{"pageNumber":"2445","pageRowStart":"61100","pageSize":"25","recordCount":68807,"records":[{"id":70039201,"text":"70039201 - 1972 - The EROS Data Center","interactions":[],"lastModifiedDate":"2017-06-05T21:55:52","indexId":"70039201","displayToPublicDate":"1972-01-01T11:28:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":363,"text":"General Interest Publication","active":false,"publicationSubtype":{"id":6}},"title":"The EROS Data Center","docAbstract":"The EROS Data Center in Sioux Falls, South Dakota, is operated for the Earth Resources Observation Systems Program of the Department of the Interior by the Topographic Division of the Geological Survey to provide access to Earth Resources Technology Satellite (ERTS) imagery, USGS aerial photography, and NASA aircraft data for the general public, domestic government agencies at all levels, and foreign government agencies at all levels, and foreign governments. Facilities are available for data storage, retrieval, reproduction, and dissemination, and for user assistance and training.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039201","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, The EROS Data Center: General Interest Publication, 18 p., https://doi.org/10.3133/70039201.","productDescription":"18 p.","numberOfPages":"20","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":261368,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039201/report.pdf"},{"id":261369,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039201/report-thumb.jpg"}],"country":"United States","state":"South Dakota","city":"Sioux Falls","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -97,43.36666666666667 ], [ -97,43.75 ], [ -96.36666666666666,43.75 ], [ -96.36666666666666,43.36666666666667 ], [ -97,43.36666666666667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba70de4b08c986b32133f","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":535240,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70121221,"text":"70121221 - 1972 - Interstitial water studies on small core samples, Leg 9","interactions":[],"lastModifiedDate":"2019-12-19T17:27:22","indexId":"70121221","displayToPublicDate":"1972-01-01T09:34:41","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1997,"text":"Initial reports of the Deep Sea Drilling Project","active":true,"publicationSubtype":{"id":10}},"title":"Interstitial water studies on small core samples, Leg 9","docAbstract":"The chemistry of the pore fluids obtained on Leg 9 is remarkable primarily in its constancy. Excepting silicon and strontium, only at one site do the concentrations of the major and minor constituents deviate notably from sea water concentrations (see Tables 1 and 2). The trends, or lack of them, seen in these samples have been discussed previously and only references will be given here. The constancy of composition and similarity to sea water is particularly noteworthy, as the sediments at all of the 9 sites are thought to be intruded by the basal basalt. The pore fluid chemistry exhibits no evidence of intrusion except possibly at Site 84.","language":"English","publisher":"National Science Foundation","doi":"10.2973/dsdp.proc.9.117.1972","usgsCitation":"Sayles, F., Waterman, L., and Manheim, F., 1972, Interstitial water studies on small core samples, Leg 9: Initial reports of the Deep Sea Drilling Project, v. 9, p. 845-855, https://doi.org/10.2973/dsdp.proc.9.117.1972.","productDescription":"11 p.","startPage":"845","endPage":"855","numberOfPages":"11","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":488223,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"http://doi.org/10.2973/dsdp.proc.9.117.1972","text":"Publisher Index Page"},{"id":292606,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":292599,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2973/dsdp.proc.9.117.1972"}],"otherGeospatial":"Pacific Ocean","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -150.0,-20.0 ], [ -150.0,20.0 ], [ -75.0,20.0 ], [ -75.0,-20.0 ], [ -150.0,-20.0 ] ] ] } } ] }","volume":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f5b655e4b09d12e0e8e6ed","contributors":{"authors":[{"text":"Sayles, F.L.","contributorId":77657,"corporation":false,"usgs":true,"family":"Sayles","given":"F.L.","email":"","affiliations":[],"preferred":false,"id":498818,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waterman, L.S.","contributorId":25474,"corporation":false,"usgs":true,"family":"Waterman","given":"L.S.","affiliations":[],"preferred":false,"id":498816,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Manheim, F.T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":55421,"corporation":false,"usgs":true,"family":"Manheim","given":"F.T.","affiliations":[],"preferred":false,"id":498817,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":25187,"text":"25187 - 1972 - Outer continental shelf statistics : oil, gas, sulfur, salt, leasing, drilling, production, income","interactions":[],"lastModifiedDate":"2014-07-15T09:13:11","indexId":"25187","displayToPublicDate":"1972-01-01T09:12:34","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Outer continental shelf statistics : oil, gas, sulfur, salt, leasing, drilling, production, income","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Dept. of Interior","publisherLocation":"Washington, D.C.","doi":"10.3133/25187","issn":"0364-7064","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Outer continental shelf statistics : oil, gas, sulfur, salt, leasing, drilling, production, income, https://doi.org/10.3133/25187.","costCenters":[],"links":[{"id":290089,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c64da9e4b0001bd5147792","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":529202,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1381,"text":"wsp1999G - 1972 - Ground-water outflow from Chino Basin, Upper Santa Ana Valley, southern California","interactions":[],"lastModifiedDate":"2023-03-24T19:16:07.213168","indexId":"wsp1999G","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1999","chapter":"G","title":"Ground-water outflow from Chino Basin, Upper Santa Ana Valley, southern California","docAbstract":"Ground-water outflow from Chino basin was calculated ,by a direct method using the equation Q = PIA, in which Q is the quantity of ground-water outflow, P is the average coefficient of permeability of the sediments through which the flow occurs, I is the average hydraulic gradient, and A is the cross-sectional area of the sediments through which the flow occurs. The period selected for the calculation was 1930-66. \r\n\r\nPermeability of the water-bearing sediments was calculated from aquifer test data and from computations involving specific-capacity data from 200 wells in the outflow area. Permeability ranged from less than 100 to more than 5,000 gallons per day per square foot. \r\n\r\nThe annual hydraulic gradient was derived from contour maps of average water levels in wells for each water year for the period 1930-66. \r\n\r\nThe cross-sectional area used to calculate ground-water outflow from Chino basin extends southwestward from Pedley Hills to Puente Hills. The area of the outflow section is the saturated thickness of permeable materials measured along the line of section. Part of the lower boundary is the interface between the alluvium and the underlying basement complex, and part is a change in permeability within sedimentary rocks. Geological methods were combined with geophysical methods to determine the cross-sectional area of the water-bearing sediments. Gravity and seismic traverses, drill-hole logs, and data from a more than 600 drill holes, including eight test holes drilled as a part of this investigation, were used to delineate the size and the shape of the outflow area. For the period of calculation, 1930-66, the total area of the outflow section varied from about 16 to 22 million square feet. The fluctuation in total area is caused by changes in the altitude of the water table. \r\n\r\nAnnual ground-water outflow from Chino basin calculated by the direct method for the period 1930-66 ranged from 38,000 acre-feet in the 1941 water year to 9,400 acre-feet in the 1966 water year.\r\n\r\nTwo indirect methods of calculating ground-water outflow were studied as a part of this project: the chemical method and the water-budget method. The chemical method was found to be unsatisfactory. Although the ground-water discharge into the Santa Ana River from Chino basin is quite different in chemical composition from the discharge from Temescal basin, there is no known way to quantitatively separate the total discharge with respect to source. In the water-budget method direct runoff and evapotranspiration were reevaluated, and the ground-water outflow from Temescal basin was calculated by the same direct method employed for Chino basin. Annual ground-water outflow from Temescal basin calculated by the direct method for the period 1930-66 ranged from 11,000 acre-feet in the 1940 and 1945 water years to 3,000 acre-feet in the 1965 water year. Annual ground-water outflow from Chino basin computed by the water-budget method for the period 1933-63 ranged from 45,000 acre-feet in the 1941 water year to 10,000 acre-feet in the 1963 water year.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1999G","usgsCitation":"French, J.J., 1972, Ground-water outflow from Chino Basin, Upper Santa Ana Valley, southern California: U.S. Geological Survey Water Supply Paper 1999, Report: iv, 28 p.; 1 Plate: 37.00 x 20.00 inches, https://doi.org/10.3133/wsp1999G.","productDescription":"Report: iv, 28 p.; 1 Plate: 37.00 x 20.00 inches","costCenters":[],"links":[{"id":414721,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25354.htm","linkFileType":{"id":5,"text":"html"}},{"id":26484,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1999g/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26483,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1999g/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137352,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1999g/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Chino basin, Upper Santa Ana Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -117.75,\n              34.033\n            ],\n            [\n              -117.75,\n              33.816\n            ],\n            [\n              -117.417,\n              33.816\n            ],\n            [\n              -117.417,\n              34.033\n            ],\n            [\n              -117.75,\n              34.033\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cee4b07f02db5455d7","contributors":{"authors":[{"text":"French, James J.","contributorId":103651,"corporation":false,"usgs":true,"family":"French","given":"James","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":143668,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70009762,"text":"70009762 - 1972 - Microcoulometric measurement of water in minerals","interactions":[],"lastModifiedDate":"2020-12-23T21:46:03.156376","indexId":"70009762","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","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":"Microcoulometric measurement of water in minerals","docAbstract":"<div id=\"aep-abstract-id6\" class=\"abstract author\"><div id=\"aep-abstract-sec-id7\"><p id=\"simple-para.0010\">A DuPont Moisture Analyzer is used in a microcoulometric method for determining water in minerals. Certain modifications, which include the heating of the sample outside the instrument, protect the system from acid gases and insure the conversion of all hydrogen to water vapor. Moisture analyzer data are compared to concurrent data obtained by a modified Penfield method. In general, there is a positive bias of from 0.1 to 0.2% in the moisture analyzer results and a similarity of bias in minerals of the same kind. Inhomogeneity, sample size, and moisture pick-up are invoked to explain deviations. The method is particularly applicable to small samples.</p></div></div><div id=\"aep-abstract-id8\" class=\"abstract author\" lang=\"fr\"><br></div>","language":"English","publisher":"Elsevier","doi":"10.1016/S0003-2670(01)81898-5","issn":"00032670","usgsCitation":"Cremer, M., Elsheimer, H., and Escher, E., 1972, Microcoulometric measurement of water in minerals: Analytica Chimica Acta, v. 60, no. 1, p. 183-192, https://doi.org/10.1016/S0003-2670(01)81898-5.","productDescription":"10 p.","startPage":"183","endPage":"192","numberOfPages":"10","costCenters":[],"links":[{"id":219268,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"60","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5672e4b0c8380cd6d5d1","contributors":{"authors":[{"text":"Cremer, M.","contributorId":28865,"corporation":false,"usgs":true,"family":"Cremer","given":"M.","email":"","affiliations":[],"preferred":false,"id":357080,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elsheimer, H.N.","contributorId":77523,"corporation":false,"usgs":true,"family":"Elsheimer","given":"H.N.","email":"","affiliations":[],"preferred":false,"id":357081,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Escher, E.E.","contributorId":94160,"corporation":false,"usgs":true,"family":"Escher","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":357082,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":93760,"text":"93760 - 1972 - Wetlands and waterfowl relationships","interactions":[],"lastModifiedDate":"2018-01-04T12:22:39","indexId":"93760","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Wetlands and waterfowl relationships","language":"English","publisher":"U.S. Department of Agriculture","usgsCitation":"Nelson, H., 1972, Wetlands and waterfowl relationships, 12 p.","productDescription":"12 p.","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":127842,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4893e4b07f02db520d7c","contributors":{"authors":[{"text":"Nelson, H.K.","contributorId":21489,"corporation":false,"usgs":true,"family":"Nelson","given":"H.K.","email":"","affiliations":[],"preferred":false,"id":297882,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000187,"text":"1000187 - 1972 - Downstream migration of recently transformed sea lampreys before and after treatment of a Lake Michigan tributary with a lampricide","interactions":[],"lastModifiedDate":"2025-03-04T16:45:25.143844","indexId":"1000187","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Downstream migration of recently transformed sea lampreys before and after treatment of a Lake Michigan tributary with a lampricide","docAbstract":"After the Pere Marquette River was treated with a lampricide in May 1964, the number of recently transformed sea lampreys (Petromyzon marinus) collected in the water-intake structure of a chemical plant near the mouth of the stream dropped 99.5%, from 13,913 (average for 1962-63 and 1963-64) to 76 (average for the next four migration seasons). Average length of the lampreys caught increased markedly after the treatment. In five of the six migration seasons, the catch of downstream migrants was higher in the fall than in the spring.","language":"English","publisher":"Canadian Science Publishing","doi":"10.1139/f72-186","usgsCitation":"Hodges, J.W., 1972, Downstream migration of recently transformed sea lampreys before and after treatment of a Lake Michigan tributary with a lampricide: Journal of the Fisheries Research Board of Canada, v. 29, no. 8, p. 1237-1240, https://doi.org/10.1139/f72-186.","productDescription":"4 p.","startPage":"1237","endPage":"1240","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":129283,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635fbf","contributors":{"authors":[{"text":"Hodges, John W.","contributorId":58593,"corporation":false,"usgs":true,"family":"Hodges","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":308206,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70009753,"text":"70009753 - 1972 - Determination of nanogram amounts of bismuth in rocks by substoichiometric isotope dilution analysis","interactions":[],"lastModifiedDate":"2020-12-23T21:47:43.550412","indexId":"70009753","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","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":"Determination of nanogram amounts of bismuth in rocks by substoichiometric isotope dilution analysis","docAbstract":"<div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><p id=\"simple-para.0010\">A rapid procedure suitable for the routine determination of 1–10 ng of bismuth in a silicate rock matrix is described. Results for the U.S. Geological Survey standard rocks are presented. Rocks and minerals are dissolved in hydrofluoric-perchloric acid in the presence of<span>&nbsp;</span><sup>207</sup>Bi tracer and the silica is removed by evaporation. The perchloric acid residue is taken up in water and bismuth iodide is extracted into methyl isobutyl ketone. After three acid-iodide washes, the bismuth is stripped into water and reacted with a substoichiometric amount of EDTA. Excess of bismuth is extracted as the iodide and the specific activity of the bismuth-EDTA complex is determined.</p></div></div><div id=\"aep-abstract-id6\" class=\"abstract author\" lang=\"fr\"><br></div>","language":"English","publisher":"Elsevier","doi":"10.1016/S0003-2670(01)81895-X","issn":"00032670","usgsCitation":"Greenland, L.P., and Campbell, E., 1972, Determination of nanogram amounts of bismuth in rocks by substoichiometric isotope dilution analysis: Analytica Chimica Acta, v. 60, no. 1, p. 159-165, https://doi.org/10.1016/S0003-2670(01)81895-X.","productDescription":"7 p.","startPage":"159","endPage":"165","numberOfPages":"7","costCenters":[],"links":[{"id":219183,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"60","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ffb7e4b0c8380cd4f358","contributors":{"authors":[{"text":"Greenland, L. Paul","contributorId":22488,"corporation":false,"usgs":true,"family":"Greenland","given":"L.","email":"","middleInitial":"Paul","affiliations":[],"preferred":false,"id":357065,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, E.Y.","contributorId":59803,"corporation":false,"usgs":true,"family":"Campbell","given":"E.Y.","email":"","affiliations":[],"preferred":false,"id":357066,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70176806,"text":"70176806 - 1972 - Annual summary of water quality data for selected sites in the Pacific Northwest, October 1971 to September 1972","interactions":[],"lastModifiedDate":"2016-10-21T13:08:54","indexId":"70176806","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Annual summary of water quality data for selected sites in the Pacific Northwest, October 1971 to September 1972","docAbstract":"<p>Water resources data collected in the Pacific Northwest during the 1972 water year include chemical and physical characteristics of surface water. Data included in this report were collected by the Water Resources Division of the U.S. Geological Survey under the direction of the following district chiefs: H.K. Hall, Idaho; George M. Pike, Montana; S.F. Kapustka, Oregon; and L.B. Laird, Washington. </p><p>The Geological Survey has published records of chemical quality, water temperatures, and sediment since 1941 in an annual series of water-supply papers entitled \"Quality of Surface Waters of the United States.\" Beginning with the 1964 water year, water-quality records have been published by the Geological Survey in annual reports on a State-boundary basis. These reports are available from the district offices. </p><p>This report is for limited distribution and is intended primarily for rapid release of selected data shortly after the end of the water year. Data contained herein is provisional and subject to revision before final publication in the foregoing reports. The following pages contain listings of selected constituents and their values&nbsp;sampled at 34 selected sites in the'Pacific Northwest. The sites are listed in downstream order by states. The constituent values recorded in the tables are the results of laboratory determinations except for water temperature, Ph, Dissolved Oxygen, Specific Conductance, Alkalinity, and Immediate Coliform count, which are the results of field determinations. </p><p>These data were collected and analyzed by the Geological Survey under cooperative programs with Environmental Protection Agency and other Federal, State, County, and municipal organizations as identified in the annual State-wide reports. Additional water-quality data may be obtained from district offices of the Geological Survey and from Environmental Protection Agency.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/70176806","usgsCitation":"U.S. Geological Survey Northwest Water Resources Data Center, 1972, Annual summary of water quality data for selected sites in the Pacific Northwest, October 1971 to September 1972, 35 p., https://doi.org/10.3133/70176806.","productDescription":"35 p.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":329383,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70176806.jpg"},{"id":330317,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70176806/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho, Montana, Oregon, Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.8486328125,\n              41.16211393939692\n            ],\n            [\n              -124.8486328125,\n              49.009050809382046\n            ],\n            [\n              -110.32470703125,\n              49.009050809382046\n            ],\n            [\n              -110.32470703125,\n              41.16211393939692\n            ],\n            [\n              -124.8486328125,\n              41.16211393939692\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57f7c08be4b0bc0bec09c7ed","contributors":{"authors":[{"text":"U.S. Geological Survey Northwest Water Resources Data Center","contributorId":175193,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey Northwest Water Resources Data Center","id":650384,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70190911,"text":"70190911 - 1972 - Water-quality data for the Flaming Gorge Reservoir area, Utah and Wyoming, 1969-72","interactions":[],"lastModifiedDate":"2017-09-17T11:51:43","indexId":"70190911","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5498,"text":"Utah Basic-Data Release","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"24","title":"Water-quality data for the Flaming Gorge Reservoir area, Utah and Wyoming, 1969-72","docAbstract":"<p>This report presents the basic data that were collected by the U.S. Geological Survey during a study of the chemical quality of water in Flaming Gorge Reservoir. An interpretive report will follow. The basic data were collected from the reservoir during six sampling runs between October 1970 and September 1972. The reservoir was sampled for chemical analyses at 17 sites. Chemical and physical data were measured in situ at 34 sites. The sites are shown in figure 1 and the data are listed in tables 1 and 3-6.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","usgsCitation":"Bolke, E., and Waddell, K., 1972, Water-quality data for the Flaming Gorge Reservoir area, Utah and Wyoming, 1969-72: Utah Basic-Data Release 24, iii, 50 p.","productDescription":"iii, 50 p.","numberOfPages":"56","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345837,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345836,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/docview.exe?Folder=TP21-1-480&Title=Basic+Data+Report+24"}],"country":"United States","state":"Utah","otherGeospatial":"Flaming Gorge Reservoir","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59bf899ce4b091459a5e0889","contributors":{"authors":[{"text":"Bolke, E.L.","contributorId":52151,"corporation":false,"usgs":true,"family":"Bolke","given":"E.L.","affiliations":[],"preferred":false,"id":710678,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waddell, K.M.","contributorId":59009,"corporation":false,"usgs":true,"family":"Waddell","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":710679,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":48075,"text":"ofr72348 - 1972 - Water-resources reconnaissance of Anaktuvuk Pass, Alaska","interactions":[],"lastModifiedDate":"2023-08-29T20:48:49.921019","indexId":"ofr72348","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","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":"72-348","title":"Water-resources reconnaissance of Anaktuvuk Pass, Alaska","docAbstract":"<p>A hydrologic reconnaissance was made of Anaktuvuk pass in the central Brooks Range during the summer of 1971 to help develop a water supply for the village school. Winter icings and summer flow conditions in Contact Creek both indicate that ground water is present beneath the creek bed. A well-site area was selected in the channel of Contact Creek near the school where the prospects of obtaining a suitable ground-water supply seem best. In the event that wells are unsuccessful, water can be hauled from Eleanor Lake to the school. Chemical quality of water at Anaktuvuk Pass is excellent, but any source of water may be subject to bacterial contamination and would require treatment.<br><br></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72348","collaboration":"Prepared in cooperation with Alaska Department of Public Works","usgsCitation":"Sloan, C.E., 1972, Water-resources reconnaissance of Anaktuvuk Pass, Alaska: U.S. Geological Survey Open-File Report 72-348, 12 p., https://doi.org/10.3133/ofr72348.","productDescription":"12 p.","costCenters":[],"links":[{"id":420269,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0348/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":161858,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0348/report-thumb.jpg"},{"id":415301,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52154.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","otherGeospatial":"Anaktuvuk Pass","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -151.7564,\n              68.1667\n            ],\n            [\n              -151.7564,\n              68.1\n            ],\n            [\n              -151.6833,\n              68.1\n            ],\n            [\n              -151.6833,\n              68.1667\n            ],\n            [\n              -151.7564,\n              68.1667\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9bea","contributors":{"authors":[{"text":"Sloan, Charles E.","contributorId":74364,"corporation":false,"usgs":true,"family":"Sloan","given":"Charles","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":236774,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70161840,"text":"70161840 - 1972 - Virucidal activity of two Iodophors to salmonid viruses","interactions":[],"lastModifiedDate":"2016-01-06T16:01:06","indexId":"70161840","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Virucidal activity of two Iodophors to salmonid viruses","docAbstract":"<p><span>Wescodyne</span><sup>&reg;</sup><span>&nbsp;and Betadine</span><sup>&reg;</sup><span>, organic iodine complexes, were compared in vitro for virucidal activity against infectious hematopoietic necrosis (IHN), infectious pancreatic necrosis (IPN), and viral hemorrhagic septicemia (VHS) viruses. Both iodophors were about equally effective on all three viruses. Each iodophor completely destroyed IHN virus within 30&ensp;sec at 12&ensp;ppm iodine, and was not affected by water hardness. Virucidal activity, however, was reduced at&nbsp;</span><i>p</i><span>H levels above 8.0 and in the presence of organic matter. Wescodyne was also compared with seven disinfectants commonly used in fish hatcheries, for virucidal properties against IHN virus. Wescodyne and chlorine were the only disinfectants to completely destroy the virus. Either Wescodyne or Betadine would effectively destroy the salmonid viruses at less than 25&ensp;ppm iodine within 5&ensp;min in solutions near neutrality.</span></p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/f72-008","usgsCitation":"Amend, D.F., and Pietsch, J.P., 1972, Virucidal activity of two Iodophors to salmonid viruses: Journal of the Fisheries Research Board of Canada, v. 29, no. 1, p. 61-65, https://doi.org/10.1139/f72-008.","productDescription":"5 p.","startPage":"61","endPage":"65","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":313983,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568e493de4b0e7a44bc41ae8","contributors":{"authors":[{"text":"Amend, Donald F.","contributorId":106543,"corporation":false,"usgs":true,"family":"Amend","given":"Donald","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":587902,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pietsch, John P.","contributorId":152099,"corporation":false,"usgs":false,"family":"Pietsch","given":"John","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":587903,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70161834,"text":"70161834 - 1972 - Some physiological consequences of handling stress in the juvenile coho salmon (Oncorhynchus kisutch) and steelhead trout (Salmo gairdneri)","interactions":[],"lastModifiedDate":"2016-01-06T15:36:13","indexId":"70161834","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Some physiological consequences of handling stress in the juvenile coho salmon (Oncorhynchus kisutch) and steelhead trout (Salmo gairdneri)","docAbstract":"<p><span>The stress of handling juvenile coho salmon (</span><i>Oncorhynchus kisutch</i><span>) and steelhead trout (</span><i>Salmo gairdneri</i><span>) in soft water and in water with added salts was evaluated using blood and tissue chemistry fluctuations as indices of metabolic and endocrine function. Changes in plasma glucose, chloride, calcium, and cholesterol levels indicated that significant osmoregulatory and metabolic dysfunctions can occur and persist for about 24&ensp;hr after handling in soft water. Pituitary activation, as judged by lack of interrenal ascorbate depletion, did not occur. Increasing the ambient NaCl and Ca</span><sup>++</sup><span>&nbsp;levels to about 100 milliosmols and 75&ndash;120&ensp;ppm, respectively, partially or completely alleviated the hyperglycemia and hypochloremia indicating that the stress of handling had been reduced.</span></p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/f72-284","usgsCitation":"Wedemeyer, G., 1972, Some physiological consequences of handling stress in the juvenile coho salmon (Oncorhynchus kisutch) and steelhead trout (Salmo gairdneri): Journal of the Fisheries Research Board of Canada, v. 29, no. 12, p. 1780-1783, https://doi.org/10.1139/f72-284.","productDescription":"4 p.","startPage":"1780","endPage":"1783","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":313975,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568e492ee4b0e7a44bc41a8f","contributors":{"authors":[{"text":"Wedemeyer, Gary gwedemeyer@usgs.gov","contributorId":5504,"corporation":false,"usgs":true,"family":"Wedemeyer","given":"Gary","email":"gwedemeyer@usgs.gov","affiliations":[],"preferred":true,"id":587882,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010130,"text":"70010130 - 1972 - The martian atmosphere: Mariner 9 television experiment progress report","interactions":[],"lastModifiedDate":"2020-12-23T01:19:15.028627","indexId":"70010130","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"The martian atmosphere: Mariner 9 television experiment progress report","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id14\" class=\"abstract author\"><div id=\"aep-abstract-sec-id15\"><p>Atmospheric phenomena appearing in the Mariner 9 television pictures are discussed in detail. The surface of the planet was heavily obscured by a global dust storm during the first month in orbit. Brightness data during this period can be fitted by a semi-infinite scattering and absorbing atmosphere model with a single-scattering albedo in the range 0.70–0.85. This low value suggests that the mean radius of the particles responsible for the obscuration was at least 10 μm. By the end of the second month, this dust storm had largely dissipated, leaving a residual optical depth ∼0.1. Much of the region north of 45°N was covered by variable clouds comprising the north polar hood. The cloud structures revealed extensive systems of lee waves generated by west-to-east flow over irregular terrain. Extensive cloud systems in this region resembled baroclinic wave cyclones. Clouds were also observed over several of the large calderas; these clouds are believed to contain water ice. Several localized dust storms were seen after the global dust storm cleared. These dust clouds appeared to be intensely convective. The convective nature of these storms and the stirring of large dust particles to great heights can be explained by vertical velocities generated by the absorption of solar radiation by the dusty atmosphere.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0019-1035(72)90006-1","issn":"00191035","usgsCitation":"Leovy, C., Briggs, G., Young, A., Smith, B., Pollack, J.B., Shipley, E., and Wildey, R., 1972, The martian atmosphere: Mariner 9 television experiment progress report: Icarus, v. 17, no. 2, p. 373-393, https://doi.org/10.1016/0019-1035(72)90006-1.","productDescription":"21 p.","startPage":"373","endPage":"393","numberOfPages":"21","costCenters":[],"links":[{"id":218992,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505badbde4b08c986b323dc0","contributors":{"authors":[{"text":"Leovy, C.B.","contributorId":95609,"corporation":false,"usgs":true,"family":"Leovy","given":"C.B.","email":"","affiliations":[],"preferred":false,"id":358058,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Briggs, G.A.","contributorId":34242,"corporation":false,"usgs":true,"family":"Briggs","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":358056,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Young, A.T.","contributorId":17757,"corporation":false,"usgs":true,"family":"Young","given":"A.T.","email":"","affiliations":[],"preferred":false,"id":358055,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, B.A.","contributorId":17616,"corporation":false,"usgs":true,"family":"Smith","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":358054,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pollack, James B.","contributorId":12616,"corporation":false,"usgs":true,"family":"Pollack","given":"James","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":358053,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Shipley, E.N.","contributorId":66407,"corporation":false,"usgs":true,"family":"Shipley","given":"E.N.","email":"","affiliations":[],"preferred":false,"id":358057,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Wildey, R.L.","contributorId":9700,"corporation":false,"usgs":true,"family":"Wildey","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":358052,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70010144,"text":"70010144 - 1972 - Mass spectrometric analysis of organic compounds, water and volatile constituents in the atmosphere and surface of Mars: The Viking Mars Lander","interactions":[],"lastModifiedDate":"2017-05-03T16:07:05","indexId":"70010144","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Mass spectrometric analysis of organic compounds, water and volatile constituents in the atmosphere and surface of Mars: The Viking Mars Lander","docAbstract":"<p>An experiment centering around a mass spectrometer is described, which is aimed at the identification of organic substances present in the top 10 cm of the surface of Mars and an analysis of the atmosphere for major and minor constituents as well as isotopic abundances. In addition, an indication of the abundance of water in the surface and some information concerning the mineralogy can be obtained by monitoring the gases produced upon heating the soil sample.</p><p>The organic material will simply be expelled by heating to 150°, 300°, and 500° into the carrier gas stream of a gas chromatograph interfaced to the mass spectrometer or by slowly heating the sample in direct communication with the spectrometer. It is planned to analyze a total of up to nine soil samples in order to study diurnal and seasonal variations. The system is designed to give useful data even for minor constituents if the total of organics should be as low as 5ppm. The spectrometer covers the mass range of 12–200 with adequate resolution.</p><p>The results of these experiments, which are deliberately designed to cover a wide spectrum of possibilities independent of terrestrial models, are expected to produce a good picture of the planet's organic chemistry and its possible biological significance as well as allow conclusions regarding the history of the planet's atmosphere.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0019-1035(72)90140-6","issn":"00191035","usgsCitation":"Anderson, D.M., Biemann, K., Orgel, L.E., Oro, J., Owen, T., Shulman, G.P., Toulmin, P., and Urey, H.C., 1972, Mass spectrometric analysis of organic compounds, water and volatile constituents in the atmosphere and surface of Mars: The Viking Mars Lander: Icarus, v. 16, no. 1, p. 111-138, https://doi.org/10.1016/0019-1035(72)90140-6.","startPage":"111","endPage":"138","numberOfPages":"28","costCenters":[],"links":[{"id":219288,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5255e4b0c8380cd6c328","contributors":{"authors":[{"text":"Anderson, Duwayne M.","contributorId":191734,"corporation":false,"usgs":false,"family":"Anderson","given":"Duwayne","email":"","middleInitial":"M.","affiliations":[{"id":33087,"text":"Cold Regions Research and Engineering Laboratory","active":true,"usgs":false}],"preferred":false,"id":358109,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Biemann, K.","contributorId":76065,"corporation":false,"usgs":true,"family":"Biemann","given":"K.","email":"","affiliations":[],"preferred":false,"id":358112,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Orgel, Leslie E.","contributorId":50652,"corporation":false,"usgs":false,"family":"Orgel","given":"Leslie","email":"","middleInitial":"E.","affiliations":[{"id":33348,"text":"Salk Institute for Biological Studies, San Diego, CA","active":true,"usgs":false}],"preferred":false,"id":358111,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Oro, John","contributorId":21683,"corporation":false,"usgs":false,"family":"Oro","given":"John","email":"","affiliations":[{"id":33349,"text":"Department of Biophysical Science, University of Houston","active":true,"usgs":false}],"preferred":false,"id":358108,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Owen, Tobias","contributorId":103788,"corporation":false,"usgs":false,"family":"Owen","given":"Tobias","affiliations":[],"preferred":false,"id":358114,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Shulman, Garson P.","contributorId":16155,"corporation":false,"usgs":false,"family":"Shulman","given":"Garson","email":"","middleInitial":"P.","affiliations":[{"id":7023,"text":"Jet Propulsion Laboratory, California Institute of Technology","active":true,"usgs":false}],"preferred":false,"id":358107,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Toulmin, Priestley III","contributorId":8522,"corporation":false,"usgs":false,"family":"Toulmin","given":"Priestley","suffix":"III","email":"","affiliations":[{"id":12805,"text":"Univ. of California at San Diego","active":true,"usgs":false}],"preferred":false,"id":358113,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Urey, H. C.","contributorId":44284,"corporation":false,"usgs":true,"family":"Urey","given":"H.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":358110,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70010128,"text":"70010128 - 1972 - Geological framework of the south polar region of Mars","interactions":[],"lastModifiedDate":"2020-12-23T01:26:10.222017","indexId":"70010128","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Geological framework of the south polar region of Mars","docAbstract":"<p>The first 4 months of Mariner 9 photography of the south polar region are discussed. Three major geological units have been recognized, separated by erosional unconformities. From oldest to youngest they are: cratered terrain, pitted plains, and laminated terrain. The latter unit is unique in occurrence to the polar region, volatiles are probably involved in its origin, and may still be present within the laminated terrain as layered ice.</p><p>The residual south polar cap has been observed to survive the disappearance of the thin annual CO<sub>2</sub><span>&nbsp;</span>frost deposit and to last virtually unchanged in outline through the southern summer. That exposed deposit is inferred to be composed of water-ice. The residual cap appears to lie at the apex of an unusual quasi-circular structure composed of laminated terrain; a similar structure also appears to exist near the north pole.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0019-1035(72)90004-8","issn":"00191035","usgsCitation":"Murray, B.C., Soderblom, L., Cutts, J., Sharp, R., Milton, D., and Leighton, R., 1972, Geological framework of the south polar region of Mars: Icarus, v. 17, no. 2, p. 328-345, https://doi.org/10.1016/0019-1035(72)90004-8.","productDescription":"18 p.","startPage":"328","endPage":"345","numberOfPages":"18","costCenters":[],"links":[{"id":218990,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2264e4b0c8380cd56fdb","contributors":{"authors":[{"text":"Murray, B. C.","contributorId":49870,"corporation":false,"usgs":false,"family":"Murray","given":"B.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":358040,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Soderblom, L.A. 0000-0002-0917-853X","orcid":"https://orcid.org/0000-0002-0917-853X","contributorId":6139,"corporation":false,"usgs":true,"family":"Soderblom","given":"L.A.","affiliations":[],"preferred":false,"id":358037,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cutts, J.A.","contributorId":56790,"corporation":false,"usgs":true,"family":"Cutts","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":358041,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sharp, R.P.","contributorId":6993,"corporation":false,"usgs":true,"family":"Sharp","given":"R.P.","email":"","affiliations":[],"preferred":false,"id":358038,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Milton, D.J.","contributorId":44121,"corporation":false,"usgs":true,"family":"Milton","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":358039,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Leighton, R.B.","contributorId":73745,"corporation":false,"usgs":true,"family":"Leighton","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":358042,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70171433,"text":"70171433 - 1972 - The relation of periphytic and planktonic algal growth in an estuary to hydrographic factors","interactions":[],"lastModifiedDate":"2016-05-31T12:53:57","indexId":"70171433","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2620,"text":"Limnology and Oceanography","active":true,"publicationSubtype":{"id":10}},"title":"The relation of periphytic and planktonic algal growth in an estuary to hydrographic factors","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"ASLO","doi":"10.4319/lo.1972.17.5.0731","usgsCitation":"Welch, E.B., Emery, R.M., Matsuda, R.I., and Dawson, W.A., 1972, The relation of periphytic and planktonic algal growth in an estuary to hydrographic factors: Limnology and Oceanography, v. 17, no. 5, p. 731-737, https://doi.org/10.4319/lo.1972.17.5.0731.","productDescription":"7 p.","startPage":"731","endPage":"737","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":321920,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"5","noUsgsAuthors":false,"publicationDate":"2003-12-22","publicationStatus":"PW","scienceBaseUri":"574eb5dde4b0ee97d51a8413","contributors":{"authors":[{"text":"Welch, Eugene Brummer","contributorId":48947,"corporation":false,"usgs":true,"family":"Welch","given":"Eugene","email":"","middleInitial":"Brummer","affiliations":[],"preferred":false,"id":630966,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Emery, Richard M.","contributorId":169735,"corporation":false,"usgs":false,"family":"Emery","given":"Richard","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":630967,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Matsuda, Robert I.","contributorId":169736,"corporation":false,"usgs":false,"family":"Matsuda","given":"Robert","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":630968,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dawson, William A.","contributorId":46496,"corporation":false,"usgs":true,"family":"Dawson","given":"William","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":630969,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1000479,"text":"1000479 - 1972 - Life history and production of walleyes of the 1959 year-class in western Lake Erie, 1959-62","interactions":[],"lastModifiedDate":"2016-03-14T12:45:48","indexId":"1000479","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Life history and production of walleyes of the 1959 year-class in western Lake Erie, 1959-62","docAbstract":"<p>Because of the near collapse of the fishery for walleyes (Stizostedion vitreum vitreum) in Lake Erie in the late 1950's, walleyes of the 1959 year-class were studied to gain a better understanding of the life history of the species and the dynamics of the population. In the summer of 1959 most walleyes of the year-class were in water 10 to 20 feet deep along the south and west shores of the western basin. By fall they averaged about 10 inches long and were rather widely distributed throughout the basin. By September 1960 most had reached legal length (then 13 inches in Ohio), and in October they made up nearly the entire commercial walleye production and made the highest monthly contribution during the life of the year-class. Walleyes of the 1959 year-class were cropped intensively and remained in the fishery for only a relatively short time. Estimated Ohio trap net production of the year-class was 261,000 fish in 1960, 168,000 in 1961, and 21,000 in 1962. Few fish survived beyond the spring of 1962. About 97% of the females of the year-class were caught before they had spawned once.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1972)101<655:LHAPOW>2.0.CO;2","usgsCitation":"Parsons, J.W., 1972, Life history and production of walleyes of the 1959 year-class in western Lake Erie, 1959-62: Transactions of the American Fisheries Society, v. 101, no. 4, p. 655-661, https://doi.org/10.1577/1548-8659(1972)101<655:LHAPOW>2.0.CO;2.","productDescription":"7 p.","startPage":"655","endPage":"661","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":132755,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"101","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a5478","contributors":{"authors":[{"text":"Parsons, John W.","contributorId":21899,"corporation":false,"usgs":true,"family":"Parsons","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":308602,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000472,"text":"1000472 - 1972 - Lake Michigan: effects of exploitation, introductions, and eutrophication on the salmonid community","interactions":[],"lastModifiedDate":"2016-03-14T13:17:13","indexId":"1000472","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Lake Michigan: effects of exploitation, introductions, and eutrophication on the salmonid community","docAbstract":"<p>Lake Michigan surface area is 22,400 square miles and its main depth is 276 ft. Its fauna is generally typical of North American oligotrophic lakes. The original fish populations included 10 coregonines and one salmonine. The lake whitefish, the lake herring, and the lake trout were most abundant. Man's activities have caused great changes in the lake in the past 120 years. Although changes in water chemistry and in the lower biota have been generally modest (except locally), those in salmonid communities have been vast. Exploitation, exotic fish species (especially the sea lamprey and alewife), and accelerated eutrophication and other pollution, all have played a role in bringing about the modifications (mostly marked declines in abundance) in salmonid communities. Commercial exploitation was largely responsible for the changes in the salmonid communities before the invasion of the lamprey (1936), although eutrophication and other pollution, and alterations of spawning streams, also were important. The lamprey and alewife (first reported in 1949), however, have exerted a greater impact than the other factors in recent decades.</p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/f72-132","usgsCitation":"Wells, L., and McLain, A.L., 1972, Lake Michigan: effects of exploitation, introductions, and eutrophication on the salmonid community: Journal of the Fisheries Research Board of Canada, v. 29, no. 6, p. 889-898, https://doi.org/10.1139/f72-132.","productDescription":"10 p.","startPage":"889","endPage":"898","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133276,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b169c","contributors":{"authors":[{"text":"Wells, LaRue","contributorId":75476,"corporation":false,"usgs":true,"family":"Wells","given":"LaRue","email":"","affiliations":[],"preferred":false,"id":308596,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McLain, Alberton L.","contributorId":15561,"corporation":false,"usgs":true,"family":"McLain","given":"Alberton","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":308595,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1000320,"text":"1000320 - 1972 - Accumulation of dieldrin in an alga (<i>Scenedesmus obliquus</i>), <i>Daphnia magna</i>, and the guppy (<i>Poecilia reticulata</i>)","interactions":[],"lastModifiedDate":"2013-01-29T10:52:45","indexId":"1000320","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Accumulation of dieldrin in an alga (<i>Scenedesmus obliquus</i>), <i>Daphnia magna</i>, and the guppy (<i>Poecilia reticulata</i>)","docAbstract":"<i>Scenedesmus obliquus</i>, <i>Daphnia magna</i>, and <i>Poecilia reticulata</i> accumulated dieldrin directly from water; average concentration factors (concentration in organism, dry weight, divided by concentration in water) were 1282 for the alga, 13,954 for<i> D. magna</i>, and 49,307 (estimated) for the guppy. The amount accumulated by each species at equilibrium (after about 1.5, 3-4, and 18 days, respectively) was directly proportional to the concentration of dieldrin in the water. <i>Daphnia magna</i> and guppies accumulated more dieldrin from water than from food that had been exposed to similar concentrations in water. When guppies were fed equal daily rations of <i>D. magna</i> containing different concentrations of insecticide, the amounts of dieldrin accumulated by the fish were directly proportional to the concentration in <i>D. magna</i>; when two lots of guppies were fed different quantities of <i>D. magna</i> (10 and 20 organisms per day) containing identical concentrations of dieldrin, however, the amounts accumulated did not differ substantially.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the Fisheries Research Board of Canada","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1139/f72-219","collaboration":"Out-of-print","usgsCitation":"Reinert, R.E., 1972, Accumulation of dieldrin in an alga (<i>Scenedesmus obliquus</i>), <i>Daphnia magna</i>, and the guppy (<i>Poecilia reticulata</i>): Journal of the Fisheries Research Board of Canada, v. 29, no. 10, p. 1413-1418, https://doi.org/10.1139/f72-219.","productDescription":"p. 1413-1418","startPage":"1413","endPage":"1418","numberOfPages":"5","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":266679,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1139/f72-219"},{"id":132890,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a35d1","contributors":{"authors":[{"text":"Reinert, Robert E.","contributorId":101214,"corporation":false,"usgs":true,"family":"Reinert","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":308383,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000385,"text":"1000385 - 1972 - Factors of ecologic succession in oligotrophic fish communities of the Laurentian Great Lakes","interactions":[],"lastModifiedDate":"2016-03-14T13:12:54","indexId":"1000385","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Factors of ecologic succession in oligotrophic fish communities of the Laurentian Great Lakes","docAbstract":"<p><span>Oligotrophic fish communities of the Great Lakes have undergone successive disruptions since the mid-1800s. Major contributing factors have been intensive selective fisheries, extreme modification of the drainage, invasion of marine species, and progressive physical&ndash;chemical changes of the lake environments. Lake Ontario was the first to be affected as its basin was settled and industrialized earliest, and it was the first to be connected by canals to the mid-Atlantic where the alewife (</span><i>Alosa pseudoharengus</i><span>) and sea lamprey (</span><i>Petromyzon marinus</i><span>) which ultimately became established in the Great Lakes were abundant. Oligotrophic fish communities were successively disrupted in Lakes Erie, Huron, Michigan, and Superior as the affects of population growth, industrialization, and marine invaders spread upward in the Laurentian drainage.The degree and sequence of response of families offish and species within families differed for each factor, but the sequence of change among families and species has been the same in response to each factor as it affected various lakes at different times. The ultimate result of the disruption of fish communities has been a reduction of productivity of oligotrophic species that ranges from extreme in Lake Ontario to moderate in Lake Superior, and which has reached a state of instability and rapid change in the upper three Great Lakes by the rnid-1900s similar to the situation in Lake Ontario in the mid-1800s. Since oligotrophic species (primarily salmonines, coregonines, and deepwater cottids) are the only kinds of fish that fully occupied the entire volume of the deepwater Great Lakes (Ontario, Huron, Michigan, and Superior), the fish biomass of these lakes has been reduced as various species declined or disappeared. In Lake Erie, which is shallow, and in the shallow bays of the deep lakes, oligotrophic species were replaced by mesotrophic species, primarily percids, which have successively increased and declined. All oligotrophic species are greatly reduced or extinct in lakes Ontario and Erie, and are in various stages of decline in lakes Huron, Michigan, and Superior, from greatest to least, respectively. The percids appear to be near the end of their sequence of succession in lakes Erie, Ontario, and Huron (primarily Saginaw Bay) where only the yellow perch (</span><i>Perca flavescens</i><span>) remains abundant. The yellow perch appears to be on the brink of decline in Lake Erie, which has been more severely influenced by water quality change than the other lakes.</span></p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/f72-117","usgsCitation":"Smith, S.H., 1972, Factors of ecologic succession in oligotrophic fish communities of the Laurentian Great Lakes: Journal of the Fisheries Research Board of Canada, v. 29, no. 6, p. 717-730, https://doi.org/10.1139/f72-117.","productDescription":"14 p.","startPage":"717","endPage":"730","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133372,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f7a50","contributors":{"authors":[{"text":"Smith, Stanford H.","contributorId":86711,"corporation":false,"usgs":true,"family":"Smith","given":"Stanford","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308489,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000350,"text":"1000350 - 1972 - The future of salmonid communities in the Laurentian Great Lakes","interactions":[],"lastModifiedDate":"2016-03-14T13:25:25","indexId":"1000350","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"The future of salmonid communities in the Laurentian Great Lakes","docAbstract":"<p><span>The effects of human population growth, industrialization, and the introduction of marine fishes have reduced the suitability of each of the Great Lakes for oligotrophic fish communities. The ultimate consequence has been a reduction of fishery productivity that has ranged from extreme in Lake Ontario to moderate in Lake Superior. If measures are not taken to alleviate the adverse effects of marine invaders and trends in environmental quality, a major reduction in fishery productivity can eventually be expected throughout the Great Lakes.Prospects for the next century will be improved if the lakes can be intensively managed. More stringent control of the sea lamprey (</span><i>Petromyzon marinus</i><span>), and subsequent reduction of the alewife (</span><i>Alosa pseudoharengus</i><span>), by the reestablishment of populations of large piscivores, should permit the recovery of some of the previous predator and prey species, or the development of populations of new species that are more compatible with a reduced number of lampreys. Even if marine species can be reduced greatly, the full restoration of the former fishery productivity remains uncertain and will require a high degree of coordination among all management and research agencies that have responsibilities on the Great Lakes.Unfavorable trends toward progressive degradation of water quality pose the greatest threat to restoration of the fishery resources of the Great Lakes. Where changes in water quality have been the greatest, oligotrophic species have become scarce or absent, and in the deepwater regions no other species have reoccupied the vacated niches.</span></p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/f72-138","usgsCitation":"Smith, S.H., 1972, The future of salmonid communities in the Laurentian Great Lakes: Journal of the Fisheries Research Board of Canada, v. 29, no. 6, p. 951-957, https://doi.org/10.1139/f72-138.","productDescription":"7 p.","startPage":"951","endPage":"957","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133478,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65da4c","contributors":{"authors":[{"text":"Smith, Stanford H.","contributorId":86711,"corporation":false,"usgs":true,"family":"Smith","given":"Stanford","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308437,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1003231,"text":"1003231 - 1972 - Exposure times necessary for antimycin and rotenone to eliminate certain freshwater fish","interactions":[],"lastModifiedDate":"2025-03-04T16:50:27.163819","indexId":"1003231","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Exposure times necessary for antimycin and rotenone to eliminate certain freshwater fish","docAbstract":"<p><span>In laboratory flowing-water troughs exposure required to induce 100% mortality, regardless of time to death for antimycin and rotenone against selected freshwater fish species was determined. Carp and white suckers required shorter exposures to antimycin (6 hr) than to rotenone (18–24 hr) at field-use concentrations of 5 and 50 ppb respectively. Bullheads were killed by 3–10 hr exposure to 100–250 ppb rotenone at 17 C or higher. However, the long exposure time necessary in colder water (25 hr at 100 ppb in 12 C water) made elimination of bullheads with rotenone difficult in cold seasons. Exposure time was influenced more by water temperature than by the toxicant concentration. The effects of rotenone were often reversible even after fish had been on their sides in the toxicant solution for 4–5 hr but irreversible for antimycin after fish showed the first signs of distress.</span></p>","language":"English","publisher":"Canadian Science Publishing","doi":"10.1139/f72-032","usgsCitation":"Gilderhus, P., 1972, Exposure times necessary for antimycin and rotenone to eliminate certain freshwater fish: Journal of the Fisheries Research Board of Canada, v. 29, no. 2, p. 199-202, https://doi.org/10.1139/f72-032.","productDescription":"4 p.","startPage":"199","endPage":"202","numberOfPages":"4","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":131372,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8b69","contributors":{"authors":[{"text":"Gilderhus, P.A.","contributorId":60156,"corporation":false,"usgs":true,"family":"Gilderhus","given":"P.A.","affiliations":[],"preferred":false,"id":313009,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70176051,"text":"70176051 - 1972 - Chemical and bacteriological quality of water at selected sites in the San Antonio area, Texas, August 1968-April 1972","interactions":[],"lastModifiedDate":"2016-08-24T11:29:10","indexId":"70176051","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"title":"Chemical and bacteriological quality of water at selected sites in the San Antonio area, Texas, August 1968-April 1972","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Reeves, R., Rawson, J., and Blakey, J., 1972, Chemical and bacteriological quality of water at selected sites in the San Antonio area, Texas, August 1968-April 1972, 69 p.","productDescription":"69 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":327787,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57c6aecfe4b0f2f0cebe43f0","contributors":{"authors":[{"text":"Reeves, R.D.","contributorId":95043,"corporation":false,"usgs":true,"family":"Reeves","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":646940,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rawson, Jack","contributorId":18345,"corporation":false,"usgs":true,"family":"Rawson","given":"Jack","affiliations":[],"preferred":false,"id":646941,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blakey, J.F.","contributorId":23969,"corporation":false,"usgs":true,"family":"Blakey","given":"J.F.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":646942,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70176063,"text":"70176063 - 1972 - Annual compilation and analysis of hydrologic data for urban studies in the Austin, Texas, metropolitan area, 1970","interactions":[],"lastModifiedDate":"2016-08-24T12:57:10","indexId":"70176063","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Annual compilation and analysis of hydrologic data for urban studies in the Austin, Texas, metropolitan area, 1970","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70176063","usgsCitation":"VanZandt, J.K., 1972, Annual compilation and analysis of hydrologic data for urban studies in the Austin, Texas, metropolitan area, 1970: Open-File Report, 70 p., https://doi.org/10.3133/70176063.","productDescription":"70 p.","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":327802,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57c6ae8ae4b0f2f0cebe3fa8","contributors":{"authors":[{"text":"VanZandt, J. K.","contributorId":173701,"corporation":false,"usgs":false,"family":"VanZandt","given":"J.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":646972,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}