No abstract available
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The alloy system is calibrated against pure sulfur. The method has the following advantages: simple apparatus; ability to cover a large range of fugacity of S2; ability to cover a large temperature range by permitting runs of long duration; ability to tolerate other components in the gas phase; and ease of recovery of the quenched charges for determinations of phases and compositions. Results obtained by the electrum-tarnish method are in satisfactory agreement with those obtained by other workers for the fs2 vs. T curves for the assemblage Ni(1–x)S + NiS2. The electrum-tarnish method shows promise for investigating many other reactions.
Univariant reactions studied by this method can be represented as lines forming a genetic grid in terms of the environmental parameters fs2 and T, The slopes of such lines can yield valuable thermodynamic data for the phases involved, but activity coefficients must be known for phases of variable composition.
","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(64)90082-1","issn":"00167037","usgsCitation":"Barton, P.B., and Toulmin, P., 1964, The electrum-tarnish method for the determination of the fugacity of sulfur in laboratory sulfide systems: Geochimica et Cosmochimica Acta, v. 28, no. 5, p. 619-640, https://doi.org/10.1016/0016-7037(64)90082-1.","productDescription":"22 p.","startPage":"619","endPage":"640","numberOfPages":"22","costCenters":[],"links":[{"id":218902,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505babc5e4b08c986b323069","contributors":{"authors":[{"text":"Barton, P. B. 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","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1964)26[11:COVMOH]2.0.CO;2","usgsCitation":"Larsen, H., 1964, Comparison of various methods of hemoglobin determination on catfish blood: Progressive Fish-Culturist, v. 26, no. 1, p. 11-15, https://doi.org/10.1577/1548-8659(1964)26[11:COVMOH]2.0.CO;2.","productDescription":"5 p.","startPage":"11","endPage":"15","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":130248,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ee4b07f02db6aa765","contributors":{"authors":[{"text":"Larsen, H.N.","contributorId":101601,"corporation":false,"usgs":true,"family":"Larsen","given":"H.N.","email":"","affiliations":[],"preferred":false,"id":318990,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":34017,"text":"b1141M - 1964 - Geology of the Jarbidge quadrangle, Nevada-Idaho","interactions":[],"lastModifiedDate":"2023-03-09T21:23:29.638612","indexId":"b1141M","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1141","chapter":"M","title":"Geology of the Jarbidge quadrangle, Nevada-Idaho","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1141M","usgsCitation":"Coats, R.R., 1964, Geology of the Jarbidge quadrangle, Nevada-Idaho: U.S. Geological Survey Bulletin 1141, Report: iii, 24 p.; 1 Plate: 23.93 x 26.56 inches, https://doi.org/10.3133/b1141M.","productDescription":"Report: iii, 24 p.; 1 Plate: 23.93 x 26.56 inches","costCenters":[],"links":[{"id":164413,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1141m/report-thumb.jpg"},{"id":92549,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1141m/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":92548,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1141m/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":109400,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20871.htm","linkFileType":{"id":5,"text":"html"},"description":"20871"}],"country":"United States","state":"Idaho, Nevada","otherGeospatial":"Jarbidge quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -115.5,\n 42\n ],\n [\n -115.5,\n 41.75\n ],\n [\n -115.25,\n 41.75\n ],\n [\n -115.25,\n 42\n ],\n [\n -115.5,\n 42\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67fe6d","contributors":{"authors":[{"text":"Coats, Robert Roy","contributorId":77131,"corporation":false,"usgs":true,"family":"Coats","given":"Robert","email":"","middleInitial":"Roy","affiliations":[],"preferred":false,"id":212325,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2233,"text":"wsp1779C - 1964 - Chemical quality of surface water in the West Branch Susquehanna River basin, Pennsylvania","interactions":[],"lastModifiedDate":"2023-03-22T18:45:31.751873","indexId":"wsp1779C","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","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":"1779","chapter":"C","title":"Chemical quality of surface water in the West Branch Susquehanna River basin, Pennsylvania","docAbstract":"The West Branch Susquehanna River is 228 miles long and drains 6,913 square miles of mountainous area in central Pennsylvania. Much of this area is forestcovered wilderness, part of which is reserved as State game land. Wild animals, such as deer, bear, turkey and grouse, are sheltered there, and many streams contain trout and other game fish. This helps to make the region one of the best hunting and fishing areas in Pennsylvania. The Congress has approved Federal funds for the construction of several reservoirs to prevent flooding of the main river and several of its tributaries. Water stored behind the dams will not be withdrawn below a minimum level designated as conservation pools. These pools will be available for recreation. Several headwater streams, such as Clearfield, Moshannon, and at times Sinnemahoning Creek, that carry drainage from coal mines are acid and contain high concentrations of dissolved solids, especially sulfates. These streams acidify the West Branch Susquehanna River downstream as far as Jersey Shore. One of the most influential tributaries affecting the quality of the West Branch Susquehanna River after they merge is Bald Eagle Creek. Bald Eagle Creek enters the main river downstream from Lock Haven which is approximately 100 river miles from the river's source. Because of its alkaline properties, water of Bald Eagle Creek can neutralize acidic water. Many streams draining small areas and several draining large areas such as Pine Creek, Lycoming Creek, and Loyalsock Creek are clear nearly neutral water low in dissolved solids whose pH is about 7.0 most of the time. These streams have a diluting and neutralizing effect on the quality of the West Branch Susquehanna River, so that from Williamsport downstream the river water is rarely acid, and for most of the time it is of good chemical quality.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1779C","usgsCitation":"McCarren, E.F., 1964, Chemical quality of surface water in the West Branch Susquehanna River basin, Pennsylvania: U.S. Geological Survey Water Supply Paper 1779, Report; iv, 40 p.; 1 Plate: 21.00 x 16.62 inches, https://doi.org/10.3133/wsp1779C.","productDescription":"Report; iv, 40 p.; 1 Plate: 21.00 x 16.62 inches","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":27992,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1779c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414560,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24956.htm","linkFileType":{"id":5,"text":"html"}},{"id":27991,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137748,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1779c/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania","otherGeospatial":"Susquehanna River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -78.667,\n 41.75\n ],\n [\n -78.667,\n 40.583\n ],\n [\n -76.25,\n 40.583\n ],\n [\n -76.25,\n 41.75\n ],\n [\n -78.667,\n 41.75\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3b11","contributors":{"authors":[{"text":"McCarren, Edward F.","contributorId":106472,"corporation":false,"usgs":true,"family":"McCarren","given":"Edward","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":144863,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2354,"text":"wsp1654 - 1964 - Ground water for irrigation in the Snake River Basin in Idaho","interactions":[],"lastModifiedDate":"2023-03-24T18:32:01.922661","indexId":"wsp1654","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","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":"1654","title":"Ground water for irrigation in the Snake River Basin in Idaho","docAbstract":"The Snake River basin, in southern Idaho, upstream from the mouth of the Powder River in Oregon, includes more than 50 percent of the land area and 65 percent of the total population of the State. More than 2.5 million acres of land is irrigated ; irrigation agriculture and industry allied with agriculture are the basis of the economy of the basin. Most of the easily developed sources of surface water are fully utilized, and few storage sites remain where water could be made available to irrigate lands under present economic conditions. Because surface-water supplies have be come more difficult to obtain, use of ground water has increased greatly. At the present time (1959), about 600,000 acres of land is irrigated with ground water. Ground-water development has been concentrated in areas where large amounts of water are available beneath or adjacent to tracts of arable land and where the depth to water is not excessive under the current economy. Under these criteria, many of the most favorable areas already have been developed; however, tremendous volumes of water are still available for development. In some places, water occurs at depths considered near or beyond the limit for economic recovery, whereas in some other places, water is reasonably close to the surface but no arable land is available in the vicinity. In other parts of the basin large tracts of arable land are without available water supply. Thus the chief tasks in development of the ground-water resources include not only locating and evaluating ground-water supplies but also the planning necessary to bring the water to the land. Irrigation began in the 1860's ; at the present time more than 10 million acre feet of surface water, some of which is recirculated water, is diverted annually for irrigation of more than 2.5 million acres. Diversion of this large quantity of water has had a marked effect on the ground-water regimen. In some areas, the water table has risen more than 100 feet and the discharge of some springs has more than doubled. Large-scale development of ground water began after World War II, and it is estimated that in 1959 about 1,500,000 acre-feet of ground water was pumped for irrigation of the 600,000 acres irrigated wholly with ground water in addition to a substantial amount of ground water pumped to supplement surface-water supplies. Ground water is also the principal source of supply for municipal, industrial, and domestic use. The water regimen in the Snake River basin is greatly influenced by the geology. The rocks forming the mountains are largely consolidated rocks of low permeability; however, a fairly deep and porous subsoil has formed on them by decay and disintegration of the parent rock. Broad intermontane valleys and basins are partly filled with alluvial sand and gravel. The subsoil and alluvial materials are utilized very little as a source of water supply but are important as seasonal ground-water reservoirs because they store water during periods of high rainfall and snowmelt. Discharge from these reservoirs maintains stream flow during periods of surface runoff. Because these aquifers are fairly thin, they drain rapidly and are considerably depleted at the end of each dry cycle. The plain and plateau areas and tributary valleys, on the other hand, are underlain chiefly by rocks of high permeability and porosity. These rocks, mostly basaltic lava flows and alluvial materials, constitute a reservoir which fluctuates only slightly from season to season. Large amounts' of water are withdrawn from them for irrigation and other uses, and discharge from the Snake Plain aquifer is an important part of the total flow of the Snake River downstream from Hagerman Valley. The ultimate source of ground water in the basin is precipitation on the basin. In the mountainous areas, aquifers mostly are recharged directly by precipitation.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1654","usgsCitation":"Mundorff, M.J., Crosthwaite, E., and Kilburn, C., 1964, Ground water for irrigation in the Snake River Basin in Idaho: U.S. Geological Survey Water Supply Paper 1654, vii, 224 p., https://doi.org/10.3133/wsp1654.","productDescription":"vii, 224 p.","costCenters":[],"links":[{"id":414716,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24846.htm","linkFileType":{"id":5,"text":"html"}},{"id":28283,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1654/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137782,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1654/report-thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Snake River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -111.048,\n 45.217\n ],\n [\n -117.213,\n 45.217\n ],\n [\n -117.213,\n 42\n ],\n [\n -111.048,\n 42\n ],\n [\n -111.048,\n 45.217\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dc28","contributors":{"authors":[{"text":"Mundorff, Maurice John","contributorId":41404,"corporation":false,"usgs":true,"family":"Mundorff","given":"Maurice","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":145067,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crosthwaite, E. G.","contributorId":83098,"corporation":false,"usgs":true,"family":"Crosthwaite","given":"E. G.","affiliations":[],"preferred":false,"id":145068,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kilburn, Chabot","contributorId":83499,"corporation":false,"usgs":true,"family":"Kilburn","given":"Chabot","email":"","affiliations":[],"preferred":false,"id":145069,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70175640,"text":"70175640 - 1964 - Records of precipitation, aquifer head, and ground-water recharge to the Edwards and associated limestones, San Antonio area, Texas, 1963","interactions":[],"lastModifiedDate":"2016-08-17T14:12:09","indexId":"70175640","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","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":"6","title":"Records of precipitation, aquifer head, and ground-water recharge to the Edwards and associated limestones, San Antonio area, Texas, 1963","docAbstract":"No abstract available.
","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Garza, S., 1964, Records of precipitation, aquifer head, and ground-water recharge to the Edwards and associated limestones, San Antonio area, Texas, 1963: Edwards Underground Water District Bulletin 6, 7 p.","productDescription":"7 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326726,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58b56e4b03bcb0104bc3f","contributors":{"authors":[{"text":"Garza, Sergio","contributorId":88713,"corporation":false,"usgs":true,"family":"Garza","given":"Sergio","email":"","affiliations":[],"preferred":false,"id":645907,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010464,"text":"70010464 - 1964 - Minor-element composition and organic carbon content of marine and nonmarine shales of Late Cretaceous age in the western interior of the United States","interactions":[],"lastModifiedDate":"2020-11-24T00:56:34.558115","indexId":"70010464","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Minor-element composition and organic carbon content of marine and nonmarine shales of Late Cretaceous age in the western interior of the United States","docAbstract":"The composition of nonmarine shales of Cretaceous age that contain less than 1 per cent organic carbon is assumed to represent the inherited minor-element composition of clayey sediments delivered to the Cretaceous sea that occupied the western interior region of North America. Differences in minor-element content between these samples and samples of
(a) nonmarine carbonaceous shales (1 to 17 per cent organic carbon),
(b) nearshore marine shales (less than 1 per cent organic carbon), and
(c) offshore marine shales (as much as 8 per cent organic carbon), all of the same age, reveal certain aspects of the role played by clay minerals and organic materials in affecting the minor-element composition of the rocks.
The organic carbon in the nonmarine rocks occurs in disseminated coaly plant remains. The organic carbon in the marine rocks occurs predominantly in humic material derived from terrestrial plants. The close similarity in composition between the organic isolates from the marine samples and low-rank coal suggests that the amount of marine organic material in these rocks is small.
The minor-element content of the two kinds of nonmarine shales is the same despite the relatively large amount of organic carbon in the carbonaceous shales. The nearshore marine shales, however, contain larger median amounts of arsenic, boron, chromium, vanadium and zinc than do the nonmarine rocks; and the offshore marine shales contain even larger amounts of these elements. Cobalt, molybdenum, lead and zirconium show insignificant differences in median content between the nonmarine and marine rocks, although as much as 25 ppm molybdenum is present in some offshore marine samples. The gallium content is lower in the marine than in the nonmarine samples. Copper and selenium contents of the two kinds of nonmarine rocks and the nearshore marine samples are the same, but those of the offshore samples are larger.
In general, arsenic, chromium, copper, molybdenum, selenium, vanadium and zinc are concentrated in those offshore marine samples having the largest amounts of organic carbon, but samples with equal amounts of vanadium, for instance, may differ by a factor of 3 in their amount of organic carbon. Arsenic and molybdenum occur in some samples chiefly in syngenetic pyrite but also are present in relatively large amounts in samples that contain little pyrite.
The data on nonmarine carbonaceous shales indicate that organic matter of terrestrial origin in marine shales contributes little to the minor-element content of such rocks. It is possible that marine organic matter, even though seemingly small in amount in marine shales, contributes to the minor-element composition of the shales. In addition to any such contribution, however, the great effectiveness in sorption processes of humic materials in conjunction with clay minerals suggests that such processes must have played an important role as these materials moved from the relatively dilute solutions of the nonmarine environment to the relatively concentrated solution of sea water. The volumes of sea water sufficient to supply for sorption the amounts of most minor elements in the offshore marine samples are insignificant compared to the volumes of water with which the clay and organic matter were in contact during their transportation and sedimentation. Consequently, the chemical characteristics of the environment in which the clay minerals and organic matter accumulated and underwent diagenesis probably were the most important factors in controlling the degree to which sorption processes and the formation of syngenetic minerals affected the final composition of the rocks.
","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(64)90008-0","issn":"00167037","usgsCitation":"Tourtelot, H.A., 1964, Minor-element composition and organic carbon content of marine and nonmarine shales of Late Cretaceous age in the western interior of the United States: Geochimica et Cosmochimica Acta, v. 28, no. 10-11, p. 1579-1604, https://doi.org/10.1016/0016-7037(64)90008-0.","productDescription":"26 p.","startPage":"1579","endPage":"1604","numberOfPages":"26","costCenters":[],"links":[{"id":219008,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"10-11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5b29e4b0c8380cd6f38b","contributors":{"authors":[{"text":"Tourtelot, H. A.","contributorId":79140,"corporation":false,"usgs":true,"family":"Tourtelot","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":358984,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1014052,"text":"1014052 - 1964 - Pseudomonadales as fish pathogens","interactions":[],"lastModifiedDate":"2012-02-02T00:04:22","indexId":"1014052","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1385,"text":"Developments in Industrial Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Pseudomonadales as fish pathogens","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Developments in Industrial Microbiology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"143a/FH","usgsCitation":"Bullock, G.L., 1964, Pseudomonadales as fish pathogens: Developments in Industrial Microbiology, v. 5, p. 101-108.","productDescription":"p. 101-108","startPage":"101","endPage":"108","numberOfPages":"8","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131457,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8ae4b07f02db651509","contributors":{"authors":[{"text":"Bullock, G. L.","contributorId":69498,"corporation":false,"usgs":true,"family":"Bullock","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":319689,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000274,"text":"1000274 - 1964 - A horizontal sampler for collection of water samples near the bottom","interactions":[],"lastModifiedDate":"2013-01-28T12:31:27","indexId":"1000274","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2620,"text":"Limnology and Oceanography","active":true,"publicationSubtype":{"id":10}},"title":"A horizontal sampler for collection of water samples near the bottom","docAbstract":"The need to obtain adequate water samples immediately above a lake bottom or at a precisely defined depth is not new. The problem is of particular concern in a large section of central Lake Erie, where dissolved oxygen concentration may be reduced to 1 ppm or less in the hypolimnion and where the metalimnion frequently extends to or within 30 or 60 cm of the bottom (Becton 1963; Cam 1962).It is impossible to sample the hypolimnrtic waters satisfactorily with the usual Nanscn, Kemmerer, and Frautschy bottles (Carr 1962). Although the 500-ml sampler described here was designed, constructed, and used extensively and successfully to meet the particular problem in Lake Erie, it should be equally useful in a varirty of situations.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Limnology and Oceanography","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.4319/lo.1964.9.4.0595","collaboration":"Out-of-print","usgsCitation":"Joeris, L.S., 1964, A horizontal sampler for collection of water samples near the bottom: Limnology and Oceanography, v. 9, no. 4, p. 595-598, https://doi.org/10.4319/lo.1964.9.4.0595.","productDescription":"p. 595-598","startPage":"595","endPage":"598","numberOfPages":"3","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128923,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266600,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.4319/lo.1964.9.4.0595"}],"volume":"9","issue":"4","noUsgsAuthors":false,"publicationDate":"2003-12-22","publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae44c","contributors":{"authors":[{"text":"Joeris, Leonard S.","contributorId":104430,"corporation":false,"usgs":true,"family":"Joeris","given":"Leonard","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":308322,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":85379,"text":"85379 - 1964 - Honkers large and small","interactions":[],"lastModifiedDate":"2012-02-02T00:04:02","indexId":"85379","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Honkers large and small","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Waterfowl tomorrow","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, DC","usgsCitation":"Hansen, H., and Nelson, H., 1964, Honkers large and small, chap. of Waterfowl tomorrow, p. 109-124 [770 pp.].","productDescription":"p. 109-124 [770 pp.]","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":128684,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62beb1","contributors":{"editors":[{"text":"Linduska, J.P.","contributorId":64308,"corporation":false,"usgs":true,"family":"Linduska","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":504455,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Hansen, H.A.","contributorId":23486,"corporation":false,"usgs":true,"family":"Hansen","given":"H.A.","email":"","affiliations":[],"preferred":false,"id":295981,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nelson, H.K.","contributorId":21489,"corporation":false,"usgs":true,"family":"Nelson","given":"H.K.","email":"","affiliations":[],"preferred":false,"id":295980,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":93717,"text":"93717 - 1964 - Lamprey control and research in the United States","interactions":[],"lastModifiedDate":"2023-04-06T16:47:55.123277","indexId":"93717","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Lamprey control and research in the United States","docAbstract":"No abstract available.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Great Lakes Fishery Commission Annual Report, 1963","largerWorkSubtype":{"id":9,"text":"Other Report"},"language":"English","usgsCitation":"Smith, B.R., 1964, Lamprey control and research in the United States, 12 p.","productDescription":"12 p.","startPage":"30","endPage":"41","numberOfPages":"12","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128462,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":415348,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.glfc.org/annual-reports.php","linkFileType":{"id":5,"text":"html"}}],"country":"United States","otherGeospatial":"Great Lakes","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -93.714444842021,\n 48.48770654175058\n ],\n [\n -93.714444842021,\n 39.19355786261647\n ],\n [\n -75.03922973389709,\n 39.19355786261647\n ],\n [\n -75.03922973389709,\n 48.48770654175058\n ],\n [\n -93.714444842021,\n 48.48770654175058\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b0daa","contributors":{"authors":[{"text":"Smith, Bernard R.","contributorId":38924,"corporation":false,"usgs":true,"family":"Smith","given":"Bernard","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":297815,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000302,"text":"1000302 - 1964 - Role of zooplankton in the freshwater strontium cycle and influence of dissolved salts","interactions":[],"lastModifiedDate":"2025-01-06T16:24:18.157908","indexId":"1000302","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2017,"text":"International Association of Theoretical and Applied Limnology","active":true,"publicationSubtype":{"id":10}},"title":"Role of zooplankton in the freshwater strontium cycle and influence of dissolved salts","docAbstract":"No abstract available.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/03680770.1962.11895588","usgsCitation":"Marshall, J., Beeton, A.M., and Chandler, D., 1964, Role of zooplankton in the freshwater strontium cycle and influence of dissolved salts: International Association of Theoretical and Applied Limnology, v. 15, no. 2, p. 665-672, https://doi.org/10.1080/03680770.1962.11895588.","productDescription":"8 p.","startPage":"665","endPage":"672","numberOfPages":"7","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":130333,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fe215","contributors":{"authors":[{"text":"Marshall, J.S.","contributorId":74712,"corporation":false,"usgs":true,"family":"Marshall","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":308362,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beeton, Alfred M.","contributorId":94247,"corporation":false,"usgs":true,"family":"Beeton","given":"Alfred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":308363,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chandler, D.C.","contributorId":58600,"corporation":false,"usgs":true,"family":"Chandler","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":308361,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1000110,"text":"1000110 - 1964 - Life history of lake herring in Lake Superior","interactions":[],"lastModifiedDate":"2012-03-02T17:16:05","indexId":"1000110","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1663,"text":"Fishery Bulletin","printIssn":"0090-0656","active":true,"publicationSubtype":{"id":10}},"title":"Life history of lake herring in Lake Superior","docAbstract":"The average annual commercial catch of lake herring (Coregonus artedi) in U.S. waters of Lake Superior was nearly 12 million pounds in 1929-61. This production contributed 62.4 percent of the total U.S. take of lake herring for the Great Lakes. About 90 percent of the annual catch is taken from small-mesh gill nets during the November-December spawning season.\rThe life-history studies were based on 12,187 fish collected in 1950-62; past growth was computed for 3,779 specimens collected from commercial landings at: Duluth, Minn.; Bayfield, Wis.; and Portage Entry and Marquette, Mich.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Fishery Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"Out-of-print","usgsCitation":"Dryer, W.R., and Beil, J., 1964, Life history of lake herring in Lake Superior: Fishery Bulletin, v. 63, no. 3, p. 493-530.","productDescription":"p. 493-530","startPage":"493","endPage":"530","numberOfPages":"37","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":131582,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"63","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a5411","contributors":{"authors":[{"text":"Dryer, William R.","contributorId":71921,"corporation":false,"usgs":true,"family":"Dryer","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":308090,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beil, Joseph","contributorId":82658,"corporation":false,"usgs":true,"family":"Beil","given":"Joseph","email":"","affiliations":[],"preferred":false,"id":308091,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":93789,"text":"93789 - 1964 - The value of soil bank lands to breeding prairie grouse","interactions":[],"lastModifiedDate":"2017-12-29T13:11:54","indexId":"93789","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"The value of soil bank lands to breeding prairie grouse","docAbstract":"No abstract available.
","language":"English","publisher":"Bureau of Sport Fisheries and Wildlife; U.S. Geological Survey Northern Prairie Wildlife Research Center","publisherLocation":"Jamestown, ND","usgsCitation":"Kirsch, L., 1964, The value of soil bank lands to breeding prairie grouse, 5 p.","productDescription":"5 p.","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":128184,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62f3cc","contributors":{"authors":[{"text":"Kirsch, L.M.","contributorId":43701,"corporation":false,"usgs":true,"family":"Kirsch","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":297924,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000165,"text":"1000165 - 1964 - Feeding by three species of fishes on the eggs of spawning alewives","interactions":[],"lastModifiedDate":"2023-12-06T12:17:00.18758","indexId":"1000165","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1337,"text":"Copeia","active":true,"publicationSubtype":{"id":10}},"title":"Feeding by three species of fishes on the eggs of spawning alewives","docAbstract":"No abstract available.
","language":"English","publisher":"American Society of Ichthyologists and Herpetologists (ASIH)","doi":"10.2307/1440867","usgsCitation":"Edsall, T.A., 1964, Feeding by three species of fishes on the eggs of spawning alewives: Copeia, v. 1964, no. 1, p. 226-227, https://doi.org/10.2307/1440867.","productDescription":"2 p.","startPage":"226","endPage":"227","numberOfPages":"2","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":130364,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1964","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635ebf","contributors":{"authors":[{"text":"Edsall, Thomas A.","contributorId":84302,"corporation":false,"usgs":true,"family":"Edsall","given":"Thomas","email":"","middleInitial":"A.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":false,"id":308173,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}