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B.","contributorId":31375,"corporation":false,"usgs":true,"family":"Simon","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":147178,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stover, Carl W.","contributorId":28955,"corporation":false,"usgs":true,"family":"Stover","given":"Carl","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":147177,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":4391,"text":"cir736D - 1977 - Seismic engineering program report, October-December 1976","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"cir736D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"736","chapter":"D","title":"Seismic engineering program report, October-December 1976","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey ;\r\nFree on application to Branch of Distribution, U.S. Geological Survey,","doi":"10.3133/cir736D","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1977, Seismic engineering program report, October-December 1976: U.S. Geological Survey Circular 736, v, 23 p. :ill. ;26 cm., https://doi.org/10.3133/cir736D.","productDescription":"v, 23 p. :ill. ;26 cm.","costCenters":[],"links":[{"id":121257,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1977/0736d/report-thumb.jpg"},{"id":31500,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1977/0736d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb826","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":528209,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3866,"text":"cir745 - 1977 - Water consumption by nuclear powerplants and some hydrological implications","interactions":[],"lastModifiedDate":"2017-07-07T08:39:03","indexId":"cir745","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"745","title":"Water consumption by nuclear powerplants and some hydrological implications","docAbstract":"Published data show that estimated water consumption varies with the cooling system adopted, being least in once-through cooling (about 18 cubic feet per second per 1,000 megawatts electrical) and greatest in closed cooling with mechanical draft towers (about 30 cubic feet per second per 1,000 megawatts electrical). When freshwater is used at this magnitude, water-resources economy may be affected in a given region. The critical need for cooling water at all times by the nuclear powerplant industry, coupled with the knowledge that water withdrawal in the basin will generally increase with time and will be at a maximum during low-flow periods, indicates a need for reexamination of the design low flow currently adopted and the methods used to estimate it. The amount of power generated, the name of the cooling water source, and the cooling method adopted for all nuclear powerplants projected to be in operation by 1985 in the United States are tabulated and the estimated annual evaporation at each powerplant site is shown on a map of the conterminous United States. Another map is presented that shows all nuclear powerplants located on river sites as well as stream reaches in the United States where the 7-day, 10-year low flow is at least 300 cubic feet per second or where this amount of flow can be developed with storage. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir745","usgsCitation":"Giusti, E.V., and Meyer, E., 1977, Water consumption by nuclear powerplants and some hydrological implications: U.S. Geological Survey Circular 745, iii, 14 p. :ill. ;26 cm. , https://doi.org/10.3133/cir745.","productDescription":"iii, 14 p. :ill. ;26 cm. 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The report for each analytical method includes conditions for application of the method, a summary of the method, interferences, required apparatus and reagents, analytical procedures, calculations, reporting of results, and estimation of precision. The fission product isotopes considered are cesium-137, strontium-90, and ruthenium-106. The natural radioelements and isotopes considered are uranium, lead-210, radium-226, radium-228, tritium, and carbon-14. A gross radioactivity survey method and a uranium isotope ratio method are given. When two analytical methods are in routine use for an individual isotope, both methods are reported with identification of the specific areas of application of each. 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The best known springs were the Smith Springs (now under the McMillan Reservoir), the Franklin Park Springs (13th and I Streets, NW.), Gibson 's Spring (15th and E Streets, NE.), Caffrey 's Spring (Ninth and F Streets, NW.), and the City Spring (C Street between Four and One-Half and Sixth Streets, NW.). Tiber Creek, flowing south to the Capitol and thence westward along Consititution Avenue, joined the Potomac River at 17th Street and Constitution Avenue. In the 1800's, the Constitution Avenue reach was made into a canal which was used by scows and steamboats up to about 1850. The canal was changed into a covered sewer in the 1870's, and the only remaining visible surface remnant is the lock-keeper 's little stone house at 17th and Constitution Avenue, NW. Because of sedimentation problems and reclamation projects, Rock Creek, the Potomac River , and the Anacostia River are considerably narrower and shallower today than they were in colonial times. For example, the mouth of Rock Creek at one time was a wide, busy ship harbor , which Georgetown used for an extensive foreign trade, and the Potomac River shore originally extended to 17th and Constitution Avenue, NW. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir752","usgsCitation":"Williams, G.P., 1977, Washington, D.C.'s vanishing springs and waterways: U.S. Geological Survey Circular 752, iii, 19 p. :ill. ;26 cm., https://doi.org/10.3133/cir752.","productDescription":"iii, 19 p. :ill. ;26 cm.","costCenters":[],"links":[{"id":138440,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1977/0752/report-thumb.jpg"},{"id":30249,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1977/0752/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb73f","contributors":{"authors":[{"text":"Williams, Garnett P.","contributorId":100361,"corporation":false,"usgs":true,"family":"Williams","given":"Garnett","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":146519,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4276,"text":"cir749C - 1977 - Earthquakes in the United States: July-September 1975","interactions":[],"lastModifiedDate":"2022-08-22T20:00:26.813734","indexId":"cir749C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"749","chapter":"C","title":"Earthquakes in the United States: July-September 1975","docAbstract":"No abstract available.
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In 1975, withdrawals for these uses exceeded by 11.7 percent the 370 bgd estimated for 1970. Increases in the various categories of off-channel water use since 1970 were: approximately 12.8 percent for self-supplied industry (mainly in electric-utility thermoelectric plants), 7.9 percent for public supplies, 10.3 percent for rural supplies, and 10.9 percent for irrigation. Industrial water withdrawals included 70 bgd of saline water, a 30 percent increase in 5 years. The fifth principal withdrawal use, hydroelectric power (an in-channel use), amounted to 3,300 bgd, a 5-year increase of 20.7 percent. In computing total withdrawals, recycling within a plant (reuse) is not counted, but withdrawal of the same water by a downstream user (cumulative withdrawals) is counted. The quantity of freshwater consumed that is, water made unavailable for further possible withdrawal because of evaporation, incorporation in crops and manufactured products, and other causes was estimated to average 96 bgd for 1975, an increase of about 10 percent since 1970.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/cir765","usgsCitation":"Murray, C.R., and Reeves, E.B., 1977, Estimated use of water in the United States in 1975: U.S. Geological Survey Circular 765, vi, 39 p., https://doi.org/10.3133/cir765.","productDescription":"vi, 39 p.","numberOfPages":"46","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":124224,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1977/0765/report-thumb.jpg"},{"id":30647,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1977/0765/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db6845fe","contributors":{"authors":[{"text":"Murray, Charles Richard","contributorId":34115,"corporation":false,"usgs":true,"family":"Murray","given":"Charles","email":"","middleInitial":"Richard","affiliations":[{"id":36966,"text":"Pennsylvania Fish and Boat Commission","active":true,"usgs":false}],"preferred":false,"id":147254,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reeves, E. Bodette","contributorId":100366,"corporation":false,"usgs":true,"family":"Reeves","given":"E.","email":"","middleInitial":"Bodette","affiliations":[],"preferred":false,"id":147255,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":4302,"text":"cir750 - 1977 - Geological studies on the COST No. B-2 well, U. S. Mid-Atlantic outer continental shelf area","interactions":[],"lastModifiedDate":"2012-02-02T00:05:33","indexId":"cir750","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"750","title":"Geological studies on the COST No. B-2 well, U. S. Mid-Atlantic outer continental shelf area","docAbstract":"The COST No. B-2 well is the first deep stratigraphic test to be drilled on the United States Atlantic Outer Continental Shelf (AOCS) area. The well was drilled on the eastern flank of the Baltimore Canyon trough to a total depth of 16,043 feet; it penetrated a section composed almost entirely of sand and shale with subordinate amounts of limestone, coal, and lignite. Biostratigraphic studies have shown that the uppermost 5,000 feet is of Tertiary and Quaternary age and was deposited in nonmarine to deep marine environments. The Upper Cretaceous section is about 3,000 feet thick and is of dominantly shallow marine origin. The basal 8,000 feet of sediment has been tentatively determined to be entirely of Early Cretaceous age, the basal sediments being dated as Berriasian. This Lower Cretaceous section is primarily nonmarine to very shallow marine in origin. \r\n\r\nExamination of cores, well cuttings, and electric logs shows that thick potential reservoir sands are found through much of the section. However, porosity and permeability decrease strikingly in the deeper parts of the Lower Cretaceous section as a result of compaction and cementation. Most of the sands are quite feldspathic, and progressive decomposition of feldspar stimulates authigenic clay and silica formation. \r\n\r\nStudies of color alteration of visible organic matter, organic geochemistry, and vitrinite reflectance show that although many units have high organic-carbon contents, moderately low geothermal gradients may have retarded thermal maturation. This, in conjunction with the scarcity of marine-derived organic matter in the lower part of the section, suggests a relatively low potential for the generation of liquid hydrocarbons. However, the overall combination of source beds, reservoirs, seals, structures, and thermal gradients may be favorable for the generation and entrapment of natural gas. \r\n\r\nFurthermore, the presence of reservoir rocks, seals, and trapping structures may indicate a significant potential for entrapment of either natural gas or petroleum that was generated deeper in the basin and then migrated either laterally or vertically.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir750","usgsCitation":"Scholle, P.A., 1977, Geological studies on the COST No. B-2 well, U. S. Mid-Atlantic outer continental shelf area: U.S. Geological Survey Circular 750, iv, 71 p. :ill., map ;26 cm. , https://doi.org/10.3133/cir750.","productDescription":"iv, 71 p. :ill., map ;26 cm. 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B.","contributorId":31375,"corporation":false,"usgs":true,"family":"Simon","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":148713,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":4414,"text":"cir715F - 1977 - A synoptic survey of trace metals in bottom sediments of the Willamette River, Oregon","interactions":[],"lastModifiedDate":"2017-02-03T13:54:50","indexId":"cir715F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"715","chapter":"F","title":"A synoptic survey of trace metals in bottom sediments of the Willamette River, Oregon","docAbstract":"For nearly half a century the Willamette River in Oregon experienced severe dissolved-oxygen problems related to large loads of organically rich waste waters from industries and municipalities. Since the mid-1950 's dissolved oxygen quality has gradually improved owing to low-flow augmentation, the achievement of basinwide secondary treatment, and the use of other waste-management practices. As a result, summer dissolved-oxygen levels have increased, salmon runs have returned, and the overall effort is widely regarded as a singular water-quality success. To document the improved dissolved-oxygen regimen, the U.S. Geological Survey conducted intensive studies of the Willamette during the summer low-flow seasons of 1973 and 1974. During each summer the mean daily dissolved-oxygen levels were found to be higher than 5 milligrams per liter throughout the river. Because of the basinwide secondary treatment, carbonaceous deoxygenation rates were low. In addition, almost half of the biochemical oxygen demand entering the Willamette was from diffuse (nonpoint) sources rather than outfalls. These results indicated that point-source biochemical oxygen demand was no longer the primary cause of dissolved-oxygen depletion. Instead, the major causes of deoxygenation were nitrification in a shallow ' surface active ' reach below Salem and an anomalous oxygen demand (believed to be primarily of benthal origin) in Portland Harbor. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/cir715F","usgsCitation":"Rickert, D.A., Kennedy, V.C., McKenzie, S.W., and Hines, W.G., 1977, A synoptic survey of trace metals in bottom sediments of the Willamette River, Oregon: U.S. Geological Survey Circular 715, vi, p F1-F27, ill., maps ;27 cm. , https://doi.org/10.3133/cir715F.","productDescription":"vi, p F1-F27, ill., maps ;27 cm. ","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":31519,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1977/0715f/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138707,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1977/0715f/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a5e2d","contributors":{"authors":[{"text":"Rickert, David A.","contributorId":80247,"corporation":false,"usgs":true,"family":"Rickert","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":149079,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kennedy, V. C.","contributorId":46080,"corporation":false,"usgs":true,"family":"Kennedy","given":"V.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":149077,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McKenzie, S. W.","contributorId":66240,"corporation":false,"usgs":true,"family":"McKenzie","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":149078,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hines, W. G.","contributorId":84742,"corporation":false,"usgs":true,"family":"Hines","given":"W.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":149080,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":3578,"text":"cir761 - 1977 - Socioeconomic impacts of outer continental shelf oil and gas development; a bibliography","interactions":[],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"cir761","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"761","title":"Socioeconomic impacts of outer continental shelf oil and gas development; a bibliography","docAbstract":"The bibliography lists reports which are concerned primarily with the socioeconomic impacts of OCS oil and gas development or which, although not primarily concerned with such impacts, include sections that contain significant discussion of them. Several of the cited reports do not address socioeconomic issues directly, but have been included because of their value in providing a broad picture of OCS oil and gas development and the associated terminology and/or techical aspects. (Sinha - OEIS)","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/cir761","usgsCitation":"Pattison, M.L., 1977, Socioeconomic impacts of outer continental shelf oil and gas development; a bibliography: U.S. Geological Survey Circular 761, iii, 63 p. ;26 cm., https://doi.org/10.3133/cir761.","productDescription":"iii, 63 p. ;26 cm.","costCenters":[],"links":[{"id":117771,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1977/0761/report-thumb.jpg"},{"id":30607,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1977/0761/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b435c","contributors":{"authors":[{"text":"Pattison, Malka L.","contributorId":27739,"corporation":false,"usgs":true,"family":"Pattison","given":"Malka","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":147188,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4272,"text":"cir715I - 1977 - Dissolved-oxygen regimen of the Willamette River, Oregon, under conditions of basinwide secondary treatment","interactions":[],"lastModifiedDate":"2017-02-03T13:55:37","indexId":"cir715I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"715","chapter":"I","title":"Dissolved-oxygen regimen of the Willamette River, Oregon, under conditions of basinwide secondary treatment","docAbstract":"For nearly half a century the Willamette River in Oregon experienced severe dissolved-oxygen problems related to large loads of organically rich waste waters from industries and municipalities. Since the mid-1950 's dissolved oxygen quality has gradually improved owing to low-flow augmentation, the achievement of basinwide secondary treatment, and the use of other waste-management practices. As a result, summer dissolved-oxygen levels have increased, salmon runs have returned, and the overall effort is widely regarded as a singular water-quality success. To document the improved dissolved-oxygen regimen, the U.S. Geological Survey conducted intensive studies of the Willamette during the summer low-flow seasons of 1973 and 1974. During each summer the mean daily dissolved-oxygen levels were found to be higher than 5 milligrams per liter throughout the river. Because of the basinwide secondary treatment, carbonaceous deoxygenation rates were low. In addition, almost half of the biochemical oxygen demand entering the Willamette was from diffuse (nonpoint) sources rather than outfalls. These results indicated that point-source biochemical oxygen demand was no longer the primary cause of dissolved-oxygen depletion. Instead, the major causes of deoxygenation were nitrification in a shallow ' surface active ' reach below Salem and an anomalous oxygen demand (believed to be primarily of benthal origin) in Portland Harbor. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir715I","usgsCitation":"Hines, W.G., McKenzie, S.W., Rickert, D.A., and Rinella, F.A., 1977, Dissolved-oxygen regimen of the Willamette River, Oregon, under conditions of basinwide secondary treatment: U.S. Geological Survey Circular 715, vii, p I1-I52, ill., maps ;26 cm. , https://doi.org/10.3133/cir715I.","productDescription":"vii, p I1-I52, ill., maps ;26 cm. ","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":123800,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1977/0715i/report-thumb.jpg"},{"id":31383,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1977/0715i/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a220","contributors":{"authors":[{"text":"Hines, Walter G.","contributorId":100360,"corporation":false,"usgs":true,"family":"Hines","given":"Walter","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":148667,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McKenzie, S. W.","contributorId":66240,"corporation":false,"usgs":true,"family":"McKenzie","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":148665,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rickert, D. A.","contributorId":53773,"corporation":false,"usgs":true,"family":"Rickert","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":148664,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rinella, F. A.","contributorId":89120,"corporation":false,"usgs":true,"family":"Rinella","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":148666,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":4030,"text":"cir748 - 1977 - A device for automatic photoelectric control of the analytical gap for emission spectrographs","interactions":[],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"cir748","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"748","title":"A device for automatic photoelectric control of the analytical gap for emission spectrographs","docAbstract":"A photoelectric device has been built that automatically controls the analytical gap between electrodes during excitation period. The control device allows for precise control of the analytical gap during the arcing process of samples, resulting in better precision of analysis.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir748","usgsCitation":"Dietrich, J., Cooley, E.F., and Curry, K., 1977, A device for automatic photoelectric control of the analytical gap for emission spectrographs: U.S. Geological Survey Circular 748, iii, 5 p. :ill. ;27 cm. , https://doi.org/10.3133/cir748.","productDescription":"iii, 5 p. :ill. ;27 cm. ","costCenters":[],"links":[{"id":120919,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1977/0748/report-thumb.jpg"},{"id":31122,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1977/0748/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aee52","contributors":{"authors":[{"text":"Dietrich, John A.","contributorId":91473,"corporation":false,"usgs":true,"family":"Dietrich","given":"John A.","affiliations":[],"preferred":false,"id":148030,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooley, Elmo F.","contributorId":71950,"corporation":false,"usgs":true,"family":"Cooley","given":"Elmo","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":148028,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Curry, Kenneth J.","contributorId":75511,"corporation":false,"usgs":true,"family":"Curry","given":"Kenneth J.","affiliations":[],"preferred":false,"id":148029,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":11127,"text":"ofr77607 - 1977 - Preliminary data on some Precambrian deposits of zinc-copper-lead sulfides and zinc spinel (granite) in Colorado","interactions":[{"subject":{"id":11127,"text":"ofr77607 - 1977 - Preliminary data on some Precambrian deposits of zinc-copper-lead sulfides and zinc spinel (granite) in Colorado","indexId":"ofr77607","publicationYear":"1977","noYear":false,"title":"Preliminary data on some Precambrian deposits of zinc-copper-lead sulfides and zinc spinel (granite) in Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":35806,"text":"b1550 - 1984 - Precambrian deposits of zinc-copper-lead sulfides and zinc spinel (gahnite) in Colorado","indexId":"b1550","publicationYear":"1984","noYear":false,"title":"Precambrian deposits of zinc-copper-lead sulfides and zinc spinel (gahnite) in Colorado"},"id":1}],"supersededBy":{"id":35806,"text":"b1550 - 1984 - Precambrian deposits of zinc-copper-lead sulfides and zinc spinel (gahnite) in Colorado","indexId":"b1550","publicationYear":"1984","noYear":false,"title":"Precambrian deposits of zinc-copper-lead sulfides and zinc spinel (gahnite) in Colorado"},"lastModifiedDate":"2022-01-03T18:17:01.023948","indexId":"ofr77607","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-607","title":"Preliminary data on some Precambrian deposits of zinc-copper-lead sulfides and zinc spinel (granite) in Colorado","docAbstract":"Precambrian sulfide deposits in the Southern Rocky Mountains in Colorado are being studied and re-evaluated according to geologic concepts which were developed in recent years in other parts of the world during successful research regarding economic massive sulfide deposits. These studies, initiated in 1974 in Colorado by the U.S. Geological Survey, have indicated that a new look at areas containing long dormant mines and prospects may well lead to the discovery of minable Precambrian sulfide deposits. The zinc, copper, and lead contents of ores investigated to date, supplemented by silver and gold contents, indicate that many long-forgotten deposits are minable in terms of grade. The deposits occur in Precambrian rocks metamorphosed to the lower amphibolite facies in one major region and to the upper amphibolite facies in other regions. Field studies have provided ample evidence indicating that the search for commercial tonnages can he facilitated by using newer concepts of economic geology regarding ore-host rock associations as prospecting guides and by using structural considerations aimed toward learning how metamorphism and folding have modified the shapes and distribution of the ore bodies. A newly recognized concept, originating from the current studies by the U.S. Geological Survey in Colorado, concerns the potential economic significance of gahnite, a zinc spinel. The field and laboratory data indicate that gahnite can be used by geologists as a prospector's guide to ore and can be considerd by mining engineers as a potential major ore mineral, contributing significant amounts of zinc to the sulfide ores in many of the deposits. Studies to date indicate that the Gunnison area, the Salida area, and the Guffey area are particularly favorable to the search for minable deposits, and the potential is equally present in many other areas.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77607","usgsCitation":"Sheridan, D.M., and Raymond, W.H., 1977, Preliminary data on some Precambrian deposits of zinc-copper-lead sulfides and zinc spinel (granite) in Colorado: U.S. Geological Survey Open-File Report 77-607, ii, 27 p., https://doi.org/10.3133/ofr77607.","productDescription":"ii, 27 p.","costCenters":[],"links":[{"id":143534,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0607/report-thumb.jpg"},{"id":393763,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0607/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109,\n 37\n ],\n [\n -104,\n 37\n ],\n [\n -104,\n 41\n ],\n [\n -109,\n 41\n ],\n [\n -109,\n 37\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c52c","contributors":{"authors":[{"text":"Sheridan, Douglas M.","contributorId":13966,"corporation":false,"usgs":true,"family":"Sheridan","given":"Douglas","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":162592,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Raymond, William H.","contributorId":48555,"corporation":false,"usgs":true,"family":"Raymond","given":"William","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":162593,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11813,"text":"ofr7756 - 1977 - Ground-water resources and geology of Colquitt County, Georgia","interactions":[],"lastModifiedDate":"2016-12-14T10:12:07","indexId":"ofr7756","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-56","title":"Ground-water resources and geology of Colquitt County, Georgia","docAbstract":"Limestone beds of Eocene, Oligocene, and lower Miocene age, called the principal artesian aquifer, are the chief source of ground water for Colquitt County. Because streams are small, undependable and relatively inaccessible to most users, ground water is the most important source for increased industrial and agricultural water use. Southeast of Moultrie the principal artesian aquifer is very productive, and has transmissivity in excess of 145,000 feet squared per day (13,500 meters squared per day). A structural or paleogeographic feature called the Suwannee strait traverses the county from near the southwest corner to the northeast corner. In this strait, limestone in the principal artesian aquifer is partly replaced by fine-grained clastic sediment, impairing transmissivity and making wells hard to construct. Transmissivity is much lower northwest of the strait than it is southeast, probably because of facies changes in the aquifer.
\nIn the belt of the hypothesized Ochlockonee fault, water containing greater-than-usual concentrations of dissolved solids is produced. This anomaly could be the result of the fault having acted as a conduit when the vertical hydraulic gradient was upward from a deeper aquifer, or be the result of the movement of ground water from a sulfate-rich source in the sediments of the Suwannee strait. In south-central Colquitt County, clay-capped permeable beds extending above potentiometric surfaces create conditions favorable for breathing wells.
\nPredominantly clastic beds of Miocene age overlie the Suwannee Limestone. These beds have a transmissivity of about 2,280 feet squared per day (215 meters squared per day), but they are of comparatively little importance because larger yields can be obtained from the underlying principal artesian aquifer. Moreover, wells are difficult to construct in the poorly consolidated clastic sediments, and water from these shallow beds is likely to be depleted during droughts.
\nThe ground water is generally hard, but is otherwise of good quality. One exception is near the hypothesized Ochlockonee fault where water contains higher-than-usual concentrations of various ions, especially sulfate. Another exception occurs along the axis of the Suwannee strait where clay minerals in the channel facies may soften the water by ion exchange.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Doraville, Georgia","doi":"10.3133/ofr7756","collaboration":"Prepared in cooperation with Georgia Department of Natural Resources, Geologic and Water Resources Division","usgsCitation":"Zimmerman, E.A., 1977, Ground-water resources and geology of Colquitt County, Georgia: U.S. Geological Survey Open-File Report 77-56, vi, 41 p., https://doi.org/10.3133/ofr7756.","productDescription":"vi, 41 p.","numberOfPages":"52","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":144821,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr7756.jpg"},{"id":325511,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0056/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Georgia","county":"Colquitt 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Oxidizing, silica undersaturated, alkaline solutions are eluted through a column of rhyolitic glass shards at a carefully controlled temperature, pressure, and flow rate. The solutions are monitored for the concentration of uranium and selected additional elements (Si, K, Li, F), and the glass is recovered and examined for physical and/or chemical evidence of attack. The flushing mode is designed to mimic leaching of glass shards by intermittent, near-surface waters with which the glass is not in equilibrium. \r\n\r\nReported rates are applicable only to the experimental conditions (120?C, 7,000 psi), but it is assumed that the reaction mechanisms and the relative importance of rate-influencing parameters remain unchanged, at reduced temperature and pressure. Results of the above experiment indicate that silica and uranium are released from glass shards at comparable rates, while lithium and potassium are released faster and fluorine slower than either Si or U. Rates of release of silica and uranium correlate positively with the surface area of the shards. Rhyolitic shards release uranium at faster rates than rhyodacitic shards of comparable surface area. Changes in the shards resulting from experimental treatment and observed in the original glass separates from an Oligocene ash (compared to a Pleistocene ash) include; surface pitting, increased surface area, devitrification rinds (<1l micron wide) and reduced lithium contents. Future investigations will study the effect of temperature, pressure, solution composition, and flow rate on the relative mobility of U, Si, Li, F, and K.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77744","usgsCitation":"Zielinski, R.A., 1977, Uranium mobility during interaction of rhyolitic glass with alkaline solutions: dissolution of glass: U.S. Geological Survey Open-File Report 77-744, 36, [5] leaves of plates :ill. ;28 cm.; (41 p. - PGS), https://doi.org/10.3133/ofr77744.","productDescription":"36, [5] leaves of plates :ill. ;28 cm.; (41 p. - PGS)","costCenters":[],"links":[{"id":145048,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0744/report-thumb.jpg"},{"id":39701,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0744/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db60541a","contributors":{"authors":[{"text":"Zielinski, Robert A. 0000-0002-4047-5129 rzielinski@usgs.gov","orcid":"https://orcid.org/0000-0002-4047-5129","contributorId":1593,"corporation":false,"usgs":true,"family":"Zielinski","given":"Robert","email":"rzielinski@usgs.gov","middleInitial":"A.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":163765,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11804,"text":"ofr77328 - 1977 - Floodflow characteristics at proposed channel-relocation site on Mohawk River near Rome, New York","interactions":[],"lastModifiedDate":"2013-02-15T07:40:04","indexId":"ofr77328","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-328","title":"Floodflow characteristics at proposed channel-relocation site on Mohawk River near Rome, New York","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77328","usgsCitation":"Zembrzuski, T., and Dunn, B., 1977, Floodflow characteristics at proposed channel-relocation site on Mohawk River near Rome, New York: U.S. Geological Survey Open-File Report 77-328, iv, 18 leaves :ill., map ;29 cm.; (28 p. - PGS), https://doi.org/10.3133/ofr77328.","productDescription":"iv, 18 leaves :ill., map ;29 cm.; (28 p. - PGS)","costCenters":[],"links":[{"id":145024,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":267458,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0328/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e73c7","contributors":{"authors":[{"text":"Zembrzuski, Thomas J.","contributorId":52573,"corporation":false,"usgs":true,"family":"Zembrzuski","given":"Thomas J.","affiliations":[],"preferred":false,"id":163757,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dunn, Bernard","contributorId":61423,"corporation":false,"usgs":true,"family":"Dunn","given":"Bernard","email":"","affiliations":[],"preferred":false,"id":163758,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11791,"text":"ofr77418 - 1977 - Water resources of the Weiser River basin, west-central Idaho","interactions":[{"subject":{"id":11791,"text":"ofr77418 - 1977 - Water resources of the Weiser River basin, west-central Idaho","indexId":"ofr77418","publicationYear":"1977","noYear":false,"title":"Water resources of the Weiser River basin, west-central Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":70047715,"text":"70047715 - 1977 - Water resources of the Weiser River basin, west-central Idaho","indexId":"70047715","publicationYear":"1977","noYear":false,"title":"Water resources of the Weiser River basin, west-central Idaho"},"id":1}],"supersededBy":{"id":70047715,"text":"70047715 - 1977 - Water resources of the Weiser River basin, west-central Idaho","indexId":"70047715","publicationYear":"1977","noYear":false,"title":"Water resources of the Weiser River basin, west-central Idaho"},"lastModifiedDate":"2013-08-20T10:35:57","indexId":"ofr77418","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-418","title":"Water resources of the Weiser River basin, west-central Idaho","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77418","usgsCitation":"Young, H., Harenberg, W.A., and Seitz, H.R., 1977, Water resources of the Weiser River basin, west-central Idaho: U.S. Geological Survey Open-File Report 77-418, 92, [96] leaves :ill., maps ;40 cm.; (188 p. - PGS), https://doi.org/10.3133/ofr77418.","productDescription":"92, [96] leaves :ill., maps ;40 cm.; (188 p. - PGS)","costCenters":[],"links":[{"id":144798,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db6985e2","contributors":{"authors":[{"text":"Young, H.W.","contributorId":68278,"corporation":false,"usgs":true,"family":"Young","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":163738,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harenberg, William A.","contributorId":31773,"corporation":false,"usgs":true,"family":"Harenberg","given":"William","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":163736,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Seitz, Harold R.","contributorId":61814,"corporation":false,"usgs":true,"family":"Seitz","given":"Harold","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":163737,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":11784,"text":"ofr77725 - 1977 - Geologic, radiometric, and mineralogic maps and underground workings of the Schwartzwalder uranium mine and area, Jefferson County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:34","indexId":"ofr77725","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-725","title":"Geologic, radiometric, and mineralogic maps and underground workings of the Schwartzwalder uranium mine and area, Jefferson County, Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77725","usgsCitation":"Young, E.J., 1977, Geologic, radiometric, and mineralogic maps and underground workings of the Schwartzwalder uranium mine and area, Jefferson County, Colorado: U.S. Geological Survey Open-File Report 77-725, ii, 38 leaves :maps ;28 cm.; 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