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,{"id":875,"text":"875 - 1965 - Water resources data for Tennessee","interactions":[],"lastModifiedDate":"2014-08-06T09:32:28","indexId":"875","displayToPublicDate":"1965-01-01T09:31:19","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data for Tennessee","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Nashville, TN","doi":"10.3133/875","issn":"0163-9447","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1965, Water resources data for Tennessee, https://doi.org/10.3133/875.","costCenters":[],"links":[{"id":291756,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Tennessee","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90.3103,34.9829 ], [ -90.3103,36.678 ], [ -81.6469,36.678 ], [ -81.6469,34.9829 ], [ -90.3103,34.9829 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e3415ae4b0567f277019a6","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":527794,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70048263,"text":"70048263 - 1965 - Directional hydraulic behavior of a fractured-shale aquifer in New Jersey","interactions":[],"lastModifiedDate":"2021-02-17T22:57:35.415612","indexId":"70048263","displayToPublicDate":"1965-01-01T09:15:00","publicationYear":"1965","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Directional hydraulic behavior of a fractured-shale aquifer in New Jersey","docAbstract":"The principal source of ground water throughout a large part of central and northeastern New Jersey is the aquifer in the Brunswick Shale -- the youngest unity of the Newark Group of Triassic Age.  Large-diameter public-supply and industrial wells tapping the Brunswick Shale commonly yield several hundred gallons per minute each.  Virtually all ground water in this aquifer occurs in interconnecting fractures; the formation has practically no effective primary porosity.  Numerous pumping tests have shown that the aquifer exhibits directional, rather than isotropic, hydraulic behavior.  Water levels in wells alined along the strike of the formation show greater magnitude of interference than those in wells alined in transverse directions.  Drawdown data evaluated by standard time-drawdown methods indicate computed coefficient of transmissibility in all cases is least in the direction of strike.  Because of the distribution of observation wells available for the tests, distance-drawdown methods of evaluation could be used in only one instance -- for just one direction; the computed coefficient compared favorably with that calculated from the time-drawdown method.  Computed values of transmissibility may be unreliable owing to the departure of the aquifer from the ideal model.  It is even possible that the direction of minimum computed transmissiblity is actually indicative of the alinement of fractures with the greatest permeability.  However, the relation of the directional behavior to the structure of the formation has practical significance when locating the new wells near existing wells.  Well interference can be greatly minimized, generally, by alining wells perpendicular to the strike.","largerWorkTitle":"Proceedings of the international symposium on hydrology of fractured rocks","conferenceTitle":"International Symposium on Hydrology of Fractured Rocks","conferenceDate":"October 1965","conferenceLocation":"Dubrovnik, Croatia","language":"English","publisher":"International Association of Scientific Hydrology","usgsCitation":"Vecchioli, J., 1965, Directional hydraulic behavior of a fractured-shale aquifer in New Jersey, <i>in</i> Proceedings of the international symposium on hydrology of fractured rocks, Dubrovnik, Croatia, October 1965, 9 p.","productDescription":"9 p.","numberOfPages":"9","costCenters":[],"links":[{"id":277842,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Jersey","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.2082,40.2451 ], [ -75.2082,41.3574 ], [ -73.9931,41.3574 ], [ -73.9931,40.2451 ], [ -75.2082,40.2451 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523c1ce6e4b024b60d4072a3","contributors":{"authors":[{"text":"Vecchioli, John","contributorId":36113,"corporation":false,"usgs":true,"family":"Vecchioli","given":"John","email":"","affiliations":[],"preferred":false,"id":484210,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2000027,"text":"2000027 - 1965 - Experimental control of sea lampreys with electricity on the south shore of Lake Superior, 1953-60","interactions":[],"lastModifiedDate":"2012-02-02T00:14:56","indexId":"2000027","displayToPublicDate":"1965-01-01T01:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":222,"text":"Technical Report","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"10","title":"Experimental control of sea lampreys with electricity on the south shore of Lake Superior, 1953-60","docAbstract":"Experimental control of the sea lamprey, Petromyzon marinus, with electric barriers was begun in Lake Superior in 1953. Electrical devices were the most practical and promising method of control then available. Installed below spawning grounds in streams and rivers tributary to Lake Superior, these barriers were designed to prevent the sexually mature sea lampreys from reproducing.\nThe catch of sea lampreys at the electric barriers increased rapidly from 1,668 in 1953 to 66,931 in 1958. The total catches dropped substantially in 1959 and 1960 to 52,173 and 39,783, respectively.\nElectric fields of sufficient intensity to block sea lampreys were potentially lethal to other fish and caused undesirable mortality. Improvements in design and installation, and the development of a direct-current diversion device reduced the mortality and increased the efficiency of operation.\nThe development of control by selective chemicals in 1958 superseded the barrier control system which was terminated at the end of the 1960 season.\nThe electric barrier operation provided considerable information on mature sea lampreys, including data on time of migration, length, weight, and sex composition.\nElectric devices of the type and design used are capable of blocking entire runs of adult sea lampreys. An accurate appraisal of the effectiveness of the barrier system is impossible, however. Most of the barriers were not operated long enough to reduce the contribution of parasites from the streams. Furthermore, a complete system of efficient electric barriers was never realized. The greatest weakness of this method of control lies in maintenance of the units in continuous, uninterrupted operation through consecutive migratory seasons.","language":"English","publisher":"Great Lakes Fishery Commission","collaboration":"Out-of-print","usgsCitation":"McLain, A.L., Smith, B.R., and Moore, H.H., 1965, Experimental control of sea lampreys with electricity on the south shore of Lake Superior, 1953-60: Technical Report 10, 48 p.","productDescription":"48 p.","startPage":"0","endPage":"48","numberOfPages":"48","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198773,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":92066,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.glfc.org/pubs/TechReports/Tr10.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9400","contributors":{"authors":[{"text":"McLain, Alberton L.","contributorId":15561,"corporation":false,"usgs":true,"family":"McLain","given":"Alberton","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":324948,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Bernard R.","contributorId":38924,"corporation":false,"usgs":true,"family":"Smith","given":"Bernard","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":324949,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moore, Harry H.","contributorId":48670,"corporation":false,"usgs":true,"family":"Moore","given":"Harry","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":324950,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1013643,"text":"1013643 - 1965 - Characteristics and identification of oxidative Pseudomonads isolated from diseased fish","interactions":[],"lastModifiedDate":"2025-02-05T16:18:27.467682","indexId":"1013643","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2300,"text":"Journal of General Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Characteristics and identification of oxidative Pseudomonads isolated from diseased fish","docAbstract":"<p><span>Several characteristics of 20 strains of oxidative pseudomonads, all but one of which were isolated from freshwater fish, were determined. All strains oxidized glucose and gluconate, produced NH</span><sub><span class=\"jp-sub\">3</span></sub><span>&nbsp;from 1 % peptone, grew at 6, 12, 20 and 30° and produced cytochrome oxidase. Lipase was produced by 17 of the strains, while 15 produced gelatinase, and 16 produced fluorescent pigment. These and other characteristics used to identify fish-spoilage pseudomonads are also useful for identification of fish-pathogenic pseudomonads. Species determinations from the present data were not attempted. However, from previously published data on speciation of&nbsp;</span><i><span class=\"jp-italic\">Pseudomonas</span></i><span>, most of the 20 strains appeared to be closely related to or identical with <i>P.&nbsp;</i></span><i><span class=\"jp-italic\">fluorescens</span></i><span>.</span></p>","language":"English","publisher":"Microbiology Society","doi":"10.1099/00221287-38-1-1","usgsCitation":"Bullock, G.L., Snieszko, S.F., and Dunbar, C.E., 1965, Characteristics and identification of oxidative Pseudomonads isolated from diseased fish: Journal of General Microbiology, v. 38, p. 1-7, https://doi.org/10.1099/00221287-38-1-1.","productDescription":"7 p.","startPage":"1","endPage":"7","numberOfPages":"7","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":486903,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1099/00221287-38-1-1","text":"Publisher Index Page"},{"id":131914,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"38","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e539f","contributors":{"authors":[{"text":"Bullock, G. L.","contributorId":69498,"corporation":false,"usgs":true,"family":"Bullock","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":318949,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":318948,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dunbar, C. E.","contributorId":96623,"corporation":false,"usgs":true,"family":"Dunbar","given":"C.","middleInitial":"E.","affiliations":[],"preferred":false,"id":318950,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5220020,"text":"5220020 - 1965 - A method for estimating fall adult sex ratios from production and survival data","interactions":[],"lastModifiedDate":"2025-02-07T16:47:41.61941","indexId":"5220020","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"A method for estimating fall adult sex ratios from production and survival data","docAbstract":"<p>This paper presents a method of utilizing data relating to the production and survival of a bird population to estimate a <i>basic</i> fall adult sex ratio. This basic adult sex ratio is an average value derived from average production and survival rates. It is an estimate of the average sex ratio about which the fall adult ratios will fluctuate according to annual variations in production and survival. The basic fall adult sex ratio has been calculated as an asymptotic value which is the limit of an infinite series wherein average population characteristics are used as constants. Graphs are provided that allow the determination of basic sex ratios from production and survival data of a population. Where the respective asymptote has been determined, it may be possible to estimate various production and survival rates by use of variations of the formula for estimating the asymptote.</p>","language":"English","publisher":"Wiley","doi":"10.2307/3798647","usgsCitation":"Wight, H.M., Heath, R.G., and Geis, A.D., 1965, A method for estimating fall adult sex ratios from production and survival data: Journal of Wildlife Management, v. 29, no. 1, p. 185-192, https://doi.org/10.2307/3798647.","productDescription":"8 p.","startPage":"185","endPage":"192","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193601,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae11f","contributors":{"authors":[{"text":"Wight, Howard M.","contributorId":22407,"corporation":false,"usgs":true,"family":"Wight","given":"Howard","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":331211,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Heath, Robert G.","contributorId":103719,"corporation":false,"usgs":true,"family":"Heath","given":"Robert","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":331213,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Geis, A. D.","contributorId":72885,"corporation":false,"usgs":true,"family":"Geis","given":"A.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":331212,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70045413,"text":"70045413 - 1965 - Computer technique for slope-area measurements","interactions":[],"lastModifiedDate":"2013-05-23T11:31:15","indexId":"70045413","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":382,"text":"Surface Water Techniques","active":false,"publicationSubtype":{"id":6}},"title":"Computer technique for slope-area measurements","docAbstract":"The report gives detailed instructions on preparation of input data for automatic computation of a discharge measurement by the slope-area method. The program follows standardized methods of computing cross section properties and uses multi-section discharge equations. The printout comprises hydraulic properties of each section and computed discharges for each component sub-reach and for the entire reach. One example demonstrates the technique.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydraulic Measurement and Computation","largerWorkSubtype":{"id":6,"text":"USGS Unnumbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, DC","doi":"10.3133/70045413","usgsCitation":"Somers, W., and Selner, G., 1965, Computer technique for slope-area measurements: Surface Water Techniques, vi, 14 p., https://doi.org/10.3133/70045413.","productDescription":"vi, 14 p.","numberOfPages":"22","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":270916,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70045413/report-thumb.jpg"},{"id":272725,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70045413/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"516d2169e4b0411d430a8a05","contributors":{"authors":[{"text":"Somers, W.P.","contributorId":79787,"corporation":false,"usgs":true,"family":"Somers","given":"W.P.","email":"","affiliations":[],"preferred":false,"id":477465,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Selner, G.I.","contributorId":13229,"corporation":false,"usgs":true,"family":"Selner","given":"G.I.","affiliations":[],"preferred":false,"id":477464,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2897,"text":"wsp1811 - 1965 - Hydrology of the Little Plover River basin, Portage County, Wisconsin, and the effects of water resource development","interactions":[],"lastModifiedDate":"2023-04-13T20:54:27.826245","indexId":"wsp1811","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"1811","title":"Hydrology of the Little Plover River basin, Portage County, Wisconsin, and the effects of water resource development","docAbstract":"<p>The Little Plover River basin is in the sand-plain area of central Wisconsin. The basin and the surrounding sand-plain area provide a good fish and wildlife habitat and is a popular locale for sport fishing. Good yields may be obtained in the area from irrigated crops, and the irrigated acreage has been increasing rapidly in recent years. Sportsmen and conservationists are concerned about the effects of increased development of the water resources on the streams as trout habitat. In the past, many political and legal conflicts among water users have arisen from erroneous opinions as to the behavior of water. Many of these conflicts would be diminished or eliminated if the participants were cognizant of fundamental hydrologic principles. </p><p>This study was made to demonstrate the extent and nature of the interrelation of ground water and surface water and the fundamental hydrologic principles governing water movement. The study was also made to determine the hydrologic changes that might occur following development, to provide information that might be used as a basis for planning water development, and for drafting legislation that recognizes the relation between ground water and surface water. </p><p>Water has been developed in the Little Plover River basin for industry, for domestic and stock supplies, and for irrigation. Irrigated acreage is increasing in the area, and the use of water for irrigation may alter the hydrology of the basin somewhat. About 4,000-4,500 acres of land within the basin, or 50-60 percent of the basin area, is suitable for irrigated farming, but probably no more than 2,500 acres will be under irrigation in any one year, unless present crop-rotation practices are changed. </p><p>Most of the Little Plover River basin is underlain by from 40 to 100 feet of glacial outwash consisting of highly permeable sand and gravel. The glacial outwash is the main aquifer in the area and is capable of yielding large quantities of water to wells. An aquifer test in the area indicated that the coefficient of transmissibility of the glacial outwash is about 140,000 gallons per day per foot. The specific yield of the outwash is about 20 percent, as determined from water-level and streamfiow data. Morainal deposits occur locally with the glacial outwash. These deposits transmit water readily and do not form barriers to ground water in the outwash. Relatively impermeable crystalline rocks underlie the glacial deposits, and a sandstone ridge of low permeability impedes the movement of ground water from the basin by underflow. </p><p>The glacial outwash and morainal deposits are recharged by infiltration of 9-10 inches of the 31 inches of precipitation that falls on the area in an average year. If it is not withdrawn by wells for consumptive use or by phreatophytes, water that infiltrates the sand and gravel discharges later into the Little Plover River. This ground-water discharge constitutes 90-95 percent of the total flow of the Little Plover River. </p><p>Annual evapotranspiration varies considerably, but generally ranges from 2 to 8 inches less than the potential evapotranspiration of 24 inches. Consumptive use of irrigation water averages about 4 inches per year. Most of the water pumped from wells otherwise would be discharged to the stream, and consumptive use of irrigation water will deplete streamflow by the amount of evapotranspiration. </p><p>Pumping wells have little effect on the water level in the highly permeable sand and gravel. Significant interference between wells would occur only if large capacity wells were within a few tens of feet of each other. </p><p>Ground water and surface water are closely interrelated in the sand-plain area and ground-water withdrawals near the Little Plover River may cause a measurable streamflow depletion. In a test, a well that was pumping about 1,120 gpm (gallons per minute) and that was 300 feet from the stream derived about 30 percent of its flow from the stream after 3 days of pumping. </p><p>For this study, the effects of increased ground-water development were evaluated from a hypothetical development schedule, for which it was assumed that 500 acres were irrigated the first year and that an additional 50 acres were irrigated in each succeeding year for 10 years. It also was assumed that the average annual consumptive-use requirement for irrigation water would be one- third of an acre-foot per acre. Calculations indicate that the maximum monthly rate of depletion due to the consumptive use of 4 inches of ground water per year on 500 acres would be about 0.4 cfs (cubic feet per second) the first year and 0.5 cfs after 10 years of pumping. Other computations indicate that the maximum monthly rate of depletion due to irrigating 500 acres the first year and 50 additional acres each year for 10 years would be about 0.8 cfs. Maximum depletion would occur during the summer months, concurrent with the irrigation withdrawals. </p><p>Because of the close interrelation between ground and surface water, surface- water withdrawals will cause an increased inflow of ground water to the stream and a decline in ground-water levels near the stream. These effects were demonstrated by pumping from the stream. After 29 hours of pumping, a depletion of 1,120 gpm at a site 7,000 feet downstream was about 200 gpm less than the diversion at the pump. Most of the 200 gpm was supplied from the stream-banks, and ground-water levels near the stream declined as much as 0.3 foot. Computations indicated that ground-water inflow, following a streamflow diver- sion that lowered the stage 0.15 foot, would be 0.14 cfs after 5 days and 0.06 cfs after 30 days. </p><p>The demonstration of the quantitative relation between ground water and surface water, as given by this study, should provide a sound basis for planning water development to minimize conflicts of interest. The demonstrations also should provide a basis for drafting legislation that recognizes the interrelation of ground water and surface water. </p><p>Because the geology and the hydrology are relatively uniform throughout the sand plains, many of the methods and hydrologic values determined for this detailed study of the Little Plover River basin may be applied to other basins in the sand-plain area.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1811","collaboration":"Prepared in cooperation with the Wisconsin Conservation Department and the University of Wisconsin Geological and Natural History Survey","usgsCitation":"Weeks, E.P., Erickson, D.W., and Holt, C.L., 1965, Hydrology of the Little Plover River basin, Portage County, Wisconsin, and the effects of water resource development: U.S. Geological Survey Water Supply Paper 1811, Report: v, 78 p.; 6 Plates: 21.00 x 18.01 inches or smaller, https://doi.org/10.3133/wsp1811.","productDescription":"Report: v, 78 p.; 6 Plates: 21.00 x 18.01 inches or smaller","numberOfPages":"85","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":415734,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25017.htm","linkFileType":{"id":5,"text":"html"}},{"id":29561,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1811/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29559,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1811/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29558,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1811/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29562,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1811/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29560,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1811/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29563,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1811/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138378,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1811/report-thumb.jpg"},{"id":29557,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1811/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","county":"Portage County","otherGeospatial":"Little Plover River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -89.589,\n              44.554\n            ],\n            [\n              -89.589,\n              44.404\n            ],\n            [\n              -89.367,\n              44.404\n            ],\n            [\n              -89.367,\n              44.554\n            ],\n            [\n              -89.589,\n              44.554\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdc0c","contributors":{"authors":[{"text":"Weeks, Edwin P. epweeks@usgs.gov","contributorId":2576,"corporation":false,"usgs":true,"family":"Weeks","given":"Edwin","email":"epweeks@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":145973,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erickson, Donald W.","contributorId":34900,"corporation":false,"usgs":true,"family":"Erickson","given":"Donald","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":145974,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Holt, Charles Lee Roy Jr.","contributorId":77913,"corporation":false,"usgs":true,"family":"Holt","given":"Charles","suffix":"Jr.","email":"","middleInitial":"Lee Roy","affiliations":[],"preferred":false,"id":145975,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1000089,"text":"1000089 - 1965 - Length-weight relationship of northern pike, Esox lucius, from East Harbor, Ohio","interactions":[],"lastModifiedDate":"2016-02-25T11:11:27","indexId":"1000089","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"Length-weight relationship of northern pike, Esox lucius, from East Harbor, Ohio","docAbstract":"<p>The northern pike is one of Ohio's largest game fish but is well known to comparatively few anglers. Large numbers of the big fish spawn in the Ohio marshes adjacent to Lake Erie. Movements related to spawning reach a peak in late March or early April. Later the spawning population disperses and is seldom represented in catches by experimental gear or by anglers. The short period of availability was used to obtain life history information in March of 1951 through 1953. No comprehensive length-weight data for this species have previously been published from this area. East Harbor is a sandspit pond separated from Lake Erie by a large sand bar. Waters and fish populations of the harbor and lake can mix freely through a permanent connecting channel. The larger part of the 850 surface acres of the harbor is normally less than 8 feet deep. The male northern pike averaged 20.5 inches in length and ranged from 13.5 to 28.5 inches. The conspicuously larger females averaged 26.0 inches and ranged from 15.5 to 37.5 inches.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1965)94[404:LRONPE]2.0.CO;2","usgsCitation":"Brown, E.H., and Clark, C.F., 1965, Length-weight relationship of northern pike, Esox lucius, from East Harbor, Ohio: Transactions of the American Fisheries Society, v. 94, no. 4, p. 404-405, https://doi.org/10.1577/1548-8659(1965)94[404:LRONPE]2.0.CO;2.","productDescription":"2 p.","startPage":"404","endPage":"405","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":132987,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"94","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6108","contributors":{"authors":[{"text":"Brown, Edward H. Jr.","contributorId":33251,"corporation":false,"usgs":true,"family":"Brown","given":"Edward","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308058,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, Clarence F.","contributorId":99101,"corporation":false,"usgs":true,"family":"Clark","given":"Clarence","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":308059,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70171153,"text":"70171153 - 1965 - Field application methods for recovery of the selective lampricide, 3-trifluoromethyl-4-nitrophenol","interactions":[],"lastModifiedDate":"2016-05-24T09:56:22","indexId":"70171153","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Field application methods for recovery of the selective lampricide, 3-trifluoromethyl-4-nitrophenol","docAbstract":"<p>Colorimetric methods are described for the detection of residues of the selective lampricide, 3-trifluoromethyl-4-nitrophenol (TFM), in natural waters and fish tissues. Solvent extraction and anion exchange were used to separate and concentrate the lampricide, and to reduce high background colors which often interfere with the determinations. Data from the Pentwater and Muskegon Rivers (Michigan) showed an exponential rate of disappearance of TFM from the water immediately after treatments to eradicate larvae of the sea lamprey (<i>Petromyzon marinus</i>). No TFM was recovered from fish exposed in their natural environment to low levels of the lampricide during treatment; residues were recovered, however, from fish exposed to high concentrations in the laboratory.</p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the 8th Conference on Great Lakes Research","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"8th Conference on Great Lakes Research","conferenceDate":"March 29-30","conferenceLocation":"Ann Arbor, MI","language":"English","publisher":"University of Michigan","usgsCitation":"Billy, T.J., Daniels, S.L., Kempe, L.L., and Beeton, A.M., 1965, Field application methods for recovery of the selective lampricide, 3-trifluoromethyl-4-nitrophenol, <i>in</i> Proceedings of the 8th Conference on Great Lakes Research, Ann Arbor, MI, March 29-30, p. 17-24.","productDescription":"8 p.","startPage":"17","endPage":"24","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":321589,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574d6505e4b07e28b6683e7b","contributors":{"authors":[{"text":"Billy, Thomas J.","contributorId":76853,"corporation":false,"usgs":true,"family":"Billy","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":630121,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Daniels, Stacy L.","contributorId":105821,"corporation":false,"usgs":true,"family":"Daniels","given":"Stacy","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":630122,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kempe, Lloyd L.","contributorId":55117,"corporation":false,"usgs":true,"family":"Kempe","given":"Lloyd","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":630123,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Beeton, Alfred M.","contributorId":94247,"corporation":false,"usgs":true,"family":"Beeton","given":"Alfred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":630124,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70185670,"text":"70185670 - 1965 - Vigil Network sites: A sample of data for permanent filing","interactions":[],"lastModifiedDate":"2017-03-27T13:03:24","indexId":"70185670","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5334,"text":"International Association of Scientific Hydrology - Bulletin ","onlineIssn":"2150-3435","printIssn":"0262-6667","active":false,"publicationSubtype":{"id":10}},"title":"Vigil Network sites: A sample of data for permanent filing","docAbstract":"<p>The Vigil Network consists of places where observations are made through time to record changes in landscape features over a long period. Resurveys will usually be made once each year or every few years and the period of observation, hopefully, will extend through and beyond the International Hydrological Decade.</p><p>Vigil Network sites will usually be chosen to represent some typical feature of a given landscape. In the example shown here, the feature is a small ephemeral channel in a basin of moderate relief underlain by silty sandstone typical of the surrounding area. Vigil sites are not protected from man's influence and indeed may be selected because of the possible or portending cultural influences. In this respect they differ from the Bench Mark Network whose purpose is to make precise observations of hydrologic factors in areas uninfluenced by and protected from man's use.</p><p>The factors which might be observed are many and varied. A few might be mentioned here, others are explained at length elsewhere (Miller and Leopold, 1963; Leopold, 1962). Streamchannel position, form, depth, and profile; vegetation in form of transects or quadrats; soil movement on slopes; rock movement on slopes or in channels. These and many more would yield valuable information on changes with time.</p><p>To assure permanence of initial field observations, including reference points, bench marks, and cross sections, brief descriptions, maps, and initial data should be filed identically in designated repositories where the data will be made available for inspection by any interested scientist. It is recommended that the designation of two such locations where records of the type here attached will be filed be taken up by the Coordinating Council of the International Hydrological Decade. In designating such repositories it should be recognized that there is no need for elaborate indexing. The main requirement is merely the maintenance of a simple file where the data are stored and can be inspected or copied by any scientist. There need be no special provision for lending or reproduction services.</p><p>The present document is an example showing what data, maps, and descriptions should be included in those permanent files at the two repositories. The material in these repositories should be sufficient to permit someone in the indefinite future to find and remeasure the same features described now. Thus the scientific value of the original surveys increases with time, - provided that the descriptions are sufficient to allow a person to find with assurance the original feature in the field.</p><p>It must be visualized that a permanent repository must economize in space. Thus, as the example here shows, the filed material is not all of the original field notes but a summary, brief but descriptive.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666509493401","usgsCitation":"Leopold, L.B., and Emmett, W.W., 1965, Vigil Network sites: A sample of data for permanent filing: International Association of Scientific Hydrology - Bulletin , v. 10, no. 3, p. 12-21, https://doi.org/10.1080/02626666509493401.","productDescription":"10 p.","startPage":"12","endPage":"21","costCenters":[],"links":[{"id":480681,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626666509493401","text":"Publisher Index Page"},{"id":338379,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58da253fe4b0543bf7fda87d","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":686308,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Emmett, William W.","contributorId":68715,"corporation":false,"usgs":true,"family":"Emmett","given":"William","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":686309,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70176115,"text":"70176115 - 1965 - Water quality records in Texas, 1964","interactions":[],"lastModifiedDate":"2016-08-26T10:16:39","indexId":"70176115","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":5196,"text":"Water Data Report","active":true,"publicationSubtype":{"id":6}},"title":"Water quality records in Texas, 1964","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70176115","usgsCitation":"U.S. Geological Survey, 1965, Water quality records in Texas, 1964: Water Data Report, 199 p., https://doi.org/10.3133/70176115.","productDescription":"199 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":327890,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57c16841e4b0f2f0ceb90899","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":128240,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":647151,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70176114,"text":"70176114 - 1965 - Surface water records of Texas, 1964","interactions":[],"lastModifiedDate":"2017-04-19T10:37:54","indexId":"70176114","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":5196,"text":"Water Data Report","active":true,"publicationSubtype":{"id":6}},"title":"Surface water records of Texas, 1964","docAbstract":"<p>The surface-water records for the 1964 water year for gaging stations, partial-record stations, miscellaneous sites, and base-flow studies within the State of Texas are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U. S. Geological Survey, under the direction of Trigg Twichell, district chief, Water Resources Division. </p><p>Through September 30, 1960, the records of discharge and stage of streams and contents and stage of lakes or reservoirs were published in an annual series of U.S. Geological Survey water supply papers, entitled \"Surface Water Supply of the United States.\" Since 1951 there have been 20 volumes in the series; each volume covered an area whose boundaries coincided with those of certain natural drainage areas. The records in Texas were contained in Parts 7 and 8 of that series. </p><p>Beginning with the 1961 water year, streamflow records and related data have been released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these basic-data reports is limited and primarily for local needs. Records will be published in Geological Survey water-supply papers at 5-year intervals.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70176114","collaboration":"Prepared in cooperation with the Texas Water Commission, Pecos River Commission, Sabine River Compact Administration, City of Dallas, City of Houston, U.S. Army Corps of Engineers, U.S. Soil Conservation Service, U.S. Public Health Service, and U.S. Bureau of Reclamation","usgsCitation":"U.S. Geological Survey, 1965, Surface water records of Texas, 1964: Water Data Report, xiv, 479 p., https://doi.org/10.3133/70176114.","productDescription":"xiv, 479 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science 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 \"}}]}","contact":"<p><a href=\"https://pubs.er.usgs.gov/contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW"}
,{"id":70180001,"text":"70180001 - 1964 - Developing a state water plan: Ground-water conditions in Utah, spring of 1964","interactions":[],"lastModifiedDate":"2017-01-23T11:29:18","indexId":"70180001","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":110,"text":"Cooperative Investigations Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"2","title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1964","docAbstract":"<p>This report is the first in a series of annual reports which will describe ground-water conditions in Utah. It was prepared cooperatively by the U.S. Geological Survey and the Utah Water and Power Board and was designed to provide the data for interested parties, such as legislators, administrators, and planners to keep abreast of changing ground-water conditions in the state. Because this report is the first of the series, it necessarily includes certain background and descriptive information which gives a broad general picture of ground-water conditions. Subsequent reports will discuss only changes that have taken place during the previous year.</p><p>Many of the data used in the preparation of the report were collected by the Geological Survey in cooperation with the Utah State Engineer during past and continuing programs. The well-location map and some statistical information about numbers of wells in the State were prepared by digital computer from the Utah Resources Information System, University of Utah, utilizing records which were compiled largely from the files of the Utah State Engineer. R.E. Marsell, geological consultant to the Utah Water and Power Board, first suggested that this report be prepared.</p>","language":"English","publisher":"Utah Water and Power Board","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the State of Utah","usgsCitation":"Arnow, T., Butler, R., Mower, R.W., Gates, J., Cordova, R., Carpenter, C., Bjorklund, L., Feltis, R., Robinson, G., and Sandberg, G.W., 1964, Developing a state water plan: Ground-water conditions in Utah, spring of 1964: Cooperative Investigations Report 2, 104 p.","productDescription":"104 p.","numberOfPages":"208","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333666,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333665,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-201"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58863a15e4b0cad700058b71","contributors":{"authors":[{"text":"Arnow, Ted","contributorId":84733,"corporation":false,"usgs":true,"family":"Arnow","given":"Ted","affiliations":[],"preferred":false,"id":659661,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Butler, R.G.","contributorId":60706,"corporation":false,"usgs":true,"family":"Butler","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":659662,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mower, R. W.","contributorId":34898,"corporation":false,"usgs":true,"family":"Mower","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659663,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gates, Joseph S.","contributorId":21647,"corporation":false,"usgs":true,"family":"Gates","given":"Joseph S.","affiliations":[],"preferred":false,"id":659664,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cordova, R.M.","contributorId":77511,"corporation":false,"usgs":true,"family":"Cordova","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":659665,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Carpenter, C.H.","contributorId":69229,"corporation":false,"usgs":true,"family":"Carpenter","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":659666,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Bjorklund, L.J.","contributorId":14035,"corporation":false,"usgs":true,"family":"Bjorklund","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":659667,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Feltis, R.D.","contributorId":93467,"corporation":false,"usgs":true,"family":"Feltis","given":"R.D.","affiliations":[],"preferred":false,"id":659668,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Robinson, G.B.","contributorId":178487,"corporation":false,"usgs":true,"family":"Robinson","given":"G.B.","email":"","affiliations":[],"preferred":false,"id":659669,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Sandberg, G. W.","contributorId":55426,"corporation":false,"usgs":true,"family":"Sandberg","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659670,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70161771,"text":"70161771 - 1964 -  The role of free and bound water in irradiation preservation: Free radical damage as a function of the physical state of water","interactions":[],"lastModifiedDate":"2017-01-11T16:33:31","indexId":"70161771","displayToPublicDate":"2015-09-07T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2293,"text":"Journal of Food Science","active":true,"publicationSubtype":{"id":10}},"title":" The role of free and bound water in irradiation preservation: Free radical damage as a function of the physical state of water","docAbstract":"<p><span>English sole fillets previously equilibrated with aqueous 0.1% cysteine were dehydrated by three methods to moisture levels ranging from 2 to 72%. Model systems using cellulose to replace the fish tissue were also used. The samples were irradiated at 1 Mrad in an air, nitrogen, or oxygen atmosphere. The destruction of −SH groups was measured and related to the amount and physical state of the tissue water. As free water was removed, destruction steadily increased, reaching a maximum at about 20% moisture. Destruction decreased markedly at moisture levels below 10%, and calorimetric measurements confirmed that 10% moisture was about the level of bound water in this species. These data suggest that dehydration favors the reaction of solute molecules with free radicals formed in the free water of muscle cells. At moisture levels greater than about 20%, simple free radical recombination is more likely than reaction with solute molecules, while below 20% moisture the reverse is true. The calculated α values support this conclusion, as do the results from model systems using cellulose.</span></p>","language":"English","publisher":"Institute of Food Technologists","doi":"10.1111/j.1365-2621.1964.tb00405.x","usgsCitation":"Wedemeyer, G., and Dollar, A., 1964,  The role of free and bound water in irradiation preservation: Free radical damage as a function of the physical state of water: Journal of Food Science, v. 29, no. 5, p. 525-529, https://doi.org/10.1111/j.1365-2621.1964.tb00405.x.","productDescription":"5 p.","startPage":"525","endPage":"529","numberOfPages":"5","costCenters":[],"links":[{"id":313882,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"5","noUsgsAuthors":false,"publicationDate":"2006-08-25","publicationStatus":"PW","scienceBaseUri":"568e48cae4b0e7a44bc41815","contributors":{"authors":[{"text":"Wedemeyer, Gary gwedemeyer@usgs.gov","contributorId":5504,"corporation":false,"usgs":true,"family":"Wedemeyer","given":"Gary","email":"gwedemeyer@usgs.gov","affiliations":[],"preferred":true,"id":587723,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dollar, A.M.","contributorId":150882,"corporation":false,"usgs":false,"family":"Dollar","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":587724,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70043613,"text":"70043613 - 1964 - Crustal structure between Lake Mead, Nevada, and Mono Lake, California","interactions":[],"lastModifiedDate":"2013-02-15T10:17:42","indexId":"70043613","displayToPublicDate":"2013-02-13T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":355,"text":"Crustal Studies Technical Letter","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"22","title":"Crustal structure between Lake Mead, Nevada, and Mono Lake, California","docAbstract":"Interpretation of a reversed seismic-refraction profile between Lake Mead, Nevada, and Mono Lake, California, indicates velocities of 6.15 km/sec for the upper layer of the crust, 7.10 km/sec for an intermediate layer, and 7.80 km/sec for the uppermost mantle. Phases interpreted to be reflections from the top of the intermediate layer and the Mohorovicic discontinuity were used with the refraction data to calculate depths. The depth to the Moho increases from about 30 km near Lake Mead to about 40 km near Mono Lake. Variations in arrival times provide evidence for fairly sharp flexures in the Moho. Offsets in the Moho of 4 km at one point and 2 1/2 km at another correspond to large faults at the surface, and it is suggested that fracture zones in the upper crust may displace the Moho and extend into the upper mantle. The phase P appears to be an extension of the reflection from the top of the intermediate layer beyond the critical angle. Bouguer gravity, computed for the seismic model of the crust, is in good agreement with the measured Bouguer gravity. Thus a model of the crustal structure is presented which is consistent with three semi-independent sources of geophysical data: seismic-refraction, seismic-reflection, and gravity.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70043613","collaboration":"In cooperation with the <a href=\"http://www.darpa.mil/\" target=\"_blank\">Defense Advanced Research Projects Agency</a>","usgsCitation":"Johnson, L.R., 1964, Crustal structure between Lake Mead, Nevada, and Mono Lake, California: Crustal Studies Technical Letter 22, 21 p., https://doi.org/10.3133/70043613.","productDescription":"21 p.","numberOfPages":"25","onlineOnly":"Y","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":379,"text":"Menlo Park Science Center","active":false,"usgs":true}],"links":[{"id":267548,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":267546,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/misc/tl/0022/"},{"id":267547,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/misc/tl/0022/tl0022.pdf"}],"country":"United States","state":"California;Nevada","otherGeospatial":"Lake Mead;Mono Lake","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -0.01611111111111111,8.333333333333334E-4 ], [ -0.01611111111111111,8.333333333333334E-4 ], [ -0.01638888888888889,8.333333333333334E-4 ], [ -0.01638888888888889,8.333333333333334E-4 ], [ -0.01611111111111111,8.333333333333334E-4 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"511f670fe4b03b29402c5dbc","contributors":{"authors":[{"text":"Johnson, Lane R.","contributorId":19049,"corporation":false,"usgs":true,"family":"Johnson","given":"Lane","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":473970,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70038669,"text":"wdrCA631 - 1964 - Surface water records of California, 1963; Volume 1: Colorado River Basin, Southern Great Basin, and Pacific Slope Basins excluding Central Valley","interactions":[],"lastModifiedDate":"2012-06-13T01:01:48","indexId":"wdrCA631","displayToPublicDate":"2012-06-04T09:11:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CA-63-1","title":"Surface water records of California, 1963; Volume 1: Colorado River Basin, Southern Great Basin, and Pacific Slope Basins excluding Central Valley","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA631","usgsCitation":"U.S. Geological Survey, 1964, Surface water records of California, 1963; Volume 1: Colorado River Basin, Southern Great Basin, and Pacific Slope Basins excluding Central Valley: U.S. Geological Survey Water Data Report CA-63-1, 463 p., https://doi.org/10.3133/wdrCA631.","productDescription":"463 p.","costCenters":[],"links":[{"id":257482,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_CA_63_1.bmp"},{"id":257475,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1963/ca-63/WDR-1963-vol1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9fcce4b08c986b31e818"}
,{"id":70038394,"text":"wdrCA64 - 1964 - Water Quality Records in California","interactions":[],"lastModifiedDate":"2012-05-22T01:01:41","indexId":"wdrCA64","displayToPublicDate":"2012-05-13T11:48:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CA-64","title":"Water Quality Records in California","docAbstract":"The quality-of-water investigations of the U.S. Geological Survey are concerned with the chemical and physical characteristics of surface and ground water supplies of the Nation in conjunction with water usage and its availability. The basic records for the 1964 water year for quality of surface waters within the State of California are given in this report. For convenience and interest there are also records for a few water quality stations in bordering States. The data were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of Eugene Brown, district chemist, Quality of Water Branch.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA64","usgsCitation":"U.S. Geological Survey, 1964, Water Quality Records in California: U.S. Geological Survey Water Data Report CA-64, x, 348 p., https://doi.org/10.3133/wdrCA64.","productDescription":"x, 348 p.","costCenters":[],"links":[{"id":256911,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":256906,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1964/ca-64/WDR-1964-wq.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc413e4b08c986b32b4af"}
,{"id":70039543,"text":"70039543 - 1964 - Compilation of seismic-refraction crustal data in the Soviet Union","interactions":[],"lastModifiedDate":"2013-01-15T11:23:26","indexId":"70039543","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":355,"text":"Crustal Studies Technical Letter","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"18","title":"Compilation of seismic-refraction crustal data in the Soviet Union","docAbstract":"The U.S. Geological Survey is preparing a series of terrain atlases of the Sino-Soviet bloc of nations for use in a possible nuclear-test detection program. Part of this project is concerned with the compilation and evaluation of crustal-structure data. To date, a compilation has been made of data from Russian publications that discuss seismic refraction and gravity studies of crustal structure. Although this compilation deals mainly with explosion seismic-refraction measurements, some results from earthquake studies are also included. None of the data have been evaluated.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/70039543","collaboration":"In cooperation with the Defense Advanced Research Projects Agency","usgsCitation":"Rodriguez, R., Durbin, W.P., Healy, J.H., and Warren, D.H., 1964, Compilation of seismic-refraction crustal data in the Soviet Union: Crustal Studies Technical Letter 18, 4 Sheets: 87 x 108 cm. or smaller, https://doi.org/10.3133/70039543.","productDescription":"4 Sheets: 87 x 108 cm. or smaller","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":259567,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/misc/tl/0018/tl0018_sheet4_northeastern_Asia.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":259562,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/misc/tl/0018/","linkFileType":{"id":5,"text":"html"}},{"id":259563,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/misc/tl/0018/tl0018_text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":259564,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/misc/tl/0018/tl0018_sheet1_Europe.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":259565,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/misc/tl/0018/tl0018_sheet2_southern_Asia.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":259566,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/misc/tl/0018/tl0018_sheet3_northwestern_Asia.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":259572,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"otherGeospatial":"Soviet Union","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 4,30 ], [ 4,80 ], [ -168.5,80 ], [ -168.5,30 ], [ 4,30 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f8eee4b0c8380cd4d35a","contributors":{"authors":[{"text":"Rodriguez, Robert","contributorId":56116,"corporation":false,"usgs":true,"family":"Rodriguez","given":"Robert","affiliations":[],"preferred":false,"id":466451,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Durbin, William P. Jr.","contributorId":10688,"corporation":false,"usgs":true,"family":"Durbin","given":"William","suffix":"Jr.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":466449,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Healy, J. H.","contributorId":48968,"corporation":false,"usgs":true,"family":"Healy","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":466450,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Warren, David H.","contributorId":106128,"corporation":false,"usgs":true,"family":"Warren","given":"David","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":466452,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":71007,"text":"wdrCO642 - 1964 - Surface water records of Colorado, water year 1964","interactions":[],"lastModifiedDate":"2012-02-02T00:13:46","indexId":"wdrCO642","displayToPublicDate":"2005-08-09T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CO-64-2","title":"Surface water records of Colorado, water year 1964","language":"ENGLISH","doi":"10.3133/wdrCO642","usgsCitation":"Geological Survey, U., 1964, Surface water records of Colorado, water year 1964: U.S. Geological Survey Water Data Report CO-64-2, 353 p., https://doi.org/10.3133/wdrCO642.","productDescription":"353 p.","costCenters":[],"links":[{"id":185753,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1964/co-64-2/report-thumb.jpg"},{"id":90535,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1964/co-64-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697887","contributors":{"authors":[{"text":"Geological Survey, U.S.","contributorId":26017,"corporation":false,"usgs":true,"family":"Geological Survey","given":"U.S.","affiliations":[],"preferred":false,"id":283483,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71006,"text":"wdrCO641 - 1964 - Water quality records in Colorado, water year 1964","interactions":[],"lastModifiedDate":"2012-02-02T00:13:46","indexId":"wdrCO641","displayToPublicDate":"2005-08-09T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CO-64-1","title":"Water quality records in Colorado, water year 1964","language":"ENGLISH","doi":"10.3133/wdrCO641","usgsCitation":"Geological Survey, U., 1964, Water quality records in Colorado, water year 1964: U.S. Geological Survey Water Data Report CO-64-1, 84 p., https://doi.org/10.3133/wdrCO641.","productDescription":"84 p.","costCenters":[],"links":[{"id":185752,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1964/co-64-1/report-thumb.jpg"},{"id":90534,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1964/co-64-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f97bf","contributors":{"authors":[{"text":"Geological Survey, U.S.","contributorId":26017,"corporation":false,"usgs":true,"family":"Geological Survey","given":"U.S.","affiliations":[],"preferred":false,"id":283482,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71100,"text":"wdrMN641 - 1964 - Surface water records of Minnesota, 1964","interactions":[],"lastModifiedDate":"2012-02-02T00:14:03","indexId":"wdrMN641","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MN-64-1","title":"Surface water records of Minnesota, 1964","language":"ENGLISH","doi":"10.3133/wdrMN641","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1964, Surface water records of Minnesota, 1964: U.S. Geological Survey Water Data Report MN-64-1, vii, 160 p., https://doi.org/10.3133/wdrMN641.","productDescription":"vii, 160 p.","costCenters":[],"links":[{"id":101518,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1964/mn-64-1/report.pdf","size":"11947","linkFileType":{"id":1,"text":"pdf"}},{"id":192933,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1964/mn-64-1/report-thumb.jpg"}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697906","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":534719,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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