{"pageNumber":"2381","pageRowStart":"59500","pageSize":"25","recordCount":68846,"records":[{"id":70232667,"text":"70232667 - 1975 - Recurrent geothermally induced debris avalanches on Boulder Glacier, Mount Baker, Washington","interactions":[],"lastModifiedDate":"2022-07-11T16:07:50.213548","indexId":"70232667","displayToPublicDate":"1975-01-01T11:00:45","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Recurrent geothermally induced debris avalanches on Boulder Glacier, Mount Baker, Washington","docAbstract":"<p>Avalanches of snow, firn and hydrothermally altered rock and mud have been released six times since 1958 from Sherman Peak, part of the crater rim south of the main summit of Mount Baker, Wash. The avalanches traveled nearly identical paths 2.0-2.6 km down Boulder Glacier on the east slope of the volcano. Debris from at least one past avalanche can be seen as a thin bed of acidic mud in the glacier terminus. Fumaroles. thermal springs, and areas of warm ground, some of which are subglacial, are concentrated in the crater and were mapped by aerial infrared thermography. The outgoing radiant flux per unit area from a cluster of infrared anomalies within 50-150 m of the avalanche source was estimated to be 319 W m<sup>-2</sup> (7,620 <i><span>μ</span></i>cal cm<sup>-2</sup>s<sup>-1</sup> ) in November 1972, which is sufficient to account for observed ice perforations. In addition vapor emission, not apparent in thermography, was observed along the source margin after the avalanche of August 1973. The principal conditions that produce the avalanches are considered to be the large accumulation of snow and firn on top of hydrothermally altered clay-rich ground at Sherman Peak and the saturation near the ground-firn interface by melt water produced both by summer snow ablation and by geothermal emission. The periodic avalanches have a potential for impounding water in the crater in addition to ponded water already known to occur. Sudden release of impounded water could present a danger to the Boulder Creek valley below. </p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Frank, D., Post, A., and Friedman, J., 1975, Recurrent geothermally induced debris avalanches on Boulder Glacier, Mount Baker, Washington: Journal of Research of the U.S. Geological Survey, v. 3, no. 1, p. 77-87.","productDescription":"11 p.","startPage":"77","endPage":"87","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":403398,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403397,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1975/vol3issue1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","otherGeospatial":"Boulder Glacier, Mount Baker","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.91116333007811,\n              48.73037931457286\n            ],\n            [\n              -121.75048828124999,\n              48.73037931457286\n            ],\n            [\n              -121.75048828124999,\n              48.828565527993234\n            ],\n            [\n              -121.91116333007811,\n              48.828565527993234\n            ],\n            [\n              -121.91116333007811,\n              48.73037931457286\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"3","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Frank, David dfrank@usgs.gov","contributorId":170058,"corporation":false,"usgs":true,"family":"Frank","given":"David","email":"dfrank@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":846214,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Post, Austin","contributorId":90709,"corporation":false,"usgs":true,"family":"Post","given":"Austin","affiliations":[],"preferred":false,"id":846215,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Friedman, Jules D.","contributorId":76757,"corporation":false,"usgs":true,"family":"Friedman","given":"Jules D.","affiliations":[],"preferred":false,"id":846216,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":25290,"text":"25290 - 1975 - Basic ground-water data for the Moscow Basin, Idaho","interactions":[],"lastModifiedDate":"2025-03-17T13:47:30.991091","indexId":"25290","displayToPublicDate":"1975-01-01T10:59:44","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Basic ground-water data for the Moscow Basin, Idaho","docAbstract":"<p>The Moscow basin encompasses an area of 65 square miles (170 square kilometres) in Latah County and borders the Idaho Washington State line (fig. 1). The basin is along the eastern edge of the \"Palouse Country\" where the rolling Palouse hills merge with the low mountains of northern Idaho. It is drained by the South Fork Palouse River, Paradise Creek, and Missouri Flat Creek, and their headwater tributaries.</p><p>All water supplies for the basin are derived from wells and springs. Virtually all large-capacity wells are owned by the City of Moscow and the University of Idaho. These wells are open to the basalt of the Columbia River Group and the interbedded sands in the Latah Formation (Stevens, 1960, p. 335; Jones and Ross, 1972, p. 12-13, fig. 4). Many domestic and a few commercial wells are also open to these same formations. Most of the City and University wells tap thick sections of these water-bearing formations. However, only about 25 percent of the total basin area is underlain by basalt. The approximate subsurface extent of the area underlain by basalt, as determined by well logs and geophysical data, is shown in figure 2.</p><p>The purpose of this report is to present basic geologic and hydrologic data that are available in the basin. Included are a table of well records, well logs, a table of annual ground-water withdrawals, water levels in observation wells, a contour map showing the approximate elevation of the water-level in the upper series of basalt flows and interbedded sediments in the southern part of the area (fig. 2), and a bibliography of the more important reports pertaining to ground water in the area. More than 90 percent of the wells tapping basalt were visited, but only a representative number of wells tapping other rocks were visited. Data that may have become available after December 1972 are not given except for water-level measurements made in March 1973.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/25290","issn":"0364-7064","collaboration":"Prepared in cooperation with the Idaho Department of Water Resources.","usgsCitation":"Crosthwaite, E.G., 1975, Basic ground-water data for the Moscow Basin, Idaho, Report: 96 p.; 1 Plate: 14.73 x 19.32 inches, https://doi.org/10.3133/25290.","productDescription":"Report: 96 p.; 1 Plate: 14.73 x 19.32 inches","numberOfPages":"96","costCenters":[],"links":[{"id":483444,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/25290/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":483443,"rank":2,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/25290/figure-2.pdf","text":"Figure 2","linkFileType":{"id":1,"text":"pdf"}},{"id":289621,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/25290/report-thumb.jpg"}],"country":"United States","state":"Idaho","city":"Moscow","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.039698,46.710912 ], [ -117.039698,46.758882 ], [ -116.962068,46.758882 ], [ -116.962068,46.710912 ], [ -117.039698,46.710912 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53be6462e4b0527d5d4097a3","contributors":{"authors":[{"text":"Crosthwaite, Emerson Gerald","contributorId":63315,"corporation":false,"usgs":true,"family":"Crosthwaite","given":"Emerson","email":"","middleInitial":"Gerald","affiliations":[],"preferred":false,"id":193372,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70232665,"text":"70232665 - 1975 - A proposed glacial history of the Henrys Lake Basin, Idaho","interactions":[],"lastModifiedDate":"2022-07-11T15:58:17.432208","indexId":"70232665","displayToPublicDate":"1975-01-01T10:41:01","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"A proposed glacial history of the Henrys Lake Basin, Idaho","docAbstract":"<p>Deposits of several glaciations from oldest to youngest, pre-Bull Lake, Bull Lake, and Pinedale are in and near the Henrys Lake basin, a northwest-trending hourglass-shaped trough in southeastern Idaho. Glacial deposits of pre-Bull Lake age are represented by till remnants confined mostly to the higher levels of the surrounding mountains. The extent of Bull Lake ice into the basin is uncertain. Glacial deposits and ice-marginal features suggest that a lobe of Bull Lake ice the Henrys Lake ice lobe moved into the basin and advanced as far north as the north edge of Henrys Lake. After this lobe melted back far enough to expose the north end of the basin, melt waters, chiefly from alpine glaciers in Targhee Creek and its tributaries, formed the broad low Howard Creek fan at the mouth of the valley of Howard Creek. Shortly thereafter, a complex of channels was cut into the fan by periodic melt-water floods which flowed westward through Targhee Pass during the waste of another Bull Lake ice lobe which lay in the West Yellowstone Basin. Melt waters from various sources ponded to form a shallow lake in front of the wasting Henrys Lake ice lobe. Waters from this lake drained southwestward around the southwest flank of the lobe via an ice-marginal channel. Upon total melt of the ice lobe, the lake was drained, the ice-marginal channel was abandoned, and the waters resumed their pre-ice course to the southeast. During the interglaciation, prior to the onset of the Pinedale Glaciation, northward-flowing streams deposited a veneer of obsidian sand and gravel along the south edge of the basin. In Pinedale time, alpine glaciers formed in the high mountain valleys near the basin, but none advanced into the basin.</p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Witkind, I.J., 1975, A proposed glacial history of the Henrys Lake Basin, Idaho: Journal of Research of the U.S. Geological Survey, v. 3, no. 1, p. 67-76.","productDescription":"10 p.","startPage":"67","endPage":"76","costCenters":[],"links":[{"id":403396,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403393,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1975/vol3issue1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","otherGeospatial":"Henry Lake Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.53869628906249,\n              44.41269287945535\n            ],\n            [\n              -111.14387512207031,\n              44.41269287945535\n            ],\n            [\n              -111.14387512207031,\n              44.722344439440775\n            ],\n            [\n              -111.53869628906249,\n              44.722344439440775\n            ],\n            [\n              -111.53869628906249,\n              44.41269287945535\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"3","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Witkind, Irving J.","contributorId":14469,"corporation":false,"usgs":true,"family":"Witkind","given":"Irving","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":846212,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":36955,"text":"36955 - 1975 - Wildlife and oil shale: a problem analysis and research program: volume 2, appendix and bibliography","interactions":[],"lastModifiedDate":"2014-07-29T10:15:54","indexId":"36955","displayToPublicDate":"1975-01-01T10:07:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"76/01.2","title":"Wildlife and oil shale: a problem analysis and research program: volume 2, appendix and bibliography","docAbstract":"<p>This appendix is designed to apply to the program of studies recommended in the problem analysis and research program Volume I.</p>\n<br>\n<p>It has two purposes:</p>\n<br>\n<p>(1) to provide reference that may be used in the preparation of requests for proposals or for studies, and</p>\n<br>\n<p>(2) to suggest a core group of references for a reference library for research.</p>\n<br>\n<p>The references that follow are listed taxonomically as follows:</p>\n<br>\n<p>A. Aquatic Ecosystems</p>\n<br>\n<p>B. Water Quality</p>\n<br>\n<p>C. Terrestrial Ecosystems</p>\n<br>\n<p>D. Industrial Impacts on Wildlife</p>\n<br>\n<p>E. Reptiles and Amphibians</p>\n<br>\n<p>F. Blood-sucking Arthropods and Disease Vectors</p>\n<br>\n<p>This bibliography is not integrated because it was believed that it would be more useful with the sources separate. It also does not attempt to cover the entire field. It is, however, a listing that will be most useful in the description of the region and its environmental processes.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"Thorne Ecological Institute","usgsCitation":"Burke, H., 1975, Wildlife and oil shale: a problem analysis and research program: volume 2, appendix and bibliography: FWS/OBS 76/01.2, 131 p.","productDescription":"131 p.","costCenters":[],"links":[{"id":291261,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffc0a7e4b0824b2d172871","contributors":{"authors":[{"text":"Burke, Hubert D.","contributorId":63328,"corporation":false,"usgs":true,"family":"Burke","given":"Hubert D.","affiliations":[],"preferred":false,"id":217233,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2000039,"text":"2000039 - 1975 - Changes in the lake trout population of southern Lake Superior in relation to the fishery, the sea lamprey, and stocking, 1950-70","interactions":[],"lastModifiedDate":"2012-02-02T00:14:57","indexId":"2000039","displayToPublicDate":"1975-01-01T01:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":222,"text":"Technical Report","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"28","title":"Changes in the lake trout population of southern Lake Superior in relation to the fishery, the sea lamprey, and stocking, 1950-70","docAbstract":"Commercial catch and effort statistics for 1929-70, samples of commercial catches in 1959-62, and records of examinations of all lake trout (Salvelinus namaycush) taken commercially in inshore waters of Michigan and Wisconsin in 1962-70 were the basis for descriptions of changes in the population in 1929-70.\nAbundance fluctuated cyclically and gradually downward in 1929-49, whereas fishing intensity tended to increase during the same period. In 1950-52, a change from cotton to nylon twine in gillnets raised effective fishing effort to 305% of the 1929-43 average in Michigan waters and to 228% in Wisconsin waters; production held near average. Abundance fell to 18% of average in Michigan in 1953-61 and to 25% of average in Wisconsin in 1956-61; in the same periods, production fell to 11% of average in Michigan and to 19% in Wisconsin. In 1962-70 abundance rose to 160% in Michigan and 246% in Wisconsin while production and fishing intensity were held low (3-14%) by regulation.\nChanges in abundance of lake trout were attributable to a sequence of developments in successive series of years; intensive fishing in the early 1950's; severe sea lamprey predation in the late 1950's; an 85% reduction in abundance of sea lampreys in mid 1961; and the combination of sea lamprey control, intensive stocking of yearling lake trout, and restrictions on fishing in 1962-70. A decline in average size of lake trout and the near elimination of spawning stocks in 1953-61 curtailed recruitment of native lake trout in the mid 1960's. Stocking of fin-clipped lake trout replaced natural reproduction in the early 1960's. In 1965-70, the lake trout population was composed mainly of hatchery-reared fish. Natural reproduction was reestablished on one major spawning shoal in Wisconsin in 1965, but in 1970 only 10% of the legal (17-inch and longer) and 17% of the undersize lake trout in Wisconsin were native fish.\nReduction of sea lamprey abundance resulted in an immediate increase in survival and abundance of lake trout, especially of the larger sizes. As abundance of lake trout progressively increased in 1962-70, survival of the smaller legal-size lake trout increased, probably due to reduction of the predator-prey ratio and an increase in availability of larger lake trout preferred by sea lampreys. Abundance of spawning-size lake trout was limited by high natural mortality in 1965-70. Circumstantial evidence suggested that sea lamprey predation contributed a major part of the high natural mortality.","language":"English","publisher":"Great Lakes Fishery Commission","collaboration":"Out-of-print","usgsCitation":"Pycha, R.L., and King, G.R., 1975, Changes in the lake trout population of southern Lake Superior in relation to the fishery, the sea lamprey, and stocking, 1950-70: Technical Report 28, 34 p.","productDescription":"34 p.","startPage":"0","endPage":"34","numberOfPages":"34","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198783,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":92053,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.glfc.org/pubs/TechReports/Tr28.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3d8e","contributors":{"authors":[{"text":"Pycha, Richard L.","contributorId":17175,"corporation":false,"usgs":true,"family":"Pycha","given":"Richard","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":324970,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, George R.","contributorId":74721,"corporation":false,"usgs":true,"family":"King","given":"George","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":324971,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1001684,"text":"1001684 - 1975 - Effects of agricultural burning on nesting waterfowl","interactions":[],"lastModifiedDate":"2023-11-15T01:40:05.912255","indexId":"1001684","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1163,"text":"Canadian Field-Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Effects of agricultural burning on nesting waterfowl","docAbstract":"Agricultural burning in an intensively farmed region within Manitoba's pothole district is shown to affect the nesting activities of ground-nesting ducks. All species, except Blue-winged Teal (Anas discors), preferred unburned nest cover, although success was higher in burned areas, where predators may have exerted less influence. Attitudes of farmers, burning chronology, and nest destruction by fires are also reported.","language":"English","publisher":"Ottawa Field-Naturalists' Club","usgsCitation":"Fritzell, E., 1975, Effects of agricultural burning on nesting waterfowl: Canadian Field-Naturalist, v. 89, no. 1, p. 21-27.","productDescription":"7 p.","startPage":"21","endPage":"27","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":422591,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.biodiversitylibrary.org/part/344797"},{"id":130304,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"89","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db6245c5","contributors":{"authors":[{"text":"Fritzell, E.K.","contributorId":35685,"corporation":false,"usgs":true,"family":"Fritzell","given":"E.K.","email":"","affiliations":[],"preferred":false,"id":311511,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175639,"text":"70175639 - 1975 - Ground-water data in the Harrisburg-Halsey area, central Willamette Valley, Oregon","interactions":[],"lastModifiedDate":"2016-08-17T14:12:43","indexId":"70175639","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":115,"text":"Ground Water Report","active":false,"publicationSubtype":{"id":2}},"title":"Ground-water data in the Harrisburg-Halsey area, central Willamette Valley, Oregon","docAbstract":"<p><span class=\"EXLDetailsDisplayVal\">THE <span class=\"searchword\">HARRISBURG</span>-<span class=\"searchword\">HALSEY</span> <span class=\"searchword\">AREA</span> COVERS ABOUT 350 SQUARE MILES IN THE <span class=\"searchword\">CENTRAL</span> <span class=\"searchword\">WILLAMETTE</span> <span class=\"searchword\">VALLEY</span>, OREG., AND IS PART OF A BROAD ALLUVIAL PLAIN THAT LIES BETWEEN THE CASCADE AND COAST RANGES IN THE <span class=\"searchword\">CENTRAL</span> PART OF THE <span class=\"searchword\">WILLAMETTE</span> <span class=\"searchword\">VALLEY</span>. MOST OF THE <span class=\"searchword\">DATA</span> FOR THE 506 WELLS IN THIS REPORT WERE OBTAINED FROM WELL DRILLERS' REPORTS. CHEMICAL ANALYSES OF <span class=\"searchword\">WATER</span> FROM 36 WELLS ARE TABULATED. MOST OF THE HIGH-YIELD WELLS IN THE <span class=\"searchword\">AREA</span> PRODUCE <span class=\"searchword\">WATER</span> FROM ALLUVIAL (SAND AND GRAVEL) AQUIFERS THAT UNDERLIE THE <span class=\"searchword\">VALLEY</span> PLAIN OR THAT ARE COEXTENSIVE WITH THE PRESENT FLOOD PLAIN OF THE <span class=\"searchword\">WILLAMETTE</span> RIVER. THE <span class=\"searchword\">WATER</span> TABLE IN THE ALLUVIAL AQUIFER IS GENERALLY ONLY A FEW FEET BELOW LAND SURFACE. PUMPING LIFTS ARE RELATIVELY SMALL, AND WELLS PRODUCE MODERATE TO LARGE QUANTITIES OF GROUNDWATER OF GOOD CHEMICAL QUALITY</span>.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Frank, F.J., and Johnson, N.A., 1975, Ground-water data in the Harrisburg-Halsey area, central Willamette Valley, Oregon: Ground Water Report.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":326727,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","city":"Halsey, Harrisburg","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58ad0e4b03bcb0104bbb6","contributors":{"authors":[{"text":"Frank, F. J.","contributorId":95037,"corporation":false,"usgs":true,"family":"Frank","given":"F.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":645905,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Nyra A.","contributorId":173771,"corporation":false,"usgs":false,"family":"Johnson","given":"Nyra","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":645906,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70171427,"text":"70171427 - 1975 - Net primary productivity of periphytic algae in the intertidal zone, Duwamish River estuary, Washington","interactions":[],"lastModifiedDate":"2016-05-31T12:32:22","indexId":"70171427","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Net primary productivity of periphytic algae in the intertidal zone, Duwamish River estuary, Washington","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Tilley, L.J., and Haushild, W., 1975, Net primary productivity of periphytic algae in the intertidal zone, Duwamish River estuary, Washington: Journal of Research of the U.S. Geological Survey, v. 3, no. 3, p. 253-259.","productDescription":"7 p.","startPage":"253","endPage":"259","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":321913,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574eb5d8e4b0ee97d51a83de","contributors":{"authors":[{"text":"Tilley, L. J.","contributorId":91836,"corporation":false,"usgs":true,"family":"Tilley","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":630955,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haushild, W.L.","contributorId":48953,"corporation":false,"usgs":true,"family":"Haushild","given":"W.L.","affiliations":[],"preferred":false,"id":630956,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70171428,"text":"70171428 - 1975 - Use of productivity of periphyton to estimate water quality","interactions":[],"lastModifiedDate":"2016-05-31T12:36:36","indexId":"70171428","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2573,"text":"Journal of the Water Pollution Control Federation","active":true,"publicationSubtype":{"id":10}},"title":"Use of productivity of periphyton to estimate water quality","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Water Pollution Control Federation","usgsCitation":"Tilley, L.J., and Haushild, W., 1975, Use of productivity of periphyton to estimate water quality: Journal of the Water Pollution Control Federation, v. 47, no. 8, p. 2157-2171.","productDescription":"15 p.","startPage":"2157","endPage":"2171","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":321915,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":321914,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/25038949?seq=1#page_scan_tab_contents"}],"volume":"47","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574eb5dde4b0ee97d51a8415","contributors":{"authors":[{"text":"Tilley, L. J.","contributorId":91836,"corporation":false,"usgs":true,"family":"Tilley","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":630957,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haushild, W.L.","contributorId":48953,"corporation":false,"usgs":true,"family":"Haushild","given":"W.L.","affiliations":[],"preferred":false,"id":630958,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1000464,"text":"1000464 - 1975 - Predation by fish on walleye eggs on a spawning reef in western Lake Erie, 1969-71","interactions":[],"lastModifiedDate":"2012-02-02T00:04:32","indexId":"1000464","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2938,"text":"Ohio Journal of Science","active":true,"publicationSubtype":{"id":10}},"title":"Predation by fish on walleye eggs on a spawning reef in western Lake Erie, 1969-71","docAbstract":"Nearly 2,000 fish representing 21 species were captured with experimental gillnets on Kelleys Island Shoal during the spawning and incubation periods of walleyes (Stizostedion v. vitreum) in 1969-71. A total of 794 stomachs were examined. Four species contained walleye eggs: yellow perch (Perca flavescens), spottail shiner (Notropis hudsonius), stonecat (Noturus flavus) and white sucker (Catostomus commersoni). Yellow perch were by far the most consistent predators of walleye eggs, and spent female perch consumed more eggs than did males. The average number of walleye eggs in perch stomachs collected on any one day ranged from 36 to 734 for females and from 4 to 237 for males. The loss of walleye eggs due to fish predation appeared to be significant only when the rate of water warming slowed or stopped, thereby creating an extended overlap in the walleye-yellow perch reproductive period. Only under the uncommon condition of an extended time interval between walleye hatching and perch spawning, coupled with the presence of a large quantity of actively feeding perch, could egg predation reduce walleye reproductive success.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ohio Journal of Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"Out-of-print","usgsCitation":"Wolfert, D.R., Busch, W.N., and Baker, C.T., 1975, Predation by fish on walleye eggs on a spawning reef in western Lake Erie, 1969-71: Ohio Journal of Science, v. 75, no. 3, p. 118-125.","productDescription":"p. 118-125","startPage":"118","endPage":"125","numberOfPages":"7","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":131537,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"75","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db680026","contributors":{"authors":[{"text":"Wolfert, David R.","contributorId":49305,"corporation":false,"usgs":true,"family":"Wolfert","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":308583,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Busch, Wolf-Dieter N.","contributorId":46039,"corporation":false,"usgs":true,"family":"Busch","given":"Wolf-Dieter","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":308582,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baker, Carl T.","contributorId":25110,"corporation":false,"usgs":true,"family":"Baker","given":"Carl","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":308581,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70175523,"text":"70175523 - 1975 - Hydrologic data for Cow Bayou, Brazos River Basin, Texas, 1973","interactions":[],"lastModifiedDate":"2016-08-16T10:13:56","indexId":"70175523","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","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":"Hydrologic data for Cow Bayou, Brazos River Basin, Texas, 1973","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70175523","usgsCitation":"VanZandt, J.K., 1975, Hydrologic data for Cow Bayou, Brazos River Basin, Texas, 1973: Open-File Report, 74 p., https://doi.org/10.3133/70175523.","productDescription":"74 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326547,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b4394fe4b03bcb01039fda","contributors":{"authors":[{"text":"VanZandt, J. K.","contributorId":173701,"corporation":false,"usgs":false,"family":"VanZandt","given":"J.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":645561,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175571,"text":"70175571 - 1975 - Land-surface subsidence in the Houston-Galveston region, Texas","interactions":[],"lastModifiedDate":"2016-08-17T11:05:56","indexId":"70175571","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5174,"text":"Texas Water Development Board Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"188","title":"Land-surface subsidence in the Houston-Galveston region, Texas","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Texas Water Development Board","usgsCitation":"Gabrysch, R., and Bonnet, C., 1975, Land-surface subsidence in the Houston-Galveston region, Texas: Texas Water Development Board Report 188, 19 p.","productDescription":"19 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326639,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58b51e4b03bcb0104bc1e","contributors":{"authors":[{"text":"Gabrysch, R.K.","contributorId":105691,"corporation":false,"usgs":true,"family":"Gabrysch","given":"R.K.","affiliations":[],"preferred":false,"id":645732,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bonnet, C.W.","contributorId":44535,"corporation":false,"usgs":true,"family":"Bonnet","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":645733,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":13814,"text":"ofr75179 - 1975 - Water-resources appraisal of the Carson River basin, western Nevada","interactions":[],"lastModifiedDate":"2023-04-05T20:40:45.943288","indexId":"ofr75179","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","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":"75-179","title":"Water-resources appraisal of the Carson River basin, western Nevada","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr75179","usgsCitation":"Glancy, P.A., and Katzer, T.L., 1975, Water-resources appraisal of the Carson River basin, western Nevada: U.S. Geological Survey Open-File Report 75-179, Report: 177 p.; 18 Plates: 24.11 x 31.09 inches or smaller, https://doi.org/10.3133/ofr75179.","productDescription":"Report: 177 p.; 18 Plates: 24.11 x 31.09 inches or smaller","costCenters":[],"links":[{"id":42398,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0179/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42397,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0179/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42396,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0179/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42395,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0179/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":415298,"rank":21,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15109.htm","linkFileType":{"id":5,"text":"html"}},{"id":42408,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0179/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42407,"rank":20,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0179/plate-18.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42406,"rank":19,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0179/plate-17.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42405,"rank":18,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0179/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42404,"rank":17,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0179/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42403,"rank":16,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0179/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42402,"rank":15,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0179/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42401,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0179/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42400,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0179/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42399,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0179/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42394,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0179/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42393,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0179/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42392,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0179/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42391,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0179/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42390,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0179/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146279,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0179/report-thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Carson River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -119.925,\n              40.291\n            ],\n            [\n              -119.925,\n              38.6667\n            ],\n            [\n              -118.016,\n              38.667\n            ],\n            [\n              -118.016,\n              40.291\n            ],\n            [\n              -119.925,\n              40.291\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4e4a","contributors":{"authors":[{"text":"Glancy, Patrick A.","contributorId":87113,"corporation":false,"usgs":true,"family":"Glancy","given":"Patrick","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":168442,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Katzer, T. L.","contributorId":15211,"corporation":false,"usgs":true,"family":"Katzer","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":168441,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1001328,"text":"1001328 - 1975 - Duck plague in free-flying waterfowl observed during the Lake Andes epizootic","interactions":[],"lastModifiedDate":"2012-03-02T17:16:05","indexId":"1001328","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3770,"text":"Wildlife Disease Conference","active":true,"publicationSubtype":{"id":10}},"title":"Duck plague in free-flying waterfowl observed during the Lake Andes epizootic","docAbstract":"The first major epizootic of duck plague in free-flying waterfowl occurred at Lake Andes, South Dakota, in January and February, 1973. Duck plague was diagnosed in black ducks, mallards, pintail-mallard hybrids, redheads, common mergansers, common golden eyes, canvasbacks, American widgeon, wood ducks, and Canada geese, indicating the general susceptibility of ducks to duck plague. Clinical signs observed in mallards were droopiness, polydipsia, lethargy, reduced wariness, weakness, reluctance to fly, swimming in circles, bloody diarrhea, bloody fluid draining from the nares and bill, and terminal convulsions.Because the mallard was the most numerous and heavily infected species during the Lake Andes epizootic, gross and microscopic lesions of the gastrointestinal tract, liver, spleen, thymus, bursa of Fabricius, heart, lung, bone marrow, pancreas, and ovaries were described. Lesions of the esophagus and cloaca were in the stratified submucosal glands. In the small and large intestine, lesions were located in lymphocytic aggregates, lamina propria, and crypt epithelium. Hemorrhages and necrosis of hepatocytes and bile duct epithelium were noted in the liver. Diffuse necrosis of lymphocytic and reticuloendothelial tissue were evident in the spleen, bursa of Fabricius, and thymus. Hemorrhages in other tissues such as the lung and heart were often associated with lymphoid nodules, while those in organs such as the pancreas were associated with acinar necrosis. Intranuclear inclusion bodies were seen in stratified squamous epithelium of the esophagus and cloaca, crypt epithelium of the intestine, hepatocytes, bile duct epithelium, cells of Hassel's corpuscles, splenic periarteriolar reticular cells, and epithelial cells in the bursa of Fabricius.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wildlife Disease Conference","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Proctor, S., Pearson, G., and Leibovitz, L., 1975, Duck plague in free-flying waterfowl observed during the Lake Andes epizootic: Wildlife Disease Conference, v. 67, p. 1-16.","productDescription":"p. 1-16","startPage":"1","endPage":"16","numberOfPages":"15","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":133549,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"67","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5ae4b07f02db63018f","contributors":{"authors":[{"text":"Proctor, S.J.","contributorId":83075,"corporation":false,"usgs":true,"family":"Proctor","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":310881,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pearson, G.L.","contributorId":83868,"corporation":false,"usgs":true,"family":"Pearson","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":310882,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leibovitz, Louis","contributorId":41781,"corporation":false,"usgs":false,"family":"Leibovitz","given":"Louis","email":"","affiliations":[],"preferred":false,"id":310880,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1001289,"text":"1001289 - 1975 - Some nutritional aspects of reproduction in prairie nesting pintails","interactions":[],"lastModifiedDate":"2025-02-18T18:48:41.636514","indexId":"1001289","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Some nutritional aspects of reproduction in prairie nesting pintails","docAbstract":"<p>The nutritional significance of invertebrate foods in the diet of breeding hen waterfowl during the period of egg formation is discussed. Proximate, elemental, and amino acid analyses of the principal foods consumed by hen pintails (<i>Anas acut</i>) during the nesting season indicate the animal foods selected are rich sources of protein and calcium, whereas plant foods tested were low in protein, particularly in the essential amino acids lysine and methionine. Calcium content in major plant foods was far below needs considered adequate for egg production. Studies with penned, hand-reared pintails indicated the inadequacy of wheat as the dietary staple during breeding. Egg production among pairs on the control diet differed significantly from that of the wheat plus oystershell (P &lt; 0.05) and wheat (P &lt; 0.01) diets. Pairs fed wheat during the breeding period experienced nearly complete reproductive failure. The poor reproductive response among hens on the diet of wheat plus oystershell suggested that calcium availability was not the only factor limiting productivity.</p>","language":"English","publisher":"Wiley","doi":"10.2307/3800479","usgsCitation":"Krapu, G., and Swanson, G., 1975, Some nutritional aspects of reproduction in prairie nesting pintails: Journal of Wildlife Management, v. 39, no. 1, p. 156-162, https://doi.org/10.2307/3800479.","productDescription":"7 p.","startPage":"156","endPage":"162","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":133829,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e8e4b07f02db5e8f4f","contributors":{"authors":[{"text":"Krapu, Gary L.","contributorId":56994,"corporation":false,"usgs":true,"family":"Krapu","given":"Gary L.","affiliations":[],"preferred":false,"id":310817,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swanson, G.A.","contributorId":49299,"corporation":false,"usgs":true,"family":"Swanson","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":310816,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010131,"text":"70010131 - 1975 - Uranium determination in natural water by the fissiontrack technique","interactions":[],"lastModifiedDate":"2021-02-17T14:11:33.890976","indexId":"70010131","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2302,"text":"Journal of Geochemical Exploration","active":true,"publicationSubtype":{"id":10}},"title":"Uranium determination in natural water by the fissiontrack technique","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id3\" class=\"abstract author\"><div id=\"aep-abstract-sec-id4\"><p>The fission track technique, utilizing the neutron-induced fission of uranium-235, provides a versatile analytical method for the routine analysis of uranium in liquid samples of natural water. A detector is immersed in the sample and both are irradiated. The fission track density observed in the detector is directly proportional to the uranium concentration. The specific advantages of this technique are: (1) only a small quantity of sample, typically 0.1–1 ml, is needed; (2) no sample concentration is necessary; (3) it is capable of providing analyses with a lower reporting limit of 1 μg per liter; and (4) the actual time spent on an analysis can be only a few minutes. This paper discusses and describes the method.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0375-6742(75)90032-1","issn":"03756742","usgsCitation":"Reimer, G., 1975, Uranium determination in natural water by the fissiontrack technique: Journal of Geochemical Exploration, v. 4, no. 4, p. 425-431, https://doi.org/10.1016/0375-6742(75)90032-1.","productDescription":"7 p.","startPage":"425","endPage":"431","numberOfPages":"7","costCenters":[],"links":[{"id":219051,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbda6e4b08c986b329143","contributors":{"authors":[{"text":"Reimer, G.M.","contributorId":59800,"corporation":false,"usgs":true,"family":"Reimer","given":"G.M.","affiliations":[],"preferred":false,"id":358059,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70195624,"text":"70195624 - 1975 - New dimensions in diseases affecting waterfowl","interactions":[],"lastModifiedDate":"2018-02-23T13:31:15","indexId":"70195624","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"New dimensions in diseases affecting waterfowl","docAbstract":"<p><span>We start off with light heart, but as we near the marsh, we stop abruptly in shock and horror. The shoreline, where only last evening we saw thousands of sleek, apparently healthy birds, is now littered with their bodies. Most of them are ducks, but here and there we see a Canada goose, a gull, an avocet, a black-necked stilt, a pelican.....</span></p><p><span>This is the way Jensen and Williams (1964) described an outbreak of avian botulism in a western marsh. It illustrates, more vividly than dry facts and body counts, the impact a disease can have on a population of waterfowl.</span></p><p><span>When we think about waterfowl diseases, we probably think first of botulism and then of lead poisoning, the result of birds swallowing spent lead shot. In fact, these are the only two diseases discussed by Kortright (1942) and Day (1949) in major books on North American waterfowl, attesting to both their importance and our years of experience with them. Botulism was probably an old problem in 1910, but the catastrophic loss that summer of millions of aquatic birds near the Great Salt Lake and in California marked the beginning of real concern about its impact on waterfowl populations (Jensen and Williams, 1964). Concern about lead poisoning of waterfowl began a few years later following the investigations of Wetmore (1919).</span></p><p><span>Today, more than 50 years after these early reports, botulism and lead poisoning are still major disease problems of North American waterfowl, but they are no longer the only ones. After years of study, we have learned much about how these two diseases occur and about their prevention and control. But now there are new pathogens and new toxic compounds that can afflict waterfowl populations. So rather than redescribe the established disease problems of the past and present, I will concentrate on some of these new waterfowl disease problems of the present and future.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the first international waterfowl symposium","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"First international waterfowl symposium","conferenceDate":"February 4-6, 1975","conferenceLocation":"St. Louis, MO","language":"English","publisher":"Ducks Unlimited","usgsCitation":"Friend, M., 1975, New dimensions in diseases affecting waterfowl, <i>in</i> Proceedings of the first international waterfowl symposium, St. Louis, MO, February 4-6, 1975, p. 155-162.","productDescription":"8 p.","startPage":"155","endPage":"162","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":351935,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff5445e4b0da30c1bfdcbd","contributors":{"authors":[{"text":"Friend, Milton 0000-0002-2882-3629","orcid":"https://orcid.org/0000-0002-2882-3629","contributorId":31332,"corporation":false,"usgs":true,"family":"Friend","given":"Milton","email":"","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":729454,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15462,"text":"ofr75249 - 1975 - Dynamics of turbidity plumes in Lake Ontario","interactions":[],"lastModifiedDate":"2024-10-07T21:08:10.580039","indexId":"ofr75249","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","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":"75-249","title":"Dynamics of turbidity plumes in Lake Ontario","docAbstract":"<p>Large-turbidity features along the 275-kilometre long south shore of Lake Ontario were analyzed using LANDSAT-1 images. The ESIAC system developed by the Stanford Research Institute, was used to obtain enlargements and false-color renditions of turbidity plumes. After projection on a video screen, individual turbidity features were analyzed, mapped, and photographed.</p><p>The Niagara River plume, as much as 500 square kilometres in area, is by far, the largest turbidity feature in the lake. Based on image tonal comparisons, turbidity in the Welland Canal is usually higher than that in any other watercourse discharging into the lake throughout the shipping season. Somewhat less turbid water enters the lake from the Port Dalhousie diversion channel and the Genesee River. Relatively clear water resulting from the deposition of suspended matter in numerous upstream lakes is discharged by the Niagara and Oswego rivers.</p><p>Plume analysis corroborates the presence of a prevailing eastward flowing longshore current along the entire south shore. This current is most persistent at the Oswego River outlet but is quite variable in the Rochester embayment, where rapid shifts in water movement were occasionally detected in LANDSAT images. The position of the spring thermal bar, a zone, of maximum density water corresponding to the 4°C isotherm, was approximately located in images obtained during April 1973. Although eastward moving currents were detected on the inshore side of the thermal bar, westward moving counter currents seem to be dominant along its offshore side.</p><p>Plumes generated by beach erosion were readily detected in the images. Such areas are identified by light to very light, long, narrow plumes paralleling the coastline. Extensive areas of the south shore are subject to erosion, but the most severely affected beaches are situated between Fifty Mile Pt., Ontario and Thirty Mile Pt., N.Y., along the Rochester embayment, and between Sodus Bay and Nine Mile Pt.</p><p>Color illustrations of figure accession numbers EDC-010077 to EDC-010106 are available for purchase from the EROS Data Center, Sioux Falls, South Dakota 57198.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr75249","collaboration":"Prepared in cooperation with the National Aeronautics Space Administration/Goddard Space Flight Center, Greenbelt, Maryland","usgsCitation":"Pluhowski, E.J., 1975, Dynamics of turbidity plumes in Lake Ontario: U.S. Geological Survey Open-File Report 75-249, Report: ix, 59 p., https://doi.org/10.3133/ofr75249.","productDescription":"Report: ix, 59 p.","costCenters":[],"links":[{"id":149041,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0249/report-thumb.jpg"},{"id":462666,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0249/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Canada, United States","otherGeospatial":"Lake Ontario","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -80.99172224212556,\n              45.15721980352575\n            ],\n            [\n              -80.99172224212556,\n              42.37218583599275\n            ],\n            [\n              -74.39757490950474,\n              42.37218583599275\n            ],\n            [\n              -74.39757490950474,\n              45.15721980352575\n            ],\n            [\n              -80.99172224212556,\n              45.15721980352575\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a59e4b07f02db62f706","contributors":{"authors":[{"text":"Pluhowski, Edward J.","contributorId":87911,"corporation":false,"usgs":true,"family":"Pluhowski","given":"Edward","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":171172,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010948,"text":"70010948 - 1975 - Mercury distribution in ancient and modern sediment of northeastern Bering Sea","interactions":[{"subject":{"id":15187,"text":"ofr72268 - 1972 - Mercury distribution in ancient and modern sediment of northeastern Bering Sea","indexId":"ofr72268","publicationYear":"1972","noYear":false,"title":"Mercury distribution in ancient and modern sediment of northeastern Bering Sea"},"predicate":"SUPERSEDED_BY","object":{"id":70010948,"text":"70010948 - 1975 - Mercury distribution in ancient and modern sediment of northeastern Bering Sea","indexId":"70010948","publicationYear":"1975","noYear":false,"title":"Mercury distribution in ancient and modern sediment of northeastern Bering Sea"},"id":1}],"lastModifiedDate":"2013-01-24T14:24:55","indexId":"70010948","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Mercury distribution in ancient and modern sediment of northeastern Bering Sea","docAbstract":"Reconnaissance sampling of surface and subsurface sediment to a maximum depth of 80 m below the sea floor shows that typical values of 0.03 p.p.m. and anomalies of 0.2-1.3 p.p.m. mercury have been present in northeastern Bering Sea since Early Pliocene time. Values are highest in modern beach (maximum 1.3 and mean 0.22 p.p.m. Hg) and nearshore subsurface gravels (maximum 0.6 and mean 0.06 p.p.m. Hg) along the highly mineralized Seward Peninsula and in clayey silt rich in organic matter (maximum 0.16 and mean 0.10 p.p.m. Hg) throughout the region. Although gold mining may be partly responsible for high mercury levels in the modern beach near Nome, Alaska (maximum 0.45 p.p.m.), equally high or greater concentrations of mercury occur in buried Pleistocene sediments immediately offshore (maximum 0.6 p.p.m.) and in modern unpolluted beach sediments at Bluff (maximum 1.3 p.p.m.); this suggests that the contamination effects of mining may be no greater than natural concentration processes in the Seward Peninsula region. The mercury content of offshore surface sediment, even adjacent to mercury-rich beaches, corresponds to that of unpolluted marine and fresh-water sediment elsewhere. The normal values that prevail offshore may be attributable to entrapment of mercury-bearing heavy minerals on beaches near sources and/or dilution effects of offshore sedimentation. The few minor anomalies offshore occur in glacial drift derived from mercury source regions of Chukotka (Siberia) and Seward Peninsula; Pleistocene shoreline processes have reworked the drift to concentrate the heavy metals. The distribution pattern of mercury indicates that particulate mercury-bearing minerals have not been widely dispersed from onland deposits in quantities sufficient to increase mercury levels above normal in offshore sediments of Bering Sea; however, it shows that natural sedimentary processes can concentrate this mercury in beaches of the coastal zone where there already is concern because of potential pollution from man's activities.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam Netherlands","doi":"10.1016/0025-3227(75)90006-7","issn":"00253227","usgsCitation":"Nelson, C., Pierce, D., Leong, K., and Wang, F., 1975, Mercury distribution in ancient and modern sediment of northeastern Bering Sea: Marine Geology, v. 18, no. 3, p. 91-104, https://doi.org/10.1016/0025-3227(75)90006-7.","productDescription":"14 p.","startPage":"91","endPage":"104","costCenters":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"links":[{"id":220949,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266423,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0025-3227(75)90006-7"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 161.98,51.22 ], [ 161.98,66.05 ], [ -157.0,66.05 ], [ -157.0,51.22 ], [ 161.98,51.22 ] ] ] } } ] }","volume":"18","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5401e4b0c8380cd6ce5c","contributors":{"authors":[{"text":"Nelson, C.H.","contributorId":88346,"corporation":false,"usgs":true,"family":"Nelson","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":359957,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pierce, D.E.","contributorId":88083,"corporation":false,"usgs":true,"family":"Pierce","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":359956,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leong, Kam","contributorId":103660,"corporation":false,"usgs":true,"family":"Leong","given":"Kam","affiliations":[],"preferred":false,"id":359958,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wang, F.F.H.","contributorId":87219,"corporation":false,"usgs":true,"family":"Wang","given":"F.F.H.","email":"","affiliations":[],"preferred":false,"id":359955,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70010098,"text":"70010098 - 1975 - PCB's in Suburban Watershed, Reston, Va","interactions":[],"lastModifiedDate":"2023-10-20T17:11:29.004395","indexId":"70010098","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"PCB's in Suburban Watershed, Reston, Va","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Chemical Society","doi":"10.1021/es60107a001","issn":"0013936X","usgsCitation":"Martell, J., Rickert, D.A., and Siegel, F., 1975, PCB's in Suburban Watershed, Reston, Va: Environmental Science & Technology, v. 9, no. 9, p. 872-875, https://doi.org/10.1021/es60107a001.","productDescription":"4 p.","startPage":"872","endPage":"875","costCenters":[],"links":[{"id":219739,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Virginia","city":"Reston","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -77.40056795260114,\n              38.9430361988814\n            ],\n            [\n              -77.395583952518,\n              38.92203585821528\n            ],\n            [\n              -77.29652695086331,\n              38.90539271207308\n            ],\n            [\n              -77.29091995076968,\n              38.943682264600966\n            ],\n            [\n              -77.31251728446408,\n              38.97436360424581\n            ],\n            [\n              -77.37564795218545,\n              38.97581660129856\n            ],\n            [\n              -77.40056795260114,\n              38.9430361988814\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"9","issue":"9","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a7335e4b0c8380cd76f0f","contributors":{"authors":[{"text":"Martell, J.M.","contributorId":90868,"corporation":false,"usgs":true,"family":"Martell","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":357890,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rickert, D. A.","contributorId":53773,"corporation":false,"usgs":true,"family":"Rickert","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":357889,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Siegel, F.R.","contributorId":105430,"corporation":false,"usgs":true,"family":"Siegel","given":"F.R.","email":"","affiliations":[],"preferred":false,"id":357891,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010099,"text":"70010099 - 1975 - Water analysis","interactions":[],"lastModifiedDate":"2023-03-20T10:55:44.308773","indexId":"70010099","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Water analysis","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60355a010","usgsCitation":"Fishman, M.J., and Erdmann, D.E., 1975, Water analysis: Analytical Chemistry, v. 47, no. 5, p. 334-361, https://doi.org/10.1021/ac60355a010.","productDescription":"28 p.","startPage":"334","endPage":"361","costCenters":[],"links":[{"id":219740,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"47","issue":"5","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505bc795e4b08c986b32c503","contributors":{"authors":[{"text":"Fishman, M. J.","contributorId":65069,"corporation":false,"usgs":true,"family":"Fishman","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":357893,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erdmann, D. E.","contributorId":30264,"corporation":false,"usgs":true,"family":"Erdmann","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":357892,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70009922,"text":"70009922 - 1975 - The determination of specific forms of aluminum in natural water","interactions":[],"lastModifiedDate":"2021-03-02T13:56:28.864336","indexId":"70009922","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"The determination of specific forms of aluminum in natural water","docAbstract":"<p id=\"simple-para.0010\">A procedure for analysis and pretreatment of natural-water samples to determine very low concentrations of Al is described which distinguishes the rapidly reacting equilibrium species from the metastable or slowly reacting macro ions and colloidal suspended material. Aluminum is complexed with 8-hydroxyquinoline (oxine), pH is adjusted to 8.3 to minimize interferences, and the aluminum oxinate is extracted with methyl isobutyl ketone (MIBK) prior to analysis by atomic absorption. To determine equilibrium species only, the contact time between sample and 8-hydroxyquinoline is minimized. The Al may be extracted at the sample site with a minimum of equipment and the MIBK extract stored for several weeks prior to atomic absorption analysis.</p><p id=\"simple-para.0015\">Data obtained from analyses of 39 natural groundwater samples indicate that filtration through a 0.1-μm pore size filter is not an adequate means of removing all insoluble and metastable Al species present, and extraction of Al immediately after collection is necessary if only dissolved and readily reactive species are to be determined. An average of 63% of the Al present in natural waters that had been filtered through 0.1-μm pore size filters was in the form of monomeric ions. The total Al concentration, which includes all forms that passed through a 0.1-μm pore size filter, ranged 2–70 μg/l. The concentration of Al in the form of monomeric ions ranged from below detection to 57 μg/l. Most of the natural water samples used in this study were collected from thermal springs and oil wells.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0009-2541(75)90018-2","issn":"00092541","usgsCitation":"Barnes, R., 1975, The determination of specific forms of aluminum in natural water: Chemical Geology, v. 15, no. 3, p. 177-191, https://doi.org/10.1016/0009-2541(75)90018-2.","productDescription":"p.","startPage":"177","endPage":"191","numberOfPages":"15","costCenters":[],"links":[{"id":218834,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baa9ee4b08c986b3228d7","contributors":{"authors":[{"text":"Barnes, R.B.","contributorId":53393,"corporation":false,"usgs":true,"family":"Barnes","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":357465,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1003481,"text":"1003481 - 1975 - Effects of pH on toxicity of antimycin to fish","interactions":[],"lastModifiedDate":"2025-03-04T16:14:14.464778","indexId":"1003481","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","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":"Effects of pH on toxicity of antimycin to fish","docAbstract":"<p><span>Detoxification of antimycin at pH 9.5 was caused by two factors. The piscicide was biologically unavailable at the high pH, and this unavailability was reversed by decreasing the pH of water solutions. Simultaneously antimycin detoxified with time, and the resulting loss in toxicity was irreversible. The toxicity of antimycin was related to the amount of un-ionized molecules; however, the dissociation curve resulting from the published pKa of 5.1 does not agree with the implied dissociation when based on toxicity. Toxicity of antimycin decreased gradually from pH 6.5 to 8.5 and abruptly from 8.5 to 9.5 with carp (</span><i>Cyprinus carpio</i><span>), green sunfish (</span><i>Lepomis cyanellus</i><span>), and bluegill (</span><i>Lepomis macrochirus</i><span>). As previously suggested, water hardness had little or no effect on toxicity.</span></p>","language":"English","publisher":"Canadian Science Publishing","doi":"10.1139/f75-100","usgsCitation":"Marking, L.L., 1975, Effects of pH on toxicity of antimycin to fish: Journal of the Fisheries Research Board of Canada, v. 32, no. 6, p. 769-773, https://doi.org/10.1139/f75-100.","productDescription":"5 p.","startPage":"769","endPage":"773","numberOfPages":"5","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":197003,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611b25","contributors":{"authors":[{"text":"Marking, L. L.","contributorId":90661,"corporation":false,"usgs":true,"family":"Marking","given":"L.","middleInitial":"L.","affiliations":[],"preferred":false,"id":313366,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1001316,"text":"1001316 - 1975 - Boreal owl taken near Watertown","interactions":[],"lastModifiedDate":"2018-01-05T10:26:45","indexId":"1001316","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3441,"text":"South Dakota Bird Notes","active":true,"publicationSubtype":{"id":10}},"title":"Boreal owl taken near Watertown","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"South Dakota Bird Notes","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Rose, W., and Springer, P.F., 1975, Boreal owl taken near Watertown: South Dakota Bird Notes, v. 27, no. 4, p. 64-65.","productDescription":"2 p.","startPage":"64","endPage":"65","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":128939,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602ac1","contributors":{"authors":[{"text":"Rose, W.A.","contributorId":93425,"corporation":false,"usgs":true,"family":"Rose","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":310870,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Springer, P. F.","contributorId":56590,"corporation":false,"usgs":false,"family":"Springer","given":"P.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":310869,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1000082,"text":"1000082 - 1975 - Effect of different constant incubation temperatures on egg survival and embryonic development in lake whitefish (Coregonus clupeaformis)","interactions":[],"lastModifiedDate":"2016-03-14T10:22:22","indexId":"1000082","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","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":"Effect of different constant incubation temperatures on egg survival and embryonic development in lake whitefish (Coregonus clupeaformis)","docAbstract":"<p><span>Eggs of lake whitefish (Coregonus clupeaformis) were incubated in a constant-flow incubator at constant temperatures of 0.5, 2.0, 4.0, 5.9, 7.8, and 10.0 C. The time from fertilization to median hatch was inversely related to temperature, and ranged from 41.7 days at 10.0 C to 182 days at 0.5 C. The percentage hatch was highest (70.9-73.3%) at 4.0, 5.9, and 7.8 C, and was greatly reduced (6.0-28.4%) at 0.5, 2.0, and 10.0 C. The mortality of embryos was greatest during the early stages of development. Abnormally developed fry were most frequent (85.9% of the hatch) at 10.0 C, and least frequent (2.8%) at 4.0 C. Mean lengths of fry at hatching were shorter at 7.8 and 10.0 C (12.4 and 8.8 mm, respectively) than at lower temperatures (13.1 to 13.5 mm). The optimum temperature range for incubation of lake whitefish eggs was 3.2 to 8.1 C. Equations were derived for predicting development time to 20 successive stages, and to hatching, at constant incubation temperatures and at fluctuating daily mean water temperatures.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1975)104<555:EODCIT>2.0.CO;2","usgsCitation":"Brooke, L., 1975, Effect of different constant incubation temperatures on egg survival and embryonic development in lake whitefish (Coregonus clupeaformis): Transactions of the American Fisheries Society, v. 104, no. 3, p. 555-559, https://doi.org/10.1577/1548-8659(1975)104<555:EODCIT>2.0.CO;2.","productDescription":"5 p.","startPage":"555","endPage":"559","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":132747,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"104","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625710","contributors":{"authors":[{"text":"Brooke, L.T.","contributorId":60589,"corporation":false,"usgs":true,"family":"Brooke","given":"L.T.","email":"","affiliations":[],"preferred":false,"id":308050,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}