{"pageNumber":"5374","pageRowStart":"134325","pageSize":"25","recordCount":184769,"records":[{"id":33325,"text":"b1514 - 1982 - Mineral resources of proposed additions to the Salmon-Trinity Alps Primitive Area, California","interactions":[{"subject":{"id":17362,"text":"ofr7471 - 1974 - Mineral resources of proposed additions to the Salmon-Trinity Alps Primitive Area, California","indexId":"ofr7471","publicationYear":"1974","noYear":false,"title":"Mineral resources of proposed additions to the Salmon-Trinity Alps Primitive Area, California"},"predicate":"SUPERSEDED_BY","object":{"id":33325,"text":"b1514 - 1982 - Mineral resources of proposed additions to the Salmon-Trinity Alps Primitive Area, California","indexId":"b1514","publicationYear":"1982","noYear":false,"title":"Mineral resources of proposed additions to the Salmon-Trinity Alps Primitive Area, California"},"id":1}],"lastModifiedDate":"2023-03-15T18:57:00.342949","indexId":"b1514","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","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":"1514","title":"Mineral resources of proposed additions to the Salmon-Trinity Alps Primitive Area, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1514","usgsCitation":"Hotz, P.E., Greene, R.C., Close, T.J., and Evans, R.K., 1982, Mineral resources of proposed additions to the Salmon-Trinity Alps Primitive Area, California: U.S. Geological Survey Bulletin 1514, Report: vii, 54 p.; 1 Plate: 31.00 x 25.00 inches, https://doi.org/10.3133/b1514.","productDescription":"Report: vii, 54 p.; 1 Plate: 31.00 x 25.00 inches","costCenters":[],"links":[{"id":109730,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21600.htm","linkFileType":{"id":5,"text":"html"},"description":"21600"},{"id":61152,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1514/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61151,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1514/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":164079,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1514/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Salmon-Trinity Alps Primitive Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -123.5,\n              41.317\n            ],\n            [\n              -123.5,\n              40.767\n            ],\n            [\n              -122.667,\n              40.767\n            ],\n            [\n              -122.667,\n              41.317\n            ],\n            [\n              -123.5,\n              41.317\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606e16","contributors":{"authors":[{"text":"Hotz, Preston Enslow","contributorId":15191,"corporation":false,"usgs":true,"family":"Hotz","given":"Preston","email":"","middleInitial":"Enslow","affiliations":[],"preferred":false,"id":210500,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Greene, R. C.","contributorId":88347,"corporation":false,"usgs":true,"family":"Greene","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":210502,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Close, T. J.","contributorId":23137,"corporation":false,"usgs":true,"family":"Close","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":210501,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Evans, R. K.","contributorId":7719,"corporation":false,"usgs":true,"family":"Evans","given":"R.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":210499,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70186628,"text":"70186628 - 1982 - Rifting his­tory and structural development of the continental margin north of Alaska","interactions":[],"lastModifiedDate":"2017-04-06T11:49:46","indexId":"70186628","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Rifting his­tory and structural development of the continental margin north of Alaska","docAbstract":"<p>Seismic-reflection profiles in the Alaskan Beaufort Sea and onshore geology indicate that the continental margin north of Alaska is of Atlantic type. Rifting appears to have begun in earliest Jurassic time, about 190 to 185 m.y. ago, when crustal extension created a rift-valley system beneath the Beaufort shelf and part of the adjacent coastal plain. Subsequent crustal warming caused rift-margin uplift and erosion, created a breakup unconformity, and initiated breakup and seafloor spreading in the Canada Basin about 125 m.y. ago. Subsequent cooling caused rapid subsidence of the margin, which was followed by vigorous progradation of the present continental terrace of the Beaufort Sea beginning in Albian time.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"M 34: Studies in continental margin geology","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"American Association of Petroleum Geologists","usgsCitation":"Grantz, A., and May, S.D., 1982, Rifting his­tory and structural development of the continental margin north of Alaska, chap. <i>of</i> M 34: Studies in continental margin geology, p. 77-100.","productDescription":"24 p. ","startPage":"77","endPage":"100","costCenters":[],"links":[{"id":339316,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58e7540fe4b09da6799c0cd2","contributors":{"authors":[{"text":"Grantz, Arthur agrantz@usgs.gov","contributorId":2585,"corporation":false,"usgs":true,"family":"Grantz","given":"Arthur","email":"agrantz@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":690083,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"May, S. D.","contributorId":12856,"corporation":false,"usgs":true,"family":"May","given":"S.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":690084,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70185335,"text":"70185335 - 1982 - Population and status of Emperor Geese along the north side of the Alaska Peninsula","interactions":[],"lastModifiedDate":"2018-07-15T10:53:04","indexId":"70185335","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3764,"text":"Wildfowl","onlineIssn":"2052-6458","printIssn":"0954-6324","active":true,"publicationSubtype":{"id":10}},"title":"Population and status of Emperor Geese along the north side of the Alaska Peninsula","docAbstract":"<p><span>We gathered information on the timing of spring and autumn migration of Emperor Geese <i>Anser canagicus</i> from Nelson Lagoon, the age ratios of geese during autumn migration, and the numbers of geese in estuaries along the north side of the Alaska Peninsula and Bristol Bay during spring and autumn migration. Birds staged in most of the lagoons and bays along the north side of the Alaska Peninsula, but Nelson Lagoon and Seal Islands Lagoon were the most heavily used. Geese concentrated in Nelson Lagoon for about six to eight weeks in both spring and autumn. We suspect that the population of Emperor Geese in Alaska may have declined by as much as 34% between the 1960's and 1981. Although the average number of young per successful breeding pair has remained high during this period, the overall proportion of young in the population has been extremely low, at least during the past five years. More studies are necessary to determine factors influencing the status of this species.</span></p>","language":"English","publisher":"Wildfowl & Wetlands Trust","usgsCitation":"Petersen, M.R., and Gill, R., 1982, Population and status of Emperor Geese along the north side of the Alaska Peninsula: Wildfowl, v. 33, p. 31-38.","productDescription":"8 p.","startPage":"31","endPage":"38","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":337880,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":337879,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://wildfowl.wwt.org.uk/index.php/wildfowl/article/view/647"}],"country":"United States","state":"Alaska","otherGeospatial":"Alaska Peninsula","volume":"33","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d0ea1fe4b0236b68f673b3","contributors":{"authors":[{"text":"Petersen, Margaret R. 0000-0001-6082-3189 mrpetersen@usgs.gov","orcid":"https://orcid.org/0000-0001-6082-3189","contributorId":167729,"corporation":false,"usgs":true,"family":"Petersen","given":"Margaret","email":"mrpetersen@usgs.gov","middleInitial":"R.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":685220,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gill, Robert E. Jr. 0000-0002-6385-4500 rgill@usgs.gov","orcid":"https://orcid.org/0000-0002-6385-4500","contributorId":171747,"corporation":false,"usgs":true,"family":"Gill","given":"Robert E.","suffix":"Jr.","email":"rgill@usgs.gov","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":685221,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70186167,"text":"70186167 - 1982 - Volatilization of organic compounds from streams","interactions":[],"lastModifiedDate":"2023-02-23T17:21:18.600332","indexId":"70186167","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2255,"text":"Journal of Environmental Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Volatilization of organic compounds from streams","docAbstract":"<p><span>Mass-transfer coefficients for the volatilization of ethylene and propane were correlated with the hydraulic and geometric properties of seven streams, and predictive equations were developed. The equations were evaluated using a normalized root-mean-square error as the criterion of comparison. The two best equations were a two-variable equation containing the energy dissipated per unit mass per unit time and the average depth of flow and a three-variable equation containing the average velocity, the average depth of flow, and the slope of the stream. Procedures for adjusting the ethylene and propane coefficients for other organic compounds were evaluated. These procedures are based on molecular diffusivity, molecular diameter, or molecular weight. Because of limited data, none of these procedures have been extensively verified. Therefore, until additional data become available, it is suggested that the mass-transfer coefficient be assumed to be inversely proportional to the square root of the molecular weight.</span></p>","language":"English","publisher":"American Society of Civil Engineers","doi":"10.1061/JEEGAV.0001356","usgsCitation":"Rathburn, R.E., and Tai, D.Y., 1982, Volatilization of organic compounds from streams: Journal of Environmental Engineering, v. 108, p. 973-989, https://doi.org/10.1061/JEEGAV.0001356.","productDescription":"17 p.","startPage":"973","endPage":"989","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338830,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"108","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58de1955e4b02ff32c699cdf","contributors":{"authors":[{"text":"Rathburn, Ronald E.","contributorId":190187,"corporation":false,"usgs":false,"family":"Rathburn","given":"Ronald","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":687738,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tai, D. Y.","contributorId":59778,"corporation":false,"usgs":true,"family":"Tai","given":"D.","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":687739,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70186913,"text":"70186913 - 1982 - Hydrates of nat­ural gas in continental margins","interactions":[],"lastModifiedDate":"2017-04-13T19:06:25","indexId":"70186913","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Hydrates of nat­ural gas in continental margins","docAbstract":"<p>Natural gas hydrates in continental margin sediment can be inferred from the widespread occurrence of an anomalous seismic reflector which coincides with the predicted transition boundary at the base of the gas hydrate zone. Direct evidence of gas hydrates is provided by visual observations of sediments from the landward wall of the Mid-America Trench off Mexico and Guatemala, from the Blake Outer Ridge off the southeastern United States, and from the Black Sea in the U.S.S.R. Where solid gas hydrates have been sampled, the gas is composed mainly of methane accompanied by CO<sub>2</sub> and low concentrations of ethane and hydrocarbons of higher molecular weight. The molecular and isotopic composition of hydrocarbons indicates that most of the methane is of biolog cal origin. The gas was probably produced by the bacterial alteration of organic matter buried in the sediment. Organic carbon contents of the sediment containing sampled gas hydrates are higher than the average organic carbon content of marine sediments. The main economic importance of gas hydrates may reside in their ability to serve as a cap under which free gas can collect. To be producible, however, such trapped gas must occur in porous and permeable reservoirs. Although gas hydrates are common along continental margins, the degree to which they are associated with significant reservoirs remains to be investigated.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Studies in continental margin geology","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Datapages, Inc.","usgsCitation":"Kvenvolden, K., and Barnard, L., 1982, Hydrates of nat­ural gas in continental margins, chap. <i>of</i> Studies in continental margin geology, p. 631-640.","productDescription":"10 p. ","startPage":"631","endPage":"640","costCenters":[],"links":[{"id":339716,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58f08e65e4b06911a29fa88c","contributors":{"authors":[{"text":"Kvenvolden, K.A.","contributorId":80674,"corporation":false,"usgs":true,"family":"Kvenvolden","given":"K.A.","email":"","affiliations":[],"preferred":false,"id":690982,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnard, L.A.","contributorId":190882,"corporation":false,"usgs":false,"family":"Barnard","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":690983,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1000341,"text":"1000341 - 1982 - Accumulation by fish of contaminants released from dredged sediments","interactions":[],"lastModifiedDate":"2013-01-29T10:45:19","indexId":"1000341","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Accumulation by fish of contaminants released from dredged sediments","docAbstract":"Inasmuch as the process of dredging and disposing of dredged materials causes a resuspension of these materials and an increase in bioavailability of associated contaminants, we conducted a series of experiments to examine the potential accumulation by fish of contaminants from suspended sediments. In the first experiment we compared accumulation of contaminants by yellow perch of hatchery and lake origin and found that after 10 days of exposure to nonaerated sediments, fish of hatchery origin accumulated PCBs and Fe, while fish of lake origin accumulated As, Cr, Fe, and Na. Two additional exposures were conducted to evaluate the effects of aerating the sediments prior to measuring bioavailability of associated contaminants. Fish of hatchery origin exposed to nonaerated sediments for 10 days accumulated PCBs and Hg, while fish of hatchery origin exposed to aerated sediments for 10 days accumulated PCBs, DDE, Zn, Fe, Cs, and Se. These results demonstrated not only the potential for uptake of contaminants by fish as a result of dredging but also the potential utility of fish bioassays in evaluating proposed dredging operations.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Science and Technology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"ACS Publications","publisherLocation":"Washington, D.C.","doi":"10.1021/es00102a006","usgsCitation":"Seelye, J.G., Hesselberg, R.J., and Mac, M.J., 1982, Accumulation by fish of contaminants released from dredged sediments: Environmental Science & Technology, v. 16, no. 8, p. 459-464, https://doi.org/10.1021/es00102a006.","productDescription":"p. 459-464","startPage":"459","endPage":"464","numberOfPages":"5","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":266678,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es00102a006"},{"id":133255,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"8","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a353b","contributors":{"authors":[{"text":"Seelye, James G.","contributorId":69919,"corporation":false,"usgs":true,"family":"Seelye","given":"James","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":308424,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hesselberg, Robert J.","contributorId":36074,"corporation":false,"usgs":true,"family":"Hesselberg","given":"Robert","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":308423,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mac, Michael J.","contributorId":16772,"corporation":false,"usgs":true,"family":"Mac","given":"Michael","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":308422,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1001550,"text":"1001550 - 1982 - Nesting of waterfowl on islands in Lake Audubon, North Dakota","interactions":[],"lastModifiedDate":"2017-10-11T11:31:12","indexId":"1001550","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3779,"text":"Wildlife Society Bulletin","onlineIssn":"1938-5463","printIssn":"0091-7648","active":true,"publicationSubtype":{"id":10}},"title":"Nesting of waterfowl on islands in Lake Audubon, North Dakota","docAbstract":"Nesting waterfowl were studied in 1978 and 1980 on 15 newly established islands with an area of 19 ha in 7,430-ha Lake Audubon in the Audubon National Wildlife Refuge (NWR), North Dakota. Islands ranged in size from 0.2 to 5.0 ha and were 60-1,600 m from the mainland. Cover available for nesting waterfowl was composed of grasses, legumes, and forbs with abundant residual plant material. In 1978 and 1980, 207 and 251 nests were found, respectively, of 10 waterfowl species primarily mallard (Anas platyrhynchos) and gadwall (A. strepera). Densities of waterfowl nests were 10.9/ha in 1978 and 13.2/ha in 1980. Nest success averaged 86% for the 2 years. Increased emphasis on construction of new islands and manipulation of plant communities on existing islands should be considered for waterfowl management programs in the prairie and parkland regions of North America.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wildlife Society Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Duebbert, H., 1982, Nesting of waterfowl on islands in Lake Audubon, North Dakota: Wildlife Society Bulletin, v. 10, no. 3, p. 232-237.","productDescription":"6 p.","startPage":"232","endPage":"237","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":133546,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -101.513671875,\n              47.42808726171425\n            ],\n            [\n              -101.07421875,\n              47.42808726171425\n            ],\n            [\n              -101.07421875,\n              47.70976154266637\n            ],\n            [\n              -101.513671875,\n              47.70976154266637\n            ],\n            [\n              -101.513671875,\n              47.42808726171425\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"10","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2f03","contributors":{"authors":[{"text":"Duebbert, Harold F.","contributorId":11544,"corporation":false,"usgs":true,"family":"Duebbert","given":"Harold F.","affiliations":[],"preferred":false,"id":311240,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000360,"text":"1000360 - 1982 - Decline of lake herring (<i>Coregonus artedii</i>) in Lake Superior: an analysis of the Wisconsin herring fishery, 1936-78","interactions":[],"lastModifiedDate":"2016-04-01T08:56:17","indexId":"1000360","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1169,"text":"Canadian Journal of Fisheries and Aquatic Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Decline of lake herring (<i>Coregonus artedii</i>) in Lake Superior: an analysis of the Wisconsin herring fishery, 1936-78","docAbstract":"<p><span>Annual harvests of lake herring (</span><i>Coregonus artedii</i><span>) in American waters of Lake Superior declined from an average of 2 million kg in 1936&ndash;62 to less than 25&ensp;000&ensp;kg in 1978. Analysis of commercial fishing records revealed that the sequential overexploitation of discrete unit stocks caused the collapse of the herring population in Wisconsin waters. In each of six major spawning areas, catch exceeded the productive capacity of the stock and the stock failed. Because stocks in the six areas were exploited sequentially, mostly in groups of two or three simultaneously, the demise of the stocks was not readily apparent until the last two failed in the early 1960s. After the collapse of the last major spawning stock, the fishery dwindled but may have continued to overexploit the remaining small stocks. The residual populations were apparently able only to replace themselves. Some form of density-independent mortality was apparently operating to prevent their recovery during the 1960s and 1970s.</span><i>Key words</i><span>: lake herring, overfishing, Lake Superior</span></p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/f82-079","usgsCitation":"Selgeby, J.H., 1982, Decline of lake herring (<i>Coregonus artedii</i>) in Lake Superior: an analysis of the Wisconsin herring fishery, 1936-78: Canadian Journal of Fisheries and Aquatic Sciences, v. 39, no. 4, p. 554-563, https://doi.org/10.1139/f82-079.","productDescription":"10 p.","startPage":"554","endPage":"563","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128957,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672716","contributors":{"authors":[{"text":"Selgeby, James H.","contributorId":89828,"corporation":false,"usgs":true,"family":"Selgeby","given":"James","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308451,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70170293,"text":"70170293 - 1982 - Sir William Hamilton; pioneer volcanologist","interactions":[],"lastModifiedDate":"2016-04-15T16:03:03","indexId":"70170293","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Sir William Hamilton; pioneer volcanologist","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Guest, J., 1982, Sir William Hamilton; pioneer volcanologist: Earthquake Information Bulletin (USGS), v. 14, no. 2, p. 48-55.","productDescription":"8 p.","startPage":"48","endPage":"55","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":320085,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"571210b8e4b0ef3b7ca64439","contributors":{"authors":[{"text":"Guest, J.","contributorId":168628,"corporation":false,"usgs":false,"family":"Guest","given":"J.","affiliations":[],"preferred":false,"id":626800,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011630,"text":"70011630 - 1982 - Ultrasonic borehole televiewer investigation of oceanic crustal layer 2A, Costa Rice Rift","interactions":[],"lastModifiedDate":"2012-03-12T17:18:34","indexId":"70011630","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Ultrasonic borehole televiewer investigation of oceanic crustal layer 2A, Costa Rice Rift","docAbstract":"In situ lithostratigraphy and the distribution of fracture and void zones in oceanic layer 2A were examined with an ultrasonic borehole televiewer at IPOD sites 501 and 504B on the south flank of the Costa Rice Rift. These records indicate a decrease in the size of basalt pillows with depth and a corresponding increase in fracture and void density. The observed increase in P-wave velocity with depth in this hole, as layer 2A merges into 2B, is best explained by an increase in the degree to which clays and zeolites fill fractures and voids. This also explains the order-of-magnitude drop in permeability observed in hole 504B. An increase in alteration-filling with age could explain the transition from convective to conductive heat flow and the correlative disappearance of layer 2A on the flanks of oceanic spreading centres. ?? 1982 Nature Publishing Group.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Nature","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1038/295375a0","issn":"00280836","usgsCitation":"Zoback, M.D., and Anderson, R., 1982, Ultrasonic borehole televiewer investigation of oceanic crustal layer 2A, Costa Rice Rift: Nature, v. 295, no. 5848, p. 375-379, https://doi.org/10.1038/295375a0.","startPage":"375","endPage":"379","numberOfPages":"5","costCenters":[],"links":[{"id":221185,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205097,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1038/295375a0"}],"volume":"295","issue":"5848","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbc04e4b08c986b328998","contributors":{"authors":[{"text":"Zoback, Mark D.","contributorId":80275,"corporation":false,"usgs":true,"family":"Zoback","given":"Mark","middleInitial":"D.","affiliations":[],"preferred":false,"id":361577,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, R.N.","contributorId":94678,"corporation":false,"usgs":true,"family":"Anderson","given":"R.N.","email":"","affiliations":[],"preferred":false,"id":361578,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011818,"text":"70011818 - 1982 - The kinetics of dissolution of dolomite in CO2-H2O systems at 1.5 to 65 degrees C and 0 to 1 atm PCO2","interactions":[],"lastModifiedDate":"2023-02-08T17:45:30.893234","indexId":"70011818","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":732,"text":"American Journal of Science","active":true,"publicationSubtype":{"id":10}},"displayTitle":"The kinetics of dissolution of dolomite in CO<sub>2</sub>-H<sub>2</sub>O systems at 1.5 to 65 degrees C and 0 to 1 atm P<sub>CO2</sub>","title":"The kinetics of dissolution of dolomite in CO2-H2O systems at 1.5 to 65 degrees C and 0 to 1 atm PCO2","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Journal of Science","doi":"10.2475/ajs.282.1.45","usgsCitation":"Busenberg, E., and Plummer, N., 1982, The kinetics of dissolution of dolomite in CO2-H2O systems at 1.5 to 65 degrees C and 0 to 1 atm PCO2: American Journal of Science, v. 282, no. 1, p. 45-78, https://doi.org/10.2475/ajs.282.1.45.","productDescription":"34 p.","startPage":"45","endPage":"78","numberOfPages":"34","costCenters":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"links":[{"id":480277,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2475/ajs.282.1.45","text":"Publisher Index Page"},{"id":221203,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"282","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bad75e4b08c986b323c0d","contributors":{"authors":[{"text":"Busenberg, Eurybiades ebusenbe@usgs.gov","contributorId":2271,"corporation":false,"usgs":true,"family":"Busenberg","given":"Eurybiades","email":"ebusenbe@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":362024,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":362025,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011859,"text":"70011859 - 1982 - Composition of estuarine colloidal material: Organic components","interactions":[],"lastModifiedDate":"2024-03-18T14:28:53.733867","indexId":"70011859","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Composition of estuarine colloidal material: Organic components","docAbstract":"<p><span>Colloidal material in the size range 1.2 nm to 0.4 μm was isolated by ultrafiltration from Chesapeake Bay and Patuxent River waters (U.S.A.). Temperature controlled, stepwise pyrolysis of the freeze-dried material, followed by gas chromatographic-mass spectrometric analyses of the volatile products indicates that the primary organic components of this polymer are carbohydrates and peptides. The major pyrolysis products at the 450°C step are acetic acid, furaldehydes, furoic acid, furanmethanol, diones and lactones characteristic of carbohydrate thermal decomposition. Pyrroles, pyridines, amides and indole (protein derivatives) become more prevalent and dominate the product yield at the 600°C pyrolysis step. Olefins and saturated hydrocarbons, originating from fatty acids, are present only in minor amounts. These results are consistent with the composition of Chesapeake phytoplankton (approximately 50% protein, 30% carbohydrate, 10% lipid and 10% nucleotides by dry weight). The pyrolysis of a cultured phytoplankton and natural particulate samples produced similar oxygen and nitrogencontaining compounds, although the proportions of some components differ relative to the colloidal fraction. There were no lignin derivatives indicative of terrestrial plant detritus in any of these samples. The data suggest that aquatic microorganisms, rather than terrestrial plants, are the dominant source of colloidal organic material in these river and estuarine surface waters.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(82)90318-0","issn":"00167037","usgsCitation":"Sigleo, A., Hoering, T., and Helz, G., 1982, Composition of estuarine colloidal material: Organic components: Geochimica et Cosmochimica Acta, v. 46, no. 9, p. 1619-1626, https://doi.org/10.1016/0016-7037(82)90318-0.","productDescription":"8 p.","startPage":"1619","endPage":"1626","numberOfPages":"8","costCenters":[],"links":[{"id":220795,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"46","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f928e4b0c8380cd4d47e","contributors":{"authors":[{"text":"Sigleo, A.C.","contributorId":20899,"corporation":false,"usgs":true,"family":"Sigleo","given":"A.C.","email":"","affiliations":[],"preferred":false,"id":362136,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoering, T.C.","contributorId":101011,"corporation":false,"usgs":true,"family":"Hoering","given":"T.C.","email":"","affiliations":[],"preferred":false,"id":362138,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Helz, G.R.","contributorId":96823,"corporation":false,"usgs":true,"family":"Helz","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":362137,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011814,"text":"70011814 - 1982 - Identification of the Holocene-Pleistocene boundary in the Bering Sea by diatoms.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:27","indexId":"70011814","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1068,"text":"Boreas","active":true,"publicationSubtype":{"id":10}},"title":"Identification of the Holocene-Pleistocene boundary in the Bering Sea by diatoms.","docAbstract":"The modern diatom flora from surface sediment of the Navarin Basin region of the Bering Sea is dominated by Denticulopsis seminae and Nitzschia oceanica. D. seminae, a north boreal species, is most abundant in the deeper waters of the slope-basin regions, whereas N. oceanica, an Arctic species associated with ice cover, dominates the shallow shelf water. Downcore studies show that these species alternate in dominance within the late Quaternary sediments suggest climatic fluctuations.-from Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Boreas","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03009483","usgsCitation":"Baldauf, J., 1982, Identification of the Holocene-Pleistocene boundary in the Bering Sea by diatoms.: Boreas, v. 11, no. 1, p. 113-118.","startPage":"113","endPage":"118","numberOfPages":"6","costCenters":[],"links":[{"id":221199,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a383fe4b0c8380cd614cd","contributors":{"authors":[{"text":"Baldauf, J.G.","contributorId":67655,"corporation":false,"usgs":true,"family":"Baldauf","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":362017,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011636,"text":"70011636 - 1982 - Multi-element analysis of manganese nodules by atomic absorption spectrometry without chemical separation","interactions":[],"lastModifiedDate":"2023-03-07T16:51:23.222075","indexId":"70011636","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":760,"text":"Analytica Chimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Multi-element analysis of manganese nodules by atomic absorption spectrometry without chemical separation","docAbstract":"<p><span>Five manganese nodules, including the USGS reference nodules A-1 and P-1, were analyzed for Co, Cu, Fe, K, Mg, Mn, Na, Ni and Zn without prior chemical separation by using a simultaneous multi-element atomic absorption spectrometer with an air—cetylene flame. The nodules were prepared in three digestion matrices. One of these solutions was measured using sixteen different combinations of burner height and air/acetylene ratios. Results for A-1 and P-1 are compared to recommended values and results for all nodules are compared to those obtained with an inductively coupled plasma. The elements Co, Cu, Fe, K, Mg, Mn, Na, Ni, and Zn are simultaneously determined with a composite recovery for all elements of 100 ± 7%, independent of the digestion matrices, heights in the flame, or flame stoichiometries examined. Individual recoveries for Co, K, and Ni are considerably poorer in two digests than this composite figure, however. The optimum individual recoveries of 100 ± 5% and imprecisions of 1–4%, except for zinc, are obtained when Co, K, Mn, Na and Ni are determined simultaneously in a concentrated digest, and in another analytical sequence, when Cu, Fe, Mg, Mn and Zn are measured simultaneously after dilution. Determination of manganese is equally accurate in the two sequences; its measurement in both assures internal consistency between the two measurement sequences. This approach improves analytical efficiency over that for conventional atomic absorption methods, while minimizing loss of accuracy or precision for individual elements.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0003-2670(01)94007-3","usgsCitation":"Kane, J.S., and Harnly, J.M., 1982, Multi-element analysis of manganese nodules by atomic absorption spectrometry without chemical separation: Analytica Chimica Acta, v. 139, no. C, p. 297-305, https://doi.org/10.1016/S0003-2670(01)94007-3.","productDescription":"9 p.","startPage":"297","endPage":"305","numberOfPages":"9","costCenters":[],"links":[{"id":221245,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"139","issue":"C","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5fb1e4b0c8380cd710a7","contributors":{"authors":[{"text":"Kane, Jean S.","contributorId":22359,"corporation":false,"usgs":true,"family":"Kane","given":"Jean","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":361587,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harnly, J. M.","contributorId":22492,"corporation":false,"usgs":false,"family":"Harnly","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":361586,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011803,"text":"70011803 - 1982 - The redox potential of boron nitride and implications for its use as a crucible material in experimental petrology.","interactions":[],"lastModifiedDate":"2013-02-14T10:07:31","indexId":"70011803","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":738,"text":"American Mineralogist","active":true,"publicationSubtype":{"id":10}},"title":"The redox potential of boron nitride and implications for its use as a crucible material in experimental petrology.","docAbstract":"-K.A.R.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Mineralogist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Mineralogical Society of America","issn":"0003004X","usgsCitation":"Wendlandt, R.F., Huebner, J., and Harrison, W., 1982, The redox potential of boron nitride and implications for its use as a crucible material in experimental petrology.: American Mineralogist, v. 67, no. 1-2, p. 170-174.","startPage":"170","endPage":"174","numberOfPages":"5","costCenters":[],"links":[{"id":220996,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267373,"type":{"id":11,"text":"Document"},"url":"https://www.minsocam.org/ammin/AM67/AM67_170.pdf"}],"volume":"67","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baf02e4b08c986b3244b0","contributors":{"authors":[{"text":"Wendlandt, R. F.","contributorId":20467,"corporation":false,"usgs":false,"family":"Wendlandt","given":"R.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":361990,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Huebner, J.S.","contributorId":41422,"corporation":false,"usgs":true,"family":"Huebner","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":361992,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harrison, W.J.","contributorId":34263,"corporation":false,"usgs":true,"family":"Harrison","given":"W.J.","email":"","affiliations":[],"preferred":false,"id":361991,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70195654,"text":"70195654 - 1982 -  A major sink and flux control for methane in marine sediments; Anaerobic consumption","interactions":[{"subject":{"id":70195654,"text":"70195654 - 1982 -  A major sink and flux control for methane in marine sediments; Anaerobic consumption","indexId":"70195654","publicationYear":"1982","noYear":false,"title":" A major sink and flux control for methane in marine sediments; Anaerobic consumption"},"predicate":"IS_PART_OF","object":{"id":70190672,"text":"70190672 - 1982 - The dynamic environment of the ocean floor","indexId":"70190672","publicationYear":"1982","noYear":false,"title":"The dynamic environment of the ocean floor"},"id":1}],"isPartOf":{"id":70190672,"text":"70190672 - 1982 - The dynamic environment of the ocean floor","indexId":"70190672","publicationYear":"1982","noYear":false,"title":"The dynamic environment of the ocean floor"},"lastModifiedDate":"2018-02-26T11:45:03","indexId":"70195654","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":" A major sink and flux control for methane in marine sediments; Anaerobic consumption","docAbstract":"<p><span>No abstract available.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The dynamic environment of the ocean floor","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Lexington Books","isbn":"9780669028096","usgsCitation":"Reeburgh, W., 1982,  A major sink and flux control for methane in marine sediments; Anaerobic consumption, chap. <i>of</i> The dynamic environment of the ocean floor, p. 203-217.","productDescription":"15 p.","startPage":"203","endPage":"217","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":352006,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff4242e4b0da30c1bfdadb","contributors":{"editors":[{"text":"Fanning, Kent A.","contributorId":138529,"corporation":false,"usgs":false,"family":"Fanning","given":"Kent","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":729582,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Manheim, Frank T.","contributorId":26991,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":729583,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Reeburgh, W.S.","contributorId":90046,"corporation":false,"usgs":false,"family":"Reeburgh","given":"W.S.","email":"","affiliations":[],"preferred":false,"id":729568,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011810,"text":"70011810 - 1982 - Holocene sedimentation in the shallow nearshore zone off Nauset Inlet, Cape Cod, Massachusetts","interactions":[],"lastModifiedDate":"2017-09-06T10:27:51","indexId":"70011810","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Holocene sedimentation in the shallow nearshore zone off Nauset Inlet, Cape Cod, Massachusetts","docAbstract":"<p>Present conditions and sedimentary evolution of the shallow offshore region near Nauset Inlet on Cape Cod, Massachusetts were clarified using high-resolution seismic-reflection profiles, sidescan-sonar records, surface grab samples and current meter measurements. The study area contains three provinces: (1) a nearshore province (shallower than 18 m) with a relatively steep slope (0.6°) and a cover of medium sand; (2) a northern offshore province covered with coarse sand, gravel, and boulders, interpreted to be glacial drift; and (3) a southern offshore province with a gentle seaward-dipping slope (0.3°) and a surface sediment of coarse sand. The glacial drift exposed in the northern offshore province can be traced southward under the coarse sand province. The overlying fill is comprised of either outwash sediment derived from the Pleistocene South Channel ice lobe to the east or Holocene-aged marine sediments eroded from seacliffs to the north. Latest Holocene sediment appears to be limited to the zone shoreward of 18 m where the medium sand occurs.</p><p>Near-bottom mean flows (measured over two winter months in 10 m water depth) average 6 cm sec<sup>−1</sup><span>&nbsp;</span>to the south. Mean flows exceeded 20 cm sec<sup>−1</sup>approx. 23% of the time. Ninety percent of the flows exceeding 20 cm sec<sup>−1</sup>were directed to the south, reflecting the dominant atmospheric forcing during these winter months. Waves had an average variance of 650 cm<sup>2</sup><span>&nbsp;</span>with variance exceeding 5000 cm<sup>2</sup>, 3% of the time, indicating moderate wave activity.</p><p>Present processes are actively reshaping the nearshore province, which is characterized by many east to northeast-trending shore-oblique channels that do not extend seaward of the 18-m contour. Coarse sand in the floors of these channels suggests they may be erosional features, and the presence of megaripples oriented perpendicular to the channel axes indicates active transport in these channels. Megaripple orientation and the current and wave regime of the study area support a rip-current origin for these channels.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/0025-3227(82)90071-8","issn":"00253227","usgsCitation":"Aubrey, D., Twichell, D., and Pfirman, S., 1982, Holocene sedimentation in the shallow nearshore zone off Nauset Inlet, Cape Cod, Massachusetts: Marine Geology, v. 47, no. 3-4, p. 243-259, https://doi.org/10.1016/0025-3227(82)90071-8.","productDescription":"17 p.","startPage":"243","endPage":"259","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":221131,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Massachussetts","otherGeospatial":"Cape Cod, Nauset Inlet","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -70.68878173828125,\n              41.693424216151314\n            ],\n            [\n              -69.9224853515625,\n              41.693424216151314\n            ],\n            [\n              -69.9224853515625,\n              42.10229818948117\n            ],\n            [\n              -70.68878173828125,\n              42.10229818948117\n            ],\n            [\n              -70.68878173828125,\n              41.693424216151314\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"47","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a31f4e4b0c8380cd5e3b3","contributors":{"authors":[{"text":"Aubrey, D.G.","contributorId":73336,"corporation":false,"usgs":true,"family":"Aubrey","given":"D.G.","email":"","affiliations":[],"preferred":false,"id":362010,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Twichell, D.C.","contributorId":84304,"corporation":false,"usgs":true,"family":"Twichell","given":"D.C.","affiliations":[],"preferred":false,"id":362011,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pfirman, S.L.","contributorId":40281,"corporation":false,"usgs":true,"family":"Pfirman","given":"S.L.","affiliations":[],"preferred":false,"id":362009,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011846,"text":"70011846 - 1982 - Fission-track ages from the Precambrian of Shropshire","interactions":[],"lastModifiedDate":"2023-11-17T12:04:27.88055","indexId":"70011846","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1783,"text":"Geological Magazine","active":true,"publicationSubtype":{"id":10}},"title":"Fission-track ages from the Precambrian of Shropshire","docAbstract":"Four samples of Longmyndian and Uriconian strata from S of Shrewsbury, England have been processed for apatite and/or zircon fission-track ages. The resultant ages illustrate how depth of burial may affect fission-track ages. The analytical procedures followed were as described in Naeser (1979).-from Authors","language":"English","publisher":"Cambridge University Press","doi":"10.1017/S0016756800025905","usgsCitation":"Naeser, C.W., Toghill, P., and Ross, R.J., 1982, Fission-track ages from the Precambrian of Shropshire: Geological Magazine, v. 119, no. 2, p. 213-214, https://doi.org/10.1017/S0016756800025905.","productDescription":"2 p.","startPage":"213","endPage":"214","numberOfPages":"2","costCenters":[],"links":[{"id":480274,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1017/s0016756800025905","text":"Publisher Index Page"},{"id":221618,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"119","issue":"2","noUsgsAuthors":false,"publicationDate":"2009-05-01","publicationStatus":"PW","scienceBaseUri":"505a10bfe4b0c8380cd53dbc","contributors":{"authors":[{"text":"Naeser, C. W.","contributorId":17582,"corporation":false,"usgs":true,"family":"Naeser","given":"C.","middleInitial":"W.","affiliations":[],"preferred":false,"id":362102,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Toghill, P.","contributorId":11334,"corporation":false,"usgs":true,"family":"Toghill","given":"P.","email":"","affiliations":[],"preferred":false,"id":362101,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ross, R. J. Jr.","contributorId":83910,"corporation":false,"usgs":true,"family":"Ross","given":"R.","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":362103,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011603,"text":"70011603 - 1982 - Sample design for estimating change in land use and land cover ( Pennsylvania).","interactions":[],"lastModifiedDate":"2012-03-12T17:18:30","indexId":"70011603","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Sample design for estimating change in land use and land cover ( Pennsylvania).","docAbstract":"The methodology of sample design which is applied to estimating change in land use and land cover is general and extendable to determination of change in any type of thematic mapping that is time variant. Land-use maps of the State of Pennsylvania at a scale of 1:250,000 were compiled circa 1958 with land use classified into six categories. The more detailed land-use and land-cover mapping of the State of Pennsylvania at a scale of 1:250,000 was completed by the U.S. Geological Survey circa 1977. With some rearrangement of these categories, the recent maps are very nearly compatible with a combination of five categories of the earlier maps. -from Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Photogrammetric Engineering and Remote Sensing","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00991112","usgsCitation":"Rosenfield, G., 1982, Sample design for estimating change in land use and land cover ( Pennsylvania).: Photogrammetric Engineering and Remote Sensing, v. 48, no. 5, p. 793-801.","startPage":"793","endPage":"801","numberOfPages":"9","costCenters":[],"links":[{"id":220779,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"48","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ab050e4b0c8380cd87a48","contributors":{"authors":[{"text":"Rosenfield, G.H.","contributorId":94670,"corporation":false,"usgs":true,"family":"Rosenfield","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":361523,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011783,"text":"70011783 - 1982 - Microfaunal analysis of late Quaternary deposits of the northern Bering Sea.","interactions":[],"lastModifiedDate":"2012-03-12T17:19:03","indexId":"70011783","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1794,"text":"Geologie en Mijnbouw","active":true,"publicationSubtype":{"id":10}},"title":"Microfaunal analysis of late Quaternary deposits of the northern Bering Sea.","docAbstract":"Holocene microfaunal associations and distribution patterns define three inner-shelf (1-20m) biofacies in Norton Sound, northern Bering Sea. The Holocene facies relations are the basis for interpreting early Holocene and late Pleistocene environmental conditions in the NE Bering Sea area. Norton Sound cores provide evidence of two marine transgressions and a varying river input.-from Author","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geologie en Mijnbouw","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"McDougall, K., 1982, Microfaunal analysis of late Quaternary deposits of the northern Bering Sea.: Geologie en Mijnbouw, v. 61, no. 1, p. 19-27.","startPage":"19","endPage":"27","numberOfPages":"9","costCenters":[],"links":[{"id":221774,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"61","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a567be4b0c8380cd6d608","contributors":{"authors":[{"text":"McDougall, K.","contributorId":106260,"corporation":false,"usgs":true,"family":"McDougall","given":"K.","email":"","affiliations":[],"preferred":false,"id":361951,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70137379,"text":"70137379 - 1982 - Geology and sediment accumulation rates at Carrie Bow Cay, Belize","interactions":[],"lastModifiedDate":"2015-03-18T13:38:40","indexId":"70137379","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3851,"text":"Smithsonian Contributions to the Marine Sciences","active":true,"publicationSubtype":{"id":10}},"seriesNumber":"12","title":"Geology and sediment accumulation rates at Carrie Bow Cay, Belize","docAbstract":"<p>A 24 km long transect of cores consisting of four rotary drill cores and seven vibrocores was drilled in a line extending from the seaward side of the reef crest at Carrie Bow Cay to the mainland at a point between Sittee Point and the town of Stann Creek. Two of the four rotary cores were drilled seaward of the reef crest, one through a spur to a depth of 7.6 m and the other into the adjacent groove to a depth of 18.3 m. The two cores show no evidence that the spur and groove system was erosional in origin; rather they demonstrate that it was constructional. Submarine cementation, chiefly in the form of fine-grained high-magnesium calcite, was found mainly in cemented internal sediment in both cores drilled seaward of the reef crest.</p>\n<p>Two other rotary cores were drilled landward of the reef crest. One was drilled on the reef flat to a depth of 8.8 m, and the other was drilled on the southwest tip of Carrie Bow Cay to a depth of 17.7 m. Both cores encountered essentially uncemented carbonate reef sands with some coral rubble. Of the four rotary cores, only the Carrie Bow Cay core encountered Pleistocene bedrock. Radiocarbon dating of a large head of <i>Siderastrea siderea</i>, growing on bedrock from the Carrie Bow Cay core at a depth of 15.04 m below sea level, gave an age of 6960&plusmn;110 years. The leached calcitic coralline bedrock, at a depth of 15.7 m below sea level in the Carrie Bow Cay core, contained root marks, and iron staining indicative of subaerial exposure.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The Atlantic Barrier Reef ecosystem at Carrie Bow Cay, Belize, I: structure and communities","language":"English","publisher":"Smithsonian Institution Press","publisherLocation":"Washington, D.C.","usgsCitation":"Shinn, E., Hudson, J., Halley, R., Lidz, B.H., Robbin, D.M., and Macintyre, I.G., 1982, Geology and sediment accumulation rates at Carrie Bow Cay, Belize: Smithsonian Contributions to the Marine Sciences, p. 63-75.","productDescription":"13 p.","startPage":"63","endPage":"75","numberOfPages":"13","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":298722,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":297055,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://repository.si.edu/handle/10088/1116"}],"country":"Belize","otherGeospatial":"Carrie Bow Cay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.31188201904297,\n              16.772658214366704\n            ],\n            [\n              -88.31188201904297,\n              16.945484423697636\n            ],\n            [\n              -88.01662445068358,\n              16.945484423697636\n            ],\n            [\n              -88.01662445068358,\n              16.772658214366704\n            ],\n            [\n              -88.31188201904297,\n              16.772658214366704\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"550aa1b7e4b02e76d7590be8","contributors":{"editors":[{"text":"Ruetzler, Klaus","contributorId":138548,"corporation":false,"usgs":false,"family":"Ruetzler","given":"Klaus","email":"","affiliations":[],"preferred":false,"id":537790,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Macintyre, Ian G.","contributorId":94037,"corporation":false,"usgs":true,"family":"Macintyre","given":"Ian","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":537791,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Shinn, Eugene A.","contributorId":6883,"corporation":false,"usgs":true,"family":"Shinn","given":"Eugene A.","affiliations":[],"preferred":false,"id":537784,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hudson, J. Harold","contributorId":138547,"corporation":false,"usgs":true,"family":"Hudson","given":"J. Harold","affiliations":[],"preferred":false,"id":537785,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Halley, Robert B.","contributorId":45692,"corporation":false,"usgs":true,"family":"Halley","given":"Robert B.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":537786,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lidz, Barbara H. blidz@usgs.gov","contributorId":2475,"corporation":false,"usgs":true,"family":"Lidz","given":"Barbara","email":"blidz@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":537787,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Robbin, Daniel M.","contributorId":42888,"corporation":false,"usgs":true,"family":"Robbin","given":"Daniel","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":537788,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Macintyre, Ian G.","contributorId":94037,"corporation":false,"usgs":true,"family":"Macintyre","given":"Ian","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":537789,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":27713,"text":"wri8253 - 1982 - Ground-water temperature of the with application to ground-water-source heat pumps","interactions":[],"lastModifiedDate":"2023-07-14T15:22:08.941467","indexId":"wri8253","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","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":"82-53","title":"Ground-water temperature of the with application to ground-water-source heat pumps","docAbstract":"Ground-water temperature was measured during a one-year period (1980-81) in 20 wells in the Wyoming Quadrangle in central Delaware. Data from thermistors set at fixed depths in two wells were collected twice each week, and vertical temperature profiles of the remaining 18 wells were made monthly. Ground-water temperature at 8 feet below land surface in well Jc55-1 ranged from 45.0 degrees F in February to 70.1 degrees F in September. Temperature at 35 feet below land surface in the same well reached a minimum of 56.0 degrees F in August, and a maximum of 57.8 degrees F in February. Average annual temperature of ground water at 25 feet below land surface in all wells ranged from 54.6 degrees F to 57.8 degrees F. Variations of average temperature probably reflect the presence or absence of forestation in the recharge areas of the wells. Ground-water-source heat pumps supplied with water from wells 30 or more feet below land surface will operate more efficiently in both heating and cooling modes than those supplied with water from shallower depths. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8253","usgsCitation":"Hodges, A.L., 1982, Ground-water temperature of the with application to ground-water-source heat pumps: U.S. Geological Survey Water-Resources Investigations Report 82-53, vi, 29 p., https://doi.org/10.3133/wri8253.","productDescription":"vi, 29 p.","costCenters":[],"links":[{"id":366225,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0053/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158501,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0053/report-thumb.jpg"}],"country":"United States","state":"Delaware","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.7562255859375,\n              38.839707613545144\n            ],\n            [\n              -75.2288818359375,\n              38.839707613545144\n            ],\n            [\n              -75.2288818359375,\n              39.2407625100131\n            ],\n            [\n              -75.7562255859375,\n              39.2407625100131\n            ],\n            [\n              -75.7562255859375,\n              38.839707613545144\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a38e","contributors":{"authors":[{"text":"Hodges, Arthur L. Jr.","contributorId":62075,"corporation":false,"usgs":true,"family":"Hodges","given":"Arthur","suffix":"Jr.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":198576,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70195647,"text":"70195647 - 1982 - Aversion substance(s) of the rat coagulating glands","interactions":[],"lastModifiedDate":"2018-02-26T09:21:17","indexId":"70195647","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2205,"text":"Journal of Chemical Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Aversion substance(s) of the rat coagulating glands","docAbstract":"<p><span>The aversive substance(s) present in adult male urine were not found in castrate rat urine. Removal of the coagulating glands also resulted in a loss of the aversion compounds. The aversion substances were restored to the urine after androgen treatment of the castrate rats.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/BF00987786","usgsCitation":"Gawienowski, A.M., Berry, I.J., and Kennelly, J.J., 1982, Aversion substance(s) of the rat coagulating glands: Journal of Chemical Ecology, v. 8, no. 2, p. 379-382, https://doi.org/10.1007/BF00987786.","productDescription":"4 p.","startPage":"379","endPage":"382","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":351992,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff4242e4b0da30c1bfdae1","contributors":{"authors":[{"text":"Gawienowski, Anthony M.","contributorId":202195,"corporation":false,"usgs":false,"family":"Gawienowski","given":"Anthony","email":"","middleInitial":"M.","affiliations":[{"id":6932,"text":"University of Massachusetts, Amherst","active":true,"usgs":false}],"preferred":false,"id":729547,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berry, Iver J.","contributorId":17974,"corporation":false,"usgs":false,"family":"Berry","given":"Iver","email":"","middleInitial":"J.","affiliations":[{"id":6932,"text":"University of Massachusetts, Amherst","active":true,"usgs":false}],"preferred":false,"id":729548,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kennelly, James J.","contributorId":33962,"corporation":false,"usgs":true,"family":"Kennelly","given":"James","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":729549,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":27711,"text":"wri8236 - 1982 - Chemical-quality reconnaissance of the water and surficial bed material in the Delaware River estuary and adjacent New Jersey tributaries, 1980-81","interactions":[],"lastModifiedDate":"2023-04-07T18:39:53.691423","indexId":"wri8236","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","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":"82-36","title":"Chemical-quality reconnaissance of the water and surficial bed material in the Delaware River estuary and adjacent New Jersey tributaries, 1980-81","docAbstract":"This report presents chemical-quality data collected from May 1980 to January 1981 at several locations within the Delaware River estuary and selected New Jersey tributaries. Samples of surface water were analyzed Environmental Protection Agency ' priority pollutants, ' including acid extractable, base/neutral extractable and volatile organic compounds, in addition to selected dissolved inorganic constituents. Surficial bed material at selected locations was examined for trace metals, insecticides, polychlorinated biphenyls, and base/neutral extractable organic compounds. Trace levels (1-50 micrograms per liter) of purgeable organic compounds, particularly those associated with the occurrence of hydrocarbons, were found in about 60% of the water samples taken. DDT, DDD, DDE, PCB 's and chlordane are present in most surficial bed material samples. Diazinon was the only organophosphorous insecticide detected in the study (1.6 micrograms per kilogram at one location). High values for select trace metals in bed material were discovered at two locations. Of the 10 sites sampled, the surficial bed material containing the most contamination was found along one cross section of Raccoon Creek at Bridgeport. An additional analysis of Raccoon Creek revealed bed material containing toluene, oil and grease, and trace quantities of 15 base/neutral extractable organic compounds, including polynuclear aromatic hydrocarbons, phthalate esters, and chlorinated benzenes.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8236","collaboration":"Prepared in cooperation with the New Jersey Department of Environmental Protection, Division of Water Resources","usgsCitation":"Hochreiter, J.J., 1982, Chemical-quality reconnaissance of the water and surficial bed material in the Delaware River estuary and adjacent New Jersey tributaries, 1980-81: U.S. Geological Survey Water-Resources Investigations Report 82-36, vii, 41 p., https://doi.org/10.3133/wri8236.","productDescription":"vii, 41 p.","numberOfPages":"50","onlineOnly":"Y","additionalOnlineFiles":"N","temporalStart":"1980-01-01","temporalEnd":"1981-12-31","costCenters":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"links":[{"id":158491,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_82_36.gif"},{"id":415449,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35530.htm","linkFileType":{"id":5,"text":"html"}},{"id":261852,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri82-36/","linkFileType":{"id":5,"text":"html"}},{"id":261853,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/wri82-36/pdf/wrir82-36.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Jersey","otherGeospatial":"Delaware River estuary","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -75.55,\n              40.144\n            ],\n            [\n              -75.55,\n              39.9\n            ],\n            [\n              -74.702,\n              39.9\n            ],\n            [\n              -74.702,\n              40.144\n            ],\n            [\n              -75.55,\n              40.144\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dee4b07f02db5e29ea","contributors":{"authors":[{"text":"Hochreiter, Joseph J. Jr.","contributorId":94345,"corporation":false,"usgs":true,"family":"Hochreiter","given":"Joseph","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":198573,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70164346,"text":"70164346 - 1982 - Working group on the “adequate minimum” V=volcanic observatory","interactions":[],"lastModifiedDate":"2016-03-21T15:15:30","indexId":"70164346","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Working group on the “adequate minimum” V=volcanic observatory","docAbstract":"<p>A working group consisting of R. I. Tilling (United States, Chairman), M. Espendola (Mexico), E. Malavassi (Costa Rica), L. Villari (Italy), and J.P Viode (France) met on the island of Guadeloupe on February 20, 1981, to discuss informally the requirements for a \"Minimum\" volcano observatory, one which would have the essential monitoring equipment and staff to provide reliable information on the state of an active volcno. Given the premise that any monitoring of a volcano is better than none at all, the owrking group then proceeded to consider the concept of an \"adequate minimum\" observatory.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Tilling, R., 1982, Working group on the “adequate minimum” V=volcanic observatory: Earthquake Information Bulletin (USGS), v. 14, no. 5, p. 185-185.","productDescription":"1 p.","startPage":"185","endPage":"185","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":316421,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Guadeloupe","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -61.467132568359375,\n              16.516416072648976\n            ],\n            [\n              -61.402587890625,\n              16.49139854629262\n            ],\n            [\n              -61.39160156249999,\n              16.422913000573978\n            ],\n            [\n              -61.387481689453125,\n              16.359674148368025\n            ],\n            [\n              -61.270751953125,\n              16.32672912425378\n            ],\n            [\n              -61.14990234374999,\n              16.25686733062344\n            ],\n            [\n              -61.17324829101562,\n              16.231816480991785\n            ],\n            [\n              -61.27899169921875,\n              16.23972762034491\n            ],\n            [\n              -61.42181396484374,\n              16.200168744729854\n            ],\n            [\n              -61.4794921875,\n              16.18302409947757\n            ],\n            [\n              -61.5728759765625,\n              16.22522362192406\n            ],\n            [\n              -61.566009521484375,\n              16.17906743138227\n            ],\n            [\n              -61.54129028320313,\n              16.04185404753606\n            ],\n            [\n              -61.612701416015625,\n              15.963969758657447\n            ],\n            [\n              -61.71295166015625,\n              15.933599871796204\n            ],\n            [\n              -61.761016845703125,\n              16.015455996341313\n            ],\n            [\n              -61.80358886718749,\n              16.11047260335594\n            ],\n            [\n              -61.832427978515625,\n              16.29509667958127\n            ],\n            [\n              -61.80633544921876,\n              16.358356454087527\n            ],\n            [\n              -61.67175292968749,\n              16.363627177831876\n            ],\n            [\n              -61.58660888671874,\n              16.29773291178066\n            ],\n            [\n              -61.5289306640625,\n              16.357038750911766\n            ],\n            [\n              -61.549530029296875,\n              16.430816412465084\n            ],\n            [\n              -61.549530029296875,\n              16.479547009916406\n            ],\n            [\n              -61.490478515625,\n              16.50719946582598\n            ],\n            [\n              -61.467132568359375,\n              16.516416072648976\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"14","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56b09005e4b010e2af2a5ebd","contributors":{"authors":[{"text":"Tilling, R.I. 0000-0003-4263-7221","orcid":"https://orcid.org/0000-0003-4263-7221","contributorId":98311,"corporation":false,"usgs":true,"family":"Tilling","given":"R.I.","affiliations":[],"preferred":false,"id":597084,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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