No abstract available.
","language":"English","publisher":"Springer","doi":"10.1007/BF01611096","usgsCitation":"Geiger, J.G., and Buikema, A., 1981, Oxygen consumption and filtering rate of Daphnia pulex after exposure to water-soluble fractions of naphthaline, phenanthrene, No. 2 fuel oil, and coal-tar creosote: Bulletin of Environmental Contamination and Toxicology, v. 27, no. 6, p. 783-789, https://doi.org/10.1007/BF01611096.","productDescription":"7 p.","startPage":"783","endPage":"789","numberOfPages":"7","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132143,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a0a6","contributors":{"authors":[{"text":"Geiger, J. G.","contributorId":29340,"corporation":false,"usgs":true,"family":"Geiger","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":319413,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buikema, A.L. Jr.","contributorId":43717,"corporation":false,"usgs":true,"family":"Buikema","given":"A.L.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":319414,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1000236,"text":"1000236 - 1981 - Loss of nitrogenous dissolved organic matter from small lakes","interactions":[],"lastModifiedDate":"2016-04-01T10:00:29","indexId":"1000236","displayToPublicDate":"1981-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2299,"text":"Journal of Freshwater Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Loss of nitrogenous dissolved organic matter from small lakes","docAbstract":"To determine how much organic nitrogen is lost from lakes during winter by natural processes, we collected water in fall and winter from six small lakes (area, 5-822 hectares) and separated organic matter dissolved in the water with n-butanol into three fractions--yellow organic acids, a white precipitate, and aqueous (nonextractable) organic matter. The nitrogen content of each fraction was measured by ultraviolet photolysis. About 25-30% of the yellow acid and white precipitate fractions were lost from the water column in each of the lakes during winter. More than 80% of the organic nitrogen dissolved in the lake water samples was found in the aqueous fraction. We believe the white precipitate is part of the humin material in lake waters because it was relatively insoluble in acidic and alkaline solutions.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02705060.1981.9664031","usgsCitation":"Manny, B.A., and Otsuki, A., 1981, Loss of nitrogenous dissolved organic matter from small lakes: Journal of Freshwater Ecology, v. 1, no. 2, p. 193-202, https://doi.org/10.1080/02705060.1981.9664031.","productDescription":"10 p.","startPage":"193","endPage":"202","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133218,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"2","noUsgsAuthors":false,"publicationDate":"2011-01-06","publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640d2e","contributors":{"authors":[{"text":"Manny, Bruce A. 0000-0002-4074-9329 bmanny@usgs.gov","orcid":"https://orcid.org/0000-0002-4074-9329","contributorId":3699,"corporation":false,"usgs":true,"family":"Manny","given":"Bruce","email":"bmanny@usgs.gov","middleInitial":"A.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":true,"id":308268,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Otsuki, Akira","contributorId":57026,"corporation":false,"usgs":true,"family":"Otsuki","given":"Akira","email":"","affiliations":[],"preferred":false,"id":308269,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011839,"text":"70011839 - 1981 - Comparison of automated segmented-flow and discrete analyzers for the determination of nutrients in water","interactions":[],"lastModifiedDate":"2013-03-13T20:38:31","indexId":"70011839","displayToPublicDate":"1981-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Comparison of automated segmented-flow and discrete analyzers for the determination of nutrients in water","docAbstract":"Water samples with specific conductances ranging from 66 to 6950 ??mho/cm at 25 ??C were analyzed for ammonia-N (NH3-N), nitrate plus nitrite-N (NO3 + NO2-N), nitrite-N (NO2-N), and phosphate-P (PO4-P) by using both a \"segmented-flow\" analyzer and a \"discrete\" analyzer. Plots of the discrete vs. the segmented-flow results showed linear correlation coefficients of 0.9980 for NH3-N, 0.9997 for NO3 + NO2-N, 0.9998 for NO2-N, and 0.9950 for PO4-P. The significances of the slope and the y intercept of each plot are discussed in terms of possible biases which may exist between the two systems. Data concerning precision and accuracy for both analyzers are presented. For the four analytes, the rate of sample analysis was 60 samples per hour on the discrete analyzer and 40 samples per hour on the segmented-flow analyzer. ?? 1981 American Chemical Society.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Science and Technology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Chemical Society","doi":"10.1021/es00088a012","issn":"0013936X","usgsCitation":"Marti, V., and Hale, D., 1981, Comparison of automated segmented-flow and discrete analyzers for the determination of nutrients in water: Environmental Science & Technology, v. 15, no. 6, p. 711-713, https://doi.org/10.1021/es00088a012.","startPage":"711","endPage":"713","numberOfPages":"3","costCenters":[],"links":[{"id":221548,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269295,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/es00088a012"}],"volume":"15","issue":"6","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059f851e4b0c8380cd4d004","contributors":{"authors":[{"text":"Marti, V.C.","contributorId":57596,"corporation":false,"usgs":true,"family":"Marti","given":"V.C.","email":"","affiliations":[],"preferred":false,"id":362081,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hale, D.R.","contributorId":15346,"corporation":false,"usgs":true,"family":"Hale","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":362080,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011837,"text":"70011837 - 1981 - Anomalous chemical changes in well waters and possible relation to earthquakes","interactions":[],"lastModifiedDate":"2024-02-15T01:19:19.730362","indexId":"70011837","displayToPublicDate":"1981-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Anomalous chemical changes in well waters and possible relation to earthquakes","docAbstract":"Water level, temperature, salinity, electric conductivity, and pH have been measured periodically for several years at three water wells located along a 17-km segment of the San Andreas fault between San Juan Bautista and Cienega Winery in central California. Water samples were collected at the same time for subsequent chemical analyses in the laboratory. Some sudden large changes in salinity and conductivity were recorded in early March 1980 at the two wells near San Juan Bautista. These changes coincided approximately with the beginning of an episode of increased local seismicity, including a magnitude 4.8 earthquake on April 13. Analyses of water samples revealed corresponding changes in ion concentrations, especially of Na+, Ca++, Mg++, SO4−−, HCO3−, F−, and Cl−. The observed changes may be the result of mixing of waters from different aquifers through cracks developed in the water barriers by a possible crustal strain episode that may have occurred in the study area.
Many recently developed watershed models utilize accumulation and washoff equations to simulate the quality of runofffrom urban impervious areas. These models often have been calibrated by trial and error and with little understanding of model sensitivity to the various parameters. Methodologies for estimating best fit values of the washoff parameters commonly used in these models have been presented previously. In this paper, parameter identification techniques for estimating the accumulation parameters from measured runoff quality data are presented along with a sensitivity analysis of the parameters. Results from application of the techniques and the sensitivity analysis suggest a need for data quantifying the magnitude and identifying the shape of constituent accumulation curves. An exponential accumulation curve is shown to be more general than the linear accumulation curves used in most urban runoff quality models. When determining accumulation rates, attention needs to be given to the effects of residual amounts of constituents remaining after the previous period of storm runoff or street sweeping.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR017i006p01657","usgsCitation":"Alley, W.M., and Smith, P.E., 1981, Estimation of accumulation parameters for urban runoff quality modeling: Water Resources Research, v. 17, no. 6, p. 1657-1664, https://doi.org/10.1029/WR017i006p01657.","productDescription":"8 p.","startPage":"1657","endPage":"1664","costCenters":[],"links":[{"id":221694,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"6","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"505a0b6fe4b0c8380cd5270c","contributors":{"authors":[{"text":"Alley, William M. walley@usgs.gov","contributorId":1661,"corporation":false,"usgs":true,"family":"Alley","given":"William","email":"walley@usgs.gov","middleInitial":"M.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":false,"id":361944,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Peter E.","contributorId":50609,"corporation":false,"usgs":true,"family":"Smith","given":"Peter","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":361945,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1001552,"text":"1001552 - 1981 - Breeding birds on waterfowl production areas in northeastern North Dakota","interactions":[],"lastModifiedDate":"2017-10-11T11:28:51","indexId":"1001552","displayToPublicDate":"1981-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3111,"text":"Prairie Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Breeding birds on waterfowl production areas in northeastern North Dakota","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Prairie Naturalist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Duebbert, H., 1981, Breeding birds on waterfowl production areas in northeastern North Dakota: Prairie Naturalist, v. 13, no. 1, p. 19-22.","productDescription":"4 p.","startPage":"19","endPage":"22","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":130479,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -98.975830078125,\n 48.10743118848039\n ],\n [\n -97.42675781249999,\n 48.10743118848039\n ],\n [\n -97.42675781249999,\n 48.96579381461063\n ],\n [\n -98.975830078125,\n 48.96579381461063\n ],\n [\n -98.975830078125,\n 48.10743118848039\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"13","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb477","contributors":{"authors":[{"text":"Duebbert, Harold F.","contributorId":11544,"corporation":false,"usgs":true,"family":"Duebbert","given":"Harold F.","affiliations":[],"preferred":false,"id":311242,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70012048,"text":"70012048 - 1981 - Flow through fractures","interactions":[],"lastModifiedDate":"2018-02-05T12:34:17","indexId":"70012048","displayToPublicDate":"1981-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Flow through fractures","docAbstract":"Flow through fractures is often idealized as flow between two parallel plates (plane Poiseuille flow). The opening or aperture between parallel plates is unambiguous and its relation to flowrate is well known. However, fractures in rock have uneven walls and a variable aperture. A model for flow in a fracture is proposed wherein the fracture is represented by a set of parallel plate openings with different apertures. The model leads to a modified Poiseuille equation for flow which includes an aperture frequency distribution for the fracture. Any arbitrary aperture distribution can be used; in order to simplify computation and demonstrate the properties of the model a log normal form of distribution is assumed. Even when an analytical form of the distribution is assumed, two parameters, rather than a single value representing ‘aperture size’ are required to determine flowrate. Models of aperture change for a fracture undergoing compression (fracture walls deforming) and extension (fracture walls separating) are developed which constrain the additional parameter and allow calculation of flowrate as a function of mean aperture. The theoretical relationships developed between mean aperture and flowrate can be used to interpret published laboratory data for single fractures.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR017i001p00191","usgsCitation":"Neuzil, C., and Tracy, J.V., 1981, Flow through fractures: Water Resources Research, v. 17, no. 1, p. 191-199, https://doi.org/10.1029/WR017i001p00191.","productDescription":"9 p.","startPage":"191","endPage":"199","costCenters":[],"links":[{"id":222694,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"505a1255e4b0c8380cd5427d","contributors":{"authors":[{"text":"Neuzil, C. E. 0000-0003-2022-4055","orcid":"https://orcid.org/0000-0003-2022-4055","contributorId":81078,"corporation":false,"usgs":true,"family":"Neuzil","given":"C. E.","affiliations":[],"preferred":false,"id":362611,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tracy, James V.","contributorId":52585,"corporation":false,"usgs":true,"family":"Tracy","given":"James","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":362610,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70195646,"text":"70195646 - 1981 - Waterfowl diseases - Changing perspectives for the future","interactions":[],"lastModifiedDate":"2018-02-26T09:12:39","indexId":"70195646","displayToPublicDate":"1981-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Waterfowl diseases - Changing perspectives for the future","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the fourth international waterfowl symposium","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Fourth international waterfowl symposium","conferenceDate":"January 30 - February 1, 1981","conferenceLocation":"New Orleans, LA","language":"English","publisher":"Ducks Unlimited","usgsCitation":"Friend, M., 1981, Waterfowl diseases - Changing perspectives for the future, in Proceedings of the fourth international waterfowl symposium, New Orleans, LA, January 30 - February 1, 1981, p. 189-196.","productDescription":"8 p.","startPage":"189","endPage":"196","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":351990,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff44cee4b0da30c1bfdb34","contributors":{"authors":[{"text":"Friend, Milton 0000-0002-2882-3629","orcid":"https://orcid.org/0000-0002-2882-3629","contributorId":31332,"corporation":false,"usgs":true,"family":"Friend","given":"Milton","email":"","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":729546,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70140589,"text":"70140589 - 1981 - Evaluation of Landsat Multispectral Scanner data for mapping vegetated soil landscapes","interactions":[],"lastModifiedDate":"2019-12-10T14:47:26","indexId":"70140589","displayToPublicDate":"1981-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3420,"text":"Soil Science Society of America Journal","active":true,"publicationSubtype":{"id":10}},"title":"Evaluation of Landsat Multispectral Scanner data for mapping vegetated soil landscapes","docAbstract":"Landsat multispectral scanner data for Brazos County, Texas, were evaluated in terms of effectiveness for classifying soils on vegetated landscapes at three times during the year: a time of normally adequate soil water, a time of expected soil water deficit, and a time when soil water is normally being replenished. Six test sites were used to evaluate LARSYS supervised and unsupervised classification of vegetated soil landscapes. Open grassland soils were best separated in the fall during a period when soil moisture was being replenished after the summer period of soil water deficit. Woodland soils were separated by Landsat data in late spring when adequate moisture was available. However, a high degree of accuracy was not achieved using Landsat for separating soil map units. Accurate separation of soil mapping units on vegetated landscapes was not possible during late summer when soil water was deficient. Selected soil properties important to plant growth were separable on the test sites using June and October Landsat data. Particle size and soil moisture regime were separated at both dates. Soils with argillic horizons were separated from soils without argillic horizons.
","language":"English","publisher":"Soil Science Society of America","doi":"10.2136/sssaj1981.03615995004500010020x","usgsCitation":"Thompson, D.R., Haas, R.H., and Milford, M.H., 1981, Evaluation of Landsat Multispectral Scanner data for mapping vegetated soil landscapes: Soil Science Society of America Journal, v. 45, no. 1, p. 91-95, https://doi.org/10.2136/sssaj1981.03615995004500010020x.","productDescription":"5 p.","startPage":"91","endPage":"95","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":297874,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","county":"Brazos 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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811158","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Aeromagnetic map of the Ugashik-Karluk area, Alaska: U.S. Geological Survey Open-File Report 81-1158, 1 Plate: 27.66 x 24.55 inches, https://doi.org/10.3133/ofr811158.","productDescription":"1 Plate: 27.66 x 24.55 inches","costCenters":[],"links":[{"id":135542,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79817,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1158/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":108099,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11899.htm","linkFileType":{"id":5,"text":"html"},"description":"11899"}],"country":"United States","state":"Alaska","otherGeospatial":"Ugashik-Karluk area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -158,\n 58\n ],\n [\n -158,\n 57\n ],\n [\n -155.333,\n 57\n ],\n [\n -155.333,\n 58\n ],\n [\n -158,\n 58\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae7e4b07f02db68c2fa","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530810,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":42013,"text":"ofr81327 - 1981 - Altitude of water table, Biscayne aquifer, Dade County, Florida, October 1978","interactions":[],"lastModifiedDate":"2023-03-21T20:11:14.04505","indexId":"ofr81327","displayToPublicDate":"1981-01-01T00:00:00","publicationYear":"1981","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":"81-327","title":"Altitude of water table, Biscayne aquifer, Dade County, Florida, October 1978","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81327","usgsCitation":"Swayze, L.J., 1981, Altitude of water table, Biscayne aquifer, Dade County, Florida, October 1978: U.S. Geological Survey Open-File Report 81-327, 1 Plate: 35.48 x 44.44 inches, https://doi.org/10.3133/ofr81327.","productDescription":"1 Plate: 35.48 x 44.44 inches","costCenters":[],"links":[{"id":169576,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414495,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75476.htm","linkFileType":{"id":5,"text":"html"}},{"id":79768,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0327/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","county":"Dade County","otherGeospatial":"Biscayne aquifer","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -80.875,\n 25.9833\n ],\n [\n -80.875,\n 25.25\n ],\n [\n -80.125,\n 25.25\n ],\n [\n -80.125,\n 25.9833\n ],\n [\n -80.875,\n 25.9833\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686a1d","contributors":{"authors":[{"text":"Swayze, L. J.","contributorId":25572,"corporation":false,"usgs":true,"family":"Swayze","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":225838,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011775,"text":"70011775 - 1981 - Variations in stable- isotope ratios of ground waters in seismically active regions of California","interactions":[],"lastModifiedDate":"2024-02-15T01:20:20.009952","indexId":"70011775","displayToPublicDate":"1981-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Variations in stable- isotope ratios of ground waters in seismically active regions of California","docAbstract":"Measurements of D and 18O concentrations of ground waters in seismically active regions are potentially useful in earthquake prediction and in elucidating mechanisms operative during earthquakes. Principles of this method are discussed and some preliminary data regarding a magnitude 5.7 earthquake at the Oroville Dam in 1975 and a series of events near San Juan Bautista in 1980 are presented to support the utility of such measurements. After earthquakes, the D content of nearby ground waters increased by several permil while the 18O content remained constant. This increase implies that H2O may have either decomposed or reacted to form molecular H2 at depth. It is emphasized that many areas must be investigated for these effects in order to find a sufficient number of \"sensitive\" water wells and springs to permit a truly effective program of earthquake research.
Quantitative calculations for the effect of a fault creep event on observations of changes in water level in wells provide an approach to the tectonic interpretation of these phenomena. For the pore pressure field associated with an idealized creep event having an exponential displacement versus time curve, an analytic expression has been obtained in terms of exponential-integral functions. The pore pressure versus time curves for observation points near the fault are pulselike; a sharp pressure increase (or decrease, depending on the direction of propagation) is followed by more gradual decay to the normal level after the creep event. The time function of the water level change may be obtained by applying the filter—derived by A. G. Johnson and others to determine the influence of atmospheric pressure on water level—to the analytic pore pressure versus time curves. The resulting water level curves show a fairly rapid increase (or decrease) and then a very gradual return to normal. The results of this analytic model do not reproduce the steplike changes in water level observed by Johnson and others. If the procedure used to obtain the water level from the pore pressure is correct, these results suggest that steplike changes in water level are not produced by smoothly propagating creep events but by creep events that propagate discontinously, by changes in the bulk properties of the region around the well, or by some other mechanism. In addition, simplistic calculations show that significant pressure field variations and water level changes near the surface may be expected to accompany a propagating creep event on a buried fault. Water level changes of as much as several meters may be expected at the surface for a creep event having a dislocation amplitude of l m on a semi-infinite dislocation surface extending downward from a depth of 10 km and propagating horizontally at a rate of 10 km/day. The maximum near-surface effect should be observed at a horizontal distance from the fault about equal to the depth of the top of the dislocation surface. These results are consistent with the observations made in China of large water level changes preceding large earthquakes, if some sort of aseismic creep event at depth precedes these earthquakes.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB086iB10p09259","issn":"01480227","usgsCitation":"Wesson, R.L., 1981, Interpretation of changes in water level accompanying fault creep and implications for earthquake prediction: Journal of Geophysical Research Solid Earth, v. 86, no. B10, p. 9259-9267, https://doi.org/10.1029/JB086iB10p09259.","productDescription":"9 p.","startPage":"9259","endPage":"9267","numberOfPages":"9","costCenters":[],"links":[{"id":221266,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"86","issue":"B10","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505a3d6ae4b0c8380cd6355f","contributors":{"authors":[{"text":"Wesson, R. L.","contributorId":51752,"corporation":false,"usgs":true,"family":"Wesson","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":362379,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":56849,"text":"wdrMDDE791 - 1980 - Water resources data for Maryland and Delaware, water year 1979","interactions":[],"lastModifiedDate":"2021-01-22T19:30:50.015756","indexId":"wdrMDDE791","displayToPublicDate":"2021-01-22T14:45:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MD-DE-79-1","displayTitle":"Water Resources Data Maryland and Delaware, Water Year 1979","title":"Water resources data for Maryland and Delaware, water year 1979","docAbstract":"No abstract available.
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\"}}]}","contact":"","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f434e","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532936,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70180029,"text":"70180029 - 1980 - Developing a state water plan: Ground-water conditions in Utah, spring of 1980","interactions":[],"lastModifiedDate":"2017-01-23T13:15:36","indexId":"70180029","displayToPublicDate":"2017-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":110,"text":"Cooperative Investigations Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"19","title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1980","docAbstract":"This is the seventeenth in a series of annual reports that describe ground-water conditions in Utah. Reports in this series, prepared cooperatively by the U.S. Geological Survey and the Utah Division of Water Resources, provide data to enable interested parties to keep abreast of changing ground-water conditions.
This report, like the others in the series, contains information on well construction, ground-water withdrawals, water-level changes, and related changes in precipitation and streamflow. Supplementary data such as graphs showing chemical quality of water and maps showing water-table configuration are included in reports of this series only for those years or areas for which applicable data are available and are important to a discussion of changing ground-water conditions.
This report includes individual discussions of selected major areas of ground-water withdrawal in the State for the calendar year 1979. Water-level fluctuations, however, are described for the period spring 1979 to spring 1980. Much of the data used in this report were collected by the U.S. Geological Survey in cooperation with the Division of Water Rights, Utah Department of Natural Resources.
","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Resources","publisherLocation":"Salt Lake City","collaboration":"Prepared in cooperation with the State of Utah","usgsCitation":"Herbert, L.R., Garrett, R., Gerhart, E., Steiger, J.I., Appel, C.L., Jensen, V., Enright, M., Dubois, S., Emett, D.C., Guhman, A., Neff, L., Sultz, L., and Sandberg, G.W., 1980, Developing a state water plan: Ground-water conditions in Utah, spring of 1980: Cooperative Investigations Report 19, vi, 72 p.","productDescription":"vi, 72 p.","numberOfPages":"78","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333725,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333722,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-185"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5887248ae4b08aa8f945abf4","contributors":{"authors":[{"text":"Herbert, L. 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Discussions of the related subjects of geology, hydrology, and chemical quality of the water are included in many of the reports. The reports were, for the most part, prepared by personnel assigned to the Water Resources Division, Utah District, in cooperation with State and local agencies.
","language":"English","publisher":"Utah Department of Natural Resources","publisherLocation":"Salt Lake City, UT","usgsCitation":"1980, Bibliography of U.S. Geological Survey water-resources reports for Utah: Utah Division of Water Rights Information Bulletin 27, 75 p.","productDescription":"75 p.","numberOfPages":"76","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333490,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333486,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=21-4-530"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5881def9e4b01192927d9fef","contributors":{"compilers":[{"text":"LaPray, Barbara A.","contributorId":178483,"corporation":false,"usgs":false,"family":"LaPray","given":"Barbara","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":659122,"contributorType":{"id":3,"text":"Compilers"},"rank":1},{"text":"Hamblin, Linda S.","contributorId":52202,"corporation":false,"usgs":true,"family":"Hamblin","given":"Linda","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":659123,"contributorType":{"id":3,"text":"Compilers"},"rank":2}]}} ,{"id":70179787,"text":"70179787 - 1980 - Utah water use data: Public water supplies, 1960-1978","interactions":[],"lastModifiedDate":"2017-01-19T09:25:40","indexId":"70179787","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5267,"text":"Utah Division of Water Rights Water-Use Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"1","title":"Utah water use data: Public water supplies, 1960-1978","docAbstract":"This report was prepared as a part of the Statewide cooperative water-resources investigation program administered jointly by the Utah Department of Natural Resources, Division of Water Rights and the United States Geological Survey. The program is conducted to meet the water administration and water-resources data needs of the State, as well as the water information needs of many units of government and the general public.
","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the State of Utah, Division of Water Rights","usgsCitation":"Mills, D., Jibson, R., Riley, J., Hooper, D., and Schwarting, R., 1980, Utah water use data: Public water supplies, 1960-1978: Utah Division of Water Rights Water-Use Report 1, vi, 250 p.","productDescription":"vi, 250 p.","numberOfPages":"260","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333282,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333281,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=21-5-020"}],"country":"United 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Water from three principal aquifers supplies most municipal, industrial, irrigation, residential, and farm water needs in these counties. These are the sand-and-gravel, Niagara, and sandstone aquifers. As much as 15 gallons per minute can be obtained from wells almost everywhere in these counties. Yields of 500 to 1,000 gallons per minute are available from the sand-and-gravel aquifer in parts of Washington County. The Niagara aquifer underlies most of the area and can yield as much as 500 gallons per minute in most of Ozaukee and eastern Washington Counties. It yields less than 100 gallons per minute in some areas, notably eastern Mequon in Ozaukee County and parts of western Washington County. The sandstone aquifer underlies the entire area and generally can yield more than 1,000 gallons per minute to wells. However, yields of less than 500 gallons per minute are common in southwestern Washington County, where the aquifer is thinnest.
","language":"English","publisher":"Wisconsin Geological & Natural History Survey","collaboration":"Prepared in cooperation with Wisconsin Geological and Natural History Survey","usgsCitation":"Young, H.L., and Batten, W.G., 1980, Ground-water resources and geology of Washington and Ozaukee Counties, Wisconsin: Wisconsin Geological & Natural History Survey Information Circular 38, iv, 38 p.","productDescription":"iv, 38 p.","numberOfPages":"43","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308477,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":350390,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://wgnhs.uwex.edu/pubs/download_ic38/"}],"country":"United States","state":"Wisconsin","county":"Ozaukee County, Washington County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-88.0402,43.5423],[-87.9215,43.5436],[-87.8009,43.543],[-87.7933,43.5434],[-87.7933,43.542],[-87.7945,43.5202],[-87.7935,43.5075],[-87.794,43.4883],[-87.798,43.4788],[-87.8086,43.4594],[-87.8184,43.4445],[-87.8334,43.4269],[-87.845,43.4152],[-87.8541,43.4044],[-87.8631,43.3946],[-87.8651,43.39],[-87.8665,43.3859],[-87.8647,43.3836],[-87.8641,43.3818],[-87.866,43.3809],[-87.8691,43.3814],[-87.8717,43.3787],[-87.8743,43.3742],[-87.875,43.3728],[-87.8784,43.3606],[-87.8819,43.3479],[-87.8828,43.3365],[-87.8862,43.3257],[-87.8864,43.3179],[-87.889,43.3125],[-87.8891,43.3075],[-87.8918,43.3007],[-87.8977,43.2903],[-87.9017,43.2826],[-87.9056,43.2754],[-87.909,43.2659],[-87.911,43.2577],[-87.9112,43.2523],[-87.9114,43.2436],[-87.9096,43.2372],[-87.9085,43.2327],[-87.9067,43.2276],[-87.9049,43.2226],[-87.9019,43.2176],[-87.8988,43.2153],[-87.8977,43.2102],[-87.8978,43.2057],[-87.8979,43.2007],[-87.8967,43.197],[-87.8949,43.1947],[-87.9433,43.1949],[-87.9873,43.1945],[-88.0639,43.194],[-88.1827,43.1948],[-88.3027,43.1954],[-88.4183,43.1964],[-88.4187,43.2856],[-88.4187,43.3703],[-88.4017,43.3701],[-88.4008,43.4598],[-88.4008,43.5435],[-88.2808,43.5429],[-88.1608,43.5431],[-88.0402,43.5423]]]},\"properties\":{\"name\":\"Ozaukee\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56051ec9e4b058f706e512d9","contributors":{"authors":[{"text":"Young, H. L.","contributorId":23922,"corporation":false,"usgs":true,"family":"Young","given":"H.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":573247,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Batten, W. G.","contributorId":89504,"corporation":false,"usgs":true,"family":"Batten","given":"W.","email":"","middleInitial":"G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":573248,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70118039,"text":"70118039 - 1980 - Modern sedimentary facies of the open Pacific coast and Pleistocene analogs from Montery Bay, California","interactions":[],"lastModifiedDate":"2014-07-25T10:30:01","indexId":"70118039","displayToPublicDate":"2013-07-25T10:07:00","publicationYear":"1980","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Modern sedimentary facies of the open Pacific coast and Pleistocene analogs from Montery Bay, California","docAbstract":"Depositional processes and sedimentary structures of wave-dominated Pacific coastal environments vary systematically with water depth. The depth-limited open-coast facies identifiable by their sedimentary structures are the inner shelf, barred or nonbarred nearshore, beach, and coastal dune facies. These facies are most commonly preserved in shallowing-upward progradational sequences.
\nThe vertical sequence of sedimentary structures preserved in marine terrace deposits in the northern Monterey Bay region is very similar to that predicted on the basis of the modern facies. Few marine sediments deposited during the marine transgression that accompanied rising sea level were preserved. Most of the the marine and eolian sediments form a progradational sequence deposited mainly during intervals of falling sea level. In contrast, the sediments that form the adjacent fluvial terraces were deposited mainly during periods of rising sea level and became entrenched during the subsequent lowering of sea level. In combination, these fluvial, marine, and eolian deposits provide a record of a complete eustatic cycle.
\nThe recognition of the role of changing sea level in controlling patterns of coastal sedimentation and landform development during the Quaternary allows the development of a generalized model for Quaternary sedimentation along a wave-dominated coastline. The application of this model has aided in the interpretation of older Pleistocene sediments in the region (e.g. the Aromas Sand). It also has resulted in the recognition of at least eleven glacio-eustatic cycles preserved in the stratigraphic record of the Monterey Bay area during the Quaternary.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Quaternary depositional environments of the Pacific Coast : Pacific Coast Paleogeography Symposium 4","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"Society of Economic Paleontologists and Mineralogists","publisherLocation":"Los Angeles, CA","usgsCitation":"Dupre, W., Clifton, H., Hunter, R.E., and Field, M.E., 1980, Modern sedimentary facies of the open Pacific coast and Pleistocene analogs from Montery Bay, California, in Quaternary depositional environments of the Pacific Coast : Pacific Coast Paleogeography Symposium 4, p. 105-120.","productDescription":"16 p.","startPage":"105","endPage":"120","costCenters":[],"links":[{"id":290982,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":290981,"type":{"id":15,"text":"Index Page"},"url":"https://archives.datapages.com/data/pac_sepm/028/028001/pdfs/105.htm"}],"country":"United States","state":"California","otherGeospatial":"Monterey Bay","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.145263,36.629278 ], [ -122.145263,36.941309 ], [ -121.827806,36.941309 ], [ -121.827806,36.629278 ], [ -122.145263,36.629278 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ff9244e4b0824b2d16eebb","contributors":{"editors":[{"text":"Field, Michael E. mfield@usgs.gov","contributorId":2101,"corporation":false,"usgs":true,"family":"Field","given":"Michael","email":"mfield@usgs.gov","middleInitial":"E.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":509919,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"et al.","contributorId":128369,"corporation":true,"usgs":false,"organization":"et al.","id":536672,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Dupre, W.R.","contributorId":57540,"corporation":false,"usgs":true,"family":"Dupre","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":496169,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clifton, H.E.","contributorId":44151,"corporation":false,"usgs":true,"family":"Clifton","given":"H.E.","affiliations":[],"preferred":false,"id":496167,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hunter, R. E.","contributorId":48148,"corporation":false,"usgs":true,"family":"Hunter","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":496168,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Field, Michael E. mfield@usgs.gov","contributorId":2101,"corporation":false,"usgs":true,"family":"Field","given":"Michael","email":"mfield@usgs.gov","middleInitial":"E.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":496166,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70047613,"text":"70047613 - 1980 - Ground-water data for the Salt Basin, Eagle Flat, Red Light Draw, Green River Valley and Presidio Bolson in westernmost Texas","interactions":[{"subject":{"id":17206,"text":"ofr77575 - 1978 - Ground-water data for the Salt Basin, Eagle Flat, Red Light Draw, Green River Valley, and Presidio Bolson in westernmost Texas","indexId":"ofr77575","publicationYear":"1978","noYear":false,"title":"Ground-water data for the Salt Basin, Eagle Flat, Red Light Draw, Green River Valley, and Presidio Bolson in westernmost Texas"},"predicate":"SUPERSEDED_BY","object":{"id":70047613,"text":"70047613 - 1980 - Ground-water data for the Salt Basin, Eagle Flat, Red Light Draw, Green River Valley and Presidio Bolson in westernmost Texas","indexId":"70047613","publicationYear":"1980","noYear":false,"title":"Ground-water data for the Salt Basin, Eagle Flat, Red Light Draw, Green River Valley and Presidio Bolson in westernmost Texas"},"id":1}],"lastModifiedDate":"2016-08-12T15:43:59","indexId":"70047613","displayToPublicDate":"2013-01-01T14:23:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":133,"text":"Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"259","title":"Ground-water data for the Salt Basin, Eagle Flat, Red Light Draw, Green River Valley and Presidio Bolson in westernmost Texas","docAbstract":"From October 1971 through October 1974. the U.S. Geological Survey collected ground-water data in the basins in Texas west of the Pecos River drainage area and northwest of the Big Bend country. The basins included are, from east to west: The Presidio Bolson; the Salt Basin; Green River Valley, Eagle Flat, and Red Light Draw. These data, which were collected in cooperation with the Texas Department of Water Resources (formerly Texas Water Development Board), will provide information for a continuing assessment of water availability within the State.
","language":"English","publisher":"Texas Department of Water Resources","publisherLocation":"San Antonio, TX","collaboration":"This report was prepared by the U.S. Geological Survey under cooperative agreement with the Texas Department of Water Resources","usgsCitation":"White, D.E., Gates, J., Smith, J.T., and Fry, B.J., 1980, Ground-water data for the Salt Basin, Eagle Flat, Red Light Draw, Green River Valley and Presidio Bolson in westernmost Texas: Report 259, iii, 97 p.","productDescription":"iii, 97 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":276609,"type":{"id":15,"text":"Index Page"},"url":"https://www.twdb.texas.gov/publications/reports/numbered_reports/doc/R259/R259.pdf"},{"id":276610,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047613.png"}],"country":"United States","state":"Texas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.65,25.84 ], [ -106.65,36.5 ], [ -93.51,36.5 ], [ -93.51,25.84 ], [ -106.65,25.84 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520ca6e5e4b081fa6136d3ea","contributors":{"authors":[{"text":"White, Donald E.","contributorId":76787,"corporation":false,"usgs":true,"family":"White","given":"Donald","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":482533,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gates, Joseph S.","contributorId":21647,"corporation":false,"usgs":true,"family":"Gates","given":"Joseph S.","affiliations":[],"preferred":false,"id":482530,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, James T.","contributorId":22670,"corporation":false,"usgs":true,"family":"Smith","given":"James","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":482531,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fry, Bonnie J.","contributorId":74285,"corporation":false,"usgs":true,"family":"Fry","given":"Bonnie","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":482532,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70047612,"text":"70047612 - 1980 - Development of Ground Water in the Houston District, Texas, 1970-1974","interactions":[{"subject":{"id":8945,"text":"ofr77413 - 1977 - Development of ground water in the Houston District, Texas, 1970-74","indexId":"ofr77413","publicationYear":"1977","noYear":false,"title":"Development of ground water in the Houston District, Texas, 1970-74"},"predicate":"SUPERSEDED_BY","object":{"id":70047612,"text":"70047612 - 1980 - Development of Ground Water in the Houston District, Texas, 1970-1974","indexId":"70047612","publicationYear":"1980","noYear":false,"title":"Development of Ground Water in the Houston District, Texas, 1970-1974"},"id":1}],"lastModifiedDate":"2016-08-12T15:41:55","indexId":"70047612","displayToPublicDate":"2013-01-01T14:03:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":133,"text":"Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"241","title":"Development of Ground Water in the Houston District, Texas, 1970-1974","docAbstract":"Total withdrawals of ground water in the Houston district increased 9 percent from about 488 million gallons per day (21.4 cubic meters per second) in 1970 to about 532 million gallons per day (23.3 cubic meters per second) in 1974. The average annual rate of increase from 1960 to 1969 was about 6.3 percent. During 1970-74, increases in pumpage occurred in the Houston, Katy, and NASA areas; decreases occurred in the Pasadena and Alta Lorna areas; and the pumpage in the Baytown-La Porte and Texas City areas remained almost constant.
","language":"English","publisher":"Texas Water Development Board","publisherLocation":"San Antonio, TX","collaboration":"This report was prepared by the U.S. Geological Survey under cooperative agreement with the Texas Department of Water Resources and the Cities of Houston and Galveston","usgsCitation":"Gabrysch, R., 1980, Development of Ground Water in the Houston District, Texas, 1970-1974: Report 241, v, 49 p.","productDescription":"v, 49 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":276608,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047612.png"},{"id":276607,"type":{"id":15,"text":"Index Page"},"url":"https://www.twdb.texas.gov/publications/reports/numbered_reports/doc/R241/R241.pdf"}],"country":"United States","state":"Texas","county":"Houston County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -95.72,30.7 ], [ -95.72,31.98 ], [ -94.44,31.98 ], [ -94.44,30.7 ], [ -95.72,30.7 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520ca6e3e4b081fa6136d3d4","contributors":{"authors":[{"text":"Gabrysch, R.K.","contributorId":105691,"corporation":false,"usgs":true,"family":"Gabrysch","given":"R.K.","affiliations":[],"preferred":false,"id":482529,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70047454,"text":"70047454 - 1980 - Summary groundwater resources of Centre County, Pennsylvania","interactions":[{"subject":{"id":48452,"text":"ofr791531 - 1979 - Summary of ground-water resources of Centre County, Pennsylvania","indexId":"ofr791531","publicationYear":"1979","noYear":false,"title":"Summary of ground-water resources of Centre County, Pennsylvania"},"predicate":"SUPERSEDED_BY","object":{"id":70047454,"text":"70047454 - 1980 - Summary groundwater resources of Centre County, Pennsylvania","indexId":"70047454","publicationYear":"1980","noYear":false,"title":"Summary groundwater resources of Centre County, Pennsylvania"},"id":1}],"lastModifiedDate":"2013-08-06T13:23:01","indexId":"70047454","displayToPublicDate":"2013-01-01T13:14:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":143,"text":"Water Resource Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"48","title":"Summary groundwater resources of Centre County, Pennsylvania","docAbstract":"The northwest third of Centre County lies in the Appalachian Plateaus physiographic province. The higher altitudes are underlain by the Conemaugh, Allegheny, and Pottsville Groups, which consist of sandstone, shale, and thin limestone and coal beds. The average yield of nondomestic wells in the Allegheny Group is 20 gpm (gallons per minute) and that in the Pottsville Group 100 gpm. Water from wells in these groups commonly has a high concentration of iron. Most of the rest of the Appalachian Plateaus province is underlain by the Burgoon Sandstone. The Burgoon yields soft water, and the average yield of nondomestic wells is 70 gpm.","language":"English","publisher":"Pennsylvania Geological Survey","publisherLocation":"Harrisburg, PA","collaboration":"Prepared by the U. S. Geological Survey, Water Resources Division, in cooperation with the Pennsylvania Geological Survey","usgsCitation":"Wood, C.R., 1980, Summary groundwater resources of Centre County, Pennsylvania: Water Resource Report 48, vii, 60 p.","productDescription":"vii, 60 p.","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":276126,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047454.PNG"},{"id":276125,"type":{"id":11,"text":"Document"},"url":"https://www.dcnr.state.pa.us/cs/groups/public/documents/document/dcnr_016331.zip"}],"country":"United States","state":"Pennsylvania","county":"Centre County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -78.3767,40.6916 ], [ -78.3767,41.2528 ], [ -77.1438,41.2528 ], [ -77.1438,40.6916 ], [ -78.3767,40.6916 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52021ae8e4b0e21cafa49c90","contributors":{"authors":[{"text":"Wood, Charles R.","contributorId":30259,"corporation":false,"usgs":true,"family":"Wood","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":482071,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70043962,"text":"70043962 - 1980 - Seepage study of the West Side and West Canals, Box Elder County, Utah","interactions":[{"subject":{"id":8475,"text":"ofr791489 - 1979 - Seepage study of the West Side and West canals, Box Elder County, Utah","indexId":"ofr791489","publicationYear":"1979","noYear":false,"title":"Seepage study of the West Side and West canals, Box Elder County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043962,"text":"70043962 - 1980 - Seepage study of the West Side and West Canals, Box Elder County, Utah","indexId":"70043962","publicationYear":"1980","noYear":false,"title":"Seepage study of the West Side and West Canals, Box Elder County, Utah"},"id":1}],"lastModifiedDate":"2016-12-12T15:03:04","indexId":"70043962","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"67","title":"Seepage study of the West Side and West Canals, Box Elder County, Utah","docAbstract":"A study of the gains or losses of the West Side and West Canals from Cutler Reservoir to near Penrose, Box Elder County, Utah, was made to aid in water allocation for the canal system. Four sets of seepage measurements made in 1978 were used in the analysis. Adjustments for fluctuations in flow in the canals were made from information obtained from water-stage recorders operated at selected locations along the canals during the time of each seepage run.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with The Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Cruff, R., 1980, Seepage study of the West Side and West Canals, Box Elder County, Utah: Technical Publication 67, iv, 38 p.","productDescription":"iv, 38 p.","numberOfPages":"42","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":268164,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331978,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-620"},{"id":268163,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009t.pdf"}],"country":"United States","state":"Utah","county":"Box Elder County","otherGeospatial":"West Side Canal, West Canal","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.642822265625,\n 41.50857729743935\n ],\n [\n -112.642822265625,\n 41.97582726102573\n ],\n [\n -112.00561523437499,\n 41.97582726102573\n ],\n [\n -112.00561523437499,\n 41.50857729743935\n ],\n [\n -112.642822265625,\n 41.50857729743935\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"512b44bde4b0523e997a81bb","contributors":{"authors":[{"text":"Cruff, R.W.","contributorId":77510,"corporation":false,"usgs":true,"family":"Cruff","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":474554,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70044398,"text":"70044398 - 1980 - Chemical quality of water in abandoned zinc mines in northeastern Oklahoma and southeastern Kansas","interactions":[{"subject":{"id":10704,"text":"ofr78294 - 1978 - Chemical quality of water in abandoned zinc mines in northeastern Oklahoma and southeastern Kansas","indexId":"ofr78294","publicationYear":"1978","noYear":false,"title":"Chemical quality of water in abandoned zinc mines in northeastern Oklahoma and southeastern Kansas"},"predicate":"SUPERSEDED_BY","object":{"id":70044398,"text":"70044398 - 1980 - Chemical quality of water in abandoned zinc mines in northeastern Oklahoma and southeastern Kansas","indexId":"70044398","publicationYear":"1980","noYear":false,"title":"Chemical quality of water in abandoned zinc mines in northeastern Oklahoma and southeastern Kansas"},"id":1}],"lastModifiedDate":"2013-03-05T09:02:17","indexId":"70044398","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":244,"text":"Circular","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"82","title":"Chemical quality of water in abandoned zinc mines in northeastern Oklahoma and southeastern Kansas","docAbstract":"Onsite measurements of pH, specific conductance, and water temperature show that water in seven mine shafts in northeastern Oklahoma and southeastern Kansas is stratified. With increasing sampling depth, specific conductance and water temperature tend to increase, and pH tends to decrease. Concentrations of dissolved solids and chemical constituents in mine-shaft water, such as total and dissolved metals and dissolved sulfate also increase with depth. The apparently unstable condition created by cooler, denser water overlying warmer, less dense water is offset by the greater density of the lower water strata due to higher dissolved solids content.","language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Norman, OK","collaboration":"Prepared by the United States Geological Survey in cooperation with the Oklahoma Geological Survey","usgsCitation":"Playton, S.J., Davis, R.E., and McClaflin, R.G., 1980, Chemical quality of water in abandoned zinc mines in northeastern Oklahoma and southeastern Kansas: Circular 82, iv, 49 p.","productDescription":"iv, 49 p.","startPage":"i","endPage":"49","numberOfPages":"53","costCenters":[],"links":[{"id":268739,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268738,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/circular82.pdf"}],"country":"United States","state":"Oklahoma","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,33.62 ], [ -103.0,37.0 ], [ -94.43,37.0 ], [ -94.43,33.62 ], [ -103.0,33.62 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"513721f4e4b02ab8869bffbf","contributors":{"authors":[{"text":"Playton, Stephen J.","contributorId":87548,"corporation":false,"usgs":true,"family":"Playton","given":"Stephen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":475512,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, Robert E.","contributorId":10403,"corporation":false,"usgs":true,"family":"Davis","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":475510,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McClaflin, Roger G.","contributorId":50157,"corporation":false,"usgs":true,"family":"McClaflin","given":"Roger","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":475511,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70046184,"text":"70046184 - 1980 - Estimated inflow and evaporation for Great Salt Lake, Utah, 1931-76, with revised model for evaluating the effects of dikes on the water and salt balance of the lake: Comprehensive water planning program","interactions":[{"subject":{"id":11535,"text":"ofr79258 - 1978 - Estimated inflow and evaporation for Great Salt Lake, Utah, 1931-76, with revised model for evaluating the effects of dikes on the water and salt balance of the lake","indexId":"ofr79258","publicationYear":"1978","noYear":false,"title":"Estimated inflow and evaporation for Great Salt Lake, Utah, 1931-76, with revised model for evaluating the effects of dikes on the water and salt balance of the lake"},"predicate":"SUPERSEDED_BY","object":{"id":70046184,"text":"70046184 - 1980 - Estimated inflow and evaporation for Great Salt Lake, Utah, 1931-76, with revised model for evaluating the effects of dikes on the water and salt balance of the lake: Comprehensive water planning program","indexId":"70046184","publicationYear":"1980","noYear":false,"title":"Estimated inflow and evaporation for Great Salt Lake, Utah, 1931-76, with revised model for evaluating the effects of dikes on the water and salt balance of the lake: Comprehensive water planning program"},"id":1}],"lastModifiedDate":"2017-09-20T14:03:10","indexId":"70046184","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":247,"text":"Cooperative Investigations Report","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"20","title":"Estimated inflow and evaporation for Great Salt Lake, Utah, 1931-76, with revised model for evaluating the effects of dikes on the water and salt balance of the lake: Comprehensive water planning program","docAbstract":"No abstract available.