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Southern Great Basin from Mexican Border to Mono Lake Basin, and Pacific Slope Basins from Tijuana River to Santa Maria River","docAbstract":"Water resources data for the 1986 water year for California consist of records of stage, discharge, and water quality of streams; stage and contents in lakes and reservoirs; and water levels and water quality in wells. Volume 1 contains discharge records for 144 gaging stations; stage and contents for 15 lakes and reservoirs; watet quality for 21 streams. Also included are crest-stage partial-record stations, 3 miscellaneous measurement sites, and 5 water-quality partial-record stations. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in California.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA861","collaboration":"Prepared in cooperation with the California Department of Water Resources and with other agencies","usgsCitation":"Bowers, J.C., McConaughy, C., Polinoski, K.G., and Smith, G., 1988, Water Resources Data for California, Water Year 1986. Volume 1. Southern Great Basin from Mexican Border to Mono Lake Basin, and Pacific Slope Basins from Tijuana River to Santa Maria River (Legacy Report): U.S. Geological Survey Water Data Report CA-86-1, x, 301 p., https://doi.org/10.3133/wdrCA861.","productDescription":"x, 301 p.","temporalStart":"1985-10-01","temporalEnd":"1986-09-30","costCenters":[{"id":631,"text":"Water Resources Division-California District","active":false,"usgs":true}],"links":[{"id":257705,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_CA_86_1.jpg"},{"id":182182,"rank":0,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1986/ca-86/WDR-1986-vol1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Southern Great Basin;Mono Lake Basin;Pacific Slope Basins;Tijuana River;Santa Maria River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.4,32.5 ], [ -124.4,42 ], [ -114.13333333333334,42 ], [ -114.13333333333334,32.5 ], [ -124.4,32.5 ] ] ] } } ] }","edition":"Legacy Report","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd14c","contributors":{"authors":[{"text":"Bowers, J. 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Southern Central Valley Basins and The Great Basin from Walker River to Truckee River","interactions":[],"lastModifiedDate":"2012-08-31T17:16:24","indexId":"wdrCA873","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"CA-87-3","title":"Water Resources Data for California, Water Year 1987. Volume 3. Southern Central Valley Basins and The Great Basin from Walker River to Truckee River","docAbstract":"Water resources data for the 1987 water year for California consist of records of stage, discharge, and water quality of streams; stage and contents in lakes and reservoirs; and water levels and water quality in wells. Volume 3 contains discharge records for 177 gaging stations; stage and contents for 46 lakes and reservoirs; and water quality for 29 stations. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in California.","language":"English","publisher":"U.S. Geological Survey, Water Resources Division","publisherLocation":"Sacramento, CA","doi":"10.3133/wdrCA873","collaboration":"Prepared in cooperation with the California Department of Water Resources and with other agencies","usgsCitation":"Hunter, T., Mullen, J., and Simpson, R., 1988, Water Resources Data for California, Water Year 1987. Volume 3. Southern Central Valley Basins and The Great Basin from Walker River to Truckee River (Legacy Report): U.S. Geological Survey Water Data Report CA-87-3, xi, 392 p., https://doi.org/10.3133/wdrCA873.","productDescription":"xi, 392 p.","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":181223,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_ca_87_3.jpg"},{"id":259982,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1987/ca-87/WDR-1987-vol3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.83333333333333,34.833333333333336 ], [ -122.83333333333333,38.583333333333336 ], [ -118,38.583333333333336 ], [ -118,34.833333333333336 ], [ -122.83333333333333,34.833333333333336 ] ] ] } } ] }","edition":"Legacy Report","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd1be","contributors":{"authors":[{"text":"Hunter, T.C.","contributorId":81172,"corporation":false,"usgs":true,"family":"Hunter","given":"T.C.","email":"","affiliations":[],"preferred":false,"id":257388,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mullen, J.R.","contributorId":92683,"corporation":false,"usgs":true,"family":"Mullen","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":257389,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Simpson, R.G.","contributorId":16016,"corporation":false,"usgs":true,"family":"Simpson","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":257387,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":21443,"text":"ofr88309 - 1988 - Quality of ground water in shallow wells in agricultural areas of Haywood, Shelby, Lake, and Obion counties, Tennessee, January and February 1988","interactions":[],"lastModifiedDate":"2012-02-02T00:07:48","indexId":"ofr88309","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-309","title":"Quality of ground water in shallow wells in agricultural areas of Haywood, Shelby, Lake, and Obion counties, Tennessee, January and February 1988","docAbstract":"Three areas with sparse data on the impact of agricultural chemicals on groundwater quality in the state of Tennessee were chosen for sampling groundwater for nitrogen species and pesticides. These sites, located in Haywood, Shelby, and Lake Counties, are all areas of high intensity agriculture. Because of the importance of the surficial alluvial aquifer to the domestic supply in West Tennessee, shallow wells at each site were sampled. Two sampling events were scheduled, in the winter and in the spring, to establish the difference between background and effected contaminant levels. Preliminary results from the first sampling event indicate a range of nitrite plus nitrate as nitrogen concentrations from less than 0.1 to 7.8 milligrams per liter. The results from triazine analyses show concentrations below the detection limit. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88309","usgsCitation":"Withington, D., 1988, Quality of ground water in shallow wells in agricultural areas of Haywood, Shelby, Lake, and Obion counties, Tennessee, January and February 1988: U.S. Geological Survey Open-File Report 88-309, iii, 12 p. :maps ;28 cm., https://doi.org/10.3133/ofr88309.","productDescription":"iii, 12 p. :maps ;28 cm.","costCenters":[],"links":[{"id":154136,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1182,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr_88-309","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a72e4b07f02db642cb5","contributors":{"authors":[{"text":"Withington, D.B.","contributorId":53830,"corporation":false,"usgs":true,"family":"Withington","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":184438,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":20367,"text":"ofr88342 - 1988 - January 1988 water levels, and data related to water-level changes, western and south-central Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:07:53","indexId":"ofr88342","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-342","title":"January 1988 water levels, and data related to water-level changes, western and south-central Kansas","docAbstract":"Hydrologic data related to water level measurements made in observation wells in western and south-central Kansas are listed. The measurements were made in midwinter when pumping was minimal and water levels had recovered, for the most part, from the effects of pumping during the previous irrigation season. Annual hydrologic data are provided for relating water level changes from a ' base year ' (predevelopment), a reference year of abnormally large amounts of rainfall and minimum pumpage (1966 or 1974), and each of 7 consecutive years of measurement (1982-88). The ' base year ' is designated as 1940 for the southwestern area, 1944 for the south-central area, and 1950 for the northwestern, west central, and Equus beds areas. Data also are provided for relating the mean annual water level changes, saturated thicknesses of the water-bearing deposits, and percentage changes in saturated thickness. Groundwater levels measured in about 1,360 wells completed in the High Plains aquifer of western and south-central Kansas had a mean net decline of 0.1 ft during 1987 compared to a 0.6 ft mean decline during 1986. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88342","usgsCitation":"Pabst, B., 1988, January 1988 water levels, and data related to water-level changes, western and south-central Kansas: U.S. Geological Survey Open-File Report 88-342, iv, 158 p. ;28 cm., https://doi.org/10.3133/ofr88342.","productDescription":"iv, 158 p. ;28 cm.","costCenters":[],"links":[{"id":154699,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0342/report-thumb.jpg"},{"id":49900,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0342/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db666fbc","contributors":{"authors":[{"text":"Pabst, B.J.","contributorId":42617,"corporation":false,"usgs":true,"family":"Pabst","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":182528,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25848,"text":"wri884233 - 1988 - Water quality of Lake Austin and Town Lake, Austin, Texas","interactions":[],"lastModifiedDate":"2016-08-10T15:48:48","indexId":"wri884233","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4233","title":"Water quality of Lake Austin and Town Lake, Austin, Texas","docAbstract":"Lake Austin and Town Lake are located on the Colorado River in Travis County, central Texas, and serve as a source of water for municipal and industrial water supplies, electrical-power generation, and recreation for more than 500,000 people in the Austin metropolitan area. Lake Austin, located immediately downstream of Lake Travis, extends for more than 20 miles into the western edge of the city of Austin. Town Lake extends through the downtown area of the city of Austin for nearly 6 miles where the Colorado River is impounded by Longhorn Dam.
\nMany of the detrimental effects of impoundment of water in a lake or reservoir are related to thermal stratification, which generally does not occur in Lake Austin or in Town Lake. The largest detected difference in vertical temperature was 6.5 degrees Celsius in Lake Austin and 3.5 degrees Celsius in Town Lake. The small vertical temperature variations in both lakes can be attributed to shallow depths in the lakes and to the short retention times of water in the lakes during the summer months.
\nLarge vertical dissolved-oxygen gradients were not detected in Lake Austin and Town Lake. Average dissolved-oxygen concentrations for Lake Austin at site Ac, a deep site (about 50 feet) at the dam, differ by about 2.5 milligrams per liter from surface to bottom during the summer. At site Ac on Town Lake, average dissolved-oxygen concentrations differ by about 1 milligram per liter from surface to bottom. The largest areal variations in dissolved oxygen generally occur in Lake Austin during the summer. Water released to Lake Austin during the summer is from below the thermocline in Lake Travis, and consequently, dissolved-oxygen concentrations generally are small. For example, in August 1984, dissolved-oxygen concentrations in Lake Austin increased from 2.8 milligrams per liter in the headwaters to slightly greater than 7.0 milligrams per liter approximately 14 miles downstream. This increase in dissolved oxygen was caused by reaeration from the atmosphere and from photosynthetic production of oxygen by aquatic plants.
\nDissolved trace-element data collected from Lake Austin and Town Lake indicate that with the exception of iron, manganese, and mercury, none of the dissolved trace elements analyzed for exceeded either the primary maximum contaminant level or secondary maximum contaminant level set by the U.S. Environmental Protection Agency. Average concentrations of dissolved iron and dissolved manganese in water collected near the bottom of Lake Austin did not exceed 40 and 50 micrograms per liter, respectively.
\nLittle seasonal or areal variation was noted in nitrogen concentrations in Lake Austin or Town Lake. Organic nitrogen is the predominant nitrogen species in both lakes. Stormwater runoff had little effect on nitrogen concentrations in Lake Austin. Nitrogen concentrations in Town Lake were slightly larger following periods of runoff. Total nitrogen concentrations in Town Lake following periods of runoff often exceed 1.0 milligram per liter.
\nTotal phosphorus concentrations are small in Lake Austin and Town Lake. About 95 percent of the total phosphorus concentrations measured in Lake Austin and about 81 percent of the total phosphorus concentrations measured in Town Lake were less than 0.03 milligram per liter. Total phosphorus concentrations are largest in Town Lake following periods of runoff.
\nDissolved-solids concentrations ranged from 240 to 340 milligrams per liter in Lake Austin and from 170 to 360 milligrams per liter in Town Lake. The smallest concentrations of dissolved solids in Town Lake occurred following periods of runoff. During periods of no runoff, dissolved-solids concentrations in Town Lake ranged from 240 to 360 milligrams per liter, which was very similar to the range in Lake Austin.
\nDensities of feca1-coliform bacteria in Lake Austin ranged from less than 1 to 600 colonies per 100 milliliters, and densities of fecal-streptococci bacteria ranged from less than 1 to 340 colonies per 100 milliliters. Densities of fecal-coliform bacteria in Town Lake ranged from 4 to 14,000 colonies per 100 milliliters, and densities of fecal-streptococci bacteria ranged from less than 1 to 15,000 colonies per 100 milliliters. The largest densities of both bacteria in Town Lake occurred following runoff.
\nLittle or no effect of stormwater runoff on temperature, dissolved oxygen, or trace elements was detected in either Lake Austin or Town Lake. Increased concentrations of total nitrogen and phosphorus were detected in Town Lake, but not in Lake Austin following runoff. A decrease in concentrations of dissolved solids and major ions occurred in Town Lake, but not in Lake Austin, following runoff. Densities of fecal-coliform and fecal-streptococci bacteria were larger in Lake Austin and Town Lake following runoff, but significantly larger increases were noted in Town Lake.
\nWater-quality data collected from Lake Austin and Town Lake, following runoff, generally were not adequate to fully determine the effects of runoff on the lakes. Data collection should not to be limited to fixed-station sampling following runoff, and both lakes need to be sampled simultaneously as soon as possible following significant precipitation.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri884233","usgsCitation":"Andrews, F.L., Wells, F.C., Shelby, W.J., and McPherson, E., 1988, Water quality of Lake Austin and Town Lake, Austin, Texas: U.S. Geological Survey Water-Resources Investigations Report 88-4233, vii, 322 p., https://doi.org/10.3133/wri884233.","productDescription":"vii, 322 p.","numberOfPages":"329","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":158245,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4233/report-thumb.jpg"},{"id":54592,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4233/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4dac","contributors":{"authors":[{"text":"Andrews, Freeman L.","contributorId":91486,"corporation":false,"usgs":true,"family":"Andrews","given":"Freeman","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":195328,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wells, Frank C.","contributorId":80664,"corporation":false,"usgs":true,"family":"Wells","given":"Frank","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":645150,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shelby, Wanda J.","contributorId":173579,"corporation":false,"usgs":false,"family":"Shelby","given":"Wanda","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":645151,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McPherson, Emma","contributorId":85629,"corporation":false,"usgs":true,"family":"McPherson","given":"Emma","email":"","affiliations":[],"preferred":false,"id":645152,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":20744,"text":"ofr88433 - 1988 - Gravity data for the state of Nevada on magnetic tape","interactions":[],"lastModifiedDate":"2012-02-02T00:07:40","indexId":"ofr88433","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-433","title":"Gravity data for the state of Nevada on magnetic tape","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr88433","usgsCitation":"Saltus, R.W., 1988, Gravity data for the state of Nevada on magnetic tape: U.S. Geological Survey Open-File Report 88-433, 20 p. :ill. ;28 cm., https://doi.org/10.3133/ofr88433.","productDescription":"20 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":152364,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0433/report-thumb.jpg"},{"id":50299,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0433/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae200","contributors":{"authors":[{"text":"Saltus, R. W.","contributorId":85588,"corporation":false,"usgs":true,"family":"Saltus","given":"R.","middleInitial":"W.","affiliations":[],"preferred":false,"id":183170,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":21284,"text":"ofr87538 - 1988 - Water-quality data from the observation-well network in Illinois, 1985-87","interactions":[],"lastModifiedDate":"2012-02-02T00:07:58","indexId":"ofr87538","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"87-538","title":"Water-quality data from the observation-well network in Illinois, 1985-87","docAbstract":"The report presents water-quality and well-site information for public water-supply wells in Illinois. These wells were sampled during the period January 1985 through June 1987 as part of an ongoing cooperative ground-water observation network in the State. Water-quality data are tabulated for physical parameters, nutrients, common constituents, metals, phenols, cyanide, and volative organic compounds. A subnetwork of wells also have data on several pesticides and herbicides. Some well-site information is also presented in this report.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87538","usgsCitation":"Voelker, D.C., Oberg, D., and Grober, M., 1988, Water-quality data from the observation-well network in Illinois, 1985-87: U.S. Geological Survey Open-File Report 87-538, iv, 725 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr87538.","productDescription":"iv, 725 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":155198,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0538/report-thumb.jpg"},{"id":50835,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0538/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e5761","contributors":{"authors":[{"text":"Voelker, D. C.","contributorId":36572,"corporation":false,"usgs":true,"family":"Voelker","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":184142,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oberg, D.J.","contributorId":6087,"corporation":false,"usgs":true,"family":"Oberg","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":184141,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grober, M.J.","contributorId":95908,"corporation":false,"usgs":true,"family":"Grober","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":184143,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":25859,"text":"wri874199 - 1988 - Water resources of Borrego Valley and vicinity, San Diego County, California: Phase 2 - Development of a ground-water flow model","interactions":[],"lastModifiedDate":"2021-11-26T21:41:48.419377","indexId":"wri874199","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4199","title":"Water resources of Borrego Valley and vicinity, San Diego County, California: Phase 2 - Development of a ground-water flow model","docAbstract":"Because of the imbalance between recharge and pumpage, groundwater levels declined as much as 100 ft in some areas of Borrego Valley, California during drinking 1945-80. As an aid to analyzing the effects of pumping on the groundwater system, a three-dimensional finite-element groundwater flow model was developed. The model was calibrated for both steady-state (1945) and transient-state (1946-79) conditions. For the steady-state calibration, hydraulic conductivities of the three aquifers were varied within reasonable limits to obtain an acceptable match between measured and computed hydraulic heads. Recharge from streamflow infiltration (4,800 acre-ft/yr) was balanced by computed evapotranspiration (3,900 acre-ft/yr) and computed subsurface outflow from the model area (930 acre-ft/yr). For the transient state calibration, the volumes and distribution of net groundwater pumpage were estimated from land-use data and estimates of consumptive use for irrigated crops. The pumpage was assigned to the appropriate nodes in the model for each of seventeen 2-year time steps representing the period 1946-79. The specific yields of the three aquifers were varied within reasonable limits to obtain an acceptable match between measured and computed hydraulic heads. Groundwater pumpage input to the model was compensated by declines in both the computed evapotranspiration and the amount of groundwater in storage. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri874199","usgsCitation":"Mitten, H., Lines, G.C., Berenbrock, C., and Durbin, T.J., 1988, Water resources of Borrego Valley and vicinity, San Diego County, California: Phase 2 - Development of a ground-water flow model: U.S. Geological Survey Water-Resources Investigations Report 87-4199, iv, 27 p., https://doi.org/10.3133/wri874199.","productDescription":"iv, 27 p.","costCenters":[],"links":[{"id":392152,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_46856.htm"},{"id":54611,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4199/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158291,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4199/report-thumb.jpg"}],"country":"United States","state":"California","county":"San Diego County","otherGeospatial":"Borrego Valley and vicinity","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.42,\n 33.1\n ],\n [\n -116.1167,\n 33.1\n ],\n [\n -116.1167,\n 33.3792\n ],\n [\n -116.42,\n 33.3792\n ],\n [\n -116.42,\n 33.1\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f086f","contributors":{"authors":[{"text":"Mitten, H. T.","contributorId":88735,"corporation":false,"usgs":true,"family":"Mitten","given":"H. T.","affiliations":[],"preferred":false,"id":195376,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lines, G. C.","contributorId":30577,"corporation":false,"usgs":true,"family":"Lines","given":"G.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":195373,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Berenbrock, Charles","contributorId":30598,"corporation":false,"usgs":true,"family":"Berenbrock","given":"Charles","email":"","affiliations":[],"preferred":false,"id":195374,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Durbin, T. J.","contributorId":55818,"corporation":false,"usgs":true,"family":"Durbin","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":195375,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":20722,"text":"ofr90123 - 1988 - Data on the distribution and abundance of submersed aquatic vegetation in the tidal Potomac River and transition zone of the Potomac Estuary, Maryland, Virginia, and the District of Columbia, 1988","interactions":[],"lastModifiedDate":"2012-02-02T00:07:48","indexId":"ofr90123","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"90-123","title":"Data on the distribution and abundance of submersed aquatic vegetation in the tidal Potomac River and transition zone of the Potomac Estuary, Maryland, Virginia, and the District of Columbia, 1988","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr90123","usgsCitation":"Rybicki, N.B., and Schening, M., 1988, Data on the distribution and abundance of submersed aquatic vegetation in the tidal Potomac River and transition zone of the Potomac Estuary, Maryland, Virginia, and the District of Columbia, 1988: U.S. Geological Survey Open-File Report 90-123, iv, 19 p. :maps ;28 cm., https://doi.org/10.3133/ofr90123.","productDescription":"iv, 19 p. :maps ;28 cm.","costCenters":[],"links":[{"id":154155,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0123/report-thumb.jpg"},{"id":50279,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0123/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c534","contributors":{"authors":[{"text":"Rybicki, N. B.","contributorId":97504,"corporation":false,"usgs":true,"family":"Rybicki","given":"N.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":183128,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schening, M.R.","contributorId":103707,"corporation":false,"usgs":true,"family":"Schening","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":183129,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":25559,"text":"wri874182 - 1988 - Ground-water resources and simulation of flow in aquifers containing freshwater and seawater, Island County, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:23","indexId":"wri874182","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4182","title":"Ground-water resources and simulation of flow in aquifers containing freshwater and seawater, Island County, Washington","docAbstract":"Aquifers in Island County, Washington, that are intruded by seawater from Puget Sound contain chloride concentrations that exceed 100 mg/L. Chloride concentrations exceeded 100 mg/L in 24 % of the wells that were drilled below sea level and sampled in August 1981, but most of the chloride concentrations did not exceed 1,000 mg/L. Groundwater occurs in glacial deposits that have a maximum thickness of 3,000 ft; the deposits were divided into five aquifers and five confining units. Four overlapping digital models were calibrated, using time-averaged data, to simulate three-dimensional steady flow of fresh groundwater in multiple aquifers containing freshwater and seawater separated by a sharp interface. Model simulations indicate that most of the recharge is discharged from aquifers C and D as springs below sea levels, and only a small fraction of the recharge moves downward below aquifer C. Simulations also indicate that aquifers beneath the islands are not recharged by groundwater that moves from the mainland through aquifers beneath Puget Sound except in the area of northeast Camano Island. Between Whidbey and Camano Islands, the freshwater-seawater interface intersects the bottom of Puget Sound and prevents movement of fresh groundwater between the two islands. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874182","usgsCitation":"Sapik, D.B., Bortleson, G.C., Drost, B., Jones, M., and Prych, E., 1988, Ground-water resources and simulation of flow in aquifers containing freshwater and seawater, Island County, Washington: U.S. Geological Survey Water-Resources Investigations Report 87-4182, vi, 67 p. :maps ;28 cm., https://doi.org/10.3133/wri874182.","productDescription":"vi, 67 p. :maps ;28 cm.","costCenters":[],"links":[{"id":124247,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4182/report-thumb.jpg"},{"id":54282,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4182/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54283,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4182/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54284,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4182/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54285,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4182/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54286,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4182/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6498c3","contributors":{"authors":[{"text":"Sapik, D. B.","contributorId":75932,"corporation":false,"usgs":true,"family":"Sapik","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":194193,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bortleson, Gilbert C.","contributorId":57472,"corporation":false,"usgs":true,"family":"Bortleson","given":"Gilbert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":194192,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Drost, B. W.","contributorId":38526,"corporation":false,"usgs":true,"family":"Drost","given":"B. W.","affiliations":[],"preferred":false,"id":194191,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jones, M. A.","contributorId":37736,"corporation":false,"usgs":true,"family":"Jones","given":"M. A.","affiliations":[],"preferred":false,"id":194190,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Prych, E. A.","contributorId":36163,"corporation":false,"usgs":true,"family":"Prych","given":"E. A.","affiliations":[],"preferred":false,"id":194189,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":25422,"text":"wri884153 - 1988 - A computer program incorporating Pitzer's equations for calculation of geochemical reactions in brines","interactions":[],"lastModifiedDate":"2018-03-21T15:28:14","indexId":"wri884153","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4153","title":"A computer program incorporating Pitzer's equations for calculation of geochemical reactions in brines","docAbstract":"The program named PHRQPITZ is a computer code capable of making geochemical calculations in brines and other electrolyte solutions to high concentrations using the Pitzer virial-coefficient approach for activity-coefficient corrections. Reaction-modeling capabilities include calculation of (1) aqueous speciation and mineral-saturation index, (2) mineral solubility, (3) mixing and titration of aqueous solutions, (4) irreversible reactions and mineral water mass transfer, and (5) reaction path. The computed results for each aqueous solution include the osmotic coefficient, water activity , mineral saturation indices, mean activity coefficients, total activity coefficients, and scale-dependent values of pH, individual-ion activities and individual-ion activity coeffients , and scale-dependent values of pH, individual-ion activities and individual-ion activity coefficients. A data base of Pitzer interaction parameters is provided at 25 C for the system: Na-K-Mg-Ca-H-Cl-SO4-OH-HCO3-CO3-CO2-H2O, and extended to include largely untested literature data for Fe(II), Mn(II), Sr, Ba, Li, and Br with provision for calculations at temperatures other than 25C. An extensive literature review of published Pitzer interaction parameters for many inorganic salts is given. Also described is an interactive input code for PHRQPITZ called PITZINPT. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884153","usgsCitation":"Plummer, N., Parkhurst, D., Fleming, G., and Dunkle, S., 1988, A computer program incorporating Pitzer's equations for calculation of geochemical reactions in brines: U.S. Geological Survey Water-Resources Investigations Report 88-4153, vi, 310 p. :ill. ;28 cm., https://doi.org/10.3133/wri884153.","productDescription":"vi, 310 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":118853,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4153/report-thumb.jpg"},{"id":54141,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4153/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cfe4b07f02db54601a","contributors":{"authors":[{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":193626,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parkhurst, D.L.","contributorId":12474,"corporation":false,"usgs":true,"family":"Parkhurst","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":193625,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fleming, G.W.","contributorId":81937,"corporation":false,"usgs":true,"family":"Fleming","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":193627,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dunkle, S.A.","contributorId":11248,"corporation":false,"usgs":true,"family":"Dunkle","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":193624,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":21513,"text":"ofr88311 - 1988 - Streamflow and water-quality data for three major tributaries to Reelfoot Lake, west Tennessee, October 1987-March 1988","interactions":[],"lastModifiedDate":"2012-02-02T00:07:44","indexId":"ofr88311","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-311","title":"Streamflow and water-quality data for three major tributaries to Reelfoot Lake, west Tennessee, October 1987-March 1988","docAbstract":"Streamflow and water quality data were collected for three major tributaries to Reelfoot Lake, in West Tennessee, for the period October 1987 through March 1988. The data are presented in graphs and tables. Mean daily discharge data were collected at one site each in the drainage basins of North Reelfoot Creek, South Reelfoot Creek, and Running Slough. Daily mean suspended-sediment concentration data were collected at a site in the North Reelfoot Creek basin. Water quality samples were collected during storm events at the same locations that daily mean streamflow data were collected. Water quality samples were analyzed for concentrations of nutrients and triazine herbicides. Water temperature and specific conductance were measured at the time that samples were collected. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88311","usgsCitation":"Yurewicz, M., Carey, W.P., and Garrett, J., 1988, Streamflow and water-quality data for three major tributaries to Reelfoot Lake, west Tennessee, October 1987-March 1988: U.S. Geological Survey Open-File Report 88-311, iii, 20 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr88311.","productDescription":"iii, 20 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":153087,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1216,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr_88-311","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4e72","contributors":{"authors":[{"text":"Yurewicz, M.C.","contributorId":40237,"corporation":false,"usgs":true,"family":"Yurewicz","given":"M.C.","email":"","affiliations":[],"preferred":false,"id":184572,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carey, W. P.","contributorId":105749,"corporation":false,"usgs":true,"family":"Carey","given":"W.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":184574,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Garrett, J.W.","contributorId":87958,"corporation":false,"usgs":true,"family":"Garrett","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":184573,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":26414,"text":"wri884012 - 1988 - Computer-program documentation of an interactive-accounting model to simulate streamflow, water quality, and water-supply operations in a river basin","interactions":[],"lastModifiedDate":"2012-02-02T00:08:33","indexId":"wri884012","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4012","title":"Computer-program documentation of an interactive-accounting model to simulate streamflow, water quality, and water-supply operations in a river basin","docAbstract":"This report describes an interactive-accounting model used to simulate streamflow, chemical-constituent concentrations and loads, and water-supply operations in a river basin. The model uses regression equations to compute flow from incremental (internode) drainage areas. Conservative chemical constituents (typically dissolved solids) also are computed from regression equations. Both flow and water quality loads are accumulated downstream. Optionally, the model simulates the water use and the simplified groundwater systems of a basin. Water users include agricultural, municipal, industrial, and in-stream users , and reservoir operators. Water users list their potential water sources, including direct diversions, groundwater pumpage, interbasin imports, or reservoir releases, in the order in which they will be used. Direct diversions conform to basinwide water law priorities. The model is interactive, and although the input data exist in files, the user can modify them interactively. A major feature of the model is its color-graphic-output options. This report includes a description of the model, organizational charts of subroutines, and examples of the graphics. Detailed format instructions for the input data, example files of input data, definitions of program variables, and listing of the FORTRAN source code are Attachments to the report. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884012","usgsCitation":"Burns, A., 1988, Computer-program documentation of an interactive-accounting model to simulate streamflow, water quality, and water-supply operations in a river basin: U.S. Geological Survey Water-Resources Investigations Report 88-4012, iv, 241 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884012.","productDescription":"iv, 241 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123236,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4012/report-thumb.jpg"},{"id":55209,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4012/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6324","contributors":{"authors":[{"text":"Burns, A.W.","contributorId":65498,"corporation":false,"usgs":true,"family":"Burns","given":"A.W.","email":"","affiliations":[],"preferred":false,"id":196345,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27880,"text":"wri874117 - 1988 - Evaluation of the flood hydrology in the Colorado Front Range using precipitation, streamflow, and paleoflood data for the Big Thompson River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:08:40","indexId":"wri874117","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4117","title":"Evaluation of the flood hydrology in the Colorado Front Range using precipitation, streamflow, and paleoflood data for the Big Thompson River basin","docAbstract":"A multidisciplinary study of precipitation and streamflow data and paleohydrologic studies of channel features was made to analyze the flood hydrology of foothill and mountain streams in the Front Range of Colorado, with emphasis on the Big Thompson River basin, because conventional hydrologic analyses do not adequately characterize the flood hydrology. In the foothills of Colorado, annual floodflows are derived from snowmelt at high elevations in the mountain regions, from rainfall at low elevation in the plains or plateau regions, or from a combination of rain falling on snow or mixed population hydrology. Above approximately 7,500 ft, snowmelt dominates; rain does not contribute to the flood potential. Regional flood-frequency relations were developed and compared with conventional flood-estimating technique results, including an evaluation of the magnitude and frequency of the probable maximum flood. Evaluation of streamflow data and paleoflood investigations provide an alternative for evaluating flood hydrology and the safety of dams. The study indicates the need for additional data collection and research to understand the complexities of the flood hydrology in mountainous regions, especially its effects on flood-plain management and the design of structures in the flood plain. (USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri874117","usgsCitation":"Jarrett, R., and Costa, J.E., 1988, Evaluation of the flood hydrology in the Colorado Front Range using precipitation, streamflow, and paleoflood data for the Big Thompson River basin: U.S. Geological Survey Water-Resources Investigations Report 87-4117, iv, 37 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874117.","productDescription":"iv, 37 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":121816,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4117/report-thumb.jpg"},{"id":56703,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4117/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611b4e","contributors":{"authors":[{"text":"Jarrett, R.D.","contributorId":36551,"corporation":false,"usgs":true,"family":"Jarrett","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":198837,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Costa, J. E.","contributorId":28977,"corporation":false,"usgs":true,"family":"Costa","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":198836,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27980,"text":"wri874232 - 1988 - Economic comparison of two types of automatic water-quality monitors","interactions":[],"lastModifiedDate":"2012-02-02T00:08:42","indexId":"wri874232","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4232","title":"Economic comparison of two types of automatic water-quality monitors","docAbstract":"A comparison of the U.S. Geological Survey's minimonitor system with a self-contained, 'package-sensor' system indicates that the package-sensor system requires less servicing time. The U.S. Geological Survey minimonitor is powered by an external battery and is housed in a weatherproof shelter. This instrument measures temperature, specific conductance, dissolved oxygen, and pH by means of sensors with extension cables having underewater connectors; data are recorder in binary coded decimal form on a 16-channel punched-paper-tape recorder that is housed in a shelter. The packaged-sensor system also measures temperature, specific conductanoe,dissolved oxygen, and pH by means of sensors housed in a package that is submerged in the stream. It has an internal power supply, no moving parts, anf does not require a weatherproof shelter; data are stored in solid-state memory.\r\n\r\nMinimonitors were installed at four sites in Ohio where U.S. Geological Survey flowthrough monitors already were in opertion. Two package-sensor systems also assigned to each site and alternated every 2 weeks. Detailed records were kept of (1) time involved in operation and maintenace of the systems, and (2) equipment problems during the test period, which lasted from October 1985 through September 1986. Equipment costs were not considered in the economic evaluation.\r\n\r\nResults of the comparisons show that the packaged-sensor system required less time to install, operate, and maintain than the minimonitor system.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874232","usgsCitation":"Katzenbach, M., 1988, Economic comparison of two types of automatic water-quality monitors: U.S. Geological Survey Water-Resources Investigations Report 87-4232, iv, 24 p. :ill., map ;28 cm., https://doi.org/10.3133/wri874232.","productDescription":"iv, 24 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":124073,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4232/report-thumb.jpg"},{"id":56796,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4232/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688ca8","contributors":{"authors":[{"text":"Katzenbach, Max","contributorId":43000,"corporation":false,"usgs":true,"family":"Katzenbach","given":"Max","affiliations":[],"preferred":false,"id":199003,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30595,"text":"wri884029 - 1988 - Ground-water conditions in the Anza-Terwilliger area, with emphasis on the Cahuilla Indian Reservation, Riverside County, California, 1973-86","interactions":[],"lastModifiedDate":"2012-02-02T00:09:12","indexId":"wri884029","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4029","title":"Ground-water conditions in the Anza-Terwilliger area, with emphasis on the Cahuilla Indian Reservation, Riverside County, California, 1973-86","docAbstract":"Demand for groundwater in the 96-sq mi Anza Terwilliger area of California has increased in recent years because of population growth and agricultural development. In order to evaluate the potential effects of continued growth and development on the water resources of Cahuilla Indian Reservation, water level, land use, and water quality data were collected and analyzed. Water level measurements indicate that, as in previous years, groundwater normally moves toward streams in Anza and Terwilliger Valleys. However, during the summer, when pumping is at a maximum, groundwater moves toward two areas of groundwater withdrawal in Anza Valley. One area where groundwater levels were lowered extends to the northern boundary of Cahuilla Indian Reservation. Groundwater use during 1986 is estimated at 10,000 acre-ft, 6,000 acre-ft more than in 1973. The water table, however, generally has risen since 1973 due to the wet climatic conditions that generally have prevailed since 1976. Dissolved-solids concentrations during 1984-86 ranged from 184 to 1,320 mg/L. Water from two wells on Cahuilla Indian Reservation had dissolved-solids concentrations higher than the U.S. Environmental Protection Agency recommended limit for drinking water of 500 mg/L. No wells sampled on the reservation contained water with nitrate concentrations above the U.S. Environmental Protection Agency recommended limit of 10 mg/L. The observation-well network was found to be generally adequate, but the addition of one water level and two water quality observation wells would enhance its effectiveness. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884029","usgsCitation":"Woolfenden, L.R., and Bright, D., 1988, Ground-water conditions in the Anza-Terwilliger area, with emphasis on the Cahuilla Indian Reservation, Riverside County, California, 1973-86: U.S. Geological Survey Water-Resources Investigations Report 88-4029, iv, 79 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884029.","productDescription":"iv, 79 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122873,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4029/report-thumb.jpg"},{"id":59353,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4029/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d1af","contributors":{"authors":[{"text":"Woolfenden, L. R. 0000-0003-3500-4709","orcid":"https://orcid.org/0000-0003-3500-4709","contributorId":36945,"corporation":false,"usgs":true,"family":"Woolfenden","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":203511,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bright, D.J.","contributorId":106159,"corporation":false,"usgs":true,"family":"Bright","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":203512,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28468,"text":"wri884109 - 1988 - Quality-assurance data for routine water analysis in the laboratories of the US Geological Survey for water-year 1985","interactions":[],"lastModifiedDate":"2012-02-02T00:08:50","indexId":"wri884109","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4109","title":"Quality-assurance data for routine water analysis in the laboratories of the US Geological Survey for water-year 1985","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884109","usgsCitation":"Lucey, K., and Peart, D., 1988, Quality-assurance data for routine water analysis in the laboratories of the US Geological Survey for water-year 1985: U.S. Geological Survey Water-Resources Investigations Report 88-4109, vii, 121 p. :chiefly ill. ;28 cm., https://doi.org/10.3133/wri884109.","productDescription":"vii, 121 p. :chiefly ill. ;28 cm.","costCenters":[],"links":[{"id":159312,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4109/report-thumb.jpg"},{"id":57270,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4109/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8ae4b07f02db6514f7","contributors":{"authors":[{"text":"Lucey, K.J.","contributorId":70002,"corporation":false,"usgs":true,"family":"Lucey","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":199855,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peart, D.B.","contributorId":45304,"corporation":false,"usgs":true,"family":"Peart","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":199854,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28455,"text":"wri884045 - 1988 - Streamflows in Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:52","indexId":"wri884045","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4045","title":"Streamflows in Wyoming","docAbstract":"A description of the occurrence and availability of surface waters in Wyoming is presented along with explanations of both streamflow-data collection and methods for estimating streamflow characteristics at gaged and ungaged sites. Mountain ranges separate the major drainage basins and have a significant effect on the quantity of precipitation and the volume of runoff that occurs in Wyoming. Perennial streams that originate in the mountains provide the most dependable source of runoff; streams that originate in the plains and deserts generally are intermittent or ephemeral and have extended periods of no flow. Streamflow data for several hundred gaged sites in the State are available for engineering and management purposes. When gaged data are not available, methods for estimating streamflow characteristics are needed. Methods presented in this report for estimating streamflow characteristics have been improved over previous methods through the use of refined analytical techniques and an updated data base. Peak-flow characteristics and mean annual runoff at ungaged sites can be estimated by using regression equations, with either basin characteristics or channel width being independent variables. Log-linear regression equations are used for estimating streamflow characteristics in the mountains; whereas, curvilinear equations of double-exponential form were determined to be more appropriate than log-linear relations for depicting peak flows in the plains and deserts. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884045","usgsCitation":"Lowham, H., 1988, Streamflows in Wyoming: U.S. Geological Survey Water-Resources Investigations Report 88-4045, vi, 84 p. :ill., maps (some col.) ;28 cm., https://doi.org/10.3133/wri884045.","productDescription":"vi, 84 p. :ill., maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":159574,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4045/report-thumb.jpg"},{"id":57256,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4045/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57257,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4045/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4c9b","contributors":{"authors":[{"text":"Lowham, H. W.","contributorId":8111,"corporation":false,"usgs":true,"family":"Lowham","given":"H. W.","affiliations":[],"preferred":false,"id":199828,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27256,"text":"wri884027 - 1988 - Tides, and tidal and residual currents in Suisun and San Pablo bays, California, results of measurements, 1986","interactions":[],"lastModifiedDate":"2021-12-09T22:42:56.670731","indexId":"wri884027","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4027","title":"Tides, and tidal and residual currents in Suisun and San Pablo bays, California, results of measurements, 1986","docAbstract":"Current meter data collected at 11 stations and water level data collected at one station in Suisun and San Pablo Bays, California, in 1986 are compiled in this report. Current-meter measurements include current speed and direction, and water temperature and salinity (computed from temperature and conductivity). For each of the 19 current-meter records, data are presented in two forms. These are: (1) results of harmonic analysis; and (2) plots of tidal current speed and direction versus time and plots of temperature and salinity versus time. Spatial distribution of the properties of tidal currents are given in graphic form. In addition, Eulerian residual currents have been compiled by using a vector-averaging technique. Water level data are presented in the form of a time-series plot and the results of harmonic analysis. (USGS)
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884027","usgsCitation":"Gartner, J.W., and Yost, B.T., 1988, Tides, and tidal and residual currents in Suisun and San Pablo bays, California, results of measurements, 1986: U.S. Geological Survey Water-Resources Investigations Report 88-4027, v, 94 p., https://doi.org/10.3133/wri884027.","productDescription":"v, 94 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true}],"links":[{"id":56122,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4027/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158565,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4027/report-thumb.jpg"},{"id":392713,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_34533.htm"}],"country":"United States","state":"California","otherGeospatial":"Suisun and San Pablo Bays","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.5,\n 37.95\n ],\n [\n -121.833,\n 37.95\n ],\n [\n -121.833,\n 38.167\n ],\n [\n -122.5,\n 38.167\n ],\n [\n -122.5,\n 37.95\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b74e","contributors":{"authors":[{"text":"Gartner, J. W.","contributorId":81903,"corporation":false,"usgs":false,"family":"Gartner","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":197808,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yost, B. T.","contributorId":19178,"corporation":false,"usgs":true,"family":"Yost","given":"B.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":197807,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27164,"text":"wri874260 - 1988 - Hydrogeology and flow of water in a sand and gravel aquifer contaminated by wood-preserving compounds, Pensacola, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:26","indexId":"wri874260","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4260","title":"Hydrogeology and flow of water in a sand and gravel aquifer contaminated by wood-preserving compounds, Pensacola, Florida","docAbstract":"The sand and gravel aquifer in southern Escambia County, Florida , is a typical surficial aquifer composed of quartz sands and gravels interbedded locally with silts and clays. Problems of groundwater contamination from leaking surface impoundments are common in surficial aquifers and are a subject of increasing concern and attention. A potentially widespread contamination problem involves organic chemicals from wood-preserving processes. Because creosote is the most extensively used industrial preservative in the United States, an abandoned wood-treatment plant near Pensacola was chosen for investigation. This report describes the hydrogeology and groundwater flow system of the sand and gravel aquifer near the plant. A three-dimensional simulation of groundwater flow in the aquifer was evaluated under steady-state conditions. The model was calibrated on the basis of observed water levels from January 1986. Calibration criteria included reproducing all water levels within the accuracy of the data (one-half contour interval in most cases). Sensitivity analysis showed that the simulations were most sensitive to recharge and vertical leakance of the confining units between layers 1 and 2, and relatively insensitive to changes in hydraulic conductivity and transmissivity and to other changes in vertical leakance. Applications of the results of the calibrated flow model in evaluation of solute transport may require further discretization of the contaminated area, including more sublayers, than were needed for calibration of the groundwater flow system itself. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874260","usgsCitation":"Franks, B., 1988, Hydrogeology and flow of water in a sand and gravel aquifer contaminated by wood-preserving compounds, Pensacola, Florida: U.S. Geological Survey Water-Resources Investigations Report 87-4260, v, 72 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874260.","productDescription":"v, 72 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123427,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4260/report-thumb.jpg"},{"id":56040,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4260/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ade66","contributors":{"authors":[{"text":"Franks, B.J.","contributorId":107739,"corporation":false,"usgs":true,"family":"Franks","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":197671,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26153,"text":"wri874258 - 1988 - Preliminary paleolimnologic data for the Walker Lake subbasin, California and Nevada","interactions":[],"lastModifiedDate":"2014-01-30T12:41:36","indexId":"wri874258","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4258","title":"Preliminary paleolimnologic data for the Walker Lake subbasin, California and Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874258","usgsCitation":"Benson, L.V., 1988, Preliminary paleolimnologic data for the Walker Lake subbasin, California and Nevada: U.S. Geological Survey Water-Resources Investigations Report 87-4258, v, 50 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874258.","productDescription":"v, 50 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158302,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4258/report-thumb.jpg"},{"id":281774,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4258/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cd58","contributors":{"authors":[{"text":"Benson, Larry V. lbenson@usgs.gov","contributorId":1655,"corporation":false,"usgs":true,"family":"Benson","given":"Larry","email":"lbenson@usgs.gov","middleInitial":"V.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":195909,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}