{"pageNumber":"2357","pageRowStart":"58900","pageSize":"25","recordCount":68857,"records":[{"id":70010252,"text":"70010252 - 1976 - Hydrogen and oxygen isotope exchange reactions between clay minerals and water","interactions":[],"lastModifiedDate":"2024-03-08T16:35:29.009976","indexId":"70010252","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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":"Hydrogen and oxygen isotope exchange reactions between clay minerals and water","docAbstract":"<div id=\"preview-section-abstract\"><div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"aep-abstract-id5\" class=\"abstract author\"><div id=\"aep-abstract-sec-id6\"><p>The extent of hydrogen and oxygen isotope exchange between clay minerals and water has been measured in the temperature range 100–350° for bomb runs of up to almost 2 years. Hydrogen isotope exchange between water and the clays was demonstrable at 100°. Exchange rates were 3–5 times greater for montmorillonite than for kaolinite or illite and this is attributed to the presence of interlayer water in the montmorillonite structure.</p><p>Negligible oxygen isotope exchange occurred at these low temperatures. The great disparity in D and O<sup>18</sup><span>&nbsp;</span>exchange rates observed in every experiment demonstrates that hydrogen isotope exchange occurred by a mechanism of proton exchange independent of the slower process of O<sup>18</sup><span>&nbsp;</span>exchange.</p><p>At 350° kaolinite reacted to form pyrophyllite and diaspore. This was accompanied by essentially complete D exchange but minor O<sup>18</sup><span>&nbsp;</span>exchange and implies that intact structural units in the pyrophyllite were inherited from the kaolinite precursor.</p></div></div></div></div><div id=\"preview-section-introduction\"><br></div><div id=\"preview-section-snippets\"><br></div><div id=\"preview-section-references\"><br></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(76)90181-2","issn":"00167037","usgsCitation":"O’Neil, J.R., and Kharaka, Y., 1976, Hydrogen and oxygen isotope exchange reactions between clay minerals and water: Geochimica et Cosmochimica Acta, v. 40, no. 2, p. 241-246, https://doi.org/10.1016/0016-7037(76)90181-2.","productDescription":"6 p.","startPage":"241","endPage":"246","numberOfPages":"6","costCenters":[],"links":[{"id":219674,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"40","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3345e4b0c8380cd5ee8a","contributors":{"authors":[{"text":"O’Neil, J. R.","contributorId":69633,"corporation":false,"usgs":true,"family":"O’Neil","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":358457,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kharaka, Y.K.","contributorId":23568,"corporation":false,"usgs":true,"family":"Kharaka","given":"Y.K.","email":"","affiliations":[],"preferred":false,"id":358456,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70162252,"text":"70162252 - 1976 - Prevention and control of viral diseases of salmonids","interactions":[],"lastModifiedDate":"2016-01-19T15:15:29","indexId":"70162252","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Prevention and control of viral diseases of salmonids","docAbstract":"<p><span>Three viral diseases of salmonids are of worldwide concern: infectious pancreatic necrosis (IPN) viral hemorrhagic septicemia (VHS), and infectious hematopoietic necrosis (IHN). Six principal approaches are being used to prevent or control these diseases: 1) preventing contact o the pathogen with the host, 2) environmental manipulation, 3) immunization, 4) chemotherapy, 5 selective breeding for disease resistance, and 6) reducing stress conditions which augment disease conditions. Preventing the introduction of a pathogen into a new stock of fish has been accomplished mainly by implementing stringent laws to prevent transport of infected fish into uninfected areas. Stocks of fish already infected are sometimes destroyed, and the hatchery is disinfected and restocked with fish free of specific pathogens. Environmental manipulation (elevated water temperature) has been successfully used to control IHN. Chemotherapeutics such as povidone-iodine for IPN and benzipyrene for IHN show promise of controlling mortalities; however, the practicality of using these drugs to eliminate the carrier fish has not been evaluated. Salmonids are capable of developing immune responses to viruses; however, development of effective vaccines, selective breeding for disease resistance, and identification of stress conditions which augment disease are still in the experimental phase.</span></p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/f76-134","usgsCitation":"Amend, D.F., 1976, Prevention and control of viral diseases of salmonids: Journal of the Fisheries Research Board of Canada, v. 33, no. 4, p. 1059-1066, https://doi.org/10.1139/f76-134.","productDescription":"8 p.","startPage":"1059","endPage":"1066","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314490,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569f6c53e4b0961cf27fd1c1","contributors":{"authors":[{"text":"Amend, Donald F.","contributorId":106543,"corporation":false,"usgs":true,"family":"Amend","given":"Donald","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":588986,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70162251,"text":"70162251 - 1976 - Physiological response of juvenile coho salmon (Oncorhynchus kisutch) and rainbow trout (Salmo gairdneri) to handling and crowding stress in intensive fish culture","interactions":[],"lastModifiedDate":"2016-01-19T15:10:15","indexId":"70162251","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Physiological response of juvenile coho salmon (Oncorhynchus kisutch) and rainbow trout (Salmo gairdneri) to handling and crowding stress in intensive fish culture","docAbstract":"<p><span>Moving 4&ndash;5-in. coho salmon (</span><i>Oncorhynchus kisutch</i><span>) held in soft (20&ensp;ppm CaCO</span><sub>3</sub><span>) water from the relatively light loading density of 0.5&ensp;lb/ft</span><sup>3</sup><span>&nbsp;to 1, 2, or 4&ensp;lb/ft</span><sup>3</sup><span>&nbsp;(density index, DI&ensp;=&ensp;0.1, 0.2, 0.4, 0.8) caused significant stress as indicated by loss of feeding behavior, but only minimal physiological disturbances, as indicated by lack of hyperglycemia or hypochloremia. However, moving them to 6 or 12&ensp;lb/ft</span><sup>3</sup><span>&nbsp;(DI&ensp;=&ensp;1.2, 2.4) caused significant physiological stress which required at least a week for recovery. Smolting coho salmon were physiologically stressed by population densities of 1&ensp;lb/ft</span><sup>3</sup><span>&nbsp;or more and a subclinical corynebacterial kidney infection was activated. Rainbow trout (</span><i>Salmo gairdneri</i><span>) (4&ndash;5&ensp;in.) were physiologically stressed when moved and held at 1&ensp;lb/ft</span><sup>3</sup><span>&nbsp;or more but retained normal feeding behavior. This indicates that handling and crowding stress will be minimized in softwater areas if densities in fish distribution trucks or in ponds or raceways during disease treatments are held to 0.1&ndash;0.5&ensp;lb/gal.</span></p>","language":"English","publisher":"NRC Reserach Press","doi":"10.1139/f76-320","usgsCitation":"Wedemeyer, G.A., 1976, Physiological response of juvenile coho salmon (Oncorhynchus kisutch) and rainbow trout (Salmo gairdneri) to handling and crowding stress in intensive fish culture: Journal of the Fisheries Research Board of Canada, v. 33, no. 12, p. 2699-2702, https://doi.org/10.1139/f76-320.","productDescription":"4 p.","startPage":"2699","endPage":"2702","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314489,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569f6c46e4b0961cf27fd1ba","contributors":{"authors":[{"text":"Wedemeyer, Gary A.","contributorId":30668,"corporation":false,"usgs":true,"family":"Wedemeyer","given":"Gary","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":588985,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010962,"text":"70010962 - 1976 - Indexes associated with information theory in water quality","interactions":[],"lastModifiedDate":"2013-03-14T19:27:33","indexId":"70010962","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2573,"text":"Journal of the Water Pollution Control Federation","active":true,"publicationSubtype":{"id":10}},"title":"Indexes associated with information theory in water quality","docAbstract":"In many biological studies of water quality, a diversity index is calculated in 'bits per individual' by using Shannon's Approximation to Brillouin's Formula. Difficulties associated with such use of Shannon's Formula and its associated parameters are discussed. Recent research has indicated that diversity indexes can be improved if (a) biological sample collection and analysis are standardized prior to use for among various aquatic systems diversity indexes and their associated parameters, (b) the diversity index is measured in 'sits per individual' rather than the presently used unit of 'bits per individual,' and (c) the equation e=(H - H(min)/(H(max) - H(min)) is used to evaluate the uniformity of distribution of individuals among species in a sample where e equals relative evenness. Relative evenness, a ratio, is an expression in which Brillouin's and Shannon's Equations are not arbitrarily mixed. Values of diversity indexes using Brillouin and Shannon Formulas, both in bits and sits per individual, and relative evenness are given for 16 hypothetical samples.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the Water Pollution Control Federation","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"JSTOR","issn":"00431303","usgsCitation":"Zand, S., 1976, Indexes associated with information theory in water quality: Journal of the Water Pollution Control Federation, v. 48, no. 8, p. 2026-2031.","startPage":"2026","endPage":"2031","numberOfPages":"6","costCenters":[],"links":[{"id":221079,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269369,"type":{"id":11,"text":"Document"},"url":"https://www.jstor.org/stable/25039974"}],"volume":"48","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3a7fe4b0c8380cd61d12","contributors":{"authors":[{"text":"Zand, S.M.","contributorId":25699,"corporation":false,"usgs":true,"family":"Zand","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":359978,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44557,"text":"wri76107 - 1976 - Map showing ground-water conditions in the Aravaipa Valley area, Graham and Pinal Counties, Arizona-1975","interactions":[],"lastModifiedDate":"2023-03-15T18:37:54.763558","indexId":"wri76107","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"76-107","title":"Map showing ground-water conditions in the Aravaipa Valley area, Graham and Pinal Counties, Arizona-1975","docAbstract":"<p>This hydrologic map of the Aravaipa Valley area includes about 500 sq mi in southeastern Arizona. Development of the ground-water resources is small, and pumpage is estimated to be less than 3,000 acre-ft annually for irrigation, livestock, and domestic uses. Hydrographs of the water level in selected wells show no long-term decline. Irrigation wells yield as much as 1 ,200 gal/min from the younger and older alluvium along Aravaipa Creek. The chemical quality of the ground water generally is good.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri76107","usgsCitation":"Gould, J.A., and Wilson, R.P., 1976, Map showing ground-water conditions in the Aravaipa Valley area, Graham and Pinal Counties, Arizona-1975: U.S. Geological Survey Water-Resources Investigations Report 76-107, Report: 1 p.; 1 Plate: 20.00 x 26.66 inches, https://doi.org/10.3133/wri76107.","productDescription":"Report: 1 p.; 1 Plate: 20.00 x 26.66 inches","costCenters":[],"links":[{"id":414245,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35017.htm","linkFileType":{"id":5,"text":"html"}},{"id":113826,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0107/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":113825,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0107/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":135044,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0107/report-thumb.jpg"}],"country":"United States","state":"Arizona","county":"Graham County, Pinal County","otherGeospatial":"Aravaipa Valley area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -110.6070,\n              33\n            ],\n            [\n              -110.6070,\n              32.579\n            ],\n            [\n              -110.05,\n              32.579\n            ],\n            [\n              -110.05,\n              33\n            ],\n            [\n              -110.6070,\n              33\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a49c8","contributors":{"authors":[{"text":"Gould, J. A.","contributorId":106856,"corporation":false,"usgs":true,"family":"Gould","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":229991,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, R. P.","contributorId":37672,"corporation":false,"usgs":true,"family":"Wilson","given":"R.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":229990,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010859,"text":"70010859 - 1976 - Studies of quaternary saline lakes-II. Isotopic and compositional changes during desiccation of the brines in Owens Lake, California, 1969-1971","interactions":[],"lastModifiedDate":"2024-03-08T16:38:00.824146","indexId":"70010859","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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":"Studies of quaternary saline lakes-II. Isotopic and compositional changes during desiccation of the brines in Owens Lake, California, 1969-1971","docAbstract":"<p>Owens Lake is an alkaline salt lake in a closed basin in southeast California. It is normally nearly dry, but in early 1969, an abnormal runoff from the Sierra Nevada flooded it to a maximum depth of 2·4 m. By late summer of 1971, the lake was again nearly dry and the dissolved salts recrystallized. Changes in the chemistry, pH, and deuterium content were monitored during desiccation.</p><p>During flooding, salts (mostly trona, halite, and burkeite) dissolved slowly from the lake floor. Their concentration in the lake waters increased as evaporation removed water and salts again crystallized, but winter temperatures caused precipitation of some salts and the following summer warming caused their solution, resulting in seasonal variations in the concentration patterns of some ions. The pH values (9·4–10·4) changed with time but showed no detectable diurnal pattern.</p><p>The deuterium concentration increased during evaporation and appeared to be in equilibrium with vapor leaving the lake according to the Rayleigh equation. The effective α(D/H in liquid/D/H in vapor) decreased as salinity increased; the earliest measured value was 1·069 [as total dissolved solids (TDS) of lake waters changed from 136,200 to 250,400 mg/1]and the last value (calc.) was 1·025 (as TDS changed from 450,000 to 470,300 mg/1). Deuterium exchange with the atmosphere was apparently small except during late desiccation stages when the isotopic contrast became great. Eventually, atmospheric exchange, combined with decreasing α and lake size and increasing salinity, stopped further deuterium concentration in the lake. The maximum contrast between atmospheric vapor and lake deuterium contents was about 110%.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(76)90218-0","issn":"00167037","usgsCitation":"Friedman, I., Smith, G., and Hardcastle, K.G., 1976, Studies of quaternary saline lakes-II. Isotopic and compositional changes during desiccation of the brines in Owens Lake, California, 1969-1971: Geochimica et Cosmochimica Acta, v. 40, no. 5, p. 501-511, https://doi.org/10.1016/0016-7037(76)90218-0.","productDescription":"11 p.","startPage":"501","endPage":"511","numberOfPages":"11","costCenters":[],"links":[{"id":218819,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"40","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9ca2e4b08c986b31d465","contributors":{"authors":[{"text":"Friedman, I.","contributorId":95596,"corporation":false,"usgs":true,"family":"Friedman","given":"I.","email":"","affiliations":[],"preferred":false,"id":359799,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, G.I.","contributorId":103694,"corporation":false,"usgs":true,"family":"Smith","given":"G.I.","email":"","affiliations":[],"preferred":false,"id":359800,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hardcastle, Kenneth G.","contributorId":40722,"corporation":false,"usgs":true,"family":"Hardcastle","given":"Kenneth","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":359798,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010215,"text":"70010215 - 1976 - Carbon, hydrogen, and oxygen isotope studies of the regional metamorphic complex at Naxos, Greece","interactions":[],"lastModifiedDate":"2024-03-08T16:53:57.178569","indexId":"70010215","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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":"Carbon, hydrogen, and oxygen isotope studies of the regional metamorphic complex at Naxos, Greece","docAbstract":"<p>At Naxos, Greece, a migmatite dome is surrounded by schists and marbles of decreasing metamorphic grade. Sillimanite, kyanite, biotite, chlorite, and glaucophane zones are recognized at successively greater distances from the migmatite dome. Quartz-muscovite and quartz-biotite oxygen isotope and mineralogie temperatures range from 350 to 700°C.</p><p>The metamorphic complex can be divided into multiple schist-rich (including migmatites) and marblerich zones. The δ<sup>18</sup>O values of silicate minerals in migmatite and schist units and quartz segregations in the schist-rich zones decrease with increase in metamorphic grades. The calculated δ<sup>18</sup>O<sub>H2O</sub><span>&nbsp;</span>values of the metamorphic fluids in the schist-rich zones decrease from about 15‰ in the lower grades to an average of about 8.5‰ in the migmatite.</p><p>The δD values of OH-minerals (muscovite, biotite, chlorite, and glaucophane) in the schist-rich zones also decrease with increase in grade. The calculated δD<sub>H2O</sub><span>&nbsp;</span>values for the metamorphic fluid decrease from −5‰ in the glaucophane zone to an average of about −70‰ in the migmatite. The δD values of water in fluid inclusions in quartz segregations in the higher grade rocks are consistent with this trend.</p><p>Theδ<sup>18</sup>O values of silicate minerals and quartz segregations in marble-rich zones are usually very large and were controlled by exchange with the adjacent marbles. The δD values of the OH minerals in some marble-rich zones may reflect the value of water contained in the rocks prior to metamorphism.</p><p>Detailed data on 20 marble units show systematic variations of δ<sup>18</sup>O values which depend upon metamorphic grade. Below the 540°C isograd very steep δ<sup>18</sup>O gradients at the margins and large δ<sup>18</sup>O values in the interior of the marbles indicate that oxygen isotope exchange with the adjacent schist units was usually limited to the margins of the marbles with more exchange occurring in the stratigraphic bottom than in the top margins. Above the 540°C isograd lower δ<sup>18</sup>O values occur in the interior of the marble units reflecting a greater degree of recrystallization and the occurrence of Ca-Mg-silicates.</p><p>Almost all the δ<sup>13</sup>C values of the marbles are in the range of unaltered marine limestones. Nevertheless, the δ<sup>13</sup>C values of most marble units show a general correlation with δ<sup>18</sup>O values.</p><p>The<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>CO</mtext><msub><mi></mi><mn>2</mn></msub><mtext>H</mtext><msub><mi></mi><mn>2</mn></msub><mtext>O</mtext></math>\"><span class=\"MJX_Assistive_MathML\">CO<sub>2</sub>H<sub>2</sub>O</span></span></span><span>&nbsp;</span>mole ratio of fluid inclusions in quartz segregations range from 0.01 to 2. Theδ<sup>13</sup>C values of the CO<sub>2</sub><span>&nbsp;</span>range from −8.0 to 3.6‰ and indicate that at some localities CO<sub>2</sub><span>&nbsp;</span>in the metamorphic fluid was not in carbon isotopic equilibrium with the marbles.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(76)90045-4","issn":"00167037","usgsCitation":"Rye, R.O., Schuiling, R., Rye, D., and Jansen, J., 1976, Carbon, hydrogen, and oxygen isotope studies of the regional metamorphic complex at Naxos, Greece: Geochimica et Cosmochimica Acta, v. 40, no. 9, p. 1031-1049, https://doi.org/10.1016/0016-7037(76)90045-4.","productDescription":"19 p.","startPage":"1031","endPage":"1049","numberOfPages":"19","costCenters":[],"links":[{"id":219131,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"40","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f36be4b0c8380cd4b7d2","contributors":{"authors":[{"text":"Rye, R. O.","contributorId":66208,"corporation":false,"usgs":true,"family":"Rye","given":"R.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":358326,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schuiling, R.D.","contributorId":69019,"corporation":false,"usgs":true,"family":"Schuiling","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":358327,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rye, D.M.","contributorId":38288,"corporation":false,"usgs":true,"family":"Rye","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":358325,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jansen, J.B.H.","contributorId":7424,"corporation":false,"usgs":true,"family":"Jansen","given":"J.B.H.","email":"","affiliations":[],"preferred":false,"id":358324,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1014349,"text":"1014349 - 1976 - Vitamin E and selenium interrelations in the diet of Atlantic salmon (Salmo salar): Gross, histological and biochemical deficiency signs","interactions":[],"lastModifiedDate":"2018-01-31T16:14:44","indexId":"1014349","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2403,"text":"Journal of Nutrition","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Vitamin E and selenium interrelations in the diet of Atlantic salmon (<i>Salmo salar</i>): Gross, histological and biochemical deficiency signs","title":"Vitamin E and selenium interrelations in the diet of Atlantic salmon (Salmo salar): Gross, histological and biochemical deficiency signs","docAbstract":"<p><span>Either simultaneous or separate dietary deficiencies of vitamin E and selenium in Atlantic salmon during first 4 weeks of feeding caused twice the mortality shown in fish fed both supplemental vitamin E (0.5 IU/g dry diet) and selenium (0.1 µg/g). Subsequent dietary repletion with both vitamin E and selenium significantly reduced mortality during the following 2 weeks. Larger salmon (0.9 g initial mean weight), with vitamin E deficiency with or without selenium resulted in the following deficiency signs: extreme anemia, pale gills, anisocytosis, poikilocytosis, elevated plasma protein, exudative diathesis, dermal depigmentation, in vitro ascorbic acid-stimulated peroxidation in hepatic microsomes, yellow-orange liver color, yellow-brown intestinal contents, enlarged gall bladder distended with dark green bile, low vitamin E in carcass and hepatic tissue, muscular dystrophy, increased carcass fat and water, and a response to handling characterized by a transitory fainting with interruption in swimming. A deficiency of dietary selenium suppressed plasma glutathione peroxidase activity. Supplemental selenium with vitamin E significantly increased tocopherol activity in hepatic, but not carcass tissues. Supplements of both vitamin E and selenium were necessary to prevent muscular dystrophy.</span></p>","language":"English","publisher":"Oxford Academic","doi":"10.1093/jn/106.7.892","usgsCitation":"Poston, H.A., Combs, G.F., and Leibovitz, L., 1976, Vitamin E and selenium interrelations in the diet of Atlantic salmon (Salmo salar): Gross, histological and biochemical deficiency signs: Journal of Nutrition, v. 106, no. 7, p. 892-904, https://doi.org/10.1093/jn/106.7.892.","productDescription":"13 p.","startPage":"892","endPage":"904","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131416,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"106","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdb2f","contributors":{"authors":[{"text":"Poston, Hugh A.","contributorId":12535,"corporation":false,"usgs":true,"family":"Poston","given":"Hugh","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":320227,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Combs, G. F. Jr.","contributorId":31352,"corporation":false,"usgs":false,"family":"Combs","given":"G.","suffix":"Jr.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":320228,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leibovitz, Louis","contributorId":41781,"corporation":false,"usgs":false,"family":"Leibovitz","given":"Louis","email":"","affiliations":[],"preferred":false,"id":320229,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011148,"text":"70011148 - 1976 - Turbidity distribution in the Atlantic Ocean","interactions":[],"lastModifiedDate":"2023-09-25T16:15:45.112517","indexId":"70011148","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1372,"text":"Deep-Sea Research and Oceanographic Abstracts","active":true,"publicationSubtype":{"id":10}},"title":"Turbidity distribution in the Atlantic Ocean","docAbstract":"<p><span>The regional coverage of Lamont nephelometer data in the North and South Atlantic can be used to map seawater turbidity at all depths. At the level of the clearest water, in the mid-depth regions, the turbidity distribution primarily reflects the pattern of productivity in the surface waters. This suggests that the ‘background’ turbidity level in the oceans is largely a function of biogenic fallout. The bottom waters of the western Atlantic generally exhibit large increases in turbidity. The most intense benthic nepheloid layers are in the southwestern Argentine basin and northern North American basin; the lowest bottom water turbidity in the western Atlantic is in the equatorial regions. Both the Argentine and North American basin bottom waters appear to derive their high turbidity largely from local resuspension of terrigenous input in these basins. In contrast to the west, the eastern Atlantic basins show very low turbidities with the exception of three regions: the Mediterranean outflow area, the Cape basin, and the West European basin.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0011-7471(76)90888-3","usgsCitation":"Eittreim, S., Thorndike, E.M., and Sullivan, L., 1976, Turbidity distribution in the Atlantic Ocean: Deep-Sea Research and Oceanographic Abstracts, v. 23, no. 12, p. 1115-1127, https://doi.org/10.1016/0011-7471(76)90888-3.","productDescription":"13 p.","startPage":"1115","endPage":"1127","numberOfPages":"13","costCenters":[],"links":[{"id":220880,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Atlantic Ocean","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n  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M.","contributorId":43101,"corporation":false,"usgs":false,"family":"Thorndike","given":"E.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":360394,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sullivan, L.","contributorId":85327,"corporation":false,"usgs":true,"family":"Sullivan","given":"L.","email":"","affiliations":[],"preferred":false,"id":360396,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2002190,"text":"2002190 - 1976 - Monitoring the breeding habitats of migratory waterfowl","interactions":[],"lastModifiedDate":"2017-10-20T12:32:54","indexId":"2002190","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Monitoring the breeding habitats of migratory waterfowl","docAbstract":"No abstract available at this time","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"ERTS-1: a new window on our planet.","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","usgsCitation":"Gilmer, D., Klett, A., and Work, E., 1976, Monitoring the breeding habitats of migratory waterfowl, chap. <i>of</i> ERTS-1: a new window on our planet., p. 321-325.","productDescription":"5 p.","startPage":"321","endPage":"325","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true},{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":199113,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635bca","contributors":{"authors":[{"text":"Gilmer, D.S.","contributorId":22270,"corporation":false,"usgs":true,"family":"Gilmer","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":326135,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klett, A.T.","contributorId":34857,"corporation":false,"usgs":true,"family":"Klett","given":"A.T.","email":"","affiliations":[],"preferred":false,"id":326136,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Work, E.A.","contributorId":7650,"corporation":false,"usgs":true,"family":"Work","given":"E.A.","affiliations":[],"preferred":false,"id":326134,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011045,"text":"70011045 - 1976 - Submarine geothermal resources","interactions":[],"lastModifiedDate":"2012-03-12T17:18:35","indexId":"70011045","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"Submarine geothermal resources","docAbstract":"Approximately 20% of the earth's heat loss (or 2 ?? 1012 cal/s) is released through 1% of the earth's surface area and takes the form of hydrothermal discharge from young (Pleistocene or younger) rocks adjacent to active seafloor-spreading centers and submarine volcanic areas. This amount is roughly equivalent to man's present gross energy consumption rate. A sub-seafloor geothermal reservoir, to be exploitable under future economic conditions, will have to be hot, porous, permeable, large, shallow, and near an energy-deficient, populated land mass. Furthermore, the energy must be recoverable using technology achievable at a competitive cost and numerous environmental, legal and institutional problems will have to be overcome. The highest-temperature reservoirs should be found adjacent to the zones of the seafloor extension or volcanism that are subject to high sedimentation rates. The relatively impermeable sediments reduce hydrothermal-discharge flow rates, forcing the heat to be either conducted away or released by high-temperature fluids, both of which lead to reservoir temperatures that can exceed 300??C. There is evidence that the oceanic crust is quite permeable and porous and that it was amenable to deep (3-5 km) penetration by seawater at least some time in the early stages of its evolution. Most of the heat escapes far from land, but there are notable exceptions. For example, in parts of the Gulf of California, thermal gradients in the bottom sediments exceed 1??C/m. In the coastal areas of the Gulf of California, where electricity and fresh water are at a premium, this potential resource lies in shallow water (< 200 m) and within sight of land. Other interesting areas include the Sea of Japan, the Sea of Okhotsk and the Andaman Sea along the margins of the western Pacific, the Tyrrhenian Sea west of Italy, and the southern California borderland and west flank of the Juan de Fuca Ridge off the west coast of the United States. Many questions remain to be answered about the physical and other characteristics of these systems before they can be considered a viable resource. Until several of the most promising areas are carefully defined and drilled, the problem will remain unresolved. ?? 1976.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03770273","usgsCitation":"Williams, D., 1976, Submarine geothermal resources: Journal of Volcanology and Geothermal Research, v. 1, no. 1, p. 85-100.","startPage":"85","endPage":"100","numberOfPages":"16","costCenters":[],"links":[{"id":220811,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9d24e4b08c986b31d67a","contributors":{"authors":[{"text":"Williams, D.L.","contributorId":7681,"corporation":false,"usgs":true,"family":"Williams","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":360150,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175585,"text":"70175585 - 1976 - Records of wells, drillers' logs, water-level measurements, and chemical analyses of ground water in Brazoria, Fort Bend, and Waller Counties, Texas, 1966-74","interactions":[],"lastModifiedDate":"2016-08-17T11:33:38","indexId":"70175585","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5174,"text":"Texas Water Development Board Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"201","title":"Records of wells, drillers' logs, water-level measurements, and chemical analyses of ground water in Brazoria, Fort Bend, and Waller Counties, Texas, 1966-74","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Texas Water Development Board","usgsCitation":"Naftel, W.L., Vaught, K.D., and Fleming, B., 1976, Records of wells, drillers' logs, water-level measurements, and chemical analyses of ground water in Brazoria, Fort Bend, and Waller Counties, Texas, 1966-74: Texas Water Development Board Report 201, 90 p.","productDescription":"90 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326654,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58b57e4b03bcb0104bc4f","contributors":{"authors":[{"text":"Naftel, W. L.","contributorId":173750,"corporation":false,"usgs":false,"family":"Naftel","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":645757,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vaught, Kenneth D.","contributorId":21956,"corporation":false,"usgs":true,"family":"Vaught","given":"Kenneth","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":645758,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fleming, Bobbie","contributorId":173751,"corporation":false,"usgs":false,"family":"Fleming","given":"Bobbie","email":"","affiliations":[],"preferred":false,"id":645759,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70171417,"text":"70171417 - 1976 - Hydrology of the North Cascades region, Washington: 1. Runoff, precipitation, and storage characteristics","interactions":[],"lastModifiedDate":"2018-02-04T14:30:25","indexId":"70171417","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Hydrology of the North Cascades region, Washington: 1. Runoff, precipitation, and storage characteristics","docAbstract":"<p>The time and space distributions of measured precipitation and measured runoff and of spring storage, which is approximately equal to the subsequent summer runoff of snowmelt and stored groundwater, have been analyzed for the North Cascades region of Washington. Neither precipitation nor runoff shows a consistent relationship with altitude, chiefly because of precipitation-shadowing effects in this region of high relief. The relationship between mean annual precipitation and altitude is improved considerably when a topographic mean altitude is used instead of the actual altitude of the weather station. However, the improvement is not sufficient to explain a number of discrepancies that still occur. Some of the scatter in a precipitation-altitude plot appears to be due to a deficient precipitation catch by high-altitude gages. When the dependence of runoff on precipitation was examined on an annual, seasonal, and monthly basis, it was found that only a few low-altitude gages correlated well with basin runoff. In several instances, annual (water year) runoff could be better predicted from winter precipitation than from annual precipitation. Precipitation and runoff were tested for changes with time and both appeared to have been increasing slightly but not at a statistically significant level. When the summer (May–September) fraction of the total annual runoff is plotted against mean basin altitude, a consistent, physically reasonable, mildly curvilinear relationship is revealed. On the basis of this relationship, by using several drainages with diverse area-altitude profiles the spring storage versus altitude distribution can be estimated for each basin. The area-altitude distribution is used instead of the mean altitude in this calculation because of the apparent nonlinear relationship between runoff and altitude.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR012i002p00187","usgsCitation":"Rasmussen, L.A., and Tangborn, W.V., 1976, Hydrology of the North Cascades region, Washington: 1. 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 \"}}]}","volume":"12","issue":"2","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"574eb5cfe4b0ee97d51a83c8","contributors":{"authors":[{"text":"Rasmussen, Lowell A.","contributorId":36930,"corporation":false,"usgs":true,"family":"Rasmussen","given":"Lowell","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":630930,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tangborn, Wendell V.","contributorId":32152,"corporation":false,"usgs":true,"family":"Tangborn","given":"Wendell","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":630931,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70171425,"text":"70171425 - 1976 - Hydrology of the North Cascades region, Washington: 2. A proposed hydrometeorological streamflow prediction method","interactions":[],"lastModifiedDate":"2018-02-04T14:32:02","indexId":"70171425","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Hydrology of the North Cascades region, Washington: 2. A proposed hydrometeorological streamflow prediction method","docAbstract":"<p>On the basis of a linear relationship between winter (October-April) precipitation and annual runoff from a drainage basin (Rasmussen and Tangborn, 1976) a physically reasonable model for predicting summer (May-September) streamflow from drainages in the North Cascades region was developed. This hydrometeorological prediction method relates streamflow for a season beginning on the day of prediction to the storage (including snow, ice, soil moisture, and groundwater) on that day. The spring storage is inferred from an input-output relationship based on the principle of conservation of mass: spring storage equals winter precipitation on the basin less winter runoff from the basin and less winter evapotranspiration, which is presumed to be small. The method of prediction is based on data only from the years previous to the one for which the prediction is made, and the system is revised each year as data for the previous year become available. To improve the basin storage estimate made in late winter or early spring, a short-season runoff prediction is made. The errors resulting from this short-term prediction are used to revise the storage estimate and improve the later prediction. This considerably improves the accuracy of the later prediction, especially for periods early in the summer runoff season. The optimum length for the test period appears to be generally less than a month for east side basins and between 1 and 2 months for those on the west side of the Cascade Range. The time distribution of the total summer runoff can be predicted when this test season is used so that on May 1 monthly streamflow for the May-September season can be predicted. It was found that summer precipitation and the time of minimum storage are two error sources that were amenable to analysis. For streamflow predictions in seasons beginning in early spring the deviation of the subsequent summer precipitation from a long-period average will contribute up to 53% of the prediction error. This contribution decreases to nearly zero during the summer and then rises slightly for late summer predictions. The reason for the smaller than expected effect of summer precipitation is thought to be due to the compensating effect of increased evaporative losses and increased infiltration when precipitation is greater than normal during the summer months. The error caused by the beginning winter month (assumed to be October in this study) not coinciding with the time of minimum storage was examined; it appears that October may be the best average beginning winter month for most drainages but that a more detailed study is needed. The optimum beginning of the winter season appears to vary from August to October when individual years are examined. These results demonstrate that standard precipitation and runoff measurements in the North Cascades region are adequate for constructing a predictive hydrologic model. This model can be used to make streamflow predictions that compare favorably with current multiple regression methods based on mountain snow surveys. This method has the added advantages of predicting the space and time distributions of storage and summer runoff.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR012i002p00203","usgsCitation":"Tangborn, W.V., and Rasmussen, L.A., 1976, Hydrology of the North Cascades region, Washington: 2. A proposed hydrometeorological streamflow prediction method: Water Resources Research, v. 12, no. 2, p. 203-216, https://doi.org/10.1029/WR012i002p00203.","productDescription":"14 p.","startPage":"203","endPage":"216","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":321911,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Cascade 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,{"id":70176026,"text":"70176026 - 1976 - Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1975","interactions":[],"lastModifiedDate":"2016-08-23T16:22:30","indexId":"70176026","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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":"35","title":"Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1975","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Rappmund, R.A., 1976, Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1975: Edwards Underground Water District Bulletin 35, 7 p.","productDescription":"7 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":327754,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73dde4b03fd6b7df2d03","contributors":{"authors":[{"text":"Rappmund, R. A.","contributorId":173985,"corporation":false,"usgs":false,"family":"Rappmund","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":646814,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175586,"text":"70175586 - 1976 - Records of wells, drillers' logs, water-level measurements, and chemical analyses of ground water in Chambers, Liberty, and Montgomery Counties, Texas, 1966-74","interactions":[],"lastModifiedDate":"2016-08-17T11:37:35","indexId":"70175586","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5174,"text":"Texas Water Development Board Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"202","title":"Records of wells, drillers' logs, water-level measurements, and chemical analyses of ground water in Chambers, Liberty, and Montgomery Counties, Texas, 1966-74","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Texas Water Development Board","usgsCitation":"Naftel, W.L., Fleming, B., and Vaught, K.D., 1976, Records of wells, drillers' logs, water-level measurements, and chemical analyses of ground water in Chambers, Liberty, and Montgomery Counties, Texas, 1966-74: Texas Water Development Board Report 202, 62 p.","productDescription":"62 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326658,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58b57e4b03bcb0104bc53","contributors":{"authors":[{"text":"Naftel, W. L.","contributorId":173750,"corporation":false,"usgs":false,"family":"Naftel","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":645762,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fleming, Bobbie","contributorId":173751,"corporation":false,"usgs":false,"family":"Fleming","given":"Bobbie","email":"","affiliations":[],"preferred":false,"id":645763,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vaught, Kenneth D.","contributorId":21956,"corporation":false,"usgs":true,"family":"Vaught","given":"Kenneth","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":645764,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":67966,"text":"ha566 - 1976 - Teton Dam flood of June 1976, St. Anthony quadrangle, Idaho","interactions":[],"lastModifiedDate":"2013-11-12T13:04:54","indexId":"ha566","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"566","title":"Teton Dam flood of June 1976, St. Anthony quadrangle, Idaho","docAbstract":"The failure of the Teton Dam caused extreme flooding along the Teton River, Henrys Fork, and Snake River in southeastern Idaho on June 5-8, 1976. No flooding occurred downstream from American Falls Reservoir. The inundated areas and maximum water-surface elevations are shown in a series of 17 hydrologic atlases. The area covered by the atlases extends from Teton Dam downstream to American Falls Reservoir, a distance of 100 miles. The extent of flooding shown on the maps was obtained by field inspections and aerial photographs made during and immediately after the flood. There may be small isolated areas within the boundaries shown that were not flooded, but the identification of these sites was beyond the scope of the study. The elevation data shown are mean-sea-level elevations of high-water marks identified in the field. This particular map (in the 17-map series) shows conditions in the St. Anthony quadrangle. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha566","usgsCitation":"Thomas, C., Ray, H.A., and Matthai, H.F., 1976, Teton Dam flood of June 1976, St. Anthony quadrangle, Idaho: U.S. Geological Survey Hydrologic Atlas 566, 1 Plate: 21.00 x 27.20 inches, https://doi.org/10.3133/ha566.","productDescription":"1 Plate: 21.00 x 27.20 inches","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":185735,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89195,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/566/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","projection":"Polyconic projection","datum":"1927 North American Datum","country":"United States","state":"Idaho","otherGeospatial":"St. Anthony Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.75,43.875 ], [ -111.75,44.0 ], [ -111.625,44.0 ], [ -111.625,43.875 ], [ -111.75,43.875 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699d7b","contributors":{"authors":[{"text":"Thomas, Cecil A.","contributorId":107373,"corporation":false,"usgs":true,"family":"Thomas","given":"Cecil A.","affiliations":[],"preferred":false,"id":277415,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ray, Herman A.","contributorId":106199,"corporation":false,"usgs":true,"family":"Ray","given":"Herman","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":277413,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Matthai, Howard F.","contributorId":106491,"corporation":false,"usgs":true,"family":"Matthai","given":"Howard","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":277414,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70195643,"text":"70195643 - 1976 - Disease problems and needs","interactions":[],"lastModifiedDate":"2018-02-26T08:19:17","indexId":"70195643","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Disease problems and needs","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Transactions of the second international waterfowl symposium","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Second international waterfowl symposium","conferenceDate":"February 13-15, 1976","conferenceLocation":"St. Louis, MO","language":"English","publisher":"Ducks Unlimited","usgsCitation":"Friend, M., 1976, Disease problems and needs, <i>in</i> Transactions of the second international waterfowl symposium, St. Louis, MO, February 13-15, 1976, p. 2-7.","productDescription":"6 p.","startPage":"2","endPage":"7","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":351988,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff5221e4b0da30c1bfdca2","contributors":{"authors":[{"text":"Friend, Milton 0000-0002-2882-3629","orcid":"https://orcid.org/0000-0002-2882-3629","contributorId":31332,"corporation":false,"usgs":true,"family":"Friend","given":"Milton","email":"","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":729537,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175539,"text":"70175539 - 1976 - Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1974","interactions":[],"lastModifiedDate":"2017-06-14T11:05:45","indexId":"70175539","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1974","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70175539","usgsCitation":"Gonzalez, V., 1976, Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1974: Open-File Report, 109 p., https://doi.org/10.3133/70175539.","productDescription":"109 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326564,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Texas","city":"San Antonio","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.8165283203125,\n              29.123373210819224\n            ],\n            [\n              -98.19580078125,\n              29.123373210819224\n            ],\n            [\n              -98.19580078125,\n              29.699982298744377\n            ],\n            [\n              -98.8165283203125,\n              29.699982298744377\n            ],\n            [\n              -98.8165283203125,\n              29.123373210819224\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b43951e4b03bcb01039ffb","contributors":{"authors":[{"text":"Gonzalez, Victor","contributorId":173702,"corporation":false,"usgs":false,"family":"Gonzalez","given":"Victor","affiliations":[],"preferred":false,"id":645581,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175535,"text":"70175535 - 1976 - Hydrologic data for Mountain Creek, Trinity River Basin, Texas, 1974","interactions":[],"lastModifiedDate":"2016-08-16T10:56:11","indexId":"70175535","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Hydrologic data for Mountain Creek, Trinity River Basin, Texas, 1974","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70175535","usgsCitation":"Buckner, H., 1976, Hydrologic data for Mountain Creek, Trinity River Basin, Texas, 1974: Open-File Report, 13 p., https://doi.org/10.3133/70175535.","productDescription":"13 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326560,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b43950e4b03bcb01039fe4","contributors":{"authors":[{"text":"Buckner, H.D.","contributorId":49783,"corporation":false,"usgs":true,"family":"Buckner","given":"H.D.","email":"","affiliations":[],"preferred":false,"id":645576,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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