Water-level, springflow, and streamflow data were used to develop simple and multiple linear-regression equations for use in estimating water levels in wells and the flow of three major springs in the Edwards aquifer in the eastern San Antonio area. The equations provide daily, monthly, and annual estimates that compare very favorably with observed data. Analyses of geologic and hydrologic data indicate that the water discharged by the major springs is supplied primarily by regional underflow from the west and southwest and by local recharge in the infiltration area in northern Bexar, Comal, and Hays Counties.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr76393","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Edwards Underground Water District, the Texas Water Development Board, and the city of San Antonio","usgsCitation":"Puente, C., 1976, Statistical analysis of water-level, springflow, and streamflow data for the Edwards Aquifer in south-central Texas: U.S. Geological Survey Open-File Report 76-393, 58 p., https://doi.org/10.3133/ofr76393.","productDescription":"58 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":143382,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0393/report-thumb.jpg"},{"id":92271,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0393/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -99.0,29.0 ], [ -99.0,30.5 ], [ -97.75,30.5 ], [ -97.75,29.0 ], [ -99.0,29.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699ea9","contributors":{"authors":[{"text":"Puente, Celso","contributorId":36140,"corporation":false,"usgs":true,"family":"Puente","given":"Celso","email":"","affiliations":[],"preferred":false,"id":161912,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11054,"text":"ofr75624 - 1976 - Streamflow in the Lake Ontario drainage basin, New York part, 1972-73","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr75624","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"75-624","title":"Streamflow in the Lake Ontario drainage basin, New York part, 1972-73","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr75624","usgsCitation":"Schultz, G.K., 1976, Streamflow in the Lake Ontario drainage basin, New York part, 1972-73: U.S. Geological Survey Open-File Report 75-624, 48 p. :ill., maps ;27 cm.; 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All references to reports of the Geological Survey, to most reports of the U.S. Bureau of Mines, and to most published reports of the State of Alaska Division of Geological and Geophysical Surveys and its predecessor State and Territorial agencies released before January 1, 1975, are summarized. An unpublished manuscript report of the Alaska Territorial Department of Mines (Reed, 1938) is included; references to it are summarized in greater detail than those to the kinds of reports listed above. Certain, mainly statistical, reports such as the annual Minerals Yearbook of the U.S. Bureau of Mines and the biennial and annual reports of the State of Alaska Division of Geological and Geophysical Surveys and its predecessor State and Territorial agencies are not included.
This report is divided into three parts: a section made up of summaries of references arranged alphabetically first by quadrangle and second by occurrence name; a section that lists synonyms for names in the first section, claim names, and the names of operators and owners of mines and prospects; and a section that lists, by author, all references summarized in the first section.
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Jr.","contributorId":107275,"corporation":false,"usgs":true,"family":"Edelen","given":"George","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":237151,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":48303,"text":"ofr76684 - 1976 - Digital-computer model of the sandstone aquifer in southeastern Wisconsin","interactions":[],"lastModifiedDate":"2014-07-15T10:30:22","indexId":"ofr76684","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-684","title":"Digital-computer model of the sandstone aquifer in southeastern Wisconsin","docAbstract":"No abstract available.","language":"English","publisher":"Southeastern Wisconsin Regional Planning Commission","publisherLocation":"Waukesha, WI","doi":"10.3133/ofr76684","usgsCitation":"Young, H.L., 1976, Digital-computer model of the sandstone aquifer in southeastern Wisconsin: U.S. Geological Survey Open-File Report 76-684, vi, 98 p., https://doi.org/10.3133/ofr76684.","productDescription":"vi, 98 p.","numberOfPages":"104","costCenters":[],"links":[{"id":171264,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64aed8","contributors":{"authors":[{"text":"Young, Harley L.","contributorId":31454,"corporation":false,"usgs":true,"family":"Young","given":"Harley","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":237148,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":21516,"text":"ofr76304 - 1976 - Some electrical and magnetic studies of Kilauea Iki lava lake, Hawaii","interactions":[],"lastModifiedDate":"2012-02-02T00:07:44","indexId":"ofr76304","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-304","title":"Some electrical and magnetic studies of Kilauea Iki lava lake, Hawaii","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76304","usgsCitation":"Zablocki, C.J., 1976, Some electrical and magnetic studies of Kilauea Iki lava lake, Hawaii: U.S. Geological Survey Open-File Report 76-304, 19 leaves :ill. ;28 cm., https://doi.org/10.3133/ofr76304.","productDescription":"19 leaves :ill. ;28 cm.","costCenters":[],"links":[{"id":153104,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699ed5","contributors":{"authors":[{"text":"Zablocki, Charles J.","contributorId":48961,"corporation":false,"usgs":true,"family":"Zablocki","given":"Charles","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":184577,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44023,"text":"ofr76464 - 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Generally, water from wells south of Valdosta is high in hydrogen sulfide; water from wells north of the city is high in color. Water with high sulfate is likely to be a problem in wells deeper than about 540 ft. Heavy pumpage concentrated in a small area may cause high-sulfate water to migrate vertically upward into shallower wells. 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The reach studied is in Butte and Glenn Counties, California, and extends northward from the present east-bank Sacramento River Flood Control Project levee near Glenn upstream to the Ord Ferry gaging station near Ordbend. There is a west-bank levee throughout the study reach. Flows analyzed range from 11,500 to 265,000 cfs. Computed water-surface elevations are based on topography obtained during September through November 1974. The present Sacramento River Flood Control Project levees at the downstream end of the study reach near Glenn are designed to contain flows up to 150,000 cfs. Water-surface elevations computed for flows of this magnitude are about 6 to 8 ft below the top of the existing west-bank levee throughout the study reach. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76526","usgsCitation":"Simpson, R., 1976, Determination of channel capacity of the Sacramento River between Ordbend and Glenn, Butte and Glenn counties, California: U.S. Geological Survey Open-File Report 76-526, iv, 48 p. :ill., maps ;27 cm.; (51 p. - PGS), https://doi.org/10.3133/ofr76526.","productDescription":"iv, 48 p. :ill., maps ;27 cm.; (51 p. - PGS)","costCenters":[],"links":[{"id":144752,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667861","contributors":{"authors":[{"text":"Simpson, R.G.","contributorId":16016,"corporation":false,"usgs":true,"family":"Simpson","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":162654,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10818,"text":"ofr76715 - 1976 - Diurnal effects on the helium concentration in soil-gas and near-surface atmosphere","interactions":[],"lastModifiedDate":"2012-02-02T00:06:33","indexId":"ofr76715","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-715","title":"Diurnal effects on the helium concentration in soil-gas and near-surface atmosphere","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76715","usgsCitation":"Reimer, G.M., Roberts, A.A., and Denton, E., 1976, Diurnal effects on the helium concentration in soil-gas and near-surface atmosphere: U.S. Geological Survey Open-File Report 76-715, i, 6 leaves ;27 cm.; (9 p. - PGS), https://doi.org/10.3133/ofr76715.","productDescription":"i, 6 leaves ;27 cm.; (9 p. - PGS)","costCenters":[],"links":[{"id":144004,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63d8da","contributors":{"authors":[{"text":"Reimer, G. 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More than two-thirds of the batholith and the contiguous wallrocks are gneissic, the gneissosity comprising strong cataclasis and mylonitization, penetrative planar and linear structures, and crystallization of muscovite and biotite in the foliation planes. New radiometric ages indicate the deformation followed the crystallization of the batholith so closely that the K-Ar dating method cannot distinguish a difference, whereas previously published ages from the gneisses indicate a short time interval between the two events.
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SUPERMOCK simulates the ground-water system and DATE and HYDROG aid in the display of computed data. During calibration, DATE is especially useful because it has the optional feature of comparing computed data with observed data. Although the programs can be run independently, experience dictates that for best results the three should be run as steps in the same job. English units of inches, feet, and days are used in each of the programs. The units for any parameters not given in the text are clearly specified in the instructions for input to the individual programs. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76792","usgsCitation":"Reed, J., Bedinger, M.S., and Terry, J.E., 1976, Simulation procedure for modeling transient water table and artesian stress and response: U.S. Geological Survey Open-File Report 76-792, 173 p., 7 tables :ill. 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