{"pageNumber":"1635","pageRowStart":"40850","pageSize":"25","recordCount":46644,"records":[{"id":10684,"text":"ofr821087 - 1982 - Test and calibration of the Digital World-Wide Standardized Seismograph","interactions":[],"lastModifiedDate":"2018-07-10T11:04:47","indexId":"ofr821087","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-1087","title":"Test and calibration of the Digital World-Wide Standardized Seismograph","docAbstract":"<p>During the past decade there has been steady progress in the modernization of the global seismograph network operated by the U.S. Geological Survey (USGS). The World-Wide Standardized Seismograph Network (WWSSN) has been augmented by new stations with advanced instrumentation, including the Seismic Research Observatories (SRO) and the modified High-Gain Long-Period (ASRO) stations. One goal in the modernization effort has been to improve signal resolution in the long-period band. A second goal has been to generate a global digital data base to support contemporary computer-based analysis and research. </p><p>In 1976, a Panel on Seismograph Networks was established by the Committee on Seismology of the National Academy of Sciences to review progress in network seismology and recommend actions that would lead to an improved global data base for seismology. One recommendation in the Panel report (Engdahl, 1977) called for upgrading selected WWSSN stations by the installation of digital recorders. This was viewed as an economical way of expanding the digital network, which had proven itself to be a very promising new tool for earthquake and explosion research. Funds for the development and assembly of 15 digital recorders were provided to the USGS by the Defense Advanced Research Projects Agency and an ad Inoc panel of scientists was convened by the Committee on Seismology to advise the USGS on the selection of stations to be upgraded and on data recording requirements, A total of 19 digital World-Wide Standardized Seismograph (DWWSS) systems will be operational when all are installed. The additional systems were made available through purchase by the USGS and other organizations; for example, the University of Bergen purchased and installed a DWWSS-type recorder and agreed to furnish the USGS with the data. A list of operational and planned DWWSS network stations is given in Table 1.1.</p><p>As one might expect, the digital recorder turned out to be somewhat more sophisticated than the original concept. It was decided to record three components of long-period data continuously, three components of intermediateperiod data in an event mode, and the vertical-component short-period data in and event mode (with the capability of adding short-period horizontal channels in the future). Special amplifiers were developed for use with the WWSS seismometers, and a 16-bit fixed-point analog-to-digital converter was chosen&nbsp;to provide increased resolution (as opposed to a 16-bit gain-ranged encoder). The microprocessor-based digital recording systems were developed and assembled at the USGS Albuquerque Seismological Laboratory (ASL) and ASL-based technicians began installation at WWSSN stations in 1980.</p><p>The current and proposed locations of the DWWSSN stations, together with other stations in the Global Digital Seismograph Network (GDSN), are shown on the map in Figure 1.1. A system was operated at Albuquerque for about 18 months, serving as a test bed for evaluation studies. Although the network hardware has been available for some time, the installation of the DWWSSN has proceeded slowly. The National Science Foundation supported installation of six stations and the USGS is funding installation of most of the others; however, the network completion date is conjectural because of funding uncertainties.</p><p>The DWWSSN stations are supported with supplies and technical assistance from ASL (subject to availability of funds). Data recorded on magnetic tapes are mailed to ASL where they are reviewed for quality, then merged with other GDSN station data on the network-day tapes. Hoffman (1980) provides a description of the network-day tape format. Zirbes and Buland (1981) have developed and published user software for reading and interpreting the day tapes. </p><p>This report will serve several purposes. One is to provide nominal system transfer functions and calibration information that are needed in the analysis of DWWSSN data. A second purpose is to report on an evaluation of operating characteristics (calibration stability, noise levels, and linearity) that may limit the usefulness of the data and to determine if modifications may be needed to improve the data. It is not an exhaustive study in this respect. We continue to depend mostly on data user feedback to point out deficiencies and we solicit comments whenever anomalies are observed in the data. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr821087","usgsCitation":"Peterson, J., and Hutt, C.R., 1982, Test and calibration of the Digital World-Wide Standardized Seismograph: U.S. Geological Survey Open-File Report 82-1087, iii, 170 p., https://doi.org/10.3133/ofr821087.","productDescription":"iii, 170 p.","costCenters":[{"id":122,"text":"Albuquerque Seismological Laboratory","active":false,"usgs":true}],"links":[{"id":144232,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1087/coverthb.jpg"},{"id":38504,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1087/ofr82-1087.pdf","text":"Report","size":"5.03 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 1982-1087"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684c77","contributors":{"authors":[{"text":"Peterson, Jon","contributorId":67522,"corporation":false,"usgs":true,"family":"Peterson","given":"Jon","affiliations":[],"preferred":false,"id":161796,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hutt, Charles R. 0000-0001-9033-9195 bhutt@usgs.gov","orcid":"https://orcid.org/0000-0001-9033-9195","contributorId":1622,"corporation":false,"usgs":true,"family":"Hutt","given":"Charles","email":"bhutt@usgs.gov","middleInitial":"R.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":161795,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11487,"text":"ofr82843 - 1982 - Research on uranium resource models, a progress report; Part V, LDIGIT, a computer program to digitize graphics data for spatial data analysis","interactions":[],"lastModifiedDate":"2012-02-02T00:06:45","indexId":"ofr82843","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-843","title":"Research on uranium resource models, a progress report; Part V, LDIGIT, a computer program to digitize graphics data for spatial data analysis","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82843","usgsCitation":"Turner, R.M., Scott, W.A., and McCammon, R.B., 1982, Research on uranium resource models, a progress report; Part V, LDIGIT, a computer program to digitize graphics data for spatial data analysis: U.S. Geological Survey Open-File Report 82-843, 31 p., ill. ;28 cm., https://doi.org/10.3133/ofr82843.","productDescription":"31 p., ill. ;28 cm.","costCenters":[],"links":[{"id":146555,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0843/report-thumb.jpg"},{"id":39356,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0843/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c603","contributors":{"authors":[{"text":"Turner, Robert M.","contributorId":96670,"corporation":false,"usgs":true,"family":"Turner","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":163224,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, William A.","contributorId":51745,"corporation":false,"usgs":true,"family":"Scott","given":"William","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":163223,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McCammon, Richard B.","contributorId":107674,"corporation":false,"usgs":true,"family":"McCammon","given":"Richard","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":163225,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":23122,"text":"ofr8285 - 1982 - Geohydrology of the valley-fill aquifer in the Corning area, Steuben County, New York","interactions":[],"lastModifiedDate":"2022-07-08T18:28:43.168936","indexId":"ofr8285","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-85","title":"Geohydrology of the valley-fill aquifer in the Corning area, Steuben County, New York","docAbstract":"<p>This report is the seventh in a series of 11 map sets depicting geohydrologic conditions in selected aquifers in upstate New York. Geohydrologic data are compiled on six maps at 1:24,000 scale. Together, the maps provide a comprehensive overview of a major valley-fill aquifer in southeastern Steuben County. The maps include surficial geology, geologic sections, water-infiltration potential of soil zone, aquifer thickness, potentiometric-surface elevations, and land use. The valley-fill deposits consist of alluvial silt, sand, and gravel, glacial-outwash (sand and gravel), till, and lacustrine silt and clay. The sand and gravel beds have relatively high permeabilities, whereas the till and silt deposits have relatively low permeabilities. Water-table conditions prevail in unconfined sand and gravel along the valley margin. Artesian conditions are found locally in sand and gravel confined under silt and clay in the middle of the valley. Recharge occurs nearly everywhere on the valley floor, but principally along the margin of the valley, where highly permeable land surface conditions exist, and runoff from the hillsides is concentrated. The use of land overlying the aquifer is a mixture of residential, commercial, agricultural, and industrial uses.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8285","usgsCitation":"Miller, T.S., Belli, J.L., and Allen, R.V., 1982, Geohydrology of the valley-fill aquifer in the Corning area, Steuben County, New York: U.S. Geological Survey Open-File Report 82-85, 6 Plates: \t40.44 × 30.18 inches or smaller, https://doi.org/10.3133/ofr8285.","productDescription":"6 Plates: \t40.44 × 30.18 inches or smaller","costCenters":[],"links":[{"id":155672,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":52489,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0085/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52484,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0085/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":403284,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_45786.htm","linkFileType":{"id":5,"text":"html"}},{"id":52488,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0085/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52487,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0085/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52486,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0085/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52485,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0085/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New York","county":"Steuben County","otherGeospatial":"Corning area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.208,\n              42.008\n            ],\n            [\n              -76.967,\n              42.008\n            ],\n            [\n              -76.967,\n              42.25\n            ],\n            [\n              -77.208,\n              42.25\n            ],\n            [\n              -77.208,\n              42.008\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a87dc","contributors":{"authors":[{"text":"Miller, Todd S.","contributorId":85623,"corporation":false,"usgs":true,"family":"Miller","given":"Todd","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":189482,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Belli, J. L.","contributorId":83561,"corporation":false,"usgs":true,"family":"Belli","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":189481,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Allen, R. V.","contributorId":100862,"corporation":false,"usgs":true,"family":"Allen","given":"R.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":189483,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":57344,"text":"wdrNE811 - 1982 - Water resources data Nebraska, water year 1981","interactions":[],"lastModifiedDate":"2020-12-07T21:42:26.43236","indexId":"wdrNE811","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NE-81-1","title":"Water resources data Nebraska, water year 1981","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNE811","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data Nebraska, water year 1981: U.S. Geological Survey Water Data Report NE-81-1, viii, 471 p., https://doi.org/10.3133/wdrNE811.","productDescription":"viii, 471 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,{"id":25806,"text":"wri824119 - 1982 - A Two-dimensional finite-element model study of backwater and flow distribution at the I-10 crossing of the Pearl River near Slidell, Louisiana","interactions":[],"lastModifiedDate":"2012-02-02T00:08:34","indexId":"wri824119","displayToPublicDate":"1994-01-01T00:00:00","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":"82-4119","title":"A Two-dimensional finite-element model study of backwater and flow distribution at the I-10 crossing of the Pearl River near Slidell, Louisiana","docAbstract":"A two-dimensional finite-element surface-water flow modeling system was used to study the effect of Interstate Highway 10 on water-surface elevations and flow distribution during the flood on the Pearl River on April 2, 1980, near Slidell, La. A finite-element network was designed to represent the topography and vegetative cover of the study reach. Hydrographic data collected for the 1980 flood were used to calibrate the flow model. The finite-element network was then modified to represent conditions prior to roadway construction, and the hydraulic impact of I-10 was determined by comparing ' before ' and ' after ' results. Upstream from the roadway, maximum backwater at the west edge of the flood plain (1.5 ft) is greater than maximum backwater at the east edge (1.1 ft). Backwater ranging from 0.6 to 0.2 ft. extends more than a mile downstream from the Pearl River bridge opening in I-10 at the east edge of the flood plain, and drawdown of 0.2 ft. or more occurs along approximately 2 miles of the west edge of the flood plain downstream from I-10. The capability of the modeling system to simulate the significant features of steady-state flow in a complicated multi-channel river-flood-plain system with variable topography and vegetative was successfully demonstrated in this study. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824119","usgsCitation":"Lee, J.K., Froelich, D., Gilbert, J.J., and Wiche, G., 1982, A Two-dimensional finite-element model study of backwater and flow distribution at the I-10 crossing of the Pearl River near Slidell, Louisiana: U.S. Geological Survey Water-Resources Investigations Report 82-4119, vi, 66 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824119.","productDescription":"vi, 66 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123982,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4119/report-thumb.jpg"},{"id":54549,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4119/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54550,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4119/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54551,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4119/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54552,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4119/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54553,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4119/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54554,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4119/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54555,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4119/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54556,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4119/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54557,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4119/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd496de4b0b290850ef288","contributors":{"authors":[{"text":"Lee, J. 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,{"id":26187,"text":"wri8226 - 1982 - Streamflow and water-quality conditions, Wilsons Creek and James River, Springfield area, Missouri","interactions":[],"lastModifiedDate":"2017-12-06T12:52:13","indexId":"wri8226","displayToPublicDate":"1994-01-01T00:00:00","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":"82-26","title":"Streamflow and water-quality conditions, Wilsons Creek and James River, Springfield area, Missouri","docAbstract":"<p>A network of water-quality-monitoring stations was established upstream and downstream from the Southwest Wastewater-Treatment Plant on Wilsons Creek to monitor the effects of sewage effluent on water quality. Data indicate that 82 percent of the time the flow in Wilsons Creek upstream from the wastewater-treatment plant is less than the effluent discharged from the plant. On October 15, 1977, an advanced wastewater-treatment facility was put into operation. Of the four water-quality indicators measured at the monitoring stations (specific conductance, dissolved oxygen, pH, and water temperature), only dissolved oxygen showed improvement downstream from the plant. During urban runoff, the specific conductance momentarily increased and dissolved-oxygen concentration momentarily decreased in Wilsons Creek upstream from the plant. Urban runoff was found to have no long-term effects on specific conductance and dissolved oxygen downstream from the plant before or after the addition of the advanced wastewater-treatment facility. Data collected monthly from the James River showed that the dissolved-oxygen concentrations and the total nitrite plus nitrate nitrogen concentrations increased, whereas the dissolved-manganese concentrations decreased after the advanced wastewater-treatment facility became operational.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8226","usgsCitation":"Berkas, W.R., 1982, Streamflow and water-quality conditions, Wilsons Creek and James River, Springfield area, Missouri: U.S. Geological Survey Water-Resources Investigations Report 82-26, v, 38 p., https://doi.org/10.3133/wri8226.","productDescription":"v, 38 p.","numberOfPages":"49","costCenters":[],"links":[{"id":157616,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0026/report-thumb.jpg"},{"id":349774,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0026/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Missouri","city":"Springfield","otherGeospatial":"James River, Wilsons Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.49983215332031,\n              36.99322996239362\n            ],\n            [\n              -93.27529907226562,\n              36.99322996239362\n            ],\n            [\n              -93.27529907226562,\n              37.20462845803212\n            ],\n            [\n              -93.49983215332031,\n              37.20462845803212\n            ],\n            [\n              -93.49983215332031,\n              36.99322996239362\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4e9b","contributors":{"authors":[{"text":"Berkas, Wayne R. wrberkas@usgs.gov","contributorId":425,"corporation":false,"usgs":true,"family":"Berkas","given":"Wayne","email":"wrberkas@usgs.gov","middleInitial":"R.","affiliations":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"preferred":true,"id":195957,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57280,"text":"wdrND812 - 1982 - Water resources data, North Dakota, water year 1981. Volume 2. Missouri River Basin","interactions":[],"lastModifiedDate":"2020-10-28T19:28:38.907593","indexId":"wdrND812","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"ND-81-2","title":"Water resources data, North Dakota, water year 1981. Volume 2. Missouri River Basin","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrND812","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data, North Dakota, water year 1981. Volume 2. Missouri River Basin: U.S. Geological Survey Water Data Report ND-81-2, vii, 492 p., https://doi.org/10.3133/wdrND812.","productDescription":"vii, 492 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":379889,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1981/nd-81-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":185014,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1981/nd-81-2/report-thumb.jpg"}],"country":"United States","state":"North 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,{"id":24903,"text":"ofr82443 - 1982 - Plankton studies in San Francisco Bay; IV, Phytoplankton abundance and species composition, January 1980 - February 1981","interactions":[],"lastModifiedDate":"2016-07-27T12:52:55","indexId":"ofr82443","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-443","title":"Plankton studies in San Francisco Bay; IV, Phytoplankton abundance and species composition, January 1980 - February 1981","docAbstract":"<p>Data are presented on the phytoplankton species composition and abundance in San Francisco Bay from January 1980 through February 1981. Phytoplankton were identified and enumerated in surface samples collected approximately every two weeks at selected stations in the main channel of the Bay, and at shoal stations in the central portion of South San Francisco Bay, San Pablo Bay, and Suisun Bay. Also reported are separate species lists for microphytoplankton (&lt; 60 micrometers) and macrophytoplankton (&gt; 60 micrometers). (Author 's abstract)</p>","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82443","issn":"0094-9140","usgsCitation":"Wong, R., and Cloern, J., 1982, Plankton studies in San Francisco Bay; IV, Phytoplankton abundance and species composition, January 1980 - February 1981: U.S. Geological Survey Open-File Report 82-443, 152 p.  ill., 1 map ;28 cm., https://doi.org/10.3133/ofr82443.","productDescription":"152 p.  ill., 1 map ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":53882,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0443/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157669,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0443/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68556e","contributors":{"authors":[{"text":"Wong, R.L.","contributorId":104068,"corporation":false,"usgs":true,"family":"Wong","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":192770,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cloern, J. E.","contributorId":59453,"corporation":false,"usgs":true,"family":"Cloern","given":"J. E.","affiliations":[],"preferred":false,"id":192769,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7777,"text":"ofr82718 - 1982 - High-resolution seismic-reflection profiles collected aboard R/V James M. Gilliss Cruise GS-7903-3, over the Atlantic Continental Slope and Rise off New England","interactions":[],"lastModifiedDate":"2018-06-18T10:55:19","indexId":"ofr82718","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-718","title":"High-resolution seismic-reflection profiles collected aboard R/V James M. Gilliss Cruise GS-7903-3, over the Atlantic Continental Slope and Rise off New England","docAbstract":"<p>During June 1979, the U.S. Geological Survey (USGS) collected 4,032 km of single-channel seismic-reflection data from the Atlantic Continental Slope and Rise off New England. The work was conducted aboard R/V JAMES M. GILLISS (cruise GS-7903-3). The purpose of the cruise was to determine the characteristics of mass sediment movement on the Continental Slope, and to study and correlate the stratigraphy of the Jurassic and Cretaceous strata lying north and south of the New England seamount chain.</p><p>Seismic instrumentation included 40-in<sup>3</sup>, 160-in<sup>3</sup>, and 500-in<sup>3</sup> airguns; a Teledyne 800-joule minisparker system; a 3-5-kHz to 7-kHz, hull-mounted tunable transducer; and a 7-channel analog tape recorder.</p><p>Navigation control during the cruise was provided by a Western Integrated Navigation System capable of integrating satellite, rho-rho Loran-C, hyperbolic Loran-C, gyro compass, and doppler speed-log position data. The prime navigation sensor was the rho-rho Loran-C automatically recorded at 20-second intervals and manually plotted every 15 minutes, backed up by hyperbolic Loran-C fixes automatically recorded every 5 minutes.</p><p>Of the 4,032 km of data collected, 3,257 km of 3-5-kHz, minisparker and 40-in<sup>3</sup> airgun were for the sediment-slump studand the other 775 km of 3-5-kHz, minis parker, 160-in<sup>3</sup> air gun and 500-in<sup>3</sup> airgun were for the deep stratigraphy study. Overall, the quality of the data is excellent with good resolution and penetration.</p><p>The original data may be examined at the U.S. Geological Survey, Woods Hole, MA 02543. Copies of the data can be purchased only from the National Geophysical and Solar-Terrestrial Data Center, NOAA/EDIS/NGSDC, Code D621, 325 Broadway, Boulder, CO 80303 (303-497-6338).</p>","language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr82718","usgsCitation":"Bailey, N.G., and Aaron, J.M., 1982, High-resolution seismic-reflection profiles collected aboard R/V James M. Gilliss Cruise GS-7903-3, over the Atlantic Continental Slope and Rise off New England: U.S. Geological Survey Open-File Report 82-718, 2 p. :map ;28 cm., https://doi.org/10.3133/ofr82718.","productDescription":"2 p. :map ;28 cm.","costCenters":[],"links":[{"id":141234,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":259853,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0718/ofr1982718.pdf","text":"Report","size":"9:40 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 1982-718"}],"contact":"<p><a href=\"https://woodshole.er.usgs.gov/\" data-mce-href=\"https://woodshole.er.usgs.gov/\">Coastal and Marine Geology Program</a><br> U.S. Geological Survey<br> 384 Woods Hole Road<br> Woods Hole, MA 02543</p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db6887d0","contributors":{"authors":[{"text":"Bailey, Norman G.","contributorId":59439,"corporation":false,"usgs":true,"family":"Bailey","given":"Norman","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":156581,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aaron, John M.","contributorId":10031,"corporation":false,"usgs":true,"family":"Aaron","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":156580,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27126,"text":"wri8221 - 1982 - Evaluation of the streamflow-data program in Pennsylvania","interactions":[],"lastModifiedDate":"2017-07-05T11:20:45","indexId":"wri8221","displayToPublicDate":"1994-01-01T00:00:00","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":"82-21","title":"Evaluation of the streamflow-data program in Pennsylvania","docAbstract":"<p>The stream-gaging program in Pennsylvania is subject to budgetary&nbsp;constraints in the next several years. Elimination of those gaging stations&nbsp;that have no current-purpose use and little utility in providing regional&nbsp;flow-characteristic information is the most effective way to reduce costs.</p>\n<p>The efficient design of a network of gaging stations for obtaining regional information requires knowledge of the information in the data base and an assessment of the potential for improving the accuracy of data-transfer mechanisms. The analytical technique known as Network Analysis for Regional Information is used to assess acquired streamflow information and to evaluate its transferability within previously determined regions of homogenous streamflow characteristics. Regression equations that relate low-, mean-, and flood-flow characteristics to basin parameters are the data-transfer mechanisms used in the evaluation. This analysis showed that only minor improvements in the regression equations can be expected after 20 additional years of data collection at gages in the 1980 program. Transfer mechanisms with less model error are needed for improved data transferability.</p>\n<p>A more efficient program can be achieved by discontinuing selected gages in the planning-and-design network. To this end, 11 continuous-record and 25 partial-record gages were selected to be discontinued by April 1, 1980. Additionally, 6 continuous-record and 29 partial-record gages are suggested to be discontinued at the end of the 1985 water year.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8221","collaboration":"Prepared in cooperation with the Pennsylvania Department of Environmental Resources","usgsCitation":"Flippo, H.N., 1982, Evaluation of the streamflow-data program in Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 82-21, Report: iv, 56 p.; Plate: 21.03 x 13.87 inches, https://doi.org/10.3133/wri8221.","productDescription":"Report: iv, 56 p.; Plate: 21.03 x 13.87 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science 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,{"id":57263,"text":"wdrID811 - 1982 - Water Resources Data, Idaho, Water Year 1981--Volume 1. Great Basin and Snake River Basin above King Hill","interactions":[],"lastModifiedDate":"2012-02-02T00:12:22","indexId":"wdrID811","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"ID-81-1","title":"Water Resources Data, Idaho, Water Year 1981--Volume 1. Great Basin and Snake River Basin above King Hill","language":"ENGLISH","doi":"10.3133/wdrID811","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water Resources Data, Idaho, Water Year 1981--Volume 1. Great Basin and Snake River Basin above King Hill: U.S. Geological Survey Water Data Report ID-81-1, 447 p., 12 Fig., https://doi.org/10.3133/wdrID811.","productDescription":"447 p., 12 Fig.","costCenters":[],"links":[{"id":183482,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fba0e","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533050,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70188986,"text":"70188986 - 1982 - Use of packrat middens to determine rates of cliff retreat in the eastern Grand Canyon, Arizona","interactions":[],"lastModifiedDate":"2020-10-21T15:57:23.856889","indexId":"70188986","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Use of packrat middens to determine rates of cliff retreat in the eastern Grand Canyon, Arizona","docAbstract":"<p><span>Packrat midden data can be used to calculate rates of cliff retreat by relating midden age to the distance between cliff face and midden. Regression analysis using 14 radiocarbon-dated packrat deposits from the Mississippian Redwall Limestone in the eastern Grand Canyon suggests that the Redwall has been retreating at an average rate of 0.45 m/10</span><sup>3</sup><span><span>&nbsp;</span></span><sup>14</sup><span>C yr. This rate of cliff retreat, which is comparable to other cliff-retreat rates reported from arid environments, implies that the Colorado River cut through the Redwall Limestone in the vicinity of Horseshoe Mesa about 3.7 m.y. B.P.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1982)10<597:UOPMTD>2.0.CO;2","usgsCitation":"Cole, K.L., and Mayer, L., 1982, Use of packrat middens to determine rates of cliff retreat in the eastern Grand Canyon, Arizona: Geology, v. 10, no. 11, p. 597-599, https://doi.org/10.1130/0091-7613(1982)10<597:UOPMTD>2.0.CO;2.","productDescription":"3 p.","startPage":"597","endPage":"599","costCenters":[],"links":[{"id":343072,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Grand Canyon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.99938964843749,\n              35.46961797120201\n            ],\n            [\n              -111.302490234375,\n              35.46961797120201\n            ],\n            [\n              -111.302490234375,\n              36.910372213522535\n            ],\n            [\n              -114.99938964843749,\n              36.910372213522535\n            ],\n            [\n              -114.99938964843749,\n              35.46961797120201\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"10","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59660d1de4b0d1f9f05cef29","contributors":{"authors":[{"text":"Cole, Kenneth L.","contributorId":48533,"corporation":false,"usgs":true,"family":"Cole","given":"Kenneth","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":702249,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mayer, Larry","contributorId":77936,"corporation":false,"usgs":true,"family":"Mayer","given":"Larry","affiliations":[],"preferred":false,"id":702250,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70188684,"text":"70188684 - 1982 - A 40-foot static cone penetrometer","interactions":[],"lastModifiedDate":"2017-06-21T11:05:12","indexId":"70188684","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"seriesTitle":{"id":5431,"text":"Proceedings of the Offshore Technology Conference","active":true,"publicationSubtype":{"id":19}},"title":"A 40-foot static cone penetrometer","docAbstract":"<p><span>The Navy needs a lightweight device for testing seafloor soils to sub bottom depths of 12 meters in water depths to 60 meters. To meet this need a quasistatic cone penetration device that uses water jetting to reduce friction on the cone rod has been developed. This device is called the XSP-40. The 5-ton XSP-40 stands 15 meters tall and pushes a standard 5-ton cone into the seafloor. It is remotely controlled with an electronic unit on the deck of the support vessel. All cone outputs are recorded directly as a function of penetration depth with a strip chart recorder. A full suite of gauges is provided. on the electronic unit for monitoring the XSP-40's performance during a test .. About 40 penetration tests have been performed with very good success. </span><br><br><span>The XSP-40 was field tested in Norton Sound, off the west coast of Alaska. The general objective, in addition to evaluation of the device, was to gather geotechnical information on sediments that may be involved in processes potentially hazardous to offshore development. Four example penetration records are presented from gas charged sediment zones and areas near the Yukon River delta. In general it was determined that soil classification from cone data agreed well with classifications from core samples. Relative densities of the silt-sand to sandy-silt soils were usually very high. The significance of these results are discussed with respect to storm wave, liquefaction. </span><br><br><span>It is concluded that the XSP-40 is a durable and reliable piece of equipment capable of achieving penetration beyond that possible when not using the water jet system.</span></p>","conferenceTitle":"Offshore Technology Conference","conferenceDate":"May 3-6, 1982","conferenceLocation":"Houston, TX","language":"English","publisher":"Offshore Technology Conference","usgsCitation":"Beard, R., and Lee, H., 1982, A 40-foot static cone penetrometer, Offshore Technology Conference, Houston, TX, May 3-6, 1982, 12 p.","productDescription":"12 p.","costCenters":[],"links":[{"id":342706,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.onepetro.org/conference-paper/OTC-4300-MS"},{"id":342707,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"594b85b7e4b062508e382bba","contributors":{"authors":[{"text":"Beard, R.M.","contributorId":63139,"corporation":false,"usgs":true,"family":"Beard","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":698899,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, H.J.","contributorId":96693,"corporation":false,"usgs":true,"family":"Lee","given":"H.J.","email":"","affiliations":[],"preferred":false,"id":698900,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70188674,"text":"70188674 - 1982 - The use of vertical seismic profiles in seismic investigations of the earth","interactions":[],"lastModifiedDate":"2017-06-21T08:15:57","indexId":"70188674","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"The use of vertical seismic profiles in seismic investigations of the earth","docAbstract":"<p><span>During the past 8 years, the U.S. Geological Survey has conducted an extensive investigation on the use of vertical seismic profiles (VSP) in a variety of seismic exploration applications. Seismic sources used were surface air guns, vibrators, explosives, marine air guns, and downhole air guns. Source offsets have ranged from 100 to 7800 ft. Well depths have been from 1200 to over 10,000 ft. We have found three specific ways in which VSPs can be applied to seismic exploration. First, seismic events observed at the surface of the ground can be traced, level by level, to their point of origin within the earth. Thus, one can tie a surface profile to a well log with an extraordinarily high degree of confidence. Second, one can establish the detectability of a target horizon, such as a porous zone. One can determine (either before or after surface profiling) whether or not a given horizon or layered sequence returns a detectable reflection to the surface. The amplitude and character of the reflection can also be observed. Third, acoustic properties of a stratigraphic sequence can be measured and sometimes correlated to important exploration parameters. For example, sometimes a relationship between apparent attenuation and sand percentage can be established. The technique shows additional promise of aiding surface exploration indirectly through studies of the evolution of the seismic pulse, studies of ghosts and multiples, and studies of seismic trace inversion techniques. Nearly all current seismic data‐processing techniques are adaptable to the processing of VSP data, such as normal moveout (NMO) corrections, stacking, single‐and multiple‐channel filtering, deconvolution, and wavelet shaping.</span><br></p>","language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/1.1441357","usgsCitation":"Balch, A.H., Lee, M.W., Miller, J.J., and Ryder, R.T., 1982, The use of vertical seismic profiles in seismic investigations of the earth: Geophysics, v. 47, no. 6, p. 906-918, https://doi.org/10.1190/1.1441357.","productDescription":"13 p.","startPage":"906","endPage":"918","costCenters":[],"links":[{"id":342696,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"47","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"594b85b8e4b062508e382bc8","contributors":{"authors":[{"text":"Balch, Alfred H.","contributorId":71553,"corporation":false,"usgs":true,"family":"Balch","given":"Alfred","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":698867,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, Myung W.","contributorId":84358,"corporation":false,"usgs":true,"family":"Lee","given":"Myung","middleInitial":"W.","affiliations":[],"preferred":false,"id":698868,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, J. J.","contributorId":54588,"corporation":false,"usgs":true,"family":"Miller","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":698869,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ryder, Robert T. rryder@usgs.gov","contributorId":119319,"corporation":false,"usgs":true,"family":"Ryder","given":"Robert","email":"rryder@usgs.gov","middleInitial":"T.","affiliations":[{"id":596,"text":"U.S. Geological Survey National Center","active":false,"usgs":true},{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":698870,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70188920,"text":"70188920 - 1982 - On the distribution of species occurrence","interactions":[],"lastModifiedDate":"2025-06-05T16:35:42.631441","indexId":"70188920","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3001,"text":"Paleobiology","active":true,"publicationSubtype":{"id":10}},"title":"On the distribution of species occurrence","docAbstract":"<p>The distribution of species abundance (number of individuals per species) is well documented. The distribution of species occurrence (number of localities per species), however, has received little attention. This study investigates the distribution of species occurrence for five large data sets. For modern benthic foraminifera, species occurrence is examined from the Atlantic continental margin of North America, where 875 species were recorded 10,017 times at 542 localities, the Gulf of Mexico, where 848 species were recorded 18,007 times at 426 localities, and the Caribbean, where 1149 species were recorded 6684 times at 268 localities. For Late Cretaceous molluscs, species occurrence is examined from the Gulf Coast where 716 species were recorded 6236 times at 166 localities and a subset of this data consisting of 643 species recorded 3851 times at 86 localities.</p><p>Logseries and lognormal distributions were fitted to these data sets. In most instances the logseries best predicts the distribution of species occurrence. The lognormal, however, also fits the data fairly well, and, in one instance, better. The use of these distributions allows the prediction of the number of species occurring once, twice, …,<span>&nbsp;</span><span class=\"italic\">n</span><span>&nbsp;</span>times.</p><p>Species abundance data are also available for the molluscan data sets. They indicate that the most abundant species (greatest number of individuals) usually occur most frequently. In all data sets approximately half the species occur four or less times. The probability of noting the presence of rarely occurring species is small, and, consequently, such species must be used with extreme caution in studies requiring knowledge of the distribution of species in space and time.</p>","language":"English","publisher":"Cambridge University Press","doi":"10.1017/S0094837300004486","usgsCitation":"Buzas, M.A., Koch, C.F., Culver, S., and Sohl, N.F., 1982, On the distribution of species occurrence: Paleobiology, v. 8, no. 2, p. 143-150, https://doi.org/10.1017/S0094837300004486.","productDescription":"8 p.","startPage":"143","endPage":"150","costCenters":[],"links":[{"id":343007,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"2","noUsgsAuthors":false,"publicationDate":"2015-07-14","publicationStatus":"PW","scienceBaseUri":"59536ee1e4b062508e3c7b25","contributors":{"authors":[{"text":"Buzas, Martin A.","contributorId":85098,"corporation":false,"usgs":true,"family":"Buzas","given":"Martin","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":701233,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Koch, Carl F.","contributorId":8331,"corporation":false,"usgs":true,"family":"Koch","given":"Carl","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":701234,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Culver, Stephen J.","contributorId":79331,"corporation":false,"usgs":true,"family":"Culver","given":"Stephen J.","affiliations":[],"preferred":false,"id":701235,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sohl, Norman F.","contributorId":27906,"corporation":false,"usgs":true,"family":"Sohl","given":"Norman","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":701236,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70195436,"text":"70195436 - 1982 - Northern East Pacific Rise: Magnetic anomaly and bathymetric framework","interactions":[],"lastModifiedDate":"2018-03-05T15:13:24","indexId":"70195436","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Northern East Pacific Rise: Magnetic anomaly and bathymetric framework","docAbstract":"<p><span>The oceanic crust in the eastern Pacific between 7°N and 30°N and east of 127°W contains a fairly complete history of the spreading centers associated with the East Pacific Rise since 25 m.y. B.P. (late Oligocene). In this paper, we have summarized the seafloor spreading magnetic-anomaly data and the bathymetric data that reflect the record of this tectonic history. The well-defined magnetic lineations north of the Clarion fracture zone, in the mouth of the Gulf of California, and on the east flank of the East Pacific Rise (EPR) are carefully examined and used to provide a guide for interpreting the spreading pattern between the Clarion and Clipperton fracture zones, southward of the Rivera fracture zone over the Mathematician Ridge, and over the entire EPR east of the Mathematician Ridge between the Rivera and Siqueiros fracture zones. The bathymetric data provide a trace of the fracture zone pattern in each of the above mentioned areas. The fracture zone bathymetry and the seafloor spreading magnetic lineations on the EPR south of the Rivera fracture zone have a distinctive fanning pattern caused by close poles of rotation and plate boundary reorganizations. All these data provide a good record of the plate reorganizations in the middle Miocene at magnetic anomaly 5 A time (12.5 to 11 m.y. B.P.), in the late Miocene at magnetic anomaly 3′−4 time (6.5 m.y. B.P.), and in the Pliocene at magnetic anomaly 2′−3 time (3.5 m.y. B.P.). Several abandoned spreading centers, including the Mathematician Ridge, were left behind as a result of these reorganizations. The Mathematician Ridge is shown to be a set of ridges and trough whose origin is related to the tectonic activity associated with each of the above mentioned reorganizations since anomaly 5A.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB087iB08p06725","usgsCitation":"Klitgord, K.D., and Mammerickx, J., 1982, Northern East Pacific Rise: Magnetic anomaly and bathymetric framework: Journal of Geophysical Research B: Solid Earth, v. 87, no. B8, p. 6725-6750, https://doi.org/10.1029/JB087iB08p06725.","productDescription":"26 p.","startPage":"6725","endPage":"6750","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":351623,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"87","issue":"B8","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"5aff4241e4b0da30c1bfdac1","contributors":{"authors":[{"text":"Klitgord, Kim D.","contributorId":82307,"corporation":false,"usgs":true,"family":"Klitgord","given":"Kim","email":"","middleInitial":"D.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":728600,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mammerickx, Jacqueline","contributorId":202504,"corporation":false,"usgs":false,"family":"Mammerickx","given":"Jacqueline","email":"","affiliations":[],"preferred":false,"id":728601,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70207172,"text":"70207172 - 1982 - Triggering of large earthquakes by magma-chamber inflation, Izu Peninsula (Japan)","interactions":[],"lastModifiedDate":"2020-06-01T12:31:49.611074","indexId":"70207172","displayToPublicDate":"1982-12-11T11:34:14","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Triggering of large earthquakes by magma-chamber inflation, Izu Peninsula (Japan)","docAbstract":"<p><span>A close spatial and temporal association between three aseismic uplift episodes and subsequent large (M ≈ 7) earthquakes on the Izu Peninsula, Japan, suggests a causal relation. Quaternary geology, as well as studies by other workers, indicates a volcanic origin for the observed uplift, and we use a simple inflation model constrained by leveling data to compute the expected increments in normal and shear stress across faults that ruptured in the earthquakes. Using a Mohr-Coulomb criterion, we find that in two cases out of three, stress changes induced by inflation are in the correct sense to trigger failure. Although changes are no more than a few bars, they represent the equivalent of several decades to a century of secular stress buildup.</span></p>","language":"English","publisher":"GSA","doi":"10.1130/0091-7613(1982)10<637:TOLEBM>2.0.CO;2","usgsCitation":"Thatcher, W.R., and Savage, J.C., 1982, Triggering of large earthquakes by magma-chamber inflation, Izu Peninsula (Japan): Geology, v. 10, no. 12, p. 637-640, https://doi.org/10.1130/0091-7613(1982)10<637:TOLEBM>2.0.CO;2.","productDescription":"4 p.","startPage":"637","endPage":"640","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":370154,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Japan","otherGeospatial":"Izu Peninsula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              138.22723388671875,\n              34.53597500508991\n            ],\n            [\n              139.735107421875,\n              34.53597500508991\n            ],\n            [\n              139.735107421875,\n              35.55457449014312\n            ],\n            [\n              138.22723388671875,\n              35.55457449014312\n            ],\n            [\n              138.22723388671875,\n              34.53597500508991\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"10","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Thatcher, Wayne R. 0000-0001-6324-545X thatcher@usgs.gov","orcid":"https://orcid.org/0000-0001-6324-545X","contributorId":2599,"corporation":false,"usgs":true,"family":"Thatcher","given":"Wayne","email":"thatcher@usgs.gov","middleInitial":"R.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":777147,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Savage, James C. 0000-0002-5114-7673 jasavage@usgs.gov","orcid":"https://orcid.org/0000-0002-5114-7673","contributorId":2412,"corporation":false,"usgs":true,"family":"Savage","given":"James","email":"jasavage@usgs.gov","middleInitial":"C.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":777148,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70120261,"text":"70120261 - 1982 - Auditory evoked potentials in the West Indian Manatee (Sirenia: <i>Trichechus manatus</i>)","interactions":[],"lastModifiedDate":"2014-08-13T13:50:49","indexId":"70120261","displayToPublicDate":"1982-12-01T13:48:08","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2225,"text":"Journal of Comparative Physiology A","active":true,"publicationSubtype":{"id":10}},"title":"Auditory evoked potentials in the West Indian Manatee (Sirenia: <i>Trichechus manatus</i>)","docAbstract":"<p>Potentials evoked by clicks and tone pips were recorded by fine wires inserted extracranially in four West Indian manatees (<i>Trichechus manatus</i>) in air. Sounds were delivered via padded ear phones.</p>\n<br/>\n<p>Averaging a few thousand trials at 20/s reveals early peaks at N5.4 (‘vertex’ negativity to a frontal reference, at 5.4 ms), P7.6, N8.8, P9.5 — probably equivalent to waves IV and VII of the typical mammalian auditory brainstem response (ABR). Averaging 100 trials at <4/s suffices to reveal a complex sequence of later peaks including N25, P80, N150 and P190; consistent smaller peaks are visible when several hundred trials are averaged.</p>\n<br/>\n<p>Using tone pips with a rise and fall time of 2–5 ms the carrier frequency becomes important. Evoked potential wave forms are not the same at different frequencies, bringing out the fact that frequency is not a scalar that can be compensated for by intensity. Therefore the method was not used to obtain audiograms; however the largest EPs occur in the range of 1–1.5 kHz. EPs are found up to 35 kHz; almost no evoked potential is discernible at 40 kHz but the undistorted intensity available was limited. This is in reasonable agreement with the theoretical expectation for the upper limit of behavioral hearing from Heffner and Masterton based on head size and aquatic medium.</p.\n<br/>\n<p>Among several ear phone placements, that over the external auditory meatus was the most effective, but only slightly so. The external canal is presumably fluid or tissue filled and sound enters over a large area.</p>\n<br/>\n<p>Comparing data for two species on the most effective range of frequencies and the power spectra of their vocalizations, <i>T. manatus</i> is lower than <i>T. inunguis</i> in both respects.</p.\n<br/>\n<p>The results show the utility and limitations of the method of recording extracranial evoked potentials to sounds, especially for large and valuable animals under makeshift conditions.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Comparative Physiology A","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer Verlag","publisherLocation":"Berlin","doi":"10.1007/BF00619792","usgsCitation":"Bullock, T.H., O'Shea, T., and McClune, M.C., 1982, Auditory evoked potentials in the West Indian Manatee (Sirenia: <i>Trichechus manatus</i>): Journal of Comparative Physiology A, v. 148, no. 4, p. 547-554, https://doi.org/10.1007/BF00619792.","productDescription":"9 p.","startPage":"547","endPage":"554","numberOfPages":"9","costCenters":[],"links":[{"id":292104,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":292103,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00619792"}],"volume":"148","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ec7bc7e4b02bf5a7673ff3","contributors":{"authors":[{"text":"Bullock, Theodore H.","contributorId":56569,"corporation":false,"usgs":true,"family":"Bullock","given":"Theodore","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":498069,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O'Shea, Thomas J. 0000-0002-0758-9730","orcid":"https://orcid.org/0000-0002-0758-9730","contributorId":78071,"corporation":false,"usgs":true,"family":"O'Shea","given":"Thomas J.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":false,"id":498070,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McClune, Michael C.","contributorId":104826,"corporation":false,"usgs":true,"family":"McClune","given":"Michael","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":498071,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70120391,"text":"70120391 - 1982 - Use and interpretation of statistics in wildlife journals","interactions":[],"lastModifiedDate":"2014-08-14T09:15:58","indexId":"70120391","displayToPublicDate":"1982-12-01T09:10:44","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":"Use and interpretation of statistics in wildlife journals","docAbstract":"Use and interpretation of statistics in wildlife journals are reviewed, and suggestions for improvement are offered.  Populations from which inferences are to be drawn should be clearly defined, and conclusions should be limited to the range of the data analyzed.  Authors should be careful to avoid improper methods of plotting data and should clearly define the use of estimates of variance, standard deviation, standard error, or confidence intervals.  Biological and statistical significant are often confused by authors and readers.  Statistical hypothesis testing is a tool, and not every question should be answered by hypothesis testing.  Meeting assumptions of hypothesis tests is the responsibility of authors, and assumptions should be reviewed before a test is employed.  The use of statistical tools should be considered carefully both before and after gathering data.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wildlife Society Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Wildlife Society","publisherLocation":"Bethesda, MD","usgsCitation":"Tacha, T.C., Warde, W.D., and Burnham, K.P., 1982, Use and interpretation of statistics in wildlife journals: Wildlife Society Bulletin, v. 10, no. 4, p. 355-362.","productDescription":"8 p.","startPage":"355","endPage":"362","numberOfPages":"8","costCenters":[],"links":[{"id":292145,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53edcd56e4b0f61b386d24b9","contributors":{"authors":[{"text":"Tacha, Thomas C.","contributorId":97434,"corporation":false,"usgs":true,"family":"Tacha","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":498127,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Warde, William D.","contributorId":84669,"corporation":false,"usgs":true,"family":"Warde","given":"William","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":498125,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Burnham, Kenneth P.","contributorId":95025,"corporation":false,"usgs":true,"family":"Burnham","given":"Kenneth","email":"","middleInitial":"P.","affiliations":[{"id":189,"text":"Colorado Cooperative Fish and Wildlife Research Unit","active":false,"usgs":true}],"preferred":false,"id":498126,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011491,"text":"70011491 - 1982 - Natural groundwater recharge in an upland area of central North Dakota, U.S.A.","interactions":[],"lastModifiedDate":"2025-04-10T23:18:52.172669","indexId":"70011491","displayToPublicDate":"1982-11-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Natural groundwater recharge in an upland area of central North Dakota, U.S.A.","docAbstract":"<p><span>The magnitude of groundwater recharge to coal aquifers in a 150-km</span><sup>2</sup><span>&nbsp;area in west-central North Dakota was determined using three separate approaches: (1) the net water level rise in water-table wells; (2) calculations of the fluid flux between nested piezometers, using the Darcy equation and measured values of hydraulic conductivity and vertical gradients; and (3) evaluation of the inputs to and outputs from the coal aquifer, using a steady-state control volume approach in which the aquifer was divided into semi-rectangular cells bounded by equipotential lines and flow lines. Measurements of potential gradients and hydraulic conductivity permitted indirect determination of all components of flow into and out of the cell except the recharge input, which was determined by difference.</span></p><p><span>All methods yielded consistent results on the order of 0.04-0.01 m yr.<sup>−1</sup>&nbsp;These values, which represent 2–9% of the annual precipitation, are consistent with results of other studies on recharge throughout the prairies of North America.</span></p><p><span>Evaluation of site hydrology and stable-isotope data indicates that recharge is restricted in both time and place. Most recharge occurs in late spring and in the fall following heavy rainfall events. During these seasons the ground is not frozen and vegetation is not transpiring large amounts of water. Some recharge may occur during very heavy localized summer storms, but it is not considered volumetrically significant. Major permanent depressions on the site are a source of significant recharge. In addition, the extensive area of ephemeral standing water bodies that result from snowmelt can produce significant amounts of infiltration over the entire site.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(82)90093-2","issn":"00221694","usgsCitation":"Rehm, B., Moran, S., and Groenewold, G., 1982, Natural groundwater recharge in an upland area of central North Dakota, U.S.A.: Journal of Hydrology, v. 59, no. 3-4, p. 293-314, https://doi.org/10.1016/0022-1694(82)90093-2.","productDescription":"22 p.","startPage":"293","endPage":"314","costCenters":[],"links":[{"id":221048,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"central North Dakota","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -102.60876813870183,\n              49.012008277756365\n            ],\n            [\n              -102.60876813870183,\n              45.988974212508225\n            ],\n            [\n              -99.24442932052045,\n              45.988974212508225\n            ],\n            [\n              -99.24442932052045,\n              49.012008277756365\n            ],\n            [\n              -102.60876813870183,\n              49.012008277756365\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"59","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a630be4b0c8380cd7227b","contributors":{"authors":[{"text":"Rehm, B.W.","contributorId":73748,"corporation":false,"usgs":true,"family":"Rehm","given":"B.W.","email":"","affiliations":[],"preferred":false,"id":361247,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moran, S.R.","contributorId":20888,"corporation":false,"usgs":true,"family":"Moran","given":"S.R.","email":"","affiliations":[],"preferred":false,"id":361246,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Groenewold, G.H.","contributorId":14113,"corporation":false,"usgs":true,"family":"Groenewold","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":361245,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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