{"pageNumber":"580","pageRowStart":"14475","pageSize":"25","recordCount":16498,"records":[{"id":10430,"text":"ofr77289 - 1977 - Water resources of the Barona, Capitan Grande, and Sycuan Indian Reservations, San Diego County, California","interactions":[],"lastModifiedDate":"2016-09-27T11:24:10","indexId":"ofr77289","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":"77-289","title":"Water resources of the Barona, Capitan Grande, and Sycuan Indian Reservations, San Diego County, California","docAbstract":"<p>The Barona and Capitan Grande Indian Reservations, California, have sufficient water to satisfy present (1976) domestic and stock needs; however, the Sycuan Indian Reservation is experiencing a shortage of water for domestic supply because of the decline of the water table beneath the reservation well field and a general decline of the water table surrounding the reservation. </p><p>The water quality on the three reservations is generally good; however, the water is at or near land surface in several areas. This shallow water could be subject to contamination by animal waste, septic tanks, or farming operations. Historical hydrologic data were obtained from government agencies and private individuals, and all wells and springs on the reservations were visited. This report summarizes the data collected and the findings of the study. (Woodard-USGS)</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Menlo Park, CA","doi":"10.3133/ofr77289","usgsCitation":"Moyle, W., and Blazs, R., 1977, Water resources of the Barona, Capitan Grande, and Sycuan Indian Reservations, San Diego County, California: U.S. Geological Survey Open-File Report 77-289, Report: iv, 33 p.; 3 Plates: 22.88 x 25.79 inches or smaller, https://doi.org/10.3133/ofr77289.","productDescription":"Report: iv, 33 p.; 3 Plates: 22.88 x 25.79 inches or smaller","numberOfPages":"40","costCenters":[],"links":[{"id":145838,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr77289.jpg"},{"id":328970,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0289/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":328968,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0289/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":328971,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0289/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":328969,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0289/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"San Diego County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.44659423828125,\n              32.63012300670739\n            ],\n            [\n              -117.44659423828125,\n              33.273139123013486\n            ],\n            [\n              -115.8233642578125,\n              33.273139123013486\n            ],\n            [\n              -115.8233642578125,\n              32.63012300670739\n            ],\n            [\n              -117.44659423828125,\n              32.63012300670739\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49b3e4b07f02db5ca071","contributors":{"authors":[{"text":"Moyle, W. R.","contributorId":27421,"corporation":false,"usgs":true,"family":"Moyle","given":"W. R.","affiliations":[],"preferred":false,"id":161378,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blazs, R.L.","contributorId":27067,"corporation":false,"usgs":true,"family":"Blazs","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":161377,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":12105,"text":"ofr77381 - 1977 - Hydrologic data for urban studies in the Dallas, Texas metropolitan area, 1975","interactions":[],"lastModifiedDate":"2017-06-14T11:28:12","indexId":"ofr77381","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":"77-381","title":"Hydrologic data for urban studies in the Dallas, Texas metropolitan area, 1975","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77381","usgsCitation":"Hampton, B., and Wood, C., 1977, Hydrologic data for urban studies in the Dallas, Texas metropolitan area, 1975: U.S. Geological Survey Open-File Report 77-381, v, 214 p., https://doi.org/10.3133/ofr77381.","productDescription":"v, 214 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":145010,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Texas","city":"Dallas","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db60810e","contributors":{"authors":[{"text":"Hampton, B.B.","contributorId":43362,"corporation":false,"usgs":true,"family":"Hampton","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":165092,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, C.M.","contributorId":106454,"corporation":false,"usgs":true,"family":"Wood","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":165093,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":12104,"text":"ofr7772 - 1977 - Hydrologic data for Mountain Creek, Trinity River basin, Texas, 1975","interactions":[],"lastModifiedDate":"2017-06-14T13:25:46","indexId":"ofr7772","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":"77-72","title":"Hydrologic data for Mountain Creek, Trinity River basin, Texas, 1975","docAbstract":"<p>Mountain Creek drains the northeast corner of Johnson County, the northwest corner of Ellis County, the southeast corner of Tarrant County, and part of the southwest corner of Dallas County, Tex. The basin is 30 miles long and averages 10 miles in width. The total drainage area at the mouth is 304 sq mi. Basin outflow for the 1975 water year was 146,400 acre-feet which is 68,880 acre-feet above the 15-year (1960-75) average of 77,520 acre-feet. Storage in Mountain Creek Lake showed a net loss of 150 acre-feet during the water year. Rainfall over the study area for the 1975 water year was about 39 inches, which is about 5 inches above the 15-year mean for the area. (Woodard-USGS)</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7772","usgsCitation":"Buckner, H., 1977, Hydrologic data for Mountain Creek, Trinity River basin, Texas, 1975: U.S. Geological Survey Open-File Report 77-72, v, 20 p., https://doi.org/10.3133/ofr7772.","productDescription":"v, 20 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":145009,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fa3f","contributors":{"authors":[{"text":"Buckner, H.D.","contributorId":49783,"corporation":false,"usgs":true,"family":"Buckner","given":"H.D.","email":"","affiliations":[],"preferred":false,"id":165091,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6045,"text":"pp655N - 1977 - The hydrologic history of the San Carlos Reservoir, Arizona, 1929-71, with particular reference to evapotranspiration and sedimentation","interactions":[],"lastModifiedDate":"2012-02-02T00:05:56","indexId":"pp655N","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"655","chapter":"N","title":"The hydrologic history of the San Carlos Reservoir, Arizona, 1929-71, with particular reference to evapotranspiration and sedimentation","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp655N","usgsCitation":"Kipple, F.P., 1977, The hydrologic history of the San Carlos Reservoir, Arizona, 1929-71, with particular reference to evapotranspiration and sedimentation: U.S. Geological Survey Professional Paper 655, 39 p., https://doi.org/10.3133/pp655N.","productDescription":"39 p.","costCenters":[],"links":[{"id":121447,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0655n/report-thumb.jpg"},{"id":33021,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0655n/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a86e4b07f02db64da2c","contributors":{"authors":[{"text":"Kipple, Frank P.","contributorId":75523,"corporation":false,"usgs":true,"family":"Kipple","given":"Frank","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":152009,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":11635,"text":"ofr77734 - 1977 - Quantity and quality of drainage from the Argo Tunnel and other sources related to metal mining in Gilpin, Clear Creek and Park Counties, Colorado","interactions":[],"lastModifiedDate":"2012-04-19T17:28:34","indexId":"ofr77734","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":"77-734","title":"Quantity and quality of drainage from the Argo Tunnel and other sources related to metal mining in Gilpin, Clear Creek and Park Counties, Colorado","docAbstract":"Eighteen metal-mine drainage sources have been located in that part of Gilpin, Clear Creek, and Park Counties, Colo., lying within the Missouri River basin. At least 13 of these sources are known to contain high acidity and (or) trace-element concentrations or to contribute water to adversely affected streams. From January 1976 to March 1977, drainage from the Argo Tunnel in Idaho Springs--one of the major metal-mine drainage sources in the study area--exhibited variations in discharge from 0.35 to 0.55 cubic feet per second (0.010 to 0.016 cubic meters per second), a relatively constant temperature of 16 degrees Celsius, and variations in specific conductance from 2,680 to 3,410 micromhos per centimeter at 25 degrees Celsius (though a value of about 3,100 micromhos persisted throughout most of the period of record). High, but relatively constant, total concentrations (in micrograms per liter) of arsenic (100 to 180), cadmium (140 to 170), copper (5,000 to 6,000), iron (160,000 to 200,000), lead (less than 100 to 200), manganese (80,000 to 110,000), and zinc (40,000 to 49,000) were measured in the Argo Tunnel drainage from March 1976 to March 1977. Except for lead, the trace elements were mostly dissolved (82 percent or greater) and appear to represent baseline concentrations. Long-term degradation of water flowing from the Argo Tunnel is shown by increases of at least 2.5 to 8.0 times for dissolved solids, dissolved iron, calcium, magnesium, and sulfate since 1906. The acidity has changed from neutral in 1906 to a median pH value of 2.9 in 1976-77. Comparison of current Argo Tunnel data with those collected previously by other investigators indicates that spring chemical flushes containing higher than baseline trace-element concentrations occurred in 1973 and 1974, but not in 1975 or 1976, and probably not in 1972. The spring chemical flushes appear to be associated with increased infiltration from snowmelt in the catchment of the Argo Tunnel. Because of the wide ranges in mine-drainage quality and quantity expected for discharges from abandoned mines in the study area, each situation must be examined  individually, and the management alternative chosen for mine-drainage abatement must be tailored to solve the particular mining and hydrologic problems at a given site.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Water and Related Land Resources Management Study","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr77734","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers Omaha District, Omaha, Nebraska","usgsCitation":"Wentz, D.A., 1977, Quantity and quality of drainage from the Argo Tunnel and other sources related to metal mining in Gilpin, Clear Creek and Park Counties, Colorado: U.S. Geological Survey Open-File Report 77-734, iv, 61 leaves :ill., maps; Volume V: Supporting Technical Reports Appendices; Appendix F: USGS Mine Drainage Study; 27 cm., https://doi.org/10.3133/ofr77734.","productDescription":"iv, 61 leaves :ill., maps; Volume V: Supporting Technical Reports Appendices; Appendix F: USGS Mine Drainage Study; 27 cm.","numberOfPages":"128","costCenters":[],"links":[{"id":144951,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_77_734.png"},{"id":254517,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0734/ofr77-0734.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","county":"Gilpin County;Clear Creek County;Park County","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64adf5","contributors":{"authors":[{"text":"Wentz, Dennis A. dawentz@usgs.gov","contributorId":1838,"corporation":false,"usgs":true,"family":"Wentz","given":"Dennis","email":"dawentz@usgs.gov","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":163482,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10583,"text":"ofr77264 - 1977 - January 1977 water levels, and data related to water-level changes since 1950, western Kansas","interactions":[],"lastModifiedDate":"2017-09-29T08:07:58","indexId":"ofr77264","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":"77-264","title":"January 1977 water levels, and data related to water-level changes since 1950, western Kansas","docAbstract":"<p>This report contains basic data on water-level measurements in observation wells in western Kansas. Most of the measurements were made in January 1977; a few were made in December 1976 and in February 1977. The measurements were made in mid-winter when pumping was minimal and water levels had recovered from the effects of pumping during the previous irrigation season. This report also contains basic hydrologic data for 1950-77 that are provided for consideration in relation to the January 1977 water-level measurements.</p><p>The annual water-level measurements are made by personnel of the Division of Water Resources of the Kansas State Board of Agriculture and of the U.S. Geological Survey. State-agency support for this program is provided through the Kansas Geological Survey.</p><p>Wells in this report are numbered according to the Bureau of Land Management's system of land subdivision. In this system, the first set of digits of a well number indicates the township; the second set, the range east or west of the sixth prinicipal meridian; and the third set, the section in which the well is situated. The first letter denotes the 160-acre tract, the second, the 40-acre tract, and the third, the 10-acre tract. The letters are designated in a counterclockwise direction beginning in the northeast quarter of the section. Where there is more than one well in a 10-acre tract, consecutive numbers, beginning with \"2\", are added in the order in which the wells are inventoried.<br></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77264","usgsCitation":"Pabst, M.E., 1977, January 1977 water levels, and data related to water-level changes since 1950, western Kansas: U.S. Geological Survey Open-File Report 77-264, 209 p., https://doi.org/10.3133/ofr77264.","productDescription":"209 p.","numberOfPages":"213","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":346201,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0264/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144315,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0264/report-thumb.jpg"}],"country":"United States","state":"Kansas","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db666fc7","contributors":{"authors":[{"text":"Pabst, Marilyn E.","contributorId":25566,"corporation":false,"usgs":true,"family":"Pabst","given":"Marilyn","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":161633,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8121,"text":"ofr77597 - 1977 - Flood-hazard study: 100-year flood stage for Lucerne Lake, San Bernadino County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr77597","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":"77-597","title":"Flood-hazard study: 100-year flood stage for Lucerne Lake, San Bernadino County, California","docAbstract":"A study of the flood hydrology of Lucerne Valley, Calif., was made to develop the 100-year stage for Lucerne Lake. Synthetic-hydrologic techniques were used; and the 100-year flood stage was estimated to be at an elevation of 2,849.3 feet above mean sea level. Channel dimensions were measured at 59 sites in Lucerne Valley. Dranage area-discharge relations developed from channel-geometry data for sites nearby were used to estimate the discharge at 12 additional sites where channel geometry could not be measured. In order to compute the total volume discharge into the playa, the peak discharges were converted to volumes. From the Apple Valley report (Busby, 1975) the equation formulated from the relation between peak discharge and flood volume for the deserts of California was used to compute the flood volumes for routing into Lucerne Lake. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77597","usgsCitation":"Busby, M.W., 1977, Flood-hazard study: 100-year flood stage for Lucerne Lake, San Bernadino County, California: U.S. Geological Survey Open-File Report 77-597, iv, 32 p. :ill., maps ;27 cm.; (37 p., 1 sheet - PGS), https://doi.org/10.3133/ofr77597.","productDescription":"iv, 32 p. :ill., maps ;27 cm.; (37 p., 1 sheet - PGS)","costCenters":[],"links":[{"id":140545,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e74b3","contributors":{"authors":[{"text":"Busby, Mark William","contributorId":67088,"corporation":false,"usgs":true,"family":"Busby","given":"Mark","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":157184,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4139,"text":"cir751B - 1977 - The United States Geological Survey in Alaska: Accomplishments during 1976","interactions":[],"lastModifiedDate":"2018-01-30T12:47:37","indexId":"cir751B","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":"751","chapter":"B","title":"The United States Geological Survey in Alaska: Accomplishments during 1976","docAbstract":"United States Geological Survey projects in Alaska include a wide range of topics of economic and scientific interest. Studies in 1976 include economic geology, regional geology, stratigraphy, environmental geology, engineering geology, hydrology, and marine geology. Discussions of the findings or, in some instances, narratives of the course of the investigations are grouped in eight subdivisions corresponding to the six major onshore geographic regions, the offshore projects, and projects that are statewide in scope. Locations of the study areas are shown. In addition, many reports and maps covering various aspects of the geology and mineral and water resources of the State were published. These publications are listed. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir751B","usgsCitation":"1977, The United States Geological Survey in Alaska: Accomplishments during 1976: U.S. Geological Survey Circular 751, vi, 112 p., https://doi.org/10.3133/cir751B.","productDescription":"vi, 112 p.","costCenters":[],"links":[{"id":31246,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1977/0751b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122784,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1977/0751b/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db6988eb","contributors":{"editors":[{"text":"Blean, Kathleen M.","contributorId":31764,"corporation":false,"usgs":true,"family":"Blean","given":"Kathleen","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":726183,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":9807,"text":"ofr77583 - 1977 - Leachate plumes in ground water from Babylon and Islip landfills, Long Island, New York","interactions":[{"subject":{"id":9807,"text":"ofr77583 - 1977 - Leachate plumes in ground water from Babylon and Islip landfills, Long Island, New York","indexId":"ofr77583","publicationYear":"1977","noYear":false,"title":"Leachate plumes in ground water from Babylon and Islip landfills, Long Island, New York"},"predicate":"SUPERSEDED_BY","object":{"id":6101,"text":"pp1085 - 1980 - Leachate plumes in ground water from Babylon and Islip landfills, Long Island, New York","indexId":"pp1085","publicationYear":"1980","noYear":false,"title":"Leachate plumes in ground water from Babylon and Islip landfills, Long Island, New York"},"id":1}],"supersededBy":{"id":6101,"text":"pp1085 - 1980 - Leachate plumes in ground water from Babylon and Islip landfills, Long Island, New York","indexId":"pp1085","publicationYear":"1980","noYear":false,"title":"Leachate plumes in ground water from Babylon and Islip landfills, Long Island, New York"},"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr77583","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":"77-583","title":"Leachate plumes in ground water from Babylon and Islip landfills, Long Island, New York","docAbstract":"Landfills operated by the towns of Babylon and Islip in southwest and central Suffolk County, N.Y., contain urban refuse , incinerated garbage, and scavenger (cesspool) waste; some industrial refuse is deposited at the Babylon site. The Islip landfill was started in 1933, the Babylon landfill in 1947. The landfills are in contact with and discharge leachate into the highly permeable upper glacial aquifer hydraulic conductivity 190 to 500 ft/d. The aquifer is 74 feet thick at the Babylon landfill and 170 feet thick at the Islip landfill. The leachate-enriched water occupies the entire thickness of the aquifer beneath both landfills, but hydrologic boundaries retard downward migration of the plumes to deeper aquifers. The Babylon plume is 1,900 feet wide at the landfill and narrows to about 700 feet near its terminus 10,000 feet from the landfill. The Islip plume is 1,400 feet wide at the landfill and narrows to 500 feet near its terminus 5,000 feet from the landfill. Hydrochemical maps and sections show the distribution of the major chemical constituents of the plumes. The most highly leachate-enriched ground water obtained was from the Babylon site; it contained 860 mg/liter sodium, 110 mg/liter potassium, 565 mg/liter calcium, 100 mg/liter magnesium, 2,700 mg/liter bicarbonate, and 1,300 mg/liter chloride. Simulation of the movement and dispersion of the Babylon plume with a mathematical dispersion model indicated the coefficient of longitudinal dispersion to be about 60 feet squared per day and the ground-water velocity to be 1 ft/d. However, the velocity determined from the hydraulic gradient and public-supply wells in the area was 4 ft/d, which would cause a plume four times as long as that predicted by the model. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77583","usgsCitation":"Kimmel, G.E., and Braids, O.C., 1977, Leachate plumes in ground water from Babylon and Islip landfills, Long Island, New York: U.S. Geological Survey Open-File Report 77-583, vi, 72 leaves :ill., maps (2 fold. in pocket) ;29 cm.; (141 p. - PGS), https://doi.org/10.3133/ofr77583.","productDescription":"vi, 72 leaves :ill., maps (2 fold. in pocket) ;29 cm.; (141 p. - PGS)","costCenters":[],"links":[{"id":141824,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b45f7","contributors":{"authors":[{"text":"Kimmel, Grant E.","contributorId":20741,"corporation":false,"usgs":true,"family":"Kimmel","given":"Grant","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":160332,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Braids, Olin C.","contributorId":84368,"corporation":false,"usgs":true,"family":"Braids","given":"Olin","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":160333,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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. ","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":30959,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1977/0745/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123994,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1977/0745/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48d8e4b07f02db54942f","contributors":{"authors":[{"text":"Giusti, Ennio V.","contributorId":35301,"corporation":false,"usgs":true,"family":"Giusti","given":"Ennio","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":147753,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, E.L.","contributorId":102870,"corporation":false,"usgs":true,"family":"Meyer","given":"E.L.","email":"","affiliations":[],"preferred":false,"id":147754,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7229,"text":"ofr77274 - 1977 - Hydrologic data for urban studies in the Houston, Texas, metropolitan area, 1975","interactions":[],"lastModifiedDate":"2017-06-14T13:13:05","indexId":"ofr77274","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":"77-274","title":"Hydrologic data for urban studies in the Houston, Texas, metropolitan area, 1975","docAbstract":"<p>Detailed rainfall-runoff computations, including hydrographs and mass curves, are presented for nine storm periods during the 1975 water year in drainage basins in the Houston, Texas metropolitan area. The information will be useful in determining the extent to which progressive urbanization will affect the yield and mode of occurrence of storm runoff. (Woodard-USGS)</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77274","usgsCitation":"Ranzau, C., 1977, Hydrologic data for urban studies in the Houston, Texas, metropolitan area, 1975: U.S. Geological Survey Open-File Report 77-274, v, 314 p., https://doi.org/10.3133/ofr77274.","productDescription":"v, 314 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":139938,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Texas","city":"Houston","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.36819458007811,\n              30.039377605001338\n            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C.E.","contributorId":23537,"corporation":false,"usgs":true,"family":"Ranzau","given":"C.E.","affiliations":[],"preferred":false,"id":154838,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9795,"text":"ofr76724 - 1977 - Hydrologic data for North Creek, Trinity River basin, Texas, 1975","interactions":[],"lastModifiedDate":"2022-01-03T20:52:43.292044","indexId":"ofr76724","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":"76-724","title":"Hydrologic data for North Creek, Trinity River basin, Texas, 1975","docAbstract":"<p>This report contains the rainfall, runoff, and storage data collected during the 1975 water year for the 21.6-square-mile area above the stream-gaging station North Creek near Jacksboro, Texas. The weighted-mean rainfall in the study area during the water year was 39.01 inches, which is greater than the 18-year average of 30.21 inches for the period 1958-75. Monthly rainfall totals ranged from 1.04 inches in November to 7.94 inches in May. The mean discharge for 1975 at the stream-gaging station was 5.98 cfs, compared with the 14-year (1957-70) average of 5.75 cfs. The annual runoff from the basin above the stream-gaging station was 4,330 acre-feet or 3.76 inches. Three storms were selected for detailed computations for the 1975 water year. The storms occurred on Oct. 30-31, 1974, May 2, 1975 , and Aug. 26, 1975. Rainfall and discharge were computed on the basis of a refined time breakdown. Patterns of the storms are illustrated by hydrographs and mass curves. A summary of rainfall-runoff data is tabulated. There are five floodwater-retarding structures in the study area. These structures have a total capacity of 4,425 acre-feet below flood-spillway crests and regulate streamflow from 16.3 square miles, or 75 percent of the study area. A summary of the physical data at each of the floodwater-retarding structures is included. (Woodard-USGS)</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr76724","collaboration":"Prepared in cooperation with the Tarrant County Water Control and Improvement District No. 1, the Soil Conservation Service, and the Texas Water Development Board","usgsCitation":"Kidwell, C., 1977, Hydrologic data for North Creek, Trinity River basin, Texas, 1975: U.S. Geological Survey Open-File Report 76-724, 50 p., https://doi.org/10.3133/ofr76724.","productDescription":"50 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":141765,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0724/report-thumb.jpg"},{"id":393797,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0724/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","otherGeospatial":"North Creek","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b16b9","contributors":{"authors":[{"text":"Kidwell, C.C.","contributorId":54998,"corporation":false,"usgs":true,"family":"Kidwell","given":"C.C.","email":"","affiliations":[],"preferred":false,"id":160315,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10616,"text":"ofr77368 - 1977 - Hydrologic monitoring of a waste-injection well near Milton, Florida, June 1975 - December 1976","interactions":[],"lastModifiedDate":"2012-02-02T00:06:21","indexId":"ofr77368","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":"77-368","title":"Hydrologic monitoring of a waste-injection well near Milton, Florida, June 1975 - December 1976","docAbstract":"Hydraulic and chemical data were collected through a monitoring program conducted by the U.S. Geological Survey at an industrial liquid-waste injection site 6 mi southwest of Milton, Fla., in Santa Rosa County. The injection system is described. Data include injection rates, volumes, and pressures; water-level data at three monitor wells and a standby injection well, and field and laboratory analyses of water samples from four wells. Hydraulic and geochemical effects of the waste-injection system at the plant as of December 31, 1976, have been detected only in the injection zone, the lower limestone of the Floridan aquifer. Increased pressures are evident at the three wells used to monitor the injection zone. Geochemical changes have been noted only at the deep-test monitor well closest to the injection well. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77368","usgsCitation":"Pascale, C.A., and Martin, J., 1977, Hydrologic monitoring of a waste-injection well near Milton, Florida, June 1975 - December 1976: U.S. Geological Survey Open-File Report 77-368, v, 46 leaves :ill., map ;27 cm.; (32 p. - PGS), https://doi.org/10.3133/ofr77368.","productDescription":"v, 46 leaves :ill., map ;27 cm.; (32 p. - PGS)","costCenters":[],"links":[{"id":142464,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606dbc","contributors":{"authors":[{"text":"Pascale, Charles A.","contributorId":99978,"corporation":false,"usgs":true,"family":"Pascale","given":"Charles","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161687,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, J.B.","contributorId":32923,"corporation":false,"usgs":true,"family":"Martin","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":161686,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11696,"text":"ofr77511 - 1977 - Hydrologic data for a subsurface waste-injection site at Mulberry, Florida, 1972-76","interactions":[],"lastModifiedDate":"2012-02-02T00:06:35","indexId":"ofr77511","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":"77-511","title":"Hydrologic data for a subsurface waste-injection site at Mulberry, Florida, 1972-76","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77511","usgsCitation":"Wilson, W.E., 1977, Hydrologic data for a subsurface waste-injection site at Mulberry, Florida, 1972-76: U.S. Geological Survey Open-File Report 77-511, 24 leaves :ill., map ;27 cm., https://doi.org/10.3133/ofr77511.","productDescription":"24 leaves :ill., map ;27 cm.","costCenters":[],"links":[{"id":145038,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60eb9f","contributors":{"authors":[{"text":"Wilson, William Edward","contributorId":82321,"corporation":false,"usgs":true,"family":"Wilson","given":"William","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":163584,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2566,"text":"wsp1608P - 1977 - Ground-water resources of Cambodia","interactions":[],"lastModifiedDate":"2012-02-02T00:05:29","indexId":"wsp1608P","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1608","chapter":"P","title":"Ground-water resources of Cambodia","docAbstract":"Cambodia (now the Khmer Republic), in tropical, humid southeast Asia, has an area of 175,630 km and a population of about 5 million. The Mekong River, one of the world's largest rivers, flows through Cambodia. Also, the Tonle Sap (Grand Lac), a highly productive fresh-water lake, functions as a huge off-channel storage reservoir for flood flow of the Mekong River. Surfacewater discharge in streams and rivers of Cambodia is abundant during the wet season, mid-May through mid-November, when 85 percent of the precipitation falls, but is frequently deficient during the remainder of the year. Annual rainfall ranges from 1,370 mm in the central lowlands to more than 5,000 mm in the mountainous highlands. The mean annual temperature for the country is 27.5?C and the evaporation rate is high. \r\n\r\nDuring 1960-63, 1,103 holes were drilled in 16 of the 18 khets (provinces), of which 795 or approximately 72 percent, were productive wells at rates ranging from 1.1 to 2,967 l/min. The productive wells ranged in depth from 2 to 209.4 m and were 23.2 m deep on the average. \r\n\r\nMr. Rasmussen ' studied the subsurface geology of Cambodia in considerable detail by examining drillers' logs and constructing nine geologic cross sections. The principal aquifer tapped by drilled wells in Cambodia is the Old Alluvium. In many places, however, dug wells and a few shallow drilled wells obtain water from the Young Alluvium. Sandstone of the Indosinias Formation yields moderate to small quantities of water to wells in a number of places. Also, wells tapping water-bearing basalt have a small to moderate yield. The quality of water is recorded in only a few analyses. The dissolved solids concentrations appear to be generally low so that the water is usable for most purposes without treatment. Some well waters, however, are high in iron and would have to be aerated and filtered before use. In this report, well records are tabulated, and the geology and hydrology is discussed by khets. The bulk of the available information is on the central lowlands and contiguous low plateaus, as the mountainous areas on the west and the high plateaus on the east are relatively unexplored with respect to their ground-water availability. \r\n\r\nNo persistent artesian aquifer has been identified nor have any large potential ground-water sources been found .although much of the country yet remains to be explored by test drilling. Well irrigation for garden produce is feasible on a modest scale in many localities throughout Cambodia. It does not seem likely, however, that large-scale irrigation from wells will come about in the future. Ground water may be regarded as a widely available supplemental source to surface water for domestic, small-scale industrial, and irrigation use.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1608P","usgsCitation":"Rasmussen, W., and Bradford, G.M., 1977, Ground-water resources of Cambodia: U.S. Geological Survey Water Supply Paper 1608, iv, 122 p. :maps (3 fold. col. in pocket) ;23 cm. --, https://doi.org/10.3133/wsp1608P.","productDescription":"iv, 122 p. :maps (3 fold. col. in pocket) ;23 cm. --","costCenters":[],"links":[{"id":138585,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1608p/report-thumb.jpg"},{"id":28832,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608p/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28833,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608p/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28834,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608p/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28835,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1608p/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696d00","contributors":{"authors":[{"text":"Rasmussen, William Charles","contributorId":12021,"corporation":false,"usgs":true,"family":"Rasmussen","given":"William Charles","affiliations":[],"preferred":false,"id":145410,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bradford, Gary M.","contributorId":21529,"corporation":false,"usgs":true,"family":"Bradford","given":"Gary","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":145411,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10685,"text":"ofr77596 - 1977 - Hydrologic reconnaissance evaluation of the Federal Capital Territory and surrounding areas, Nigeria","interactions":[],"lastModifiedDate":"2012-02-02T00:06:28","indexId":"ofr77596","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":"77-596","title":"Hydrologic reconnaissance evaluation of the Federal Capital Territory and surrounding areas, Nigeria","docAbstract":"Initial moderate water requirements of the new Federal Capital Territory in Central Nigeria are available from the two large rivers, the Niger and Benue, from the smaller Gurara River, and possibly from several smaller streams. Ground water in the southwestern part of the Territory and in adjacent areas along the Niger River is also a potential source. The Niger and Benue Rivers are obvious sources of major supply for eventual large demands, and the Gurara River and sedimentary aquifers also may have that potential. Available data are sparse and highly inadequate for satisfactory design of assessment, development, and management plans for the Territory. Initiation of systematic investigation and collection of data at an early date is recommended. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77596","usgsCitation":"Peterson, L., and Meyer, G., 1977, Hydrologic reconnaissance evaluation of the Federal Capital Territory and surrounding areas, Nigeria: U.S. Geological Survey Open-File Report 77-596, 30 leaves :maps ;27 cm.; (31 p. - PGS), https://doi.org/10.3133/ofr77596.","productDescription":"30 leaves :maps ;27 cm.; (31 p. - PGS)","costCenters":[],"links":[{"id":144233,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605619","contributors":{"authors":[{"text":"Peterson, L.R.","contributorId":40993,"corporation":false,"usgs":true,"family":"Peterson","given":"L.R.","email":"","affiliations":[],"preferred":false,"id":161797,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, Gerald","contributorId":76721,"corporation":false,"usgs":true,"family":"Meyer","given":"Gerald","email":"","affiliations":[],"preferred":false,"id":161798,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10754,"text":"ofr77566 - 1977 - Ground-water hydrology and subsurface migration of radioisotopes at a low-level solid radioactive-waste disposal site, West Valley, New York","interactions":[{"subject":{"id":10754,"text":"ofr77566 - 1977 - Ground-water hydrology and subsurface migration of radioisotopes at a low-level solid radioactive-waste disposal site, West Valley, New York","indexId":"ofr77566","publicationYear":"1977","noYear":false,"title":"Ground-water hydrology and subsurface migration of radioisotopes at a low-level solid radioactive-waste disposal site, West Valley, New York"},"predicate":"SUPERSEDED_BY","object":{"id":38538,"text":"pp1325 - 1986 - Ground-water hydrology and subsurface migration of radionuclides at a commercial radioactive-waste burial site, West Valley, Cattaraugus County, New York","indexId":"pp1325","publicationYear":"1986","noYear":false,"title":"Ground-water hydrology and subsurface migration of radionuclides at a commercial radioactive-waste burial site, West Valley, Cattaraugus County, New York"},"id":1}],"supersededBy":{"id":38538,"text":"pp1325 - 1986 - Ground-water hydrology and subsurface migration of radionuclides at a commercial radioactive-waste burial site, West Valley, Cattaraugus County, New York","indexId":"pp1325","publicationYear":"1986","noYear":false,"title":"Ground-water hydrology and subsurface migration of radionuclides at a commercial radioactive-waste burial site, West Valley, Cattaraugus County, New York"},"lastModifiedDate":"2012-02-02T00:06:23","indexId":"ofr77566","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":"77-566","title":"Ground-water hydrology and subsurface migration of radioisotopes at a low-level solid radioactive-waste disposal site, West Valley, New York","docAbstract":"Burial trenches for disposal of solid radioactive waste at West Valley, N.Y., are excavated in till that has very low hydraulic conductivity (about 5 x 10 to the minus 8th power centimeters per second). Fractures and root tubes with chemically oxidized and (or) reduced soil in their walls extend to 3 to 4.5 meters below natural land surface. Preliminary simulations of pressure heads with a digital model suggest that hydraulic conductivity is an order of magnitude greater in the fractured till near land surface than at greater depth. Hydraulic gradients are predominantly downward, even beneath small valleys. The upper part of a body of underlying lacustrine silt is unsaturated; in the lower, saturated part, slow lateral flow may occur. In the older trenches, water began to build up in 1971, overflowed briefly in 1975, and was pumped out in 1975-76. Water levels rose abruptly during major rainstorms in mid-1975, indicating rapid infiltration through cracks in the cover material. The new trenches have maintained low, stable water levels, perhaps because of thicker, more compact cover and less waste settlement; pressure heads near these trenches are low, locally approaching zero, perhaps because of slight infiltration and limited near-surface storage. Peak tritium concentrations in test-hole cores (generally 0.00001 to 0.001 microcuries per milliliter) were found within 3 meters of land surface and are attributed to surface contamination. Concentrations declined rapidly with depth within the fractured till; secondary peaks found at about 9 meters in three holes are attributed to lateral migration from trenches. Other radioisotopes were detected only near land surface. Samples from the walls of shallow fractures revealed no accumulation of radioisotopes. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77566","usgsCitation":"Prudic, D.E., and Randall, A.D., 1977, Ground-water hydrology and subsurface migration of radioisotopes at a low-level solid radioactive-waste disposal site, West Valley, New York: U.S. Geological Survey Open-File Report 77-566, iv, 28 leaves :ill., map ;27 cm., https://doi.org/10.3133/ofr77566.","productDescription":"iv, 28 leaves :ill., map ;27 cm.","costCenters":[],"links":[{"id":143580,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0566/report-thumb.jpg"},{"id":38559,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0566/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668c43","contributors":{"authors":[{"text":"Prudic, David E. deprudic@usgs.gov","contributorId":3430,"corporation":false,"usgs":true,"family":"Prudic","given":"David","email":"deprudic@usgs.gov","middleInitial":"E.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":161905,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Randall, Allan D. arandall@usgs.gov","contributorId":1168,"corporation":false,"usgs":true,"family":"Randall","given":"Allan","email":"arandall@usgs.gov","middleInitial":"D.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":161904,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10049,"text":"ofr7818 - 1977 - Hydrology and surface morphology of the Bonneville Salt Flats and Pilot Valley playa, Utah","interactions":[{"subject":{"id":10049,"text":"ofr7818 - 1977 - Hydrology and surface morphology of the Bonneville Salt Flats and Pilot Valley playa, Utah","indexId":"ofr7818","publicationYear":"1977","noYear":false,"title":"Hydrology and surface morphology of the Bonneville Salt Flats and Pilot Valley playa, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":2129,"text":"wsp2057 - 1979 - Hydrology and surface morphology of the Bonneville Salt Flats and Pilot Valley Playa, Utah","indexId":"wsp2057","publicationYear":"1979","noYear":false,"title":"Hydrology and surface morphology of the Bonneville Salt Flats and Pilot Valley Playa, Utah"},"id":1}],"supersededBy":{"id":2129,"text":"wsp2057 - 1979 - Hydrology and surface morphology of the Bonneville Salt Flats and Pilot Valley Playa, Utah","indexId":"wsp2057","publicationYear":"1979","noYear":false,"title":"Hydrology and surface morphology of the Bonneville Salt Flats and Pilot Valley Playa, Utah"},"lastModifiedDate":"2012-02-02T00:06:40","indexId":"ofr7818","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":"78-18","title":"Hydrology and surface morphology of the Bonneville Salt Flats and Pilot Valley playa, Utah","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr7818","usgsCitation":"Lines, G.C., 1977, Hydrology and surface morphology of the Bonneville Salt Flats and Pilot Valley playa, Utah: U.S. Geological Survey Open-File Report 78-18, 196 p., :ill., maps ;27 cm. --, https://doi.org/10.3133/ofr7818.","productDescription":"196 p., :ill., maps ;27 cm. --","costCenters":[],"links":[{"id":145607,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e8a5","contributors":{"authors":[{"text":"Lines, Gregory C.","contributorId":50502,"corporation":false,"usgs":true,"family":"Lines","given":"Gregory","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":160729,"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":19486,"text":"ofr77803 - 1977 - Summary of hydrologic data collected during 1975 in Dade County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:07:29","indexId":"ofr77803","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":"77-803","title":"Summary of hydrologic data collected during 1975 in Dade County, Florida","docAbstract":"During the 1975 calendar year rainfall in Dade County, Fla., was 14.89 inches below the long-term average (57.17 in.). Ground-water levels ranged from 0.1 foot above to 1.1 feet below average. The highest and lowest ground-water levels for the year were both 1 foot below their long-term averages. In the Hialeah-Miami Springs area, ground-water levels in wells near the centers of the heaviest pumping ranged from 9.8 to 11.2 feet below mean sea level and in the Southwest well field area, ground-water levels near the centers of pumping ranged from 3.5 feet above to 3.4 feet below mean sea level. The combined average daily discharge from eight major streams and canals that flow into Biscayne Bay was 1,014 cubic feet per second (cfs), 124 cfs above the combined average daily flow for the 1974 water year. The combined average daily flow through the Tamiami Canal outlets was 568 cfs, 202 cfs below that of the 1974 water year. The position of the salt front in 1975 in the coastal part of the Biscayne aquifer was about the same as in 1974 except at Miami International Airport and Homestead Air Force Base where the salt front had encroached farther inland. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77803","usgsCitation":"Hull, J.E., and Beaven, T., 1977, Summary of hydrologic data collected during 1975 in Dade County, Florida: U.S. Geological Survey Open-File Report 77-803, 120 p. :ill., maps ;27 cm., https://doi.org/10.3133/ofr77803.","productDescription":"120 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":151882,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699184","contributors":{"authors":[{"text":"Hull, John E.","contributorId":15616,"corporation":false,"usgs":true,"family":"Hull","given":"John","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":180993,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beaven, T.R.","contributorId":84757,"corporation":false,"usgs":true,"family":"Beaven","given":"T.R.","email":"","affiliations":[],"preferred":false,"id":180994,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7228,"text":"ofr77266 - 1977 - Hydrologic Data for Urban Studies in the Fort Worth, Texas Metropolitan Area, 1975","interactions":[],"lastModifiedDate":"2016-08-10T16:39:24","indexId":"ofr77266","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":"77-266","title":"Hydrologic Data for Urban Studies in the Fort Worth, Texas Metropolitan Area, 1975","docAbstract":"<p>This report contains rainfall and runoff data collected during the 1975 water year for Sycamore Creek, Sycamore Creek tributary , Dry Branch, and Little Fossil Creek study areas in Fort Worth, Texas. The information will be useful in determining the extent to which progressive urbanization will affect the yield and mode of occurrence of storm runoff. Detailed rainfall-runoff computations, including hydrographs and mass curves, are presented for nine storm periods during the water year. (Woodard-USGS)</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77266","collaboration":"Prepared in cooperation with the City of Fort Worth","usgsCitation":"Slade, R., and Taylor, J., 1977, Hydrologic Data for Urban Studies in the Fort Worth, Texas Metropolitan Area, 1975: U.S. Geological Survey Open-File Report 77-266, 96 p., https://doi.org/10.3133/ofr77266.","productDescription":"96 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":258462,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0266/report-thumb.jpg"},{"id":258461,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0266/report.pdf","size":"14587","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db6142f3","contributors":{"authors":[{"text":"Slade, R.M. Jr.","contributorId":40595,"corporation":false,"usgs":true,"family":"Slade","given":"R.M.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":154836,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, J.M.","contributorId":42587,"corporation":false,"usgs":true,"family":"Taylor","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":154837,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":18258,"text":"ofr78200 - 1977 - Quality of rivers of the United States, 1975 water year; based on the National Stream Quality Accounting Network (NASQAN)","interactions":[],"lastModifiedDate":"2016-11-02T15:19:36","indexId":"ofr78200","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":"78-200","title":"Quality of rivers of the United States, 1975 water year; based on the National Stream Quality Accounting Network (NASQAN)","docAbstract":"<p>The National Stream Quality Accounting Network (NASQAN) was established by the U.S. Geological Survey to provide a nationally uniform basis for continuously assessing the quality of U.S. rivers. Stations generally are at the downstream end of hydrologic accounting units in order to measure the quantity and quality of water flowing from the units. The 1975 water year was the first year of operation of the network that represents essentially all of the accounting units and thereby describes the water- quality of the entire country. Data are available on a large number of water-quality constituents measured at 345 stations during the 1975 water year. </p><p>Temperature data (usually continuous or daily measurements) from NASQAN stations were fitted to a first order harmonic equation and the parameters for the harmonic function are reported for each station. Mean temperatures generally range from 5°-10°C in the North to more than 20°C along the southern border of the continental United States and in Hawaii and Puerto Rico; means were less than 10°C at 63 stations and greater than 25°C at only 7 stations. Amplitudes of the temperature curves are greatest (greater than 12°C) for the streams at midlatitudes and in the Great and Central Plains, and they are smallest for the subtropical and cold-climate streams. </p><p>Considering chemical and biological characteristics of U.S. streams as described by NASQAN data, water quality is best (by many standards) in the Northeast, Southeast, and Northwest. Waters there generally are low in dissolved solids and major and minor chemical constituents, generally are soft (except in Florida), and carry relatively small amounts of sediment. These conditions mainly reflect the geology of the regions and the relatively large amounts of precipitation. However, many of these waters show the effects of pollution and carry moderate or high levels of major nutrients and have correspondingly high populations of attached and floating plants. High counts of indicator bacteria also show signs of local pollution, particularly in regions of the country with large human and animal populations. In the Northeast, some heavy metals are at moderate levels, but not above most water-quality criteria.</p><p>Rivers of most of the Mid-Continent and Southwest reflect the arid or semi-arid climate, erodible soils, and agricultural activities. They are characterized by moderate to high levels of dissolved major and minor constituents, sediment, major nutrients, and biota (floating and attached aquatic plants and indicator bacteria). In addition, the most incidences of pesticides in stream and bottom sediments were found in these regions. </p><p>A special analysis was made to study the patterns of dissolved solids, major nutrients, phytoplankton, and zinc in the Mississippi River above Memphis, Tennessee. It was found that flow volume is an important factor in influencing river quality, and that stations with low concentration of major nutrients generally had low phytoplankton populations as well.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr78200","usgsCitation":"Briggs, J.C., and Ficke, J.F., 1977, Quality of rivers of the United States, 1975 water year; based on the National Stream Quality Accounting Network (NASQAN): U.S. Geological Survey Open-File Report 78-200, viii, 436 p., https://doi.org/10.3133/ofr78200.","productDescription":"viii, 436 p.","numberOfPages":"446","costCenters":[],"links":[{"id":151776,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr78200.jpg"},{"id":330665,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0200/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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States\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db654a8d","contributors":{"authors":[{"text":"Briggs, John C.","contributorId":24349,"corporation":false,"usgs":true,"family":"Briggs","given":"John","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":178791,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ficke, John F.","contributorId":86750,"corporation":false,"usgs":true,"family":"Ficke","given":"John","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":178792,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9183,"text":"ofr77741 - 1977 - Ground-water data for the Drewsey Resource Area, Harney and Malheur counties, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:06:16","indexId":"ofr77741","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":"77-741","title":"Ground-water data for the Drewsey Resource Area, Harney and Malheur counties, Oregon","docAbstract":"Appraisals of the resources of selected management areas in eastern Oregon are being made by the U.S. Bureau of Land Management. To provide needed hydrologic information the Bureau of Land Management requested the U.S. Geological Survey Water Resources Division to inventory ground-water data for the Drewsey Resource Area. Included in this report are well data, drillers ' lithologic logs, hydrographs, a summary of observation-well data, and chemical analyses of ground water. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77741","usgsCitation":"Gonthier, J.B., Collins, C.A., and Anderson, D.B., 1977, Ground-water data for the Drewsey Resource Area, Harney and Malheur counties, Oregon: U.S. Geological Survey Open-File Report 77-741, iv, 28 leaves :ill., maps (1 fold. in envelope) ;27 cm., https://doi.org/10.3133/ofr77741.","productDescription":"iv, 28 leaves :ill., maps (1 fold. in envelope) ;27 cm.","costCenters":[],"links":[{"id":141629,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0741/report-thumb.jpg"},{"id":36796,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0741/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36797,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0741/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1468","contributors":{"authors":[{"text":"Gonthier, Joseph B.","contributorId":74350,"corporation":false,"usgs":true,"family":"Gonthier","given":"Joseph","email":"","middleInitial":"B.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":159239,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Collins, C. A.","contributorId":43731,"corporation":false,"usgs":true,"family":"Collins","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":159237,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Anderson, David B.","contributorId":67511,"corporation":false,"usgs":true,"family":"Anderson","given":"David","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":159238,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9162,"text":"ofr77238 - 1977 - Ground-water levels in observation wells in Oklahoma, 1975","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr77238","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":"77-238","title":"Ground-water levels in observation wells in Oklahoma, 1975","docAbstract":"The objectives of the observation-well program are (1) to provide long-term records of water-level fluctuations in representative wells, (2) to facilitate the prediction of water-level trends and indicate the future availability of ground-water supplies, and (3) to provide information for use in basic research. These selected records serve as a framework to which other types of hydrologic data may be related.\r\nThe stratigraphic nomenclature and age determinations used in this report are those accepted by the Oklahoma Geological Survey and do not necessarily agree with those of the U.S. Geological Survey.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77238","usgsCitation":"Goemaat, R.L., 1977, Ground-water levels in observation wells in Oklahoma, 1975: U.S. Geological Survey Open-File Report 77-238, iv, 35 p. :map ;27 cm.; (39 p. - PGS), https://doi.org/10.3133/ofr77238.","productDescription":"iv, 35 p. :map ;27 cm.; (39 p. - PGS)","costCenters":[],"links":[{"id":142652,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6675eb","contributors":{"authors":[{"text":"Goemaat, Robert L.","contributorId":64256,"corporation":false,"usgs":true,"family":"Goemaat","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":159206,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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