{"pageNumber":"57","pageRowStart":"1400","pageSize":"25","recordCount":2263,"records":[{"id":16377,"text":"ofr886 - 1988 - Structural evolution of a Grand Canyon breccia pipe; the Ridenour copper-vanadium-uranium mine, Hualapai Indian Reservation, Coconino County, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:07:02","indexId":"ofr886","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"88-6","title":"Structural evolution of a Grand Canyon breccia pipe; the Ridenour copper-vanadium-uranium mine, Hualapai Indian Reservation, Coconino County, Arizona","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr886","usgsCitation":"Verbeek, E.R., Grout, M.A., and Van Gosen, B.S., 1988, Structural evolution of a Grand Canyon breccia pipe; the Ridenour copper-vanadium-uranium mine, Hualapai Indian Reservation, Coconino County, Arizona: U.S. Geological Survey Open-File Report 88-6, i, 75 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr886.","productDescription":"i, 75 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":147824,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0006/report-thumb.jpg"},{"id":45315,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0006/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4aa9","contributors":{"authors":[{"text":"Verbeek, Earl R.","contributorId":64222,"corporation":false,"usgs":true,"family":"Verbeek","given":"Earl","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":172747,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grout, Marilyn A.","contributorId":47343,"corporation":false,"usgs":true,"family":"Grout","given":"Marilyn","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":172746,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Van Gosen, B. S. 0000-0003-4214-3811","orcid":"https://orcid.org/0000-0003-4214-3811","contributorId":97907,"corporation":false,"usgs":true,"family":"Van Gosen","given":"B.","middleInitial":"S.","affiliations":[],"preferred":false,"id":172748,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":39793,"text":"b1713D - 1988 - Mineral resources of the Whipple Mountains and Whipple Mountains Addition Wilderness Study Areas, San Bernardino County, California","interactions":[{"subject":{"id":7331,"text":"ofr82956 - 1982 - Mineral-resource potential of the Whipple Mountains Wilderness Study Area(CDCA-312), San Bernardino County, California","indexId":"ofr82956","publicationYear":"1982","noYear":false,"title":"Mineral-resource potential of the Whipple Mountains Wilderness Study Area(CDCA-312), San Bernardino County, California"},"predicate":"SUPERSEDED_BY","object":{"id":39793,"text":"b1713D - 1988 - Mineral resources of the Whipple Mountains and Whipple Mountains Addition Wilderness Study Areas, San Bernardino County, California","indexId":"b1713D","publicationYear":"1988","noYear":false,"chapter":"D","title":"Mineral resources of the Whipple Mountains and Whipple Mountains Addition Wilderness Study Areas, San Bernardino County, California"},"id":1}],"lastModifiedDate":"2017-07-05T12:49:41","indexId":"b1713D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1713","chapter":"D","title":"Mineral resources of the Whipple Mountains and Whipple Mountains Addition Wilderness Study Areas, San Bernardino County, California","docAbstract":"<p>At the request of the U.S. Bureau of Land Management, approximately 85,100 acres of the Whipple Mountains Wilderness Study Area (CDCA-312) and 1,380 acres of the Whipple Mountains Addition Wilderness Study Area (AZ-050-010) were evaluated for identified mineral resources (known) and mineral resource potential (undiscovered). In this report, the Whipple Mountains and Whipple Mountains Addition Wilderness Study Areas are referred to as simply \"the study area.\" </p><p>Most of the mines and prospects with identified resources in the Whipple Mountains Wilderness Study Area are within areas designated as having mineral resource potential. The area in and around the Turk Silver mine and the Lucky Green group and the area near the northwest boundary of the study area have high mineral resource potential for copper, lead, zinc, gold, and silver. An area along the west boundary of the study area has moderate resource potential for copper lead, zinc, gold, and silver. An area in the east adjacent to the Whipple Mountains Addition Wilderness Study Area has moderate resource potential for copper, gold, and silver resources. One area on the north boundary and one on the southeast boundary of the study area have low mineral resource potential for copper, lead, zinc, gold, and silver. Two areas, one on the north boundary and one inside the east boundary of the study area, have moderate resource potential for manganese. A small area inside the south boundary of the study area has high resource potential for decorative building stone, and the entire study area has low resource potential for&nbsp;sand and gravel and other rock products suitable for construction. Two areas in the eastern part of the study area have low resource potential for uranium. There is no resource potential for oil and gas or geothermal resources in the Whipple Mountains Wilderness Study Area. </p><p>Sites within the Whipple Mountains Wilderness Study Area with identified resources of copper, gold, silver, manganese and (or) decorative building stone are located at the Stewart mine, New American Eagle mine, Turk Silver mine, Twin Lode mine, decorative stone property, Lucky Green group, Blue Cloud mine, Nickel Plate mine, Crescent mine, Quadrangle Copper group, and the Copper Basin mine. </p><p>The Whipple Mountains Addition Wilderness Study Area has moderate resource potential for copper, gold, and silver resources and low resource potential for sand and gravel and other rock products. There is no resource potential for oil and gas or for geothermal energy in the Whipple Mountains Addition Wilderness Study Area. </p><p>Although there are no identified resources in the Whipple Mountains Addition Wilderness Study Area, sites within and immediately adjacent warrant further study because of gold assays from widespread, numerous samples.</p>","largerWorkTitle":"Mineral resources of Wilderness Study Areas: Eastern California Desert Conservation Area","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b1713D","usgsCitation":"Marsh, S.P., Raines, G.L., Diggles, M.F., Howard, K.A., Simpson, R.W., Hoover, D.B., Ridenour, J., Moyle, P.R., and Willett, S.L., 1988, Mineral resources of the Whipple Mountains and Whipple Mountains Addition Wilderness Study Areas, San Bernardino County, California: U.S. Geological Survey Bulletin 1713, Report: vi, 36 p.; Plate: 36.50 x 25.00 inches, https://doi.org/10.3133/b1713D.","productDescription":"Report: vi, 36 p.; Plate: 36.50 x 25.00 inches","startPage":"D1","endPage":"D36","costCenters":[],"links":[{"id":67672,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1713d/report.pdf","text":"Report","size":"2.02 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":173394,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1713d/report-thumb.jpg"},{"id":67671,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1713d/plate-1.pdf","text":"Plate","size":"5.14 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate"}],"country":"United States","state":"California","county":"San Bernardino County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.378662109375,\n              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P.","contributorId":42950,"corporation":false,"usgs":true,"family":"Marsh","given":"Sherman","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":222190,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Raines, Gary L.","contributorId":48162,"corporation":false,"usgs":true,"family":"Raines","given":"Gary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":222194,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Diggles, Michael F. 0000-0002-9946-0247 mdiggles@usgs.gov","orcid":"https://orcid.org/0000-0002-9946-0247","contributorId":810,"corporation":false,"usgs":true,"family":"Diggles","given":"Michael","email":"mdiggles@usgs.gov","middleInitial":"F.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":501,"text":"Office of Science Quality and Integrity","active":true,"usgs":true},{"id":5066,"text":"Office of the Director USGS","active":true,"usgs":true},{"id":5053,"text":"IPDS Training","active":true,"usgs":true}],"preferred":true,"id":222189,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Howard, Keith A. 0000-0002-6462-2947 khoward@usgs.gov","orcid":"https://orcid.org/0000-0002-6462-2947","contributorId":3439,"corporation":false,"usgs":true,"family":"Howard","given":"Keith","email":"khoward@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":222191,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Simpson, Robert W. simpson@usgs.gov","contributorId":1053,"corporation":false,"usgs":true,"family":"Simpson","given":"Robert","email":"simpson@usgs.gov","middleInitial":"W.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":222192,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hoover, Donald B.","contributorId":89877,"corporation":false,"usgs":true,"family":"Hoover","given":"Donald","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":222188,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ridenour, James","contributorId":87540,"corporation":false,"usgs":true,"family":"Ridenour","given":"James","email":"","affiliations":[],"preferred":false,"id":222193,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Moyle, Phillip R.","contributorId":100898,"corporation":false,"usgs":true,"family":"Moyle","given":"Phillip","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":222187,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Willett, Spencee L.","contributorId":48621,"corporation":false,"usgs":true,"family":"Willett","given":"Spencee","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":222195,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70206764,"text":"70206764 - 1988 - Age of native copper mineralization, Keweenaw Peninsula, Michigan","interactions":[],"lastModifiedDate":"2019-11-21T11:33:38","indexId":"70206764","displayToPublicDate":"1988-11-21T11:20:13","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Age of native copper mineralization, Keweenaw Peninsula, Michigan","docAbstract":"<p><span>Amygdaloidal flood basalts and conglomerates are the host for substantial deposits of native copper within the Portage Lake Volcanics in the Keweenaw Peninsula of Michigan. A wide variety of gangue minerals are associated with the regional hydrothermal alteration-mineralization event. Application of the Rb-Sr method to amygdule-filling microcline, calcite, epidote, and chlorite suggests an age of mineralization between 1,060 and 1,047 m.y. (+ or - [asymp] 20 m.y.). These results are supported by a fission track age on epidote of 1,044 + or - 169 m.y. The age of native copper mineralization determined in this study is consistent with geologic evidence which suggests that mineralization postdated the deposition of most or all of the overlying Freda Sandstone. Variable initial&nbsp;</span><sup>87</sup><span>&nbsp;Sr/&nbsp;</span><sup>86</sup><span>&nbsp;Sr ratios between the low Rb/Sr phases suggest mixing of isotopically distinct sources of Sr during the generation and equilibration of the hydrothermal solutions.</span></p>","language":"English","publisher":"Society if Economic Geologist","doi":"10.2113/gsecongeo.83.3.619","usgsCitation":"Bornhorst, T.J., Paces, J.B., Grant, N.K., Obradovich, J., and Huber, N.K., 1988, Age of native copper mineralization, Keweenaw Peninsula, Michigan: Economic Geology, v. 83, no. 3, p. 619-625, https://doi.org/10.2113/gsecongeo.83.3.619.","productDescription":"7 p.","startPage":"619","endPage":"625","costCenters":[],"links":[{"id":369386,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Michigan","otherGeospatial":"Keweenaw Peninsula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.92608642578125,\n              47.15797242686648\n            ],\n            [\n              -88.38226318359375,\n              46.9052455464292\n            ],\n            [\n              -87.47039794921874,\n              47.42251265435723\n            ],\n            [\n              -88.033447265625,\n              47.69682297134991\n            ],\n            [\n              -88.92608642578125,\n              47.15797242686648\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"83","issue":"3","noUsgsAuthors":false,"publicationDate":"1988-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Bornhorst, Theodore J.","contributorId":68375,"corporation":false,"usgs":true,"family":"Bornhorst","given":"Theodore","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":775705,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Paces, James B. 0000-0002-9809-8493 jbpaces@usgs.gov","orcid":"https://orcid.org/0000-0002-9809-8493","contributorId":2514,"corporation":false,"usgs":true,"family":"Paces","given":"James","email":"jbpaces@usgs.gov","middleInitial":"B.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":775706,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grant, Norman K.","contributorId":220769,"corporation":false,"usgs":false,"family":"Grant","given":"Norman","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":775707,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Obradovich, J.","contributorId":53953,"corporation":false,"usgs":true,"family":"Obradovich","given":"J.","email":"","affiliations":[],"preferred":false,"id":775708,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Huber, N. King","contributorId":51284,"corporation":false,"usgs":true,"family":"Huber","given":"N.","email":"","middleInitial":"King","affiliations":[],"preferred":false,"id":775709,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70122682,"text":"70122682 - 1988 - Antler anomalies in tule elk","interactions":[],"lastModifiedDate":"2024-07-12T11:26:50.756469","indexId":"70122682","displayToPublicDate":"1988-11-01T11:54:32","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Antler anomalies in tule elk","docAbstract":"Antler anomalies were evident in tule elk (<i>Cervus elaphus nannodes</i>) within 1 yr of reintroduction to Point Reyes, California (USA). These anomalies are consistent with previously described mineral deficiency-induced anomalies in cervids. The elk were judged deficient in copper. Low levels of copper in soils and vegetation at the release site, exacerbated by possible protein deficiency due to poor range conditions, are postulated as likely causes of the antler anomalies.","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-24.4.656","usgsCitation":"Gogan, P., Jessup, D., and Barrett, R.H., 1988, Antler anomalies in tule elk: Journal of Wildlife Diseases, v. 24, no. 4, p. 656-662, https://doi.org/10.7589/0090-3558-24.4.656.","productDescription":"7 p.","startPage":"656","endPage":"662","numberOfPages":"7","costCenters":[],"links":[{"id":479978,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.7589/0090-3558-24.4.656","text":"Publisher Index Page"},{"id":293109,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53fef0c8e4b01f35f8fd691d","contributors":{"authors":[{"text":"Gogan, Peter J.P.","contributorId":91205,"corporation":false,"usgs":true,"family":"Gogan","given":"Peter J.P.","affiliations":[],"preferred":false,"id":499600,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jessup, David A.","contributorId":43206,"corporation":false,"usgs":false,"family":"Jessup","given":"David A.","affiliations":[{"id":6952,"text":"California Department of Fish and Wildlife","active":true,"usgs":false}],"preferred":false,"id":499598,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barrett, Reginald H.","contributorId":48261,"corporation":false,"usgs":true,"family":"Barrett","given":"Reginald","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":499599,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":33499,"text":"b1713B - 1988 - Mineral resources of the Turtle Mountains Wilderness Study Area, San Bernardino County, California","interactions":[],"lastModifiedDate":"2022-09-29T19:50:32.260331","indexId":"b1713B","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1713","chapter":"B","title":"Mineral resources of the Turtle Mountains Wilderness Study Area, San Bernardino County, California","docAbstract":"<p>At the request of the U.S. Bureau of Land Management, approximately 105,200 acres of the Turtle Mountains Wilderness Study Area (CDCA-307) were evaluated for mineral resources (known) and resource potential (undiscovered). In this report, the area studied is referred to as \"the wilderness study area\" or simply \"the study area\"; any reference to the Turtle Mountain Wilderness Study Area refers only to that part of the wilderness study area for which a mineral survey was requested by the U.S. Bureau of Land Management.</p><p>The wilderness study area is in southeastern San Bernardino County, Calif. Gold, silver, copper, and lead have been mined within and adjacent to the study area. Copper-zinc-silver-gold mineral occurrences are found in the southern part and gold-silver mineral occurrences are found in the northern part of the study area; identified low- to moderate-grade gold-silver resources occur adjacent to the study area along the western boundary. Six areas in the south-central and northwestern parts of the study area have high resource potential, two broad areas have moderate resource potential, and part of the southwest corner has low resource potential for lode gold, silver, and associated copper, lead, zinc, molybdenum, and tungsten. Alluvium locally within one of these areas has moderate resource potential for placer gold and silver, and the entire area has low resource potential for placer gold and silver. There is low resource potential for perlite, ornamental stone (onyx marble and opal), manganese, uranium and thorium, pegmatite minerals, and oil and gas within the study area. Sand and gravel are abundant but are readily available outside the wilderness study area.</p>","largerWorkTitle":"Mineral resources of Wilderness Study Areas: Eastern California Desert Conservation Area, California","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b1713B","usgsCitation":"Howard, K.A., Nielson, J.E., Simpson, R.W., Hazlett, R.W., Alminas, H.V., Nakata, J.K., and McDonnell, J.R., 1988, Mineral resources of the Turtle Mountains Wilderness Study Area, San Bernardino County, California: U.S. Geological Survey Bulletin 1713, Report: vi, 28 p.; Plate: 29.72 x 40.72 inches, https://doi.org/10.3133/b1713B.","productDescription":"Report: vi, 28 p.; Plate: 29.72 x 40.72 inches","costCenters":[],"links":[{"id":407645,"rank":4,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9NBU9PY","text":"USGS data release","description":"USGS data release","linkHelpText":"Digital database of geologic units, contacts, and faults for Mineral Resource Potential Map of the Turtle Mountains Wilderness Study Area, San Bernardino County, California"},{"id":340334,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1713b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":340333,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1713b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":165937,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1713b/report-thumb.jpg"}],"country":"United States","state":"California","county":"San Bernardino County","otherGeospatial":"Turtle Mountains Wilderness Study Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.6,\n              34.5\n            ],\n            [\n              -115,\n              34.5\n            ],\n            [\n              -115,\n              34.1\n            ],\n            [\n              -114.6,\n              34.1\n            ],\n            [\n              -114.6,\n              34.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a00f","contributors":{"authors":[{"text":"Howard, Keith A. 0000-0002-6462-2947 khoward@usgs.gov","orcid":"https://orcid.org/0000-0002-6462-2947","contributorId":3439,"corporation":false,"usgs":true,"family":"Howard","given":"Keith","email":"khoward@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":211397,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nielson, Jane E.","contributorId":9701,"corporation":false,"usgs":true,"family":"Nielson","given":"Jane","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":211403,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Simpson, Robert W. simpson@usgs.gov","contributorId":1053,"corporation":false,"usgs":true,"family":"Simpson","given":"Robert","email":"simpson@usgs.gov","middleInitial":"W.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":211399,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hazlett, Richard W.","contributorId":89201,"corporation":false,"usgs":true,"family":"Hazlett","given":"Richard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":211401,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Alminas, Henry V.","contributorId":59783,"corporation":false,"usgs":true,"family":"Alminas","given":"Henry","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":211400,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Nakata, John K.","contributorId":32518,"corporation":false,"usgs":true,"family":"Nakata","given":"John","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":211398,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"McDonnell, John R. Jr.","contributorId":32898,"corporation":false,"usgs":true,"family":"McDonnell","given":"John","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":211402,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":28258,"text":"wri864053 - 1988 - Yield and quality of ground water from stratified-drift aquifers, Taunton River basin, Massachusetts","interactions":[],"lastModifiedDate":"2023-02-21T14:56:14.468209","indexId":"wri864053","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4053","title":"Yield and quality of ground water from stratified-drift aquifers, Taunton River basin, Massachusetts","docAbstract":"<p>Glacial stratified-drift deposits composed primarily of sand and gravel form the major aquifers in the Taunton River basin. In the northern half of the basin, the aquifers are long, narrow, and thin, and saturated thicknesses range from about 20 feet to slightly more than 100 feet. Aquifer widths range from about 0.1 mile to 1.5 miles, and lengths range from about 1 mile to 5 miles.</p><p>Aquifer yield from storage, representative of short-term yield during severe drought conditions, were estimated for 26 selected aquifers in the basin. For a 30-day pumping period, 14 aquifers have yields less than 5 ft<sup>3</sup>/s (cubic feet per second), 7 have yields of from 5 to 10 ft<sup>3</sup>/s; and 5 have yields of from 10 to 15 ft<sup>3</sup>/s. Aquifer yields under normal climatic conditions were estimated for the 26 aquifers by considering the cumulative yield from intercepted ground-water discharge, induced infiltration, and storage. These yield estimates are related to the estimated duration of flow of the stream that drains the aquifer. The two highest aquifer yields equal or exceed 11.9 and 11.3 ft<sup>3</sup>/s 90 percent of the time, respectively, if minimum stream discharge is maintained at 99.5 percent flow duration. Water for public supply was pumped in 18 of the 26 aquifers during 1983, and all the developed aquifers were pumped at a rate either equal to or greater than 70 percent of the estimated rate of aquifer yield determined in this study.</p><p>The pH of the ground water ranges from 5.4 to 7.0, which categorizes the water as mildly corrosive. Hardness of the ground water ranges from 9 to 112 mg/L (milligrams per liter). No concentrations of sulfate or chloride exceeded EPA recommended limits for drinking water. However, concentrations of sodium exceeded the Massachusetts recommended limit for drinking water for those individuals on a sodium-restricted diet of 20 mg/L in 19 of the samples. Natural concentrations of iron and manganese commonly exceed the limits of 0.3 mg/L and 0.05 mg/L recommended for drinking water.</p><p>Of 51 analyses for trace metals, including arsenic, barium, cadmium, chromium, copper, cyanide, lead, mercury, selenium, silver, zinc, and nickel, only lead, with a concentration of 60 ug/L (micrograms per liter) exceeded the recommended limit of 50 ug/L at one site. In 13 of 74 analyses for selected organic compounds, one or more of the following compounds were detected: Chloroform; carbon tetrachloride; 1,1 dichloroethane; 1,2 transdichloroethylene; tetrachloroethylene; toluene; 1,1,1 trichloroethane; and trichloroethylene. The U.S. Environmental Protection Agency has set Maximum Contaminant Levels (MCLs) for three of these compounds. These three compounds and their MCLs are: Trichloroethylene, 5 ug/L; carbon tetrachloride, 5 ug/L; and 1,1,1-trichloroethane, 200 ug/L. Trichloroethylene was detected in five samples. The concentration of trichloroethylene in one of these five samples exceeded the limit of 5 ug/L. A concentration of carbon tetrachloride of 0.8 ug/L was detected in one sample, which is below the limit of 5 ug/L. Concentrations of 1,1,1 trichloroethane were detected in ten samples, but none exceeded the limit for that compound.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864053","collaboration":"Prepared in cooperation with the Department of Environmental Management Division of Water Resources","usgsCitation":"Lapham, W.W., 1988, Yield and quality of ground water from stratified-drift aquifers, Taunton River basin, Massachusetts: U.S. Geological Survey Water-Resources Investigations Report 86-4053, Report: vii, 69 p.; 2 Plates: 42.00 x 55.68 inches and 42.57 x 55.67 inches, https://doi.org/10.3133/wri864053.","productDescription":"Report: vii, 69 p.; 2 Plates: 42.00 x 55.68 inches and 42.57 x 55.67 inches","costCenters":[],"links":[{"id":413235,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4053/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":413234,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4053/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57083,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4053/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118919,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4053/report-thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Taunton River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -71.41662745828884,\n              41.43500749851978\n            ],\n            [\n              -70.70768488845253,\n              41.43500749851978\n            ],\n            [\n              -70.70768488845253,\n              42.16985112683676\n            ],\n            [\n              -71.41662745828884,\n              42.16985112683676\n            ],\n            [\n              -71.41662745828884,\n              41.43500749851978\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de473","contributors":{"authors":[{"text":"Lapham, Wayne W.","contributorId":74734,"corporation":false,"usgs":true,"family":"Lapham","given":"Wayne","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":199483,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70184466,"text":"70184466 - 1988 - Survival of aluminum and monel bands on black brant","interactions":[],"lastModifiedDate":"2017-03-09T15:10:33","indexId":"70184466","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2881,"text":"North American Bird Bander","active":true,"publicationSubtype":{"id":10}},"title":"Survival of aluminum and monel bands on black brant","docAbstract":"<p>Three recoveries of Black Brant (<i>Branta bernicla</i> <i>nigricans</i>) were recently reported in the \"Significant Encounters\" section of North American Bird Bander (Anon. 1986). At the time of recovery these Brant were 21.5, 22 and at least 22.5 years old. The significance of these recoveries caught my attention as all were of birds banded on the Yukon Delta, Alaska in 1963 by the Alaska Department of Fish and Game. In that year bands made of monel metal, a corrosion-resistant alloy consisting mainly of nickel and copper, were used for the first time in anticipation that they would survive significantly longer than standard aluminum bands in the estuarine and marine habitats used by Brant. Follow-up studies of the experimental banding were conducted by the Yukon Delta National Wildlife Refuge of which I was manager from 1964-1975.</p>","language":"English","publisher":"Western, Inland, and Eastern Bird Banding Associations","usgsCitation":"Lensink, C.J., 1988, Survival of aluminum and monel bands on black brant: North American Bird Bander, v. 13, no. 2, p. 33-35.","productDescription":"3 p.","startPage":"33","endPage":"35","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":337253,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":337248,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.westernbirdbanding.org/publications_NABB.html","text":"Journal's Website"}],"volume":"13","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58c277f9e4b014cc3a3e7706","contributors":{"authors":[{"text":"Lensink, Calvin J.","contributorId":99612,"corporation":false,"usgs":false,"family":"Lensink","given":"Calvin","email":"","middleInitial":"J.","affiliations":[{"id":33810,"text":"National Wildlife Refuge Association","active":true,"usgs":false}],"preferred":false,"id":681626,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1804,"text":"wsp2329 - 1988 - Effects of highway runoff on streamflow and water quality in the Sevenmile Creek basin, a rural area in the Piedmont Province of North Carolina, July 1981 to July 1982","interactions":[],"lastModifiedDate":"2023-04-07T20:35:42.292711","indexId":"wsp2329","displayToPublicDate":"1988-01-01T00:00:00","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":"2329","title":"Effects of highway runoff on streamflow and water quality in the Sevenmile Creek basin, a rural area in the Piedmont Province of North Carolina, July 1981 to July 1982","docAbstract":"An evaluation of water-quality data from streams that receive stormwater runoff from a segment of Interstate Highway 85 in North Carolina indicated increased levels of many constituents compared to levels in nearby undeveloped basins. Additional data collected from a network of dry and wet atmospheric deposition collectors, lysimeter samples, soil surveys, wind measurements, and road sweepings helped define the general sources and migration of chemical substances near the highway. The eight study basins, located in a rural area in the Piedmont of North Carolina, had a combined area of 17.5 square miles and drained a 4.8-mile-long segment of the interstate. The average traffic flow along this section was 25,000 vehicles per day.\r\n\r\nDuring storm runoff, streamflow in basins traversed by the highway rose and fell more rapidly than that in the undeveloped basins. This more rapid response is due to the impervious, paved area of the basins and the manmade drainage systems designed to rapidly move water off the highway.\r\n\r\nAlkalinity, specific conductance, and concentrations of calcium, sodium, and chloride were greater at the highway stations than in the undeveloped basins as a result of highway salting for control of ice. Specific conductance and concentrations of dissolved and total nitrogen peaked at the beginning of each storm event. The data indicated that, for the study basins, highway runoff had little or no effect on suspended sediment, water temperature, dissolved oxygen, and pH. However, the pH at all stations decreased during stormflow because the rainfall drained off by the streams had pH values less than 5.7.\r\n\r\nHigh metals concentrations were found in the soils within 100 feet of the highway and in the soil water infiltrating the soil zone. Chromium, copper, nickel, and zinc concentrations in the streams near the highway generally were above the maximum levels recommended by the U.S. Environmental Protection Agency (EPA) for the protection of aquatic life. Lead and cadmium concentrations frequently exceeded the maximum levels recommended by the EPA for drinking water.\r\n\r\n\r\nThe highway is a source of contaminants to surrounding areas. Particulate and metal loads in dustfall and chemical-constituent concentrations in soils decrease exponentially with distance from the highway. The highest concentrations of contaminants were found on the downwind side. Increased concentrations of metals (cadmium, chromium, iron, lead, nickel, and zinc) in rainfall were observed in samples collected near the highway and in samples collected approximately one-half mile away. Material loading due to dustfall was greater than loading due to rainfall. Loading due to saltated particles, those heavier particles bounced along the highway surface, was higher than loading due to dustfall. Saltation loads were greatest during the winter months because of highway deicing and sanding, which supplied an estimated two-thirds of the saltated materials. The remaining one-third of the saltated load came primarily from the deposition of particles from vehicles. Some of the greatest constituent concentrations were measured in the soil water sampled from the lysimeters located adjacent to the highway.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2329","usgsCitation":"Harned, D., 1988, Effects of highway runoff on streamflow and water quality in the Sevenmile Creek basin, a rural area in the Piedmont Province of North Carolina, July 1981 to July 1982: U.S. Geological Survey Water Supply Paper 2329, vi, 33 p., https://doi.org/10.3133/wsp2329.","productDescription":"vi, 33 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":415468,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25311.htm","linkFileType":{"id":5,"text":"html"}},{"id":26958,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2329/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137031,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2329/report-thumb.jpg"}],"country":"United States","state":"North Carolina","otherGeospatial":"Piedmont Province, Sevenmile Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.223,\n              36.019\n            ],\n            [\n              -79.125,\n              36.019\n            ],\n            [\n              -79.125,\n              36.083\n            ],\n            [\n              -79.223,\n              36.083\n            ],\n            [\n              -79.223,\n              36.019\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aea2c","contributors":{"authors":[{"text":"Harned, Douglas","contributorId":11195,"corporation":false,"usgs":true,"family":"Harned","given":"Douglas","affiliations":[],"preferred":false,"id":144184,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70014465,"text":"70014465 - 1988 - Mechanistic characterization of chloride interferences in electrothermal atomization systems","interactions":[],"lastModifiedDate":"2020-01-12T14:22:27","indexId":"70014465","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Mechanistic characterization of chloride interferences in electrothermal atomization systems","docAbstract":"<p>A computer-controlled spectrometer with a photodiode array detector has been used for wavelength and temperature resolved characterization of the vapor produced by an electrothermal atomizer. The system has been used to study the chloride matrix interference on the atomic absorption spectrometric determination of manganese and copper. The suppression of manganese and copper atom populations by matrix chlorides such as those of calcium and magnesium is due to the gas-phase formation of an analyte chloride species followed by the diffusion of significant fractions of these species from the atom cell prior to completion of the atomization process. The analyte chloride species cannot be formed when matrix chlorides with metal-chloride bond dissociation energies above those of the analyte chlorides are the principal entitles present. The results indicate that multiple wavelength spectrometry used to obtain temperature-resolved spectra is a viable tool in the mechanistic characterization of interference effects observed with electrothermal atomization systems.&nbsp;</p>","language":"English","publisher":"ACS","doi":"10.1021/ac00174a010","issn":"00032700","usgsCitation":"Shekiro, J., Skogerboe, R., and Taylor, H.E., 1988, Mechanistic characterization of chloride interferences in electrothermal atomization systems: Analytical Chemistry, v. 60, no. 23, p. 2578-2582, https://doi.org/10.1021/ac00174a010.","productDescription":"5 p.","startPage":"2578","endPage":"2582","numberOfPages":"5","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":225958,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"60","issue":"23","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a5373e4b0c8380cd6cac4","contributors":{"authors":[{"text":"Shekiro, J.M. Jr.","contributorId":11773,"corporation":false,"usgs":true,"family":"Shekiro","given":"J.M.","suffix":"Jr.","affiliations":[],"preferred":false,"id":368459,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Skogerboe, R.K.","contributorId":7348,"corporation":false,"usgs":true,"family":"Skogerboe","given":"R.K.","email":"","affiliations":[],"preferred":false,"id":368458,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Taylor, Howard E. hetaylor@usgs.gov","contributorId":1551,"corporation":false,"usgs":true,"family":"Taylor","given":"Howard","email":"hetaylor@usgs.gov","middleInitial":"E.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":368460,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70014383,"text":"70014383 - 1988 - Estimation of urban stormwater quality","interactions":[],"lastModifiedDate":"2012-03-12T17:19:30","indexId":"70014383","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Estimation of urban stormwater quality","docAbstract":"Two data-based methods for estimating urban stormwater quality have recently been made available - a planning level method developed by the U.S. Environmental Protection Agency (EPA), and a nationwide regression method developed by the U.S. Geological Survey. Each method uses urban stormwater water-quality constituent data collected for the Nationwide Urban Runoff Program (NURP) during 1979-83. The constituents analyzed include 10 chemical constituents - chemical oxygen demand (COD), total suspended solids (TSS), dissolved solids (DS), total nitrogen (TN), total ammonia plus nitrogen (AN), total phosphorus (TP), dissolved phosphorous (DP), total copper (CU), total lead (PB), and total zinc (ZN). The purpose of this report is to briefly compare features of the two estimation methods.","conferenceTitle":"Hydraulic Engineering: Proceedings of the 1988 National Conference on Hydraulic Engineering","conferenceDate":"8 August 1988 through 12 August 1988","conferenceLocation":"Colorado Springs, CO, USA","language":"English","publisher":"Publ by ASCE","publisherLocation":"New York, NY, United States","isbn":"0872626709; 0872626709","usgsCitation":"Jennings, M.E., and Tasker, G.D., 1988, Estimation of urban stormwater quality, Hydraulic Engineering: Proceedings of the 1988 National Conference on Hydraulic Engineering, Colorado Springs, CO, USA, 8 August 1988 through 12 August 1988, p. 78-83.","startPage":"78","endPage":"83","numberOfPages":"6","costCenters":[],"links":[{"id":225571,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0bbde4b0c8380cd52861","contributors":{"authors":[{"text":"Jennings, Marshall E.","contributorId":55813,"corporation":false,"usgs":true,"family":"Jennings","given":"Marshall","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":368272,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tasker, Gary D.","contributorId":95035,"corporation":false,"usgs":true,"family":"Tasker","given":"Gary","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":368273,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70014346,"text":"70014346 - 1988 - Geologic characterization of seismic sources: Moving into the 1990s","interactions":[],"lastModifiedDate":"2012-03-12T17:19:28","indexId":"70014346","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Geologic characterization of seismic sources: Moving into the 1990s","docAbstract":"The objective of this paper is to discuss leading-edge directions in paleoseismology and seismic geology, particularly as they relate to characterizing seismic sources. The paper builds on earlier articles that discuss some of these trends (Schwartz and Coppersmith, 1986; Schwartz, 1987). There are several areas that appear to be especially important. These are: fault segmentation, which provides a physical framework for evaluating both the size and potential location of future earthquakes on a fault zone; earthquake recurrence models, which provide information on the frequency of different size earthquakes on a fault; and long-term earthquake potential, an area in which significant advances have been made through development of earthquake hazard models that use probabilistic methodology to incorporate the uncertainties in seismic source characterization and the evolving understanding of the earthquake process.","largerWorkTitle":"Geotechnical Special Publication","conferenceTitle":"Earthquake Engineering and Soil Dynamics II - Recent Advances in Ground-Motion Evaluation: Proceedings of the Specialty Conference","conferenceDate":"27 June 1988 through 30 June 1988","conferenceLocation":"Park City, UT, USA","language":"English","publisher":"Publ by ASCE","publisherLocation":"New York, NY, United States","issn":"08950563","usgsCitation":"Schwartz, D.P., 1988, Geologic characterization of seismic sources: Moving into the 1990s, <i>in</i> Geotechnical Special Publication, no. n, Park City, UT, USA, 27 June 1988 through 30 June 1988, p. 1-42.","startPage":"1","endPage":"42","numberOfPages":"42","costCenters":[],"links":[{"id":225950,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"n","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1936e4b0c8380cd558ed","contributors":{"authors":[{"text":"Schwartz, David P. 0000-0001-5193-9200 dschwartz@usgs.gov","orcid":"https://orcid.org/0000-0001-5193-9200","contributorId":1940,"corporation":false,"usgs":true,"family":"Schwartz","given":"David","email":"dschwartz@usgs.gov","middleInitial":"P.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":368188,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70013846,"text":"70013846 - 1988 - Nationwide regression models for predicting urban runoff water quality at unmonitored sites","interactions":[],"lastModifiedDate":"2013-02-19T14:30:13","indexId":"70013846","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3718,"text":"Water Resources Bulletin","printIssn":"0043-1370","active":true,"publicationSubtype":{"id":10}},"title":"Nationwide regression models for predicting urban runoff water quality at unmonitored sites","docAbstract":"Regression models are presented that can be used to estimate mean loads for chemical oxygen demand, suspended solids, dissolved solids, total nitrogen, total ammonia plus nitrogen, total phosphorous, dissolved phosphorous, total copper, total lead, and total zinc at unmonitored sites in urban areas. Explanatory variables include drainage area, imperviousness of drainage basin to infiltration, mean annual rainfall, a land-use indicator variable, and mean minimum January temperature. Model parameters are estimated by a generalized-least-squares regression method that accounts for cross correlation and differences in reliability of sample estimates between sites. The regression models account for 20 to 65 percent of the total variation in observed loads.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Water Resources Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Water Resources Association","doi":"10.1111/j.1752-1688.1988.tb03026.x","issn":"00431370","usgsCitation":"Tasker, G.D., and Driver, N.E., 1988, Nationwide regression models for predicting urban runoff water quality at unmonitored sites: Water Resources Bulletin, v. 24, no. 5, p. 1091-1101, https://doi.org/10.1111/j.1752-1688.1988.tb03026.x.","startPage":"1091","endPage":"1101","numberOfPages":"11","costCenters":[],"links":[{"id":267754,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1752-1688.1988.tb03026.x"},{"id":219899,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"5","noUsgsAuthors":false,"publicationDate":"2007-06-08","publicationStatus":"PW","scienceBaseUri":"505a6299e4b0c8380cd71fe7","contributors":{"authors":[{"text":"Tasker, Gary D.","contributorId":83097,"corporation":false,"usgs":true,"family":"Tasker","given":"Gary","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":366998,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Driver, N. E.","contributorId":63398,"corporation":false,"usgs":true,"family":"Driver","given":"N.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":366997,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1013837,"text":"1013837 - 1988 - Concurrent mobile on-site and in situ striped bass contaminant and water quality studies in the Choptank River and upper Chesapeake Bay","interactions":[],"lastModifiedDate":"2024-02-12T17:29:16.686982","indexId":"1013837","displayToPublicDate":"1988-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Concurrent mobile on-site and <i>in situ</i> striped bass contaminant and water quality studies in the Choptank River and upper Chesapeake Bay","title":"Concurrent mobile on-site and in situ striped bass contaminant and water quality studies in the Choptank River and upper Chesapeake Bay","docAbstract":"<p><i>In situ</i><span>&nbsp;</span>and mobile on-site striped bass prolarval and yearling survival studies were conducted in the Choptank River and in the Chesapeake and Delaware (C &amp; D) Canal area of the Upper Chesapeake Bay. Extensive chemical analyses of both organic and inorganic contaminants in the habitat water were performed and water quality parameters were monitored during these experiments. Surviving yearling striped bass were subjected to histological examination.</p><p>Prolarval survival data from both the<span>&nbsp;</span><i>in situ</i><span>&nbsp;</span>and mobile on-site studies were similar for each spawning area. Prolarval survival ranged from 30 to 45% after 96 h of exposure to Choptank River water in four separate experiments (two<span>&nbsp;</span><i>in situ</i>, two on-site); control survival was greater than 74%. Based on a comparison of laboratory toxicity data and reported field concentrations in the Choptank River for various water quality and contaminant conditions, the following combination of conditions was potentially stressful to striped bass prolarvae: low hardness (36 to 48 mg/L CaCO<sub>3</sub>), monomeric aluminum (0.150 mg/L), cadmium (0.003 mg/L) and copper (0.040 mg/L). Yearling survival in both<span>&nbsp;</span><i>in situ</i><span>&nbsp;</span>and on-site tests ranged from 93 to 100% in both the control and Choptank River water after 9<span>&nbsp;</span><i>d</i><span>&nbsp;</span>of exposure. Survival of striped bass prolarvae in C &amp; D Canal water ranged from 52.5 to 70% after 96 h of exposure in four separate experiments. Control survival of prolarvae was not significantly different. Survival of yearling striped bass in on-site and<span>&nbsp;</span><i>in situ</i><span>&nbsp;</span>tests was 95% or greater in C &amp; D Canal water and control water. Acute contaminant effects were not verified in the C &amp; D Canal area.</p>","language":"English","publisher":"Society of Environmental Toxicology and Chemistry","doi":"10.1002/etc.5620071004","usgsCitation":"Hall, L.W., Bushong, S.J., Ziegenfuss, M., Hall, W.S., and Herman, R.L., 1988, Concurrent mobile on-site and in situ striped bass contaminant and water quality studies in the Choptank River and upper Chesapeake Bay: Environmental Toxicology and Chemistry, v. 7, p. 815-830, https://doi.org/10.1002/etc.5620071004.","productDescription":"16 p.","startPage":"815","endPage":"830","numberOfPages":"16","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132025,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","noUsgsAuthors":false,"publicationDate":"1988-10-01","publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a485c","contributors":{"authors":[{"text":"Hall, L. W. Jr.","contributorId":6010,"corporation":false,"usgs":false,"family":"Hall","given":"L.","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":319307,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bushong, S. J.","contributorId":71927,"corporation":false,"usgs":false,"family":"Bushong","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":319311,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ziegenfuss, M.C.","contributorId":57797,"corporation":false,"usgs":true,"family":"Ziegenfuss","given":"M.C.","email":"","affiliations":[],"preferred":false,"id":319310,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hall, W. S.","contributorId":14773,"corporation":false,"usgs":false,"family":"Hall","given":"W.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":319308,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Herman, R. L.","contributorId":21101,"corporation":false,"usgs":true,"family":"Herman","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":319309,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":33663,"text":"b1803 - 1987 - White mica geochemistry of the Catheart Mountain porphyry copper deposit, Maine","interactions":[],"lastModifiedDate":"2018-10-19T10:41:44","indexId":"b1803","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1803","title":"White mica geochemistry of the Catheart Mountain porphyry copper deposit, Maine","docAbstract":"<p>White micas from hydrothermally altered and mineralized zones in the Catheart Mountain Cu-Mo porphyry deposit have regular compositional variations that are generally related to the contents of copper, total iron, and sulfur in the whole rock. Micas in unmineralized rocks exhibit no such relationship. White mica compositions reflect primarily the control imposed by the celadonitic substitution AIIV +Aiv1 =Si+ (Fe, Mg). </p><p>The variation in white mica composition in the Catheart Mountain porphyry may be explained by superposition and overprinting of mineral assemblages by ore fluids during mineralization and during the waning stages of hydrothermal alteration. Local bulk compositional differences, changing PHao and fluid compositions during mineralization, and superposition of mineral assemblages along microzoned veins contributed to variation in white mica composition. However, the general relation between white mica composition and base-metal content in the mineralized rocks at Catheart Mountain suggests that identification of this white mica population might be useful as an indicator of mineralization gradients. </p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington,D.C.","doi":"10.3133/b1803","usgsCitation":"Ayuso, R.A., 1987, White mica geochemistry of the Catheart Mountain porphyry copper deposit, Maine: U.S. Geological Survey Bulletin 1803, iv, l6 p., https://doi.org/10.3133/b1803.","productDescription":"iv, l6 p.","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":164124,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1803/report-thumb.jpg"},{"id":61566,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1803/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e48d4","contributors":{"authors":[{"text":"Ayuso, Robert A. 0000-0002-8496-9534 rayuso@usgs.gov","orcid":"https://orcid.org/0000-0002-8496-9534","contributorId":2654,"corporation":false,"usgs":true,"family":"Ayuso","given":"Robert","email":"rayuso@usgs.gov","middleInitial":"A.","affiliations":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true},{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":211744,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33428,"text":"b1731A - 1987 - Mineral Resources of the Morey and Fandango Wilderness Study Areas, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-10T00:10:09","indexId":"b1731A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1731","chapter":"A","title":"Mineral Resources of the Morey and Fandango Wilderness Study Areas, Nye County, Nevada","docAbstract":"The Morey (NV-060-191) and Fandango (NV-060-190) Wilderness Study Areas are located in the northern Hot Creek Range about 25 mi north of Warm Springs, Nev. At the request of the Bureau of Land Management, 46,300 acres of the Morey and Fandango Wilderness Study Areas were studied. In this report, the area studied is referred to as 'the wilderness study area', or simply 'the study area'. Geologic, geochemical, geophysical, and mineral surveys were conducted by the USGS and the USBM in 1984 to appraise the identified mineral resources and to assess the mineral resource potential of the study areas. These studies indicate that there are small identified resources of zinc, lead, and silver at the Lead Pipe property in the Fandango Wilderness Study Area, several areas of high potential for the occurrence of gold resources in the Fandango study area, small areas of low and moderate potential for the occurrence of silver, lead, and zinc resources in the Fandango study area, areas of moderate and high potential for the occurrence of silver, lead, and zinc resources in the Morey study area, and an area of low potential for copper, molybdenum, and tin in the Morey study area. Both study areas have low resource potential for petroleum, natural gas, uranium, and geothermal energy.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/b1731A","usgsCitation":"John, D.A., Nash, J.T., Plouff, D., and McDonnell, J.R., 1987, Mineral Resources of the Morey and Fandango Wilderness Study Areas, Nye County, Nevada: U.S. Geological Survey Bulletin 1731, Report: vi, A19; Plate, https://doi.org/10.3133/b1731A.","productDescription":"Report: vi, A19; Plate","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":95975,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1731a/plate-1.pdf","size":"4944","linkFileType":{"id":1,"text":"pdf"}},{"id":167685,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1731a/report-thumb.jpg"},{"id":61306,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1731a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.25,38 ], [ -117.25,39 ], [ -116,39 ], [ -116,38 ], [ -117.25,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db6357ba","contributors":{"authors":[{"text":"John, David A. 0000-0001-7977-9106 djohn@usgs.gov","orcid":"https://orcid.org/0000-0001-7977-9106","contributorId":1748,"corporation":false,"usgs":true,"family":"John","given":"David","email":"djohn@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":211030,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nash, J. Thomas","contributorId":26306,"corporation":false,"usgs":true,"family":"Nash","given":"J.","email":"","middleInitial":"Thomas","affiliations":[],"preferred":false,"id":211031,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Plouff, Donald","contributorId":94657,"corporation":false,"usgs":true,"family":"Plouff","given":"Donald","email":"","affiliations":[],"preferred":false,"id":211033,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McDonnell, John R. Jr.","contributorId":32898,"corporation":false,"usgs":true,"family":"McDonnell","given":"John","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":211032,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":3731,"text":"cir858C - 1987 - Preliminary Metallogenic Map of North America: A listing of deposits by commodity","interactions":[],"lastModifiedDate":"2019-12-20T06:50:54","indexId":"cir858C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"858","chapter":"C","title":"Preliminary Metallogenic Map of North America: A listing of deposits by commodity","docAbstract":"The 4,215 ore deposits shown on the Preliminary Metallogenic Map of North America and contained in the Metallogenic Map file have been sorted by their principal (first-listed) commodities and grouped into metallic and nonmetallic categories. Deposit listings for 56 individual metals and minerals have been assembled using the data base and are arranged alphabetically by country, political subdivision (for the larger countries), and deposit name. Map numbers, major and minor constituents, geographic coordinates, and a geologic code are given for each deposit; additionally, the relative size and deposit class have been derived from the code and are listed separately. \r\n\r\nThe frequencies of individual commodities and commodity groups by type, geographic distribution, and geologic occurrence are summarized in tables, and the relationships of associated commodities to principal commodities in the data base are emphasized in both tables and brief texts. \r\n\r\nIn all, 49 metals and minerals are listed as principal (first or only) commodities and 7 more are shown as 'major' but not principal commodities. (Commodities listed as 'minor' in the data base were not sorted or tabulated separately.) Metals, divided into six subgroups, predominate over nonmetallic minerals by a ratio of about 7 to 1, although in terms of quantities and value the disparity is not so great. Within the metals group, the ranking according to frequency is as follows: base, precious, iron and alloying, other (antimony, beryllium, and others), nuclear-fuel, and light metals. \r\n\r\nThe most frequently occurring commodity in the Metallogenic Map file is gold. Copper is ranked second, both in number of occurrences and as the principal commodity in deposits. Silver is ranked third in frequency of occurrence; lead and zinc are ranked fourth and fifth, respectively. Iron, ranked sixth in frequency of occurrence as a major commodity, is the third most reported principal commodity in the data base, ahead of silver (ranked fourth), lead (ranked fifth), and zinc (ranked sixth).","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/cir858C","issn":"03646017","usgsCitation":"Lee, M.P., Guild, P.W., and Schruben, P.G., 1987, Preliminary Metallogenic Map of North America: A listing of deposits by commodity: U.S. Geological Survey Circular 858, iv, 138 p., https://doi.org/10.3133/cir858C.","productDescription":"iv, 138 p.","costCenters":[],"links":[{"id":30792,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1987/0858c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124663,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1987/0858c/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66c99a","contributors":{"authors":[{"text":"Lee, Michael P.","contributorId":81890,"corporation":false,"usgs":true,"family":"Lee","given":"Michael","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":147496,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Guild, Philip White","contributorId":94285,"corporation":false,"usgs":true,"family":"Guild","given":"Philip","email":"","middleInitial":"White","affiliations":[],"preferred":false,"id":147497,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schruben, Paul G.","contributorId":38974,"corporation":false,"usgs":true,"family":"Schruben","given":"Paul","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":147495,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":16218,"text":"ofr8799 - 1987 - Proterozoic gold, silver, copper, lead, zinc, and tungsten deposits and occurrences in Colorado, an experimental publication on 5 1/4 inch disk for microcomputers that use the DOS operating system","interactions":[],"lastModifiedDate":"2013-02-11T14:29:04","indexId":"ofr8799","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-99","title":"Proterozoic gold, silver, copper, lead, zinc, and tungsten deposits and occurrences in Colorado, an experimental publication on 5 1/4 inch disk for microcomputers that use the DOS operating system","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8799","collaboration":"The USGS does not support this software or technical questions for the software associated with the publication.","usgsCitation":"Taylor, R.B., Sheridan, D.M., and Selner, G., 1987, Proterozoic gold, silver, copper, lead, zinc, and tungsten deposits and occurrences in Colorado, an experimental publication on 5 1/4 inch disk for microcomputers that use the DOS operating system: U.S. Geological Survey Open-File Report 87-99, 1 computer disk ;5 1/4 in., https://doi.org/10.3133/ofr8799.","productDescription":"1 computer disk ;5 1/4 in.","costCenters":[],"links":[{"id":150547,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":267207,"type":{"id":4,"text":"Application Site"},"url":"https://pubs.usgs.gov/of/1987/0099/application.zip"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a91e4b07f02db656b4d","contributors":{"authors":[{"text":"Taylor, R. B.","contributorId":65065,"corporation":false,"usgs":true,"family":"Taylor","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":172441,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sheridan, D. M.","contributorId":26304,"corporation":false,"usgs":true,"family":"Sheridan","given":"D.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":172440,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Selner, G.I.","contributorId":13229,"corporation":false,"usgs":true,"family":"Selner","given":"G.I.","affiliations":[],"preferred":false,"id":172439,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":29793,"text":"wri864037 - 1987 - Chemical quality of precipitation at Greenville, Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:08:57","indexId":"wri864037","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4037","title":"Chemical quality of precipitation at Greenville, Maine","docAbstract":"Weekly composite precipitation samples were collected at a rural site located in Greenville, Maine for analysis of trace metals and organic compounds. Samples collected during February 1982, through May 1984, were analyzed for cadmium, chromium, copper, lead, mercury, nickel, and zinc and during February 1982, through March 1983, for chlorinated hydrocarbon pesticides, pthalate ester plasticizers, and polychlorinated biphenyls. Deposition rates were computed. Data reported by the NADP (National Atmospheric Deposition Program) was used to evaluate the general chemical quality of the precipitation. The precipitation had relatively high concentrations of hydrogen ions, sulfate, and nitrate, compared to other constituents. Of the trace metals included for analysis, only copper, lead, and zinc were consistently detected. Lead concentrations exceeded the U.S. EPA recommended limit for domestic water supply in three samples. High deposition rates for some of the metals were episodic. Alpha-hexachlorocyclohexane was the only organic compound that was consistently detected (maximum 120 nanograms/L). None of the other organic compounds were detected in any of the samples. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864037","usgsCitation":"Smath, J., and Potter, T., 1987, Chemical quality of precipitation at Greenville, Maine: U.S. Geological Survey Water-Resources Investigations Report 86-4037, vi, 54 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri864037.","productDescription":"vi, 54 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119611,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4037/report-thumb.jpg"},{"id":58598,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4037/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bb49","contributors":{"authors":[{"text":"Smath, J.A.","contributorId":15174,"corporation":false,"usgs":true,"family":"Smath","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":202136,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Potter, T.L.","contributorId":75191,"corporation":false,"usgs":true,"family":"Potter","given":"T.L.","email":"","affiliations":[],"preferred":false,"id":202137,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29485,"text":"wri864163 - 1987 - Effects of land use on ground-water quality in central Florida — Preliminary results: U.S. Geological Survey Toxic Waste — Ground-water Contamination Program","interactions":[],"lastModifiedDate":"2022-01-05T21:57:19.082231","indexId":"wri864163","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4163","title":"Effects of land use on ground-water quality in central Florida — Preliminary results: U.S. Geological Survey Toxic Waste — Ground-water Contamination Program","docAbstract":"Groundwater is the principal source of drinking water in central Florida. The most important hydrogeologic unit is the Floridan aquifer system, consisting of fractured limestone and dolomite limestone. Activities of man in areas of recharge to the Floridian aquifer system that may be affecting groundwater quality include: (1) the use of drainage wells for stormwater disposal in urban areas, (2) the use of pesticides and fertilizers in citrus groves, and (3) the mining and processing of phosphate ore in mining areas. Preliminary findings about the impacts of these land uses on ground-water quality by comparison with a fourth land use representing the absence of human activity in another area of recharge are presented. Drainage wells convey excess urban stormwater directly to the Upper Floridian aquifer. The volatile organic compounds are the most common contaminants in ground water. Trace elements such as chromium and lead are entering the aquifer but their movement is apparently attenuated by precipitation reactions associated with high pH or by cation-exchange reactions. Among the trace elements and organic chemicals, most ground-water contamination in citrus production areas is caused by pesticides, which include the organic compounds simazine, ametryne, chlordane, DDE , bromacil, aldicarb, EDB, trifluralin, and diazinon, and the trace elements zinc and copper; other contaminants include benzene, toluene, napthalene, and indene compounds. In the phosphate mining area, constituents of concern are arsenic, selenium, and mercury, and secondarily lead, chromium, cadmium, and others. Organic compounds such as fluorene, naphthalene, di-n-butyl phthalate, alkylated benzenes and naphthalenes, and indene compounds also are entering groundwater. (Author 's abstract)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864163","usgsCitation":"Rutledge, A.T., 1987, Effects of land use on ground-water quality in central Florida — Preliminary results: U.S. Geological Survey Toxic Waste — Ground-water Contamination Program: U.S. Geological Survey Water-Resources Investigations Report 86-4163, v, 49 p., https://doi.org/10.3133/wri864163.","productDescription":"v, 49 p.","costCenters":[],"links":[{"id":393940,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36588.htm"},{"id":58328,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4163/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124031,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4163/report-thumb.jpg"}],"country":"United States","state":"Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82,\n              27.739\n            ],\n            [\n              -81.25,\n              27.739\n            ],\n            [\n              -81.25,\n              29.1980\n            ],\n            [\n              -82,\n              29.1980\n            ],\n            [\n              -82,\n              27.739\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611d98","contributors":{"authors":[{"text":"Rutledge, A. T.","contributorId":38532,"corporation":false,"usgs":true,"family":"Rutledge","given":"A.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":201596,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61034,"text":"mf1834C - 1987 - Maps showing anomalous copper concentrations in stream sediments and heavy-mineral concentrates from the Ajo and Lukeville 1 degree by 2 degrees quadrangles, Arizona","interactions":[],"lastModifiedDate":"2016-08-23T10:01:25","indexId":"mf1834C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1834","chapter":"C","title":"Maps showing anomalous copper concentrations in stream sediments and heavy-mineral concentrates from the Ajo and Lukeville 1 degree by 2 degrees quadrangles, Arizona","docAbstract":"<p>This map is part of a folio of maps of the Ajo and Lukeville 1 &deg; x 2&deg; quadrangles, Arizona, prepared under the Conterminous United States Mineral Assessment Program. Other publications in this folio include U.S. Geological Survey Miscellaneous Field Studies Maps MF-1831-A and MF-1831-B and Open-File Reports 82-119, 82&ndash;599, and 83&ndash;734. Open-File Reports 82-119 and 83&ndash;731 constitute the basic data and initial interpretation on which this discussion is predicated.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1834C","usgsCitation":"Theobald, P., and Barton, H.N., 1987, Maps showing anomalous copper concentrations in stream sediments and heavy-mineral concentrates from the Ajo and Lukeville 1 degree by 2 degrees quadrangles, Arizona: U.S. Geological Survey Miscellaneous Field Studies Map 1834, Plate: 35.48 x 32.10 inches, https://doi.org/10.3133/mf1834C.","productDescription":"Plate: 35.48 x 32.10 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326167,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1834C.JPG"},{"id":327546,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1834-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","country":"United States","state":"Arizona","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114,32 ], [ -114,33 ], [ -112,33 ], [ -112,32 ], [ -114,32 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db60468c","contributors":{"authors":[{"text":"Theobald, P. K.","contributorId":45293,"corporation":false,"usgs":true,"family":"Theobald","given":"P. K.","affiliations":[],"preferred":false,"id":264870,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barton, H. N.","contributorId":99546,"corporation":false,"usgs":true,"family":"Barton","given":"H.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":264871,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":15331,"text":"ofr87453 - 1987 - Chemical analyses of water samples from the Picher mining area, northeast Oklahoma and southeast Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:06:58","indexId":"ofr87453","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-453","title":"Chemical analyses of water samples from the Picher mining area, northeast Oklahoma and southeast Kansas","docAbstract":"Chemical analyses are presented for 169 water samples from Tar Creek drainage and the Picher lead-zinc mining area of northeast Oklahoma and southeast Kansas. Water samples were taken from November 1983 through February 1986 from the abandoned mines, from points of mine-water discharge, and from surface-water locations upstream and downstream from mine discharge area. The pH, temperature, alkalinity, dissolved oxygen, and specific conductance were measured in the field. Laboratory analyses routinely included the major ions plus aluminum, cadmium, copper, iron, lead, manganese, nickel, and zinc. Non-routine analyses of dissolved gases and tritium are presented. Stable carbon-isotope ratios for 11 mine-water samples and three carbonate-rock samples are reported. Miscellaneous stream-discharge measurements made at the time of sampling or taken from gaging-station records are included in the report.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87453","usgsCitation":"Parkhurst, D.L., 1987, Chemical analyses of water samples from the Picher mining area, northeast Oklahoma and southeast Kansas: U.S. Geological Survey Open-File Report 87-453, iv, 43 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr87453.","productDescription":"iv, 43 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":147972,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":997,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1987/ofr87-453/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4a15","contributors":{"authors":[{"text":"Parkhurst, David L. 0000-0003-3348-1544 dlpark@usgs.gov","orcid":"https://orcid.org/0000-0003-3348-1544","contributorId":1088,"corporation":false,"usgs":true,"family":"Parkhurst","given":"David","email":"dlpark@usgs.gov","middleInitial":"L.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":170969,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57057,"text":"b1674B - 1987 - A resource assessment of copper and nickel sulfides within the Mountain View area of the Stillwater Complex, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:12:03","indexId":"b1674B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1674","chapter":"B","title":"A resource assessment of copper and nickel sulfides within the Mountain View area of the Stillwater Complex, Montana","language":"ENGLISH","doi":"10.3133/b1674B","usgsCitation":"Attanasi, E.D., and Bawiec, W., 1987, A resource assessment of copper and nickel sulfides within the Mountain View area of the Stillwater Complex, Montana: U.S. Geological Survey Bulletin 1674, p. B1-B27, https://doi.org/10.3133/b1674B.","productDescription":"p. B1-B27","costCenters":[],"links":[{"id":181870,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1674b/report-thumb.jpg"},{"id":88233,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1674b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a83a5","contributors":{"authors":[{"text":"Attanasi, E. D. 0000-0001-6845-7160","orcid":"https://orcid.org/0000-0001-6845-7160","contributorId":107672,"corporation":false,"usgs":true,"family":"Attanasi","given":"E.","middleInitial":"D.","affiliations":[],"preferred":false,"id":256193,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bawiec, W.J.","contributorId":71540,"corporation":false,"usgs":true,"family":"Bawiec","given":"W.J.","affiliations":[],"preferred":false,"id":256192,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14887,"text":"ofr87543 - 1987 - Data-collection methods and data summary for the assessment of water quality in Cedar Creek, west-central Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:06:54","indexId":"ofr87543","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-543","title":"Data-collection methods and data summary for the assessment of water quality in Cedar Creek, west-central Illinois","docAbstract":"A water-quality, data-collection network on a 26.2-mile reach of Cedar Creek in west-central Illinois was operated from May through December 1985 and from March through October 1986. The study reach drains a 60.8-square-mile area of predominantly agricultural land. However, the city of Galesburg contributes combined- and storm-sewer discharge to the creek that can affect the water quality.\r\nThis report presents the streamflow and water-quality data collected and describes the methods and instrumentation used. Continuous discharge data were determined at eight gaging stations--five on the main stem and three on tributaries of Cedar Creek. Flows ranged from 0 to 1,200 cubic feet per second. A total of 8 storm sewers and 51 combined sewers were monitored or inspected as part of the study.\r\n\r\nContinuous precipitation data were collected at five sites. The maximum hourly precipitation intensity during the study period was 1.97 inches per hour. The maximum total precipitation for a storm during the study period was 4.16 inches.\r\n\r\nSediment-oxygen-demand rates were measured at 45 locations in the creek. The measured sediment-oxygen-demand rates ranged from 0.4 to 9.1 grams of oxygen per square meter per day. Ninety-seven bottom-material samples were collected and analyzed for chemical oxygen demand, percentage of volatile organic constituents, and concentrations of total organic plus ammonia nitrogen, arsenic, cadmium, chromium, copper, iron, lead, manganese, mercury, and zinc.\r\n\r\nTraveltime and reaeration rates were determined for 15 subreaches of Cedar Creek during various flow conditions. The reaeration rates ranged from 3.10 to 20.8 per day.\r\n\r\nThree intensive diel (24-hour) data collections were conducted during low-flow conditions. Data included dissolved oxygen concentration, biochemical oxygen demand, nutrient concentrations, and metal concentrations. During storm-related high-flow conditions, water-quality samples were collected at 5 main-stem sites, 3 tributary sites, the Galesburg wastewater treatment-facility outfall, and 15 sewer outfalls. These samples were analyzed for nutrients and metals, suspended solids, chemical oxygen demands, and biochemical oxygen demands.\r\n\r\nThis report describes methods for measuring stage, discharge, precipitation, sediment oxygen demand, traveltime, and reaeration rate. Collection methods for bottom-material samples, diel water-quality data and samples, combined-sewer overflow frequency and duration, and storm- related sampling of combined sewers, storm sewers, and streams are described. A brief discussion of streamflow computation methods also is presented.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87543","usgsCitation":"McFarlane, R., Freeman, W., and Schmidt, A., 1987, Data-collection methods and data summary for the assessment of water quality in Cedar Creek, west-central Illinois: U.S. Geological Survey Open-File Report 87-543, vi, 177 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr87543.","productDescription":"vi, 177 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":146825,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0543/report-thumb.jpg"},{"id":43693,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0543/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db67437a","contributors":{"authors":[{"text":"McFarlane, R.D.","contributorId":105728,"corporation":false,"usgs":true,"family":"McFarlane","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":170184,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Freeman, W.O.","contributorId":30238,"corporation":false,"usgs":true,"family":"Freeman","given":"W.O.","email":"","affiliations":[],"preferred":false,"id":170182,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schmidt, A.R.","contributorId":79898,"corporation":false,"usgs":true,"family":"Schmidt","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":170183,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":4262,"text":"cir975 - 1987 - The Conterminous United States Mineral Assessment Program: Background information to accompany folio of geologic and mineral resource maps of the Silver City 1° x 2° quadrangle, New Mexico and Arizona","interactions":[],"lastModifiedDate":"2021-09-29T11:58:38.525386","indexId":"cir975","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"975","title":"The Conterminous United States Mineral Assessment Program: Background information to accompany folio of geologic and mineral resource maps of the Silver City 1° x 2° quadrangle, New Mexico and Arizona","docAbstract":"<p>The Silver City 1° x 2° quadrangle, consisting of about 20,650 km2 in southwestern New Mexico and southeastern Arizona, has been investigated by a multidisciplinary research team for the purpose of assessing its mineral resource potential. The results of this investigation are in a folio of 21 maps that contain detailed information on the geology, geochemistry, geophysics, mineral deposits, and potential mineral resources of the quadrangle. This Circular provides background information on the various studies and integrates the component maps. It contains an extensive selected bibliography pertinent to the geology and mineral deposits of the quadrangle. The quadrangle has produced more than $3.5 billion in mineral products since about 1850 and contains significant resources of gold, silver, copper, molybdenum, lead, zinc, iron, manganese-iron, zeolite minerals, and possibly tin and tungsten.</p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/cir975","usgsCitation":"Richter, D.H., Houser, B.B., Watts, K.C., Klein, D.P., Sharp, W.N., Drewes, H., Hedlund, D.C., Raines, G.L., and Hassemer, J., 1987, The Conterminous United States Mineral Assessment Program: Background information to accompany folio of geologic and mineral resource maps of the Silver City 1° x 2° quadrangle, New Mexico and Arizona: U.S. Geological Survey Circular 975, iii, 22 p., https://doi.org/10.3133/cir975.","productDescription":"iii, 22 p.","costCenters":[],"links":[{"id":389894,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24031.htm"},{"id":123190,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1987/0975/report-thumb.jpg"},{"id":31374,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1987/0975/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona, New Mexico","otherGeospatial":"Silver City 1° x 2° quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110,\n              32\n            ],\n            [\n              -108,\n              32\n            ],\n            [\n              -108,\n              33\n            ],\n            [\n              -110,\n              33\n            ],\n            [\n              -110,\n              32\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ecb4","contributors":{"authors":[{"text":"Richter, Donald H.","contributorId":61021,"corporation":false,"usgs":true,"family":"Richter","given":"Donald","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":148610,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Houser, B. B.","contributorId":46092,"corporation":false,"usgs":true,"family":"Houser","given":"B.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":148607,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Watts, K. C.","contributorId":49344,"corporation":false,"usgs":true,"family":"Watts","given":"K.","middleInitial":"C.","affiliations":[],"preferred":false,"id":148608,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Klein, D. P.","contributorId":36555,"corporation":false,"usgs":true,"family":"Klein","given":"D.","email":"","middleInitial":"P.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":148606,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sharp, W. N.","contributorId":21958,"corporation":false,"usgs":true,"family":"Sharp","given":"W.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":148605,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Drewes, Harald","contributorId":52567,"corporation":false,"usgs":true,"family":"Drewes","given":"Harald","affiliations":[],"preferred":false,"id":148609,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Hedlund, D. C.","contributorId":101624,"corporation":false,"usgs":true,"family":"Hedlund","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":148612,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Raines, G. L.","contributorId":90720,"corporation":false,"usgs":true,"family":"Raines","given":"G.","middleInitial":"L.","affiliations":[],"preferred":false,"id":148611,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Hassemer, J.R.","contributorId":18761,"corporation":false,"usgs":true,"family":"Hassemer","given":"J.R.","affiliations":[],"preferred":false,"id":148604,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":28042,"text":"wri874146 - 1987 - Trace-metal leaching from plumbing materials exposed to acidic ground water in three areas of the coastal plain of New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:08:25","indexId":"wri874146","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4146","title":"Trace-metal leaching from plumbing materials exposed to acidic ground water in three areas of the coastal plain of New Jersey","docAbstract":"The U.S. Geological Survey analyzed trace metal concentrations in tap water from domestic wells in newly constructed homes in Berkeley Township, Ocean County and Galloway Township, Atlantic County, N. J. The potable water distribution systems in all of the homes sampled are constructed primarily of copper with lead-based solder points. Home water treatment is used in Berkeley Township but not in Galloway Township. Tap water was collected after the water had been standing in the pipes overnight. In Berkeley, 6 to 11 samples exceeded both the U.S. Environmental Protection Agency 's primary drinking water regulation (DWR) for lead (50 microgram/L) and the secondary drinking water regulation (SDWR) for copper (1,000 microgram/L). In Galloway, 12 of 14 samples exceeded the DWR for lead and 13 of 14 exceeded the SDWR for copper. After collecting the standing-water samples, the water was left running for 15 minutes and a second sample was collected. None of the running-water samples exceeded the regulations for lead or copper. Available data suggest a correlation between the residence time of soft, acidic groundwater in new home plumbing systems and elevated trace-metal concentrations in drinking water derived from domestic wells within the New Jersey Coastal Plain. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874146","usgsCitation":"Kish, G.R., Macy, J.A., and Mueller, R., 1987, Trace-metal leaching from plumbing materials exposed to acidic ground water in three areas of the coastal plain of New Jersey: U.S. Geological Survey Water-Resources Investigations Report 87-4146, iv, 19 p. :ill., map ;28 cm., https://doi.org/10.3133/wri874146.","productDescription":"iv, 19 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":157950,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4146/report-thumb.jpg"},{"id":56880,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4146/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f1a0e","contributors":{"authors":[{"text":"Kish, G. R.","contributorId":65118,"corporation":false,"usgs":true,"family":"Kish","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":199118,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Macy, J. A.","contributorId":10047,"corporation":false,"usgs":true,"family":"Macy","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":199117,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mueller, R.T.","contributorId":6481,"corporation":false,"usgs":true,"family":"Mueller","given":"R.T.","email":"","affiliations":[],"preferred":false,"id":199116,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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