Continuing studies are being made in west-central Kansas to provide up-to-date information to aid in the management of groundwater for irrigation. This report, prepared in cooperation with the Western Kansas Groundwater Management District No. 1, presents the fifth in a series of studies that uses a statistical technique, called kriging, to produce hydrologic maps that are used as management tools.
Kriging is a statistical technique that was used to interpolate water level altitudes at the center of each 1-square-mile section in the study area based on measured water levels at 165 observation wells. These interpolation altitudes (1,859 in all), along with bedrock surface and base year water table altitudes, were used to prepare a geohydrologic map illustrating percentage change in saturated thickness. Saturated thickness, as used in this report, is the thickness of the High Plains aquifer between the groundwater surface indicated by water table altitudes and the bedrock surface. Because irrigation development in west-central Kansas was minimal prior to 1950, the saturated thickness during 1950 represented a nearly static condition in the aquifer. Thus, the effects of irrigation withdrawalson the volume of water in storage could be related to the decrease or percentage change in saturated thickness of the aquifer from 1950 to average saturated thickness during 1983-85.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854255","usgsCitation":"Dague, B.J., 1985, Percentage change in saturated thickness of the High Plains aquifer, west-central Kansas, 1950 to average 1983-85: U.S. Geological Survey Water-Resources Investigations Report 85-4255, 53.06 x 30.64 inches, https://doi.org/10.3133/wri854255.","productDescription":"53.06 x 30.64 inches","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":161900,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4255/report-thumb.jpg"},{"id":359299,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4255/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Kansas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -102,\n 38.3\n ],\n [\n -100.245,\n 38.3\n ],\n [\n -100.25,\n 38.55\n ],\n [\n -102,\n 38.55\n ],\n [\n -102,\n 38.3\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a68e4b07f02db63b538","contributors":{"authors":[{"text":"Dague, Barbara J.","contributorId":84811,"corporation":false,"usgs":true,"family":"Dague","given":"Barbara","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":229799,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44471,"text":"wri854101 - 1985 - Synopsis of saltwater intrusion in Dade County, Florida, through 1984","interactions":[],"lastModifiedDate":"2012-02-02T00:04:55","indexId":"wri854101","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4101","title":"Synopsis of saltwater intrusion in Dade County, Florida, through 1984","docAbstract":"The inland position of saltwater at the base of the highly permeable limestone of the Biscayne aquifer in Dade County in 1984 is a consequence of: (1) years of adjustment to lowered water levels resulting from regional drainage for flood control and land reclamation; (2) increased freshwater withdrawals; and (3) water-control and water-management practices implemented at the south part of the hydrologic system as well as in upgradient areas. As water demands in southeast Florida continue to increase, further intrusion could be related to increased pumping from well fields. Implementation of additional management practices to further reduce canal discharge to the ocean would tend to sustain water levels high enough to retard intrusion during dry seasons. (USGS)","language":"ENGLISH","doi":"10.3133/wri854101","usgsCitation":"Klein, H., and Waller, B.G., 1985, Synopsis of saltwater intrusion in Dade County, Florida, through 1984: U.S. Geological Survey Water-Resources Investigations Report 85-4101, 12 maps on 1 sheet ; 44 x 25 cm. and smaller, sheet 73 x 91 cm., folded in envelope 31 x 23 cm., https://doi.org/10.3133/wri854101.","productDescription":"12 maps on 1 sheet ; 44 x 25 cm. and smaller, sheet 73 x 91 cm., folded in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":134857,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81820,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4101/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db687ce4","contributors":{"authors":[{"text":"Klein, Howard","contributorId":62189,"corporation":false,"usgs":true,"family":"Klein","given":"Howard","email":"","affiliations":[],"preferred":false,"id":229831,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waller, Bradley G.","contributorId":83492,"corporation":false,"usgs":true,"family":"Waller","given":"Bradley","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":229832,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29529,"text":"wri854279 - 1985 - A two-constituent solute-transport model for ground water having variable density","interactions":[],"lastModifiedDate":"2018-02-21T15:33:42","indexId":"wri854279","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4279","title":"A two-constituent solute-transport model for ground water having variable density","docAbstract":"A numerical model has been developed to simulate solute transport and dispersion of either one or two constituents in groundwater where there is two-dimensional, density-dependent flow. The model is a modified version of the one documented by Konikow and Bredehoeft (1978), which uses finite-difference methods and the method of characteristics to solve the flow and transport equations. The model was tested on an idealized seawater intrusion problem for which an analytical solution has been developed. The results were nearly identical to those of other numerical models tested on the same problem. A description of the formats for the input data, a sample of input and output for a two-constituent example problem, and a listing of the Fortran program are presented. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854279","usgsCitation":"Sanford, W., and Konikow, L.F., 1985, A two-constituent solute-transport model for ground water having variable density: U.S. Geological Survey Water-Resources Investigations Report 85-4279, v, 88 p. :ill. ;28 cm., https://doi.org/10.3133/wri854279.","productDescription":"v, 88 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":58367,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4279/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123479,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4279/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a54d8","contributors":{"authors":[{"text":"Sanford, W. E. 0000-0002-6624-0280","orcid":"https://orcid.org/0000-0002-6624-0280","contributorId":102112,"corporation":false,"usgs":true,"family":"Sanford","given":"W. E.","affiliations":[],"preferred":false,"id":201668,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Konikow, Leonard F. 0000-0002-0940-3856 lkonikow@usgs.gov","orcid":"https://orcid.org/0000-0002-0940-3856","contributorId":158,"corporation":false,"usgs":true,"family":"Konikow","given":"Leonard","email":"lkonikow@usgs.gov","middleInitial":"F.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":201667,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":30251,"text":"wri854064 - 1985 - Ground-water contamination in East Bay Township, Michigan","interactions":[],"lastModifiedDate":"2017-02-06T10:15:47","indexId":"wri854064","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4064","title":"Ground-water contamination in East Bay Township, Michigan","docAbstract":"Glacial deposits, as much as 360 feet thick, underlie the study area. The upper 29 to 118 feet, a sand and gravel unit, is the aquifer tapped for water by all wells in the area. This unit is underlain by impermeable clay that is at least 100 feet thick.
Ground-water flow is northeastward at an estimated rate of 3 to 6 feet per day. Hydraulic conductivities in the aquifer range from 85 to 150 feet per day; 120 feet per day provided the best match of field data in a ground-water flow model. The depth to water ranged from 1 to 20 feet.
Chemical anlayses indicate that ground water is contaminated with organic chemicals from near the Hangar/Administration building at the U.S. Coast Guard Air Station to East Bay, about 4,300 feet northeast. The plume, which follows ground-water flow lines, ranges from 180 to 400 feet wide. In the upper reach of the plume, hydrocarbons less dense than water occur at the surface of the water table; they move downward in the aquifer as they move toward East Bay. Maximum concentrations of the major organic compounds include: benzene, 3,390 micrograms per liter; toluene, 55,500 micrograms per liter; xylene, 3,900 micrograms per liter; tetrachloroethylene, 3,410 micrograms per liter; and bis (2-ethyl hexyl) phthalate, 2,100 micrograms per liter. Soils are generally free of these hydrocarbons; however, in the vicinity of past drum storage, aircraft maintenance operations, and fuel storage and dispensing, as much as 1,100 micrograms per kilogram of tetrachloroethylene and 1,500 micrograms per kilogram of bis (2-ethyl hexyl) phthalate were detected. At a few locations higher molecular weight hydrocarbons, characteristic of petroleum distillates, were found.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/wri854064","collaboration":"Prepared in cooperation with the U.S. Coast Guard","usgsCitation":"Twenter, F.R., Cummings, T., and Grannemann, N., 1985, Ground-water contamination in East Bay Township, Michigan: U.S. Geological Survey Water-Resources Investigations Report 85-4064, Document: ix, 63 p.; 5 Plates: 23.24 x 35.59 inches or smaller, https://doi.org/10.3133/wri854064.","productDescription":"Document: ix, 63 p.; 5 Plates: 23.24 x 35.59 inches or smaller","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":59038,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4064/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59039,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4064/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123443,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4064/report-thumb.jpg"},{"id":59040,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4064/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59041,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4064/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59042,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4064/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59043,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4064/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Michigan","otherGeospatial":"East Bay Township","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -85.57439804077148,\n 44.74164292754147\n ],\n [\n -85.56602954864502,\n 44.75276788055599\n ],\n [\n -85.5673599243164,\n 44.7531640722716\n ],\n [\n -85.56911945343018,\n 44.753986923310066\n ],\n [\n -85.57062149047852,\n 44.75490118850054\n ],\n [\n -85.57225227355957,\n 44.75599828763615\n ],\n [\n -85.57353973388672,\n 44.75706489182693\n ],\n [\n -85.57529926300047,\n 44.7584971579133\n ],\n [\n -85.57585716247559,\n 44.7592894600709\n ],\n [\n -85.57611465454102,\n 44.760234113828844\n ],\n [\n -85.58675765991211,\n 44.746885637908065\n ],\n [\n -85.57439804077148,\n 44.74164292754147\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699997","contributors":{"authors":[{"text":"Twenter, F. R.","contributorId":81080,"corporation":false,"usgs":true,"family":"Twenter","given":"F.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":202934,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cummings, T. R.","contributorId":104082,"corporation":false,"usgs":true,"family":"Cummings","given":"T. R.","affiliations":[],"preferred":false,"id":202935,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grannemann, N.G.","contributorId":11221,"corporation":false,"usgs":true,"family":"Grannemann","given":"N.G.","affiliations":[],"preferred":false,"id":202933,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":12097,"text":"ofr85683 - 1985 - Ground-water quality data from the northern Mississippi embayment; Arkansas, Missouri, Kentucky, Tennessee, and Mississippi","interactions":[],"lastModifiedDate":"2012-02-02T00:06:35","indexId":"ofr85683","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-683","title":"Ground-water quality data from the northern Mississippi embayment; Arkansas, Missouri, Kentucky, Tennessee, and Mississippi","docAbstract":"Groundwater quality data were collected from 42 selected wells in the McNairy-Nacatoch-Ripley and the lower Wilcox aquifers of the northern Mississippi embayment. The study is part of the Gulf Coast Regional Aquifer System Analysis (GC RASA) study; the data will be used for geochemical modeling of mineral saturation and mass transfer in the McNairy-Nacatoch-Ripley aquifer. The report contains two figures showing the location of sampling sites for each of the two aquifers, six tables of data which contain (1) well descriptions and (2) concentrations of major constituents, trace constituents, dissolved gases, stable and unstable isotopes of low mass (C, H, O, and S), and unstable isotopes of high mass (Rn, Ra, and U), and a brief documentation of the methods used for sample collection and analysis. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85683","usgsCitation":"Brahana, J., Mesko, T.O., Busby, J., and Kraemer, T.F., 1985, Ground-water quality data from the northern Mississippi embayment; Arkansas, Missouri, Kentucky, Tennessee, and Mississippi: U.S. Geological Survey Open-File Report 85-683, iii, 15 p. :maps ;28 cm., https://doi.org/10.3133/ofr85683.","productDescription":"iii, 15 p. :maps ;28 cm.","costCenters":[],"links":[{"id":977,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr85-683","linkFileType":{"id":5,"text":"html"}},{"id":144759,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d939","contributors":{"authors":[{"text":"Brahana, J. V.","contributorId":32926,"corporation":false,"usgs":true,"family":"Brahana","given":"J. V.","affiliations":[],"preferred":false,"id":165054,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mesko, T. O.","contributorId":83934,"corporation":false,"usgs":true,"family":"Mesko","given":"T.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":165056,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Busby, J.F.","contributorId":105300,"corporation":false,"usgs":true,"family":"Busby","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":165057,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kraemer, T. F.","contributorId":63400,"corporation":false,"usgs":true,"family":"Kraemer","given":"T.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":165055,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":12094,"text":"ofr85331 - 1985 - Ground-water data for Georgia, 1984","interactions":[],"lastModifiedDate":"2024-12-04T20:53:11.631017","indexId":"ofr85331","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-331","title":"Ground-water data for Georgia, 1984","docAbstract":"Continuous water-level records from 155 wells and more than 800 water-level measurements made in Georgia during 1984 provide the basic data for this report. Selected wells illustrate the effects that changes in recharge and pumping have had on the various ground-water resources in the State. Daily mean water levels are shown in hydrographs for 1984. Monthly means are shown for the 10-year period 1975-84. Mean annual water levels ranged from 7 feet lower to 7 feet higher in 1984 than in 1983. Water-quality samples are collected periodically throughout Georgia and analyzed as part of a real and regional ground-water studies. Along the coast, chloride concentrations in the Floridan aquifer system generally remained steady. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr85331","usgsCitation":"Clarke, J., Longsworth, S., McFadden, K., and Peck, M., 1985, Ground-water data for Georgia, 1984: U.S. Geological Survey Open-File Report 85-331, xiii, 150 p., https://doi.org/10.3133/ofr85331.","productDescription":"xiii, 150 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":144740,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0331/report-thumb.jpg"},{"id":464764,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16774.htm","linkFileType":{"id":5,"text":"html"}},{"id":40128,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0331/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cfab","contributors":{"authors":[{"text":"Clarke, J.S.","contributorId":89526,"corporation":false,"usgs":true,"family":"Clarke","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":165043,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Longsworth, S.A.","contributorId":47784,"corporation":false,"usgs":true,"family":"Longsworth","given":"S.A.","affiliations":[],"preferred":false,"id":165042,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McFadden, K.W.","contributorId":22766,"corporation":false,"usgs":true,"family":"McFadden","given":"K.W.","email":"","affiliations":[],"preferred":false,"id":165041,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Peck, M.F.","contributorId":93049,"corporation":false,"usgs":true,"family":"Peck","given":"M.F.","email":"","affiliations":[],"preferred":false,"id":165044,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":28232,"text":"wri854155 - 1985 - A preliminary assessment of land-surface subsidence in the El Paso area, Texas","interactions":[],"lastModifiedDate":"2018-10-30T12:49:42","indexId":"wri854155","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4155","title":"A preliminary assessment of land-surface subsidence in the El Paso area, Texas","docAbstract":"The northeast and southeast parts of the El Paso area are underlain by Hueco bolson deposits as much as 9,000 feet thick. The deposits consist of lenses of gravel, sand, silt, and clay. In the Rio Grande Valley, about 400 to 450 feet of these deposits have been eroded and replaced with as much as 200 feet of alluvium. Ground water in the shallow alluvial aquifer in the Rio Grande Valley and in the Hueco bolson aquifer outside the valley is under water-table conditions, whereas ground water in the bolson aquifer in the valley is under leaky artesian conditions. Maximum water-level declines in the Hueco bolson aquifer are 110 feet east of the Franklin Mountains and 150 feet in the downtown El Paso area. For the shallow aquifer, the maximum declines have been 125 feet in the downtown area. Compressable materials in the freshwater zone of the aquifer range from 50 to 450 feet.
\nRecharge from the Rio Grande to the shallow alluvial aquifer has increased from an estimated 15,000 acre-feet during 1968 to 30,000 acre-feet during 1983, an increase of about 1,000 acre-feet per year. Leakage from the Rio Grande is expected to continually increase in the near future because of a continued decline in ground-water levels. The amount of leakages from the canals is much less than from the river.
\nReleveling of bench marks along lines to the northeast and the southeast of the Rio Grande, and along its channel commonly show land subsidence of about 0.2 foot. The maximum measured subsidence is 0.41 foot along the river in the Chamizal zone. No subsidence was detected at the Riverside Diversion Dam. A comparison of subsidence, water-level declines, and clay thickness along the three survey lines shows the expected correlation of greater subsidence with thicker accumulated clay material for a given decline in water levels. The preconsolidation stress was expected to range from 85 to 115 feet of water-level decline on the basis of subsidence studies in Arizona and California. A study of specific-unit compaction along the three survey lines shows that the values usually range between 1.0 to 2.5 x 10-5 feet per feet squared. These values are comparable to the ones computed in the Tulare-Wasco, California, and Houston-Galveston, Texas, areas following the exceedance of the local preconsolidation stress. Because of this comparability, the specific-unit compaction for future periods in the El Paso area probably will not increase dramatically when the preconsolidation stress is exceeded, if it has not already been exceeded.
\nIn addition to regional subsidence, local subsidence is indicated by observable surface fractures but has not been verified by precise leveling. These local areas coincide with areas that historically were swamps along the Rio Grande.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri854155","collaboration":"Prepared in cooperation with the Bureau of Reclamation","usgsCitation":"Land, L.F., and Armstrong, C.A., 1985, A preliminary assessment of land-surface subsidence in the El Paso area, Texas: U.S. Geological Survey Water-Resources Investigations Report 85-4155, vi, 96 p., https://doi.org/10.3133/wri854155.","productDescription":"vi, 96 p.","numberOfPages":"108","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":57062,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4155/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123872,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4155/report-thumb.jpg"}],"country":"United States","state":"Texas","city":"El Paso","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.32293701171874,\n 31.647536225797772\n ],\n [\n -106.35314941406249,\n 31.701882151861714\n ],\n [\n -106.37443542480469,\n 31.71122878128754\n ],\n [\n -106.38198852539062,\n 31.73400724374667\n ],\n [\n -106.45271301269531,\n 31.764369817056387\n ],\n [\n -106.468505859375,\n 31.76145077153307\n ],\n [\n -106.47468566894531,\n 31.750941445321764\n ],\n [\n -106.48773193359375,\n 31.74918977495709\n ],\n [\n -106.50421142578125,\n 31.756780107186728\n ],\n [\n -106.51588439941406,\n 31.770791393089315\n ],\n [\n -106.52961730957031,\n 31.783633207994736\n ],\n [\n -106.53648376464844,\n 31.94633593313394\n ],\n [\n -106.32980346679686,\n 31.94808386339691\n ],\n [\n -106.32293701171874,\n 31.647536225797772\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6aaf25","contributors":{"authors":[{"text":"Land, L. F.","contributorId":17253,"corporation":false,"usgs":true,"family":"Land","given":"L.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":199433,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Armstrong, C. A.","contributorId":66231,"corporation":false,"usgs":true,"family":"Armstrong","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":199434,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":42114,"text":"ofr85750 - 1985 - Aeromagnetic map of Blue Eagle Mountain and vicinity, eastern Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:11:06","indexId":"ofr85750","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-750","title":"Aeromagnetic map of Blue Eagle Mountain and vicinity, eastern Nevada","language":"ENGLISH","doi":"10.3133/ofr85750","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1985, Aeromagnetic map of Blue Eagle Mountain and vicinity, eastern Nevada: U.S. Geological Survey Open-File Report 85-750, 1 map :photocopy ;64 x 58 cm., on sheet 92 x 77 cm., https://doi.org/10.3133/ofr85750.","productDescription":"1 map :photocopy ;64 x 58 cm., on sheet 92 x 77 cm.","costCenters":[],"links":[{"id":168491,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79855,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1985/0750/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6982b8","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":530840,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26455,"text":"wri844240 - 1985 - Estimating average base flow at low-flow partial-record stations on the south shore of Long Island, New York","interactions":[],"lastModifiedDate":"2013-01-22T14:39:07","indexId":"wri844240","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4240","title":"Estimating average base flow at low-flow partial-record stations on the south shore of Long Island, New York","docAbstract":"Base flows of the 29 major streams in southeast Nassau and southwest Suffolk Counties, New York, were statistically analyzed to discern the correlation among flows of adjacent streams. Concurrent base-flow data from a partial-record and a nearby continuous-record station were related; the data were from 1968-75, a period near hydrologic equilibrium on Long Island. The average base flow at each partial-record station was estimated from a regression equation and average measured base flow for the period at the continuous-record stations. Regression analyses are presented for the 20 streams with partial-record stations. Average base flow of the nine streams with a continuous record totaled 90 cu ft/sec; the predicted average base flow for the 20 streams with a partial record was 73 cu ft/sec (with a 95% confidence interval of 63 to 84 cu ft/sec.) Results indicate that this method provides reliable estimates of average low flow for streams such as those on Long Island, which consist mostly of base flow and are geomorphically similar. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844240","usgsCitation":"Buxton, H., 1985, Estimating average base flow at low-flow partial-record stations on the south shore of Long Island, New York: U.S. Geological Survey Water-Resources Investigations Report 84-4240, iv, 32 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844240.","productDescription":"iv, 32 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123874,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_84_4240.jpg"},{"id":266237,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4240/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc9bf","contributors":{"authors":[{"text":"Buxton, H. T.","contributorId":67873,"corporation":false,"usgs":true,"family":"Buxton","given":"H. T.","affiliations":[],"preferred":false,"id":196422,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43400,"text":"ofr85320 - 1985 - Land use and land cover and associated maps for Lewistown, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:04:56","indexId":"ofr85320","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-320","title":"Land use and land cover and associated maps for Lewistown, Montana","language":"ENGLISH","doi":"10.3133/ofr85320","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1985, Land use and land cover and associated maps for Lewistown, Montana: U.S. Geological Survey Open-File Report 85-320, maps :photocopy ;45 x 61 cm., on sheets 76 x 107 cm., https://doi.org/10.3133/ofr85320.","productDescription":"maps :photocopy ;45 x 61 cm., on sheets 76 x 107 cm.","costCenters":[],"links":[{"id":134867,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b0e90","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":531150,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":56231,"text":"wdrOK831 - 1985 - Water resources data for Oklahoma, water year 1983","interactions":[],"lastModifiedDate":"2020-09-25T16:29:52.727377","indexId":"wdrOK831","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"OK-83-1","title":"Water resources data for Oklahoma, water year 1983","docAbstract":"No abstract available.
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G.","contributorId":19983,"corporation":false,"usgs":true,"family":"Spinello","given":"A.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":254936,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nakao, J.H.","contributorId":16088,"corporation":false,"usgs":true,"family":"Nakao","given":"J.H.","affiliations":[],"preferred":false,"id":254935,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Flipse, W.J. Jr.","contributorId":98733,"corporation":false,"usgs":true,"family":"Flipse","given":"W.J.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":254937,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Carcaci, J.G.","contributorId":106195,"corporation":false,"usgs":true,"family":"Carcaci","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":254938,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":55180,"text":"wdrHI841 - 1985 - Water resources data for Hawaii and other Pacific areas, water year 1984: Volume 1. Hawaii","interactions":[],"lastModifiedDate":"2026-03-24T16:32:40.2351","indexId":"wdrHI841","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"HI-84-1","title":"Water resources data for Hawaii and other Pacific areas, water year 1984: Volume 1. Hawaii","docAbstract":"Water resources data for the 1984 water year for Hawaii and other Pacific Areas consist of records of stage, discharge, and water quality of streams and springs; and water levels and water quality in wells. This report, volume 1, contains discharge records for 96 gaging stations; water quality for 13 gaging stations, 102 partial-record flow stations, and 153 wells; and water levels for 39 observation wells. Also included are 108 crest-stage partial-record stations and 21 low-flow partial-record stations. Additional water data were collected at various sites, not part of the systematic data collection program, are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by theU.S. Geological Survey and cooperating State, Federal, and other agencies in Hawaii.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f6f52","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":532283,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29198,"text":"wri854220 - 1985 - Dissolved constituents including selenium in waters in the vicinity of Kesterson National Wildlife Refuge and the west grassland, Fresno and Merced Counties, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:50","indexId":"wri854220","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4220","title":"Dissolved constituents including selenium in waters in the vicinity of Kesterson National Wildlife Refuge and the west grassland, Fresno and Merced Counties, California","docAbstract":"Analyses were made for dissolved constituents including selenium (Se) in waters associated with subsurface agricultural drainage from the western San Joaquin Valley of California. In the vicinity of Kesterson National Wildlife Refuge and the Grassland wetlands area Se was found to be mobilized in water. As a consequence of this mobility and bioaccumulation in the aquatic food chain, Se occurred in waterfowl at levels toxic enough to cause deformities and deaths. Se concentrations in sumps that collect subsurface agricultural drainage water and inflows to drains sampled, ultimately leading into Kesterson National Wildlife Refuge and the Grassland, ranged from 84 to 4200 microgram/L (ug/L) Se. Levels of Se were reduced in the San Luis Drain flowing into Kesterson National Wildlife Refute to approximately 300 ug/L Se and in three of the drains sampled flowing into the Grassland to approximately 50 ug/L Se. Serious effects on water fowl habitat were caused by both these levels. Se contents of algal mats and salt crusts from evaporation ponds of the San Luis Drain contained up to parts per million Se. Total ecosystem assessment of Se may be necessary for the evaluation of the toxicity of Se to the environment. No other trace element reported exceeded the various criteria for water at the level of magnitude of Se. Other dissolved constituents and the isotopic ratios of oxygen and hydrogen were analyzed to elucidate water types, reaction states of the aqueous solution with respect to minerals, and the origin of mixed waters. These data will be used later to evaluate the geologic source of Se. Methods used for collection and analysis are described and documented. Hydrologic effects were found to be complex. Preliminary indications from wells are also given. A historical sequence is adhered to and other data from the study area which serve as a guide to the toxicity of Se are included. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854220","usgsCitation":"Presser, T.S., and Barnes, I., 1985, Dissolved constituents including selenium in waters in the vicinity of Kesterson National Wildlife Refuge and the west grassland, Fresno and Merced Counties, California: U.S. Geological Survey Water-Resources Investigations Report 85-4220, vi, 73 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854220.","productDescription":"vi, 73 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123319,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4220/report-thumb.jpg"},{"id":58059,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4220/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a281","contributors":{"authors":[{"text":"Presser, T. S.","contributorId":93875,"corporation":false,"usgs":true,"family":"Presser","given":"T.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":201130,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, Ivan","contributorId":56619,"corporation":false,"usgs":true,"family":"Barnes","given":"Ivan","email":"","affiliations":[],"preferred":false,"id":201129,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":65271,"text":"i1737 - 1985 - Controlled photomosaic of part of the Alba Patera Region of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:09","indexId":"i1737","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1737","subseriesTitle":"NONE","title":"Controlled photomosaic of part of the Alba Patera Region of Mars","language":"ENGLISH","doi":"10.3133/i1737","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1985, Controlled photomosaic of part of the Alba Patera Region of Mars: U.S. Geological Survey IMAP 1737, 1 remote-sensing image ;62 x 49 cm., on sheet 97 x 57 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1737.","productDescription":"1 remote-sensing image ;62 x 49 cm., on sheet 97 x 57 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190223,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260755,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1737/plate-1.pdf"}],"scale":"502000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a8c7","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":533660,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1899,"text":"wsp2258 - 1985 - Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico","interactions":[{"subject":{"id":19423,"text":"ofr83774 - 1983 - Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico","indexId":"ofr83774","publicationYear":"1983","noYear":false,"title":"Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":1899,"text":"wsp2258 - 1985 - Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico","indexId":"wsp2258","publicationYear":"1985","noYear":false,"title":"Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico"},"id":1}],"lastModifiedDate":"2023-01-06T21:50:17.069165","indexId":"wsp2258","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2258","title":"Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico","docAbstract":"The Papago Farms-Great Plain and upper Rio Sonoyta study area includes about 490 square miles in south-central Arizona and north-central Sonora, Mexico. The area is characterized by a broad, deep, sediment-filled basin bounded by low, jagged fault-block mountains. The climate is arid to semiarid. The climate and abundant ground water provide favorable conditions for irrigated agriculture. Annual precipitation averages 5 to 8 inches per year on the desert floor. Runoff, which occurs as intermittent streamflow and sheetflow, is too short lived and too laden with suspended sediment to be a reliable source for irrigation or public supply. \r\n\r\nNearly all the water used to irrigate more than 5,000 cultivated acres in the study area is withdrawn from the unconsolidated to partly consolidated basin fill. The ground water occurs in the deposits under unconfined (water-table) conditions with a saturated thickness that ranges from zero along the mountain fronts to more than 8,000 feet in the center of the basin. The amount of recoverable ground water in storage to a depth of 400 feet below the 1978-80 water table is estimated to be about 10 million acre-feet. Depths to water range from about 500 feet near the southern boundary of the study area to about 150 feet in the center of the study area. Ground water enters the area principally as underflow beneath the San Simon and Chukut Kuk Washes and as recharge along the mountain fronts. On the basis of model results, annual inflow to the ground-water system is estimated to be about 4,390 acre-feet. Ground water moves through the study area along paths that encircle a virtually impermeable unit in the basin center, termed 'the lakebed-clay deposits,' and moves westward to an outflow point beneath the Rio Sonoyta south of Cerro La Nariz. Rates of water movement range from less than I foot per year in clays to about 160 feet per year in well-sorted, coarse stream-channel deposits. Transmissivities along the basin margins range from 10,000 to 40,000 feet squared per day, whereas transmissivities in the basin-center lakebed-clay deposits are estimated to be less than 100 feet squared per day. Most Wells that are located along the basin margin and tap more than 300 feet of saturated basin fill in the upper1,000 feet of the aquifer should yield from 500 to 3,000 gallons per minute to properly constructed and developed wells. Specific capacities should range from 10 to 50 gallons per minute per foot of drawdown. \r\n\r\nThe water in the aquifer is moderate to poor in chemical quality for irrigation and public-supply use. The ground water is mainly a sodium bicarbonate type with dissolved-solids concentrations that range from about 250 to 5,000 milligrams per liter and average about 530 milligrams per liter. The poorest quality water is associated with the basin-center lakebed-clay deposits. In most of the basin, the water contains fluoride concentrations that exceed the maximum contaminant levels acceptable for drinking water. Waters from the basin-center lakebed-clay deposits are also anomalously high in dissolved arsenic and unacceptable for public supply. High concentrations of sodium and bicarbonate in the ground water of the study area present potential hazards to most crops, and the use of this type of water requires careful farm-management practices. \r\n\r\nIn 1981 outflow resulting from withdrawals of water from the aquifer was about 23,2'00 acre-feet. Storage is being depleted at a rate of about 19,000 acre-feet per year. On the basis of a mathematical simulation of the groundwater system and withdrawal rates in 1981, storage depletion and drawdown of the water table were projected to 1991. Water-level declines in 199t were estimated to be as much as 20 feet at Papago Farms and more than 40 feet in the area south of the basin-center lakebed-clay deposits. The estimated amount of depletion in 1991 of ground water stored in the upper 400 feet of the aquifer is less than 3.0 percent of the total amou","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2258","usgsCitation":"Hollett, K.J., 1985, Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico: U.S. Geological Survey Water Supply Paper 2258, v, 44 p., https://doi.org/10.3133/wsp2258.","productDescription":"v, 44 p.","costCenters":[],"links":[{"id":411525,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25496.htm","linkFileType":{"id":5,"text":"html"}},{"id":138423,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2258/report-thumb.jpg"},{"id":27196,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2258/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Mexico, United States","state":"Arizona, Sonora","otherGeospatial":"Papago Farms-Great Plain area, Papago Indian Reservation, upper Rio Sonoyta area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -112.083,\n 31.908\n ],\n [\n -112.566,\n 31.908\n ],\n [\n -112.566,\n 31.375\n ],\n [\n -112.083,\n 31.375\n ],\n [\n -112.083,\n 31.908\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8b1c","contributors":{"authors":[{"text":"Hollett, Kenneth J.","contributorId":40580,"corporation":false,"usgs":true,"family":"Hollett","given":"Kenneth","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":144334,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30207,"text":"wri854241 - 1985 - Hydrogeology and water quality of the Catoctin Mountain National Park Area, Frederick County, Maryland","interactions":[],"lastModifiedDate":"2023-01-06T22:42:24.788177","indexId":"wri854241","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4241","title":"Hydrogeology and water quality of the Catoctin Mountain National Park Area, Frederick County, Maryland","docAbstract":"The Catoctin Mountain National Park area, located in the Blue Ridge physiographic province of central Maryland, is characterized by high local relief, an average annual precipitation of 44 inches, and stony soils underlain by weathered and fractured metamorphic rocks. The park is mostly forested land and includes several camps and roads. The groundwater reservoir consists of regolith and underlying fractured bedrock and is recharged by precipitation. Discharge from the groundwater flow system is mainly to nearby streams adjacent to areas of recharge. Approximately 56% of annual streamflow is contributed by groundwater. Wells located at Camp Round Meadow and Staff Quarters No. 5 can sustain pumping rates of 45 to 60 gal/min for several hours, with drawdown of 40 to 50 ft. Water quality samples from wells, springs, and streams indicate that groundwater is slightly affected by septic waste and road salt. Groundwater in remote areas is not affected by either source. Concentrations of chloride from road salt and concentrations of nitrate plus nitrite (as N) were below U.S. EPA drinking water limits in all groundwater and surface water samples.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854241","usgsCitation":"Trombley, T.J., and Zynjuk, L.D., 1985, Hydrogeology and water quality of the Catoctin Mountain National Park Area, Frederick County, Maryland: U.S. Geological Survey Water-Resources Investigations Report 85-4241, v, 41 p., https://doi.org/10.3133/wri854241.","productDescription":"v, 41 p.","costCenters":[],"links":[{"id":411537,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36388.htm","linkFileType":{"id":5,"text":"html"}},{"id":58996,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4241/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123704,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4241/report-thumb.jpg"}],"country":"United States","state":"Maryland","county":"Frederick County","otherGeospatial":"Catoctin Mountain National Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -77.42645011667537,\n 39.616936790338286\n ],\n [\n -77.42771790984752,\n 39.66915479468962\n ],\n [\n -77.42771790984752,\n 39.70380034757878\n ],\n [\n -77.5240701909294,\n 39.70380034757878\n ],\n [\n -77.52153460458503,\n 39.61791265187179\n ],\n [\n -77.42645011667537,\n 39.616936790338286\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db6251c8","contributors":{"authors":[{"text":"Trombley, T. J.","contributorId":75161,"corporation":false,"usgs":true,"family":"Trombley","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":202859,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zynjuk, Linda D.","contributorId":108101,"corporation":false,"usgs":true,"family":"Zynjuk","given":"Linda","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":202860,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":12116,"text":"ofr83761 - 1985 - Hydrology of Area 52, Rocky Mountain coal province, Wyoming, Colorado, Idaho, and Utah","interactions":[],"lastModifiedDate":"2023-08-24T21:35:23.69872","indexId":"ofr83761","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"83-761","title":"Hydrology of Area 52, Rocky Mountain coal province, Wyoming, Colorado, Idaho, and Utah","docAbstract":"This report is one of a series designed to characterize the hydrology of drainage basins within coal provinces, nationwide. Area 52 (in the Rocky Mountain Coal Province) includes the Green River Basin upstream from the Yampa River, and the Bear River upstream from the Bear Lake - a total of 23,870 sq mi. Area 52 contains over 3 billion tons of strippable coal, most of which is located in the arid and semiarid plains. The report represents a summary of results of the water resources investigations of the U.S. Geological Survey, carried out in cooperation with State and other Federal agencies. More than 40 individual topics are discussed in a brief text that is accompanied by maps, graphs, photographs, and other illustrations. Primary topics in the report are: general features, resources and economy, surface-water quantity and quality, and groundwater. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83761","usgsCitation":"Lowham, H., Peterson, D.A., Larson, L.R., Zimmerman, E.A., Ringen, B.H., and Mora, K.L., 1985, Hydrology of Area 52, Rocky Mountain coal province, Wyoming, Colorado, Idaho, and Utah: U.S. Geological Survey Open-File Report 83-761, vi, 96 p., https://doi.org/10.3133/ofr83761.","productDescription":"vi, 96 p.","costCenters":[],"links":[{"id":144805,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0761/report-thumb.jpg"},{"id":95061,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0761/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":420139,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14212.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado, Idaho, Utah, Wyoming","otherGeospatial":"Area 52, Rocky Mountain Coal Province","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -111.454,\n 43.447\n ],\n [\n -111.454,\n 40.525\n ],\n [\n -107.091,\n 40.525\n ],\n [\n -107.091,\n 43.447\n ],\n [\n -111.454,\n 43.447\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601fd3","contributors":{"authors":[{"text":"Lowham, H. W.","contributorId":8111,"corporation":false,"usgs":true,"family":"Lowham","given":"H. W.","affiliations":[],"preferred":false,"id":165132,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, D. A.","contributorId":6453,"corporation":false,"usgs":true,"family":"Peterson","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":165131,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Larson, L. R.","contributorId":41421,"corporation":false,"usgs":true,"family":"Larson","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":165134,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zimmerman, E. A.","contributorId":75533,"corporation":false,"usgs":true,"family":"Zimmerman","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":165136,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ringen, B. H.","contributorId":13987,"corporation":false,"usgs":true,"family":"Ringen","given":"B.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":165133,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Mora, K. L.","contributorId":55008,"corporation":false,"usgs":true,"family":"Mora","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":165135,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":26078,"text":"wri844305 - 1985 - Hydrology of the southern parts of Okaloosa and Walton Counties, northwest Florida, with special emphasis on the upper limestone of the Floridan aquifer","interactions":[],"lastModifiedDate":"2023-01-10T21:38:36.387139","indexId":"wri844305","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4305","title":"Hydrology of the southern parts of Okaloosa and Walton Counties, northwest Florida, with special emphasis on the upper limestone of the Floridan aquifer","docAbstract":"Increasing population in southern Okaloosa and Walton Counties have resulted in regional declines in the potentiometric surface of the upper limestone of the Floridan aquifer. Water levels have declined as much as 160 feet since 1940, and during peak seasonal demand as much as 190 feet. The Pensacola clay confining bed inhibits interchange of water between the Floridan aquifer and the surficial sand-and-gravel aquifer. The latter aquifer is of secondary importance as a public supply source. The Bucatunna clay confining bed separates the Floridan into upper and lower limestone units; the Floridan is underlain by the relatively impermeable Lisbon/Tallahatta confining unit. The Floridan aquifer dips south to the Gulf of Mexico, and is recharged by rainfall in northern Okaloosa and Walton Counties and in Alabama. The regional gradient of the potentiometric surface of the upper limestone, and presumably that of the lower limstone also, is south. Pumpage was variable in 1978; from 10.9 to 19.0 million gallons per day in January and June, respectively. Saline water in the upper limestone of the Floridan aquifer is less than 10 milligrams per liter inland but may be more than 150 milligrams per liter along the coast. Lower limestone water may exceed 250 milligrams per liter chloride.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844305","usgsCitation":"Barr, D.E., Hayes, L.R., and Kwader, T., 1985, Hydrology of the southern parts of Okaloosa and Walton Counties, northwest Florida, with special emphasis on the upper limestone of the Floridan aquifer: U.S. Geological Survey Water-Resources Investigations Report 84-4305, vi, 66 p., https://doi.org/10.3133/wri844305.","productDescription":"vi, 66 p.","costCenters":[],"links":[{"id":411671,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36146.htm","linkFileType":{"id":5,"text":"html"}},{"id":54850,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4305/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123434,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4305/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Okaloosa County, Walton County","otherGeospatial":"Florida aquifer","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -86.817,\n 30.417\n ],\n [\n -86.083,\n 30.417\n ],\n [\n -86.083,\n 30.717\n ],\n [\n -86.817,\n 30.717\n ],\n [\n -86.817,\n 30.417\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667057","contributors":{"authors":[{"text":"Barr, D. E.","contributorId":55469,"corporation":false,"usgs":true,"family":"Barr","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":195765,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hayes, L. R.","contributorId":50931,"corporation":false,"usgs":true,"family":"Hayes","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":195764,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kwader, Thomas","contributorId":9301,"corporation":false,"usgs":true,"family":"Kwader","given":"Thomas","email":"","affiliations":[],"preferred":false,"id":195763,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}