{"pageNumber":"2382","pageRowStart":"59525","pageSize":"25","recordCount":68846,"records":[{"id":70010948,"text":"70010948 - 1975 - Mercury distribution in ancient and modern sediment of northeastern Bering Sea","interactions":[{"subject":{"id":15187,"text":"ofr72268 - 1972 - Mercury distribution in ancient and modern sediment of northeastern Bering Sea","indexId":"ofr72268","publicationYear":"1972","noYear":false,"title":"Mercury distribution in ancient and modern sediment of northeastern Bering Sea"},"predicate":"SUPERSEDED_BY","object":{"id":70010948,"text":"70010948 - 1975 - Mercury distribution in ancient and modern sediment of northeastern Bering Sea","indexId":"70010948","publicationYear":"1975","noYear":false,"title":"Mercury distribution in ancient and modern sediment of northeastern Bering Sea"},"id":1}],"lastModifiedDate":"2013-01-24T14:24:55","indexId":"70010948","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Mercury distribution in ancient and modern sediment of northeastern Bering Sea","docAbstract":"Reconnaissance sampling of surface and subsurface sediment to a maximum depth of 80 m below the sea floor shows that typical values of 0.03 p.p.m. and anomalies of 0.2-1.3 p.p.m. mercury have been present in northeastern Bering Sea since Early Pliocene time. Values are highest in modern beach (maximum 1.3 and mean 0.22 p.p.m. Hg) and nearshore subsurface gravels (maximum 0.6 and mean 0.06 p.p.m. Hg) along the highly mineralized Seward Peninsula and in clayey silt rich in organic matter (maximum 0.16 and mean 0.10 p.p.m. Hg) throughout the region. Although gold mining may be partly responsible for high mercury levels in the modern beach near Nome, Alaska (maximum 0.45 p.p.m.), equally high or greater concentrations of mercury occur in buried Pleistocene sediments immediately offshore (maximum 0.6 p.p.m.) and in modern unpolluted beach sediments at Bluff (maximum 1.3 p.p.m.); this suggests that the contamination effects of mining may be no greater than natural concentration processes in the Seward Peninsula region. The mercury content of offshore surface sediment, even adjacent to mercury-rich beaches, corresponds to that of unpolluted marine and fresh-water sediment elsewhere. The normal values that prevail offshore may be attributable to entrapment of mercury-bearing heavy minerals on beaches near sources and/or dilution effects of offshore sedimentation. The few minor anomalies offshore occur in glacial drift derived from mercury source regions of Chukotka (Siberia) and Seward Peninsula; Pleistocene shoreline processes have reworked the drift to concentrate the heavy metals. The distribution pattern of mercury indicates that particulate mercury-bearing minerals have not been widely dispersed from onland deposits in quantities sufficient to increase mercury levels above normal in offshore sediments of Bering Sea; however, it shows that natural sedimentary processes can concentrate this mercury in beaches of the coastal zone where there already is concern because of potential pollution from man's activities.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam Netherlands","doi":"10.1016/0025-3227(75)90006-7","issn":"00253227","usgsCitation":"Nelson, C., Pierce, D., Leong, K., and Wang, F., 1975, Mercury distribution in ancient and modern sediment of northeastern Bering Sea: Marine Geology, v. 18, no. 3, p. 91-104, https://doi.org/10.1016/0025-3227(75)90006-7.","productDescription":"14 p.","startPage":"91","endPage":"104","costCenters":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"links":[{"id":220949,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266423,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0025-3227(75)90006-7"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 161.98,51.22 ], [ 161.98,66.05 ], [ -157.0,66.05 ], [ -157.0,51.22 ], [ 161.98,51.22 ] ] ] } } ] }","volume":"18","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5401e4b0c8380cd6ce5c","contributors":{"authors":[{"text":"Nelson, C.H.","contributorId":88346,"corporation":false,"usgs":true,"family":"Nelson","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":359957,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pierce, D.E.","contributorId":88083,"corporation":false,"usgs":true,"family":"Pierce","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":359956,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leong, Kam","contributorId":103660,"corporation":false,"usgs":true,"family":"Leong","given":"Kam","affiliations":[],"preferred":false,"id":359958,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wang, F.F.H.","contributorId":87219,"corporation":false,"usgs":true,"family":"Wang","given":"F.F.H.","email":"","affiliations":[],"preferred":false,"id":359955,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70009922,"text":"70009922 - 1975 - The determination of specific forms of aluminum in natural water","interactions":[],"lastModifiedDate":"2021-03-02T13:56:28.864336","indexId":"70009922","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"The determination of specific forms of aluminum in natural water","docAbstract":"<p id=\"simple-para.0010\">A procedure for analysis and pretreatment of natural-water samples to determine very low concentrations of Al is described which distinguishes the rapidly reacting equilibrium species from the metastable or slowly reacting macro ions and colloidal suspended material. Aluminum is complexed with 8-hydroxyquinoline (oxine), pH is adjusted to 8.3 to minimize interferences, and the aluminum oxinate is extracted with methyl isobutyl ketone (MIBK) prior to analysis by atomic absorption. To determine equilibrium species only, the contact time between sample and 8-hydroxyquinoline is minimized. The Al may be extracted at the sample site with a minimum of equipment and the MIBK extract stored for several weeks prior to atomic absorption analysis.</p><p id=\"simple-para.0015\">Data obtained from analyses of 39 natural groundwater samples indicate that filtration through a 0.1-μm pore size filter is not an adequate means of removing all insoluble and metastable Al species present, and extraction of Al immediately after collection is necessary if only dissolved and readily reactive species are to be determined. An average of 63% of the Al present in natural waters that had been filtered through 0.1-μm pore size filters was in the form of monomeric ions. The total Al concentration, which includes all forms that passed through a 0.1-μm pore size filter, ranged 2–70 μg/l. The concentration of Al in the form of monomeric ions ranged from below detection to 57 μg/l. Most of the natural water samples used in this study were collected from thermal springs and oil wells.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0009-2541(75)90018-2","issn":"00092541","usgsCitation":"Barnes, R., 1975, The determination of specific forms of aluminum in natural water: Chemical Geology, v. 15, no. 3, p. 177-191, https://doi.org/10.1016/0009-2541(75)90018-2.","productDescription":"p.","startPage":"177","endPage":"191","numberOfPages":"15","costCenters":[],"links":[{"id":218834,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baa9ee4b08c986b3228d7","contributors":{"authors":[{"text":"Barnes, R.B.","contributorId":53393,"corporation":false,"usgs":true,"family":"Barnes","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":357465,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010989,"text":"70010989 - 1975 - Interstitial solutions and diagenesis in deeply buried marine sediments: Results from the Deep Sea Drilling Project","interactions":[],"lastModifiedDate":"2019-12-17T12:57:58","indexId":"70010989","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","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":"Interstitial solutions and diagenesis in deeply buried marine sediments: Results from the Deep Sea Drilling Project","docAbstract":"<p><span>Through the Deep Sea Drilling Project samples of interstitial solutions of deeply buried marine sediments throughout the World Ocean have been obtained and analyzed. The studies have shown that in all but the most slowly deposited sediments pore fluids exhibit changes in composition upon burial. These changes can be grouped into a few consistent patterns that facilitate identification of the diagenetic reactions occurring in the sediments. Pelagic clays and slowly deposited (&lt;1 cm/10</span><sup>3</sup><span>yr) biogenic sediments are the only types that exhibit little evidence of reaction in the pore waters. In most biogenic sediments sea water undergoes considerable alteration. In sediments deposited at rates up to a few cm/10</span><sup>3</sup><span>&nbsp;yr the changes chiefly involve gains of Ca</span><sup>2+</sup><span>&nbsp;and Sr</span><sup>2+</sup><span>&nbsp;and losses of Mg</span><sup>2+</sup><span>&nbsp;which balance the Ca</span><sup>2+</sup><span>&nbsp;enrichment. The Ca-Mg substitution may often reach 30 mM/kg while Sr</span><sup>2+</sup><span>&nbsp;may be enriched 15-fold over sea water. These changes reflect recrystallization of biogenic calcite and the substitution of Mg</span><sup>2+</sup><span>&nbsp;for Ca</span><sup>2+</sup><span>&nbsp;during this reaction. The Ca-Mg-carbonate formed is most likely a dolomitic phase. A related but more complex pattern is found in carbonate sediments deposited at somewhat greater rates. Ca</span><sup>2+</sup><span>&nbsp;and Sr</span><sup>2+</sup><span>&nbsp;enrichment is again characteristic, but Mg</span><sup>2+</sup><span>&nbsp;losses exceed Ca</span><sup>2+</sup><span>&nbsp;gains with the excess being balanced by SO</span><sub>4</sub><sup>post staggered2-</sup><span>&nbsp;losses. The data indicate that the reactions are similar to those noted above, except that the Ca</span><sup>2+</sup><span>&nbsp;released is not kept in solution but is precipitated by the HCO</span><sub>3</sub><sup>post staggered-</sup><span>&nbsp;produced in SO</span><sub>4</sub><sup>post staggered2-</sup><span>&nbsp;reduction. In both these types of pore waters Na</span><sup>+</sup><span>&nbsp;is usually conservative, but K</span><sup>+</sup><span>&nbsp;depletions are frequent. In several partly consolidated sediment sections approaching igneous basement contact, very marked interstitial calcium enrichment has been found (to 5.5 g/kg). These phenomena are marked by pronounced depletion in Na</span><sup>+</sup><span>, Si and CO</span><sub>2</sub><span>, and slight enhancement in Cl</span><sup>-</sup><span>. The changes are attributed to exchange of Na</span><sup>+</sup><span>&nbsp;for Ca</span><sup>2+</sup><span>&nbsp;in silicate minerals forming from submarine weathering of igneous rocks such as basalts. Water is also consumed in these reactions, accounting for minor increases in total interstitial salinity. Terrigenous, organic-rich sediments deposited rapidly along continental margins also exhibit significant evidences of alteration. Microbial reactions involving organic matter lead to complete removal of SO</span><sub>4</sub><sup>post staggered2-</sup><span>, strong HCO</span><sub>3</sub><sup>post staggered-</sup><span>&nbsp;enrichment, formation of NH</span><sub>4</sub><sup>post staggered+</sup><span>, and methane synthesis from H</span><sub>2</sub><span>&nbsp;and CO</span><sub>2</sub><span>&nbsp;once SO</span><sub>4</sub><sup>post staggered2-</sup><span>&nbsp;is eliminated. K</span><sup>+</sup><span>&nbsp;and often Na</span><sup>+</sup><span>&nbsp;(slightly) are depleted in the interstitial waters. Ca</span><sup>2+</sup><span>&nbsp;depletion may occur owing to precipitation of CaCO</span><sub>3</sub><span>. In most cases interstitial Cl</span><sup>-</sup><span>&nbsp;remains relatively constant, but increases are noted over evaporitic strata, and decreases in interstitial Cl</span><sup>-</sup><span>&nbsp;are observed in some sediments adjacent to continents.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(75)90165-9","issn":"00167037","usgsCitation":"Sayles, F., and Manheim, F., 1975, Interstitial solutions and diagenesis in deeply buried marine sediments: Results from the Deep Sea Drilling Project: Geochimica et Cosmochimica Acta, v. 39, no. 2, p. 103-127, https://doi.org/10.1016/0016-7037(75)90165-9.","productDescription":"25 p.","startPage":"103","endPage":"127","numberOfPages":"25","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":221419,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3db1e4b0c8380cd63772","contributors":{"authors":[{"text":"Sayles, F.L.","contributorId":77657,"corporation":false,"usgs":true,"family":"Sayles","given":"F.L.","email":"","affiliations":[],"preferred":false,"id":360035,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Manheim, F.T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":55421,"corporation":false,"usgs":true,"family":"Manheim","given":"F.T.","affiliations":[],"preferred":false,"id":360034,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010116,"text":"70010116 - 1975 - Short chain aliphatic acid anions in oil field waters and their contribution to the measured alkalinity","interactions":[],"lastModifiedDate":"2021-02-17T14:15:18.281662","indexId":"70010116","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","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":"Short chain aliphatic acid anions in oil field waters and their contribution to the measured alkalinity","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id6\" class=\"abstract author\"><div id=\"aep-abstract-sec-id7\"><p>High alkalinity values found in some formation waters from Kettleman North Dome oil field are due chiefly to acetate and propionate ions, with some contribution from higher molecular weight organic acid ions. Some of these waters contain no detectable bicarbonate alkalinity. For waters such as these, high supersaturation with respect to calcite will be incorrectly indicated by thermodynamic calculations based upon carbonate concentrations inferred from traditional alkalinity measurements</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(75)90092-7","issn":"00167037","usgsCitation":"Willey, L., Kharaka, Y., Presser, T.S., Rapp, J.B., and Barnes, I., 1975, Short chain aliphatic acid anions in oil field waters and their contribution to the measured alkalinity: Geochimica et Cosmochimica Acta, v. 39, no. 12, p. 1707-1711, https://doi.org/10.1016/0016-7037(75)90092-7.","productDescription":"5 p.","startPage":"1707","endPage":"1711","numberOfPages":"5","costCenters":[],"links":[{"id":218843,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8e98e4b08c986b318a24","contributors":{"authors":[{"text":"Willey, L.M.","contributorId":44607,"corporation":false,"usgs":true,"family":"Willey","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":357991,"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":357988,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Presser, T. S.","contributorId":93875,"corporation":false,"usgs":true,"family":"Presser","given":"T.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":357992,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rapp, J. B.","contributorId":28987,"corporation":false,"usgs":true,"family":"Rapp","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":357990,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Barnes, I.","contributorId":23678,"corporation":false,"usgs":true,"family":"Barnes","given":"I.","affiliations":[],"preferred":false,"id":357989,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70010099,"text":"70010099 - 1975 - Water analysis","interactions":[],"lastModifiedDate":"2023-03-20T10:55:44.308773","indexId":"70010099","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","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":"Water analysis","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60355a010","usgsCitation":"Fishman, M.J., and Erdmann, D.E., 1975, Water analysis: Analytical Chemistry, v. 47, no. 5, p. 334-361, https://doi.org/10.1021/ac60355a010.","productDescription":"28 p.","startPage":"334","endPage":"361","costCenters":[],"links":[{"id":219740,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"47","issue":"5","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505bc795e4b08c986b32c503","contributors":{"authors":[{"text":"Fishman, M. J.","contributorId":65069,"corporation":false,"usgs":true,"family":"Fishman","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":357893,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erdmann, D. E.","contributorId":30264,"corporation":false,"usgs":true,"family":"Erdmann","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":357892,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56746,"text":"wdrNY742 - 1975 - Water resources data for New York, water year 1974; Part 2, Water quality records","interactions":[],"lastModifiedDate":"2023-05-01T14:50:43.429985","indexId":"wdrNY742","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NY-74-2","title":"Water resources data for New York, water year 1974; Part 2, Water quality records","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNY742","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1975, Water resources data for New York, water year 1974; Part 2, Water quality records: U.S. Geological Survey Water Data Report NY-74-2, vi, 360 p., https://doi.org/10.3133/wdrNY742.","productDescription":"vi, 360 p.","costCenters":[],"links":[{"id":416550,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1974/ny-74-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175189,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1974/ny-74-2/report-thumb.jpg"}],"country":"United States","state":"New 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,{"id":56538,"text":"wdrND741 - 1975 - Water resources data for North Dakota, water year 1974; Part 1, Surface water records","interactions":[],"lastModifiedDate":"2023-03-16T14:29:44.367581","indexId":"wdrND741","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"ND-74-1","title":"Water resources data for North Dakota, water year 1974; Part 1, Surface water records","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrND741","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1975, Water resources data for North Dakota, water year 1974; Part 1, Surface water records: U.S. Geological Survey Water Data Report ND-74-1, 187 p., https://doi.org/10.3133/wdrND741.","productDescription":"187 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":414283,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wdr/1974/nd-74-1/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414282,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1974/nd-74-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":181284,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1974/nd-74-1/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2685","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532719,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70139636,"text":"70139636 - 1975 - Hydrologic data of the coastal drainage basins of southeastern Massachusetts, Weir River, Hingham, to Jonas River, Kingston","interactions":[],"lastModifiedDate":"2016-05-20T14:30:18","indexId":"70139636","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":367,"text":"Massachusetts Hydrologic - Data Report","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"16","title":"Hydrologic data of the coastal drainage basins of southeastern Massachusetts, Weir River, Hingham, to Jonas River, Kingston","docAbstract":"<p>The principal basins are those of Weir River, James Brook, Bound Brook, North River, South River, and Jones River, all draining to Massachusetts Bay and Cape Cod Bay. These basins are bounded on the north by the Weymouth River basins, on the west by the Taunton River basin, and on the south by small basins that drain to Cape Cod Bay. The basins included all, or parts of, the Norwell, Pembroke, Plymouth, Plympton, Rockland, Scituate, Weymouth, and Whitman. With the following exceptions, each town is served by its own municipal water system--Hingham and northwest Cohasset by the Hingham Water Company; Abington and Rockland by the Abington-Rockland Joint Water Works; and Plympton lacks a public water supply. Weymouth and Cohasset are in Norfolk County; the other towns are in Plymouth County.</p>\n<p>This report presents, in tabular form, selected records of wells, test wells, borings, and springs; measurements of stream discharge, specific conductance, and temperature at partial-record stations; chemical analyses of ground water and surface water; and a summary of municipal water sources and additional sources available. The data were collected during a study of the drainage basins from 1969 to 1971 in cooperation with the Massachusetts Water Resources Commission. The report is released in order to make available to the public and to local, state, and federal agencies basic hydrologic information that may aid in planning water-resources development. Basic records contained in this report and streamflow data published elsewhere (U.S. Geol. Survey, 1960 et seq.) complement an interpretive report (Williams and Tasker, 1974).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Boston, MA","doi":"10.3133/70139636","collaboration":"Prepared in cooperation with the Commonwealth of Massachusetts, Water Resources Commission","usgsCitation":"Williams, J.R., Willey, R.E., and Tasker, G.D., 1975, Hydrologic data of the coastal drainage basins of southeastern Massachusetts, Weir River, Hingham, to Jonas River, Kingston: U.S. Geological Survey Massachusetts Hydrologic - Data Report 16, Report: 63 p.; Plate: 31.41 x 36.55 inches, https://doi.org/10.3133/70139636.","productDescription":"Report: 63 p.; Plate: 31.41 x 36.55 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":297607,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70139636.jpg"},{"id":321465,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70139636/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":321466,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70139636/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","country":"United States","state":"Massachusetts","otherGeospatial":"Jonas River, Weir River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.00807189941406,\n              41.90789845299648\n            ],\n            [\n              -71.00807189941406,\n              42.26816325848521\n            ],\n            [\n              -70.6036376953125,\n              42.26816325848521\n            ],\n            [\n              -70.6036376953125,\n              41.90789845299648\n            ],\n            [\n              -71.00807189941406,\n              41.90789845299648\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54dd2bcbe4b08de9379b34d7","contributors":{"authors":[{"text":"Williams, John R.","contributorId":107260,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"","middleInitial":"R.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":539470,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Willey, Richard E.","contributorId":30972,"corporation":false,"usgs":true,"family":"Willey","given":"Richard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":539471,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tasker, Gary D.","contributorId":95035,"corporation":false,"usgs":true,"family":"Tasker","given":"Gary","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":539472,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1003387,"text":"1003387 - 1975 - Residue dynamics of quinaldine and TFM in rainbow trout","interactions":[],"lastModifiedDate":"2023-11-14T17:35:18.112397","indexId":"1003387","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1736,"text":"General Pharmacology","active":true,"publicationSubtype":{"id":10}},"title":"Residue dynamics of quinaldine and TFM in rainbow trout","docAbstract":"<p>Study of the residue dynamics of 2-methylquinoline (quinaldine) and 3-trifluoromethyl-4-nitrophenol (TFM) in rainbow trout yielded the following findings:</p><p>1. Uptake and distribution of TFM by trout was influenced by the biotransformation of the lipidsoluble free phenol. No such effect was observed with quinaldine.</p><p>2. Disappearance of quinaldine and TFM from gallbladder bile was slower than from plasma or muscle during 24 hr of withdrawal in fresh water.</p><p>3. The concentration of TFM conjugate may exceed that of free TFM in bile by a factor of 10<sup>3</sup>.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0306-3623(75)90004-X","usgsCitation":"Hunn, J.B., and Allen, J.L., 1975, Residue dynamics of quinaldine and TFM in rainbow trout: General Pharmacology, v. 6, no. 1, p. 15-18, https://doi.org/10.1016/0306-3623(75)90004-X.","productDescription":"4 p.","startPage":"15","endPage":"18","numberOfPages":"4","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":130561,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b9b2","contributors":{"authors":[{"text":"Hunn, J. B.","contributorId":15133,"corporation":false,"usgs":true,"family":"Hunn","given":"J.","middleInitial":"B.","affiliations":[],"preferred":false,"id":313216,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allen, J. L.","contributorId":49295,"corporation":false,"usgs":true,"family":"Allen","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":313217,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70195624,"text":"70195624 - 1975 - New dimensions in diseases affecting waterfowl","interactions":[],"lastModifiedDate":"2018-02-23T13:31:15","indexId":"70195624","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"New dimensions in diseases affecting waterfowl","docAbstract":"<p><span>We start off with light heart, but as we near the marsh, we stop abruptly in shock and horror. The shoreline, where only last evening we saw thousands of sleek, apparently healthy birds, is now littered with their bodies. Most of them are ducks, but here and there we see a Canada goose, a gull, an avocet, a black-necked stilt, a pelican.....</span></p><p><span>This is the way Jensen and Williams (1964) described an outbreak of avian botulism in a western marsh. It illustrates, more vividly than dry facts and body counts, the impact a disease can have on a population of waterfowl.</span></p><p><span>When we think about waterfowl diseases, we probably think first of botulism and then of lead poisoning, the result of birds swallowing spent lead shot. In fact, these are the only two diseases discussed by Kortright (1942) and Day (1949) in major books on North American waterfowl, attesting to both their importance and our years of experience with them. Botulism was probably an old problem in 1910, but the catastrophic loss that summer of millions of aquatic birds near the Great Salt Lake and in California marked the beginning of real concern about its impact on waterfowl populations (Jensen and Williams, 1964). Concern about lead poisoning of waterfowl began a few years later following the investigations of Wetmore (1919).</span></p><p><span>Today, more than 50 years after these early reports, botulism and lead poisoning are still major disease problems of North American waterfowl, but they are no longer the only ones. After years of study, we have learned much about how these two diseases occur and about their prevention and control. But now there are new pathogens and new toxic compounds that can afflict waterfowl populations. So rather than redescribe the established disease problems of the past and present, I will concentrate on some of these new waterfowl disease problems of the present and future.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the first international waterfowl symposium","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"First international waterfowl symposium","conferenceDate":"February 4-6, 1975","conferenceLocation":"St. Louis, MO","language":"English","publisher":"Ducks Unlimited","usgsCitation":"Friend, M., 1975, New dimensions in diseases affecting waterfowl, <i>in</i> Proceedings of the first international waterfowl symposium, St. Louis, MO, February 4-6, 1975, p. 155-162.","productDescription":"8 p.","startPage":"155","endPage":"162","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":351935,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff5445e4b0da30c1bfdcbd","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":729454,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70190186,"text":"70190186 - 1975 - Limnological data for Donner Lake, California, May 1973 through December 1973","interactions":[],"lastModifiedDate":"2017-08-16T11:04:35","indexId":"70190186","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","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":"Limnological data for Donner Lake, California, May 1973 through December 1973","docAbstract":"<p>Donner Lake is easily accessible to the metropolitan areas of Sacramento and San Francisco and is close to many recreational areas in the Sierra Nevada. The lake is used for recreation and is bordered by commercial establishments, summer vacation homes, and a large state campground. Domestic wastes around the lake have received only septic tank treatment. A sewerage system under construction and partly in use at the time of this study has been completed and now (January 1975) all domestic wastes are transported out of the basin.</p><p>In September of 1969 and 1970, a brief survey of the lake was conducted (Iwatsubo and others, 1972, p. 28). The results of that study indicated a well-established thermocline between 33 and 66 ft (10 and 20 m). A subsurface maximum in the dissolved-oxygen concentration occurred between 46 and 66 ft (14 and 20 m). In the shallow littoral zone, periphyton and patches of submerged rooted plants were visible.</p><p>In order to remain attractive for recreational use, Donner Lake will require sound management. A thorough understanding of the water quality in the lake and the quality of inflow and outflow is of paramount importance.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70190186","usgsCitation":"Dong, A.E., 1975, Limnological data for Donner Lake, California, May 1973 through December 1973: Open-File Report, iv, 51 p., https://doi.org/10.3133/70190186.","productDescription":"iv, 51 p.","costCenters":[],"links":[{"id":344891,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70190186/report-thumb.jpg"},{"id":344890,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70190186/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Donner Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": 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,{"id":70181898,"text":"70181898 - 1975 - Gas bubble disease: mortalities of coho salmon, Oncorhynchus kisutch, in water with constant total gas pressure and different oxygen-nitrogen ratios","interactions":[],"lastModifiedDate":"2018-02-27T17:59:12","indexId":"70181898","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1663,"text":"Fishery Bulletin","printIssn":"0090-0656","active":true,"publicationSubtype":{"id":10}},"title":"Gas bubble disease: mortalities of coho salmon, Oncorhynchus kisutch, in water with constant total gas pressure and different oxygen-nitrogen ratios","docAbstract":"<p>A review of the literature regarding gas-bubble disease can be found in a recent publication by Rucker (1972); one by the National Academy of Science (Anonymous in press); and an unpublished report by Weitkamp and Katz (1973).\" Most discussions on gas-bubble disease have dealt with the inert gas, nitrogen-oxygen was given a secondary role. It is important to know the relationship of nitrogen and oxygen when we are concerned with the total gas pressure in water. Where water becomes aerated at dams or falls, oxygen and nitrogen are usually about equally saturated, however, many of the samples analyzed from the Columbia River indicate that nitrogen is often about 7% higher than oxygen when expressed as a percentage. When oxygen is removed from water by metabolic and chemical action, or when oxygen is added to the water by photosynthesis, there is a definite change in the ratio of oxygen and the inert gases (mainly nitrogen with some argon, etc.). This present study shows the effect of varying the oxygen and nitrogen ratio in water on fingerling coho salmon, Oncorh.llnchllS kislltch, while maintaining a constant total gas pressure. The primary purpose of these experiments was to determine differences in lethality of various gas ratios of oxygen and nitrogen at a constant total gas pressure of 119%. I also wished to determine whether there was a difference in susceptibility between sizes and stocks of juvenile coho. Also to be examined was the effect of reducing the oJl:ygen while holding the nitrogen constant.</p>","language":"English","usgsCitation":"Rucker, R., 1975, Gas bubble disease: mortalities of coho salmon, Oncorhynchus kisutch, in water with constant total gas pressure and different oxygen-nitrogen ratios: Fishery Bulletin, v. 73, no. 4, p. 915-918.","productDescription":"4 p. ","startPage":"915","endPage":"918","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":335438,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"73","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58a4254be4b0c825128ad4ef","contributors":{"authors":[{"text":"Rucker, R.R.","contributorId":104000,"corporation":false,"usgs":true,"family":"Rucker","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":668953,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70190623,"text":"70190623 - 1975 - Water development for irrigation in northwestern Kansas ","interactions":[],"lastModifiedDate":"2017-09-29T09:00:44","indexId":"70190623","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","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":"Water development for irrigation in northwestern Kansas ","docAbstract":"<p>Northwestern Kansas, an area of 8,050 square miles (21,000 square kilometres), is a flat to gently rolling plain that is dissected by the Smoky Hill and Republican Rivers. Loessial soils underlying the plain are ideal for cultivation.</p><p>The climate is semiarid with the mean annual precipitation ranging from 16 to 21 inches (41 to 53 centimetres). Precipitation occurring mainly as thunderstorms during the 6-month growing season is four to five times less than the potential evaporation.</p><p>Principal aquifers are the Dakota Formation, which yields a few gallons per minute of water to domestic and stock wells; the Ogallala Formation, which commonly yields 500 to 1,200 gallons per minute (32 to 76 litres per second) to irrigation wells; and the alluvium, which locally yields as much as 1,500 gallons per minute (95 litres per second) to irrigation wells.</p><p>Irrigation by ground water from wells has developed principally since the early 1950's. Development has increased from about 100 wells irrigating 10,000 acres (4,000 hectares) in 1950 to about 2,200 wells irrigating 300,000 acres (120,000 hectares) in 1972. The rate of withdrawal by irrigation, municipal, and industrial wells in 1972 was about 500,000 acre-feet (620 x 10<sup>6</sup> cubic metres) of water per year, of which about 99 percent was for irrigation.</p><p>A comparison of water levels measured in 1950 and in 1973 indicates that declines greater than 10 feet (3 metres) are common in much of the area. Declines greater than 30 feet (9 metres) have occurred near Goodland and Colby. The areas of greatest irrigation-well density correspond to the areas of greatest water-level decline.</p><p>More ground water could be withdrawn annually for irrigation, but additional water-level declines in some areas may make the wells uneconomical to pump. The ground-water reservoir can be managed to prolong the irrigation economy of the area.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70190623","usgsCitation":"Jenkins, E., and Pabst, M.E., 1975, Water development for irrigation in northwestern Kansas : Open-File Report, 39 p., https://doi.org/10.3133/70190623.","productDescription":"39 p.","numberOfPages":"49","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":346240,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70190623/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":345616,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70190623/report-thumb.jpg"}],"country":"United States","state":"Kansas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -102.052001953125,\n              38.698372305893294\n            ],\n            [\n              -100.15411376953125,\n              38.698372305893294\n            ],\n            [\n              -100.15411376953125,\n              40.00447583427404\n            ],\n            [\n              -102.052001953125,\n              40.00447583427404\n            ],\n            [\n              -102.052001953125,\n              38.698372305893294\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publicComments":"Open-File Report 4-75, Water Resources Division, U.S. Geological Survey","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59b7a0a9e4b08b1644df31cb","contributors":{"authors":[{"text":"Jenkins, Edward D.","contributorId":17972,"corporation":false,"usgs":true,"family":"Jenkins","given":"Edward D.","affiliations":[],"preferred":false,"id":710031,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pabst, Marilyn E.","contributorId":25566,"corporation":false,"usgs":true,"family":"Pabst","given":"Marilyn","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":710032,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70190913,"text":"70190913 - 1975 - Streamflow characteristics in northeastern Utah and adjacent areas","interactions":[],"lastModifiedDate":"2017-09-17T12:01:13","indexId":"70190913","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5498,"text":"Utah Basic-Data Release","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"25","title":"Streamflow characteristics in northeastern Utah and adjacent areas","docAbstract":"<p>This report contains statistical summaries of streamflow records from 74 gaging stations, which are mostly in northeastern Utah. Low- flow, high-flow, and flow-duration summaries were compiled from daily discharge values; and flows of each month are compared through correlation with flows of 1, 2, and 12 months in the future.<br></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources","usgsCitation":"Fields, F.K., 1975, Streamflow characteristics in northeastern Utah and adjacent areas: Utah Basic-Data Release 25, iv, 190 p.","productDescription":"iv, 190 p.","endPage":"191","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345841,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345840,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/docview.exe?Folder=TP21-1-490&Title=Basic+Data+Report+25"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59bf899ce4b091459a5e0885","contributors":{"authors":[{"text":"Fields, Fred K.","contributorId":69981,"corporation":false,"usgs":true,"family":"Fields","given":"Fred","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":710682,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70171428,"text":"70171428 - 1975 - Use of productivity of periphyton to estimate water quality","interactions":[],"lastModifiedDate":"2016-05-31T12:36:36","indexId":"70171428","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","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":"Use of productivity of periphyton to estimate water quality","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Water Pollution Control Federation","usgsCitation":"Tilley, L.J., and Haushild, W., 1975, Use of productivity of periphyton to estimate water quality: Journal of the Water Pollution Control Federation, v. 47, no. 8, p. 2157-2171.","productDescription":"15 p.","startPage":"2157","endPage":"2171","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":321915,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":321914,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/25038949?seq=1#page_scan_tab_contents"}],"volume":"47","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574eb5dde4b0ee97d51a8415","contributors":{"authors":[{"text":"Tilley, L. J.","contributorId":91836,"corporation":false,"usgs":true,"family":"Tilley","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":630957,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haushild, W.L.","contributorId":48953,"corporation":false,"usgs":true,"family":"Haushild","given":"W.L.","affiliations":[],"preferred":false,"id":630958,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175525,"text":"70175525 - 1975 - Hydrologic data for Mountain Creek, Trinity River Basin, Texas, 1973","interactions":[],"lastModifiedDate":"2016-08-16T10:26:41","indexId":"70175525","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","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, 1973","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70175525","usgsCitation":"Buckner, H., 1975, Hydrologic data for Mountain Creek, Trinity River Basin, Texas, 1973: Open-File Report, 13 p., https://doi.org/10.3133/70175525.","productDescription":"13 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326550,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b43950e4b03bcb01039fe2","contributors":{"authors":[{"text":"Buckner, H.D.","contributorId":49783,"corporation":false,"usgs":true,"family":"Buckner","given":"H.D.","email":"","affiliations":[],"preferred":false,"id":645564,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175526,"text":"70175526 - 1975 - Hydrologic data for Mukewater Creek, Colorado River Basin, Texas, 1973","interactions":[],"lastModifiedDate":"2016-08-16T10:28:35","indexId":"70175526","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","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 Mukewater Creek, Colorado River Basin, Texas, 1973","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70175526","usgsCitation":"Lee, J.N., 1975, Hydrologic data for Mukewater Creek, Colorado River Basin, Texas, 1973: Open-File Report, 65 p., https://doi.org/10.3133/70175526.","productDescription":"65 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326551,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b43950e4b03bcb01039fe6","contributors":{"authors":[{"text":"Lee, J. N.","contributorId":117799,"corporation":false,"usgs":true,"family":"Lee","given":"J.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":645566,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175528,"text":"70175528 - 1975 - Hydrologic data for North Creek, Trinity River basin, Texas, 1973","interactions":[],"lastModifiedDate":"2017-06-14T14:15:46","indexId":"70175528","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","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 North Creek, Trinity River basin, Texas, 1973","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70175528","usgsCitation":"Slade, R., 1975, Hydrologic data for North Creek, Trinity River basin, Texas, 1973: Open-File Report, 44 p., https://doi.org/10.3133/70175528.","productDescription":"44 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326552,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b43950e4b03bcb01039fe8","contributors":{"authors":[{"text":"Slade, R.M. Jr.","contributorId":40595,"corporation":false,"usgs":true,"family":"Slade","given":"R.M.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":645567,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70171427,"text":"70171427 - 1975 - Net primary productivity of periphytic algae in the intertidal zone, Duwamish River estuary, Washington","interactions":[],"lastModifiedDate":"2016-05-31T12:32:22","indexId":"70171427","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Net primary productivity of periphytic algae in the intertidal zone, Duwamish River estuary, Washington","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Tilley, L.J., and Haushild, W., 1975, Net primary productivity of periphytic algae in the intertidal zone, Duwamish River estuary, Washington: Journal of Research of the U.S. Geological Survey, v. 3, no. 3, p. 253-259.","productDescription":"7 p.","startPage":"253","endPage":"259","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":321913,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574eb5d8e4b0ee97d51a83de","contributors":{"authors":[{"text":"Tilley, L. J.","contributorId":91836,"corporation":false,"usgs":true,"family":"Tilley","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":630955,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haushild, W.L.","contributorId":48953,"corporation":false,"usgs":true,"family":"Haushild","given":"W.L.","affiliations":[],"preferred":false,"id":630956,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175529,"text":"70175529 - 1975 - Ground-water data for Orange County and vicinity, Texas and Louisiana, 1971–74","interactions":[],"lastModifiedDate":"2016-08-17T11:28:03","indexId":"70175529","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","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":"197","title":"Ground-water data for Orange County and vicinity, Texas and Louisiana, 1971–74","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Texas Water Development Board","usgsCitation":"Bonnet, C., 1975, Ground-water data for Orange County and vicinity, Texas and Louisiana, 1971–74: Texas Water Development Board Report 197, 26 p.","productDescription":"26 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326553,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b4394ae4b03bcb01039fcb","contributors":{"authors":[{"text":"Bonnet, C.W.","contributorId":44535,"corporation":false,"usgs":true,"family":"Bonnet","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":645568,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175575,"text":"70175575 - 1975 - Chemical and physical characteristics of water in estuaries of Texas, October 1970-September 1971","interactions":[],"lastModifiedDate":"2016-08-17T11:12:41","indexId":"70175575","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","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":"191","title":"Chemical and physical characteristics of water in estuaries of Texas, October 1970-September 1971","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Texas Water Development Board","usgsCitation":"Hahl, D.C., and Ratzlaff, K.W., 1975, Chemical and physical characteristics of water in estuaries of Texas, October 1970-September 1971: Texas Water Development Board Report 191, 153 p.","productDescription":"153 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326643,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58ac0e4b03bcb0104bb70","contributors":{"authors":[{"text":"Hahl, D. C.","contributorId":57436,"corporation":false,"usgs":true,"family":"Hahl","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":645739,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ratzlaff, Karl W.","contributorId":99177,"corporation":false,"usgs":true,"family":"Ratzlaff","given":"Karl","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":645740,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175577,"text":"70175577 - 1975 - Water-quality records for selected reservoirs in Texas, 1972-73 water years","interactions":[],"lastModifiedDate":"2016-08-17T11:15:01","indexId":"70175577","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","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":"194","title":"Water-quality records for selected reservoirs in Texas, 1972-73 water years","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Texas Water Development Board","usgsCitation":"Rawson, J., and Davidson, H., 1975, Water-quality records for selected reservoirs in Texas, 1972-73 water years: Texas Water Development Board Report 194, 132 p.","productDescription":"132 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326646,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58b72e4b03bcb0104bcb7","contributors":{"authors":[{"text":"Rawson, Jack","contributorId":18345,"corporation":false,"usgs":true,"family":"Rawson","given":"Jack","affiliations":[],"preferred":false,"id":645743,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davidson, H.J.","contributorId":108177,"corporation":false,"usgs":true,"family":"Davidson","given":"H.J.","email":"","affiliations":[],"preferred":false,"id":645744,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175639,"text":"70175639 - 1975 - Ground-water data in the Harrisburg-Halsey area, central Willamette Valley, Oregon","interactions":[],"lastModifiedDate":"2016-08-17T14:12:43","indexId":"70175639","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":115,"text":"Ground Water Report","active":false,"publicationSubtype":{"id":2}},"title":"Ground-water data in the Harrisburg-Halsey area, central Willamette Valley, Oregon","docAbstract":"<p><span class=\"EXLDetailsDisplayVal\">THE <span class=\"searchword\">HARRISBURG</span>-<span class=\"searchword\">HALSEY</span> <span class=\"searchword\">AREA</span> COVERS ABOUT 350 SQUARE MILES IN THE <span class=\"searchword\">CENTRAL</span> <span class=\"searchword\">WILLAMETTE</span> <span class=\"searchword\">VALLEY</span>, OREG., AND IS PART OF A BROAD ALLUVIAL PLAIN THAT LIES BETWEEN THE CASCADE AND COAST RANGES IN THE <span class=\"searchword\">CENTRAL</span> PART OF THE <span class=\"searchword\">WILLAMETTE</span> <span class=\"searchword\">VALLEY</span>. MOST OF THE <span class=\"searchword\">DATA</span> FOR THE 506 WELLS IN THIS REPORT WERE OBTAINED FROM WELL DRILLERS' REPORTS. CHEMICAL ANALYSES OF <span class=\"searchword\">WATER</span> FROM 36 WELLS ARE TABULATED. MOST OF THE HIGH-YIELD WELLS IN THE <span class=\"searchword\">AREA</span> PRODUCE <span class=\"searchword\">WATER</span> FROM ALLUVIAL (SAND AND GRAVEL) AQUIFERS THAT UNDERLIE THE <span class=\"searchword\">VALLEY</span> PLAIN OR THAT ARE COEXTENSIVE WITH THE PRESENT FLOOD PLAIN OF THE <span class=\"searchword\">WILLAMETTE</span> RIVER. THE <span class=\"searchword\">WATER</span> TABLE IN THE ALLUVIAL AQUIFER IS GENERALLY ONLY A FEW FEET BELOW LAND SURFACE. PUMPING LIFTS ARE RELATIVELY SMALL, AND WELLS PRODUCE MODERATE TO LARGE QUANTITIES OF GROUNDWATER OF GOOD CHEMICAL QUALITY</span>.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Frank, F.J., and Johnson, N.A., 1975, Ground-water data in the Harrisburg-Halsey area, central Willamette Valley, Oregon: Ground Water Report.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":326727,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","city":"Halsey, Harrisburg","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58ad0e4b03bcb0104bbb6","contributors":{"authors":[{"text":"Frank, F. J.","contributorId":95037,"corporation":false,"usgs":true,"family":"Frank","given":"F.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":645905,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Nyra A.","contributorId":173771,"corporation":false,"usgs":false,"family":"Johnson","given":"Nyra","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":645906,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70176025,"text":"70176025 - 1975 - Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1974","interactions":[],"lastModifiedDate":"2016-08-23T15:33:56","indexId":"70176025","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","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":"34","title":"Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1974","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Rappmund, R.A., 1975, Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1974: Edwards Underground Water District Bulletin 34, 8 p.","productDescription":"8 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":327751,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73dde4b03fd6b7df2d01","contributors":{"authors":[{"text":"Rappmund, R. A.","contributorId":173985,"corporation":false,"usgs":false,"family":"Rappmund","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":646813,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175524,"text":"70175524 - 1975 - Hydrologic data for Little Elm Creek, Trinity River Basin, Texas, 1973","interactions":[],"lastModifiedDate":"2021-11-09T20:42:23.281807","indexId":"70175524","displayToPublicDate":"1975-01-01T00:00:00","publicationYear":"1975","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 Little Elm Creek, Trinity River Basin, Texas, 1973","docAbstract":"<p>The U.S. Soil Conservation Service is actively engaged in the implementation of flood- and soil-erosion reducing measures in Texas under the authority of \"The Flood Control Act of 1936 and 1944\" and \"Watershed Protection and Flood Prevention Act\" (Public Law 566), as amended. The Soil Conservation Service has found that approximately 3,500 floodwater-retarding structures would be physically and economically feasible in Texas. As of September 30, 1973. 1,587 of these structures had been built. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70175524","collaboration":"Prepared in cooperation with the city of Dallas and the Texas Water Development Board","usgsCitation":"Slade, R., and Taylor, J., 1975, Hydrologic data for Little Elm Creek, Trinity River Basin, Texas, 1973: Open-File Report, 74 p., https://doi.org/10.3133/70175524.","productDescription":"74 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":391531,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70175524/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":326549,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70175524/report-thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Little Elm Creek","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b4394fe4b03bcb01039fde","contributors":{"authors":[{"text":"Slade, R.M. Jr.","contributorId":40595,"corporation":false,"usgs":true,"family":"Slade","given":"R.M.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":645562,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, J.M.","contributorId":42587,"corporation":false,"usgs":true,"family":"Taylor","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":645563,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}