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,{"id":28776,"text":"wri7610 - 1976 - Geohydrology of the Anza-Terwilliger area, Riverside County, California","interactions":[],"lastModifiedDate":"2016-09-29T15:24:02","indexId":"wri7610","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-10","title":"Geohydrology of the Anza-Terwilliger area, Riverside County, California","docAbstract":"<p>The Anza-Terwilliger area consists of about 96 square miles (24-9 square kilometres) in the upper parts of the Santa Margarita River and Coyote Creek drainage basins in Riverside County, Calif., about 90 miles (145 kilometres) southeast of Los Angeles. This report deals with geology, steady state and transient state of ground water, net depletion of ground water, surface-water flow, precipitation, chemistry of water, land and water use, and gravity data for the Anza-Terwilliger area. The data indicate that the rate of ground-water depletion ha's accelerated since 1950. Pumping depressions adjacent to the Cahuilla Indian Reservation have increased the hydraulic gradient and are.causing water beneath the reservation to flow toward these depressions. Total depletion of ground water since 1950 is about 14,000 acre-feet (17.3 cubic hectometres). Chemical analyses indicate that the ground water in local areas contains concentrations of nitrate above that recommended by the Environmental Protection Agency for human consumption.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Menlo Park, CA","doi":"10.3133/wri7610","usgsCitation":"Moyle, W.R., 1976, Geohydrology of the Anza-Terwilliger area, Riverside County, California: U.S. Geological Survey Water-Resources Investigations Report 76-10, iv, 25 p., https://doi.org/10.3133/wri7610.","productDescription":"iv, 25 p.","numberOfPages":"32","costCenters":[],"links":[{"id":159583,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri7610.PNG"},{"id":329144,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0010/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Riverside County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.83685302734375,\n              33.456651301881855\n            ],\n            [\n              -116.83685302734375,\n              33.601466321878846\n            ],\n            [\n              -116.51550292968749,\n              33.601466321878846\n            ],\n            [\n              -116.51550292968749,\n              33.456651301881855\n            ],\n            [\n              -116.83685302734375,\n              33.456651301881855\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a89fb","contributors":{"authors":[{"text":"Moyle, W. R. Jr.","contributorId":85938,"corporation":false,"usgs":true,"family":"Moyle","given":"W.","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":200377,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10403,"text":"ofr76673 - 1976 - Effects of drain wells on the ground-water quality of the western Snake Plain Aquifer, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:06:32","indexId":"ofr76673","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-673","title":"Effects of drain wells on the ground-water quality of the western Snake Plain Aquifer, Idaho","docAbstract":"Approximately 3,100 drain wells injects irrigation waste water, urban runoff, septic-tank effluent, and industrial waste water into the Snake Plain aquifer in Minidoka, Gooding, Jerome, and Lincoln Counties, Idaho. About 29,000 acre-feet of irrigation waste water, 100 acre-feet of urban runoff, 400 acre-feet of septic-tank effluent, and 1,000 acre-feet of industrial waste water are injected annually. The quality of irrigation waste water is highly variable, depending upon its source, method and rate of application, amount of fertilizer added, and other factors. The quality of urban runoff water is generally much better than irrigation waste water. Septic-tank effluent is relatively high in nutrient concentrations. Chloride concentrations also are high, and bacterial concentrations are exceedingly high. The only industrial waste water sampled during this study had been used for cooling. No chemical changes were noted, but temperature was significantly increased. The data indicate that drain-well inflow does move appreciable distances through the aquifer and can be detected in downgradient wells. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76673","usgsCitation":"Moreland, J.A., Seitz, H.R., and LaSala, A.M., 1976, Effects of drain wells on the ground-water quality of the western Snake Plain Aquifer, Idaho: U.S. Geological Survey Open-File Report 76-673, 81 leaves :maps (3 fold.) ;28 cm.; (83 p., 1 sheet, scale 1:31,680 - PGS), https://doi.org/10.3133/ofr76673.","productDescription":"81 leaves :maps (3 fold.) ;28 cm.; (83 p., 1 sheet, scale 1:31,680 - PGS)","costCenters":[],"links":[{"id":143815,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0673/report-thumb.jpg"},{"id":38249,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0673/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38250,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0673/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38251,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0673/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38252,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0673/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38253,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0673/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38254,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0673/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38255,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0673/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38256,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0673/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38257,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0673/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38258,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0673/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"31680","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2fe4b07f02db615c2c","contributors":{"authors":[{"text":"Moreland, Joe A.","contributorId":48171,"corporation":false,"usgs":true,"family":"Moreland","given":"Joe","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161328,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Seitz, Harold R.","contributorId":61814,"corporation":false,"usgs":true,"family":"Seitz","given":"Harold","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":161329,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"LaSala, Albert Mario","contributorId":74754,"corporation":false,"usgs":true,"family":"LaSala","given":"Albert","email":"","middleInitial":"Mario","affiliations":[],"preferred":false,"id":161330,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26135,"text":"wri76109 - 1976 - Magnitude and frequency of floods in Nebraska","interactions":[],"lastModifiedDate":"2016-07-11T11:24:18","indexId":"wri76109","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-109","title":"Magnitude and frequency of floods in Nebraska","docAbstract":"<p>Estimates of flood characteristics with recurrence intervals up to 100 years can be obtained at most sites in Nebraska by use of techniques presented in this report. Instructions, equations, and graphs are presented to aid the design engineer in estimating the magnitude and frequency of floods.</p>\n<p>For natural-flow streams, the estimating equations and graphical solutions are based on regional relations between floods of a specific return period and selected basin characteristics. Nebraska was subdivided into five hydrologic regions by means of regressions and residuals from the regressions. The boundaries of Regions 1 and 2 were determined to a great extent by differences in soil type. The divisions between Region 2 and Region 4 were also determined by differences in soil type. Boundaries of Region 3 and Region 5 are along or near basin divides.</p>\n<p>Flood magnitude and frequency solution diagrams are presented for major controlled streams such as the North Platte, South Platte, Platte, and Republican Rivers. Flood information on small controlled streams is limited to available station data.</p>\n<p>Flood characteristics are tabulated for 303 gaging stations having 13 or more years of record. These flood characteristics provide the best information on floods at these gaged sites.</p>\n<p>Observed maximum flood peaks at 303 gaging stations with 13 or more years of record and significant peaks at 57 short-term stations and 31 miscellaneous sites are useful in designing flood-control works for maximum safety from flood damage. 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,{"id":10378,"text":"ofr76808 - 1976 - Outline of the water resources of the Status Creek basin, Yakima Indian Reservation, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr76808","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-808","title":"Outline of the water resources of the Status Creek basin, Yakima Indian Reservation, Washington","docAbstract":"On the Yakima Indian Reservation, Washington, only about 5 percent of the Satus Creek basin--in the relatively flat eastern lowland adjacent to and including part of the Yakima River lowland--is agriculturally developed, mostly through irrigation. Because the basin 's streams do not contain adequate water for irrigation, most irrigation is by canal diversion from the adjoining Toppenish Creek basin. Irrigation application of as much as 9.25 acre-feet per acre per year, combined with the presence of poorly drained silt and clay layers in this area, and the natural upward discharge of ground water from deeper aquifers (water-bearing layers), has contributed to a waterlogging problem, which has affected about 10,500 acres, or about 25 percent of the irrigated area. In the upland of the basin, a large average annual base flow of about 30 cubic feet per second in Logy Creek indicates the presence of a potentially highly productive aquifer in young (shallow) basalt lavas underlying the higher western parts of the upland. This aquifer may provide a reservoir from which streamflow may be augmented by ground-water pumping or, alternatively, it may be used as a source of ground water for irrigation of upland areas directly. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76808","usgsCitation":"Molenaar, D., 1976, Outline of the water resources of the Status Creek basin, Yakima Indian Reservation, Washington: U.S. Geological Survey Open-File Report 76-808, ix, 31 leaves :ill., maps(2 fold.) ;27 cm., https://doi.org/10.3133/ofr76808.","productDescription":"ix, 31 leaves :ill., maps(2 fold.) ;27 cm.","costCenters":[],"links":[{"id":142299,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a33d","contributors":{"authors":[{"text":"Molenaar, Dee","contributorId":34485,"corporation":false,"usgs":true,"family":"Molenaar","given":"Dee","email":"","affiliations":[],"preferred":false,"id":161284,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43600,"text":"ofr7639 - 1976 - Land use and land cover and associated maps for Sacramento, California","interactions":[],"lastModifiedDate":"2012-02-02T00:11:02","indexId":"ofr7639","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-39","title":"Land use and land cover and associated maps for Sacramento, California","language":"ENGLISH","doi":"10.3133/ofr7639","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Land use and land cover and associated maps for Sacramento, California: U.S. Geological Survey Open-File Report 76-39, 4 maps., https://doi.org/10.3133/ofr7639.","productDescription":"4 maps.","costCenters":[],"links":[{"id":168656,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af46f","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":531256,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3452,"text":"cir715H - 1976 - Reservoir-system model for the Willamette River basin, Oregon","interactions":[],"lastModifiedDate":"2017-02-03T13:57:45","indexId":"cir715H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"715","chapter":"H","title":"Reservoir-system model for the Willamette River basin, Oregon","docAbstract":"For nearly half a century the Willamette River in Oregon experienced severe dissolved-oxygen problems related to large loads of organically rich waste waters from industries and municipalities. Since the mid-1950 's dissolved oxygen quality has gradually improved owing to low-flow augmentation, the achievement of basinwide secondary treatment, and the use of other waste-management practices. As a result, summer dissolved-oxygen levels have increased, salmon runs have returned, and the overall effort is widely regarded as a singular water-quality success. To document the improved dissolved-oxygen regimen, the U.S. Geological Survey conducted intensive studies of the Willamette during the summer low-flow seasons of 1973 and 1974. During each summer the mean daily dissolved-oxygen levels were found to be higher than 5 milligrams per liter throughout the river. Because of the basinwide secondary treatment, carbonaceous deoxygenation rates were low. In addition, almost half of the biochemical oxygen demand entering the Willamette was from diffuse (nonpoint) sources rather than outfalls. These results indicated that point-source biochemical oxygen demand was no longer the primary cause of dissolved-oxygen depletion. Instead, the major causes of deoxygenation were nitrification in a shallow ' surface active ' reach below Salem and an anomalous oxygen demand (believed to be primarily of benthal origin) in Portland Harbor. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/cir715H","usgsCitation":"Shearman, J.O., 1976, Reservoir-system model for the Willamette River basin, Oregon: U.S. Geological Survey Circular 715, vi, p H1-H22, ill., map ;26 cm. , https://doi.org/10.3133/cir715H.","productDescription":"vi, p H1-H22, ill., map ;26 cm. ","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":30464,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1976/0715h/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123995,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1976/0715h/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a054","contributors":{"authors":[{"text":"Shearman, James O.","contributorId":95048,"corporation":false,"usgs":true,"family":"Shearman","given":"James","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":146947,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28872,"text":"wri7673 - 1976 - Geology and ground-water resources of Union County, New Jersey","interactions":[{"subject":{"id":56040,"text":"ofr70243 - 1970 - Geology and ground-water resources of Union County, New Jersey","indexId":"ofr70243","publicationYear":"1970","noYear":false,"title":"Geology and ground-water resources of Union County, New Jersey"},"predicate":"SUPERSEDED_BY","object":{"id":28872,"text":"wri7673 - 1976 - Geology and ground-water resources of Union County, New Jersey","indexId":"wri7673","publicationYear":"1976","noYear":false,"title":"Geology and ground-water resources of Union County, New Jersey"},"id":1}],"lastModifiedDate":"2019-11-12T14:33:31","indexId":"wri7673","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations 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This report contains discharge records for 89 gaging stations; stage and contents for 14 lakes and reservoirs; water quality for 2 gaging stations, 46 partial-record flow stations, and water levels for 20 observation wells. Also included are data for 12 crest-stage partial-record stations and 27 low-flow partial-record stations. Additional 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 Pennsylvania.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrPA753","collaboration":"Prepared in cooperation with the Pennsylvania Department of Environmental Resources and with other State, municipal, and Federal agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Water resources data for Pennsylvania, water year 1975; Volume 3. 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,{"id":43510,"text":"ofr7611 - 1976 - Land use and land cover and associated maps for Tallahassee, Fla.","interactions":[],"lastModifiedDate":"2012-02-02T00:11:01","indexId":"ofr7611","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-11","title":"Land use and land cover and associated maps for Tallahassee, Fla.","language":"ENGLISH","doi":"10.3133/ofr7611","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Land use and land cover and associated maps for Tallahassee, Fla.: U.S. Geological Survey Open-File Report 76-11, 7 maps., https://doi.org/10.3133/ofr7611.","productDescription":"7 maps.","costCenters":[],"links":[{"id":168920,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af59f","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":531212,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10877,"text":"ofr76717 - 1976 - Numerical modeling of subsurface radioactive solute transport from waste seepage ponds at the Idaho National Engineering Laboratory","interactions":[],"lastModifiedDate":"2012-02-02T00:06:33","indexId":"ofr76717","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-717","title":"Numerical modeling of subsurface radioactive solute transport from waste seepage ponds at the Idaho National Engineering Laboratory","docAbstract":"Aqueous chemical and low-level radioactive effluents have been disposed to seepage ponds since 1952 at the Idaho National Engineering Laboratory. The solutions percolate toward the Snake River Plain aquifer (135 m below) through interlayered basalts and unconsolidated sediments and an extensive zone of ground water perched on a sedimentary layer about 40 m beneath the ponds. A three-segment numerical model was developed to simulate the system, including effects of convection, hydrodynamic dispersion, radioactive decay, and adsorption. Simulated hydraulics and solute migration patterns for all segments agree adequately with the available field data. The model can be used to project subsurface distributions of waste solutes under a variety of assumed conditions for the future. Although chloride and tritium reached the aquifer several years ago, the model analysis suggests that the more easily sorbed solutes, such as cesium-137 and strontium-90, would not reach the aquifer in detectable concentrations within 150 years for the conditions assumed. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76717","usgsCitation":"Robertson, J.B., 1976, Numerical modeling of subsurface radioactive solute transport from waste seepage ponds at the Idaho National Engineering Laboratory: U.S. Geological Survey Open-File Report 76-717, vi, 59, [39] leaves :ill., maps ;28 cm., https://doi.org/10.3133/ofr76717.","productDescription":"vi, 59, [39] leaves :ill., maps ;28 cm.","costCenters":[],"links":[{"id":143708,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a7fe6","contributors":{"authors":[{"text":"Robertson, John B.","contributorId":36562,"corporation":false,"usgs":true,"family":"Robertson","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":162120,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65954,"text":"i967 - 1976 - Topographic map of the Surtis Major Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:10","indexId":"i967","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"967","subseriesTitle":"NONE","title":"Topographic map of the Surtis Major Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i967","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Topographic map of the Surtis Major Quadrangle of Mars: U.S. Geological Survey IMAP 967, 1 map :col. ;37 x 53 cm. on sheet 86 x 70 cm. fold. in envelope 30 x 24 cm., https://doi.org/10.3133/i967.","productDescription":"1 map :col. ;37 x 53 cm. on sheet 86 x 70 cm. fold. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190436,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101265,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0967/plate-1.pdf","size":"4016","linkFileType":{"id":1,"text":"pdf"}}],"scale":"5000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629bf4","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":534307,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10808,"text":"ofr76792 - 1976 - Simulation procedure for modeling transient water table and artesian stress and response","interactions":[],"lastModifiedDate":"2012-02-02T00:06:32","indexId":"ofr76792","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-792","title":"Simulation procedure for modeling transient water table and artesian stress and response","docAbstract":"The series of computer programs described in this report were designed specifically to model the ground-water regime in sufficient detail to determine the effects of the imposition of various types of stress upon the system, and to display the results in a convenient manner during calibration and when presenting projected data. SUPERMOCK simulates the ground-water system and DATE and HYDROG aid in the display of computed data. During calibration, DATE is especially useful because it has the optional feature of comparing computed data with observed data. Although the programs can be run independently, experience dictates that for best results the three should be run as steps in the same job. English units of inches, feet, and days are used in each of the programs. The units for any parameters not given in the text are clearly specified in the instructions for input to the individual programs. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76792","usgsCitation":"Reed, J., Bedinger, M.S., and Terry, J.E., 1976, Simulation procedure for modeling transient water table and artesian stress and response: U.S. Geological Survey Open-File Report 76-792, 173 p., 7 tables :ill. (some fold.) ;28 cm., https://doi.org/10.3133/ofr76792.","productDescription":"173 p., 7 tables :ill. (some fold.) ;28 cm.","costCenters":[],"links":[{"id":112954,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0792/report.pdf","size":"6966","linkFileType":{"id":1,"text":"pdf"}},{"id":143889,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0792/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f1c7b","contributors":{"authors":[{"text":"Reed, J.E.","contributorId":41801,"corporation":false,"usgs":true,"family":"Reed","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":162004,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bedinger, M. S.","contributorId":65452,"corporation":false,"usgs":true,"family":"Bedinger","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":162005,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Terry, J. E.","contributorId":87930,"corporation":false,"usgs":true,"family":"Terry","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":162006,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26944,"text":"wri769 - 1976 - A technique for estimating the time of travel of water in Indiana streams","interactions":[],"lastModifiedDate":"2016-05-16T10:23:38","indexId":"wri769","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-9","title":"A technique for estimating the time of travel of water in Indiana streams","docAbstract":"<p>Estimates of the traveltime of waterborne particles in streams is important for pollution studies and in the event of spills of contaminants. This report provides data for the 16 Indiana streams on which time-of-travel information has been obtained and a means for estimating the velocity of any naturally flowing stream in Indiana with a drainage area of 80 square miles (210 square kilometres) or more.</p>\n<p>Measured velocity rates compiled from the time-of-travel data collected in Indiana are releated to 25, 50, 100, and 200 percent of the average discharge of streams shown in this report. Velocities at these discharges are significantly related to their respective watershed characteristics (average discharge and slope). Generalized relations of the velocities as functions of the streams' watershed characteristics are developed as multivariate regression equations using the data from each of the measured streams.</p>\n<p>Examples of uses and applications of the measured data and the predictive equations are given.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/wri769","collaboration":"Prepared in cooperation with Indiana Department of Natural Resources and Indiana State Board of Health","usgsCitation":"Eikenberry, S.E., and Davis, L.G., 1976, A technique for estimating the time of travel of water in Indiana streams: U.S. Geological Survey Water-Resources Investigations Report 76-9, vi, 39 p., https://doi.org/10.3133/wri769.","productDescription":"vi, 39 p.","startPage":"1","endPage":"39","numberOfPages":"48","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":321229,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri769.GIF"},{"id":287931,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0009/report.pdf"}],"country":"United 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,{"id":27759,"text":"wri7535 - 1976 - Statistical summaries of Indiana streamflow data","interactions":[{"subject":{"id":27759,"text":"wri7535 - 1976 - Statistical summaries of Indiana streamflow data","indexId":"wri7535","publicationYear":"1976","noYear":false,"title":"Statistical summaries of Indiana streamflow data"},"predicate":"SUPERSEDED_BY","object":{"id":12485,"text":"ofr8962 - 1989 - Statistical summary of streamflow data for Indiana","indexId":"ofr8962","publicationYear":"1989","noYear":false,"title":"Statistical summary of streamflow data for Indiana"},"id":1}],"supersededBy":{"id":12485,"text":"ofr8962 - 1989 - Statistical summary of streamflow data for Indiana","indexId":"ofr8962","publicationYear":"1989","noYear":false,"title":"Statistical summary of streamflow data for Indiana"},"lastModifiedDate":"2020-08-08T00:10:31.472491","indexId":"wri7535","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"75-35","title":"Statistical summaries of Indiana streamflow data","docAbstract":"<p><span>Complete statistical analyses are presented in tabular form for all </span><span>gaging stations in Indiana, regardless of length of record. Each station </span><span>analysis includes lowest and highest mean daily discharges, flow duration, </span><span>statistics on normal monthly means, statistics on normal annual means, </span><span>statistics on log monthly means, statistics on log annual means, and annual </span><span>peak discharges.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7535","collaboration":"Prepared in cooperation with Indiana Department of Natural Resources, Division of Water","usgsCitation":"Horner, R., 1976, Statistical summaries of Indiana streamflow data: U.S. Geological Survey Water-Resources Investigations Report 75-35, iv, 526 p., https://doi.org/10.3133/wri7535.","productDescription":"iv, 526 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science 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,{"id":55209,"text":"wdrFL753 - 1976 - Water resources data for Florida, water year 1975, v. 3, west-central Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:11:57","indexId":"wdrFL753","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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-75-3","title":"Water resources data for Florida, water year 1975, v. 3, west-central Florida","language":"ENGLISH","doi":"10.3133/wdrFL753","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Water resources data for Florida, water year 1975, v. 3, west-central Florida: U.S. Geological Survey Water Data Report FL-75-3, 1209 p., https://doi.org/10.3133/wdrFL753.","productDescription":"1209 p.","costCenters":[],"links":[{"id":181198,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f72fd","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":532303,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29405,"text":"wri7626 - 1976 - Water resources of the Warm Springs Indian Reservation, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:09:02","indexId":"wri7626","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-26","title":"Water resources of the Warm Springs Indian Reservation, Oregon","docAbstract":"Water-resources data for the 1,000-square-mile Warm Springs Indian Reservation in north-central Oregon were obtained and evaluated. The area is bounded on the west by the crest of the Cascade Range and on the south and east by the Metolius and Deschutes Rivers. The mountainous western part is underlain by young volcanic rocks, and the plateaus and valleys of the eastern part are underlain by basalt, tuff, sand, and gravel of Tertiary and Quaternary ages. There are numerous springs, some developed for stock use, and about 50 domestic and community wells; yields are small, ranging from less than 1 to as much as 25 gallons per minute. Chemical quality of most ground water is suitable for stock or human consumption and for irrigation. Average flows of the Warm Springs River, Metolius River, and Deschutes River are 440, 1,400, and 4,040 cubic feet per second (cfs), respectively. Shitike Creek, which has an average flow of 108 cfs had a peak of 4,000 cfs in January 1974. Most streams have fewer than 100 milligrams per liter (mg/liter) of dissolved solids. Chemical and biological quality of the mountain lakes is also good; of 10 lakes studied, all had fewer than 50 mg/liter of dissolved solids and none had measurable fecal coliform bacteria. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri7626","usgsCitation":"Robison, J.H., and Laenen, A., 1976, Water resources of the Warm Springs Indian Reservation, Oregon: U.S. Geological Survey Water-Resources Investigations Report 76-26, v, 85 p. :ill., maps ;27 cm., https://doi.org/10.3133/wri7626.","productDescription":"v, 85 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":260337,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0026/plate-1.pdf"},{"id":260338,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0026/report.pdf"},{"id":260339,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0026/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699bc3","contributors":{"authors":[{"text":"Robison, J. H.","contributorId":60183,"corporation":false,"usgs":true,"family":"Robison","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":201477,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Laenen, Antonius","contributorId":107673,"corporation":false,"usgs":true,"family":"Laenen","given":"Antonius","email":"","affiliations":[],"preferred":false,"id":201478,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3111,"text":"wsp2113 - 1976 - Surface water supply of the United States, 1966-70, Part 5, Hudson Bay and upper Mississippi River basins, v. 1, Hudson Bay basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:36","indexId":"wsp2113","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"2113","title":"Surface water supply of the United States, 1966-70, Part 5, Hudson Bay and upper Mississippi River basins, v. 1, Hudson Bay basin","language":"ENGLISH","publisher":"USGS,","doi":"10.3133/wsp2113","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Surface water supply of the United States, 1966-70, Part 5, Hudson Bay and upper Mississippi River basins, v. 1, Hudson Bay basin: U.S. Geological Survey Water Supply Paper 2113, 425 p. ;23 cm., https://doi.org/10.3133/wsp2113.","productDescription":"425 p. ;23 cm.","costCenters":[],"links":[{"id":139356,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2113/report-thumb.jpg"},{"id":30023,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2113/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db692078","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":528088,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55207,"text":"wdrFL751 - 1976 - Water resources data for Florida, water year 1975; Volume 1. Northern Florida--surface water, ground water, and quality of water","interactions":[],"lastModifiedDate":"2023-01-06T18:49:25.186301","indexId":"wdrFL751","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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-75-1","title":"Water resources data for Florida, water year 1975; Volume 1. Northern Florida--surface water, ground water, and quality of water","docAbstract":"<p>Water resources data for the 1975 water year for northern 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.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrFL751","collaboration":"Prepared in cooperation with the State of Florida and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Water resources data for Florida, water year 1975; Volume 1. 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,{"id":55208,"text":"wdrFL752 - 1976 - Water resources data for Florida, water year 1975, v. 2, southern Florida","interactions":[],"lastModifiedDate":"2025-05-22T18:29:43.246722","indexId":"wdrFL752","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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-75-2","title":"Water resources data for Florida, water year 1975, v. 2, southern Florida","docAbstract":"<p>Water resources data for the 1975 water year for southern Florida consist of records of stage, discharge, and water quality of streams; elevation and water quality of lakes and reservoirs; and water-levels and water quality of wells and 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.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrFL752","collaboration":"Prepared in cooperation with the State of Florida and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Water resources data for Florida, water year 1975, v. 2, southern Florida: U.S. Geological Survey Water Data Report FL-75-2, xiv, 1451 p., https://doi.org/10.3133/wdrFL752.","productDescription":"xiv, 1451 p.","costCenters":[],"links":[{"id":486419,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1975/fl-75-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":181197,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1975/fl-75-2/report-thumb.jpg"}],"country":"United 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,{"id":738,"text":"wsp2102 - 1976 - Surface water supply of the United States, 1966-70, Part 1, North Atlantic slope basins, v. 2, Basins from New York to Delaware","interactions":[],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp2102","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"2102","title":"Surface water supply of the United States, 1966-70, Part 1, North Atlantic slope basins, v. 2, Basins from New York to Delaware","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp2102","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Surface water supply of the United States, 1966-70, Part 1, North Atlantic slope basins, v. 2, Basins from New York to Delaware: U.S. Geological Survey Water Supply Paper 2102, x, 985 p. :ill. ;23 cm., https://doi.org/10.3133/wsp2102.","productDescription":"x, 985 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136351,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2102/report-thumb.jpg"},{"id":25307,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2102/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db6941aa","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":527674,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4724,"text":"twri07C1 - 1976 - Finite difference model for aquifer simulation in two dimensions with results of numerical experiments","interactions":[{"subject":{"id":56027,"text":"ofr70211 - 1970 - A program to simulate and aquifer using alternating direction implicit-iterative procedure","indexId":"ofr70211","publicationYear":"1970","noYear":false,"title":"A program to simulate and aquifer using alternating direction implicit-iterative procedure"},"predicate":"SUPERSEDED_BY","object":{"id":4724,"text":"twri07C1 - 1976 - Finite difference model for aquifer simulation in two dimensions with results of numerical experiments","indexId":"twri07C1","publicationYear":"1976","noYear":false,"title":"Finite difference model for aquifer simulation in two dimensions with results of numerical experiments"},"id":1}],"lastModifiedDate":"2021-04-05T15:32:12.694992","indexId":"twri07C1","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"07-C1","title":"Finite difference model for aquifer simulation in two dimensions with results of numerical experiments","docAbstract":"<p>The model will simulate ground-water flow in an artesian aquifer, a water-table aquifer, or a combined artesian and water-table aquifer. The aquifer may be heterogeneous and anisotropic and have irregular boundaries. The source term in the flow equation may include well discharge, constant recharge, leakage from confining beds in which the effects of storage are considered, and evapotranspiration as a linear function of depth to water. </p><p>The theoretical development includes presentation of the appropriate flow equations and derivation of the finite-difference approximations (written for a variable grid). The documentation emphasizes the numerical techniques that can be used for solving the simultaneous equations and describes the results of numerical experiments using these techniques. Of the three numerical techniques available in the model, the strongly implicit procedure, in general, requires less computer time and has fewer numerical difficulties than do the iterative alternating direction implicit procedure and line successive overrelaxation (which includes a two-dimensional correction procedure to accelerate convergence). </p><p>The documentation includes a flow chart, program listing, an example simulation, and sections on designing an aquifer model and requirements for data input. It illustrates how model results can be presented on the line printer and pen plotters with a program that utilizes the graphical display software available from the Geological Survey Computer Center Division. In addition the model includes options for reading input data from a disk and writing intermediate results on a disk.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/twri07C1","issn":"0565-596X","usgsCitation":"Trescott, P.C., Pinder, G.F., and Larson, S.P., 1976, Finite difference model for aquifer simulation in two dimensions with results of numerical experiments (Revision -1976): U.S. Geological Survey Techniques of Water-Resources Investigations 07-C1, vi, 116 p., https://doi.org/10.3133/twri07C1.","productDescription":"vi, 116 p.","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":384872,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/twri/twri7-c1/html/pdf/TWRI_7-C1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139097,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":352,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri7-c1/","linkFileType":{"id":5,"text":"html"}}],"edition":"Revision -1976","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f46b3","contributors":{"authors":[{"text":"Trescott, Peter C.","contributorId":21533,"corporation":false,"usgs":true,"family":"Trescott","given":"Peter","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":149685,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pinder, George Francis","contributorId":99964,"corporation":false,"usgs":true,"family":"Pinder","given":"George","email":"","middleInitial":"Francis","affiliations":[],"preferred":false,"id":149687,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Larson, S. P.","contributorId":34903,"corporation":false,"usgs":true,"family":"Larson","given":"S.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":149686,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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