{"pageNumber":"4201","pageRowStart":"105000","pageSize":"25","recordCount":165969,"records":[{"id":3463,"text":"cir969 - 1988 - The role of sediments in the chemistry of aquatic systems - Proceedings of the sediment chemistry workshop, February 8-12, 1982","interactions":[],"lastModifiedDate":"2018-02-08T16:23:52","indexId":"cir969","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"969","title":"The role of sediments in the chemistry of aquatic systems - Proceedings of the sediment chemistry workshop, February 8-12, 1982","docAbstract":"A workshop on sediment chemistry was held at the U.S. Geological Survey National Headquarters in Reston, Virginia, February 8-12, 1982, to discuss the state of the science and possible future directions for research and operational programs in the Water Resources Division of the U.S. Geological Survey. Technical papers presented broad overviews of current conceptual models for and research on the interactions between sediments, water, and biota with respect to the occurrence, distribution, movement, and fate of metals and organic substances in aquatic systems. Five separate disciplines within the overall theme were discussed: physical and chemical partitioning of inorganic constituents; analysis association, and effects of organic constituents; bioavailability of sediment-bound metals; concepts and methods regarding physical properties of sediments; and simulation of transport-related properties. The discussions of the participants regarding needs and possible future directions are summarized. The papers and discussions should help guide individual investigators and policy/program managers alike for the next several years.","conferenceTitle":"Sediment Chemistry Workshop","conferenceDate":"February 8-12, 1982","conferenceLocation":"Reston, VA","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir969","usgsCitation":"1988, The role of sediments in the chemistry of aquatic systems - Proceedings of the sediment chemistry workshop, February 8-12, 1982: U.S. Geological Survey Circular 969, iv, 75 p., https://doi.org/10.3133/cir969.","productDescription":"iv, 75 p.","costCenters":[],"links":[{"id":30474,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1988/0969/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124726,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1988/0969/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1558","contributors":{"editors":[{"text":"Bradford, Wesley L.","contributorId":95451,"corporation":false,"usgs":true,"family":"Bradford","given":"Wesley","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":727924,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Horowitz, Arthur J. 0000-0002-3296-730X horowitz@usgs.gov","orcid":"https://orcid.org/0000-0002-3296-730X","contributorId":1400,"corporation":false,"usgs":true,"family":"Horowitz","given":"Arthur","email":"horowitz@usgs.gov","middleInitial":"J.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true},{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true}],"preferred":true,"id":727925,"contributorType":{"id":2,"text":"Editors"},"rank":2}]}}
,{"id":4032,"text":"cir996 - 1988 - A modification of the U.S. Geological Survey one-sixth order semiquantitative spectrographic method for the analysis of geologic materials that improves limits of determination of some volatile to moderately volatile elements","interactions":[],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"cir996","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"996","title":"A modification of the U.S. Geological Survey one-sixth order semiquantitative spectrographic method for the analysis of geologic materials that improves limits of determination of some volatile to moderately volatile elements","docAbstract":"A modification of the one-sixth order semi-quantitative emission spectrographic method for the analysis of 30 elements in geologic materials (Grimes and Marranzino 1968) improves the limits of determination of some volatile to moderately volatile elements. The modification uses a compound-pendulum-mounted filter to regulate the amount of emitted light passing into the spectrograph. One hundred percent transmission of emitted light is allowed during the initial 20 seconds of the burn, then continually reduced to 40 percent over the next 32 seconds using the pendulum-mounted filter, and followed by an additional 68 seconds of burn time. The reduction of light transmission during the latter part of the burn decreases spectral background and the line emission of less volatile elements commonly responsible for problem-causing interferences. The sensitivity of the method for some geochemically important trace elements commonly determined in mineral exploration (Ag, As, Au, Be, Bi, Cd, Cr, Cu, Pb, Sb, Sn, and Zn) is improved up to five-fold under ideal conditions without compromising precision or accuracy","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir996","usgsCitation":"Detra, D., and Cooley, E.F., 1988, A modification of the U.S. Geological Survey one-sixth order semiquantitative spectrographic method for the analysis of geologic materials that improves limits of determination of some volatile to moderately volatile elements: U.S. Geological Survey Circular 996, iii, 22 p. :ill. ;26 cm., https://doi.org/10.3133/cir996.","productDescription":"iii, 22 p. :ill. ;26 cm.","costCenters":[],"links":[{"id":124729,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1988/0996/report-thumb.jpg"},{"id":31124,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1988/0996/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adeb8","contributors":{"authors":[{"text":"Detra, D.E.","contributorId":72358,"corporation":false,"usgs":true,"family":"Detra","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":148035,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooley, Elmo F.","contributorId":71950,"corporation":false,"usgs":true,"family":"Cooley","given":"Elmo","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":148034,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3432,"text":"cir1007 - 1988 - Manmade organic compounds in the surface waters of the United States; a review of current understanding","interactions":[{"subject":{"id":16037,"text":"ofr87209 - 1987 - Manmade organic compounds in the surface waters of the United States: a review of current understanding","indexId":"ofr87209","publicationYear":"1987","noYear":false,"title":"Manmade organic compounds in the surface waters of the United States: a review of current understanding"},"predicate":"SUPERSEDED_BY","object":{"id":3432,"text":"cir1007 - 1988 - Manmade organic compounds in the surface waters of the United States; a review of current understanding","indexId":"cir1007","publicationYear":"1988","noYear":false,"title":"Manmade organic compounds in the surface waters of the United States; a review of current understanding"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:33","indexId":"cir1007","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1007","title":"Manmade organic compounds in the surface waters of the United States; a review of current understanding","docAbstract":"This report reviews the occurrence and distribution of manmade organic compounds in the surface waters of the United States. On the basis of their aqueous solubilities, nonionic organic compounds partition themselves among water, dissolved organic matter, particulate organic matter, and the lipid reservoirs of aquatic organisms. Ionized organic compounds can be adsorbed to sediments, thereby reducing their aqueous concentrations. Transformation processes of photolysis, hydrolysis, biodegradation, and volatilization can attenuate organic compounds, and attenuation rates commonly follow a first-order kinetic process. \r\n\r\nEight groups of manmade organic compounds are discussed: \r\n\r\n1. Polychlorinated biphenyls and organochlorine insecticides, \r\n2. Carbamate and organophosphorus insecticides, \r\n3. Herbicides, \r\n4. Phenols, \r\n5. Halogenated aliphatic and monocyclic aromatic hydrocarbons, \r\n6. Phthalate esters, \r\n7. Polychlorinated dibenzo-p-dioxins, and \r\n8. Polycyclic aromatic hydrocarbons. \r\n\r\nFor each compound group, data pertaining to use, production, and properties are presented and discussed. Processes that influence the environmental fate of each group, as determined primarily through laboratory studies, are reviewed, and important fate processes are identified. Environmental concentrations of compounds from each group in water, biota, and sediment are given to demonstrate representative values for comparison with concentrations determined during ongoing research. Finally, where data are sufficient, regional and temporal contamination trends in the United States are discussed.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/cir1007","usgsCitation":"Smith, J., Witkowski, P., and Fusillo, T.V., 1988, Manmade organic compounds in the surface waters of the United States; a review of current understanding: U.S. Geological Survey Circular 1007, viii, 92 p. :ill. ;28 cm., https://doi.org/10.3133/cir1007.","productDescription":"viii, 92 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":124429,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1988/1007/report-thumb.jpg"},{"id":30447,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1988/1007/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ae88","contributors":{"authors":[{"text":"Smith, James A.","contributorId":68718,"corporation":false,"usgs":true,"family":"Smith","given":"James A.","affiliations":[],"preferred":false,"id":146898,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Witkowski, P.J.","contributorId":87120,"corporation":false,"usgs":true,"family":"Witkowski","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":146899,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fusillo, Thomas V.","contributorId":106097,"corporation":false,"usgs":true,"family":"Fusillo","given":"Thomas","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":146900,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3627,"text":"cir1019 - 1988 - Review of the general geology and solid-phase geochemical studies in the vicinity of the Central Oklahoma aquifer","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"cir1019","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1019","title":"Review of the general geology and solid-phase geochemical studies in the vicinity of the Central Oklahoma aquifer","docAbstract":"The Central Oklahoma aquifer is the principal source of ground water for municipal, industrial, and rural use in central Oklahoma. Ground water in the aquifer is contained in consolidated sedimentary rocks consisting of the Admire, Council Grove, and Chase Groups, Wellington Formation, and Garber Sandstone and in the unconsolidated Quaternary alluvium and terrace deposits that occur along the major stream systems in the study area. The Garber Sandstone and the Wellington Formation comprise the main flow system and, as such, the aquifer is often referred to as the 'Garber-Wellington aquifer.' The consolidated sedimentary rocks consist of interbedded lenticular sandstone, shale, and siltstone beds deposited in similar deltaic environments in early Permian time. Arsenic, chromium, and selenium are found in the ground water of the Central Oklahoma aquifer in concentrations that, in places, exceed the primary drinking-water standards of the Environmental Protection Agency. Gross-alpha concentrations also exceed the primary standards in some wells, and uranium concentrations are uncommonly high in places. \r\n\r\nAs a prerequisite to a surface and subsurface solid-phase geochemical study, this report summarizes the general geology of the Central Oklahoma study area. Summaries of results from certain previously reported solid-phase geochemical studies that relate to the vicinity of the Central Oklahoma aquifer are also given; including a summary of the analytical results and distribution plots for arsenic, selenium, chromium, thorium, uranium, copper, and barium from the U.S. Department of Energy's National Uranium Resource Evaluation (NURE) Program.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/cir1019","usgsCitation":"Mosier, E.L., and Bullock, J., 1988, Review of the general geology and solid-phase geochemical studies in the vicinity of the Central Oklahoma aquifer: U.S. Geological Survey Circular 1019, iii, 18 p. :ill., maps ;28 cm., https://doi.org/10.3133/cir1019.","productDescription":"iii, 18 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":117413,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1988/1019/report-thumb.jpg"},{"id":30670,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1988/1019/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbe12","contributors":{"authors":[{"text":"Mosier, Elwin L.","contributorId":70374,"corporation":false,"usgs":true,"family":"Mosier","given":"Elwin","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":147284,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bullock, John H.","contributorId":43336,"corporation":false,"usgs":true,"family":"Bullock","given":"John H.","affiliations":[],"preferred":false,"id":147283,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4494,"text":"cir1023 - 1988 - 1988 annual report on Alaska's mineral resources","interactions":[],"lastModifiedDate":"2017-08-29T18:42:41","indexId":"cir1023","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1023","title":"1988 annual report on Alaska's mineral resources","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir1023","usgsCitation":"1988, 1988 annual report on Alaska's mineral resources: U.S. Geological Survey Circular 1023, viii, 57 p. :ill., maps ;28 cm.28 cm., https://doi.org/10.3133/cir1023.","productDescription":"viii, 57 p. :ill., maps ;28 cm.28 cm.","costCenters":[],"links":[{"id":31554,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1988/1023/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117167,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1988/1023/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4914e4b0b290850eede3","contributors":{"editors":[{"text":"Bohn, Diedra","contributorId":90819,"corporation":false,"usgs":true,"family":"Bohn","given":"Diedra","email":"","affiliations":[],"preferred":false,"id":708980,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":3967,"text":"cir1018 - 1988 - Proceedings of the 1987 Exclusive Economic Zone symposium on mapping and research; planning for the next 10 years","interactions":[],"lastModifiedDate":"2012-02-02T00:05:29","indexId":"cir1018","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1018","title":"Proceedings of the 1987 Exclusive Economic Zone symposium on mapping and research; planning for the next 10 years","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/cir1018","usgsCitation":"Lockwood, M., and McGregor, B.A., 1988, Proceedings of the 1987 Exclusive Economic Zone symposium on mapping and research; planning for the next 10 years: U.S. Geological Survey Circular 1018, iii, 175 p. :ill., maps ;28 cm., https://doi.org/10.3133/cir1018.","productDescription":"iii, 175 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":117580,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1988/1018/report-thumb.jpg"},{"id":31053,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1988/1018/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db6605ab","contributors":{"authors":[{"text":"Lockwood, Millington","contributorId":91843,"corporation":false,"usgs":true,"family":"Lockwood","given":"Millington","email":"","affiliations":[],"preferred":false,"id":147916,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGregor, Bonnie A.","contributorId":61022,"corporation":false,"usgs":true,"family":"McGregor","given":"Bonnie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":147915,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3810,"text":"cir997 - 1988 - Geochemical sampling in arid environments by the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2012-02-02T00:05:38","indexId":"cir997","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"997","title":"Geochemical sampling in arid environments by the U.S. Geological Survey","docAbstract":"The U.S. Geological Survey (USGS) is responsible for the geochemical evaluations used for mineral resource assessments of large tracts of public lands in the Western United States. Many of these lands are administered by the Bureau of Land Management (BLM) and are studied to determine their suitability or nonsuitability for wilderness designation. \r\n\r\nMuch of the Western United States is arid or semiarid. This report discusses various geochemical sample media that have been used for evaluating areas in arid environments and describes case histories in BLM wilderness study areas in which stream-sediment and heavy-mineral-concentrate sample media were compared. As a result of these case history studies, the nonmagnetic fraction of panned heavy-mineral concentrates was selected as the most effective medium for reconnaissance geochemical sampling for resources other than gold, in arid areas. Nonmagnetic heavy-mineral-concentrate samples provide the primary analytical information currently used in geochemical interpretations of mineral resource potential assessment of BLM lands.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir997","usgsCitation":"Hinkle, M., 1988, Geochemical sampling in arid environments by the U.S. Geological Survey: U.S. Geological Survey Circular 997, iii, 26 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir997.","productDescription":"iii, 26 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":126521,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1988/0997/report-thumb.jpg"},{"id":30880,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1988/0997/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ade21","contributors":{"authors":[{"text":"Hinkle, Margaret","contributorId":36918,"corporation":false,"usgs":true,"family":"Hinkle","given":"Margaret","affiliations":[],"preferred":false,"id":147646,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3041,"text":"wsp2324 - 1988 - The geochemical evolution of aqueous sodium in the Black Creek Aquifer, Horry and Georgetown counties, South Carolina","interactions":[],"lastModifiedDate":"2017-02-01T10:18:21","indexId":"wsp2324","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2324","title":"The geochemical evolution of aqueous sodium in the Black Creek Aquifer, Horry and Georgetown counties, South Carolina","docAbstract":"The Black Creek aquifer contains dilute seawater near the North Carolina State line, probably the result of incomplete flushing of ancient seawater. Data do not indicate that the dilute seawater has migrated toward areas of fresh ground-water withdrawals. The concentration of chloride in ground-water samples ranges from 5 to 720 milligrams per liter and that of sodium from 160 to 690 milligrams per liter. \r\n\r\nIon-exchange reactions (sodium for calcium and fluoride for hydroxyl) occur with the calcium carbonate dissolution reaction which produces calcium, bicarbonate, and hydroxyl ions. The reaction sequence and stoichiometry result in an aqueous solution in which the sum of bicarbonate and chloride equivalents per liter is equal to the equivalents per liter of sodium. \r\n\r\nCalcium ions are exchanged for sodium ions derived from sodium-rich clays upgradient of the dilute seawater. The cation-exchange reaction equilibrates at a sodium concentration of 280 milligrams per liter. Amounts of sodium greater than 280 milligrams per liter are contributed from dilute seawater. The cation-exchange reaction approaches an equilibrium which represents a mass-action limit in terms of the ratio of sodium to calcium in solution versus the ratio of exchangeable sodium to calcium on clay surfaces. Where the limit of calcium carbonate solubility is approached and dissolution ceases, some precipitation of calcite probably takes place. The dissolution of calcite exposes fossil shark teeth which release fluoride ions to the ground water through anion exchange with aqueous hydroxyl ions.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2324","usgsCitation":"Zack, A.L., and Roberts, I., 1988, The geochemical evolution of aqueous sodium in the Black Creek Aquifer, Horry and Georgetown counties, South Carolina: U.S. Geological Survey Water Supply Paper 2324, iv, 15 p. :ill., maps ;28 cm., https://doi.org/10.3133/wsp2324.","productDescription":"iv, 15 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":139240,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2324/report-thumb.jpg"},{"id":29891,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2324/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South Carolina","county":"Georgetown County, Horry County","otherGeospatial":"Black Creek 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Allen L.","contributorId":47775,"corporation":false,"usgs":true,"family":"Zack","given":"Allen","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":146198,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roberts, Ivan","contributorId":87919,"corporation":false,"usgs":true,"family":"Roberts","given":"Ivan","email":"","affiliations":[],"preferred":false,"id":146199,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4169,"text":"cir1022 - 1988 - Catalog of worldwide tidal bore occurrences and characteristics","interactions":[],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"cir1022","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1022","title":"Catalog of worldwide tidal bore occurrences and characteristics","docAbstract":"Documentation of tidal bore phenomena occurring throughout the world aids in defining the typical geographical setting of tidal bores and enables prediction of their occurrence in remote areas. Tidal bores are naturally occurring, tidally generated, solitary, moving water waves up to 6 meters in height that form upstream in estuaries with semidiurnal or nearly semidiurnal tide ranges exceeding 4 meters. Estuarine settings that have tidal bores typically include meandering fluvial systems with shallow gradients. Bores are well defined, having amplitudes greater than wind- or turbulence-caused waves, and may be undular or breaking. Formation of a bore is dependent on depth and velocity of the incoming tide and river outflow. Bores may occur in series (in several channels) or in succession (marking each tidal pulse). Tidal bores propagate up tidal estuaries a greater distance than the width of the estuary and most occur within 100 kilometers upstream of the estuary mouth. Because they are dynamic, bores cause difficulties in some shipping ports and are targets for eradication. \r\n\r\nTidal bores are known to occur, or to have occurred in the recent past, in at least 67 localities in 16 countries at all latitudes, including every continent except Antarctica. Parts of Argentina, Canada, Central America, China, Mozambique, Madagascar, Northern Europe, North and South Korea, the United Kingdom, and the U.S.S.R. probably have additional undiscovered or unreported tidal bores. \r\n\r\nIn Turnagain Arm estuary in Alaska, bores cause an abrupt increase in salinity, suspended sediment, surface character, and bottom pressure, a decrease in illumination of the water column, and a change in water temperature. Tidal bores occurring in Turnagain Arm, Alaska, have the","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/cir1022","usgsCitation":"Bartsch-Winkler, S., and Lynch, D.K., 1988, Catalog of worldwide tidal bore occurrences and characteristics: U.S. Geological Survey Circular 1022, iii, 17 p. :ill., maps ;28 cm., https://doi.org/10.3133/cir1022.","productDescription":"iii, 17 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":138926,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1988/1022/report-thumb.jpg"},{"id":31278,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1988/1022/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6f8d","contributors":{"authors":[{"text":"Bartsch-Winkler, S.","contributorId":31388,"corporation":false,"usgs":true,"family":"Bartsch-Winkler","given":"S.","affiliations":[],"preferred":false,"id":148334,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lynch, David K.","contributorId":88600,"corporation":false,"usgs":true,"family":"Lynch","given":"David","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":148335,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3334,"text":"cir1035 - 1988 - USGS research on mineral resources - 1989: Program and abstracts","interactions":[{"subject":{"id":70180234,"text":"70180234 - 1988 - Geology and mineral resources of the Port Moller region, western Alaska Peninsula, Aleutian arc: A section in <i>USGS research on mineral resources - 1989: Program and abstracts</i>","indexId":"70180234","publicationYear":"1988","noYear":false,"title":"Geology and mineral resources of the Port Moller region, western Alaska Peninsula, Aleutian arc: A section in <i>USGS research on mineral resources - 1989: Program and abstracts</i>"},"predicate":"IS_PART_OF","object":{"id":3334,"text":"cir1035 - 1988 - USGS research on mineral resources - 1989: Program and abstracts","indexId":"cir1035","publicationYear":"1988","noYear":false,"title":"USGS research on mineral resources - 1989: Program and abstracts"},"id":1}],"lastModifiedDate":"2017-01-27T11:10:38","indexId":"cir1035","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1035","title":"USGS research on mineral resources - 1989: Program and abstracts","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/cir1035","usgsCitation":"1988, USGS research on mineral resources - 1989: Program and abstracts: U.S. Geological Survey Circular 1035, ix, 98 p., https://doi.org/10.3133/cir1035.","productDescription":"ix, 98 p.","numberOfPages":"110","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":118003,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1988/1035/report-thumb.jpg"},{"id":30343,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1988/1035/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f921","contributors":{"editors":[{"text":"Schindler, Katharine S. kschindl@usgs.gov","contributorId":178,"corporation":false,"usgs":true,"family":"Schindler","given":"Katharine","email":"kschindl@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":660838,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":4705,"text":"twri06A1 - 1988 - A modular three-dimensional finite-difference ground-water flow model","interactions":[{"subject":{"id":20038,"text":"ofr83875 - 1984 - A modular three-dimensional finite-difference ground-water flow model","indexId":"ofr83875","publicationYear":"1984","noYear":false,"title":"A modular three-dimensional finite-difference ground-water flow model"},"predicate":"SUPERSEDED_BY","object":{"id":4705,"text":"twri06A1 - 1988 - A modular three-dimensional finite-difference ground-water flow model","indexId":"twri06A1","publicationYear":"1988","noYear":false,"title":"A modular three-dimensional finite-difference ground-water flow model"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:31","indexId":"twri06A1","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"06-A1","title":"A modular three-dimensional finite-difference ground-water flow model","docAbstract":"This report presents a finite-difference model and its associated modular computer program. The model simulates flow in three dimensions. The report includes detailed explanations of physical and mathematical concepts on which the model is based and an explanation of how those concepts are incorporated in the modular structure of the computer program. The modular structure consists of a Main Program and a series of highly independent subroutines called 'modules.' The modules are grouped into 'packages.' Each package deals with a specific feature of the hydrologic system which is to be simulated, such as flow from rivers or flow into drains, or with a specific method of solving linear equations which describe the flow system, such as the Strongly Implicit Procedure or Slice-Successive Overrelaxation. \r\n\r\nThe division of the program into modules permits the user to examine specific hydrologic features of the model independently. This also facilita development of additional capabilities because new packages can be added to the program without modifying the existing packages. The input and output systems of the computer program are also designed to permit maximum flexibility. \r\n\r\nGround-water flow within the aquifer is simulated using a block-centered finite-difference approach. Layers can be simulated as confined, unconfined, or a combination of confined and unconfined. Flow associated with external stresses, such as wells, areal recharge, evapotranspiration, drains, and streams, can also be simulated. The finite-difference equations can be solved using either the Strongly Implicit Procedure or Slice-Successive Overrelaxation. \r\n\r\nThe program is written in FORTRAN 77 and will run without modification on most computers that have a FORTRAN 77 compiler. For each program ,module, this report includes a narrative description, a flow chart, a list of variables, and a module listing.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/twri06A1","issn":"0565-596X","usgsCitation":"McDonald, M.G., and Harbaugh, A.W., 1988, A modular three-dimensional finite-difference ground-water flow model: U.S. Geological Survey Techniques of Water-Resources Investigations 06-A1, 586 p. :ill. ;28 cm., https://doi.org/10.3133/twri06A1.","productDescription":"586 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":139143,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":295,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri6a1/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae07b","contributors":{"authors":[{"text":"McDonald, Michael G.","contributorId":47352,"corporation":false,"usgs":true,"family":"McDonald","given":"Michael","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":149652,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harbaugh, Arlen W. harbaugh@usgs.gov","contributorId":426,"corporation":false,"usgs":true,"family":"Harbaugh","given":"Arlen","email":"harbaugh@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":149651,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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R.","contributorId":50931,"corporation":false,"usgs":true,"family":"Hayes","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":219883,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38469,"text":"pp1440 - 1988 - Quaternary movement along the La Jencia Fault, central New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:09:55","indexId":"pp1440","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1440","title":"Quaternary movement along the La Jencia Fault, central New Mexico","language":"ENGLISH","doi":"10.3133/pp1440","usgsCitation":"Machette, M.N., 1988, Quaternary movement along the La Jencia Fault, central New Mexico: U.S. Geological Survey Professional Paper 1440, 82 p., 2 plates in pocket, https://doi.org/10.3133/pp1440.","productDescription":"82 p., 2 plates in pocket","costCenters":[],"links":[{"id":122558,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1440/report-thumb.jpg"},{"id":65024,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1440/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65025,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1440/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65026,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1440/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a1c7","contributors":{"authors":[{"text":"Machette, M. N.","contributorId":19561,"corporation":false,"usgs":true,"family":"Machette","given":"M.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":219880,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38464,"text":"pp1432 - 1988 - Determination of rock properties by borehole-geophysical and physical-testing techniques and ground-water quality and movement in the Durham Triassic basin, North Carolina","interactions":[],"lastModifiedDate":"2012-02-02T00:09:55","indexId":"pp1432","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1432","title":"Determination of rock properties by borehole-geophysical and physical-testing techniques and ground-water quality and movement in the Durham Triassic basin, North Carolina","language":"ENGLISH","doi":"10.3133/pp1432","usgsCitation":"Brown, C.E., 1988, Determination of rock properties by borehole-geophysical and physical-testing techniques and ground-water quality and movement in the Durham Triassic basin, North Carolina: U.S. Geological Survey Professional Paper 1432, 29 p., 1 plate in pocket, https://doi.org/10.3133/pp1432.","productDescription":"29 p., 1 plate in pocket","costCenters":[],"links":[{"id":119668,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1432/report-thumb.jpg"},{"id":65019,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1432/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65020,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1432/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667676","contributors":{"authors":[{"text":"Brown, C. Erwin","contributorId":96261,"corporation":false,"usgs":true,"family":"Brown","given":"C.","email":"","middleInitial":"Erwin","affiliations":[],"preferred":false,"id":219872,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38506,"text":"pp1393 - 1988 - Upper Cambrian-Lower Ordovician Notch Peak Formation in western Utah","interactions":[{"subject":{"id":23359,"text":"ofr80776 - 1980 - Upper Cambrian-Lower Ordovician Notch Peak Formation in western Utah","indexId":"ofr80776","publicationYear":"1980","noYear":false,"title":"Upper Cambrian-Lower Ordovician Notch Peak Formation in western Utah"},"predicate":"SUPERSEDED_BY","object":{"id":38506,"text":"pp1393 - 1988 - Upper Cambrian-Lower Ordovician Notch Peak Formation in western Utah","indexId":"pp1393","publicationYear":"1988","noYear":false,"title":"Upper Cambrian-Lower Ordovician Notch Peak Formation in western Utah"},"id":1}],"lastModifiedDate":"2012-02-02T00:10:20","indexId":"pp1393","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1393","title":"Upper Cambrian-Lower Ordovician Notch Peak Formation in western Utah","language":"ENGLISH","doi":"10.3133/pp1393","usgsCitation":"Hintze, L., Taylor, M., and Miller, J., 1988, Upper Cambrian-Lower Ordovician Notch Peak Formation in western Utah: U.S. Geological Survey Professional Paper 1393, 30 p.; 1 plate in pocket, https://doi.org/10.3133/pp1393.","productDescription":"30 p.; 1 plate in pocket","costCenters":[],"links":[{"id":110590,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74201.htm","linkFileType":{"id":5,"text":"html"},"description":"74201"},{"id":122233,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1393/report-thumb.jpg"},{"id":65222,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1393/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65223,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1393/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a24e4b07f02db60e680","contributors":{"authors":[{"text":"Hintze, L. F.","contributorId":85589,"corporation":false,"usgs":true,"family":"Hintze","given":"L. F.","affiliations":[],"preferred":false,"id":219957,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, M.E.","contributorId":33713,"corporation":false,"usgs":true,"family":"Taylor","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":219956,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, J.F.","contributorId":29830,"corporation":false,"usgs":true,"family":"Miller","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":219955,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":38450,"text":"pp1408E - 1988 - Water use on the Snake River plain, Idaho and eastern Oregon","interactions":[{"subject":{"id":13849,"text":"ofr85559 - 1986 - Water use on the Snake River plain, Idaho and eastern Oregon","indexId":"ofr85559","publicationYear":"1986","noYear":false,"title":"Water use on the Snake River plain, Idaho and eastern Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":38450,"text":"pp1408E - 1988 - Water use on the Snake River plain, Idaho and eastern Oregon","indexId":"pp1408E","publicationYear":"1988","noYear":false,"chapter":"E","title":"Water use on the Snake River plain, Idaho and eastern Oregon"},"id":1}],"lastModifiedDate":"2013-11-19T15:49:31","indexId":"pp1408E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1408","chapter":"E","title":"Water use on the Snake River plain, Idaho and eastern Oregon","docAbstract":"Amounts of water withdrawn and consumptively used for irrigation \nand other uses on the Snake River Plain were estimated to help deter- \nmine hydrologic effects of ground- and surface-water use. Irrigation is \nthe largest off stream use of water on the plain. Surface-water irriga- \ntion began in the 1840's and increased rapidly through the early 1900's. \nUse of ground water for irrigation accelerated after World War II. In \n1980, about 3.1 million acres were irrigated: 1.0 million acres were \nirrigated with about 2.3 million acre-feet of ground water; 2.0 million \nacres were irrigated with about 12.7 million acre-feet of surface water; \n0.1 million acres were irrigated with combined surface and ground water. \nHistorical changes in aquifer storage and spring discharge are closely \nrelated to changes in irrigation practices.\nIndustries, including aquaculture, withdrew an estimated 1.97 million \nacre-feet of water. Withdrawals for other offstream uses, including public \nand rural supplies, totaled 132,000 acre-feet. Hydroelectric power \ngeneration is an economically important instream use of water. In \n1980, about 52 million acre-feet of surface water was used to generate \n2.6 million megawatt-hours of electricity. Native vegetation evapo- \ntranspired an estimated 3.7 million acre-feet, and 900,000 acre-feet \nevaporated from bare ground and open water.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp1408E","usgsCitation":"Goodell, S.A., 1988, Water use on the Snake River plain, Idaho and eastern Oregon: U.S. Geological Survey Professional Paper 1408, vi, 51 p., https://doi.org/10.3133/pp1408E.","productDescription":"vi, 51 p.","numberOfPages":"63","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":122089,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1408e/report-thumb.jpg"},{"id":64930,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1408e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho;Oregon","otherGeospatial":"Snake River Plain","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.0,42.0 ], [ -117.0,45.0 ], [ -111.0,45.0 ], [ -111.0,42.0 ], [ -117.0,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5eff26","contributors":{"authors":[{"text":"Goodell, S. A.","contributorId":38168,"corporation":false,"usgs":true,"family":"Goodell","given":"S.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":219844,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38449,"text":"pp1408D - 1988 - Solute geochemistry of the Snake River plain regional aquifer system, Idaho and eastern Oregon","interactions":[{"subject":{"id":21461,"text":"ofr86247 - 1987 - Solute geochemistry of the Snake River plain regional aquifer system, Idaho and eastern Oregon","indexId":"ofr86247","publicationYear":"1987","noYear":false,"title":"Solute geochemistry of the Snake River plain regional aquifer system, Idaho and eastern Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":38449,"text":"pp1408D - 1988 - Solute geochemistry of the Snake River plain regional aquifer system, Idaho and eastern Oregon","indexId":"pp1408D","publicationYear":"1988","noYear":false,"chapter":"D","title":"Solute geochemistry of the Snake River plain regional aquifer system, Idaho and eastern Oregon"},"id":1}],"lastModifiedDate":"2013-11-19T15:49:12","indexId":"pp1408D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1408","chapter":"D","title":"Solute geochemistry of the Snake River plain regional aquifer system, Idaho and eastern Oregon","docAbstract":"Four geochemical approaches were used to determine chemical \nreactions controlling solute concentrations in the Snake River Plain \nregional aquifer system: (1) calculation of a solute balance within the \naquifer, (2) identification of weathered products in the aquifer frame- \nwork, (3) comparison of thermodynamic mineral saturation indices with \nplausible solute reactions, and (4) comparison of stable-isotope ratios \nof the solutes with those in the aquifer framework. Solutes in the geo- \nthermal groundwater system underlying the main aquifer were examined \nby calculating thermodynamic mineral saturation indices, stable-isotope \nratios, geothermometry, and radiocarbon dating.\nWater budgets, hydrologic arguments, and isotopic analyses for the \neastern Snake River Plain aquifer system demonstrate that most, if not \nall, water is of local meteoric and not juvenile or formation origin. Thus, \nthe solutes must also originate within the basin. Solute balance, isotopic, \nmineralogic, and thermodynamic arguments suggest that about 20 per- \ncent of the solutes leaving the basin are derived from reactions with \nrocks forming the aquifer framework. Most of the remaining solutes \nare introduced from tributary drainage basins.\nMass-balance calculations, thermodynamic arguments, and petro- \ngraphic observations indicate that calcite and silica are precipitated in \nthe aquifer. Petrographic evidence and thermodynamic arguments sug- \ngest that olivine, pyroxene, plagioclase, pyrite, and anhydrite are being \nweathered from the aquifer framework. Large amounts of sodium, \nchloride, and sulfate, relative to their concentration in the igneous rock, \nare being removed from the aquifer. Release of fluids from inclusions \nin the igneous rocks and initial flushing of grain boundaries and pores \nof detrital marine sediments in interbeds are believed to be a major \nsource of these solutes. Identification and quantification of reactions \ncontrolling solute concentrations in ground water in the eastern plain \nindicate that the aquifer is not a large mixing vessel that simply stores \nand transmits water and solutes but is undergoing diagenesis and is \nboth a source and a sink for solutes.\nEvaluation of solute concentrations and stable-isotope ratios of \nhydrogen, oxygen, carbon, and sulfur along groundwater flowpaths that \ntransect irrigated areas suggests that irrigation water may have altered \nsolute concentrations and isotope ratios in the eastern Snake River Plain \naquifer system. The changes, however, have been small because of the \nsimilarity of solute concentrations and ratios in applied irrigation water \nand in native ground water, and because of rapid movement and large \ndispersivity of the aquifer.\nReactions controlling solutes in the western Snake River basin are \nbelieved to be similar to those in the eastern basin but, because of dif- \nferent hydrologic conditions, a definitive analysis could not be made.\nThe regional geothermal system that underlies the Snake River Plain \ncontains total dissolved solids similar to those in the overlying Snake \nRiver Plain aquifer system but contains higher concentrations of sodium, \nbicarbonate, silica, fluoride, sulfate, chloride, arsenic, boron, and lithium,\nand lower concentrations of calcium, magnesium, and hydrogen. These \nsolutes are believed to be derived from reactions similar to those in the \nSnake River Plain aquifer system, except that ion exchange and hydrol- \nysis play a role in controlling solute concentrations in the geothermal \nsystem.\nGeothermometry calculations of selected ground-water samples from \nknown geothermal areas throughout the basin suggest that the geother- \nmal system is large in areal extent but has relatively low temperatures. \nApproximately half of the silica-quartz calculated water temperatures \nare greater than 90 °C. Radiocarbon dating of geothermal water in the \nSalmon Falls and Bruneau-Grand View areas in the south central part \nof the Snake River basin suggests that residence time of the geother- \nmal water is about 17,700 years.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp1408D","usgsCitation":"Wood, W., and Low, W.H., 1988, Solute geochemistry of the Snake River plain regional aquifer system, Idaho and eastern Oregon: U.S. Geological Survey Professional Paper 1408, vi, 79 p., https://doi.org/10.3133/pp1408D.","productDescription":"vi, 79 p.","numberOfPages":"91","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":123112,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1408d/report-thumb.jpg"},{"id":64929,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1408d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho;Oregon","otherGeospatial":"Snake River Plain","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.0,42.0 ], [ -111.0,45.0 ], [ -117.0,45.0 ], [ -117.0,42.0 ], [ -111.0,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49efe4b07f02db5ed9fc","contributors":{"authors":[{"text":"Wood, Warren W.","contributorId":47770,"corporation":false,"usgs":false,"family":"Wood","given":"Warren W.","affiliations":[{"id":6601,"text":"Michigan State University","active":true,"usgs":false}],"preferred":false,"id":219842,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Low, Walton H.","contributorId":92672,"corporation":false,"usgs":true,"family":"Low","given":"Walton","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":219843,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38514,"text":"pp1343 - 1988 - Precambrian petrochemistry of the northern Park Range, Colorado, and its implications for studies of crustal derivation","interactions":[{"subject":{"id":47337,"text":"ofr80787 - 1980 - Generalized map showing Precambrian rocks and metamorphic facies, keyed to aluminosilicate minerals in meta-shales with excess alumina, northern Park Range, Colorado","indexId":"ofr80787","publicationYear":"1980","noYear":false,"title":"Generalized map showing Precambrian rocks and metamorphic facies, keyed to aluminosilicate minerals in meta-shales with excess alumina, northern Park Range, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":38514,"text":"pp1343 - 1988 - Precambrian petrochemistry of the northern Park Range, Colorado, and its implications for studies of crustal derivation","indexId":"pp1343","publicationYear":"1988","noYear":false,"title":"Precambrian petrochemistry of the northern Park Range, Colorado, and its implications for studies of crustal derivation"},"id":1}],"lastModifiedDate":"2012-02-02T00:10:20","indexId":"pp1343","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1343","title":"Precambrian petrochemistry of the northern Park Range, Colorado, and its implications for studies of crustal derivation","language":"ENGLISH","doi":"10.3133/pp1343","usgsCitation":"Snyder, G.L., Brandt, E.L., and Smith, V.C., 1988, Precambrian petrochemistry of the northern Park Range, Colorado, and its implications for studies of crustal derivation: U.S. Geological Survey Professional Paper 1343, 116 p.; 2 plates in pocket, https://doi.org/10.3133/pp1343.","productDescription":"116 p.; 2 plates in pocket","costCenters":[],"links":[{"id":104606,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4808.htm","linkFileType":{"id":5,"text":"html"},"description":"4808"},{"id":119995,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1343/report-thumb.jpg"},{"id":65250,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1343/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65251,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1343/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65252,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1343/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a85a6","contributors":{"authors":[{"text":"Snyder, G. L.","contributorId":34505,"corporation":false,"usgs":true,"family":"Snyder","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":219970,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brandt, E. L.","contributorId":40997,"corporation":false,"usgs":true,"family":"Brandt","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":219971,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, V. C.","contributorId":74027,"corporation":false,"usgs":true,"family":"Smith","given":"V.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":219972,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":38436,"text":"pp1404C - 1988 - Hydrogeologic framework of the Virginia coastal plain","interactions":[{"subject":{"id":10306,"text":"ofr84728 - 1984 - Hydrogeologic framework of the Virginia coastal plain","indexId":"ofr84728","publicationYear":"1984","noYear":false,"title":"Hydrogeologic framework of the Virginia coastal plain"},"predicate":"SUPERSEDED_BY","object":{"id":38436,"text":"pp1404C - 1988 - Hydrogeologic framework of the Virginia coastal plain","indexId":"pp1404C","publicationYear":"1988","noYear":false,"chapter":"C","title":"Hydrogeologic framework of the Virginia coastal plain"},"id":1}],"lastModifiedDate":"2025-04-17T19:12:46.556498","indexId":"pp1404C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1404","chapter":"C","title":"Hydrogeologic framework of the Virginia coastal plain","docAbstract":"<p>This report defines the hydrogeologic framework of the Virginia Coastal Plain and is a product of a comprehensive regional study to define the geology, hydrology, and geochemistry of the northern Atlantic Coastal Plain aquifer system extending from North Carolina to Long Island, New York. </p><p>The Virginia Coastal Plain consists of an eastward-thickening wedge of generally unconsolidated, interbedded sands and clays, ranging in age from Early Cretaceous to Holocene. These sediments range in thickness from more than 6,000 feet beneath the northeastern part of the Eastern Shore Peninsula to nearly 0 feet along the Fall Line. Eight confined aquifers, eight confining units, and an uppermost water table aquifer are delineated as the hydrogeologic framework of the Coastal Plain sediments in Virginia. The nine regional aquifers, from oldest to youngest, are lower, middle, and upper Potomac, Brightseat, Aquia, Chickahominy-Piney Point, St. Marys-Choptank, Yorktown-Eastover, and Columbia. The Brightseat is a newly identified and correlated aquifer of early Paleoceneage. This study is one of other, similar studies of the Coastal Plain areas in North Carolina, Maryland-Delaware, New Jersey, and Long Island, New York. These combined studies provide a system of hydrogeologic units that can be identified and correlated throughout the northern Atlantic Coastal Plain. </p><p>Data for this study were collected and analyzed from October 1979 to May 1983. The nine aquifers and eight confining units are identified and delineated by use of geophysical logs, drillers' information, and stratigraphic and paleontologic data. By correlating geophysical logs with hydrologic, stratigraphic, and paleontologic data throughout the Coastal Plain, a comprehensive multilayered framework of aquifers and confining units, each with distinct lithologic properties, was developed. Cross sections show the stratigraphic relationships of aquifers and confining units in the hydrogeologic framework of the Virginia Coastal Plain. Maps show confining-unit thicknesses and altitudes of aquifer tops, provide the basis for assigning aquifers to screened intervals of observation and production wells, and are used for the development of a comprehensive observation-well network in the Virginia Coastal Plain.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1404C","usgsCitation":"Meng, A.A., and Harsh, J.F., 1988, Hydrogeologic framework of the Virginia coastal plain: U.S. Geological Survey Professional Paper 1404, Report: iv, 82 p.: 4 Plates: 49.25 x 31.7 inches or smaller, https://doi.org/10.3133/pp1404C.","productDescription":"Report: iv, 82 p.: 4 Plates: 49.25 x 31.7 inches or smaller","costCenters":[],"links":[{"id":484735,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4843.htm","linkFileType":{"id":5,"text":"html"}},{"id":3447,"rank":7,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/pp1404-C/","linkFileType":{"id":5,"text":"html"}},{"id":337655,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/pp1404-C/pdf/pp_1404-c.pdf","text":"Report","size":"8.38 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       38.91668153637508\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db6279ce","contributors":{"authors":[{"text":"Meng, Andrew A. III","contributorId":63858,"corporation":false,"usgs":true,"family":"Meng","given":"Andrew","suffix":"III","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":219819,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harsh, John F.","contributorId":81905,"corporation":false,"usgs":true,"family":"Harsh","given":"John","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":219820,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38433,"text":"pp1449 - 1988 - Paleontology of late Proterozoic and Early Cambrian rocks of east-central Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:09:53","indexId":"pp1449","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1449","title":"Paleontology of late Proterozoic and Early Cambrian rocks of east-central Alaska","language":"ENGLISH","doi":"10.3133/pp1449","usgsCitation":"Allison, C., 1988, Paleontology of late Proterozoic and Early Cambrian rocks of east-central Alaska: U.S. Geological Survey Professional Paper 1449, 50 p., https://doi.org/10.3133/pp1449.","productDescription":"50 p.","costCenters":[],"links":[{"id":165613,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1449/report-thumb.jpg"},{"id":64832,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1449/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689b29","contributors":{"authors":[{"text":"Allison, C.W.","contributorId":46586,"corporation":false,"usgs":true,"family":"Allison","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":219815,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38432,"text":"pp1448 - 1988 - Sporomorph biostratigraphy, floral changes, and paleoclimatology, Eocene and earliest Oligocene of the eastern Gulf Coast","interactions":[],"lastModifiedDate":"2012-02-02T00:09:53","indexId":"pp1448","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1448","title":"Sporomorph biostratigraphy, floral changes, and paleoclimatology, Eocene and earliest Oligocene of the eastern Gulf Coast","language":"ENGLISH","doi":"10.3133/pp1448","usgsCitation":"Frederiksen, N.O., 1988, Sporomorph biostratigraphy, floral changes, and paleoclimatology, Eocene and earliest Oligocene of the eastern Gulf Coast: U.S. Geological Survey Professional Paper 1448, 68 p.; 2 plates in pocket, https://doi.org/10.3133/pp1448.","productDescription":"68 p.; 2 plates in pocket","costCenters":[],"links":[{"id":119211,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1448/report-thumb.jpg"},{"id":64829,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1448/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64830,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1448/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64831,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1448/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4ad0","contributors":{"authors":[{"text":"Frederiksen, N. O.","contributorId":78356,"corporation":false,"usgs":true,"family":"Frederiksen","given":"N.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":219814,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38430,"text":"pp1446 - 1988 - Stratigraphic distribution of fusulinid foraminifera from the Manzano Mountains, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:09:53","indexId":"pp1446","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1446","title":"Stratigraphic distribution of fusulinid foraminifera from the Manzano Mountains, New Mexico","language":"ENGLISH","doi":"10.3133/pp1446","usgsCitation":"Myers, D.A., 1988, Stratigraphic distribution of fusulinid foraminifera from the Manzano Mountains, New Mexico: U.S. Geological Survey Professional Paper 1446, 64 p., [18] leaves of plates : ill., map ; 29 cm. , https://doi.org/10.3133/pp1446.","productDescription":"64 p., [18] leaves of plates : ill., map ; 29 cm. ","costCenters":[],"links":[{"id":122075,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1446/report-thumb.jpg"},{"id":64827,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1446/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629d80","contributors":{"authors":[{"text":"Myers, Donald A.","contributorId":100906,"corporation":false,"usgs":true,"family":"Myers","given":"Donald","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":219812,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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