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,{"id":1014341,"text":"1014341 - 1978 - Abundant supply of clean water is absolutely essential for commercial fish farming","interactions":[],"lastModifiedDate":"2012-02-02T00:04:31","indexId":"1014341","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1277,"text":"Commercial Fish Farmer and Aquaculture News","active":true,"publicationSubtype":{"id":10}},"title":"Abundant supply of clean water is absolutely essential for commercial fish farming","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Commercial Fish Farmer and Aquaculture News","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"None/FF","usgsCitation":"Martin, M., 1978, Abundant supply of clean water is absolutely essential for commercial fish farming: Commercial Fish Farmer and Aquaculture News, v. 4, no. 4, p. 15-18.","productDescription":"p. 15-18","startPage":"15","endPage":"18","numberOfPages":"4","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131550,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a36a7","contributors":{"authors":[{"text":"Martin, M.","contributorId":103217,"corporation":false,"usgs":true,"family":"Martin","given":"M.","affiliations":[],"preferred":false,"id":320217,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012860,"text":"70012860 - 1978 - The potential source of lead in the Permian Kupferschiefer bed of Europe and some selected Paleozoic mineral deposits in the Federal Republic of Germany","interactions":[],"lastModifiedDate":"2012-03-12T17:19:02","indexId":"70012860","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1336,"text":"Contributions to Mineralogy and Petrology","active":true,"publicationSubtype":{"id":10}},"title":"The potential source of lead in the Permian Kupferschiefer bed of Europe and some selected Paleozoic mineral deposits in the Federal Republic of Germany","docAbstract":"New lead isotopic compositions have been measured for Paleozoic bedded and vein ore deposits of Europe by the high precision thermal emission (triple filament) technique. Eleven samples have been analyzed from the Upper Permian Kupferschiefer bed with representatives from Poland to England, three samples from the Middle Devonian Rammelsberg deposit and one from the Middle Devonian Meggen deposit, both of which are conformable ore lenses and are in the Federal Republic of Germany (FRG); and also two vein deposits from the FRG were analyzed, from Ramsbeck in Devonian host rocks and from Grund in Carboniferous host rocks. For Kupferschiefer bed samples from Germany, the mineralization is of variable lead isotopic composition and appears to have been derived about 250 m.y. ago from 1700 m.y. old sources, or detritus of this age, in Paleozoic sedimentary rocks. Samples from England, Holland, and Poland have different isotopic characteristics from the German samples, indicative of significantly different source material (perhaps older). The isotopic variability of the samples from the Kupferschiefer bed in Germany probably favors the lead containing waters coming from shoreward (where poor mixing is to be expected) rather than basinward (where better mixing is likely) directions. The data thus support the interpretation of the metal source already given by Wedepohl in 1964. Data on samples from Rammelsberg and Meggen tend to be slightly less radiogenic than for the Kupferschiefer, about the amount expected if the leads were all derived from the same source material but 100 to 150 m.y. apart in time. The vein galena from Ramsbeck is similar to that from Rammelsberg conformable ore lenses, both in rocks of Devonian age; vein galena from Grund in Upper Carboniferous country rocks is similar to some bedded Kupferschiefer mineralization in Permian rocks, as if the lead composition was formed at about the same time and from similar source material as the bedded deposits. Although heat has played a more significant role in the formation of some of these deposits (veins and Rammelsberg-Meggen) than in others (Kupferschiefer), there is no indication of radically different sources for the lead, all apparently coming from sedimentary source material containing Precambrian detritus. One feldspar lead sample from the Brocken-Oker Granite is not the same in isotopic composition as any of the ores analyzed. ?? 1978 Springer-Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Contributions to Mineralogy and Petrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF00375513","issn":"00107999","usgsCitation":"Wedepohl, K., Delevaux, M., and Doe, B.R., 1978, The potential source of lead in the Permian Kupferschiefer bed of Europe and some selected Paleozoic mineral deposits in the Federal Republic of Germany: Contributions to Mineralogy and Petrology, v. 65, no. 3, p. 273-281, https://doi.org/10.1007/BF00375513.","startPage":"273","endPage":"281","numberOfPages":"9","costCenters":[],"links":[{"id":222383,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205230,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00375513"}],"volume":"65","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baebce4b08c986b3242e0","contributors":{"authors":[{"text":"Wedepohl, K.H.","contributorId":74639,"corporation":false,"usgs":true,"family":"Wedepohl","given":"K.H.","email":"","affiliations":[],"preferred":false,"id":364694,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Delevaux, M.H.","contributorId":27853,"corporation":false,"usgs":true,"family":"Delevaux","given":"M.H.","email":"","affiliations":[],"preferred":false,"id":364692,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Doe, B. R.","contributorId":52173,"corporation":false,"usgs":true,"family":"Doe","given":"B.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":364693,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70182450,"text":"70182450 - 1978 - Arsenic in streams, stream sediments, and ground water, Fairbanks area, Alaska","interactions":[],"lastModifiedDate":"2017-06-07T17:01:06","indexId":"70182450","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1539,"text":"Environmental Geology","active":true,"publicationSubtype":{"id":10}},"title":"Arsenic in streams, stream sediments, and ground water, Fairbanks area, Alaska","docAbstract":"<p><span>Arsenic concentrations of less than 5 ppb to as large as 1,260 ppb in stream waters and from 5 ppm to 4,000 ppm in stream sediments were found in the Pedro Dome-Cleary Summit area, Alaska. Waters from three of 20 wells sampled had arsenic concentrations exceeding the U.S. Public Health Service recommended limit of 50 ppb. The high arsenic levels are a consequence of arsenic enrichment in the rocks of the area. Placer and lode-gold mining may increase the arsenic content of the waters by exposing arsenic-containing rocks to surface waters and by increasing the load of arsenic-rich sediments in the streams. Finding these disturbingly large concentrations of arsenic in the waters of the Fairbanks area was the major result of this work, inasmuch as a subsequent study (to be published) revealed arsenic concentrations as large as 10 ppm in domestic wells and prompted an extensive study by Federal and State agencies of the health hazard posed by these arsenic-rich waters.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/BF02380485","usgsCitation":"Wilson, F.H., and Hawkins, D.B., 1978, Arsenic in streams, stream sediments, and ground water, Fairbanks area, Alaska: Environmental Geology, v. 2, no. 4, p. 195-202, https://doi.org/10.1007/BF02380485.","productDescription":"8 p.","startPage":"195","endPage":"202","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":336054,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","city":"Fairbanks","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -147.81280517578125,\n              64.86177466110345\n            ],\n            [\n              -147.030029296875,\n              64.86177466110345\n            ],\n            [\n              -147.030029296875,\n              65.23370465451454\n            ],\n            [\n              -147.81280517578125,\n              65.23370465451454\n            ],\n            [\n              -147.81280517578125,\n              64.86177466110345\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"2","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58b002dee4b01ccd54fb2839","contributors":{"authors":[{"text":"Wilson, Frederic H. 0000-0003-1761-6437 fwilson@usgs.gov","orcid":"https://orcid.org/0000-0003-1761-6437","contributorId":67174,"corporation":false,"usgs":true,"family":"Wilson","given":"Frederic","email":"fwilson@usgs.gov","middleInitial":"H.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":671154,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hawkins, D. B.","contributorId":43366,"corporation":false,"usgs":true,"family":"Hawkins","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":671155,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":96530,"text":"96530 - 1978 - Use of Landsat data to assess waterfowl habitat quality","interactions":[],"lastModifiedDate":"2012-02-02T00:03:56","indexId":"96530","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Use of Landsat data to assess waterfowl habitat quality","docAbstract":"No abstract available at this time","language":"English","collaboration":"Final Rept. NASA Goddard Space Flight Center, Greenbelt, MD.","usgsCitation":"Colwell, J., Gilmer, D., Work, E., Rebel, D., and Roller, N., 1978, Use of Landsat data to assess waterfowl habitat quality, 83 p.","productDescription":"83 p.","startPage":"83","numberOfPages":"83","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":128176,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0e9e","contributors":{"authors":[{"text":"Colwell, J.","contributorId":61773,"corporation":false,"usgs":true,"family":"Colwell","given":"J.","email":"","affiliations":[],"preferred":false,"id":299768,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gilmer, D.S.","contributorId":22270,"corporation":false,"usgs":true,"family":"Gilmer","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":299767,"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":299766,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rebel, D.L.","contributorId":74700,"corporation":false,"usgs":true,"family":"Rebel","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":299769,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Roller, N.E.G.","contributorId":74703,"corporation":false,"usgs":true,"family":"Roller","given":"N.E.G.","email":"","affiliations":[],"preferred":false,"id":299770,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70012492,"text":"70012492 - 1978 - Empirical model of Skeletonema costatum photosynthetic rate, with applications in the San Francisco Bay estuary","interactions":[],"lastModifiedDate":"2023-02-01T17:40:47.965072","indexId":"70012492","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":664,"text":"Advances in Water Resources","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Empirical model of <i>Skeletonema costatum</i> photosynthetic rate, with applications in the San Francisco Bay estuary","title":"Empirical model of Skeletonema costatum photosynthetic rate, with applications in the San Francisco Bay estuary","docAbstract":"<p>An empirical model of<span>&nbsp;</span><i>Skeletonema costatum</i><span>&nbsp;</span>photosynthetic rate is developed and fit to measurements of photosynthesis selected from the literature. Because the model acknowledges existence of: 1) a light-temperature interaction (by allowing optimum irradiance to vary with temperature), 2) light inhibition, 3) temperature inhibition, and 4) a salinity effect, it accurately estimates photosynthetic rates measured over a wide range of temperature, light intensity, and salinity. Integration of predicted instantaneous rate of photosynthesis with time and depth yields daily net carbon assimilation (pg C cell<sup>−1</sup><span>&nbsp;</span>day<sup>−1</sup>) in a mixed layer of specified depth, when salinity, temperature, daily irradiance and extinction coefficient are known. The assumption of constant carbon quota (pg C cell<sup>−1</sup>) allows for prediction of mean specific growth rate (day<sup>−1</sup>), which can be used in numerical models of<span>&nbsp;</span><i>Skeletonema costatum</i><span>&nbsp;</span>population dynamics.</p><p>Application of the model to northern San Francisco Bay clearly demonstrates the limitation of growth by low light availability, and suggests that large population densities of<span>&nbsp;</span><i>S. costatum</i><span>&nbsp;</span>observed during summer months are not the result of active growth in the central deep channels (where growth rates are consistently predicted to be negative). But predicted growth rates in the lateral shallows are positive during summer and fall, thus offering a testable hypothesis that shoals are the only sites of active population growth by<span>&nbsp;</span><i>S. costatum</i><span>&nbsp;</span>(and perhaps other neritic diatoms) in the northern reach of San Francisco Bay.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0309-1708(78)90040-4","usgsCitation":"Cloern, J.E., 1978, Empirical model of Skeletonema costatum photosynthetic rate, with applications in the San Francisco Bay estuary: Advances in Water Resources, v. 1, no. 5, p. 267-274, https://doi.org/10.1016/0309-1708(78)90040-4.","productDescription":"8 p.","startPage":"267","endPage":"274","numberOfPages":"8","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":222256,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay estuary","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -121.22039965621613,\n              38.24440703031118\n            ],\n            [\n              -122.57745968735097,\n              38.24440703031118\n            ],\n            [\n              -122.57745968735097,\n              37.3957605043622\n            ],\n            [\n              -121.22039965621613,\n              37.3957605043622\n            ],\n            [\n              -121.22039965621613,\n              38.24440703031118\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"1","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a090ce4b0c8380cd51d98","contributors":{"authors":[{"text":"Cloern, James E. 0000-0002-5880-6862 jecloern@usgs.gov","orcid":"https://orcid.org/0000-0002-5880-6862","contributorId":1488,"corporation":false,"usgs":true,"family":"Cloern","given":"James","email":"jecloern@usgs.gov","middleInitial":"E.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":363746,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012524,"text":"70012524 - 1978 - Interpretation of a Landsat image of an unusual flood phenomenon in Australia","interactions":[],"lastModifiedDate":"2017-01-18T15:12:24","indexId":"70012524","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3254,"text":"Remote Sensing of Environment","printIssn":"0034-4257","active":true,"publicationSubtype":{"id":10}},"title":"Interpretation of a Landsat image of an unusual flood phenomenon in Australia","docAbstract":"A Landsat image of part of the flooded area of Cooper Creek, Queensland, Australia, in February 1974, shows large dark areas within the flooded valley. The dark areas are believed to be wet, but unflooded, areas of dark alluvial soil. These striking features, which have not previously been identified on Landsat images, must be properly interpreted so as not to confuse them with clear water.","language":"English","publisher":"Elsevier","doi":"10.1016/0034-4257(78)90033-0","issn":"00344257","usgsCitation":"Robinove, C.J., 1978, Interpretation of a Landsat image of an unusual flood phenomenon in Australia: Remote Sensing of Environment, v. 7, no. 3, p. 219-225, https://doi.org/10.1016/0034-4257(78)90033-0.","productDescription":"7 p.","startPage":"219","endPage":"225","numberOfPages":"7","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":222664,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":289862,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0034-4257(78)90033-0"}],"country":"Australia","state":"Queensland","otherGeospatial":"Cooper Creek","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 140.8027,-26.8875 ], [ 140.8027,-25.006 ], [ 142.9985,-25.006 ], [ 142.9985,-26.8875 ], [ 140.8027,-26.8875 ] ] ] } } ] }","volume":"7","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3d60e4b0c8380cd6350b","contributors":{"authors":[{"text":"Robinove, Charles J.","contributorId":16983,"corporation":false,"usgs":true,"family":"Robinove","given":"Charles","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":363815,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012631,"text":"70012631 - 1978 - Minerals produced during cooling and hydrothermal alteration of ash flow tuff from Yellowstone drill hole Y-5","interactions":[],"lastModifiedDate":"2012-03-12T17:19:03","indexId":"70012631","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","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":"Minerals produced during cooling and hydrothermal alteration of ash flow tuff from Yellowstone drill hole Y-5","docAbstract":"A rhyolitic ash-flow tuff in a hydrothermally active area within the Yellowstone caldera was drilled in 1967, and cores were studied to determine the nature and distribution of primary and secondary mineral phases. The rocks have undergone a complex history of crystallization and hydrothermal alteration since their emplacement 600,000 years ago. During cooling from magmatic temperatures, the glassy groundmass underwent either devitrification to alkali feldspar + ??-cristobalite ?? tridymite or granophyric crystallization to alkali feldspar + quartz. Associated with the zones of granophyric crystallization are prismatic quartz crystals in cavities similar to those termed miarolitic in plutonic rocks. Vapor-phase alkali feldspar, tridymite, magnetite, and sporadic ??-cristobalite were deposited in cavities and in void spaces of pumice fragments. Subsequently, some of the vapor-phase alkali feldspar crystals were replaced by microcrystalline quartz, and the vapor-phase minerals were frosted by a coating of saccharoidal quartz. Hydrothermal minerals occur primarily as linings and fillings of cavities and fractures and as altered mafic phenocrysts. Chalcedony is the dominant mineral related to the present hydrothermal regime and occurs as microcrystalline material mixed with various amounts of hematite and goethite. The chalcedony displays intricate layering and was apparently deposited as opal from silica-rich water. Hematite and goethite also replace both mafic phenocrysts and vapor-phase magnetite. Other conspicuous hydrothermal minerals include montmorillonite, pyrite, mordenite, calcite, and fluorite. Clinoptilolite, erionite, illite, kaolinite, and manganese oxides are sporadic. The hydrothermal minerals show little correlation with temperature, but bladed calcite is restricted to a zone of boiling in the tuff and clearly was deposited when CO2 was lost during boiling. Fractures and breccias filled with chalcedony are common throughout Y-5 and may have been produced by rapid disruption of rock caused by sudden decrease of fluid pressure in fractures, most likely a result of fracturing during resurgent doming in this part of the Yellowstone caldera. The chalcedony probably was deposited as opal or ??-cristobalite from a pre-existing silica floc that moved rapidly into the fractures and breccias immediately after the sudden pressure drop. ?? 1978.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03770273","usgsCitation":"Keith, T.E., and Muffler, L., 1978, Minerals produced during cooling and hydrothermal alteration of ash flow tuff from Yellowstone drill hole Y-5: Journal of Volcanology and Geothermal Research, v. 3, no. 3-4, p. 373-402.","startPage":"373","endPage":"402","numberOfPages":"30","costCenters":[],"links":[{"id":222668,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5ae7e4b0c8380cd6f1df","contributors":{"authors":[{"text":"Keith, T. E. C.","contributorId":11681,"corporation":false,"usgs":true,"family":"Keith","given":"T.","email":"","middleInitial":"E. C.","affiliations":[],"preferred":false,"id":364098,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Muffler, L.J.P.","contributorId":63383,"corporation":false,"usgs":true,"family":"Muffler","given":"L.J.P.","affiliations":[],"preferred":false,"id":364099,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":46273,"text":"ofr78478 - 1978 - Leasable mineral and waterpower land classification map of the Shiprock quadrangle, New Mexico, Arizona, Colorado, and Utah","interactions":[],"lastModifiedDate":"2023-04-18T20:43:13.693648","indexId":"ofr78478","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"78-478","title":"Leasable mineral and waterpower land classification map of the Shiprock quadrangle, New Mexico, Arizona, Colorado, and Utah","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr78478","usgsCitation":"DeCicco, D.A., Patterson, E., and Lutz, G., 1978, Leasable mineral and waterpower land classification map of the Shiprock quadrangle, New Mexico, Arizona, Colorado, and Utah: U.S. Geological Survey Open-File Report 78-478, 1 Plate: 38.40 x 23.67 inches, https://doi.org/10.3133/ofr78478.","productDescription":"1 Plate: 38.40 x 23.67 inches","costCenters":[],"links":[{"id":172244,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":415953,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12955.htm","linkFileType":{"id":5,"text":"html"}},{"id":254787,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0478/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona, Colorado, New Mexico, Utah","otherGeospatial":"Ship Rock quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -110,\n              37\n            ],\n            [\n              -110,\n              36\n            ],\n            [\n              -108,\n              36\n            ],\n            [\n              -108,\n              37\n            ],\n            [\n              -110,\n              37\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8659","contributors":{"authors":[{"text":"DeCicco, Donald A.","contributorId":50173,"corporation":false,"usgs":true,"family":"DeCicco","given":"Donald","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":232989,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Patterson, E. D.","contributorId":56278,"corporation":false,"usgs":true,"family":"Patterson","given":"E. D.","affiliations":[],"preferred":false,"id":232990,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lutz, Gale A.","contributorId":32507,"corporation":false,"usgs":true,"family":"Lutz","given":"Gale A.","affiliations":[],"preferred":false,"id":232988,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26397,"text":"wri7894 - 1978 - Hydrologic appraisal of the water resources of the Homer-Preble Valley, New York","interactions":[],"lastModifiedDate":"2023-03-14T19:44:50.633293","indexId":"wri7894","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","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":"78-94","title":"Hydrologic appraisal of the water resources of the Homer-Preble Valley, New York","docAbstract":"<p>Water resources of Homer-Preble Valley, 1 to 2 miles wide and 9 miles long, in central New York, were appraised because the area is expected to undergo considerable residential development in the near future. The main source of water supply to the residents of the area is the glacial-outwash aquifer. Data indicate that additional pumpage of 5 million to 10 million gallons per day from the aquifer would not seriously reduce the quantity and quality of the water supply. Water-quality analyses indicate that ground water and surface water in the valley are suitable for most uses and generally meet State standards for source waters for drinking.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7894","usgsCitation":"Buller, W., 1978, Hydrologic appraisal of the water resources of the Homer-Preble Valley, New York: U.S. Geological Survey Water-Resources Investigations Report 78-94, v, 31 p., https://doi.org/10.3133/wri7894.","productDescription":"v, 31 p.","costCenters":[],"links":[{"id":157876,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":266236,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0094/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414121,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35281.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New York","otherGeospatial":"Homer-Preble Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -76.208,\n              42.767\n            ],\n            [\n              -76.208,\n              42.642\n            ],\n            [\n              -76.117,\n              42.642\n            ],\n            [\n              -76.117,\n              42.767\n            ],\n            [\n              -76.208,\n              42.767\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6116c2","contributors":{"authors":[{"text":"Buller, William","contributorId":16449,"corporation":false,"usgs":true,"family":"Buller","given":"William","email":"","affiliations":[],"preferred":false,"id":196317,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012550,"text":"70012550 - 1978 - Prediction of capacity factors for aqueous organic solutes adsorbed on a porous acrylic resin","interactions":[],"lastModifiedDate":"2023-03-10T17:47:53.733634","indexId":"70012550","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Prediction of capacity factors for aqueous organic solutes adsorbed on a porous acrylic resin","docAbstract":"<p>The capacity factors of 20 aromatic, allphatic, and allcycllc organic solutes with carboxyl, hydroxyl, amine, and methyl functional groups were determined on Amberlite XAD-8, a porous acrylic resin. The logarithm of the capacity factor, <i>k'</i>, correlated inversely with the logarithm of the aqueous molar solubility with significance of less than 0.001. The log <i>k'</i>-log solubility relationship may be used to predict the capacity of any organic solute for XAD-8 using only the solubility of the solute. The prediction is useful as a guide for determining the proper ratio of sample to column size In the preconcentration of organic solutes from water. The inverse relationship of solubility and capacity is due to the unfavorable entropy of solution of organic solutes which affects both solubility and sorption.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/ac50027a028","usgsCitation":"Thurman, E., Malcolm, R., and Aiken, G., 1978, Prediction of capacity factors for aqueous organic solutes adsorbed on a porous acrylic resin: Analytical Chemistry, v. 50, no. 6, p. 775-779, https://doi.org/10.1021/ac50027a028.","productDescription":"5 p.","startPage":"775","endPage":"779","numberOfPages":"5","costCenters":[],"links":[{"id":222086,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"50","issue":"6","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a81eae4b0c8380cd7b7d1","contributors":{"authors":[{"text":"Thurman, E.M.","contributorId":102864,"corporation":false,"usgs":true,"family":"Thurman","given":"E.M.","affiliations":[],"preferred":false,"id":363879,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Malcolm, Ronald L.","contributorId":46075,"corporation":false,"usgs":true,"family":"Malcolm","given":"Ronald L.","affiliations":[],"preferred":false,"id":866164,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Aiken, G. R. 0000-0001-8454-0984","orcid":"https://orcid.org/0000-0001-8454-0984","contributorId":14452,"corporation":false,"usgs":true,"family":"Aiken","given":"G. R.","affiliations":[],"preferred":false,"id":866165,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012444,"text":"70012444 - 1978 - The solubility of the noble gases He, Ne, Ar, Kr, and Xe in water up to the critical point","interactions":[],"lastModifiedDate":"2012-03-12T17:19:07","indexId":"70012444","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2460,"text":"Journal of Solution Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"The solubility of the noble gases He, Ne, Ar, Kr, and Xe in water up to the critical point","docAbstract":"The solubility of the noble gases Ar, He, Ne, Kr, and Xe in pure water was measured from 298 to 561??K. These data in turn were extrapolated to the critical point of water, thus providing a complete set of Henry's law constants from 274 to 647??K when combined with the existing literature data. Equations describing the behavior of the Henry's law constants over this temperature range are also given. The data do not confirm extrapolations of empirical correlations based on low-temperature solubility data. ?? 1978 Plenum Publishing Corporation.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Solution Chemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers-Plenum Publishers","doi":"10.1007/BF00650811","issn":"00959782","usgsCitation":"Potter, R., and Clynne, M., 1978, The solubility of the noble gases He, Ne, Ar, Kr, and Xe in water up to the critical point: Journal of Solution Chemistry, v. 7, no. 11, p. 837-844, https://doi.org/10.1007/BF00650811.","startPage":"837","endPage":"844","numberOfPages":"8","costCenters":[],"links":[{"id":205226,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00650811"},{"id":222354,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb045e4b08c986b324d49","contributors":{"authors":[{"text":"Potter, R.W. II","contributorId":16857,"corporation":false,"usgs":true,"family":"Potter","given":"R.W.","suffix":"II","email":"","affiliations":[],"preferred":false,"id":363594,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clynne, M.A.","contributorId":90722,"corporation":false,"usgs":true,"family":"Clynne","given":"M.A.","affiliations":[],"preferred":false,"id":363595,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1014061,"text":"1014061 - 1978 - Nifurpirinol (Furanace: P-7138) related lesions on channel catfish Ictalurus punctatus (Rafinesque)","interactions":[],"lastModifiedDate":"2025-02-04T16:46:33.888052","indexId":"1014061","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2286,"text":"Journal of Fish Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Nifurpirinol (Furanace: P-7138) related lesions on channel catfish Ictalurus punctatus (Rafinesque)","docAbstract":"<p><span>Skin lesions developed on channel catfish,&nbsp;</span><i>Ictalurus punctatus</i><span>, exposed to 0-5 mg/1 Furanace for 4 or 14 days. Lesions developed 3 days after the 4-day exposure and on the eleventh day of the 14-day exposure. The lesions continued to develop after the fish were moved to untreated water. The lesions which began as dull areas of skin, sometimes resulted in erosion of skin and muscle which exposed the vertebrae. Bacteria were not isolated from the lesions except those with severely eroded muscle. The gills possessed lesions characteristic of a response to a toxic chemical agent.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1365-2761.1978.tb00010.x","usgsCitation":"Mitchell, A., Grizzle, J., and Plumb, J., 1978, Nifurpirinol (Furanace: P-7138) related lesions on channel catfish Ictalurus punctatus (Rafinesque): Journal of Fish Diseases, v. 1, no. 1, p. 115-121, https://doi.org/10.1111/j.1365-2761.1978.tb00010.x.","productDescription":"7 p.","startPage":"115","endPage":"121","numberOfPages":"7","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131482,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-04-07","publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697466","contributors":{"authors":[{"text":"Mitchell, A.J.","contributorId":16345,"corporation":false,"usgs":true,"family":"Mitchell","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":319695,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grizzle, J.M.","contributorId":57016,"corporation":false,"usgs":true,"family":"Grizzle","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":319697,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Plumb, J.A.","contributorId":38106,"corporation":false,"usgs":true,"family":"Plumb","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":319696,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1003111,"text":"1003111 - 1978 - Feeding habitat use by colonially-breeding herons, egrets, and ibises in North Carolina","interactions":[],"lastModifiedDate":"2017-05-14T09:24:26","indexId":"1003111","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3544,"text":"The Auk","onlineIssn":"1938-4254","printIssn":"0004-8038","active":true,"publicationSubtype":{"id":10}},"title":"Feeding habitat use by colonially-breeding herons, egrets, and ibises in North Carolina","docAbstract":"<p><span>Nine species of herons, egrets, and ibises were followed by airplane from a nesting colony near Beaufort, North Carolina to their feeding sites. Except for Cattle Egrets, which flew exclusively to fields and dumps, the birds flew mainly to saltmarsh habitat. The selection of feeding habitats by Great Egrets and Louisiana Herons was directly related to tidal depth. The Great Egret was the only species that effectively used eelgrass beds, and its use of this habitat was restricted to between 1.5 h before and after low tide. We suspect that shorter-legged herons did not use eelgrass regularly because the water was too deep. Most Great Egrets, White Ibises, Louisiana Herons, and Snowy Egrets used areas near the colony (&lt;4 km). Great Egrets, Black-crowned Night Herons, and White Ibises flew farther from the colony at high than at low tide. Great Egrets traveled farther from the colony when they used thermals; rate of travel to feeding sites was the same, however, whether or not they used thermals. Aggressive encounters were observed at the landing sites of Great Egrets, Louisiana Herons, Snowy Egrets, and Black-crowned Night Herons. In contrast to the other species studied, Cattle Egrets and White Ibises often flew in groups to feeding sites. Indirect evidence supports the hypothesis that colonies can act as \"information centres,\" wherein unsuccessful birds follow successful ones to better feeding locations.</span></p>","language":"English","publisher":"American Ornithological Society","usgsCitation":"Custer, T.W., and Osborn, R.G., 1978, Feeding habitat use by colonially-breeding herons, egrets, and ibises in North Carolina: The Auk, v. 95, no. 4, p. 733-743.","productDescription":"11 p.","startPage":"733","endPage":"743","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true},{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":337810,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/4085359"},{"id":134360,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Carolina","volume":"95","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fde4b07f02db5f5d8a","contributors":{"authors":[{"text":"Custer, Thomas W. 0000-0003-3170-6519 tcuster@usgs.gov","orcid":"https://orcid.org/0000-0003-3170-6519","contributorId":2835,"corporation":false,"usgs":true,"family":"Custer","given":"Thomas","email":"tcuster@usgs.gov","middleInitial":"W.","affiliations":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"preferred":true,"id":312756,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Osborn, Ronald G.","contributorId":76793,"corporation":false,"usgs":true,"family":"Osborn","given":"Ronald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":312755,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1003110,"text":"1003110 - 1978 - Seasonal trends in summer diet of the lapland longspur near Barrow Alaska USA","interactions":[],"lastModifiedDate":"2023-11-29T12:22:00.445513","indexId":"1003110","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3551,"text":"The Condor","active":true,"publicationSubtype":{"id":10}},"title":"Seasonal trends in summer diet of the lapland longspur near Barrow Alaska USA","docAbstract":"Contents of lapland longspur [Calcarius lapponicus] stomachs and esophagi were sampled near Barrow, Alaska [USA], from May-Aug. in 1969, 1971, 1972 and 1973. Data from stomach contents were corrected for differential digestion of prey items. Longspurs shifted seasonally from larval to adult arthropods and back to larvae, responding to changes in the abundance of these prey items. Seeds were a vital supplementary food in late May and Aug., when arthropods were scarce or inaccessible. One species of crane fly was the major dietary component for longspurs during June and July. Its high abundance and substantial dry weight per individual may contribute to the success of longspurs at Barrow. The diets of longspurs and 4 common shorebirds (Calidris spp.) at Barrow were similar in the range of prey items taken except for seeds and tenthredinid larvae. Their diets overlapped closely when feeding sites were restricted because of snow and surface water (chiefly at the beginning of the season) and when prey was abundant in early to mid-July. Competition is possible early in the season but unlikely in July when surface insects are very abundant. Habitat separation and the advantages of fringillid form apparently contribute to the success of longspors in a tundra community of insectivores dominated by shorebirds.","language":"English","publisher":"Oxford Academic","doi":"10.2307/1368039","usgsCitation":"Custer, T., and Pitelka, F., 1978, Seasonal trends in summer diet of the lapland longspur near Barrow Alaska USA: The Condor, v. 80, no. 3, p. 295-301, https://doi.org/10.2307/1368039.","productDescription":"7 p.","startPage":"295","endPage":"301","numberOfPages":"7","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":503054,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digitalcommons.usf.edu/condor/vol80/iss3/6","text":"External Repository"},{"id":133933,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"80","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc2ec","contributors":{"authors":[{"text":"Custer, T. W. 0000-0003-3170-6519","orcid":"https://orcid.org/0000-0003-3170-6519","contributorId":91802,"corporation":false,"usgs":true,"family":"Custer","given":"T. W.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":312754,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pitelka, F.A.","contributorId":7676,"corporation":false,"usgs":true,"family":"Pitelka","given":"F.A.","email":"","affiliations":[],"preferred":false,"id":312753,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1001801,"text":"1001801 - 1978 - Changes in submerged aquatic macrophyte populations at the head of Chesapeake Bay, 1958-1975","interactions":[],"lastModifiedDate":"2023-10-16T17:12:09.415132","indexId":"1001801","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1583,"text":"Estuaries","active":true,"publicationSubtype":{"id":10}},"title":"Changes in submerged aquatic macrophyte populations at the head of Chesapeake Bay, 1958-1975","docAbstract":"<p><span>Submerged aquatic plant populations in the Susquehanna Flats of the Chesapeake Bay were followed for 18 years. An exotic species, eurasian water milfoil, </span><i>Myriophyllum spicatum</i><span>, increased dramatically from 1958 to 1962; at the same time the dominant native species declined. After 1962, milfoil populations declined and the native rooted aquatics gradually began to return to their former levels. In the late 1960's all species declined and in 1972 almost disappeared from the Susquehanna Flats. These fluctuations may have been related to several interrelated environmental factors in the Chesapeake Bay, including tropical storms, turbidity, salinity and disease. The utilization of the Susquehanna Flats by waterfowl appears to be related to the abundance and species composition of the submerged macrophytes present.</span></p>","language":"English","publisher":"Springer","doi":"10.2307/1351459","usgsCitation":"Bayley, S., Stotts, V.D., Springer, P.F., and Steenis, J., 1978, Changes in submerged aquatic macrophyte populations at the head of Chesapeake Bay, 1958-1975: Estuaries, v. 1, no. 3, p. 171-182, https://doi.org/10.2307/1351459.","productDescription":"12 p.","startPage":"171","endPage":"182","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":130462,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland, Virginia","otherGeospatial":"Chesapeake Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.673583984375,\n              36.91915611148194\n            ],\n            [\n              -75.69030761718749,\n              36.91915611148194\n            ],\n            [\n              -75.69030761718749,\n              39.63530729658601\n            ],\n            [\n              -76.673583984375,\n              39.63530729658601\n            ],\n            [\n              -76.673583984375,\n              36.91915611148194\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"1","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e52d1","contributors":{"authors":[{"text":"Bayley, S.","contributorId":83066,"corporation":false,"usgs":true,"family":"Bayley","given":"S.","email":"","affiliations":[],"preferred":false,"id":311815,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stotts, Vernon D.","contributorId":86724,"corporation":false,"usgs":false,"family":"Stotts","given":"Vernon","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":311816,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Springer, P. F.","contributorId":56590,"corporation":false,"usgs":false,"family":"Springer","given":"P.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":311814,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Steenis, J.","contributorId":26656,"corporation":false,"usgs":true,"family":"Steenis","given":"J.","email":"","affiliations":[],"preferred":false,"id":311813,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70162258,"text":"70162258 - 1978 - Survival of the salmonid viruses infectious hematopoietic necrosis (IHNV) and infectious pancreatic necrosis (IPNV) in ozonated, chlorinated, and Untreated waters","interactions":[],"lastModifiedDate":"2016-01-19T15:45:03","indexId":"70162258","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","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":"Survival of the salmonid viruses infectious hematopoietic necrosis (IHNV) and infectious pancreatic necrosis (IPNV) in ozonated, chlorinated, and Untreated waters","docAbstract":"<p><span>Ozone and chlorine inactivation curves were determined in three water types at 10 &deg;C for the fish pathogenic viruses infectious hematopoietic necrosis (IHNV) and infectious pancreatic necrosis (IPNV). In phosphate-buffered, distilled water (PBDW) an ozone dose of 0.01&ensp;mg/L for 30 or 60&ensp;s inactivated IHNV or IPNV, respectively, suspended at a tissue culture 50% infective dose (TCID50) of 10</span><sup>4</sup><span>&ndash;10</span><sup>5</sup><span>/mL. In hard (120&ensp;mg/L as CaCO</span><sub>3</sub><span>) and soft water (30&ensp;mg/L) lake waters, an ozone application rate of 70&ensp;mg∙h</span><sup>&minus;1</sup><span>∙L</span><sup>&minus;1</sup><span>&nbsp;for 10&ensp;min destroyed IHNV. IPNV inactivation in hard water required 90&ensp;mg∙O</span><sub>3</sub><span>∙h</span><sup>&minus;1</sup><span>∙L</span><sup>&minus;1</sup><span>&nbsp;for 10&ensp;min but only a 30-s contact time in soft water. The IPNV was also somewhat more resistant to chlorine. In PBDW, a residual of 0.1&ensp;mg/L with contact times of 30 and 60&ensp;s, respectively, destroyed IHNV and IPNV. In soft lake water IHNV was destroyed within 5&ensp;min at 0.5&ensp;mg/L, while in hard water a 10-min contact time was required. For IPNV disinfection in soft water, 0.2&ensp;mg/L for 10&ensp;min was sufficient but this chlorine residual had essentially no effect on IPNV in hard water. Increasing this dose to 0.7&ensp;mg/L destroyed IPNV in hard water within 2&ensp;min. In untreated waters, IPNV was stable for at least 8&ensp;wk in either distilled, soft, or hard lake waters. However, IHNV survived only about 2&ensp;wk in distilled and 7&ensp;wk in the soft or hard lake waters. We suggest the serious consideration of ozone as a fish disease control agent.&nbsp;</span><i>Key words</i><span>: ozone, chlorine disinfection, fish pathogens, viruses</span></p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/f78-140","usgsCitation":"Wedemeyer, G.A., Nelson, N.C., and Smith, C.A., 1978, Survival of the salmonid viruses infectious hematopoietic necrosis (IHNV) and infectious pancreatic necrosis (IPNV) in ozonated, chlorinated, and Untreated waters: Journal of the Fisheries Research Board of Canada, v. 35, no. 6, p. 875-879, https://doi.org/10.1139/f78-140.","productDescription":"5 p.","startPage":"875","endPage":"879","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314496,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"35","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569f6c54e4b0961cf27fd1cf","contributors":{"authors":[{"text":"Wedemeyer, Gary A.","contributorId":30668,"corporation":false,"usgs":true,"family":"Wedemeyer","given":"Gary","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":588997,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nelson, Nancy C.","contributorId":152336,"corporation":false,"usgs":false,"family":"Nelson","given":"Nancy","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":588998,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, Cathy A.","contributorId":152096,"corporation":false,"usgs":false,"family":"Smith","given":"Cathy","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":588999,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70162257,"text":"70162257 - 1978 - Prevention and treatment of Nitrite toxicity in juvenile steelhead trout (<i>Salmo gairdneri</i>)","interactions":[],"lastModifiedDate":"2016-08-15T20:56:21","indexId":"70162257","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","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 treatment of Nitrite toxicity in juvenile steelhead trout (<i>Salmo gairdneri</i>)","docAbstract":"<p><span>The efficacy of mineral salts, pH, and tetramethylthianine (methylene blue) treatment in reducing the acute toxicity of nitrite to fingerling steelhead trout (</span><i>Salmo gairdneri</i><span>) was determined using a static bioassay system at 10 &deg;C. The acute toxicity (96-h LC50) was reduced by a factor of about 24 for 5-g steelhead and 13 for 10-g fish when the total water hardness was increased from 25 to 300&ensp;mg/L (as CaCO</span><sub>3</sub><span>). NaCl or CaCl</span><sub>2</sub><span>&nbsp;additions (0&ndash;200&ensp;mg/L) reduced toxicity by a factor of up to 3 for NaCl and 50 for CaCl</span><sub>2</sub><span>. Increasing the pH from 6.0 to 8.0 decreased toxicity by a factor of about 8 for the smaller and 3 for the larger fish. Methylene blue at 0.1 or 1.0&ensp;mg/L was effective in decreasing acute toxicity. For alleviating methemoglobinemia, removing the fish to freshwater for 48&ensp;h was about as effective as 1.0&ensp;mg/L methylene blue. Chronic exposure in soft water to 0.03&ensp;mg/L NO</span><sub>2</sub><span>-N for 6&ensp;mo caused no significant growth reduction, gill histological changes, hematological dyscrasias, or impaired ability of the smolts to adapt to 30&permil; seawater and grow for an additional 2&ensp;mo.&nbsp;</span><i>Key words</i><span>: nitrite, toxicity, fish, methylene blue, pH, salts, acute toxicity, chronic toxicity</span></p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/f78-132","usgsCitation":"Wedemeyer, G.A., and Yasutake, W.T., 1978, Prevention and treatment of Nitrite toxicity in juvenile steelhead trout (<i>Salmo gairdneri</i>): Journal of the Fisheries Research Board of Canada, v. 35, no. 6, p. 822-827, https://doi.org/10.1139/f78-132.","productDescription":"6 p.","startPage":"822","endPage":"827","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314495,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"35","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569f6c53e4b0961cf27fd1c3","contributors":{"authors":[{"text":"Wedemeyer, Gary A.","contributorId":30668,"corporation":false,"usgs":true,"family":"Wedemeyer","given":"Gary","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":588995,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yasutake, W. T.","contributorId":103222,"corporation":false,"usgs":true,"family":"Yasutake","given":"W.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":588996,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":94742,"text":"94742 - 1978 - Studies on vertical and horizontal transmission of duck plague virus in apparently healthy waterfowl","interactions":[],"lastModifiedDate":"2015-05-18T10:17:53","indexId":"94742","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":21,"text":"Thesis"},"publicationSubtype":{"id":28,"text":"Thesis"},"title":"Studies on vertical and horizontal transmission of duck plague virus in apparently healthy waterfowl","docAbstract":"<p>Healthy waterfowl were found to be carriers of duck plague (DP) virus. Black ducks (Anas rubripes) and Canada geese (Branta canadensis) surviving a natural outbreak of DP at Coloma, Wisconsin, in 1973 yielded DP virus in cloacal swabs taken four years postinfection. Experimental infection of previously unexposed mallard ducks (Anas platyrhynochos) with the Coloma strain of DP virus CO-WI (73) also produced cloacal virus shedding for up to four years after infection. A second DP virus strain, LA-SD (73) from the Lake Andes, South Dakota, epornitic, was detected from cloacal swabs of pintail ducks (Anas acuta), gadwall ducks (Anas strepera), wood ducks (Aix sponsa), and Canada geese infected experimentally one year before. The frequency of swabs positive for DP virus varied between individuals within each of the tested species. The amount of detectable DP virus shed was about 100 plaqueforming units of virus percloacal swab. Oral erosions were present in all species tested except Canada geese and gadwall ducks. Erosions occurred at the openings of the sublingual salivary gland ducts. DP virus was isolated from erosions. All ducks with lesions proved to shed DP virus, although not necessarily at the time they had the lesion. Three pintail ducks treated with dexamethasone for ten days, shed DP virus daily for 19 days after the first day of treatment. These birds also shed DP virus the one time they were tested prior to dexamethosone treatment. An acute lethal outbreak occurred in CO-WI (73) carrier birds. Both DP virus and specific lesions were found in dead birds. The deaths coincided with a change in housing and with the simultaneous introduction of co-housed LA-SD (73) infected ducklings. DP virus was isolated from the chorio-allantoic (CA) fluid of a fourteen day pekin embryo and from five of ten infertile pekin eggs laid by DP carrier birds.</p>","language":"English","publisher":"University of Wisconsin","usgsCitation":"Burgess, E.C., 1978, Studies on vertical and horizontal transmission of duck plague virus in apparently healthy waterfowl, 34 p.","productDescription":"34 p.","startPage":"1","endPage":"34","numberOfPages":"34","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":128532,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Dakota, Wisconsin","city":"Coloma, Lake Andes","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": 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,{"id":96541,"text":"96541 - 1978 - Proceedings of a workshop on techniques of rehabilitation and erosion control in recently roaded and logged watersheds, with emphasis to north coastal California. March 13-14, 1978","interactions":[],"lastModifiedDate":"2018-03-21T14:54:07","indexId":"96541","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Proceedings of a workshop on techniques of rehabilitation and erosion control in recently roaded and logged watersheds, with emphasis to north coastal California. March 13-14, 1978","docAbstract":"No abstract available at this time","language":"English","publisher":"National Park Service, Redwood National Park, Resources Management Div.","publisherLocation":"Arcata, CA","usgsCitation":"Madej, M.A., and Kelsey, H., 1978, Proceedings of a workshop on techniques of rehabilitation and erosion control in recently roaded and logged watersheds, with emphasis to north coastal California. March 13-14, 1978, 89 p.","productDescription":"89 p.","startPage":"89","numberOfPages":"89","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":127742,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db66061c","contributors":{"authors":[{"text":"Madej, Mary Ann 0000-0003-2831-3773 mary_ann_madej@usgs.gov","orcid":"https://orcid.org/0000-0003-2831-3773","contributorId":40304,"corporation":false,"usgs":true,"family":"Madej","given":"Mary","email":"mary_ann_madej@usgs.gov","middleInitial":"Ann","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":299785,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kelsey, H.M.","contributorId":84300,"corporation":false,"usgs":true,"family":"Kelsey","given":"H.M.","email":"","affiliations":[],"preferred":false,"id":299786,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70168577,"text":"70168577 - 1978 - Gilbert White talks about natural hazards","interactions":[],"lastModifiedDate":"2016-03-22T14:22:16","indexId":"70168577","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Gilbert White talks about natural hazards","docAbstract":"<p>Dr. Gilbert White is Director of the Institute of Behavioral Science at the University of Colorado, Boulder, where he is responsible for natural Hazards Research and Applications Information Center supported by the National Science Foundation. He served in the Executive Office of the president in 1941-42, on the Federal Flood Control Policy Task Force in 1964-65, and on the U.S Geological Survey Advisory Panel on Earthquake Studies. Dr. White has authored five books on the social and economic aspects of natural resources, including water supply and river development, and on floods and other natural hazards.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Spall, H., 1978, Gilbert White talks about natural hazards: Earthquake Information Bulletin (USGS), v. 10, no. 1, p. 16-19.","productDescription":"4 p.","startPage":"16","endPage":"19","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318197,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56c84ac9e4b0b3c9ae38106b","contributors":{"authors":[{"text":"Spall, H.","contributorId":99290,"corporation":false,"usgs":true,"family":"Spall","given":"H.","affiliations":[],"preferred":false,"id":620945,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70168578,"text":"70168578 - 1978 - Clarence Allen talks about the responsibilities in earthquake prediction","interactions":[],"lastModifiedDate":"2016-03-22T14:25:13","indexId":"70168578","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Clarence Allen talks about the responsibilities in earthquake prediction","docAbstract":"<p>Dr. Clarence R. Allen is professor of geology and geophysics at the California Institute of Technology. He has been a member of advisory panels to the Executive Office of the President, National Academy of Sciences, National Science Foundation, U.S Geological Survey, UNESCO, California State Mining and Geology Board, and the California Department of Water Resources. Dr. Allen has been President of both the Geological Society of America and the Seismological Society of America (SSA). The title of this interview is based on his presidential address to the SSA in 1976.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Spall, H., 1978, Clarence Allen talks about the responsibilities in earthquake prediction: Earthquake Information Bulletin (USGS), v. 10, no. 4, p. 116-119.","productDescription":"4 p.","startPage":"116","endPage":"119","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318198,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56c84ac4e4b0b3c9ae381012","contributors":{"authors":[{"text":"Spall, H.","contributorId":99290,"corporation":false,"usgs":true,"family":"Spall","given":"H.","affiliations":[],"preferred":false,"id":620946,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":93771,"text":"93771 - 1978 - Use of Landsat data to assess waterfowl habitat quality","interactions":[],"lastModifiedDate":"2017-09-14T10:06:17","indexId":"93771","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Use of Landsat data to assess waterfowl habitat quality","docAbstract":"This report is a discussion of the feasibility of using Landsat data to generate information of value for effective management of migratory waterfowl. Effective management of waterfowl includes regulating waterfowl populations through hunting regulations and habitat management. This report examines the ability to analyze annual production by monitoring the number of breeding and brood ponds that are present, and the ability to assess waterfowl habitat based on the various relationships between ponds and the surrounding upland terrain types. The basic conclusions of this report are that: 1) Landsat data can be used to improve estimates of pond numbers which may be correlated with duck production; and 2) Landsat data can be used to generate information on terrain types which subsequently can be used to assess relative waterfowl habitat quality.","language":"English","publisher":"Environmental Research Institute of Michigan","publisherLocation":"Ann Arbor, MI","usgsCitation":"Colwell, J., Gilmer, D., Work, E., and Rebel, D., 1978, Use of Landsat data to assess waterfowl habitat quality, 83 pp.","productDescription":"83 pp.","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":128244,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db6051be","contributors":{"authors":[{"text":"Colwell, J.E.","contributorId":79048,"corporation":false,"usgs":true,"family":"Colwell","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":297901,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gilmer, D.S.","contributorId":22270,"corporation":false,"usgs":true,"family":"Gilmer","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":297898,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Work, E.A. Jr.","contributorId":33654,"corporation":false,"usgs":true,"family":"Work","given":"E.A.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":297900,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rebel, D.","contributorId":33255,"corporation":false,"usgs":true,"family":"Rebel","given":"D.","email":"","affiliations":[],"preferred":false,"id":297899,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":7858,"text":"ofr78913 - 1978 - Quality of water in Pascagoula and Escatawpa Rivers, Jackson County, Mississippi","interactions":[],"lastModifiedDate":"2023-03-03T21:24:47.196279","indexId":"ofr78913","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"78-913","title":"Quality of water in Pascagoula and Escatawpa Rivers, Jackson County, Mississippi","docAbstract":"<p>The chemical and physical properties and the range of concentrations of most constituents in water in the Pascagoula and Escatawpa Rivers during the period May 17-19, 1977, varied rapidly between high and low tides, primarily as the result of interactions of freshwater inflow with highly mineralized Gulf waters. The water at a downstream site of the 11-mile study reach on the Pascagoula River was saline. On May 19, 1977, the dissolved-solids concentration at that site was 14,500 milligrams per liter. At the same time, the water at the mouth of Escatawpa River had a dissolved-solids concentration of 4,600 milligrams per liter. The specific conductance of the water at the downstream sites of both rivers increased with depth and progressively decreased upstream to sites where freshwater inflow was predominant. The specific conductance decreased upstream from a maximum of 40,000 micromhos per centimeter at 25°Celsius at site P1 to 60 micromhos at site P12 on Pascagoula River and from 30,000 micromhos at site E1 to 45 micromhos at site E9 on Escatawpa River.</p><p>There was evidence of oxygen deficiency (less than 3.0 milligrams per liter) at many sites in deep pools where there is little circulation and mixing of the more dense saltwater. Dissolved-oxygen concentrations ranged from 2.1 to 8.2 milligrams per liter.</p><p>Biochemical oxygen demand ranged from 0.1 to 3.5 milligrams per liter and was generally less than 2.0 milligrams per liter at most sites.</p><p>A large part of the total organic carbon in the lower Pascagoula River was carried into the study area by freshwater inflow. Very little organic carbon was being discharged by the Escatawpa River into the Pascagoula River.</p><p>Total nitrogen moved out of Pascagoula and Escatawpa Rivers at an extremely slow rate and in concentrations of less than 0.1 milligram per liter.</p><p>The water temperature near the surface at downstream sites on Escatawpa River at low tide was elevated as much as 2.5°C (4.5°F), suggesting thermal loading.</p><p>The fecal coliform and fecal streptococcal bacteria in Pascagoula and Escatawpa Rivers were in concentrations indicative of manmade pollution. The ratio of the concentrations in which these bacteria were present suggests that both rivers receive human enteric wastes.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78913","collaboration":"Prepared in cooperation with Mississippi Air and Water Pollution Control Commission","usgsCitation":"Bednar, G.A., 1978, Quality of water in Pascagoula and Escatawpa Rivers, Jackson County, Mississippi: U.S. Geological Survey Open-File Report 78-913, v, 91 p., https://doi.org/10.3133/ofr78913.","productDescription":"v, 91 p.","costCenters":[],"links":[{"id":141453,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0913/report-thumb.jpg"},{"id":413500,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0913/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Mississippi","county":"Jackson County","otherGeospatial":"Escatawpa River, Pascagoula River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.83333333,\n              30.321915039121063\n            ],\n            [\n              -88.39462280273438,\n              30.321915039121063\n            ],\n            [\n              -88.39462280273438,\n              30.70833333\n            ],\n            [\n              -88.83333333,\n              30.70833333\n            ],\n            [\n              -88.83333333,\n              30.321915039121063\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db6516b2","contributors":{"authors":[{"text":"Bednar, Gene A.","contributorId":81881,"corporation":false,"usgs":true,"family":"Bednar","given":"Gene","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":156742,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11044,"text":"ofr78422 - 1978 - U.S. Geological Survey offshore program of resource and geo-environmental studies and topical investigations, Pacific-Arctic region","interactions":[],"lastModifiedDate":"2024-01-23T15:59:21.688922","indexId":"ofr78422","displayToPublicDate":"1978-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"78-422","title":"U.S. Geological Survey offshore program of resource and geo-environmental studies and topical investigations, Pacific-Arctic region","docAbstract":"<p>The Geological Survey's marine geology investigations in the Pacific-Arctic area are presented in this report in the context of the underlying socio-economic problem of expanding the domestic production of oil and gas and other mineral and hard- and soft-rock resources while maintaining acceptable standards in the marine environment. The primary mission of the Survey 's Pacific-Arctic Branch of Marine Geology is to provide scientifically interpreted information about the (1) resource potential, (2) geo-environmental setting, and (3) overall geologic characteristics of the continental margins (that is, the continental shelf, slope and rise) and adjacent deeper water and shallower coastal areas off California, Oregon, Washington, Alaska and Hawaii and also, where it is of interest to the U.S. Government, more remote deep-sea areas of the Pacific-Arctic realm.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78422","usgsCitation":"Scholl, D.W., 1978, U.S. Geological Survey offshore program of resource and geo-environmental studies and topical investigations, Pacific-Arctic region: U.S. Geological Survey Open-File Report 78-422, 109 p., https://doi.org/10.3133/ofr78422.","productDescription":"109 p.","costCenters":[],"links":[{"id":142606,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0422/report-thumb.jpg"},{"id":424764,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0422/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"otherGeospatial":"Pacific-Arctic region","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db6121e7","contributors":{"authors":[{"text":"Scholl, David William","contributorId":22357,"corporation":false,"usgs":true,"family":"Scholl","given":"David","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":162431,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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