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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha529","usgsCitation":"Prescott, G., 1974, Ground-water favorability and surficial geology of the Cherryfield-Jonesboro area, Maine: U.S. Geological Survey Hydrologic Atlas 529, 1 Plate: 37.00 × 41.25 inches, https://doi.org/10.3133/ha529.","productDescription":"1 Plate: 37.00 × 41.25 inches","costCenters":[],"links":[{"id":89339,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/529/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":187923,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":398606,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15919.htm"}],"scale":"62500","country":"United States","state":"Maine","otherGeospatial":"Cherryfield-Jonesboro area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -68,\n 44.423\n ],\n [\n -67.5,\n 44.423\n ],\n [\n -67.5,\n 44.75\n ],\n [\n -68,\n 44.75\n ],\n [\n -68,\n 44.423\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ce57","contributors":{"authors":[{"text":"Prescott, Glenn C.","contributorId":38126,"corporation":false,"usgs":true,"family":"Prescott","given":"Glenn C.","affiliations":[],"preferred":false,"id":277610,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70175504,"text":"70175504 - 1974 - Flood stages and discharges for small streams in Texas : compilation of data through September 1972","interactions":[],"lastModifiedDate":"2016-08-15T15:00:06","indexId":"70175504","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","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":"Flood stages and discharges for small streams in Texas : compilation of data through September 1972","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70175504","usgsCitation":"Schroeder, E., 1974, Flood stages and discharges for small streams in Texas : compilation of data through September 1972: Open-File Report, Report: ix, 283 p.; Plate, https://doi.org/10.3133/70175504.","productDescription":"Report: ix, 283 p.; Plate","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326501,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b2e7bae4b03bcb0102e8ac","contributors":{"authors":[{"text":"Schroeder, E.E.","contributorId":19970,"corporation":false,"usgs":true,"family":"Schroeder","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":645513,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010217,"text":"70010217 - 1974 - Spectrophotometric determination of molybdenum in rocks with thiocyanate","interactions":[],"lastModifiedDate":"2021-01-22T14:18:04.09582","indexId":"70010217","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","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":"Spectrophotometric determination of molybdenum in rocks with thiocyanate","docAbstract":"A rapid procedure for the determination of microgram amounts of molybdenum in rocks is described. After acid decomposition, molybdenum is extracted from a hydrochloric acid solution into xylene with tributyl phosphate. After back-extraction with water, molybdenum is extracted as the α-benzoinoximate into chloroform, stripped into hydrochloric acid extracted as the thiocyanate into amyl alcohol, and determined spectrophotometrically. The molybdenum thiocyanate color produced is stable, sensitive, and reproducible. Results of analyses of several of the U.S. Geological Survey standard rocks are given.
Fifty-five of the principal hot springs in northern and central Nevada have been sampled for chemical analyses. Major element constituents, sodium, potassium, calcium, and silica suggest minimum thermal-aquifer temperatures of 140°C or more at 16 of the hot spring complexes. At least five of the hot springs issue mixed waters which may indicate thermal-aquifer temperatures significantly lower than the true thermal-aquifer temperature.
Sodium is the principal cation in almost all the spring waters. Four springs in northern Nye County and adjacent Eureka County have approximately equal amounts of sodium and calcium. Bicarbonate is the principal anion in most of the spring waters. However, the sampled hot springs on the western edge of the State have chloride as the principal anion. A diffuse zone of bicarbonate chloride waters with or without sulfate separates the chloride and bicarbonate regions.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr741066","usgsCitation":"Mariner, R.H., Rapp, J.B., Willey, L., and Presser, T.S., 1974, The chemical composition and estimated minimum thermal reservoir temperatures of the principal hot springs of northern and central Nevada: U.S. Geological Survey Open-File Report 74-1066, 32 p., https://doi.org/10.3133/ofr741066.","productDescription":"32 p.","costCenters":[],"links":[{"id":403210,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/1066/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":172000,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/1066/report-thumb.jpg"}],"country":"United States","state":"Nevada","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.003662109375,\n 42.00032514831621\n ],\n [\n -120.0146484375,\n 39.01918369029134\n ],\n [\n -118.421630859375,\n 37.88352498087131\n ],\n [\n -114.04907226562499,\n 38.004819966413194\n ],\n [\n -114.0380859375,\n 42.00848901572399\n ],\n [\n -120.003662109375,\n 42.00032514831621\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db66939c","contributors":{"authors":[{"text":"Mariner, Robert H.","contributorId":81075,"corporation":false,"usgs":true,"family":"Mariner","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":237027,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rapp, J. B.","contributorId":28987,"corporation":false,"usgs":true,"family":"Rapp","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":237025,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Willey, L.M.","contributorId":44607,"corporation":false,"usgs":true,"family":"Willey","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":237026,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Presser, T. S.","contributorId":93875,"corporation":false,"usgs":true,"family":"Presser","given":"T.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":237028,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":7000076,"text":"7000076 - 1974 - The United States Geological Survey","interactions":[],"lastModifiedDate":"2012-02-02T00:15:08","indexId":"7000076","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","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 United States Geological Survey","language":"ENGLISH","doi":"10.3133/7000076","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, The United States Geological Survey: General Interest Publication, 27 p. : ill. ; 24 cm., https://doi.org/10.3133/7000076.","productDescription":"27 p. : ill. ; 24 cm.","costCenters":[],"links":[{"id":196279,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d5f7","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":535099,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70175566,"text":"70175566 - 1974 - Ground-water resources of Brazos and Burleson Counties, Texas","interactions":[],"lastModifiedDate":"2016-08-17T10:53:36","indexId":"70175566","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","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":"185","title":"Ground-water resources of Brazos and Burleson Counties, Texas","docAbstract":"No abstract available.
","language":"English","publisher":"Texas Water Development Board","usgsCitation":"Follett, C., 1974, Ground-water resources of Brazos and Burleson Counties, Texas: Texas Water Development Board Report 185, 196 p.","productDescription":"196 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326631,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58ad3e4b03bcb0104bbd8","contributors":{"authors":[{"text":"Follett, C.R.","contributorId":14800,"corporation":false,"usgs":true,"family":"Follett","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":645725,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70176024,"text":"70176024 - 1974 - Records of precipitation, water levels, and ground-water recharge to the Edwards and associated limestones, San Antonio area, Texas, 1972-73","interactions":[],"lastModifiedDate":"2016-08-23T15:31:49","indexId":"70176024","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5177,"text":"Edwards Underground Water District Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"33","title":"Records of precipitation, water levels, and ground-water recharge to the Edwards and associated limestones, San Antonio area, Texas, 1972-73","docAbstract":"No abstract available.
","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Puente, C., 1974, Records of precipitation, water levels, and ground-water recharge to the Edwards and associated limestones, San Antonio area, Texas, 1972-73: Edwards Underground Water District Bulletin 33, 12 p.","productDescription":"12 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":327750,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73eee4b03fd6b7df2d83","contributors":{"authors":[{"text":"Puente, Celso","contributorId":36140,"corporation":false,"usgs":true,"family":"Puente","given":"Celso","email":"","affiliations":[],"preferred":false,"id":646812,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70176023,"text":"70176023 - 1974 - Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1973","interactions":[],"lastModifiedDate":"2016-08-23T15:30:09","indexId":"70176023","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5177,"text":"Edwards Underground Water District Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"32","title":"Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1973","docAbstract":"No abstract available.
","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Rappmund, R.A., 1974, Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1973: Edwards Underground Water District Bulletin 32, 9 p.","productDescription":"9 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":327748,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73dde4b03fd6b7df2cff","contributors":{"authors":[{"text":"Rappmund, R. A.","contributorId":173985,"corporation":false,"usgs":false,"family":"Rappmund","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":646811,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70175568,"text":"70175568 - 1974 - Ground-water resources of Grimes County, Texas","interactions":[],"lastModifiedDate":"2016-08-17T10:56:34","indexId":"70175568","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","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":"186","title":"Ground-water resources of Grimes County, Texas","docAbstract":"No abstract available.
","language":"English","publisher":"Texas Water Development Board","usgsCitation":"Baker, E.T., Follett, C., McAdoo, G., and Bonnet, C., 1974, Ground-water resources of Grimes County, Texas: Texas Water Development Board Report 186, 109 p.","productDescription":"109 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326632,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58ad4e4b03bcb0104bbda","contributors":{"authors":[{"text":"Baker, E. T. Jr.","contributorId":88366,"corporation":false,"usgs":true,"family":"Baker","given":"E.","suffix":"Jr.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":645727,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Follett, C.R.","contributorId":14800,"corporation":false,"usgs":true,"family":"Follett","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":645728,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McAdoo, G.D.","contributorId":99823,"corporation":false,"usgs":true,"family":"McAdoo","given":"G.D.","email":"","affiliations":[],"preferred":false,"id":645729,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bonnet, C.W.","contributorId":44535,"corporation":false,"usgs":true,"family":"Bonnet","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":645730,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":1014280,"text":"1014280 - 1974 - Nitrogen and phosphorus balance of grass carp, Ctenopharyngodon idella, fed elodea, Egeria denea","interactions":[],"lastModifiedDate":"2026-04-14T18:15:32.815088","indexId":"1014280","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","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":"Nitrogen and phosphorus balance of grass carp, Ctenopharyngodon idella, fed elodea, Egeria denea","docAbstract":"The herbivorous grass carp fed winter elodea exhibited a negative nitrogen balance in metabolism, suggesting that food having a higher protein content would be required for normal growth. About a third of the phosphorus contained in food was retained; hence, a combination of aquatic plants and grass carp might afford an effective biological method for removing phosphorus from water. Water quality was altered by the excretion of ammonium and orthophosphate by grass carp. Even though the grass carp might be useful in removing some phosphorus from water, its principal impact was to increase the rate of recycling of nitrogen and phosphorus.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1974)103<587:NAPBOG>2.0.CO;2","usgsCitation":"Stanley, J., 1974, Nitrogen and phosphorus balance of grass carp, Ctenopharyngodon idella, fed elodea, Egeria denea: Transactions of the American Fisheries Society, v. 103, no. 3, p. 587-592, https://doi.org/10.1577/1548-8659(1974)103<587:NAPBOG>2.0.CO;2.","productDescription":"6 p.","startPage":"587","endPage":"592","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132058,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"103","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697340","contributors":{"authors":[{"text":"Stanley, J.G.","contributorId":31700,"corporation":false,"usgs":true,"family":"Stanley","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":320109,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":42456,"text":"ofr741023 - 1974 - Preliminary map showing availability of ground water from major glacial-drift aquifers in Griggs and Steele Counties, North Dakota","interactions":[{"subject":{"id":42456,"text":"ofr741023 - 1974 - Preliminary map showing availability of ground water from major glacial-drift aquifers in Griggs and Steele Counties, North Dakota","indexId":"ofr741023","publicationYear":"1974","noYear":false,"title":"Preliminary map showing availability of ground water from major glacial-drift aquifers in Griggs and Steele Counties, North Dakota"},"predicate":"SUPERSEDED_BY","object":{"id":70046305,"text":"70046305 - 1977 - Ground-water resources of Griggs and Steele Counties, North Dakota","indexId":"70046305","publicationYear":"1977","noYear":false,"title":"Ground-water resources of Griggs and Steele Counties, North Dakota"},"id":1}],"supersededBy":{"id":70046305,"text":"70046305 - 1977 - Ground-water resources of Griggs and Steele Counties, North Dakota","indexId":"70046305","publicationYear":"1977","noYear":false,"title":"Ground-water resources of Griggs and Steele Counties, North Dakota"},"lastModifiedDate":"2023-03-06T14:04:34.585183","indexId":"ofr741023","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","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":"74-1023","title":"Preliminary map showing availability of ground water from major glacial-drift aquifers in Griggs and Steele Counties, North Dakota","docAbstract":"This investigation is part of a statewide program to determine the location, extent, and hydrologic characteristics of the ground-water reservoirs (aquifers).
The investigation was made cooperatively by the U.S. Geological Survey, North Dakota State Water Commission, North Dakota Geological Survey, and Griggs and Steele Counties Water Management Districts.
This preliminary map is the first product of an intensive study of Griggs and Steele Counties. A well inventory provided data on depth, construction, and productivity of private and public wells. Test drilling by the North Dakota State Water Commission, Federal agencies, and commercial well drillers provided information regarding the thickness, grain size, and extent of the aquifers. Potential well yields were estimated from the thickness and hydraulic conductivity of the water-bearing materials logged at each test hole, and from aquifer tests. Generally, the yield of a well is proportional to the hydraulic conductivity and thickness of the aquifer.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr741023","collaboration":"Prepared in cooperation with the North Dakota State Water Commission, North Dakota Geological Survey, and Griggs and Steele Counties Water Management Districts","usgsCitation":"Downey, J.S., 1974, Preliminary map showing availability of ground water from major glacial-drift aquifers in Griggs and Steele Counties, North Dakota: U.S. Geological Survey Open-File Report 74-1023, 1 Plate: 35.29 21.60 inches, https://doi.org/10.3133/ofr741023.","productDescription":"1 Plate: 35.29 21.60 inches","costCenters":[],"links":[{"id":136614,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/1023/report-thumb.jpg"},{"id":412566,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/1023/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"126720","country":"United States","state":"North Dakota","county":"Griggs County, Steele County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -98.5019,47.2394 ], [ -98.5019,47.6742 ], [ -97.4504,47.6742 ], [ -97.4504,47.2394 ], [ -98.5019,47.2394 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696910","contributors":{"authors":[{"text":"Downey, Joe S.","contributorId":102454,"corporation":false,"usgs":true,"family":"Downey","given":"Joe","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":226526,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70161851,"text":"70161851 - 1974 - Effect of nitrogen supersaturated water on coho and chinook salmon","interactions":[],"lastModifiedDate":"2016-01-06T16:35:27","indexId":"70161851","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Effect of nitrogen supersaturated water on coho and chinook salmon","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1974)36[152:EONSWO]2.0.CO;2","usgsCitation":"Rucker, R.R., and Kangas, P.M., 1974, Effect of nitrogen supersaturated water on coho and chinook salmon: Progressive Fish-Culturist, v. 36, no. 3, p. 152-156, https://doi.org/10.1577/1548-8659(1974)36[152:EONSWO]2.0.CO;2.","productDescription":"5 p.","startPage":"152","endPage":"156","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":313990,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"36","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568e48f0e4b0e7a44bc418f3","contributors":{"authors":[{"text":"Rucker, Robert R.","contributorId":69615,"corporation":false,"usgs":true,"family":"Rucker","given":"Robert","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":587925,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kangas, Paul M.","contributorId":152102,"corporation":false,"usgs":false,"family":"Kangas","given":"Paul","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":587926,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70164355,"text":"70164355 - 1974 - New seismic study begins in Puerto Rico","interactions":[],"lastModifiedDate":"2016-03-22T10:17:04","indexId":"70164355","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"New seismic study begins in Puerto Rico","docAbstract":"A new seismological project is now underway in Puerto Rico to provide information needed for accurate assessment of the island's seismic hazard. The project should also help to increase understanding of the tectonics and geologic evolution of the Caribbean region. The Puerto Rico Seismic Program is being conducted by the Geological Survey with support provided by the Puerto Rico Water Resources Authority, an agency responsible for generation and distribution of electric power throughout the Commonwealth. The Program will include the installation of a network of high quality seismograph stations to monitor seismic activity on and around Puerto Rico. These stations will be distributed across the island to record the seismicity as uniformly as possible. The detection and accurate location of small earthquakes, as well as moderate magnitude shocks, will aid in mapping active seismic zones and in compiling frequency of occurrence statistics which ultimately wil be useful in seismic risk-zoning of hte island.
","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Tarr, A., 1974, New seismic study begins in Puerto Rico: Earthquake Information Bulletin (USGS), v. 6, no. 4, p. 23-26.","productDescription":"4 p.","startPage":"23","endPage":"26","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":316432,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Puerto Rico","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -67.15393066406249,\n 18.516074596589366\n ],\n [\n -67.19512939453125,\n 18.461373375441447\n ],\n [\n -67.30224609375,\n 18.351918656384534\n ],\n [\n -67.18963623046875,\n 18.22674258246203\n ],\n [\n -67.23907470703125,\n 18.054478439496076\n ],\n [\n -67.22259521484375,\n 17.91863608052212\n ],\n [\n -67.05780029296875,\n 17.91602270387768\n ],\n [\n -66.829833984375,\n 17.921249418623304\n ],\n [\n -66.70898437499999,\n 17.934315530810004\n ],\n [\n -66.4837646484375,\n 17.947380678685217\n ],\n [\n -66.33819580078125,\n 17.913409288694826\n ],\n [\n -66.1761474609375,\n 17.908182342733486\n ],\n [\n -66.00860595703125,\n 17.939541705711544\n ],\n [\n -65.80810546875,\n 17.981345545819597\n ],\n [\n -65.7696533203125,\n 18.091033487001273\n ],\n [\n -65.7147216796875,\n 18.158901213171138\n ],\n [\n -65.61859130859375,\n 18.187606552494625\n ],\n [\n -65.5609130859375,\n 18.245003052249718\n ],\n [\n -65.58013916015625,\n 18.325847765727083\n ],\n [\n -65.621337890625,\n 18.40665471391906\n ],\n [\n -65.81085205078125,\n 18.445741249840804\n ],\n [\n -66.082763671875,\n 18.47960905583197\n ],\n [\n -66.39312744140625,\n 18.51347017266187\n ],\n [\n -66.796875,\n 18.505656663040533\n ],\n [\n -67.11822509765625,\n 18.529096121414817\n ],\n [\n -67.15393066406249,\n 18.516074596589366\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"6","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56b08fe1e4b010e2af2a5dec","contributors":{"authors":[{"text":"Tarr, Arthur C.","contributorId":75903,"corporation":false,"usgs":true,"family":"Tarr","given":"Arthur C.","affiliations":[],"preferred":false,"id":597098,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70162243,"text":"70162243 - 1974 - Comparative toxicity of two Iodophors to rainbow trout eggs","interactions":[],"lastModifiedDate":"2016-01-19T14:24:08","indexId":"70162243","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","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":"Comparative toxicity of two Iodophors to rainbow trout eggs","docAbstract":"Toxicity of Wescodyne(R) and Betadine(R) to eyed eggs was not adversely affected by water hardness (as calcium and magnesium) or by exposure periods up to 60 min. Both iodophors were much more toxic below pH 6.0 than at pH 8.0. In general Wescodyne was slightly more toxic than Betadine. Significant egg loss occurred if freshly fertilized eggs were water-hardened in either iodophor at 100 ppm of iodine, but egg loss at 25 ppm of iodine or at 100 ppm if the eggs were disinfected 30 min after water hardening was comparable to the control. Also, there was no effect on the egg mortality or fry development following single or multiple exposures after eggs were water hardened. At pH 6.0 and above, Wescodyne and Betadine at 100 ppm iodine in a 15-min dip would be safe to use on rainbow trout eggs at any stage of development after water hardening. Recommendations and precautions for hatchery use are given.
","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1974)103<73:CTOTIT>2.0.CO;2","usgsCitation":"Amend, D.F., 1974, Comparative toxicity of two Iodophors to rainbow trout eggs: Transactions of the American Fisheries Society, v. 103, no. 1, p. 73-78, https://doi.org/10.1577/1548-8659(1974)103<73:CTOTIT>2.0.CO;2.","productDescription":"6 p.","startPage":"73","endPage":"78","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314481,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"103","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569f6c41e4b0961cf27fd194","contributors":{"authors":[{"text":"Amend, Donald F.","contributorId":106543,"corporation":false,"usgs":true,"family":"Amend","given":"Donald","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":588969,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":96451,"text":"96451 - 1974 - Potential enviornmental impact of proposed water supply systems in Furnace Creek and Cow Creek, Death Valley National Monument","interactions":[],"lastModifiedDate":"2012-02-02T00:03:52","indexId":"96451","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Potential enviornmental impact of proposed water supply systems in Furnace Creek and Cow Creek, Death Valley National Monument","docAbstract":"No abstract available at this time","language":"English","usgsCitation":"Douglas, C.L., and Sanchez, P., 1974, Potential enviornmental impact of proposed water supply systems in Furnace Creek and Cow Creek, Death Valley National Monument, 17 p.","productDescription":"17 p.","startPage":"17","numberOfPages":"17","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":127118,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db68378d","contributors":{"authors":[{"text":"Douglas, C. L.","contributorId":64586,"corporation":false,"usgs":true,"family":"Douglas","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":299662,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sanchez, P.G.","contributorId":51678,"corporation":false,"usgs":true,"family":"Sanchez","given":"P.G.","email":"","affiliations":[],"preferred":false,"id":299661,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1013758,"text":"1013758 - 1974 - Effect of dietary biotin and lipid on growth, stamina, lipid metabolism and biotin-containing enzymes in brook trout (Salvelinus fontinalis)","interactions":[],"lastModifiedDate":"2025-02-27T17:16:03.513633","indexId":"1013758","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2403,"text":"Journal of Nutrition","active":true,"publicationSubtype":{"id":10}},"title":"Effect of dietary biotin and lipid on growth, stamina, lipid metabolism and biotin-containing enzymes in brook trout (Salvelinus fontinalis)","docAbstract":"Simultaneous dietary fat and biotin deficiencies in brook trout suppressed weight gain, feed/gain efficiency, swimming stamina, and total liver lipids. Dietary fat alone reduced body water, increased body fat and ash, reversed the elevating effect of biotin plus fat on liver palmitic and stearic acids, and widened the 16:0 to 16:1, 18:0 to 18:1, 18:2 to 20:4 and 18:3 to 22:5 liver fatty acid ratios. Fat also accentuated the accumulation of liver oleic and linoleic acids caused by biotin deprivation and apparently prevented docosapentaenoic acid biosynthesis in biotin-deprived trout. Fish fed fat with no biotin had the least, and those fed biotin with no fat the most, liver acetyl CoA carboxylase (ACC) and pyruvate carboxylase (PC) activities. Those fed neither supplemental biotin nor fat and those fed both showed equal liver ACC activity.
","language":"English","publisher":"Elsevier","doi":"10.1093/jn/104.3.315","usgsCitation":"Poston, H.A., and McCartney, T., 1974, Effect of dietary biotin and lipid on growth, stamina, lipid metabolism and biotin-containing enzymes in brook trout (Salvelinus fontinalis): Journal of Nutrition, v. 104, no. 3, p. 315-322, https://doi.org/10.1093/jn/104.3.315.","productDescription":"8 p.","startPage":"315","endPage":"322","numberOfPages":"8","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129290,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"104","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db62572d","contributors":{"authors":[{"text":"Poston, H. A.","contributorId":21893,"corporation":false,"usgs":true,"family":"Poston","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":319203,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCartney, T.H.","contributorId":70720,"corporation":false,"usgs":true,"family":"McCartney","given":"T.H.","email":"","affiliations":[],"preferred":false,"id":319204,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":37604,"text":"37604 - 1974 - Invertebrate macrobenthos of Lake Oahe, 1968-69","interactions":[],"lastModifiedDate":"2012-02-02T00:09:52","indexId":"37604","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":89,"text":"Technical Paper","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"73","title":"Invertebrate macrobenthos of Lake Oahe, 1968-69","docAbstract":"The benthos in Lake Oahe, as determined from about 450 bottom samples collected during the open water season in 1968 and 1969, was dominated by oligochaetes and chironomids; Caenis (Ephemeroptera) and Chaoborus (Diptera) were occasionally abundant. Total benthos was estimated at 3,600 organisms/mA? with an ash-free dry weight of about 2.2 g/mA? (about 33 kg/hectare dry weight). Estimated biomass was 1.3 g/mA? (about 18.5 kg/hectare dry weight) and depths of 0.5-10 m and 3.5 g/mA? (about 52.5 kg/hectare dry weight) at greater depths.","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"Out-of-print","usgsCitation":"Jones, W.E., and Selgeby, J.H., 1974, Invertebrate macrobenthos of Lake Oahe, 1968-69: Technical Paper 73, 11 p.","productDescription":"11 p.","startPage":"0","endPage":"11","numberOfPages":"11","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":164796,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":94273,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/uc1.31822006841605?urlappend=%3Bseq=89"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3e5fe4b0c8380cd63d0c","contributors":{"authors":[{"text":"Jones, William E.","contributorId":16883,"corporation":false,"usgs":true,"family":"Jones","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":218327,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Selgeby, James H.","contributorId":89828,"corporation":false,"usgs":true,"family":"Selgeby","given":"James","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":218328,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1689,"text":"wsp2033 - 1974 - Availability of ground water in the lower Pawcatuck River basin, Rhode Island","interactions":[],"lastModifiedDate":"2023-10-31T20:19:36.788644","indexId":"wsp2033","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","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":"2033","title":"Availability of ground water in the lower Pawcatuck River basin, Rhode Island","docAbstract":"The lower Pawcatuck River basin in southwestern Rhode Island is an area of about 169 square miles underlain by crystalline bedrock over which lies a relatively thin mantle of glacial till and stratified drift. Stratified drift, consisting dominantly of sand and gravel, occurs in irregularly shaped linear deposits that are generally less than a mile wide and less than 125 feet thick; these deposits are found along the Pawcatuck River, its tributaries, and abandoned preglacial channels. Deposits of stratified sand and gravel constitute the principal aquifer in the lower Pawcatuck basin and the only one capable of sustaining yields of 100 gallons per minute or more to individual wells. \r\n\r\nWater available for development in this aquifer consists of water in storage--potential ground-water runoff to streams--plus infiltration that can be induced from streams. Minimum annual ground-water runoff from the sand and gravel aquifer is calculated to be at least 1.17 cubic feet per second per square mile, or 0.76 million gallons per day per square mile. Potential recharge by induced infiltration is estimated to range from about 250 to 600 gallons per day per linear foot of streambed for the principal streams. In most areas, induced infiltration from streams constitutes the major source of water potentially available for development by wells. \r\n\r\nBecause subsurface hydraulic connection in the sand and gravel aquifer is poor in several places, the deposits are conveniently divisible into several ground-water reservoirs. The potential yield from five of the most promising ground-water reservoirs is evaluated by means of mathematical models. Results indicate that continuous withdrawals ranging from 1.3 to 10.3 million gallons per day, and totaling 31 million gallons per day, are obtainable from these reservoirs. Larger yields may be recovered by different well placement, spacing, construction and development, pumping practice, and so forth. \r\n\r\nWithdrawals at the rates indicated will reduce streamflow downstream from pumping centers but generally will not result in streams going dry, provided the water is returned to the basin. Export of water from the basin will require careful consideration of the effects of such withdrawals on low streamflow. Export from the Pawcatuck basin of 27 million gallons per day, estimated to be available from ground-water reservoirs in the upper Pawcatuck basin, in addition to 37.5 million gallons per day available in the lower Pawcatuck basin, will markedly reduce low streamflow. The 90-percent duration flow of the Pawcatuck River at Westerly would be reduced from 75 million gallons per day to perhaps as little as 21 million gallons per day. \r\n\r\nThe chemical quality of water from both the sand and gravel aquifer and associated streams is suitable for most purposes. The water is soft, slightly acidic, and typically has a dissolved-solids content of less than 75 milligrams per liter. Some treatment may be required locally for removal of iron and manganese to meet recommended standards of the U.S. Public Health Service for drinking water.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2033","usgsCitation":"Gonthier, J.B., Johnston, H.E., and Malmberg, G.T., 1974, Availability of ground water in the lower Pawcatuck River basin, Rhode Island: U.S. Geological Survey Water Supply Paper 2033, Report: iv, 40 p.; 5 Plates: 20.00 x 38.88 inches or smaller, https://doi.org/10.3133/wsp2033.","productDescription":"Report: iv, 40 p.; 5 Plates: 20.00 x 38.88 inches or smaller","costCenters":[],"links":[{"id":422303,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25524.htm","linkFileType":{"id":5,"text":"html"}},{"id":26771,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2033/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26769,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2033/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137039,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2033/report-thumb.jpg"},{"id":26773,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2033/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26772,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2033/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26774,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2033/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26770,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2033/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Rhode Island","otherGeospatial":"lower Pawcatuck River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -71.843,\n 41.667\n ],\n [\n -71.843,\n 41.345\n ],\n [\n -71.614,\n 41.345\n ],\n [\n -71.614,\n 41.667\n ],\n [\n -71.843,\n 41.667\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d91d","contributors":{"authors":[{"text":"Gonthier, Joseph B.","contributorId":74350,"corporation":false,"usgs":true,"family":"Gonthier","given":"Joseph","email":"","middleInitial":"B.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":143976,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnston, Herbert E.","contributorId":16392,"corporation":false,"usgs":true,"family":"Johnston","given":"Herbert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":143975,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Malmberg, Glenn T.","contributorId":11196,"corporation":false,"usgs":true,"family":"Malmberg","given":"Glenn","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":143974,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1014366,"text":"1014366 - 1974 - Yield of channel catfish and composition of effluents from shallow-water raceways","interactions":[],"lastModifiedDate":"2025-08-05T16:26:17.960045","indexId":"1014366","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Yield of channel catfish and composition of effluents from shallow-water raceways","docAbstract":"No abstract available.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1974)36[46:YOCCAC]2.0.CO;2","usgsCitation":"Tackett, D.L., 1974, Yield of channel catfish and composition of effluents from shallow-water raceways: Progressive Fish-Culturist, v. 36, no. 1, p. 46-48, https://doi.org/10.1577/1548-8659(1974)36[46:YOCCAC]2.0.CO;2.","productDescription":"3 p.","startPage":"46","endPage":"48","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129615,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"36","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de42c","contributors":{"authors":[{"text":"Tackett, Dewey L.","contributorId":8024,"corporation":false,"usgs":true,"family":"Tackett","given":"Dewey","middleInitial":"L.","affiliations":[],"preferred":false,"id":320258,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1001620,"text":"1001620 - 1974 - Feeding ecology of pintail hens during reproduction","interactions":[],"lastModifiedDate":"2018-01-02T10:52:24","indexId":"1001620","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3544,"text":"The Auk","onlineIssn":"1938-4254","printIssn":"0004-8038","active":true,"publicationSubtype":{"id":10}},"title":"Feeding ecology of pintail hens during reproduction","docAbstract":"Food supply has been acknowledged as one of eight major external factors regulating the sexual cycles of birds (Marshall 1961). Several hypotheses have been advanced to explain the role of food supply as an ultimate factor regulating breeding (Marshall 1951; Lack 1954, 1968; Wynne-Edwards 1962; and others). Another potential influence of food is its being a proximate stimulus to breeding. When certain foods become available they may act as a stimulus as the female requires them to meet her dietary needs during egg formation. Lack (1966a: 24) suggested that the average date of laying by the Great Tit (Parus major) probably resulted from a correlation between spring temperatures and the time of appearance of the insect foods the adult females need to form eggs. He also cited other passerines whose breeding was affected by food supply available to the female. In waterfowl it has been suggested that laying females require invertebrate foods (Moyle 1961, Leitch 1964). If true, this implies that the timing of laying is influenced by those environmental changes that affect food supply.
The Pintail (Anas acuta) lives primarily on plant foods during much of the year (Martin et al. 1951); thus a study of feeding ecology during the nesting season provided an opportunity to evaluate the significance of an invertebrate food source to females during the period of egg formation. Marshall (1951) stated that essentially vegetarian species appear compelled to switch at least partially to a heavier protein diet when feeding their developing young. Production of a clutch of eggs, like tissue growth in the young, requires a special dietary need that presumably should be reflected in the diet of vegetarian species during the period that eggs are being formed. This paper describes the diet of the female Pintail prior to, during, and after laying and discusses the impact of certain environmental and physiological changes on Pintail breeding.
Studies of the effect of dissolved salts on the oxygen isotope activity ratio of water have been extended to 275°C. Dehydrated salts were added to water of known isotope composition and the solutions were equilibrated with CO2 which was sampled for analysis. For comparison similar studies were made using pure water. Results on water nearly coincide with earlier calculations. Salt effects diminish with increasing temperature only for solutions of MgCl2 and LiCl. Other salt solutions show complex behavior due to the temperature-dependent formation of ion pairs of changing character. Equilibrium fractionations (103 ln α) between 1 molal solutions and pure water at 25, 100, and 275°C are: NaCl 0.0, −1.5, +1.0; KCl 0.0, −1.0, +2.0; LiCl −1.0, −0.6, −0.5; CaCl2 −0.4, −1.8, +0.8; MgCl2 −1.1, −0.7, −0.3; MgSO4 −1.1, +0.1, −; NaF (0.8 m) 0.0, −1.5, −0.3; and NH4Cl (0.55 m) 0.0, −1.2, −1.3. These effects are significant in the isotope study of hot saline fluids responsible for ore deposition and of fluids found in certain geothermal systems. Minor modification of published isotope geothermometers may be required.
The implication by Murthy and Ferrell (1972)that interstitial water studies are in a confused state is criticized on the basis that the authors have not drawn on a considerable body of data, especially Soviet studies since the 1950's, and results of the Deep Sea Drilling Project. Pressure filtration systems for extracting interstitial waters are currently the methods of choice for marine studies and have achieved substantial reliability and reproducibility. Although gaps and problems remain, many aspects of interstitial composition of marine sediments have been clarified; these include the substantial constancy of composition of interstitial waters in deep sea pelagic deposits, depletion of interstitial cations owing to authigenic mineral formation in more rapidly accumulated (especially terrigenous) sediments, and special phenomena in sediments overlying salt deposits.
","language":"English","publisher":"The Clay Minerals Society","doi":"10.1346/CCMN.1974.0220404","usgsCitation":"Manheim, F., 1974, Comparative studies on extraction of sediment interstitial waters: Discussion and comment on the current state of interstitial water studies: Clays and Clay Minerals, v. 22, no. 4, p. 337-343, https://doi.org/10.1346/CCMN.1974.0220404.","productDescription":"7 p.","startPage":"337","endPage":"343","costCenters":[],"links":[{"id":218771,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"4","noUsgsAuthors":false,"publicationDate":"2024-07-01","publicationStatus":"PW","scienceBaseUri":"5059f828e4b0c8380cd4cef7","contributors":{"authors":[{"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":357772,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70009751,"text":"70009751 - 1974 - Erosion by catastrophic floods on Mars and Earth","interactions":[],"lastModifiedDate":"2025-02-28T16:47:07.608559","indexId":"70009751","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Erosion by catastrophic floods on Mars and Earth","docAbstract":"The large Martian channels, especially Kasei, Ares, Tiu, Simud, and Mangala Valles, show morphologic features strikingly similar to those of the Channeled Scabland of eastern Washington, produced by the catastrophic breakout floods of Pleistocene Lake Missoula. Features in the overall pattern include the great size, regional anastomosis, and low sinuosity of the channels. Erosional features are streamlined hills, longitudinal grooves, inner channel cataracts, scour upstream of flow obstacles, and perhaps marginal cataracts and butte and basin topography. Depositional features are bar complexes in expanding reaches and perhaps pendant bars and alcove bars. Scabland erosion takes place in exceedingly deep, swift floodwater acting on closely jointed bedrock as a hydrodynamic consequence of secondary flow phenomena, including various forms of macroturbulent votices and flow separations. If the analogy to the Channeled Scabland is correct, floods involving water discharges of millions of cubic meters per second and peak flow velocities of tens of meters per second, but perhaps lasting no more than a few days, have occurred on Mars.