, Biostratigraphy and paleoenvironment of Miocene- Pliocene hemipelagic limestone: Kingshill Seaway, St. Croix, US Virgin Islands.: Journal of Foraminiferal Research, v. 12, no. 3, p. 205-233, https://doi.org/10.2113/gsjfr.12.3.205.","startPage":"205","endPage":"233","numberOfPages":"29","costCenters":[],"links":[{"id":269900,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2113/gsjfr.12.3.205"},{"id":221121,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f19be4b0c8380cd4ad2a","contributors":{"authors":[{"text":"Lidz, B. H.","contributorId":30651,"corporation":false,"usgs":true,"family":"Lidz","given":"B.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":361402,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011229,"text":"70011229 - 1982 - Obtaining maps and data from the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2023-09-21T16:24:00.08603","indexId":"70011229","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1317,"text":"Computers, Environment and Urban Systems","active":true,"publicationSubtype":{"id":10}},"title":"Obtaining maps and data from the U.S. Geological Survey","docAbstract":"<p><span>The U.S. Geological Survey produces a variety of resource information for the United States. This includes many data bases of particular interest to planners such as land use and terrain information prepared by the National Mapping Division, water quantity and quality data collected by Water Resources Division, and coal resource information gathered by the Geologic Division. These data are stored in various forms, and information on their availability can be obtained from appropriate offices in the U.S. Geological Survey as well as from USGS Circular 777. These data have been used for the management, development, and monitoring of our Nation's resources by Federal, State, and local agencies.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0198-9715(82)90016-3","usgsCitation":"Hallam, C.A., 1982, Obtaining maps and data from the U.S. Geological Survey: Computers, Environment and Urban Systems, v. 7, no. 4, p. 283-294, https://doi.org/10.1016/0198-9715(82)90016-3.","productDescription":"12 p.","startPage":"283","endPage":"294","numberOfPages":"12","costCenters":[],"links":[{"id":221032,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6b0ee4b0c8380cd744c6","contributors":{"authors":[{"text":"Hallam, Cheryl A.","contributorId":59012,"corporation":false,"usgs":true,"family":"Hallam","given":"Cheryl","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":360619,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010435,"text":"70010435 - 1982 - Automated standardization technique for an inductively-coupled plasma emission spectrometer","interactions":[],"lastModifiedDate":"2023-03-07T16:33:07.780652","indexId":"70010435","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":760,"text":"Analytica Chimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Automated standardization technique for an inductively-coupled plasma emission spectrometer","docAbstract":"<p><span>The manifold assembly subsystem described permits real-time computer-controlled standardization and quality control of a commercial inductively-coupled plasma atomic emission spectrometer. The manifold assembly consists of a branch-structured glass manifold, a series of microcomputer-controlled solenoid valves, and a reservoir for each standard. Automated standardization involves selective actuation of each solenoid valve that permits a specific mixed standard solution to be pumped to the nebulizer of the spectrometer. Quality control is based on the evaluation of results obtained for a mixed standard containing 17 analytes, that is measured periodically with unknown samples. An inaccurate standard evaluation triggers restandardization of the instrument according to a predetermined protocol. Interaction of the computer-controlled manifold assembly hardware with the spectrometer system is outlined. Evaluation of the automated standardization system with respect to reliability, simplicity, flexibility, and efficiency is compared to the manual procedure.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0003-2670(01)84186-6","usgsCitation":"Garbarino, J.R., and Taylor, H.E., 1982, Automated standardization technique for an inductively-coupled plasma emission spectrometer: Analytica Chimica Acta, v. 134, no. C, p. 153-165, https://doi.org/10.1016/S0003-2670(01)84186-6.","productDescription":"13 p.","startPage":"153","endPage":"165","numberOfPages":"13","costCenters":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":5046,"text":"Branch of Analytical Serv (NWQL)","active":true,"usgs":true}],"links":[{"id":219690,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"134","issue":"C","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059eef6e4b0c8380cd4a087","contributors":{"authors":[{"text":"Garbarino, John R. jrgarb@usgs.gov","contributorId":2189,"corporation":false,"usgs":true,"family":"Garbarino","given":"John","email":"jrgarb@usgs.gov","middleInitial":"R.","affiliations":[{"id":5046,"text":"Branch of Analytical Serv (NWQL)","active":true,"usgs":true}],"preferred":true,"id":358923,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, Howard E. hetaylor@usgs.gov","contributorId":1551,"corporation":false,"usgs":true,"family":"Taylor","given":"Howard","email":"hetaylor@usgs.gov","middleInitial":"E.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":358922,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011560,"text":"70011560 - 1982 - Late Eocene- Oligocene magnetostratigraphy and biostratigraphy at South Atlantic DSDP site 522","interactions":[],"lastModifiedDate":"2024-02-01T11:59:47.73662","indexId":"70011560","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Late Eocene- Oligocene magnetostratigraphy and biostratigraphy at South Atlantic DSDP site 522","docAbstract":"<div id=\"15565064\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>Upper Eocene to lowest Miocene sediments recovered at Deep Sea Drilling Project (DSDP) Site 522 in the South Atlantic Ocean allow direct calibration of magnetostratigraphy and calcareous plankton biostratigraphy. The results from Site 522 show that the Eocene/Oligocene boundary occurs in the reversed interval of magnetic Chron C13 (= C13R) and that the Oligocene/IMiocene boundary probably occurs in the upper part of Chron C6C.</p></div>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1982)10<508:LEMABA>2.0.CO;2","issn":"00917613","usgsCitation":"Poore, R., Tauxe, L., Percival, S., and LaBrecque, J.L., 1982, Late Eocene- Oligocene magnetostratigraphy and biostratigraphy at South Atlantic DSDP site 522: Geology, v. 10, no. 10, p. 508-511, https://doi.org/10.1130/0091-7613(1982)10<508:LEMABA>2.0.CO;2.","productDescription":"4 p.","startPage":"508","endPage":"511","numberOfPages":"4","costCenters":[],"links":[{"id":221180,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a44e1e4b0c8380cd66e79","contributors":{"authors":[{"text":"Poore, R.Z.","contributorId":35314,"corporation":false,"usgs":true,"family":"Poore","given":"R.Z.","email":"","affiliations":[],"preferred":false,"id":361405,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tauxe, L.","contributorId":53522,"corporation":false,"usgs":true,"family":"Tauxe","given":"L.","affiliations":[],"preferred":false,"id":361406,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Percival, S.F. Jr.","contributorId":105852,"corporation":false,"usgs":true,"family":"Percival","given":"S.F.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":361407,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"LaBrecque, John L.","contributorId":31113,"corporation":false,"usgs":true,"family":"LaBrecque","given":"John","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":361404,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70142169,"text":"70142169 - 1982 - Evaluating depth to shallow groundwater using Heat Capacity Mapping Mission (HCMM) data","interactions":[],"lastModifiedDate":"2017-01-18T14:51:34","indexId":"70142169","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Evaluating depth to shallow groundwater using Heat Capacity Mapping Mission (HCMM) data","docAbstract":"<p>Four dates of Heat Capacity Mapping Mission (HCMM) data were analyzed to evaluate the utility of HCMM thermal data for evaluating depth to shallow groundwater. During the summer, shallow water tables can create lower soil temperatures throughout the diurnal temperature cycle. Because of large spatial and temporal ground cover variations, HCMM daytime radiometric temperatures alone did not correlate with water table depth. The radiometric temperatures consisted of radiance contributions from different crop canopies and their respective soil backgrounds. However, when surface soil temperatures were empirically estimated from HCMM temperatures and percent cover of each pixel, significant correlations were obtained between estimated soil temperatures and water table depth. Correlations increased as the season progressed and temperature gradients within the soil profile increased. However, estimated soil temperatures were also correlated with near-surface soil moisture since during the daytime, increasing soil moisture reduced surface soil temperature. Complementary effects of shallow water tables and soil moisture on daytime temperatures cannot be separated.</p>","language":"English","publisher":"American Society for Photogrammetry and Remote Sensing","usgsCitation":"Heilman, J.L., and Moore, D.G., 1982, Evaluating depth to shallow groundwater using Heat Capacity Mapping Mission (HCMM) data: Photogrammetric Engineering and Remote Sensing, v. 48, no. 12, p. 1903-1906.","productDescription":"4 p.","startPage":"1903","endPage":"1906","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":298206,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"48","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54f597c7e4b02419550d2f42","contributors":{"authors":[{"text":"Heilman, J. L.","contributorId":85723,"corporation":false,"usgs":true,"family":"Heilman","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":541655,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, Donald G.","contributorId":41146,"corporation":false,"usgs":true,"family":"Moore","given":"Donald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":541656,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1000360,"text":"1000360 - 1982 - Decline of lake herring (<i>Coregonus artedii</i>) in Lake Superior: an analysis of the Wisconsin herring fishery, 1936-78","interactions":[],"lastModifiedDate":"2016-04-01T08:56:17","indexId":"1000360","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1169,"text":"Canadian Journal of Fisheries and Aquatic Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Decline of lake herring (<i>Coregonus artedii</i>) in Lake Superior: an analysis of the Wisconsin herring fishery, 1936-78","docAbstract":"<p><span>Annual harvests of lake herring (</span><i>Coregonus artedii</i><span>) in American waters of Lake Superior declined from an average of 2 million kg in 1936&ndash;62 to less than 25&ensp;000&ensp;kg in 1978. Analysis of commercial fishing records revealed that the sequential overexploitation of discrete unit stocks caused the collapse of the herring population in Wisconsin waters. In each of six major spawning areas, catch exceeded the productive capacity of the stock and the stock failed. Because stocks in the six areas were exploited sequentially, mostly in groups of two or three simultaneously, the demise of the stocks was not readily apparent until the last two failed in the early 1960s. After the collapse of the last major spawning stock, the fishery dwindled but may have continued to overexploit the remaining small stocks. The residual populations were apparently able only to replace themselves. Some form of density-independent mortality was apparently operating to prevent their recovery during the 1960s and 1970s.</span><i>Key words</i><span>: lake herring, overfishing, Lake Superior</span></p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/f82-079","usgsCitation":"Selgeby, J.H., 1982, Decline of lake herring (<i>Coregonus artedii</i>) in Lake Superior: an analysis of the Wisconsin herring fishery, 1936-78: Canadian Journal of Fisheries and Aquatic Sciences, v. 39, no. 4, p. 554-563, https://doi.org/10.1139/f82-079.","productDescription":"10 p.","startPage":"554","endPage":"563","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128957,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672716","contributors":{"authors":[{"text":"Selgeby, James H.","contributorId":89828,"corporation":false,"usgs":true,"family":"Selgeby","given":"James","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308451,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70170293,"text":"70170293 - 1982 - Sir William Hamilton; pioneer volcanologist","interactions":[],"lastModifiedDate":"2016-04-15T16:03:03","indexId":"70170293","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Sir William Hamilton; pioneer volcanologist","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Guest, J., 1982, Sir William Hamilton; pioneer volcanologist: Earthquake Information Bulletin (USGS), v. 14, no. 2, p. 48-55.","productDescription":"8 p.","startPage":"48","endPage":"55","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":320085,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"571210b8e4b0ef3b7ca64439","contributors":{"authors":[{"text":"Guest, J.","contributorId":168628,"corporation":false,"usgs":false,"family":"Guest","given":"J.","affiliations":[],"preferred":false,"id":626800,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1007583,"text":"1007583 - 1982 - Evaluation of the river die-away biodegradation test","interactions":[],"lastModifiedDate":"2017-05-15T20:08:11","indexId":"1007583","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2573,"text":"Journal of the Water Pollution Control Federation","active":true,"publicationSubtype":{"id":10}},"title":"Evaluation of the river die-away biodegradation test","docAbstract":"<p>The reliability of the river die-away (RDA) test for establishing the biodegradability of chemicals was assessed. Reproducibility of biodegradation in the RDA test was analyzed under conditions in which the test is commonly done. Biodegradation results were not reproducible for di-2-ethylexyl phthalate (DEHP) and phthalic acid in replicated RDA tests using Missouri River water. Chemical and biological changes during the RDA tests probably reflected relative laboratory conditions. Initial suspended solids and subsequent DEHP biodegradation were directly related. Interpretation of RDA test results is enhanced by replicating experiments and comparing biodegradation of the test compound with a compound whose degradation properties are known. However, biodegradation measured with the RDA test is too variable and too dependent on laboratory treatment of samples to apply results directly to the aquatic environment.</p>","language":"English","publisher":"Water Environment Federation","usgsCitation":"Wylie, G.D., Jones, J., and Johnson, B., 1982, Evaluation of the river die-away biodegradation test: Journal of the Water Pollution Control Federation, v. 54, no. 8, p. 1231-1236.","productDescription":"6 p.","startPage":"1231","endPage":"1236","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":129843,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269371,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/25041661"}],"volume":"54","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa25a","contributors":{"authors":[{"text":"Wylie, Glenn D. 0000-0002-7061-6658 glenn_wylie@usgs.gov","orcid":"https://orcid.org/0000-0002-7061-6658","contributorId":3052,"corporation":false,"usgs":true,"family":"Wylie","given":"Glenn","email":"glenn_wylie@usgs.gov","middleInitial":"D.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":315666,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, John R.","contributorId":48459,"corporation":false,"usgs":false,"family":"Jones","given":"John R.","affiliations":[{"id":6754,"text":"University of Missouri","active":true,"usgs":false}],"preferred":false,"id":315665,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnson, B. Thomas","contributorId":105101,"corporation":false,"usgs":true,"family":"Johnson","given":"B. Thomas","affiliations":[],"preferred":false,"id":315667,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}