The U.S. Army Corps of Engineers' plan to control the natural chloride pollution in the Wichita River basin includes the construction of Truscott Brine Lake on a tributary of the North Wichita River. In connection with the proposed brine lake, the U.S. Geological Survey was requested to: (1) Define the existing ground-water conditions in the shallow fresh-water system of the project area; and (2) project the post-construction effects of the proposed lake on the fresh-water aquifer, especially in relation to hydraulic-head changes but also with respect to possible changes in the chemical quality of the ground water.
\nThe fresh-water aquifer in the project area is a shallow water-table system with relatively fresh water (generally a calcium sulfate type) that contains approximately 500 to 5,000 milligrams per liter of dissolved solids. The aquifer consists of Permian rocks with very small values of hydraulic conductivity and overlies a brine system (sodium chloride type) that is even less permeable. A thin transition zone separates the fresh-water aquifer and the brine system. Small quantities of infiltration from precipitation throughout the area's watershed constitute the recharge to the aquifer. Discharge from the aquifer consists of the small base flow along creeks; well discharge is negligible.
\nTwo-dimensional mathematical computer models were developed for aquifer simulation of: (1) Steady-state conditions in a fresh-water system and (2) transient conditions in a brine- fresh-water system where the density effects of the brine are considered. The main results 'of projecting the effects of the proposed Truscott Brine Lake on the fresh-water aquifer are: (1) Hydraulic head rises of 5 to 40 feet would be confined to areas near the proposed dam and along the lake shoreline, and (2) migration of salt water downstream from the dam generally would be limited to less than 1 mile and apparently would not reach equilibrium during the 100-year duration of the project. The modeling efforts did not include possible effects related to hydrodynamic dispersion in the brine- fresh-water system. Possible changes in the hydraulic conductivity of the aquifer, due to physical and chemical interactions in the brine and fresh-water environments, also were not considered.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri834026","usgsCitation":"Garza, S., 1983, Projected effects of proposed chloride-control projects on shallow ground water– Preliminary results for the Wichita River basin, Texas: U.S. Geological Survey Water-Resources Investigations Report 83-4026, Report: v, 40 p.; 8 Plates: 13.37 x 9.25 inches or smaller, https://doi.org/10.3133/wri834026.","productDescription":"Report: v, 40 p.; 8 Plates: 13.37 x 9.25 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":56131,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4026/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56127,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4026/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56126,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4026/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56123,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4026/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56125,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4026/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158575,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4026/report-thumb.jpg"},{"id":56124,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4026/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":110157,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35671.htm","linkFileType":{"id":5,"text":"html"},"description":"35671"},{"id":56130,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4026/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56129,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4026/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56128,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4026/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","otherGeospatial":"Wichita River Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -99.782,\n 33.694\n ],\n [\n -99.964,\n 33.694\n ],\n [\n -99.964,\n 33.833\n ],\n [\n -99.782,\n 33.833\n ],\n [\n -99.782,\n 33.694\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d9d4","contributors":{"authors":[{"text":"Garza, Sergio","contributorId":88713,"corporation":false,"usgs":true,"family":"Garza","given":"Sergio","email":"","affiliations":[],"preferred":false,"id":197811,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":66445,"text":"i1445 - 1983 - Geologic map of the northwest-quarter of the Beaver Quadrangle, Beaver County, Utah","interactions":[{"subject":{"id":42673,"text":"ofr801270 - 1980 - Preliminary geologic map of the northwest quarter of the Beaver Quadrangle, Beaver County, Utah","indexId":"ofr801270","publicationYear":"1980","noYear":false,"title":"Preliminary geologic map of the northwest quarter of the Beaver Quadrangle, Beaver County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":66445,"text":"i1445 - 1983 - Geologic map of the northwest-quarter of the Beaver Quadrangle, Beaver County, Utah","indexId":"i1445","publicationYear":"1983","noYear":false,"title":"Geologic map of the northwest-quarter of the Beaver Quadrangle, Beaver County, Utah"},"id":1}],"lastModifiedDate":"2012-02-10T00:11:15","indexId":"i1445","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"1445","subseriesTitle":"NONE","title":"Geologic map of the northwest-quarter of the Beaver Quadrangle, Beaver County, Utah","language":"ENGLISH","doi":"10.3133/i1445","usgsCitation":"Machette, M.N., and Steven, T.A., 1983, Geologic map of the northwest-quarter of the Beaver Quadrangle, Beaver County, Utah: U.S. Geological Survey IMAP 1445, 1 map :col. ;58 x 46 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1445.","productDescription":"1 map :col. ;58 x 46 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":106757,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9244.htm","linkFileType":{"id":5,"text":"html"},"description":"9244"},{"id":187650,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.75,38.3675 ], [ -112.75,38.5 ], [ -112.61749999999999,38.5 ], [ -112.61749999999999,38.3675 ], [ -112.75,38.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688831","contributors":{"authors":[{"text":"Machette, M. N.","contributorId":19561,"corporation":false,"usgs":true,"family":"Machette","given":"M.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":274543,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steven, T. A.","contributorId":42575,"corporation":false,"usgs":true,"family":"Steven","given":"T.","middleInitial":"A.","affiliations":[],"preferred":false,"id":274544,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":57293,"text":"wdrWV821 - 1983 - Water resources data West Virginia, water year 1982","interactions":[],"lastModifiedDate":"2025-02-26T20:00:54.138059","indexId":"wdrWV821","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"WV-82-1","title":"Water resources data West Virginia, water year 1982","docAbstract":"Water resources data for the 1982 water year for West Virginia consist of records of stage, discharge, and water quality of streams and springs; stage and contents of lakes and reservoirs; and water levels in wells. This report contains discharge records for 116 gaging stations; stage only records for 9 gaging stations; stage and contents for 8 lakes and reservoirs; contents for 1 reservoir; change in contents for 1 reservoir; water quality for 55 gaging stations; and water levels for 29 observation wells. Also included are 2 crest-stage partial-record stations, and 1 low-flow partial record station. Additional water data were collected at various sites, not part of the systematic data collections program, and are published as miscellaneous measurements and analyses. 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 West Virginia.
Water in Lake Arlington on Village Creek in north-central Texas had volume-weighted average concentrations of less than 240 milligrams per liter of dissolved solids, less than 30 milligrams per liter of dissolved chloride, and less than 40 milligrams per liter of dissolved sulfate between January 29, 1973, and August 20, 1981. The water was moderately hard (hardness greater than 60 but less than 120 milligrams per liter as calcium carbonate). The concentrations of each of these constituents were usually greatest during winter, especially during the first few years of the study, but decreased significantly as discharges of municipal wastes were systematically and progressively diverted to treatment facilities downstream from the reservoir.
\nThermal stratification in Lake Arlington usually begins during March or April and persists until October. Thermal stratification has resulted in significant seasonal and areal variations in the concentration of dissolved oxygen, dissolved iron, dissolved manganese, total inorganic nitrogen, and total phosphorus. Oxygen utilized in the decay of organic matter is not replenished during periods of summer stagnation, and water below depths of 30 to 40 feet usually contains less than 2 milligrams per liter of dissolved oxygen during stagnation. Even though heated effluent from an electrical generating plant is returned to the reservoir at site GC and causes an elevation of water temperature, average dissolved oxygen levels at this site are not significantly different from levels at other sites.
\nDuring summer stagnation, reducing conditions result in the dissolution of iron and manganese from bottom deposits at deep sites in the reservoir. At site AQ, a deep site near Arlington Dam, dissolved iron concentrations in water near the bottom during summer stagnation ranged from less than 10 to 1,100 micrograms per liter and averaged about 640 micrograms per liter. Dissolved manganese concentrations near the bottom at site AC during summer staynation ranged from 20 to 2,700 micrograms per liter and averaged about 1,500 micrograms per liter. The concentrations of dissolved iron and dissolved manganese in water throughout the reservoir during winter circulation and in water near the reservoir surface during summer stagnation averaged less than 50 micrograms per liter.
\nSeasonal temperature and dissolved oxygen cycles resulted in the recycling of dissolved iron and dissolved manganese between the water and bottom sediments. However, no significant accumulation of these constituents within the reservoir was detected during the study.
\nThe concentrations of total inorganic nitrogen and total phosphorus are greatest during summer stagnation in water near the bottom at deep sites. At site AC during the summer, the concentrations of total inorganic nitrogen in the hypolimnion averaged about 0.9 milligram per liter, and the concentration of total phosphorus near the bottom averaged about 0.2 milligram per liter. The concentrations of total inorganic nitrogen in the epilimnion at site AC averaged about 0.1 milligram per liter; the concentrations of total phosphorus averaged less than 0.1 milligram per liter.
\nThe densities and composition of algal populations varied seasonally. At site AC, total algae counts ranged from 200 to 240,000 cells per mi Hi liter and averaged about 50,000 cells per milliliter. At site FC, total algae counts ranged from 1,000 to 290,000 cells per milliliter and averaged about 56,000 cells per milliliter. Algal densities were greatest during the summer with blue-green algae being the predominant phyla.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri834196","usgsCitation":"Andrews, F.L., and Gibbons, W.J., 1983, Water quality of Lake Arlington on Village Creek, north-central Texas; 1973 to 1981: U.S. Geological Survey Water-Resources Investigations Report 83-4196, vi, 126 p., https://doi.org/10.3133/wri834196.","productDescription":"vi, 126 p.","numberOfPages":"132","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":408941,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35843.htm","linkFileType":{"id":5,"text":"html"}},{"id":157166,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4196/report-thumb.jpg"},{"id":54696,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4196/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","otherGeospatial":"Lake Arlington","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -97.24342346191406,\n 32.66278938534136\n ],\n [\n -97.24342346191406,\n 32.73646168396554\n ],\n [\n -97.17716217041014,\n 32.73646168396554\n ],\n [\n -97.17716217041014,\n 32.66278938534136\n ],\n [\n -97.24342346191406,\n 32.66278938534136\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa982","contributors":{"authors":[{"text":"Andrews, Freeman L.","contributorId":91486,"corporation":false,"usgs":true,"family":"Andrews","given":"Freeman","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":195518,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gibbons, Willard J.","contributorId":173568,"corporation":false,"usgs":false,"family":"Gibbons","given":"Willard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":195517,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":26874,"text":"wri834088 - 1983 - Automatic dilution gaging of rapidly varying flow","interactions":[],"lastModifiedDate":"2015-10-19T15:53:48","indexId":"wri834088","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4088","title":"Automatic dilution gaging of rapidly varying flow","docAbstract":"It is often difficult to obtain discharge ratings at urban gaging stations. This report presents the results of using an automated constant-rate dyedilution technique to measure discharge at two sites in Madison, Wisconsin. The sites selected have well-defined stage-discharge ratings, developed during previous hydrologic studies. One site has a 60-inch diameter concrete storm sewer and the other a concrete-lined open trapezoidal channel.
\nEquipment selected to automate the method included a portable automatic water sampler, a four-channel event recorder, and a variable-speed peristaltic pump for dye injection. An electrical switching circuit was designed to coordinate the operation of this equipment.
\nDuring the data-collection period of 1 year, a total of 20 storms were monitored.
\nThe analysis showed that the discharges measured by dye-dilution techniques were generally within ± 10 percent of the discharges determined from ratings established by current-meter measurements. Larger differences were noted at the start of and on the rising limb of four hydrographs. Of the 20 storms monitored, dilution measurements on 17 were of acceptable accuracy. Peak discharges from the open-channel site ranged from 0 to 12 percent departures from the existing rating whereas the comparison of peak discharge at the storm sewer site ranged from 0 to 5 percent departures from the existing rating.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834088","usgsCitation":"Duerk, M., 1983, Automatic dilution gaging of rapidly varying flow: U.S. Geological Survey Water-Resources Investigations Report 83-4088, v, 17 p., https://doi.org/10.3133/wri834088.","productDescription":"v, 17 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":123423,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4088/report-thumb.jpg"},{"id":55767,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4088/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6674a7","contributors":{"authors":[{"text":"Duerk, M.D.","contributorId":18806,"corporation":false,"usgs":true,"family":"Duerk","given":"M.D.","affiliations":[],"preferred":false,"id":197163,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43767,"text":"ofr83109 - 1983 - Land use and land cover and associated maps for Elko, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:10:10","indexId":"ofr83109","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-109","title":"Land use and land cover and associated maps for Elko, Nevada","language":"ENGLISH","doi":"10.3133/ofr83109","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Land use and land cover and associated maps for Elko, Nevada: U.S. Geological Survey Open-File Report 83-109, maps :photocopy ;44 x 68 cm., https://doi.org/10.3133/ofr83109.","productDescription":"maps :photocopy ;44 x 68 cm.","costCenters":[],"links":[{"id":162065,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1423","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":531354,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25718,"text":"wri834013 - 1983 - Preliminary appraisal of the hydrology of the Rock Island area, Le Flore County, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:08:15","indexId":"wri834013","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4013","title":"Preliminary appraisal of the hydrology of the Rock Island area, Le Flore County, Oklahoma","docAbstract":"Bed rock in the Rock Island area of northeastern Le Flore County in southeastern Oklahoma consists of shale, siltstone, and sandstone of the McAlester, Hartshorne, and Atoka Formations of Pennsylvanian age. The area is on the south flank of the Backbone anticline; the rocks dip to the south at 5o-45o. Alluvium along James Fork consists of sandy and clayey silt and may be as much as 30 feet thick.\r\nWater in bedrock is under artesian conditions. The depth to water in most wells is less than 20 feet below the surface; a few wells flow. Yields of most wells probably are less than 5 gallons per minute. Water from nine wells was a sodium carbonate or sodium mixed anion type; dissolved-solids concentrations ranged from 294 to 1,250 milligrams per liter. No relationship between variations in chemistry of ground water and well depth, geographic distribution, or geologic formation is apparent.\r\n\r\nJames Fork has flow most of the time and discharge exceeds 25 cubic feet per second about one-half the time. The mean dissolved-solids concentration in James Fork water ranged from 224 milligrams per liter near Williams, Oklahoma, to 332 milligrams per liter near Hackett, Arkansas. Water in James Fork is a calcium magnesium sulfate type about 75 percent of the time. Maximum suspended sediment discharge was 2,720 tons per day. Silt-clay particles (diameters less than 0.062 millimeter) are the dominant sediment size.\r\n\r\nPotential hydrologic effects of surface mining for coal include: (1) Creation of additional water storage in surface-mine ponds, (2) changes in rock permeability and ground-water storage, (3) changes in runoff and streamflow characteristics, (4) changes in drainage patterns, and (5) changes in the chemical quality and sediment load of James Fork. Although mining may increase the quantities of sediment and dissolved minerals added to James Fork, detection of these increases would be difficult because the potentially mineable area is very small in proportion to the total area of the basin.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834013","usgsCitation":"Marcher, M., 1983, Preliminary appraisal of the hydrology of the Rock Island area, Le Flore County, Oklahoma: U.S. Geological Survey Water-Resources Investigations Report 83-4013, iv, 39 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834013.","productDescription":"iv, 39 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":156904,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4013/report-thumb.jpg"},{"id":54480,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4013/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54481,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4013/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54482,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4013/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54483,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4013/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67ca7e","contributors":{"authors":[{"text":"Marcher, M.V.","contributorId":9267,"corporation":false,"usgs":true,"family":"Marcher","given":"M.V.","affiliations":[],"preferred":false,"id":194784,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3491,"text":"cir912 - 1983 - The U.S. Exclusive Economic Zone; a summary of its geology, exploration, and resource potential","interactions":[],"lastModifiedDate":"2012-02-02T00:05:45","indexId":"cir912","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"912","title":"The U.S. Exclusive Economic Zone; a summary of its geology, exploration, and resource potential","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir912","usgsCitation":"Rowland, R.W., Goud, M., and McGregor, B.A., 1983, The U.S. Exclusive Economic Zone; a summary of its geology, exploration, and resource potential: U.S. Geological Survey Circular 912, iii, 29 p. :ill., maps ;27 cm., https://doi.org/10.3133/cir912.","productDescription":"iii, 29 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":260256,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1983/0912/report.pdf"},{"id":260257,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1983/0912/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db6735af","contributors":{"authors":[{"text":"Rowland, Robert W.","contributorId":42200,"corporation":false,"usgs":true,"family":"Rowland","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":147026,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goud, M.R.","contributorId":11599,"corporation":false,"usgs":true,"family":"Goud","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":147025,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McGregor, Bonnie A.","contributorId":61022,"corporation":false,"usgs":true,"family":"McGregor","given":"Bonnie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":147027,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":25716,"text":"wri834060 - 1983 - A preliminary appraisal of sediment sources and transport in Kings Bay and vicinity, Georgia and Florida","interactions":[],"lastModifiedDate":"2017-01-27T08:42:17","indexId":"wri834060","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4060","title":"A preliminary appraisal of sediment sources and transport in Kings Bay and vicinity, Georgia and Florida","docAbstract":"Water-quality, bottom-material, suspended-sediment, and current-velocity data were collected during November 1981 in Kings Bay and vicinity to provide information on the sources and transport of estuarine sediments. Kings Bay and Cumberland Sound , the site of the Poseidon Submarine Base in southeast Georgia, are experiencing high rates of sediment deposition and accumulation, which are causing serious navigational and operational problems. Velocity, bathymetry, turbidity, and bottom-material data suggest that the area in the vicinity of lower Kings Bay is accumulating deposits of suspended sediment transported from Cumberland Sound on the floodtide and from upper Kings Bay and the tidal marsh drained by Marianna Creek on the ebbtide. Suspended-sediment discharges computed for consecutive 13-hour ebbtides and floodtides showed that a net quantity of suspended sediment was transported seaward from upper Kings Bay and Marianna Creek. A net landward transport of suspended sediment computed at the St. Marys Entrance indicated areas seaward of St. Marys Entrance may be supplying sediment to the shoaling areas of the estuary, including lower Kings Bay. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834060","usgsCitation":"McConnell, J.B., Radtke, D.B., Hale, T., and Buell, G.R., 1983, A preliminary appraisal of sediment sources and transport in Kings Bay and vicinity, Georgia and Florida: U.S. Geological Survey Water-Resources Investigations Report 83-4060, vi, 68 p. :ill., map ;28 cm., https://doi.org/10.3133/wri834060.","productDescription":"vi, 68 p. :ill., map ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":54475,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4060/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123500,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4060/report-thumb.jpg"}],"country":"United States","state":"Florida, Georgia","otherGeospatial":"Kings 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R.","contributorId":57103,"corporation":false,"usgs":true,"family":"Buell","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":194778,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":57313,"text":"wdrFL821B - 1983 - Water resources data, Florida, water year 1982; Volume 1B. Northeast Florida ground water","interactions":[],"lastModifiedDate":"2023-01-10T19:43:31.856753","indexId":"wdrFL821B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"FL-82-1B","title":"Water resources data, Florida, water year 1982; Volume 1B. Northeast Florida ground water","docAbstract":"Water resources data for the 1982 water year for northeast Florida consist of records of stage, discharge, and water quality of streams; elevation and water quality of lakes and reservoirs; water-levels and water quality of wells; and discharge and water quality of springs. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. 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 Florida.
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Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:05:01","indexId":"ofr83624A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-624","chapter":"A","title":"Preliminary chart A-A' showing electric log correlation, facies, and test data of some Cretaceous and Tertiary rocks, Wind River basin, Wyoming","language":"ENGLISH","doi":"10.3133/ofr83624A","usgsCitation":"Fox, J.E., and Priestley, R.L., 1983, Preliminary chart A-A' showing electric log correlation, facies, and test data of some Cretaceous and Tertiary rocks, Wind River basin, Wyoming: U.S. Geological Survey Open-File Report 83-624, 8 well logs on 1 sheet :photocopy ;on sheet 212 x 108 cm., https://doi.org/10.3133/ofr83624A.","productDescription":"8 well logs on 1 sheet :photocopy ;on sheet 212 x 108 cm.","costCenters":[],"links":[{"id":135297,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20950,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0624a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20951,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0624a/plate-1-preview.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c7a9","contributors":{"authors":[{"text":"Fox, J. 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Excessive rainfall (12.6 inches in Raytown, MO) caused flash flooding during the nighttime and early daylight hours. Four deaths and damages unofficially estimated in excess of $30 million, occurred in the three-county area of Jackson, Cass, and Clay counties. Peak discharges were determined at 12 current or discontinued streamflow-gaging stations and 17 miscellaneous sites. Flood peaks and volumes at many locations exceeded estimated 100-year recurrence-interval floods and equaled or exceeded the 1977 floods in some drainage basins. Significant flooding occurred in the Blue, East Fork Little Blue, and Little Blue River basins and in the Rock, Wilkerson, Sni-A-Bar, Shoal, and Big Creek drainage basins. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834141","usgsCitation":"Becker, L., Alexander, T., and Waite, L., 1983, Floods in Kansas City, Missouri and vicinity, August 12-13, 1982: U.S. Geological Survey Water-Resources Investigations Report 83-4141, iv, 35 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834141.","productDescription":"iv, 35 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123298,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4141/report-thumb.jpg"},{"id":54926,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4141/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e498de4b07f02db5b060e","contributors":{"authors":[{"text":"Becker, L.D.","contributorId":84797,"corporation":false,"usgs":true,"family":"Becker","given":"L.D.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":195862,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alexander, T.W.","contributorId":9680,"corporation":false,"usgs":true,"family":"Alexander","given":"T.W.","email":"","affiliations":[],"preferred":false,"id":195860,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waite, L.A.","contributorId":40995,"corporation":false,"usgs":true,"family":"Waite","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":195861,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":36556,"text":"fwsobs82_10_41 - 1983 - Habitat Suitability Information: Blacknose dace","interactions":[],"lastModifiedDate":"2022-02-09T15:36:36.044016","indexId":"fwsobs82_10_41","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/10.41","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Information: Blacknose dace","docAbstract":"A review and synthesis of existing information were used to develop riverine and lacustrine habitat models for Blacknose dace, a freshwater species. The models are scaled to produce an index of habitat suitability between 0 (unsuitable habitat) to 1 (optimally suitable habitat) for freshwater, marine, and estuarine areas of the continental United States. Habitat suitability indexes (HSI's) are designed for use with the habitat evaluation procedures developed by the U.S. Fish and Wildlife Service.\r\n\r\nAlso included are discussions of Suitability Index (SI) curves as used in the Instream Flow Incremental Methodology (IFIM) and SI curves available for an IFIM analysis of Blacknose dace.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Trial, J.G., Stanley, J.G., Batcheller, M., Gebhart, G., Maughan, O.E., and Nelson, P.C., 1983, Habitat Suitability Information: Blacknose dace: FWS/OBS 82/10.41, vi, 28 p.","productDescription":"vi, 28 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":164614,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6496d3","contributors":{"authors":[{"text":"Trial, Joan G.","contributorId":91156,"corporation":false,"usgs":true,"family":"Trial","given":"Joan","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":216536,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stanley, Jon G.","contributorId":62958,"corporation":false,"usgs":true,"family":"Stanley","given":"Jon","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":216533,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Batcheller, Mary","contributorId":30672,"corporation":false,"usgs":true,"family":"Batcheller","given":"Mary","email":"","affiliations":[],"preferred":false,"id":216531,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gebhart, Gary","contributorId":82764,"corporation":false,"usgs":true,"family":"Gebhart","given":"Gary","email":"","affiliations":[],"preferred":false,"id":216535,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Maughan, O. Eugene","contributorId":43006,"corporation":false,"usgs":true,"family":"Maughan","given":"O.","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":216532,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Nelson, Patrick C.","contributorId":68799,"corporation":false,"usgs":true,"family":"Nelson","given":"Patrick","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":216534,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":61279,"text":"mf1661A - 1983 - Preliminary surficial geologic map of the northern part of the Tyonek B-5 Quadrangle, south-central Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:10:32","indexId":"mf1661A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1661","chapter":"A","title":"Preliminary surficial geologic map of the northern part of the Tyonek B-5 Quadrangle, south-central Alaska","language":"ENGLISH","doi":"10.3133/mf1661A","usgsCitation":"Yehle, L., Schmoll, H., and Gardner, C.A., 1983, Preliminary surficial geologic map of the northern part of the Tyonek B-5 Quadrangle, south-central Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 1661, 1 map ;36 x 63 cm., on sheet 99 x 70 cm, folded in envelope 25 x 32 cm., https://doi.org/10.3133/mf1661A.","productDescription":"1 map ;36 x 63 cm., on sheet 99 x 70 cm, folded in envelope 25 x 32 cm.","costCenters":[],"links":[{"id":106269,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7788.htm","linkFileType":{"id":5,"text":"html"},"description":"7788"},{"id":179734,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -151.8675,61.416666666666664 ], [ -151.8675,61.5 ], [ -151.5,61.5 ], [ -151.5,61.416666666666664 ], [ -151.8675,61.416666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aabe4b07f02db669b1d","contributors":{"authors":[{"text":"Yehle, L. A.","contributorId":44536,"corporation":false,"usgs":true,"family":"Yehle","given":"L. A.","affiliations":[],"preferred":false,"id":265308,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schmoll, H. R.","contributorId":71543,"corporation":false,"usgs":true,"family":"Schmoll","given":"H. R.","affiliations":[],"preferred":false,"id":265309,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gardner, C. A.","contributorId":75916,"corporation":false,"usgs":true,"family":"Gardner","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":265310,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":57270,"text":"wdrMN822 - 1983 - Water Resources Data, Minnesota Water Year 1982, Volume 2: Upper Mississippi and Missouri River Basins","interactions":[],"lastModifiedDate":"2012-02-02T00:12:17","indexId":"wdrMN822","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"MN-82-2","title":"Water Resources Data, Minnesota Water Year 1982, Volume 2: Upper Mississippi and Missouri River Basins","language":"ENGLISH","doi":"10.3133/wdrMN822","usgsCitation":"Gunard, K., Hess, J., Zirbel, J., and Cornelius, C., 1983, Water Resources Data, Minnesota Water Year 1982, Volume 2: Upper Mississippi and Missouri River Basins: U.S. Geological Survey Water Data Report MN-82-2, 449 p., 9 fig., https://doi.org/10.3133/wdrMN822.","productDescription":"449 p., 9 fig.","costCenters":[],"links":[{"id":184911,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1982/mn-82-2/report-thumb.jpg"},{"id":88255,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1982/mn-82-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb631","contributors":{"authors":[{"text":"Gunard, K.T.","contributorId":103733,"corporation":false,"usgs":true,"family":"Gunard","given":"K.T.","affiliations":[],"preferred":false,"id":256530,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hess, J.H.","contributorId":100465,"corporation":false,"usgs":true,"family":"Hess","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":256529,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zirbel, J.L.","contributorId":70837,"corporation":false,"usgs":true,"family":"Zirbel","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":256528,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cornelius, C.E.","contributorId":106190,"corporation":false,"usgs":true,"family":"Cornelius","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":256531,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ]}