{"pageNumber":"2317","pageRowStart":"57900","pageSize":"25","recordCount":68867,"records":[{"id":8442,"text":"ofr77275 - 1977 - Preliminary study of subsurface wastewater movement in and near Grand Teton National Park, Wyoming, through October 1976","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr77275","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":"77-275","title":"Preliminary study of subsurface wastewater movement in and near Grand Teton National Park, Wyoming, through October 1976","docAbstract":"Investigations were made by the U.S. Geological Survey in cooperation with Teton County, Wyoming and the National Park Service to determine the effects on nearby lakes and streams of percolating wastewater effluent at three sites in and near Grand Teton National Park. Observation wells were drilled at two of the sites, and water samples were collected from the wells. Sites were established on selected streams to collect water samples and to measure streamflow. Sufficient data have not been collected at this time to determine in detail the baseline quality of water in the selected streams or the rate, direction, and velocity of movement of percolating effluents. However, theoretical concepts and data collected to date suggest that effluent percolating near Colter Bay Village is most likely moving westward and southwestward toward Swan Lake and Colter Bay. Effluent percolating near Moose is most likely moving southeastward and southward toward the Snake River. Effluents near Flagg Ranch and Huckleberry Hot Springs probably discharge into the Snake River and Polecat Creek, but the amounts are small. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77275","usgsCitation":"Cox, E.R., 1977, Preliminary study of subsurface wastewater movement in and near Grand Teton National Park, Wyoming, through October 1976: U.S. Geological Survey Open-File Report 77-275, v, 35 leaves :ill., maps ;28 cm., https://doi.org/10.3133/ofr77275.","productDescription":"v, 35 leaves :ill., maps ;28 cm.","costCenters":[],"links":[{"id":140486,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0275/report-thumb.jpg"},{"id":36007,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0275/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aabe4b07f02db669fea","contributors":{"authors":[{"text":"Cox, Edward Riley","contributorId":40966,"corporation":false,"usgs":true,"family":"Cox","given":"Edward","email":"","middleInitial":"Riley","affiliations":[],"preferred":false,"id":157722,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8909,"text":"ofr77128 - 1977 - Quality of surface and ground waters, Yakima Indian Reservation, Washington, 1973-74","interactions":[],"lastModifiedDate":"2022-01-13T16:07:29.178647","indexId":"ofr77128","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":"77-128","title":"Quality of surface and ground waters, Yakima Indian Reservation, Washington, 1973-74","docAbstract":"<p>This report describes the quality of the surface and ground waters of the Yakima Indian Reservation in south-central Washington, during the period November 1973-October 1974. </p><p>The average dissolved-solids concentrations ranged from 48 to 116 mg/L (milligrams per liter) in the mountain streams, and from 88 to 372 mg/L in the lowland streams, drains, and a canal. All the mountain streams contain soft water (classified as 0-60 mg/L hardness as CaC03), and the lowland streams, drains, and canal contain soft to very hard water (more than 180 mg/L hardness as CaC03). The water is generally of suitable quality for irrigation, and neither salinity nor sodium hazards are a problem in waters from any of the streams studied. </p><p>The specific conductance of water from the major aquifers ranged from 20 to 1 ,540 micromhos. Ground water was most dilute in mineral content in the Klickitat River basin and most concentrated in part of the Satus Creek basin. The ground water in the Satus Creek basin with the most concentrated mineral content also contained the highest percentage composition of sulfate, chloride, and nitrate. For drinking water, the nitrate-nitrogen concentrations exceeded the U.S. Public Health Service 's recommended limit of 10 mg/L over an area of several square miles, with a maximum observed concentration of 170 mg/L. (Woodard-USGS).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77128","collaboration":"Prepared in cooperation with the Yakima Tribal Council","usgsCitation":"Fretwell, M.O., 1977, Quality of surface and ground waters, Yakima Indian Reservation, Washington, 1973-74: U.S. Geological Survey Open-File Report 77-128, Report: ix, 215 p.; 3 Tables, https://doi.org/10.3133/ofr77128.","productDescription":"Report: ix, 215 p.; 3 Tables","costCenters":[],"links":[{"id":141749,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0128/report-thumb.jpg"},{"id":394311,"rank":4,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1977/0128/table-5.pdf","text":"Table 5","linkFileType":{"id":1,"text":"pdf"}},{"id":394310,"rank":3,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1977/0128/table-4.pdf","text":"Table 4","linkFileType":{"id":1,"text":"pdf"}},{"id":394312,"rank":5,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1977/0128/table-6.pdf","text":"Table 6","linkFileType":{"id":1,"text":"pdf"}},{"id":394309,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0128/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","otherGeospatial":"Yakima Indian Reservation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.39343261718749,\n              45.867062714815475\n            ],\n            [\n              -119.86633300781249,\n              45.867062714815475\n            ],\n            [\n              -119.86633300781249,\n              46.61548796222358\n            ],\n            [\n              -121.39343261718749,\n              46.61548796222358\n            ],\n            [\n              -121.39343261718749,\n              45.867062714815475\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8ee4b07f02db6549bc","contributors":{"authors":[{"text":"Fretwell, M. O.","contributorId":50518,"corporation":false,"usgs":true,"family":"Fretwell","given":"M.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":158531,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9917,"text":"ofr77771 - 1977 - Fluctuations of ground-water levels in Lee County, Florida, in 1976 water year","interactions":[],"lastModifiedDate":"2012-02-02T00:06:29","indexId":"ofr77771","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":"77-771","title":"Fluctuations of ground-water levels in Lee County, Florida, in 1976 water year","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77771","usgsCitation":"La Rose, H.R., 1977, Fluctuations of ground-water levels in Lee County, Florida, in 1976 water year: U.S. Geological Survey Open-File Report 77-771, vii, 98 leaves :ill., map ;27 cm.; (94 p. - PGS), https://doi.org/10.3133/ofr77771.","productDescription":"vii, 98 leaves :ill., map ;27 cm.; (94 p. - PGS)","costCenters":[],"links":[{"id":144203,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de7b5","contributors":{"authors":[{"text":"La Rose, Henry R.","contributorId":76313,"corporation":false,"usgs":true,"family":"La Rose","given":"Henry","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":160508,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11138,"text":"ofr77776 - 1977 - The Pierre Shale, northern Great Plains; a potential isolation medium for radioactive waste","interactions":[],"lastModifiedDate":"2022-02-09T21:09:36.914496","indexId":"ofr77776","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":"77-776","title":"The Pierre Shale, northern Great Plains; a potential isolation medium for radioactive waste","docAbstract":"The purpose of this reconnaissance is to assess the potential of the Pierre Shale, of Late Cretaceous age, as a possible isolation medium for radioactive wastes. The regional stratigraphic and structural setting of the Pierre Shale in the northern Great Plains is summarized from subsurface data. \r\n\r\nGeologic attributes mapped and employed in the identification of areas warranting further evaluation are: depth to the base of the Pierre Shale, shale thickness, overburden thickness, lithology and mineralogy of the shale, and penetrations by oil and gas wells. Three areas emerge as most favorable; each may contain many potential disposal sites. These large geologic study areas are further described on the basis of general structural and seismic considerations and are compared with respect to topography and mineral and water resources. \r\n\r\nA large area in west-central South Dakota is recommended for extensive further study. A smaller area in northeastern Colorado also may warrant additional investigation. A relatively small area in north-central North Dakota is also delineated, but currently is not proposed for further studies.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77776","usgsCitation":"Shurr, G.W., 1977, The Pierre Shale, northern Great Plains; a potential isolation medium for radioactive waste: U.S. Geological Survey Open-File Report 77-776, ii, 27 p., https://doi.org/10.3133/ofr77776.","productDescription":"ii, 27 p.","costCenters":[],"links":[{"id":38902,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0776/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":395730,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74784.htm"},{"id":142465,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0776/report-thumb.jpg"}],"country":"United States","state":"Colorado, Kansas, Montana, Nebraska, North Dakota, South Dakota, Wyoming","otherGeospatial":"Great Plains, Pierre Shale","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105,\n              39\n            ],\n            [\n              -98,\n              39\n            ],\n            [\n              -98,\n              49\n            ],\n            [\n              -105,\n              49\n            ],\n            [\n              -105,\n              39\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67adfd","contributors":{"authors":[{"text":"Shurr, George W.","contributorId":78741,"corporation":false,"usgs":true,"family":"Shurr","given":"George","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":162607,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8938,"text":"ofr77261 - 1977 - Trap-efficiency investigation, Bernalillo Floodwater Retarding Reservoir No. 1 (Piedra Lisa Arroyo) near Bernalillo, New Mexico, water years 1956-1974","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr77261","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":"77-261","title":"Trap-efficiency investigation, Bernalillo Floodwater Retarding Reservoir No. 1 (Piedra Lisa Arroyo) near Bernalillo, New Mexico, water years 1956-1974","docAbstract":"The U.S. Geological Survey, in cooperation with the U.S. Soil Conservation Service, began an investigation of sedimentation of Bernalillo Floodwater Retarding Reservoir No. 1 (Piedra Lisa Arroyo) near Bernalillo, New Mexico in 1956. This investigation was part of a nationwide investigation of the trap efficiency of detention reservoirs. Reservoirs No. 1 is normally a dry reservoir and runoff from the 10.6 sq km drainage area generally occurs from high-intensity summer thundershowers. The mesa area of the drainage basin was treated to prevent erosion and gullying and to retard rapid runoff of rainfall. The land treatment consisted of pits, terraces, seeding, and restricted grazing. The total outflow recorded for the period of record (July 19, 1956 to June 30, 1974) was 133 acre-feet, yielding 1 ,439 tons of sediment. Over 99 percent of the coarse sediments and a high percentage of the silts and clays were deposited in the reservoir before reaching the outflow pipe. The determined trap efficiency of Reservoir No. 1 was 96 percent for the period of record. (Woordard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77261","usgsCitation":"Funderburg, D., 1977, Trap-efficiency investigation, Bernalillo Floodwater Retarding Reservoir No. 1 (Piedra Lisa Arroyo) near Bernalillo, New Mexico, water years 1956-1974: U.S. Geological Survey Open-File Report 77-261, vi, 43 p. :ill., graphs ;28 cm.; (52 p. - PGS), https://doi.org/10.3133/ofr77261.","productDescription":"vi, 43 p. :ill., graphs ;28 cm.; (52 p. - PGS)","costCenters":[],"links":[{"id":141199,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0261/report-thumb.jpg"},{"id":36545,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0261/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ce4b07f02db626b84","contributors":{"authors":[{"text":"Funderburg, D.E.","contributorId":79101,"corporation":false,"usgs":true,"family":"Funderburg","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":158590,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8945,"text":"ofr77413 - 1977 - Development of ground water in the Houston District, Texas, 1970-74","interactions":[{"subject":{"id":8945,"text":"ofr77413 - 1977 - Development of ground water in the Houston District, Texas, 1970-74","indexId":"ofr77413","publicationYear":"1977","noYear":false,"title":"Development of ground water in the Houston District, Texas, 1970-74"},"predicate":"SUPERSEDED_BY","object":{"id":70047612,"text":"70047612 - 1980 - Development of Ground Water in the Houston District, Texas, 1970-1974","indexId":"70047612","publicationYear":"1980","noYear":false,"title":"Development of Ground Water in the Houston District, Texas, 1970-1974"},"id":1}],"supersededBy":{"id":70047612,"text":"70047612 - 1980 - Development of Ground Water in the Houston District, Texas, 1970-1974","indexId":"70047612","publicationYear":"1980","noYear":false,"title":"Development of Ground Water in the Houston District, Texas, 1970-1974"},"lastModifiedDate":"2016-08-10T16:41:26","indexId":"ofr77413","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":"77-413","title":"Development of ground water in the Houston District, Texas, 1970-74","docAbstract":"<p>Total withdrawals of ground water in the Houston district, Texas , increased 9 percent from about 488 million gallons per day in 1970 to about 532 million gallons per day in 1974. The average annual rate of increase from 1960 to 1969 was about 6.3 percent. During 1970-74, increases in pumpage occurred in the Houston, Katy, and NASA areas; decreases occurred in the Pasadena and Alta Loma areas; and the pumpage in the Baytown-La Porte and Texas City areas remained almost constant. Water levels continued to decline throughout the district during 1970-74, but the rate of decline generally was not as great as in previous years. The greatest declines in the past several years were in the Houston area, but the center of decline is still in the Pasadena and Baytown-La Porte areas. The decrease in the rate of decline suggests that the aquifers in the Houston district could support the amount of pumping during 1970-74 with little, if any , further decline. Although saltwater encroachment has probably occurred in the district, particularly in Galveston County, no large increases in chloride were measured at the monitoring points. (Woodard-USGS)</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77413","usgsCitation":"Gabrysch, R., 1977, Development of ground water in the Houston District, Texas, 1970-74: U.S. Geological Survey Open-File Report 77-413, v, 44 leaves, [21] leaves of plates (some fold.) :ill., graphs, maps (some fold.) ;28 cm.; (55 p., 1 sheet, scale 1:275,000 - PGS), https://doi.org/10.3133/ofr77413.","productDescription":"v, 44 leaves, [21] leaves of plates (some fold.) :ill., graphs, maps (some fold.) ;28 cm.; (55 p., 1 sheet, scale 1:275,000 - PGS)","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":141121,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"275000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65df24","contributors":{"authors":[{"text":"Gabrysch, R.K.","contributorId":105691,"corporation":false,"usgs":true,"family":"Gabrysch","given":"R.K.","affiliations":[],"preferred":false,"id":158603,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9342,"text":"ofr77148 - 1977 - Analog-model analysis of effects of waste-water management on the ground-water reservoir in Nassau and Suffolk counties, New York; Report III: Reduction and redistribution of ground-water pumpage","interactions":[],"lastModifiedDate":"2012-02-02T00:06:24","indexId":"ofr77148","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":"77-148","title":"Analog-model analysis of effects of waste-water management on the ground-water reservoir in Nassau and Suffolk counties, New York; Report III: Reduction and redistribution of ground-water pumpage","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77148","usgsCitation":"Harbaugh, A.W., and Reilly, T.E., 1977, Analog-model analysis of effects of waste-water management on the ground-water reservoir in Nassau and Suffolk counties, New York; Report III: Reduction and redistribution of ground-water pumpage: U.S. Geological Survey Open-File Report 77-148, 24 leaves :8 maps (6 fold.) ;33 cm.; (23 p., 6 sheets, scale125,000 - PGS), https://doi.org/10.3133/ofr77148.","productDescription":"24 leaves :8 maps (6 fold.) ;33 cm.; (23 p., 6 sheets, scale125,000 - PGS)","costCenters":[],"links":[{"id":143037,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"25000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683ac1","contributors":{"authors":[{"text":"Harbaugh, Arlen W. harbaugh@usgs.gov","contributorId":426,"corporation":false,"usgs":true,"family":"Harbaugh","given":"Arlen","email":"harbaugh@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":159507,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reilly, Thomas E. tereilly@usgs.gov","contributorId":1660,"corporation":false,"usgs":true,"family":"Reilly","given":"Thomas","email":"tereilly@usgs.gov","middleInitial":"E.","affiliations":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":159508,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":15702,"text":"ofr77460 - 1977 - A water-quality assessment of the Northeast Creek and Desper Creek watersheds: South Anna River basin, Louisa County, Virginia","interactions":[],"lastModifiedDate":"2019-08-26T16:00:10","indexId":"ofr77460","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":"77-460","title":"A water-quality assessment of the Northeast Creek and Desper Creek watersheds: South Anna River basin, Louisa County, Virginia","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr77460","usgsCitation":"Rogers, S.M., 1977, A water-quality assessment of the Northeast Creek and Desper Creek watersheds: South Anna River basin, Louisa County, Virginia: U.S. Geological Survey Open-File Report 77-460, 38 p., https://doi.org/10.3133/ofr77460.","productDescription":"38 p.","costCenters":[],"links":[{"id":366942,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0460/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148374,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0460/report-thumb.jpg"}],"country":"United States","state":"Virginia","county":"Louisa County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-77.96,38.1192],[-77.9559,38.1183],[-77.9524,38.1178],[-77.9477,38.1191],[-77.9436,38.1195],[-77.9367,38.1162],[-77.9285,38.1156],[-77.9174,38.1169],[-77.9145,38.1164],[-77.9087,38.1118],[-77.9006,38.1094],[-77.8929,38.1116],[-77.8894,38.112],[-77.8749,38.1072],[-77.8626,38.1057],[-77.8597,38.1039],[-77.8551,38.1006],[-77.8493,38.1006],[-77.8452,38.1014],[-77.8416,38.1054],[-77.8381,38.1058],[-77.8157,38.0874],[-77.8117,38.0801],[-77.8077,38.0782],[-77.7919,38.078],[-77.785,38.0752],[-77.7821,38.0715],[-77.784,38.0652],[-77.7823,38.0634],[-77.7638,38.0531],[-77.7592,38.0494],[-77.7545,38.0498],[-77.751,38.0525],[-77.7481,38.0516],[-77.7458,38.0488],[-77.7467,38.0361],[-77.7481,38.0257],[-77.7464,38.0248],[-77.7446,38.0252],[-77.7416,38.0297],[-77.7386,38.0324],[-77.7351,38.0323],[-77.7304,38.0313],[-77.7299,38.0286],[-77.7306,38.0236],[-77.7289,38.0223],[-77.7225,38.0235],[-77.7201,38.0226],[-77.719,38.0199],[-77.711,38.0134],[-77.6999,38.0123],[-77.6936,38.0081],[-77.6878,38.0081],[-77.8004,37.7332],[-77.8332,37.754],[-77.8907,37.7598],[-77.8947,37.7621],[-77.906,37.7794],[-77.9103,37.7931],[-77.917,37.8068],[-77.9465,37.8452],[-77.9923,37.8572],[-78.0059,37.8745],[-78.0417,37.8936],[-78.0631,37.9056],[-78.1146,37.9257],[-78.1407,37.9364],[-78.1609,37.9462],[-78.1702,37.9508],[-78.1731,37.9513],[-78.1859,37.9519],[-78.1964,37.9538],[-78.2068,37.9584],[-78.2131,37.9639],[-78.2211,37.9763],[-78.2234,37.9772],[-78.2589,37.9866],[-78.2908,37.9987],[-78.3058,38.007],[-78.2552,38.0636],[-78.2253,38.1046],[-78.2079,38.1307],[-78.1914,38.1341],[-78.1692,38.1339],[-78.1627,38.1375],[-78.1522,38.1382],[-78.1486,38.14],[-78.1444,38.1445],[-78.1427,38.1445],[-78.1351,38.1412],[-78.1264,38.1407],[-78.1187,38.1415],[-78.1146,38.1446],[-78.1133,38.1496],[-78.1051,38.1522],[-78.094,38.1521],[-78.0899,38.1489],[-78.0772,38.1433],[-78.0713,38.1428],[-78.0661,38.1418],[-78.0562,38.1381],[-78.0393,38.1356],[-78.0293,38.1382],[-78.024,38.1404],[-78.0199,38.1404],[-78.0146,38.138],[-78.0094,38.1362],[-78.0018,38.1365],[-77.9983,38.136],[-77.9948,38.1333],[-77.9845,38.1227],[-77.9787,38.1208],[-77.9699,38.1221],[-77.96,38.1192]]]},\"properties\":{\"name\":\"Louisa\",\"state\":\"VA\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4ecb","contributors":{"authors":[{"text":"Rogers, Stanley M.","contributorId":37761,"corporation":false,"usgs":true,"family":"Rogers","given":"Stanley","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":171573,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11605,"text":"ofr77346 - 1977 - Field determination of vertical permeability to air in the unsaturated zone","interactions":[{"subject":{"id":11605,"text":"ofr77346 - 1977 - Field determination of vertical permeability to air in the unsaturated zone","indexId":"ofr77346","publicationYear":"1977","noYear":false,"title":"Field determination of vertical permeability to air in the unsaturated zone"},"predicate":"SUPERSEDED_BY","object":{"id":6515,"text":"pp1051 - 1978 - Field determination of vertical permeability to air in the unsaturated zone","indexId":"pp1051","publicationYear":"1978","noYear":false,"title":"Field determination of vertical permeability to air in the unsaturated zone"},"id":1}],"supersededBy":{"id":6515,"text":"pp1051 - 1978 - Field determination of vertical permeability to air in the unsaturated zone","indexId":"pp1051","publicationYear":"1978","noYear":false,"title":"Field determination of vertical permeability to air in the unsaturated zone"},"lastModifiedDate":"2016-08-10T16:40:45","indexId":"ofr77346","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":"77-346","title":"Field determination of vertical permeability to air in the unsaturated zone","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/ofr77346","usgsCitation":"Weeks, E.P., 1977, Field determination of vertical permeability to air in the unsaturated zone: U.S. Geological Survey Open-File Report 77-346, v, 92 leaves :ill. ;27 cm.; (171 p. - PGS), https://doi.org/10.3133/ofr77346.","productDescription":"v, 92 leaves :ill. ;27 cm.; (171 p. - PGS)","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":144646,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae9df","contributors":{"authors":[{"text":"Weeks, Edwin P. epweeks@usgs.gov","contributorId":2576,"corporation":false,"usgs":true,"family":"Weeks","given":"Edwin","email":"epweeks@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":163429,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11130,"text":"ofr7761 - 1977 - Geology and ground water in Door County, Wisconsin, with emphasis on contamination potential in the Silurian dolomite","interactions":[{"subject":{"id":11130,"text":"ofr7761 - 1977 - Geology and ground water in Door County, Wisconsin, with emphasis on contamination potential in the Silurian dolomite","indexId":"ofr7761","publicationYear":"1977","noYear":false,"title":"Geology and ground water in Door County, Wisconsin, with emphasis on contamination potential in the Silurian dolomite"},"predicate":"SUPERSEDED_BY","object":{"id":2679,"text":"wsp2047 - 1978 - Geology and ground water in Door County, Wisconsin, with emphasis on contamination potential in the Silurian dolomite","indexId":"wsp2047","publicationYear":"1978","noYear":false,"title":"Geology and ground water in Door County, Wisconsin, with emphasis on contamination potential in the Silurian dolomite"},"id":1}],"supersededBy":{"id":2679,"text":"wsp2047 - 1978 - Geology and ground water in Door County, Wisconsin, with emphasis on contamination potential in the Silurian dolomite","indexId":"wsp2047","publicationYear":"1978","noYear":false,"title":"Geology and ground water in Door County, Wisconsin, with emphasis on contamination potential in the Silurian dolomite"},"lastModifiedDate":"2012-02-02T00:06:24","indexId":"ofr7761","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":"77-61","title":"Geology and ground water in Door County, Wisconsin, with emphasis on contamination potential in the Silurian dolomite","docAbstract":"Door County, a recreational and fruit-growing area bordering Lake Michigan in northeastern Wisconsin, has had a long history of ground-water contamination from surface and near-surface sources. Contamination is most severe in late summer when fruit-canning operations and the influx of tourists create additional wastes. Silurian dolomite is the upper bedrock unit in the county and yields generally adequate supplies of very hard water with locally objectionable concentrations of iron and nitrate. Thin soil cover and well-fractured dolomitic bedrock give easy entry to ground-water contaminants throughout large parts of Door County. Many contaminants enter the dolomite by surface or near-surface seepage. There is little attenuation of contamination concentrations in the well-jointed dolomite, and contaminants may travel long distances underground in a relatively short time. The major source of ground-water contamination is bacteria, from individual waste-disposal systems, agricultural, industrial, and municipal wastes. Areas of the county underlain by contaminated zones include only a small percentage of the total ground-water system and are separated by large volumes of ground water free of contamination. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr7761","usgsCitation":"Sherrill, M.G., 1977, Geology and ground water in Door County, Wisconsin, with emphasis on contamination potential in the Silurian dolomite: U.S. Geological Survey Open-File Report 77-61, 92 leaves :8 ill., 13 maps (some fold.) ;28 cm.; (6 sheets, scale 1:62,500 - PGS), https://doi.org/10.3133/ofr7761.","productDescription":"92 leaves :8 ill., 13 maps (some fold.) ;28 cm.; (6 sheets, scale 1:62,500 - PGS)","costCenters":[],"links":[{"id":143537,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"62500","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db68428a","contributors":{"authors":[{"text":"Sherrill, Marvin G.","contributorId":91469,"corporation":false,"usgs":true,"family":"Sherrill","given":"Marvin","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":162598,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8974,"text":"ofr77219 - 1977 - Artificial recharge for subsidence abatement at the NASA-Johnson Space Center, Phase I","interactions":[],"lastModifiedDate":"2017-06-14T13:16:24","indexId":"ofr77219","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":"77-219","title":"Artificial recharge for subsidence abatement at the NASA-Johnson Space Center, Phase I","docAbstract":"<p>Regional decline of aquifer head due to ground-water withdrawal in the Houston area has caused extensive land-surface subsidence. The NASA-Johnson Space Center (NASA-JSC) in southeastern Harris County, Texas, was about 13 to 19 feet above mean sea level in 1974 and sinking at a rate of more than 0.2 foot per year. NASA-JSC officials, concerned about the hurricane flooding hazard, requested the U.S. Geological Survey to study the feasibility of artificially recharging the aquifers for subsidence abatement. Hydrologic digital models were developed for theoretical determinations of quantities of water needed, under various well-array plans, for artificial recharge of the Chicot and Evangeline aquifers in order to halt the local subsidence at NASA-JSC. The programs for the models were developed for analysis of three-dimensional ground-water flow. Total injection rates of between 2,000 and 14,000 gallons per minute under three general well-array plans were determined for a range of residual clay pore pressures of 10 to 70 feet of hydraulic head. The space distributions of the resultant hydraulic heads, illustrated for injection rates of 3,600 and 8 ,400 gallons per minute, indicated that, for the same rate, increasing the number and spread of the injection locations reduces the head gradients within NASA-JSC. (Woodard-USGS)</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77219","usgsCitation":"Garza, S., 1977, Artificial recharge for subsidence abatement at the NASA-Johnson Space Center, Phase I: U.S. Geological Survey Open-File Report 77-219, 77 p., https://doi.org/10.3133/ofr77219.","productDescription":"77 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":142383,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672c35","contributors":{"authors":[{"text":"Garza, Sergio","contributorId":88713,"corporation":false,"usgs":true,"family":"Garza","given":"Sergio","email":"","affiliations":[],"preferred":false,"id":158648,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9634,"text":"ofr77257 - 1977 - Water table in the surficial aquifer and potentiometric surface of the Floridan Aquifer in selected well fields, west-central Florida, May 1976","interactions":[],"lastModifiedDate":"2012-02-02T00:06:22","indexId":"ofr77257","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":"77-257","title":"Water table in the surficial aquifer and potentiometric surface of the Floridan Aquifer in selected well fields, west-central Florida, May 1976","docAbstract":"The water table in the surficial aquifer (sand) and the potentiometric surface of the Floridan aquifer (limestone) in a 1,200-square-mile area in west-central Florida are mapped semiannually by the U.S. Geological Survey. Maps are prepared each May and September to coincide with seasonal low and high ground-water levels. The mapped area contains nine producing well fields which supplied 92.8 million gallons on May 12, 1976 to municipalities along the Gulf Coast. This pumpage came from the Floridan aquifer, the major aquifer in the State of Florida. The effect of well-field withdrawals is shown on the maps as cones of depression in both the potentiometric and water-table surfaces. The May 1976 maps indicate that water levels have declined below sea level in some areas. The decline results from reduced recharge during the dry spring combined with an increase in pumpage for lawn irrigation.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77257","usgsCitation":"Hutchinson, C.B., and Mills, L.R., 1977, Water table in the surficial aquifer and potentiometric surface of the Floridan Aquifer in selected well fields, west-central Florida, May 1976: U.S. Geological Survey Open-File Report 77-257, 14 leaves :4 maps (fold.) ;29 cm.; scale 1:24,000, https://doi.org/10.3133/ofr77257.","productDescription":"14 leaves :4 maps (fold.) ;29 cm.; scale 1:24,000","costCenters":[],"links":[{"id":143570,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0257/report-thumb.jpg"},{"id":37363,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0257/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37364,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0257/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37365,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0257/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37366,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0257/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37367,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0257/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee413","contributors":{"authors":[{"text":"Hutchinson, C. B.","contributorId":94655,"corporation":false,"usgs":true,"family":"Hutchinson","given":"C.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":160025,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mills, L. R.","contributorId":26281,"corporation":false,"usgs":true,"family":"Mills","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":160024,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10491,"text":"ofr77634 - 1977 - Aquatic organisms from selected sites along the Trans-Alaska Pipeline corridor, September 1970 to September 1972: supplement","interactions":[],"lastModifiedDate":"2012-02-02T00:06:40","indexId":"ofr77634","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":"77-634","title":"Aquatic organisms from selected sites along the Trans-Alaska Pipeline corridor, September 1970 to September 1972: supplement","docAbstract":"This report is a supplement to earlier preconstruction studies of benthic invertebrates and water quality at selected sites along the trans-Alaska pipeline corridor. Some of the problems which arose during the course of data collection and analysis are discussed. Benthic invertebrate abundance and community-structure data are presented for 20 sites along the trans-Alaska pipeline for the period September 1970 to September 1972. In addition, a list of invertebrate taxa identified to various taxonomic levels is given for 42 sites along the pipeline. (See also W74-08369) (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77634","usgsCitation":"Nauman, J.W., and Kernodle, D.R., 1977, Aquatic organisms from selected sites along the Trans-Alaska Pipeline corridor, September 1970 to September 1972: supplement: U.S. Geological Survey Open-File Report 77-634, iii, 55 leaves :map ;27 cm.; (59 p. - PGS), https://doi.org/10.3133/ofr77634.","productDescription":"iii, 55 leaves :map ;27 cm.; (59 p. - PGS)","costCenters":[],"links":[{"id":145684,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0634/report-thumb.jpg"},{"id":38351,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0634/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679fdd","contributors":{"authors":[{"text":"Nauman, Jon W.","contributorId":56232,"corporation":false,"usgs":true,"family":"Nauman","given":"Jon","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":161486,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kernodle, Donald R.","contributorId":63003,"corporation":false,"usgs":true,"family":"Kernodle","given":"Donald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":161487,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10490,"text":"ofr77791 - 1977 - Program objectives for the National Water Data Exchange (NAWDEX) for fiscal year 1978","interactions":[],"lastModifiedDate":"2012-02-02T00:06:40","indexId":"ofr77791","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":"77-791","title":"Program objectives for the National Water Data Exchange (NAWDEX) for fiscal year 1978","docAbstract":"This report presents the program objectives for the National Water Data Exchange (Nawdex) for Fiscal Year 1978, October 1, 1977 to September 30, 1978. Objectives covered include Nawdex mambership, membership participation, Nawdex services, identification of sources of water data, the indexing of water data, systems development and implementation, training, recommended standards for the handling and exchange of water data, and program management. The report provides advance information on Nawdex activities, thereby, allowing the activities to be better integrated into the planning and operation of programs of member organizations. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey]","doi":"10.3133/ofr77791","usgsCitation":"Edwards, M.D., 1977, Program objectives for the National Water Data Exchange (NAWDEX) for fiscal year 1978: U.S. Geological Survey Open-File Report 77-791, v. ;28 cm.; (13 p. - PGS), https://doi.org/10.3133/ofr77791.","productDescription":"v. ;28 cm.; (13 p. - PGS)","costCenters":[],"links":[{"id":94977,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0791/report.pdf","size":"646","linkFileType":{"id":1,"text":"pdf"}},{"id":145683,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0791/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e0f3","contributors":{"authors":[{"text":"Edwards, Melvin D.","contributorId":94305,"corporation":false,"usgs":true,"family":"Edwards","given":"Melvin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":161485,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8217,"text":"ofr77278 - 1977 - A preliminary appraisal of the Garber-Wellington Aquifer, southern Logan and northern Oklahoma counties, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:06:08","indexId":"ofr77278","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":"77-278","title":"A preliminary appraisal of the Garber-Wellington Aquifer, southern Logan and northern Oklahoma counties, Oklahoma","docAbstract":"The Garber-Wellington aquifer, which dips westward at 30 to 40 feet per mile, consists of about 900 feet of interbedded sandstone, shale, and siltstone. Sandstone comprises 35 to 75 percent of the aquifer and averages about 50 percent. Water-table conditions generally exist in the upper 200 feet in the outcrop area of the aquifer; semi-artesian or artesian conditions exist below a depth of 200 feet and beneath rocks of the Hennessey Group (predominantly shale) where the aquifer is fully saturated. Water containing more than 1,000 milligrams per liter dissolved solids occurs at various depths through the area. The altitude of the base of fresh water ranges from 250 feet above sea level in the south-central part of the area to 950 feet in the northwestern part. The thickness of the fresh-water zone ranges from less than 150 feet in the northern part of the area to about 850 feet in the southern part. The total amount of water stored in the fresh-water zone is estimated to be 21 million acre-feet based on specific yield of 0.20.\r\nMinimum recharge to the aquifer in 1975 is estimated to be 190 acre-feet per square mile or about 10 percent of the annual precipitation. Total minimum recharge to the aquifer in the study area in 1975 is estimated to be 129,000 acre-feet. Streams in the area are the principal means of ground-water discharge; the amount of discharge is essentially the same as recharge. The amount of groundwater used for municipal and rural water supply in 1975 is estimated to have been 5,000 acre-feet; a similar amount may have been used for industrial purposes. As a result of pumping, the potentiometric surface in 1975 had been lowered about 200 feet in the vicinity of Edmond and about 100 feet in the vicinity of Nichols Hills.\r\n\r\nChemical analyses of water from the aquifer indicates that hardness is greater in the upper part of the aquifer than in the lower part, and that sulfate, chloride, and dissolved solids increase with depth.\r\n\r\nReported yields of wells more than 250 feet deep range from 70 to 475 gallons per minute and average 240 gallons per minute. Potential well yields range from 225 gallons per minute when the fresh-water zone is 350 feet thick to about 550 gallons per minute where the fresh water zone is 850 feet thick. These estimates of potential yield are based on an available drawdown of half the thickness of the fresh-water zone and a specific capacity of 1.3 gallons per minute per foot.\r\n\r\nIntrusion of saline water into the fresh-water zone is a potential threat to water quality in the aquifer if the pressure head in the fresh-water zone is reduced sufficiently to allow upconing of saline water. One way to avoid the problem of upconing is by steady pumping at low rates from widely spaced wells; however, information required to determine pumping rates and well spacing is not available.\r\n\r\nFor proper aquifer management the distribution of wells and rates of withdrawals should be designed to capture maximum recharge to the ground-water system. This may be accomplished by developing regional ground-water gradients that are sufficiently large to move water to pumpage centers but not so steep as to cause upconing of saline water or excessive water-level declines.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77278","usgsCitation":"Carr, J.E., and Marcher, M.V., 1977, A preliminary appraisal of the Garber-Wellington Aquifer, southern Logan and northern Oklahoma counties, Oklahoma: U.S. Geological Survey Open-File Report 77-278, v, 23 p. :ill., maps (5 fold. in pocket) ;26 cm.; (49 p., 5 sheets - PGS), https://doi.org/10.3133/ofr77278.","productDescription":"v, 23 p. :ill., maps (5 fold. in pocket) ;26 cm.; (49 p., 5 sheets - PGS)","costCenters":[],"links":[{"id":141558,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0278/report-thumb.jpg"},{"id":35843,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0278/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35844,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0278/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35845,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0278/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35846,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0278/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35847,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0278/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35848,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0278/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a9072","contributors":{"authors":[{"text":"Carr, Jerry E.","contributorId":47758,"corporation":false,"usgs":true,"family":"Carr","given":"Jerry","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":157360,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marcher, Melvin V.","contributorId":11590,"corporation":false,"usgs":true,"family":"Marcher","given":"Melvin","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":157359,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10478,"text":"ofr77592 - 1977 - Geology of the Midnite uranium mine area, Washington — Maps, description, and interpretation","interactions":[],"lastModifiedDate":"2021-12-08T22:09:56.728257","indexId":"ofr77592","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":"77-592","title":"Geology of the Midnite uranium mine area, Washington — Maps, description, and interpretation","docAbstract":"<p>Bedrock geology of about 12 km<sup>2</sup> near the Midnite mine has been mapped at the surface, in mine exposures, and from drilling, at scales from 1:600 to 1:12,000 and is presented here at 1:12,000 to provide description of the setting of uranium deposits. Oldest rocks in the area are metapelitic and metacarbonate rocks of the Precambrian (Y) Togo Formation. The chief host for uranium deposits is graphitic and pyritic mica phyllite and muscovite schist. Ore also occurs in calc-silicate hornfels and marble at the western edge of a calcareous section about 1,150 m thick. Calcareous rocks of the Togo are probably older than the pelitic as they are interpreted to be near the axis of a broad anticline. The composition and structural position of the calcareous unit suggests correlation with less metamorphosed carbonate-bearing rocks of the Lower Wallace Formation, Belt Supergroup, about 200 km to the east. Basic sills intrusive into the Togo have been metamorphosed to amphibolite.</p><p> Unmetamorphosed rocks in the mine area are Cretaceous(?) and Eocene igneous rocks. Porphyritic quartz monzonite of Cretaceous age, part of the Loon Lake batholith, is exposed over one third of the mine area. It underlies the roof pendant of Precambrian rocks in which the Midnite mine occurs at depths of generally less than 300 m. The pluton is a two-mica granite and exhibits pegmatitic and aplitic textural features indicative of water saturation and pressure quenching. Eocene intrusive and extrusive rocks in the area provide evidence that the Eocene surface was only a short distance above the present uranium deposits. </p><p>Speculative hypotheses are presented for penesyngenetic, hydrothermal, and supergene modes of uranium emplacement. The Precambrian Stratigraphy, similar in age and pre-metamorphic lithology to that of rocks hosting large uranium deposits in Saskatchewan and Northern Territory, Australia, suggests the possibility of uranium accumulation along with diagenetic pyrite in carbonaceous muds in a marine shelf environment. This hypothesis is not favored by the author because there is no evidence for stratabound uranium such as high regional radioactivity in the Togo. A hydrothermal mode of uranium emplacement is supported by the close apparent ages of mineralization and plutonism, and by petrology of the pluton. I speculate that uranium may have become enriched in postmagmatic fluids at the top of the pluton, possibly by hydrothermal leaching of soluble uranium associated with magnetite, and diffused outward into metasedimentary wall rocks to create an aureole about 100 m thick containing about 100 ppm uranium. Chemistry of the hydrothermal process is not understood, but uranium does not appear to have been transported by an oxidizing fluid, and the fluid did not produce veining and alteration comparable to that of base-metal sulfide deposits. Uranium in the low-grade protore is believed to have been redistributed into permeable zones in the Tertiary to create ore grades. Geologic and isotopic ages of uranium mineralization, and the small volume of porphyritic quartz monzonite available for leaching, are not supportive of supergene emplacement of uranium.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77592","usgsCitation":"Nash, J.T., 1977, Geology of the Midnite uranium mine area, Washington — Maps, description, and interpretation: U.S. Geological Survey Open-File Report 77-592, Report: ii, 39 p.; 2 Plates: 15.00 × 20.00 inches and 16.00 × 17.00 inches, https://doi.org/10.3133/ofr77592.","productDescription":"Report: ii, 39 p.; 2 Plates: 15.00 × 20.00 inches and 16.00 × 17.00 inches","costCenters":[],"links":[{"id":392655,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14485.htm"},{"id":38343,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0592/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143959,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0592/report-thumb.jpg"},{"id":94974,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0592/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":94973,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0592/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"12000","country":"United States","state":"Washington","otherGeospatial":"Midnite uranium mine area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.118,\n              47.933\n            ],\n            [\n              -118.0670,\n              47.933\n            ],\n            [\n              -118.0670,\n              47.962\n            ],\n            [\n              -118.118,\n              47.962\n            ],\n            [\n              -118.118,\n              47.933\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e9da","contributors":{"authors":[{"text":"Nash, J. Thomas","contributorId":26306,"corporation":false,"usgs":true,"family":"Nash","given":"J.","email":"","middleInitial":"Thomas","affiliations":[],"preferred":false,"id":161468,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8228,"text":"ofr77408 - 1977 - Low-flow characteristics of the upper Flint River, Georgia","interactions":[],"lastModifiedDate":"2016-12-14T10:11:14","indexId":"ofr77408","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":"77-408","title":"Low-flow characteristics of the upper Flint River, Georgia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77408","usgsCitation":"Carter, R., 1977, Low-flow characteristics of the upper Flint River, Georgia: U.S. Geological Survey Open-File Report 77-408, ii, 10 p. :ill., map ;26 cm.; (15 p. - PGS), https://doi.org/10.3133/ofr77408.","productDescription":"ii, 10 p. :ill., map ;26 cm.; (15 p. - 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,{"id":10475,"text":"ofr77354 - 1977 - Biogeochemical prospecting for uranium with conifers: results from the Midnite Mine area, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:06:32","indexId":"ofr77354","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":"77-354","title":"Biogeochemical prospecting for uranium with conifers: results from the Midnite Mine area, Washington","docAbstract":"The ash of needles, cones, and duff from Ponderosa pine (Pinus ponderosa Laws) growing near uranium deposits of the Midnite mine, Stevens County, Wash., contain as much as 200 parts per million (ppm) uranium. Needle samples containing more than 10 ppm uranium define zones that correlate well with known uranium deposits or dumps. Dispersion is as much as 300 m but generally is less. Background is about 1 ppm. Tree roots are judged to be sampling ore, low-grade uranium halo, or ground water to a depth of about 15 m. Uptake of uranium by Douglas fir (Pseudotsuga menziesii (Mirb.) Franco) needles appears to be about the same as by Ponderosa pine needles. Cones and duff are generally enriched in uranium relate to needles. Needles, cones, and duff are recommended as easily collected, uncomplicated sample media for geochemical surveys. Samples can be analyzed by standard methods and total cost per sample kept to about $6.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77354","usgsCitation":"Nash, J.T., and Ward, F.N., 1977, Biogeochemical prospecting for uranium with conifers: results from the Midnite Mine area, Washington: U.S. Geological Survey Open-File Report 77-354, i, 20 leaves :maps (1 fold. in pocket) ;27 cm.; (23 p., 1 sheet - PGS), https://doi.org/10.3133/ofr77354.","productDescription":"i, 20 leaves :maps (1 fold. in pocket) ;27 cm.; (23 p., 1 sheet - PGS)","costCenters":[],"links":[{"id":143935,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0354/report-thumb.jpg"},{"id":38339,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0354/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38340,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0354/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625d18","contributors":{"authors":[{"text":"Nash, J. Thomas","contributorId":26306,"corporation":false,"usgs":true,"family":"Nash","given":"J.","email":"","middleInitial":"Thomas","affiliations":[],"preferred":false,"id":161463,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ward, Frederick Norville","contributorId":105698,"corporation":false,"usgs":true,"family":"Ward","given":"Frederick","email":"","middleInitial":"Norville","affiliations":[],"preferred":false,"id":161464,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9003,"text":"ofr77698 - 1977 - Comparative assessment of water use and environmental implications of coal slurry pipelines","interactions":[],"lastModifiedDate":"2012-02-02T00:06:28","indexId":"ofr77698","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":"77-698","title":"Comparative assessment of water use and environmental implications of coal slurry pipelines","docAbstract":"With other studies conducted by the U.S. Geological Survey of water use in the conversion and transportation of the West 's coal, an analysis of water use and environmental implications of coal-slurry pipeline transport is presented. Simulations of a hypothetical slurry pipeline of 1000-mile length transporting 12.5 million tons per year indicate that pipeline costs and energy requirements are quite sensitive to the coal-to-water ratio. For realistic water prices, the optimal ratio will not vary far from the 50/50 ratio by weight. In comparison to other methods of energy conversion and transport, coal-slurry pipeline utilize about 1/3 the amount of water required for coal gasification, and about 1/5 the amount required for on-site electrical generation. An analysis of net energy output from operating alternative energy transportation systems for the assumed conditions indicates that both slurry pipeline and rail shipment require approximately 4.5 percent of the potential electrical energy output of the coal transported, and high-voltage, direct-current transportation requires approximately 6.5 percent. The environmental impacts of the different transports options are so substantially different that a common basis for comparison does not exist. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77698","usgsCitation":"Palmer, R.N., James II, I., and Hirsch, R., 1977, Comparative assessment of water use and environmental implications of coal slurry pipelines: U.S. Geological Survey Open-File Report 77-698, iv, 29 p. :ill. ;28 cm.; (28 p. - PGS), https://doi.org/10.3133/ofr77698.","productDescription":"iv, 29 p. :ill. ;28 cm.; (28 p. - PGS)","costCenters":[],"links":[{"id":112911,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0698/report.pdf","size":"1183","linkFileType":{"id":1,"text":"pdf"}},{"id":144277,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0698/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae52a","contributors":{"authors":[{"text":"Palmer, Richard N.","contributorId":18372,"corporation":false,"usgs":true,"family":"Palmer","given":"Richard","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":158721,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"James II, I. C.","contributorId":91112,"corporation":false,"usgs":true,"family":"James II","given":"I. C.","affiliations":[],"preferred":false,"id":158723,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hirsch, R.M.","contributorId":58639,"corporation":false,"usgs":true,"family":"Hirsch","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":158722,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10464,"text":"ofr77314 - 1977 - Hydrologic maps and data in the Mimbres Basin, New Mexico","interactions":[],"lastModifiedDate":"2019-03-13T09:02:25","indexId":"ofr77314","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":"77-314","title":"Hydrologic maps and data in the Mimbres Basin, New Mexico","docAbstract":"<p>This report was prepared by the U.S. Geological Survey in cooperation with the New Mexico State Engineer Office and lists well and spring data, including well locations, water levels, well yields, and chemical analyses of well and spring water. Maps in the report show well locations, water-level contours, and water-level declines at a scale of 1:250,000. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77314","collaboration":"Prepared in cooperation with the Office of the New Mexico State Engineer","usgsCitation":"McLean, J.S., 1977, Hydrologic maps and data in the Mimbres Basin, New Mexico: U.S. Geological Survey Open-File Report 77-314, Report: 531 p.; 6 Plates: 24.85 x 30.66 inches or smaller, https://doi.org/10.3133/ofr77314.","productDescription":"Report: 531 p.; 6 Plates: 24.85 x 30.66 inches or smaller","costCenters":[],"links":[{"id":362024,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0314/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":362025,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1977/0314/figure-3.pdf","text":"Figure 3","linkFileType":{"id":1,"text":"pdf"}},{"id":362026,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1977/0314/figure-4.pdf","text":"Figure 4","linkFileType":{"id":1,"text":"pdf"}},{"id":362027,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1977/0314/figure-5.pdf","text":"Figure 5","linkFileType":{"id":1,"text":"pdf"}},{"id":362029,"rank":7,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1977/0314/figure-7.pdf","text":"Figure 7","linkFileType":{"id":1,"text":"pdf"}},{"id":362030,"rank":8,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1977/0314/figure-8.pdf","text":"Figure 8","linkFileType":{"id":1,"text":"pdf"}},{"id":145055,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0314/report-thumb.jpg"},{"id":362028,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1977/0314/figure-6.pdf","text":"Figure 6","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Mexico","otherGeospatial":"Mimbres Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.5,\n              31.781882156411022\n            ],\n            [\n              -107,\n              31.781882156411022\n            ],\n            [\n              -107,\n              33.15\n            ],\n            [\n              -108.5,\n              33.15\n            ],\n            [\n              -108.5,\n              31.781882156411022\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606bfb","contributors":{"authors":[{"text":"McLean, John S.","contributorId":102897,"corporation":false,"usgs":true,"family":"McLean","given":"John","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":161446,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12379,"text":"ofr77222 - 1977 - Water-resources investigations of the U.S. Geological Survey in Wyoming, October 1976 to September 1977","interactions":[],"lastModifiedDate":"2012-02-02T00:06:39","indexId":"ofr77222","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":"77-222","title":"Water-resources investigations of the U.S. Geological Survey in Wyoming, October 1976 to September 1977","language":"ENGLISH","doi":"10.3133/ofr77222","usgsCitation":"Boner, F.C., 1977, Water-resources investigations of the U.S. Geological Survey in Wyoming, October 1976 to September 1977: U.S. Geological Survey Open-File Report 77-222, v. :ill., maps. ;26 cm.; (58 p. - PGS), https://doi.org/10.3133/ofr77222.","productDescription":"v. :ill., maps. ;26 cm.; (58 p. - PGS)","costCenters":[],"links":[{"id":145515,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0222/report-thumb.jpg"},{"id":40614,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0222/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4e32","contributors":{"authors":[{"text":"Boner, F. C.","contributorId":32136,"corporation":false,"usgs":true,"family":"Boner","given":"F.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":166033,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9297,"text":"ofr76791 - 1977 - Use of water in Arkansas, 1975","interactions":[{"subject":{"id":9297,"text":"ofr76791 - 1977 - Use of water in Arkansas, 1975","indexId":"ofr76791","publicationYear":"1977","noYear":false,"title":"Use of water in Arkansas, 1975"},"predicate":"SUPERSEDED_BY","object":{"id":70047770,"text":"70047770 - 1977 - Use of water in Arkansas, 1975","indexId":"70047770","publicationYear":"1977","noYear":false,"title":"Use of water in Arkansas, 1975"},"id":1}],"supersededBy":{"id":70047770,"text":"70047770 - 1977 - Use of water in Arkansas, 1975","indexId":"70047770","publicationYear":"1977","noYear":false,"title":"Use of water in Arkansas, 1975"},"lastModifiedDate":"2013-08-22T14:42:56","indexId":"ofr76791","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":"76-791","title":"Use of water in Arkansas, 1975","language":"ENGLISH","publisher":"State of Arkansas, Arkansas Dept. of Commerce, Arkansas Geological Commission,","doi":"10.3133/ofr76791","usgsCitation":"Halberg, H.N., 1977, Use of water in Arkansas, 1975: U.S. Geological Survey Open-File Report 76-791, iv, 28 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr76791.","productDescription":"iv, 28 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":141223,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db6041ae","contributors":{"authors":[{"text":"Halberg, Henry Nicholas","contributorId":41804,"corporation":false,"usgs":true,"family":"Halberg","given":"Henry","email":"","middleInitial":"Nicholas","affiliations":[],"preferred":false,"id":159440,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11464,"text":"ofr77647 - 1977 - Ground-water resources of the North Beach Peninsula, Pacific County, Washington","interactions":[],"lastModifiedDate":"2019-05-10T13:38:39","indexId":"ofr77647","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":"77-647","title":"Ground-water resources of the North Beach Peninsula, Pacific County, Washington","docAbstract":"<p>The anticipated water demand of 425 million gallons per year for the North Beach Peninsula, Pacific County, Wash., can be met by properly developing the ground-water supplies of the area's water-table aquifer. Of the approximately 77 inches of precipitation on the peninsula, an estimated 23 inches is lost to evapotranspiration, and approximately 36 inches is discharged by the water-table aquifer into the ocean and bay. The remaining water either runs off the surface or is leaked to a deeper aquifer that ultimately discharges to the ocean. In some areas of the peninsula, particularly those that are low lying and covered with poorly permeable soils, runoff is promoted by an artificial drainage system developed to alleviate waterlogging. In these areas, it is estimated that natural discharge through the aquifer would be less than that of the artificial drainage system. By a conservative estimate, at least 12 inches of the water that discharges naturally through the aquifer is available for additional development. This quantity of water is approximately equivalent to 860,000 gallons per day or 320 million gallons per year per mile of peninsula length. Under specified idealized conditions wells spaced at least 1,000 feet apart along the major axis of the peninsula and pumped at average rates of no more than 80 gallons per minute would ensure that water-level declines do not exceed 6 feet near the wells and 1 foot at the shoreline, thereby preventing seawater intrusion. Lowering of the water table may be beneficial in reducing waterlogging problems, but care must be taken not to lower the levels near cranberry bogs, which require a shallow water table. Treatment of the otherwise good quality water for iron may be required, as about 75 percent of the well water sampled from the aquifer had iron concentrations in excess of limits recommended by the U.S. Environmental Protection Agency. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77647","collaboration":"Prepared in cooperation with the Pacific County Board of Commissioners and the State of Washington Department of Ecology","usgsCitation":"Tracy, J.V., 1977, Ground-water resources of the North Beach Peninsula, Pacific County, Washington: U.S. Geological Survey Open-File Report 77-647, vi, 45 p., https://doi.org/10.3133/ofr77647.","productDescription":"vi, 45 p.","costCenters":[],"links":[{"id":145091,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0647/report-thumb.jpg"},{"id":363673,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0647/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","county":"Pacific County","otherGeospatial":"North Beach Peninsula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.17572021484375,\n              46.240651955001695\n            ],\n            [\n              -123.66348266601562,\n              46.240651955001695\n            ],\n            [\n              -123.66348266601562,\n              46.76056154244133\n            ],\n            [\n              -124.17572021484375,\n              46.76056154244133\n            ],\n            [\n              -124.17572021484375,\n              46.240651955001695\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a74a","contributors":{"authors":[{"text":"Tracy, James V.","contributorId":52585,"corporation":false,"usgs":true,"family":"Tracy","given":"James","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":163180,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9281,"text":"ofr77594 - 1977 - Graded layering in the Al Hadah pluton near At Ta'if, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr77594","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":"77-594","title":"Graded layering in the Al Hadah pluton near At Ta'if, Kingdom of Saudi Arabia","docAbstract":"To assess urban storm-water-quality characteristics in the metropolitan area of Portland, Oreg., seven drainage basins were selected with varying drainage areas, basin slopes, impervious areas, land uses, and active construction areas. Automatic water-quality samplers, rain gages, and stream gages were installed in each basin. From September 1, 1975, to May 1, 1976, data were collected to determine rainfall intensities and stream discharge. Almost 500 samples from the seven basins were analyzed to describe pollutants for at least four complete storms on each of the basins. In addition to the storm samples, several base-flow samples were collected and analyzed for each site. Stream discharge and water-quality data are tabulated. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77594","usgsCitation":"Hadley, D.G., and Greenwood, W., 1977, Graded layering in the Al Hadah pluton near At Ta'if, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 77-594, iv, 39 leaves :ill., maps ;28 cm., https://doi.org/10.3133/ofr77594.","productDescription":"iv, 39 leaves :ill., maps ;28 cm.","costCenters":[],"links":[{"id":140913,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0594/report-thumb.jpg"},{"id":36993,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0594/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db673f65","contributors":{"authors":[{"text":"Hadley, Donald G.","contributorId":19527,"corporation":false,"usgs":true,"family":"Hadley","given":"Donald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":159414,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Greenwood, William R.","contributorId":53789,"corporation":false,"usgs":true,"family":"Greenwood","given":"William R.","affiliations":[],"preferred":false,"id":159415,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9594,"text":"ofr77676 - 1977 - Digital model of the Arikaree Aquifer near Wheatland, southeastern Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:06:14","indexId":"ofr77676","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":"77-676","title":"Digital model of the Arikaree Aquifer near Wheatland, southeastern Wyoming","docAbstract":"A digital model that mathematically simulates the flow of ground water, approximating the flow system as two-dimensional, has been applied to predict the long-term effects of irrigation and proposed industrial pumping from the unconfined Arikaree aquifer in a 400 square-mile area in southeastern Wyoming. Three cases that represent projected maximum, mean, and minimum combined irrigation and industrial ground-water withdrawals at annual rates of 16,176, 11,168, and 6,749 acre-feet, respectively, were considered. Water-level declines of more than 5 feet over areas of 124, 120, and 98 square miles and depletions in streamflow of 14.4, 8.9, and 7.2 cfs from the Laramie and North Laramie Rivers were predicted to occur at the end of a 40-year simulation period for these maximum, mean, and minimum withdrawal rates, respectively. A tenfold incrase in the vertical hydraulic conductivity that was assumed for the streambeds results in smaller predicted drawdowns near the Laramie and North Laramie Rivers and a 36 percent increase in the predicted depletion in streamflow for the North Laramie River. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77676","usgsCitation":"Hoxie, D.T., 1977, Digital model of the Arikaree Aquifer near Wheatland, southeastern Wyoming: U.S. Geological Survey Open-File Report 77-676, vi, 54 p. :ill., maps ;28 cm.; (88 p. - PGS), https://doi.org/10.3133/ofr77676.","productDescription":"vi, 54 p. :ill., maps ;28 cm.; (88 p. - PGS)","costCenters":[],"links":[{"id":142137,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0676/report-thumb.jpg"},{"id":37323,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0676/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a94e4b07f02db6594f5","contributors":{"authors":[{"text":"Hoxie, Dwight T.","contributorId":77531,"corporation":false,"usgs":true,"family":"Hoxie","given":"Dwight","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":159970,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}