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B.","contributorId":78039,"corporation":false,"usgs":true,"family":"Johnston","given":"James","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":781213,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnson, Craig 0000-0002-1334-2996","orcid":"https://orcid.org/0000-0002-1334-2996","contributorId":59714,"corporation":false,"usgs":true,"family":"Johnson","given":"Craig","affiliations":[],"preferred":false,"id":781214,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70205240,"text":"70205240 - 1993 - The use of geographic information system technology to compare the environmental impacts of human development on Mobile Bay, Alabama and Galveston Bay, Texas","interactions":[],"lastModifiedDate":"2019-09-10T14:57:43","indexId":"70205240","displayToPublicDate":"2019-12-31T12:54:41","publicationYear":"1993","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"title":"The use of geographic information system technology to compare the environmental impacts of human development on Mobile Bay, Alabama and Galveston Bay, Texas","docAbstract":"<p>No abstract available</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Coastal zone '93 - Proceedings of the eighth sysmposium on coastal and ocean management","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Coastal zone '93 - Eighth sysmposium on coastal and ocean management","conferenceDate":"July 19-23, 1993","conferenceLocation":"New Orleans, LA","language":"English","publisher":"American Society of Civil Engineers","isbn":"087262918X","usgsCitation":"Roscigno, P.F., McNiff, M., Watzin, M.C., and Ji, W., 1993, The use of geographic information system technology to compare the environmental impacts of human development on Mobile Bay, Alabama and Galveston Bay, Texas, <i>in</i> Coastal zone '93 - Proceedings of the eighth sysmposium on coastal and ocean management, New Orleans, LA, July 19-23, 1993, p. 825-837.","productDescription":"13 p.","startPage":"825","endPage":"837","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":367327,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alabama, Texas","otherGeospatial":"Galveston Bay, Mobile Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.21197509765624,\n              30.22822147272596\n            ],\n            [\n              -87.71759033203125,\n              30.22822147272596\n            ],\n            [\n              -87.71759033203125,\n              30.784317689718897\n            ],\n            [\n              -88.21197509765624,\n              30.784317689718897\n            ],\n            [\n              -88.21197509765624,\n              30.22822147272596\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.21575927734375,\n              29.30077105450428\n            ],\n            [\n              -94.44671630859375,\n              29.30077105450428\n            ],\n            [\n              -94.44671630859375,\n              29.816816857649936\n            ],\n            [\n              -95.21575927734375,\n              29.816816857649936\n            ],\n            [\n              -95.21575927734375,\n              29.30077105450428\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Roscigno, Pasquale F.","contributorId":214752,"corporation":false,"usgs":false,"family":"Roscigno","given":"Pasquale","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":770602,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McNiff, Marcia 0000-0003-0709-6992 mmcniff@usgs.gov","orcid":"https://orcid.org/0000-0003-0709-6992","contributorId":4025,"corporation":false,"usgs":true,"family":"McNiff","given":"Marcia","email":"mmcniff@usgs.gov","affiliations":[{"id":208,"text":"Core Science Analytics and Synthesis","active":true,"usgs":true}],"preferred":true,"id":770492,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Watzin, Mary C.","contributorId":214534,"corporation":false,"usgs":false,"family":"Watzin","given":"Mary","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":770493,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ji, Wei","contributorId":218024,"corporation":false,"usgs":false,"family":"Ji","given":"Wei","email":"","affiliations":[],"preferred":false,"id":770494,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70206414,"text":"70206414 - 1993 - The effects of habitat productivity on competition intensity","interactions":[],"lastModifiedDate":"2019-11-01T11:32:38","indexId":"70206414","displayToPublicDate":"2019-12-31T11:29:43","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3653,"text":"Trends in Ecology and Evolution","active":true,"publicationSubtype":{"id":10}},"title":"The effects of habitat productivity on competition intensity","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0169-5347(93)90194-T","usgsCitation":"Grace, J.B., 1993, The effects of habitat productivity on competition intensity: Trends in Ecology and Evolution, v. 8, no. 7, p. 229-230, https://doi.org/10.1016/0169-5347(93)90194-T.","productDescription":"2 p.","startPage":"229","endPage":"230","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":368882,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Grace, James B. 0000-0001-6374-4726 gracej@usgs.gov","orcid":"https://orcid.org/0000-0001-6374-4726","contributorId":884,"corporation":false,"usgs":true,"family":"Grace","given":"James","email":"gracej@usgs.gov","middleInitial":"B.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true},{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true},{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":774471,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70180649,"text":"70180649 - 1993 -  System-wide significance of predation on juvenile salmonids in the Columbia and Snake River reservoirs. Report of research, 1992","interactions":[],"lastModifiedDate":"2017-01-31T11:03:19","indexId":"70180649","displayToPublicDate":"2017-01-31T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":" System-wide significance of predation on juvenile salmonids in the Columbia and Snake River reservoirs. Report of research, 1992","docAbstract":"<p>No abstract available&nbsp;</p>","language":"English","publisher":"Bonneville Power Administration","publisherLocation":"Portland, OR","usgsCitation":"Petersen, H., and Poe, T., 1993,  System-wide significance of predation on juvenile salmonids in the Columbia and Snake River reservoirs. Report of research, 1992.","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":334430,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5891b0b9e4b072a7ac129940","contributors":{"authors":[{"text":"Petersen, H.","contributorId":178980,"corporation":false,"usgs":false,"family":"Petersen","given":"H.","email":"","affiliations":[],"preferred":false,"id":661880,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poe, T.P.","contributorId":51687,"corporation":false,"usgs":true,"family":"Poe","given":"T.P.","email":"","affiliations":[],"preferred":false,"id":661881,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70179974,"text":"70179974 - 1993 - Ground-water conditions in Utah, spring of 1993","interactions":[],"lastModifiedDate":"2017-01-20T15:10:41","indexId":"70179974","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":110,"text":"Cooperative Investigations Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"33","title":"Ground-water conditions in Utah, spring of 1993","docAbstract":"<p>This is the thirtieth in a series of annual reports that describe ground-water conditions in Utah. Reports in this series, published cooperatively by the U.S. Geological Survey and the Utah Division of Water Resources, provide data to enable interested parties to keep abreast of changing ground-water conditions.</p><p>This report, like the others in the series, contains information on well construction, ground-water withdrawal from wells, water-level changes, related changes in precipitation and streamflow, and chemical quality of water. Supplementary data, such as maps showing water-level contours, are included in reports of this series only for those years or areas for which applicable data are available and are important to a discussion of changing ground-water conditions.</p><p>This report includes individual discussions of selected major areas of ground-water development in the State for the calendar year 1992. Water-level fluctuations and selected related data, however, are described from the spring of 1988 to the spring of 1993. Much of the data used in this report were collected by the U.S. Geological Survey in cooperation with the Divisions of Water Rights and Water Resources, Utah Department of Natural Resources.</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Resources","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the State of Utah, Division of Water Resources and Division of Water Rights","usgsCitation":"Batty, D., Allen, D., Sory, J., Hanson, K., Thomas, W., Greene, M., Danner, M., Herbert, L.R., Hadley, H., Gerner, S., Slaugh, B., Swenson, R., Howells, J., and Christiansen, H., 1993, Ground-water conditions in Utah, spring of 1993: Cooperative Investigations Report 33, x, 106 p.","productDescription":"x, 106 p.","numberOfPages":"116","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333630,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333628,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-172"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5883303be4b0d0023163781a","contributors":{"authors":[{"text":"Batty, D.M.","contributorId":178513,"corporation":false,"usgs":false,"family":"Batty","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":659393,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allen, D.V.","contributorId":6129,"corporation":false,"usgs":true,"family":"Allen","given":"D.V.","email":"","affiliations":[],"preferred":false,"id":659394,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sory, J.D.","contributorId":178510,"corporation":false,"usgs":false,"family":"Sory","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":659395,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hanson, K.M.","contributorId":83557,"corporation":false,"usgs":true,"family":"Hanson","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":659396,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Thomas, W.J.","contributorId":178518,"corporation":false,"usgs":false,"family":"Thomas","given":"W.J.","email":"","affiliations":[],"preferred":false,"id":659397,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Greene, M.R.","contributorId":96723,"corporation":false,"usgs":true,"family":"Greene","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":659398,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Danner, M.R.","contributorId":178514,"corporation":false,"usgs":false,"family":"Danner","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":659399,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Herbert, L. R.","contributorId":39865,"corporation":false,"usgs":true,"family":"Herbert","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":659400,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Hadley, H.K.","contributorId":61086,"corporation":false,"usgs":true,"family":"Hadley","given":"H.K.","email":"","affiliations":[],"preferred":false,"id":659401,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Gerner, S.J.","contributorId":16083,"corporation":false,"usgs":true,"family":"Gerner","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":659402,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Slaugh, B.A.","contributorId":178515,"corporation":false,"usgs":false,"family":"Slaugh","given":"B.A.","affiliations":[],"preferred":false,"id":659403,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Swenson, R.L.","contributorId":178508,"corporation":false,"usgs":false,"family":"Swenson","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":659404,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Howells, J.H.","contributorId":178516,"corporation":false,"usgs":false,"family":"Howells","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":659405,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Christiansen, H.K.","contributorId":178517,"corporation":false,"usgs":false,"family":"Christiansen","given":"H.K.","email":"","affiliations":[],"preferred":false,"id":659406,"contributorType":{"id":1,"text":"Authors"},"rank":14}]}}
,{"id":70179663,"text":"70179663 - 1993 - Acid Rain","interactions":[],"lastModifiedDate":"2017-01-19T14:35:19","indexId":"70179663","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":806,"text":"Annual Review of Earth and Planetary Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Acid Rain","docAbstract":"<p>Acid deposition, or acid rain as it is more commonly referred to, has become a widely publicized environmental issue in the U.S. over the past decade. The term usually conjures up images of fish kills, dying forests, \"dead\" lakes, and damage to monuments and other historic artifacts. The primary cause of acid deposition is emission of S0<sub>2</sub> and NO<sub>x</sub> to the atmosphere during the combustion of fossil fuels. Oxidation of these compounds in the atmosphere forms strong acids - H<sub>2</sub>SO<sub>4</sub> and HNO<sub>3</sub> -&nbsp;which are returned to the Earth in rain, snow, fog, cloud water, and as dry deposition.</p><p>Although acid deposition has only recently been recognized as an environmental problem in the U.S., it is not a new phenomenon (Cogbill &amp; Likens 1974). As early as the middle of the 17th century in England, the deleterious effects of industrial emissions on plants, animals, and humans, and the atmospheric transport of pollutants between England and France had become issues of concern (Evelyn 1661, Graunt 1662). It is interesting that well over three hundred years ago in England, recommendations were made to move industry outside of towns and build higher chimneys to spread the pollution into \"distant parts.\" Increasing the height of smokestacks has helped alleviate local problems, but has exacerbated others. In the U.S. the height of the tallest smokestack has more than doubled, and the average height of smokestacks has tripled since the 1950s (Patrick et al 1981). This trend occurred in most industrialized nations during the 20th century and has had the effect of transforming acid rain from a local urban problem into a problem of global scale.  </p>","language":"English","publisher":"Annual Reviews","doi":"10.1146/annurev.ea.21.050193.001055","usgsCitation":"Bricker, O.P., and Rice, K.C., 1993, Acid Rain: Annual Review of Earth and Planetary Sciences, v. 21, no. 1, p. 151-174, https://doi.org/10.1146/annurev.ea.21.050193.001055.","productDescription":"24 p.","startPage":"151","endPage":"174","costCenters":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"links":[{"id":333026,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333079,"rank":2,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/70179669","text":"Article republished in a compilation"}],"volume":"21","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58760117e4b04eac8e0746ed","contributors":{"authors":[{"text":"Bricker, Owen P.","contributorId":25142,"corporation":false,"usgs":true,"family":"Bricker","given":"Owen","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":658119,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rice, Karen C. 0000-0002-9356-5443 kcrice@usgs.gov","orcid":"https://orcid.org/0000-0002-9356-5443","contributorId":1998,"corporation":false,"usgs":true,"family":"Rice","given":"Karen","email":"kcrice@usgs.gov","middleInitial":"C.","affiliations":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"preferred":false,"id":658120,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70179349,"text":"70179349 - 1993 - Uptake of planar polychlorinated biphenyls and 2,3,7,8-substituted polychlorinated dibenzofurans and dibenzo-<i>p</i>-dioxins by birds nesting in the lower Fox River and Green Bay, Wisconsin, USA","interactions":[],"lastModifiedDate":"2017-05-18T11:23:37","indexId":"70179349","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":887,"text":"Archives of Environmental Contamination and Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Uptake of planar polychlorinated biphenyls and 2,3,7,8-substituted polychlorinated dibenzofurans and dibenzo-<i>p</i>-dioxins by birds nesting in the lower Fox River and Green Bay, Wisconsin, USA","docAbstract":"<p>The uptake of persistent polychlorinated hydrocarbons (PCHs) by four avian species was investigated at upper trophic levels of two aquatic food chains of the lower Fox River and Green Bay, Wisconsin. Accumulation of total and specific planar polychlorinated biphenyls (PCBs), polychlorinated dibenzofurans (PCDFs), polychlorinated dibenzo-p-dioxin (PCDDs), and H411E rat hepatoma cell bioassay-derived 2,37,8-tetrachlorodibenzop-dioxin equivalents (TCDD-EQ) was evaluated in Forster's tern (<i>Sterna forsteri</i>) and common tern (<i>Sterna hirundo</i>) chicks, and in tree swallow (<i>Tachycineta bicolor</i>) and red-winged blackbird (<i>Agelaius phoeniceus</i>) nestlings from colonies nesting in several locations within the watershed. Concentrations of the PCHs were greatest in eggs and chicks of the two tern species, less in the tree swallows and least in the red-winged blackbirds. Young of all four species accumulated total PCBs, PCB congeners 77, 105, 126, and 169, and TCDD-EQ. The young birds also accumulated small concentrations of several 2,3,7,8-sbustituted PCDF and PCDD congeners. Uptake rates for certain of the PCHs for the Forster's tern chicks were: 15 μg/day for total PCBs, 70, 200, 6.5, and 0.14 ng/day for PCB congeners 77, 105, 126, and 169, respectively, and 270 μg/day for TCDD-EQ. Principal components analysis revealed that the patterns of PCH concentrations in the samples were influenced by species of bird, their age (or length of exposure) and nesting location. Collectively, our findings demonstrate that exposure of avian species to contaminants derived from aquatic food chains can be characterized and quantified for the purposes of ecological risk assessment.</p>","publisher":"Springer-Verlag","doi":"10.1007/BF01128731","usgsCitation":"Ankley, G., Niemi, G.J., Lodge, K.B., Harris, H.J., Beaver, D.L., Tillitt, D.E., Schwartz, T.R., Giesy, J.P., Jones, P.D., and Hagley, C., 1993, Uptake of planar polychlorinated biphenyls and 2,3,7,8-substituted polychlorinated dibenzofurans and dibenzo-<i>p</i>-dioxins by birds nesting in the lower Fox River and Green Bay, Wisconsin, USA: Archives of Environmental Contamination and Toxicology, v. 24, no. 3, p. 332-344, https://doi.org/10.1007/BF01128731.","productDescription":"13 p.","startPage":"332","endPage":"344","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":332631,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wisconsin","otherGeospatial":"Green Bay, Lower Fox River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.18519592285156,\n              44.386200799061896\n            ],\n            [\n              -88.18519592285156,\n              44.73258898857743\n            ],\n            [\n              -87.74642944335938,\n              44.73258898857743\n            ],\n            [\n              -87.74642944335938,\n              44.386200799061896\n            ],\n            [\n              -88.18519592285156,\n              44.386200799061896\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"24","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58662f1ee4b0cd2dabe7c4eb","contributors":{"authors":[{"text":"Ankley, Gerald T.","contributorId":67382,"corporation":false,"usgs":true,"family":"Ankley","given":"Gerald T.","affiliations":[],"preferred":false,"id":656881,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Niemi, Gerald J.","contributorId":71904,"corporation":false,"usgs":true,"family":"Niemi","given":"Gerald","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":656882,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lodge, Keith B.","contributorId":175374,"corporation":false,"usgs":false,"family":"Lodge","given":"Keith","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":656883,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Harris, Hallett J.","contributorId":177749,"corporation":false,"usgs":false,"family":"Harris","given":"Hallett","email":"","middleInitial":"J.","affiliations":[{"id":24697,"text":"Department of Natural and Applied Sciences, University of Wisconsin - Green Bay, Green Bay, WI","active":true,"usgs":false}],"preferred":false,"id":656884,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Beaver, Donald L.","contributorId":175373,"corporation":false,"usgs":false,"family":"Beaver","given":"Donald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":656885,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Tillitt, Donald E. 0000-0002-8278-3955 dtillitt@usgs.gov","orcid":"https://orcid.org/0000-0002-8278-3955","contributorId":1875,"corporation":false,"usgs":true,"family":"Tillitt","given":"Donald","email":"dtillitt@usgs.gov","middleInitial":"E.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":656886,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Schwartz, Ted R.","contributorId":36510,"corporation":false,"usgs":true,"family":"Schwartz","given":"Ted","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":656887,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Giesy, John P.","contributorId":57426,"corporation":false,"usgs":true,"family":"Giesy","given":"John","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":656888,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Jones, Paul D.","contributorId":175332,"corporation":false,"usgs":false,"family":"Jones","given":"Paul","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":656889,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Hagley, Cynthia","contributorId":177750,"corporation":false,"usgs":false,"family":"Hagley","given":"Cynthia","email":"","affiliations":[],"preferred":false,"id":656890,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70179664,"text":"70179664 - 1993 - Comparison of episodic acidification of Mid-Atlantic Upland and Coastal Plain streams","interactions":[],"lastModifiedDate":"2018-03-06T14:27:21","indexId":"70179664","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1993","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 episodic acidification of Mid-Atlantic Upland and Coastal Plain streams","docAbstract":"<p><span>Episodic acidification was examined in five mid-Atlantic watersheds representing three physiographic provinces: Coastal Plain, Valley and Ridge, and Blue Ridge. Each of the watersheds receives a similar loading of atmospheric pollutants (SO</span><sub>4</sub><sup>2−</sup><span><span>&nbsp;</span>and NO</span><sub>3</sub><sup>−</sup><span>) and is underlain by different bedrock type. The purpose of this research was to quantify and compare the episodic variability in storm flow chemistry in Reedy Creek, Virginia (Coastal Plain), Mill Run and Shelter Run, Virginia (Valley and Ridge), and Fishing Creek Tributary and Hunting Creek, Maryland (Blue Ridge). Because episodic responses were similar from storm to storm in each of the watersheds, a representative storm from each watershed was discussed. Acidification, defined as the loss of acid-neutralizing capacity (ANC), was observed in all streams except Mill Run. Mill Run chemistry showed little episodic variability. During storms in the other streams,<span>&nbsp;</span></span><i>p</i><span>H decreased while SO</span><sub>4</sub><sup>2−</sup><span>, NO</span><sub>3</sub><sup>−</sup><span>, and K</span><sup>+</sup><span><span>&nbsp;</span>concentrations increased. Concentrations of Mg</span><sup>2+</sup><span><span>&nbsp;</span>and Ca</span><sup>2+</sup><span><span>&nbsp;</span>increased in Reedy Creek and Fishing Creek Tributary, but decreased in Shelter Run and Hunting Creek. Therefore the net effect of episodic changes on the acid-base status differed among the streams. In general, greater losses of ANC were observed during storms at Shelter Run and Hunting Creek, watersheds underlain by reactive bedrock (carbonate, metabasalt); comparatively smaller losses in ANC were observed at Reedy Creek and Fishing Creek Tributary, watersheds underlain by quartzites and unconsolidated quartz sands and cobbles. Increased SO</span><sub>4</sub><sup>2−</sup><span><span>&nbsp;</span>concentrations were most important during storms at Reedy Creek and Fishing Creek Tributary, but organic anions (inferred by anion deficit) were also a factor in causing the loss of ANC. Dilution of base cations was the most important factor in the loss of ANC at Shelter Run. Both increased sulfate and dilution of base flow were important in causing the episodic acidification at Hunting Creek. The role of SO</span><sub>4</sub><sup>2−</sup><span><span>&nbsp;</span>in contributing to episodic acidification in these watersheds is similar to that documented in studies conducted in other regions of the United States, Scandinavia, Canada, and the United Kingdom. The importance of SO</span><sub>4</sub><sup>2−</sup><span><span>&nbsp;</span>in mid-Atlantic United States streams contrasts with northeastern United States streams, in which increased NO</span><sub>3</sub><sup>-</sup><span><span>&nbsp;</span>derived from snowpack is more important in causing episodic acidification. Results support the importance of shallow subsurface processes in determining storm flow chemistry, regional climatic characteristics in determining the different sources of acidity during episodes, and the importance of bedrock geology in determining the amount of ANC loss.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/93WR01408","usgsCitation":"O’Brien, A.K., Rice, K.C., Kennedy, M.M., and Bricker, O.P., 1993, Comparison of episodic acidification of Mid-Atlantic Upland and Coastal Plain streams: Water Resources Research, v. 29, no. 9, p. 3029-3039, https://doi.org/10.1029/93WR01408.","productDescription":"11 p.","startPage":"3029","endPage":"3039","costCenters":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"links":[{"id":333028,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland, Virginia, West Virginia","otherGeospatial":"Fishing Creek Tributary, Hunting Creek, Mill  Run, Reedy Creek, Shelter Run","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.266357421875,\n              37.93553306183642\n            ],\n            [\n              -79.266357421875,\n              39.7240885773337\n            ],\n            [\n              -77.0361328125,\n              39.7240885773337\n            ],\n            [\n              -77.0361328125,\n              37.93553306183642\n            ],\n            [\n              -79.266357421875,\n              37.93553306183642\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"29","issue":"9","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"58760117e4b04eac8e0746eb","contributors":{"authors":[{"text":"O’Brien, Anne K.","contributorId":52955,"corporation":false,"usgs":true,"family":"O’Brien","given":"Anne","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":658121,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rice, Karen C. 0000-0002-9356-5443 kcrice@usgs.gov","orcid":"https://orcid.org/0000-0002-9356-5443","contributorId":1998,"corporation":false,"usgs":true,"family":"Rice","given":"Karen","email":"kcrice@usgs.gov","middleInitial":"C.","affiliations":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"preferred":false,"id":658122,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kennedy, Margaret M.","contributorId":178170,"corporation":false,"usgs":true,"family":"Kennedy","given":"Margaret","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":658123,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bricker, Owen P.","contributorId":25142,"corporation":false,"usgs":true,"family":"Bricker","given":"Owen","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":658124,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70179662,"text":"70179662 - 1993 - Investigations of acid depositions","interactions":[],"lastModifiedDate":"2018-11-06T13:43:33","indexId":"70179662","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":242,"text":"Bulletin","active":false,"publicationSubtype":{"id":4}},"title":"Investigations of acid depositions","docAbstract":"<p>No abstract available.</p>","language":"English","usgsCitation":"Bricker, O.P., and Rice, K.C., 1993, Investigations of acid depositions: Bulletin, 5 p.","productDescription":"5 p.","startPage":"29","endPage":"33","costCenters":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true},{"id":37280,"text":"Virginia and West Virginia Water Science Center ","active":true,"usgs":true}],"links":[{"id":333066,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publicComments":"WRD Bulletin, 81st Year","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5878a4b7e4b04df303d95871","contributors":{"authors":[{"text":"Bricker, Owen P.","contributorId":25142,"corporation":false,"usgs":true,"family":"Bricker","given":"Owen","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":658117,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rice, Karen C. 0000-0002-9356-5443 kcrice@usgs.gov","orcid":"https://orcid.org/0000-0002-9356-5443","contributorId":1998,"corporation":false,"usgs":true,"family":"Rice","given":"Karen","email":"kcrice@usgs.gov","middleInitial":"C.","affiliations":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"preferred":false,"id":658118,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70179417,"text":"70179417 - 1993 - Toxicity of contaminated sediments in dilution series with control sediments","interactions":[],"lastModifiedDate":"2016-12-31T14:31:29","indexId":"70179417","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1226,"text":"Chemosphere","active":true,"publicationSubtype":{"id":10}},"title":"Toxicity of contaminated sediments in dilution series with control sediments","docAbstract":"<p>T<span>he use of dilutions has been the foundation of our approach for assessing contaminated water, and accordingly, it may be important to establish similar or parallel approaches for sediment dilutions. Test organism responses to dilution gradients can identify the degree of necessary sediment alteration to reduce the toxicity. Using whole sediment dilutions to represent the complex interactions of in situ sediments can identify the toxicity, but the selection of the appropriate diluent for the contaminated sediment may affect the results and conclusions drawn. Contaminated whole sediments were examined to evaluate the toxicity of dilutions of sediments with a diversity of test organisms. Dilutions of the contaminated sediments were prepared with differing diluents that varied in organic carbon content, particle size distribution, and volatile solids. Studies were conducted using four macroinvertebrates and a vascular, rooted plant. Responses by some test organisms followed a sigmoidal dose-response curve, but others followed a U-shaped curve. Initial dilutions reduced toxicity as expected, but further dilution resulted in an increase in toxicity. The type of diluent used was an important factor in assessing the sediment toxicity, because the control soil reduced toxicity more effectively than sand as a diluent of the same sediment. Using sediment chemical and physical characteristics as an indicator of sediment dilution may not be as useful as chemical analysis of contaminants, but warrants further investigation.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0045-6535(93)90158-2","usgsCitation":"Nelson, M., Landrum, P., Burton, G., Klaine, S., Crecelius, E., Byl, T., Gossiaux, D.C., Tsymbal, V., Cleveland, L., Ingersoll, C.G., and Sasson-Brickson, G., 1993, Toxicity of contaminated sediments in dilution series with control sediments: Chemosphere, v. 27, no. 9, p. 1789-1812, https://doi.org/10.1016/0045-6535(93)90158-2.","productDescription":"24 p.","startPage":"1789","endPage":"1812","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":332720,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5868d226e4b0cd2dabe7c809","contributors":{"authors":[{"text":"Nelson, M.K.","contributorId":80583,"corporation":false,"usgs":true,"family":"Nelson","given":"M.K.","email":"","affiliations":[],"preferred":false,"id":657172,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Landrum, P.F.","contributorId":98423,"corporation":false,"usgs":true,"family":"Landrum","given":"P.F.","email":"","affiliations":[],"preferred":false,"id":657173,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Burton, G.A. Jr.","contributorId":91959,"corporation":false,"usgs":true,"family":"Burton","given":"G.A.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":657174,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Klaine, S.J.","contributorId":38304,"corporation":false,"usgs":true,"family":"Klaine","given":"S.J.","affiliations":[],"preferred":false,"id":657175,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Crecelius, E.A.","contributorId":50787,"corporation":false,"usgs":true,"family":"Crecelius","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":657176,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Byl, T.D.","contributorId":86373,"corporation":false,"usgs":true,"family":"Byl","given":"T.D.","email":"","affiliations":[],"preferred":false,"id":657177,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Gossiaux, Duane C.","contributorId":7225,"corporation":false,"usgs":true,"family":"Gossiaux","given":"Duane","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":657178,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Tsymbal, V.N.","contributorId":177807,"corporation":false,"usgs":false,"family":"Tsymbal","given":"V.N.","email":"","affiliations":[],"preferred":false,"id":657179,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Cleveland, L.","contributorId":82084,"corporation":false,"usgs":true,"family":"Cleveland","given":"L.","email":"","affiliations":[],"preferred":false,"id":657180,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Ingersoll, Christopher G. 0000-0003-4531-5949 cingersoll@usgs.gov","orcid":"https://orcid.org/0000-0003-4531-5949","contributorId":2071,"corporation":false,"usgs":true,"family":"Ingersoll","given":"Christopher","email":"cingersoll@usgs.gov","middleInitial":"G.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":657181,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Sasson-Brickson, G.","contributorId":177808,"corporation":false,"usgs":false,"family":"Sasson-Brickson","given":"G.","email":"","affiliations":[{"id":13348,"text":"Wright State University","active":true,"usgs":false}],"preferred":false,"id":657182,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":70179264,"text":"70179264 - 1993 - Use of mesocosm data to predict effects in aquatic ecosystems: Limits to interpretation: Chapter 16","interactions":[],"lastModifiedDate":"2016-12-27T12:15:02","indexId":"70179264","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"16","title":"Use of mesocosm data to predict effects in aquatic ecosystems: Limits to interpretation: Chapter 16","docAbstract":"<p><span>Aquatic mesocosm studies are being used to refute a presumption of risk derived from laboratory toxicity tests conducted under the Federal Insecticide, Fungicide, and Rodenticide Act (FIFRA). Mesocosm studies incorporate many biological, chemical and physical characteristics of natural ecosystems. Hence, they serve as realistic surrogates of natural ecosystems and allow tests of pesticide effect at the population, community, and ecosystem level. We discuss two factors, ecosystem trophic status and organism life history, which influence the results derived from aquatic mesocosm studies. &nbsp;Trophic status influences the fat and effects of chemicals which strongly sorb or biologically degrade, yet may not be as important in the fate and effects of more water soluble chemicals. &nbsp;Life history traits of organisms and the intensity, frequency, and duration of the pesticide disturbance also determine the mesocosm response pattern.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Aquatic mesocosm studies in ecological risk assessment","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Taylor and Francis","isbn":"9780873715928","usgsCitation":"La Point, T.W., and Fairchild, J.F., 1993, Use of mesocosm data to predict effects in aquatic ecosystems: Limits to interpretation: Chapter 16, chap. 16 <i>of</i> Aquatic mesocosm studies in ecological risk assessment, p. 241-256.","productDescription":"16 p.","startPage":"241","endPage":"256","numberOfPages":"16","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":332531,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":332530,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.crcpress.com/Aquatic-Mesocosm-Studies-in-Ecological-Risk-Assessment/Graney/p/book/9780873715928"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"585e45e0e4b01224f329bf17","contributors":{"editors":[{"text":"Graney, Robert L.","contributorId":37294,"corporation":false,"usgs":true,"family":"Graney","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":656589,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Kennedy, James H.","contributorId":177666,"corporation":false,"usgs":false,"family":"Kennedy","given":"James","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":656590,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Rodgers, John H. Jr.","contributorId":87065,"corporation":false,"usgs":true,"family":"Rodgers","given":"John","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":656591,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"La Point, Thomas W.","contributorId":114142,"corporation":false,"usgs":true,"family":"La Point","given":"Thomas","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":656587,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fairchild, James F. jfairchild@usgs.gov","contributorId":492,"corporation":false,"usgs":true,"family":"Fairchild","given":"James","email":"jfairchild@usgs.gov","middleInitial":"F.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":false,"id":656588,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70179038,"text":"70179038 - 1993 - Ground-water hydrology of the upper Sevier River Basin, south-central Utah, and simulation of ground-water flow in the valley-fill in Panguitch Valley.","interactions":[],"lastModifiedDate":"2016-12-14T09:31:32","indexId":"70179038","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"102","title":"Ground-water hydrology of the upper Sevier River Basin, south-central Utah, and simulation of ground-water flow in the valley-fill in Panguitch Valley.","docAbstract":"<p>The ground-water hydrology of the upper Sevier River basin, primarily of the unconsolidated valley-fill aquifers, was studied from 1988 to 1989. Recharge to the valley-fill aquifers is mostly by seepage from surface-water sources. Changes in soil-moisture content am water levels were measured in Panguitch Valley both at a flood-irrigated and at a sprinkler-irrigated alfalfa field to quantify seepage from unconsumed irrigation water. Lag time between irrigation and water-level response decreased from 6 to 2 days in the flood-irrigated field as the soil-moisture content increased. Water levels measured in the sprinkler-irrigated field did not respond to irrigation. Discharge from the valley-fill aquifer to the Sevier River in Panguitch Valley is about 53,570 acre-feet per year.</p><p>Water levels measured in wells from 1951 to 1989 tend to fluctuate with the quantity of precipitation falling at higher elevations. Ground-water discharge to the Sevier River in Panguitch Valley causes a general increase in the specific conductance of the river in a downstream direction.</p><p>A three-layered ground-water-flow model was used to simulate the effects of changes in irrigation practices am increased ground-water withdrawals in Panguitch Valley. The establishment of initial conditions consisted of comparing simulated water levels and simulated gains and losses from the Sevier River and selected canals with values measured during the 1988 irrigation season. The model was calibrated by comparing water-level changes measured from 1961 to 1963 to simulated changes. A simulated change from flood to sprinkler irrigation resulted in a maximum decline in water level of 0.9 feet after the first year of change. Simulating additional discharge from wells resulted in drawdowns of about 20 feet after the first year of pumping.</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United State Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Thiros, S.A., and Brothers, W.C., 1993, Ground-water hydrology of the upper Sevier River Basin, south-central Utah, and simulation of ground-water flow in the valley-fill in Panguitch Valley.: Technical Publication 102, vii, 121 p.","productDescription":"vii, 121 p.","numberOfPages":"129","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":332093,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":332091,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-6-511"},{"id":332092,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/y920/y920000a.pdf"}],"country":"United States","state":"Utah","otherGeospatial":"Sevier River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.862548828125,\n              37.400710068740565\n            ],\n            [\n              -111.6046142578125,\n              37.36579146999664\n            ],\n            [\n              -111.4947509765625,\n              39.56758783088905\n            ],\n            [\n              -111.7034912109375,\n              39.56758783088905\n            ],\n            [\n              -112.532958984375,\n              38.14319750166766\n            ],\n            [\n              -112.862548828125,\n              37.400710068740565\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"585268e5e4b0e2663625eca2","contributors":{"authors":[{"text":"Thiros, Susan A. 0000-0002-8544-553X sthiros@usgs.gov","orcid":"https://orcid.org/0000-0002-8544-553X","contributorId":965,"corporation":false,"usgs":true,"family":"Thiros","given":"Susan","email":"sthiros@usgs.gov","middleInitial":"A.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":655852,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brothers, William C.","contributorId":68891,"corporation":false,"usgs":true,"family":"Brothers","given":"William","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":655853,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70176564,"text":"70176564 - 1993 - Challenges in real-time data collection at active volcanoes in the Pacific Northwest, the Philippines, and Alaska [abs.]","interactions":[],"lastModifiedDate":"2016-09-21T13:46:22","indexId":"70176564","displayToPublicDate":"2016-04-13T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Challenges in real-time data collection at active volcanoes in the Pacific Northwest, the Philippines, and Alaska [abs.]","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":" American Water Resources Association, Alaska Chapter Proceedings of 1993 Annual Conference","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"American Water Resources Association 1993 Annual Conference","conferenceDate":"April 8-9, 1993","conferenceLocation":"Alaska","language":"English","publisher":"American Water Resources Association","publisherLocation":"Middleburg, VA","usgsCitation":"Dorava, J., and May, B., 1993, Challenges in real-time data collection at active volcanoes in the Pacific Northwest, the Philippines, and Alaska [abs.], chap. <i>of</i>  American Water Resources Association, Alaska Chapter Proceedings of 1993 Annual Conference, p. 1-1.","productDescription":"1 p.","startPage":"1","endPage":"1","numberOfPages":"1","costCenters":[],"links":[{"id":328818,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Phillipines, United States","state":"Alaska, Oregon, 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57feb33ae4b0824b2d154766","contributors":{"authors":[{"text":"Dorava, J.M.","contributorId":68756,"corporation":false,"usgs":true,"family":"Dorava","given":"J.M.","affiliations":[],"preferred":false,"id":649213,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"May, B.A.","contributorId":8872,"corporation":false,"usgs":true,"family":"May","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":649214,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175166,"text":"70175166 - 1993 - Coupled effects of vertical mixing and benthic grazing on phytoplankton populations in shallow, turbid estuaries","interactions":[],"lastModifiedDate":"2019-03-06T06:11:07","indexId":"70175166","displayToPublicDate":"2016-03-07T06:15:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2379,"text":"Journal of Marine Research","active":true,"publicationSubtype":{"id":10}},"title":"Coupled effects of vertical mixing and benthic grazing on phytoplankton populations in shallow, turbid estuaries","docAbstract":"<p><span>Coastal ocean waters tend to have very different patterns of phytoplankton biomass variability from the open ocean, and the connections between physical variability and phytoplankton bloom dynamics are less well established for these shallow systems. Predictions of biological responses to physical variability in these environments is inherently difficult because the recurrent seasonal patterns of mixing are complicated by aperiodic fluctuations in river discharge and the high-frequency components of tidal variability. We might expect, then, less predictable and more complex bloom dynamics in these shallow coastal systems compared with the open ocean. Given this complex and dynamic physical environment, can we develop a quantitative framework to define the physical regimes necessary for bloom inception, and can we identify the important mechanisms of physical-biological coupling that lead to the initiation and termination of blooms in estuaries and shallow coastal waters? Numerical modeling provides one approach to address these questions. Here we present results of simulation experiments with a refined version of Cloern's (1991) model in which mixing processes are treated more realistically to reflect the dynamic nature of turbulence generation in estuaries. We investigated several simple models for the turbulent mixing coefficient. We found that the addition of diurnal tidal variation to Cloern's model greatly reduces biomass growth indicating that variations of mixing on the time scale of hours are crucial. Furthermore, we found that for conditions representative of South San Francisco Bay, numerical simulations only allowed for bloom development when the water column was stratified and when minimal mixing was prescribed in the upper layer. Stratification, however, itself is&nbsp;</span><i>not</i><span>&nbsp;sufficient to ensure that a bloom will develop: minimal wind stirring is a further prerequisite to bloom development in shallow turbid estuaries with abundant populations of benthic suspension feeders.</span></p>","language":"English","publisher":"Sears Foundation for Marine Research","doi":"10.1357/0022240933223954","usgsCitation":"Koseff, J.R., Holen, J.K., Monismith, S., and Cloern, J.E., 1993, Coupled effects of vertical mixing and benthic grazing on phytoplankton populations in shallow, turbid estuaries: Journal of Marine Research, v. 51, no. 4, p. 843-868, https://doi.org/10.1357/0022240933223954.","productDescription":"26 p.","startPage":"843","endPage":"868","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":325890,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"51","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57a072b1e4b060ce18fb2d94","contributors":{"authors":[{"text":"Koseff, Jeffrey R.","contributorId":37915,"corporation":false,"usgs":false,"family":"Koseff","given":"Jeffrey","email":"","middleInitial":"R.","affiliations":[{"id":6986,"text":"Stanford University","active":true,"usgs":false}],"preferred":false,"id":644182,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holen, Jacqueline K.","contributorId":173302,"corporation":false,"usgs":false,"family":"Holen","given":"Jacqueline","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":644183,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Monismith, Stephen G.","contributorId":57228,"corporation":false,"usgs":true,"family":"Monismith","given":"Stephen G.","affiliations":[],"preferred":false,"id":644184,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cloern, James E. 0000-0002-5880-6862 jecloern@usgs.gov","orcid":"https://orcid.org/0000-0002-5880-6862","contributorId":1488,"corporation":false,"usgs":true,"family":"Cloern","given":"James","email":"jecloern@usgs.gov","middleInitial":"E.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":644185,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70176430,"text":"70176430 - 1993 - Mt. Spurr's 1992 eruptions","interactions":[],"lastModifiedDate":"2023-12-18T12:57:09.125964","indexId":"70176430","displayToPublicDate":"2016-02-09T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Mt. Spurr's 1992 eruptions","docAbstract":"<div class=\"\"><div class=\"article-section__content en main\"><p>On June 27, 1992, the Crater Peak vent on the south side of Mt. Spurr awoke from 39 years of dormancy and burst into subplinian eruption after 10 months of elevated seismicity. Two more eruptions followed in August and September. The volcano lies 125-km west of Anchorage, which is Alaska's largest city and an important international hub for air travel. The Alaska Volcano Observatory (AVO) was able to warn communities and the aviation industry well in advance of these eruptions.</p></div></div>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/93EO00284","usgsCitation":"American Geophysical Union, 1993, Mt. Spurr's 1992 eruptions: Eos, Transactions, American Geophysical Union, v. 74, no. 19, p. 217-222, https://doi.org/10.1029/93EO00284.","productDescription":"5 p.","startPage":"217","endPage":"222","numberOfPages":"3","temporalStart":"1992-07-27","temporalEnd":"1992-09-30","costCenters":[{"id":121,"text":"Alaska Volcano Observatory","active":false,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":328610,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Aleutian Arc","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -152.501220703125,\n              61.19952130477601\n            ],\n            [\n              -152.501220703125,\n              61.3611962736049\n            ],\n            [\n              -151.98486328125,\n              61.3611962736049\n            ],\n            [\n              -151.98486328125,\n              61.19952130477601\n            ],\n            [\n              -152.501220703125,\n              61.19952130477601\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"74","issue":"19","noUsgsAuthors":false,"publicationDate":"2011-06-03","publicationStatus":"PW","scienceBaseUri":"57d9233de4b090824ffa1aea"}
,{"id":70174859,"text":"70174859 - 1993 - 1993 Annual Report: San Francisco estuary regional monitoring program for trace substances","interactions":[],"lastModifiedDate":"2016-07-18T19:57:26","indexId":"70174859","displayToPublicDate":"2016-02-01T09:15:00","publicationYear":"1993","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"title":"1993 Annual Report: San Francisco estuary regional monitoring program for trace substances","docAbstract":"<p>This first annual report of the San Francisco Estuary Regional Monitoring Program contains the results of monitoring measurements made in 1993. Measurements of conventional water quality parameters and trace contaminant concentrations were made at 16 stations throughout the Estuary three times during the year: the wet period (March), during declining Delta outflow (May), and during the dry period (September). Water toxicity tests were conducted at 8 of those stations. Measurements of sediment quality and contaminant concentrations were made at the same 16 stations during the wet and dry sampling periods. Sediment toxicity was measured at 8 of those stations. Transplanted, bagged bivalve bioaccumulation and condition was measured at 11 stations during the wet and dry sampling periods.</p>\n<p>Water Monitoring. Total or near-total (dissolved + particulate, see text) arsenic, cadmium, selenium, and dissolved (0.45 &micro;m filtered) arsenic, cadmium, copper, nickel, silver, and zinc in water were highest in the South Bay. In general, dissolved metals in water were usually lowest in the Central Bay due to ocean influences. Near-total nickel and total mercury in water were highest in the northern estuary (San Pablo and Suisun Bays). Dissolved chromium and lead were highest at the Sacramento and San Joaquin River confluence stations. Six of the ten dissolved trace metals were highest in March during high runoff. Dissolved and total arsenic, selenium, and near-total cadmium were highest in September.</p>\n<p>Concentrations of trace organic contaminants are reported for the March sampling period. Total PAHs and PCBs were highest in the South Bay, but PCBs were also high in the Napa River. Dissolved PAHs were highest in the Central Bay, and dissolved PCBs were highest in the Napa River. Total and dissolved pesticides were highest in the Sacramento River and in the Extreme South Bay.</p>\n<p>Concentrations of trace elements in water (except selenium) were usually closely related with other environmental parameters. Total or near-total metals concentrations in water were most often associated with the amount of particulate material (TSS) in the water. Dissolved concentrations were usually associated with salinity or dissolved organic carbon (DOC) content. Dissolved PAHs were well correlated with TSS, but dissolved and total trace organic contaminants were poorly correlated with other water parameters.</p>\n<p>Based on deviations from conservative mixing of fresh and salt water, three different patterns of possible sources of metals were identified in 1993. For dissolved chromium and lead, rivers and local runoff appeared to be important sources. For dissolved arsenic, cadmium, copper, and nickel year-round inputs from the South Bay appeared to be important sources. Dissolved mercury, selenium, and zinc were associated with local runoff in the South Bay during the wet period. Dissolved silver did not fit any of these patterns.</p>\n<p>Although most contaminant concentrations were below water quality objectives, several trace contaminants were above the objectives at some stations. Comparisons to water quality objectives are used as a guide for evaluation of contaminant concentrations, but there are some differences in the way the RMP data are measured and that prescribed for regulatory purposes (see text). Concentrations of 5 metals in water were above EPA or Regional Basin Plan water quality objectives at six stations (see Table 30). Most of these elevated levels occurred at the northern estuary stations. Total PCB concentrations were above EPA human health objectives at all RMP stations. The pesticides chlordane, dieldrin, and DDTs were above the EPA objectives at several RMP stations, particularly at the northern-most, and river confluence stations.</p>\n<p>Although some of the contaminant concentrations were above water quality objectives, water toxicity tests (96 hour algal growth and 48 hour bivalve larval development tests) did not indicate toxicity (sometimes inconclusive) associated with the water samples collected at any of the RMP stations in 1993. Exposure to Bay San Francisco Estuary Regional Monitoring Program Regional Monitoring Program 1993 Report ii water actually enhanced algal growth at most stations.</p>\n<p>In addition to the Estuary-wide sampling, the Sacramento and San Joaquin Rivers were sampled upstream from their confluence. Stations in each river were sampled six times over a 6 week period of high flows. In the Sacramento River, seven of the ten dissolved metals measured had concentrations lower than those measured at the river confluence stations. Some metals concentrations in the San Joaquin River were higher, and some were lower than concentrations from the river confluence station. Metals concentrations in the Sacramento River were poorly related to river flow because the station at Rio Vista is under considerable tidal influence. In the San Joaquin River, flows were inversely related to 7 of 10 total metals concentrations.</p>\n<p>Sediment Monitoring. Concentrations of silver, mercury, and lead in sediment were highest in the South Bay. However, concentrations of most trace metals in sediments were highest in the northern estuary at stations with the finest (silt, clay) sediments. The northern estuary stations with the coarsest (sand, shell) sediments generally had the lowest metals concentrations. There were differences in concentrations of cadmium, lead, and selenium in sediments between the sampling periods, but no consistent trend as to which sampling period had higher values. In September, PAHs and PCBs in sediments were highest in the Central Bay, but pesticides in sediments were highest in the northern estuary and Extreme South Bay.</p>\n<p>NOAA&rsquo;s Median Effects Ranges (ERM) for sediments were used as a guide for evaluation of sediment contaminant concentrations. Nickel was the only trace contaminant in sediment above the ERM guidelines, and it was high at all RMP stations. These high levels are probably due to natural, geologic sources.</p>\n<p>Although sediment contaminant concentrations were below ERMs, sediment toxicity tests (10 day amphipod mortality, and 48 hour bivalve larval development in elutriates) indicated toxicity at all stations tested. Sediment factors that could have caused the toxicity were not investigated.</p>\n<p>Bivalve Bioaccumulation. Mussels, oysters, and freshwater clams were transplanted to the RMP stations to evaluate bioaccumulation of trace substances. Trace metals were bioaccumulated at nearly all RMP stations. However, arsenic, lead, and mercury did not appear to bioaccumulate. There was generally more bioaccumulation during the dry season than during the wet season. In September, PAHs, PCBs, and pesticides accumulated in all samples. Bioaccumulation of PAHs and pesticides was generally highest at the river confluence stations, and the Napa River. PCBs accumulated most at Redwood Creek.</p>\n<p>There were substantial differences in the degree of bioaccumulation among the species. Oysters appeared to accumulate higher concentrations of trace metals than the other species, especially copper, which may be a natural phenomenon.</p>\n<p>There are no established tissue contaminant standards for trace metal and organic contaminants. Therefore, comparisons to Median International Standards (MIS) for human consumption, or U.S. Food and Drug Administration (USFDA) action levels for trace organics are used to evaluate the bioaccumulation results. Concentrations of selenium were higher than MIS guidelines at all stations during the wet season. Other trace metal concentrations were higher than MIS guidelines at various stations during one or the other sampling period. However, none of the bivalves contained concentrations above the USFDA or National Academy of Sciences (NAS) guidelines for trace organic contaminants.</p>\n<p>The transplanted bivalves survived well at all stations except in the Napa River where less than 35% survived during both sampling seasons. Measures of bivalve condition (dry weight, shell volume) indicated that bivalves deployed in the Central Bay grew significantly, but those at most other stations actually lost weight. Whether these differences were due to natural causes such as salinity or food supply, or to contamination, was not determined.</p>\n<p>Pilot Studies. Two pilot monitoring studies were conducted in 1993. A pilot study of Estuary hydrography and phytoplankton was conducted by scientists from the U.S. Summary Geological Survey in Menlo Park and U.C. Davis. Water column profiles at up to 37 stations were monitored along a transect of the Estuary run monthly between the South Bay and the Delta.</p>\n<p>The primary objective of this study was to define physical (salinity, temperature, suspended particulate matter, and light penetration), chemical (dissolved oxygen) and biological (chlorophyll a) characteristics of Estuary water that may influence other chemical and biological reactions. A second objective was to investigate planktonic indicators of ecosystem structure and function.</p>\n<p>The data collected in 1993 showed the extent and duration of the spring phytoplankton bloom in the South Bay, other localized blooms in the northern estuary, the stratification and mixing associated with the entrapment zone in the northern estuary, and mixing in the Estuary resulting from the high rainfall in 1993. Knowledge of the duration and extent of these natural features of the Estuary provide context for interpretation of the RMP contaminant data collected only 3 times per year.</p>\n<p>Another pilot study of suspended sediment transport processes was conducted by the USGS in Sacramento. This study used continuous recording sensors at Point San Pablo and the Bay Bridge to measure the amount of suspended sediment in the water at mid-depth and near the bottom, as well as tide height.</p>\n<p>The objectives of this study were to estimate which factors determine suspended solids concentrations in the Central Bay and to collect time series of suspended solids that are appropriate for continuous monitoring of suspended solids and for calibration and validation of numerical models.</p>\n<p>The investigators determined that spring tides accounted for most of the variation in suspended solids concentrations at the stations monitored, not runoff from the Sacramento or San Joaquin Rivers, or semidiurnal and diurnal tides.</p>\n<p>Comparisons were also made between measurements made by the continuous recordings and the RMP samples collected during the regular monitoring cruises. The different ways of measuring TSS were generally comparable, however only 3 measurements per year as made by the RMP could not provide the information of TSS variation actually occurring in the Estuary.</p>\n<p>This information is important because as shown by the RMP data, total contaminant concentrations in Estuary water is largely dependent on the TSS in the water. This implies that the RMP measurements alone cannot determine accurately the range of contaminant concentrations without better characterizing the dynamics of TSS.</p>\n<p>The RMP Pilot Studies are important to the developing RMP because they will help put RMP measurements into the perspective of Estuary processes and mechanisms at other time scales. The studies can relate those processes to the RMP measurements and will facilitate revision of sampling design and interpretation.</p>\n<p>Summaries of other monitoring activities pertinent to regional monitoring are also included in the Report: a description of the Regional Board&rsquo;s Bay Protection Studies, the Sacramento Coordinated Monitoring Program, and a wetlands monitoring plan are included.</p>","language":"English","publisher":"San Francisco Estuary Institute","publisherLocation":"San Francisco, CA","collaboration":"A Cooperative Program Managed and Administered by the San Francisco Estuary Institute","usgsCitation":"Thompson, B., Lacy, J., Hardin, D., Grovhaug, T., Taberski, K., Jassby, A.D., Cloern, J.E., Caffrey, J., Cole, B., and Schoellhamer, D., 1993, 1993 Annual Report: San Francisco estuary regional monitoring program for trace substances, 226 p.","productDescription":"226 p.","startPage":"1","endPage":"226","numberOfPages":"226","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1993-03-01","costCenters":[],"links":[{"id":325419,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":325418,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.sfei.org/sites/default/files/biblio_files/1993_RMP_Annual_Report.pdf","text":"1993 Annual Report: San Francisco Estuary Regional Monitoring Program for Trace Substances","size":"2.7 MB","linkFileType":{"id":1,"text":"pdf"},"description":"1993 Annual Report: San Francisco Estuary Regional Monitoring Program for Trace Substances"}],"country":"United States","state":"California","county":"San Francisco","city":"San Francisco","otherGeospatial":"San Francisco Estuary","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.04962158203124,\n              38.22739287920163\n            ],\n            [\n              -121.39617919921874,\n              38.302869955150044\n            ],\n            [\n              -121.322021484375,\n              37.76854362092148\n            ],\n            [\n              -121.92901611328125,\n              37.155938651244625\n            ],\n            [\n              -122.48931884765626,\n              37.16469418870222\n            ],\n            [\n              -123.04962158203124,\n              38.22739287920163\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"578dfdace4b0f1bea0e0f80c","contributors":{"authors":[{"text":"Thompson, B.","contributorId":13810,"corporation":false,"usgs":true,"family":"Thompson","given":"B.","affiliations":[],"preferred":false,"id":642846,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lacy, Jessica","contributorId":71277,"corporation":false,"usgs":true,"family":"Lacy","given":"Jessica","affiliations":[],"preferred":false,"id":642847,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hardin, Dane","contributorId":92898,"corporation":false,"usgs":true,"family":"Hardin","given":"Dane","affiliations":[],"preferred":false,"id":642848,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Grovhaug, Tom","contributorId":172974,"corporation":false,"usgs":false,"family":"Grovhaug","given":"Tom","email":"","affiliations":[],"preferred":false,"id":642849,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Taberski, K.","contributorId":80075,"corporation":false,"usgs":true,"family":"Taberski","given":"K.","email":"","affiliations":[],"preferred":false,"id":642851,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Jassby, Alan D.","contributorId":66403,"corporation":false,"usgs":true,"family":"Jassby","given":"Alan","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":642853,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Cloern, James E. 0000-0002-5880-6862 jecloern@usgs.gov","orcid":"https://orcid.org/0000-0002-5880-6862","contributorId":1488,"corporation":false,"usgs":true,"family":"Cloern","given":"James","email":"jecloern@usgs.gov","middleInitial":"E.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":642854,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Caffrey, J.","contributorId":147320,"corporation":false,"usgs":false,"family":"Caffrey","given":"J.","email":"","affiliations":[],"preferred":false,"id":642855,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Cole, B.","contributorId":36744,"corporation":false,"usgs":true,"family":"Cole","given":"B.","email":"","affiliations":[],"preferred":false,"id":642856,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Schoellhamer, David H. 0000-0001-9488-7340 dschoell@usgs.gov","orcid":"https://orcid.org/0000-0001-9488-7340","contributorId":631,"corporation":false,"usgs":true,"family":"Schoellhamer","given":"David H.","email":"dschoell@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":642857,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70174192,"text":"70174192 - 1993 - Research and education to improve surface and ground-water quality of a claypan soil--Proceedings of agricultural research to protect water quality","interactions":[],"lastModifiedDate":"2016-08-09T15:53:01","indexId":"70174192","displayToPublicDate":"2016-01-06T10:30:00","publicationYear":"1993","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Research and education to improve surface and ground-water quality of a claypan soil--Proceedings of agricultural research to protect water quality","docAbstract":"<p>No abstract available.</p>","conferenceTitle":"Agricultural research to protect water quality","conferenceDate":"February 21-24, 1993","conferenceLocation":"Minneapolis, Minnesota, USA","publisher":"Soil and Water Conservation Society","publisherLocation":"Ankeny, Iowa","isbn":"0935734341","collaboration":"In cooperation with Agricultural Research Service, Cooperative State Research Service, Extension Service, Soil Conservation Service, U.S. Environmental Protection Agency, U.S. Geological Survey","usgsCitation":"Alberts, E., Blevins, D.W., Kitchen, N.K., and Prato, T., 1993, Research and education to improve surface and ground-water quality of a claypan soil--Proceedings of agricultural research to protect water quality, Agricultural research to protect water quality, Minneapolis, Minnesota, USA, February 21-24, 1993, p. 21-38.","productDescription":"18 p.","startPage":"21","endPage":"38","numberOfPages":"18","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"links":[{"id":324592,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5774f2c0e4b07dd077c6a9d2","contributors":{"authors":[{"text":"Alberts, E.E.","contributorId":169236,"corporation":false,"usgs":false,"family":"Alberts","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":641214,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blevins, D. W.","contributorId":75940,"corporation":false,"usgs":true,"family":"Blevins","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":641215,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kitchen, N. K.","contributorId":172545,"corporation":false,"usgs":false,"family":"Kitchen","given":"N.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":641216,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Prato, Tony","contributorId":97394,"corporation":false,"usgs":true,"family":"Prato","given":"Tony","affiliations":[],"preferred":false,"id":641217,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70174578,"text":"70174578 - 1993 - Organic carbon sources and sinks in San Francisco Bay: variability induced by river flow","interactions":[],"lastModifiedDate":"2019-03-01T07:23:40","indexId":"70174578","displayToPublicDate":"2016-01-05T10:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2663,"text":"Marine Ecology Progress Series","active":true,"publicationSubtype":{"id":10}},"title":"Organic carbon sources and sinks in San Francisco Bay: variability induced by river flow","docAbstract":"<div id=\"yui_3_14_1_1_1468429681350_906\" class=\"publication-abstract\" data-reactid=\"105\">\n<div id=\"yui_3_14_1_1_1468429681350_905\" class=\"nova-e-text nova-e-text--size-l nova-e-text--family-sans-serif nova-e-text--spacing-auto\" data-reactid=\"108\">Sources and sinks of organic carbon for San Francisco Bay (California, USA) were estimated for 1980. Sources for the southern reach were dominated by phytoplankton and benthic microalgal production. River loading of organic matter was an additional important factor in the northern reach. Tidal marsh export and point sources played a secondary role. Autochthonous production in San Francisco Bay appears to be less than the mean for temperate-zone estuaries, primarily because turbidity limits microalgal production and the development of seagrass beds. Exchange between the Bay and Pacific Ocean plays an unknown but potentially important role in the organic carbon balance. Interannual variability in the organic carbon supply was assessed for Suisun Bay, a northern reach subembayment that provides habitat for important fish species (delta smelt Hypomesus transpacificus and larval striped bass Morone saxatilus). The total supply fluctuated by an order of magnitude; depending on the year, either autochthonous sources (phytoplankton production) or allochthonous sources (riverine loading) could be dominant. The primary cause of the year-to-year change was variability of freshwater inflows from the Sacramento and San Joaquin rivers, and its magnitude was much larger than long-term changes arising from marsh destruction and point source decreases. Although interannual variability of the total organic carbon supply could not be assessed for the southern reach, year-to-year changes in phytoplankton production were much smaller than in Suisun Bay, reflecting a relative lack of river influence.</div>\n</div>","language":"English","publisher":"Inter-Research","doi":"10.3354/meps095039","usgsCitation":"Jassby, A.D., Powell, T., and Cloern, J.E., 1993, Organic carbon sources and sinks in San Francisco Bay: variability induced by river flow: Marine Ecology Progress Series, v. 95, no. 1-2, p. 39-54, https://doi.org/10.3354/meps095039.","productDescription":"16 p.","startPage":"39","endPage":"54","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":488503,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3354/meps095039","text":"Publisher Index Page"},{"id":325187,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","county":"San Francisco","city":"San Franciso","otherGeospatial":"San Francisco Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.03314208984374,\n              37.14499280340638\n            ],\n            [\n              -123.03314208984374,\n              38.30933576918588\n            ],\n            [\n              -121.2506103515625,\n              38.30933576918588\n            ],\n            [\n              -121.2506103515625,\n              37.14499280340638\n            ],\n            [\n              -123.03314208984374,\n              37.14499280340638\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"95","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57876630e4b0d27deb36e19a","contributors":{"authors":[{"text":"Jassby, Alan D.","contributorId":66403,"corporation":false,"usgs":true,"family":"Jassby","given":"Alan","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":642361,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Powell, T.M.","contributorId":88090,"corporation":false,"usgs":true,"family":"Powell","given":"T.M.","email":"","affiliations":[],"preferred":false,"id":642362,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cloern, James E. 0000-0002-5880-6862 jecloern@usgs.gov","orcid":"https://orcid.org/0000-0002-5880-6862","contributorId":1488,"corporation":false,"usgs":true,"family":"Cloern","given":"James","email":"jecloern@usgs.gov","middleInitial":"E.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":642363,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70018034,"text":"70018034 - 1993 - Ice thickness, ablation, and other glaciological measurements on Upper Fremont Glacier, Wyoming","interactions":[],"lastModifiedDate":"2025-06-17T16:54:55.179077","indexId":"70018034","displayToPublicDate":"2013-05-15T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3059,"text":"Physical Geography","active":true,"publicationSubtype":{"id":10}},"title":"Ice thickness, ablation, and other glaciological measurements on Upper Fremont Glacier, Wyoming","docAbstract":"<p><span class=\"single_highlight_class\">Glaciological</span><span>&nbsp;investigations of the&nbsp;</span><span class=\"single_highlight_class\">Upper</span><span>&nbsp;</span><span class=\"single_highlight_class\">Fremont</span><span>&nbsp;</span><span class=\"single_highlight_class\">Glacier</span><span>&nbsp;in the Wind River Range of&nbsp;</span><span class=\"single_highlight_class\">Wyoming</span><span>&nbsp;were conducted during 1990–1991. The&nbsp;</span><span class=\"single_highlight_class\">glaciological</span><span>&nbsp;data will provide baseline information for monitoring future changes to the&nbsp;</span><span class=\"single_highlight_class\">glacier</span><span>&nbsp;and support ongoing research utilizing&nbsp;</span><span class=\"single_highlight_class\">glacial</span><span>-</span><span class=\"single_highlight_class\">ice</span><span>-core composition to reconstruct paleoenvironmental records.&nbsp;</span><span class=\"single_highlight_class\">Ice</span><span>&nbsp;</span><span class=\"single_highlight_class\">thickness</span><span>, determined by radio-echo sounding, ranged from 60 to 172 m in the&nbsp;</span><span class=\"single_highlight_class\">upper</span><span>&nbsp;half of the&nbsp;</span><span class=\"single_highlight_class\">glacier</span><span>. Radio-echo sounding of&nbsp;</span><span class=\"single_highlight_class\">ice</span><span>&nbsp;</span><span class=\"single_highlight_class\">thickness</span><span>&nbsp;at one point was confirmed by drilling 159.7 m to bedrock. The difference between radio-echo sounding depth and&nbsp;</span><span class=\"single_highlight_class\">measured</span><span>&nbsp;drilling depth was about 4 m. Annual&nbsp;</span><span class=\"single_highlight_class\">ablation</span><span>&nbsp;(including snow, firn, and&nbsp;</span><span class=\"single_highlight_class\">ice</span><span>)&nbsp;</span><span class=\"single_highlight_class\">measured</span><span>&nbsp;for the 1990–1991 period averaged about 0.93 m/a. Densification proceeds rapidly on&nbsp;</span><span class=\"single_highlight_class\">Upper</span><span>&nbsp;</span><span class=\"single_highlight_class\">Fremont</span><span>&nbsp;</span><span class=\"single_highlight_class\">Glacier</span><span>.&nbsp;</span><span class=\"single_highlight_class\">Measured</span><span>&nbsp;densities in the near-surface parts of the&nbsp;</span><span class=\"single_highlight_class\">glacier</span><span>&nbsp;ranged from 4.4 x 10</span><sup>5</sup><span>&nbsp;g/m</span><sup>3</sup><span>&nbsp;at the surface to larger than 8.5 x 10</span><sup>5</sup><span>&nbsp;g/m</span><sup>3</sup><span>&nbsp;at depths exceeding 14 m. Surface&nbsp;</span><span class=\"single_highlight_class\">ice</span><span>&nbsp;velocity and direction were monitored from July 1990 to August 1991.&nbsp;</span><span class=\"single_highlight_class\">Ice</span><span>&nbsp;velocity decreased in a downslope direction. The largest&nbsp;</span><span class=\"single_highlight_class\">measured</span><span>&nbsp;velocity was about 3.1 m/a and the smallest was 0.8 m/a. The yearly mean air temperature of the study site during the period from July 11, 1990 to July 10, 1991 was -6.9°. Borehole temperatures from 10-m depths are 0 ± 0.4°. The warmer borehole temperatures relative to the yearly mean air temperature may be caused by the latent heat of freezing, as meltwater from the surface percolates into the&nbsp;</span><span class=\"single_highlight_class\">glacier</span><span>&nbsp;and refreezes.&nbsp;</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02723646.1993.10642488","issn":"02723646","usgsCitation":"Naftz, D.L., and Smith, M., 1993, Ice thickness, ablation, and other glaciological measurements on Upper Fremont Glacier, Wyoming: Physical Geography, v. 14, no. 4, p. 404-414, https://doi.org/10.1080/02723646.1993.10642488.","productDescription":"11 p.","startPage":"404","endPage":"414","costCenters":[],"links":[{"id":228642,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Upper Fremont Glacier","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -109.72994107718391,\n              43.854490295941474\n            ],\n            [\n              -109.72994107718391,\n              42.91105485137706\n            ],\n            [\n              -108.47855150485833,\n              42.91105485137706\n            ],\n            [\n              -108.47855150485833,\n              43.854490295941474\n            ],\n            [\n              -109.72994107718391,\n              43.854490295941474\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"14","issue":"4","noUsgsAuthors":false,"publicationDate":"2013-05-15","publicationStatus":"PW","scienceBaseUri":"505a37f4e4b0c8380cd612f6","contributors":{"authors":[{"text":"Naftz, D. L.","contributorId":40624,"corporation":false,"usgs":true,"family":"Naftz","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":378249,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, M.E.","contributorId":104525,"corporation":false,"usgs":true,"family":"Smith","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":378250,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70047422,"text":"70047422 - 1993 - Map projections","interactions":[],"lastModifiedDate":"2019-10-07T10:56:56","indexId":"70047422","displayToPublicDate":"2013-01-01T14:42:46","publicationYear":"1993","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":362,"text":"General Information Product","active":false,"publicationSubtype":{"id":6}},"title":"Map projections","docAbstract":"A map projection is used to portray all or part of the round Earth on a flat surface. This cannot be done without some distortion. Every projection has its own set of advantages and disadvantages. There is no \"best\" projection. The mapmaker must select the one best suited to the needs, reducing distortion of the most important features. Mapmakers and mathematicians have devised almost limitless ways to project the image of the globe onto paper. Scientists at the U. S. Geological Survey have designed projections for their specific needs—such as the Space Oblique Mercator, which allows mapping from satellites with little or no distortion. This document gives the key properties, characteristics, and preferred uses of many historically important projections and of those frequently used by mapmakers today.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70047422","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1993, Map projections: General Information Product, 2 p., https://doi.org/10.3133/70047422.","productDescription":"2 p.","costCenters":[{"id":210,"text":"Core Science Systems","active":false,"usgs":true}],"links":[{"id":276060,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047422.PNG"},{"id":276057,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70047422/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5200c965e4b009d47a4c23a3","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535571,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70045785,"text":"70045785 - 1993 - Construction aggregates","interactions":[],"lastModifiedDate":"2013-05-05T17:53:34","indexId":"70045785","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2755,"text":"Mining Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Construction aggregates","docAbstract":"Part of a special section on the market performance of industrial minerals in 1992. Production of construction aggregates increased by 4.6 percent in 1992. This increase was due, in part, to the increased funding for transportation and infrastructure projects. The U.S. produced about 1.05 Gt of crushed stone and an estimated 734 Mt of construction sand and gravel in 1992. Demand is expected to increase by about 5 percent in 1993.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Mining Engineering","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"SME","usgsCitation":"Tepordei, V., 1993, Construction aggregates: Mining Engineering, v. 45, p. 567-568.","productDescription":"2 p.","startPage":"567","endPage":"568","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":271843,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51877f64e4b078fc9c244b7a","contributors":{"authors":[{"text":"Tepordei, V.V.","contributorId":34406,"corporation":false,"usgs":true,"family":"Tepordei","given":"V.V.","affiliations":[],"preferred":false,"id":478356,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70043847,"text":"70043847 - 1993 - Exploring maps","interactions":[],"lastModifiedDate":"2024-07-31T16:59:18.350797","indexId":"70043847","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":362,"text":"General Information Product","active":false,"publicationSubtype":{"id":6}},"title":"Exploring maps","docAbstract":"Exploring Maps is an interdisciplinary set of materials on mapping for grades 7-12. Students will learn basic mapmaking and map reading skills and will see how maps can answer fundamental geographic questions: \"Where am I?\" \"What else is here?\" \"Where am I going?\"","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70043847","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1993, Exploring maps: General Information Product, Report: 29 p.; 4 Figures: 59.86 x 22.13 inches or smaller, https://doi.org/10.3133/70043847.","productDescription":"Report: 29 p.; 4 Figures: 59.86 x 22.13 inches or smaller","costCenters":[],"links":[{"id":267861,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://egsc.usgs.gov/isb//pubs/teachers-packets/exploringmaps/"},{"id":431725,"rank":7,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70043847/figure-8-2.pdf","text":"Figure 8-2","linkFileType":{"id":1,"text":"pdf"}},{"id":431724,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70043847/figure-8-1.pdf","text":"Figure 8-1","linkFileType":{"id":1,"text":"pdf"}},{"id":431723,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70043847/figure-7-2.pdf","text":"Figure 7-2","linkFileType":{"id":1,"text":"pdf"}},{"id":431722,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70043847/figure-7-1.pdf","text":"Figure 7-1","linkFileType":{"id":1,"text":"pdf"}},{"id":431721,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70043847/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":267862,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70043847/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5125fe81e4b09d00759cd085","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535435,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70045807,"text":"70045807 - 1993 - Strontium","interactions":[],"lastModifiedDate":"2013-05-06T13:04:18","indexId":"70045807","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2755,"text":"Mining Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Strontium","docAbstract":"Part of a special section reviewing the market performance of industrial minerals in 1992. Imports of celestite (strontium ore) reached nearly 45 kt, which represents an increase of 35 percent over 1991. Mexico supplied almost all of the celestite. Nearly 70 percent of the strontium consumed in the U.S. is used in television picture tube faceplate glass to block X-ray emissions.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Mining Engineering","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"SME","usgsCitation":"Ober, J., 1993, Strontium: Mining Engineering, v. 45, p. 586-587.","productDescription":"2 p.","startPage":"586","endPage":"587","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":271886,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5188d4e8e4b023d2d75b9aa9","contributors":{"authors":[{"text":"Ober, J.A.","contributorId":76351,"corporation":false,"usgs":true,"family":"Ober","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":478379,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70045632,"text":"70045632 - 1993 - Fluorspar","interactions":[],"lastModifiedDate":"2013-04-27T15:54:57","indexId":"70045632","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2755,"text":"Mining Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Fluorspar","docAbstract":"The U.S. produced 50 kt of fluorspar in 1992 and imported nearly 409 kt. Almost all the fluorspar was imported from China. The U.S. consumption of 467 kt represents the lowest level since 1958. This is due to the continuing decrease in consumption by the steel and aluminum industries.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Mining Engineering","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"SME","usgsCitation":"Miller, M., 1993, Fluorspar: Mining Engineering, v. 45, no. 6, p. 569-569.","productDescription":"1 p.","startPage":"569","endPage":"569","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":271535,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"517cf36be4b0d8907b2881db","contributors":{"authors":[{"text":"Miller, M.","contributorId":13178,"corporation":false,"usgs":false,"family":"Miller","given":"M.","email":"","affiliations":[],"preferred":false,"id":477978,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70003908,"text":"70003908 - 1993 - Dynamics and distribution of black abalone populations at San Nicolas Island","interactions":[],"lastModifiedDate":"2013-06-19T13:45:04","indexId":"70003908","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1993","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Dynamics and distribution of black abalone populations at San Nicolas Island","docAbstract":"Dense populations of black abalones (Haliotis cracherodii Leach) were monitored in permanent intertidal plots at nine sites on San Nicolas Island from 1981 through 1990. Densities were essentially constant at all four sites along the north shore of the island throughout the study period. Densities at five sites along the south shore were more variable, possibly reflecting asynchronous variation in recruitment, mortality resulting from wave disturbance, and removal by people. Temporal variation of abalone densities apparently was not influenced by sea otters or abalone withering syndrome during this study. Abalones were strongly aggregated in space. Highest densities occurred in areas of irregular substrata, apparently as a result of preference for crevices and vertical faces. The locations of dense patches were persistent in time.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Third California Islands Symposium: Recent Advances in research on the California Islands","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"Santa Barbara Museum of Natural History","publisherLocation":"Santa Barbara, California","usgsCitation":"VanBlaricom, G., 1993, Dynamics and distribution of black abalone populations at San Nicolas Island, <i>in</i> Third California Islands Symposium: Recent Advances in research on the California Islands, p. 323-334.","productDescription":"12 p.","startPage":"323","endPage":"334","ipdsId":"IP-029448","costCenters":[{"id":621,"text":"Washington Cooperative Fish and Wildlife Research Unit","active":false,"usgs":true}],"links":[{"id":274005,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":274004,"type":{"id":11,"text":"Document"},"url":"https://repository.library.csuci.edu/bitstream/handle/10139/4012/VanBlaricom_1987_DynamicsDistribution~.pdf?sequence=1"}],"country":"United States","state":"California","otherGeospatial":"San Nicolas Island","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.57531,33.214195 ], [ -119.57531,33.284599 ], [ -119.421234,33.284599 ], [ -119.421234,33.214195 ], [ -119.57531,33.214195 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51c2d2e0e4b08857aac4238f","contributors":{"editors":[{"text":"Hochberg, F.G.","contributorId":112350,"corporation":false,"usgs":true,"family":"Hochberg","given":"F.G.","email":"","affiliations":[],"preferred":false,"id":508215,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"VanBlaricom, Glenn R.","contributorId":39273,"corporation":false,"usgs":true,"family":"VanBlaricom","given":"Glenn R.","affiliations":[],"preferred":false,"id":349426,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}