A study was undertaken to evaluate the processes affecting the chemistry of shallow ground water associated with agricultural drainage systems in the western San Joaquin Valley, California. The study was prompted by a need for an understanding of selenium mobility in areas having high selenium concentrations in shallow ground water. Groundwater samples were collected along transects in three artificially drained fields where the age of the drainage system varied (15, 6, and 1.5 years). Selenium concentrations in the drainage water also varied (0F30, 58, and 3700 micrograms per liter, respectively). Isotopic enrichment and chemical composition of the ground-water samples indicate that saline- and selenium-enriched water has evolved as a result of evaporation of ground water. This evaporated, isotopically enriched water is being displaced by more recent, less saline irrigation water percolating through the root zone. This displace-ment seems to be a process whereby sodium chloride and sodium sulfate water is being replaced by more dilute calcium sulfate and calcium bicarbonate water.
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The atmospheric-boundary layer and the unsaturated and saturated soil zones were monitored as a single regime. Direct observations also were used to evaluate the measurements. Atmospheric sensors included an anemometer, a tipping-bucket rain gage, an air-temperature thermistor, a relative-humidity probe, a net radiometer, and a barometric-pressure transducer. Sensors in the unsaturated zone consisted of soil-temperature thermocouples, tensiometers coupled with pressure transducers and dial gages, gypsum blocks, and a neutron-moisture probe. The saturated-zone sensors consisted of a water-level pressure transducer, a conventional float gage connected to a variable potentiometer, soil thermocouples, and a number of multiple-depth piezometers. Evaluation of the operation of these sensors and recorders indicates that certain types of equipment, such as pressure transducers, are very sensitive to environmental conditions. A number of suggestions aimed at improving instrumentation of recharge investigations are outlined. Precipitation and evapotranspiration data, taken together with soil moisture profiles and storage changes, water fluxes in the unsaturated zone and hydraulic gradients in the saturated zone at various depths, soil temperature, water table hydrographs, and water level changes in nearby wells, describe the recharge process. Although the two instrumented sites are located in sand-dune environments in area characterized by a shallow water table and a sub-humid continental climate, a significant difference was observed in the estimated total recharge. The estimates ranged from less than 2.5 mm at the Zenith site to approximately 154 mm at the Burrton site from February to June 1983. The principal reasons that the Burrton site had more recharge than the Zenith site were more precipitation, less evapotranspiration, and a shallower depth to the water table. Effective recharge took place only during late winter and spring. No summer or fall recharge was observed at either site during the observation period of this study. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874097","usgsCitation":"Sophocleous, M., and Perry, C.A., 1987, Measuring and computing natural ground-water recharge at sites in south-central Kansas: U.S. Geological Survey Water-Resources Investigations Report 87-4097, viii, 48 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874097.","productDescription":"viii, 48 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":125115,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4097/report-thumb.jpg"},{"id":58636,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4097/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db611395","contributors":{"authors":[{"text":"Sophocleous, M.A.","contributorId":18032,"corporation":false,"usgs":true,"family":"Sophocleous","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":202216,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Perry, C. A.","contributorId":106149,"corporation":false,"usgs":true,"family":"Perry","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":202217,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28168,"text":"wri874091 - 1987 - Computer program for solving ground-water flow equations by the preconditioned conjugate gradient method","interactions":[],"lastModifiedDate":"2012-02-02T00:08:50","indexId":"wri874091","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4091","title":"Computer program for solving ground-water flow equations by the preconditioned conjugate gradient method","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874091","usgsCitation":"Kuiper, L., 1987, Computer program for solving ground-water flow equations by the preconditioned conjugate gradient method: U.S. Geological Survey Water-Resources Investigations Report 87-4091, iii, 34 p. :ill. ;28 cm., https://doi.org/10.3133/wri874091.","productDescription":"iii, 34 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":126547,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4091/report-thumb.jpg"},{"id":57002,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4091/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a79db","contributors":{"authors":[{"text":"Kuiper, L.K.","contributorId":34557,"corporation":false,"usgs":true,"family":"Kuiper","given":"L.K.","email":"","affiliations":[],"preferred":false,"id":199326,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52687,"text":"b1757B - 1987 - Mineral resources of the Honeycomb Buttes Wilderness Study Area, Fremont and Sweetwater counties, Wyoming","interactions":[{"subject":{"id":52687,"text":"b1757B - 1987 - Mineral resources of the Honeycomb Buttes Wilderness Study Area, Fremont and Sweetwater counties, Wyoming","indexId":"b1757B","publicationYear":"1987","noYear":false,"chapter":"B","title":"Mineral resources of the Honeycomb Buttes Wilderness Study Area, Fremont and Sweetwater counties, Wyoming"},"predicate":"IS_PART_OF","object":{"id":33502,"text":"b1757 - 1987 - Mineral resources of wilderness study areas: southern Wyoming","indexId":"b1757","publicationYear":"1987","noYear":false,"title":"Mineral resources of wilderness study areas: southern Wyoming"},"id":1}],"isPartOf":{"id":33502,"text":"b1757 - 1987 - Mineral resources of wilderness study areas: southern Wyoming","indexId":"b1757","publicationYear":"1987","noYear":false,"title":"Mineral resources of wilderness study areas: southern Wyoming"},"lastModifiedDate":"2017-08-09T09:12:18","indexId":"b1757B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1757","chapter":"B","title":"Mineral resources of the Honeycomb Buttes Wilderness Study Area, Fremont and Sweetwater counties, Wyoming","language":"ENGLISH","doi":"10.3133/b1757B","usgsCitation":"Patterson, C., Kulik, D.M., Loen, J.S., Koesterer, M., and Scott, D., 1987, Mineral resources of the Honeycomb Buttes Wilderness Study Area, Fremont and Sweetwater counties, Wyoming: U.S. Geological Survey Bulletin 1757, p. B1-B19; 1 plate in pocket, https://doi.org/10.3133/b1757B.","productDescription":"p. B1-B19; 1 plate in pocket","costCenters":[],"links":[{"id":109758,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21772.htm","linkFileType":{"id":5,"text":"html"},"description":"21772"},{"id":87015,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1757b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87016,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1757b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174811,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1757b/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a93e4b07f02db6584a4","contributors":{"authors":[{"text":"Patterson, C. G.","contributorId":87132,"corporation":false,"usgs":true,"family":"Patterson","given":"C. 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Chloride concentrations ranged from 23 to 320 milligrams per liter; the median concentration was 70 milligrams per liter. Nitrogen concentrations ranged from less than 0.1 to 11.0 milligrams per liter; the median concentration was 3.7 milligrams per liter. Chloride concentrations in 6 samples and nitrogen concentrations in 3 samples equaled or exceeded the U.S. Environmental Protection Agency public drinking-water limits of 250 and 10 milligrams per liter, respectively.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87466","usgsCitation":"Parliman, D., and Young, H., 1987, Selected water-quality data for the Murtaugh Lake area, south-central Idaho, June 1987: U.S. Geological Survey Open-File Report 87-466, 1 Plate: 37.54 × 26.35 inches, https://doi.org/10.3133/ofr87466.","productDescription":"1 Plate: 37.54 × 26.35 inches","costCenters":[],"links":[{"id":176192,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0466/report-thumb.jpg"},{"id":396294,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17272.htm"},{"id":80865,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0466/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","otherGeospatial":"Murtaugh Lake area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.24476623535156,\n 42.407234661551875\n ],\n [\n -114.02469635009764,\n 42.407234661551875\n ],\n [\n -114.02469635009764,\n 42.53309727228419\n ],\n [\n -114.24476623535156,\n 42.53309727228419\n ],\n [\n -114.24476623535156,\n 42.407234661551875\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a01e4b07f02db5f7ee5","contributors":{"authors":[{"text":"Parliman, D. 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Nitrogen concentrations ranged from 0.2 to 76 milligrams per liter; the median concentrations was 6.6 milligrams per liter. Nitrogen concentrations in 9 samples exceeded the U. S. Environmental Protection Agency public drinking-water limit of 10 milligrams per liter. 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