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,{"id":41837,"text":"ofr88505 - 1988 - Aeromagnetic map of part of the Middleton Island Quadrangle and vicinity, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:11:02","indexId":"ofr88505","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"88-505","title":"Aeromagnetic map of part of the Middleton Island Quadrangle and vicinity, Alaska","language":"ENGLISH","doi":"10.3133/ofr88505","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1988, Aeromagnetic map of part of the Middleton Island Quadrangle and vicinity, Alaska: U.S. Geological Survey Open-File Report 88-505, 1 map :photocopy ;71 x 103 cm., on sheet 93 x 130 cm., https://doi.org/10.3133/ofr88505.","productDescription":"1 map :photocopy ;71 x 103 cm., on sheet 93 x 130 cm.","costCenters":[],"links":[{"id":169034,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79559,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1988/0505/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69795a","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":530653,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41825,"text":"ofr88334 - 1988 - Approximate altitude of water levels in wells in the Chicot and Evangeline aquifers in the Houston area, Texas, spring 1988","interactions":[],"lastModifiedDate":"2016-08-12T15:20:08","indexId":"ofr88334","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"88-334","title":"Approximate altitude of water levels in wells in the Chicot and Evangeline aquifers in the Houston area, Texas, spring 1988","docAbstract":"<p>Two maps show water levels in wells in the Houston, Texas, area in the Chicot aquifer and the Evangeline aquifer, spring 1988. Both the Chicot and the Evangeline aquifers are composed of several sand layers with different potentiometric surfaces. These maps, however, show approximations of single potentiometric surfaces that represent composite hydraulic heads. (USGS)</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr88334","usgsCitation":"Gabrysch, R., Ranzau, C., and Coplin, L., 1988, Approximate altitude of water levels in wells in the Chicot and Evangeline aquifers in the Houston area, Texas, spring 1988: U.S. Geological Survey Open-File Report 88-334, 2 Plates: 17.65 x 12.19 inches and 16.26 x 11.43 inches, https://doi.org/10.3133/ofr88334.","productDescription":"2 Plates: 17.65 x 12.19 inches and 16.26 x 11.43 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":79548,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1988/0334/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79549,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1988/0334/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":168921,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a28a","contributors":{"authors":[{"text":"Gabrysch, R.K.","contributorId":105691,"corporation":false,"usgs":true,"family":"Gabrysch","given":"R.K.","affiliations":[],"preferred":false,"id":225582,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ranzau, C.E. Jr.","contributorId":41831,"corporation":false,"usgs":true,"family":"Ranzau","given":"C.E.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":225580,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coplin, L.S.","contributorId":49366,"corporation":false,"usgs":true,"family":"Coplin","given":"L.S.","affiliations":[],"preferred":false,"id":225581,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":38450,"text":"pp1408E - 1988 - Water use on the Snake River plain, Idaho and eastern Oregon","interactions":[{"subject":{"id":13849,"text":"ofr85559 - 1986 - Water use on the Snake River plain, Idaho and eastern Oregon","indexId":"ofr85559","publicationYear":"1986","noYear":false,"title":"Water use on the Snake River plain, Idaho and eastern Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":38450,"text":"pp1408E - 1988 - Water use on the Snake River plain, Idaho and eastern Oregon","indexId":"pp1408E","publicationYear":"1988","noYear":false,"chapter":"E","title":"Water use on the Snake River plain, Idaho and eastern Oregon"},"id":1}],"lastModifiedDate":"2013-11-19T15:49:31","indexId":"pp1408E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1408","chapter":"E","title":"Water use on the Snake River plain, Idaho and eastern Oregon","docAbstract":"Amounts of water withdrawn and consumptively used for irrigation \nand other uses on the Snake River Plain were estimated to help deter- \nmine hydrologic effects of ground- and surface-water use. Irrigation is \nthe largest off stream use of water on the plain. Surface-water irriga- \ntion began in the 1840's and increased rapidly through the early 1900's. \nUse of ground water for irrigation accelerated after World War II. In \n1980, about 3.1 million acres were irrigated: 1.0 million acres were \nirrigated with about 2.3 million acre-feet of ground water; 2.0 million \nacres were irrigated with about 12.7 million acre-feet of surface water; \n0.1 million acres were irrigated with combined surface and ground water. \nHistorical changes in aquifer storage and spring discharge are closely \nrelated to changes in irrigation practices.\nIndustries, including aquaculture, withdrew an estimated 1.97 million \nacre-feet of water. Withdrawals for other offstream uses, including public \nand rural supplies, totaled 132,000 acre-feet. Hydroelectric power \ngeneration is an economically important instream use of water. In \n1980, about 52 million acre-feet of surface water was used to generate \n2.6 million megawatt-hours of electricity. Native vegetation evapo- \ntranspired an estimated 3.7 million acre-feet, and 900,000 acre-feet \nevaporated from bare ground and open water.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp1408E","usgsCitation":"Goodell, S.A., 1988, Water use on the Snake River plain, Idaho and eastern Oregon: U.S. Geological Survey Professional Paper 1408, vi, 51 p., https://doi.org/10.3133/pp1408E.","productDescription":"vi, 51 p.","numberOfPages":"63","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":122089,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1408e/report-thumb.jpg"},{"id":64930,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1408e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho;Oregon","otherGeospatial":"Snake River Plain","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.0,42.0 ], [ -117.0,45.0 ], [ -111.0,45.0 ], [ -111.0,42.0 ], [ -117.0,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5eff26","contributors":{"authors":[{"text":"Goodell, S. A.","contributorId":38168,"corporation":false,"usgs":true,"family":"Goodell","given":"S.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":219844,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38449,"text":"pp1408D - 1988 - Solute geochemistry of the Snake River plain regional aquifer system, Idaho and eastern Oregon","interactions":[{"subject":{"id":21461,"text":"ofr86247 - 1987 - Solute geochemistry of the Snake River plain regional aquifer system, Idaho and eastern Oregon","indexId":"ofr86247","publicationYear":"1987","noYear":false,"title":"Solute geochemistry of the Snake River plain regional aquifer system, Idaho and eastern Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":38449,"text":"pp1408D - 1988 - Solute geochemistry of the Snake River plain regional aquifer system, Idaho and eastern Oregon","indexId":"pp1408D","publicationYear":"1988","noYear":false,"chapter":"D","title":"Solute geochemistry of the Snake River plain regional aquifer system, Idaho and eastern Oregon"},"id":1}],"lastModifiedDate":"2013-11-19T15:49:12","indexId":"pp1408D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1408","chapter":"D","title":"Solute geochemistry of the Snake River plain regional aquifer system, Idaho and eastern Oregon","docAbstract":"Four geochemical approaches were used to determine chemical \nreactions controlling solute concentrations in the Snake River Plain \nregional aquifer system: (1) calculation of a solute balance within the \naquifer, (2) identification of weathered products in the aquifer frame- \nwork, (3) comparison of thermodynamic mineral saturation indices with \nplausible solute reactions, and (4) comparison of stable-isotope ratios \nof the solutes with those in the aquifer framework. Solutes in the geo- \nthermal groundwater system underlying the main aquifer were examined \nby calculating thermodynamic mineral saturation indices, stable-isotope \nratios, geothermometry, and radiocarbon dating.\nWater budgets, hydrologic arguments, and isotopic analyses for the \neastern Snake River Plain aquifer system demonstrate that most, if not \nall, water is of local meteoric and not juvenile or formation origin. Thus, \nthe solutes must also originate within the basin. Solute balance, isotopic, \nmineralogic, and thermodynamic arguments suggest that about 20 per- \ncent of the solutes leaving the basin are derived from reactions with \nrocks forming the aquifer framework. Most of the remaining solutes \nare introduced from tributary drainage basins.\nMass-balance calculations, thermodynamic arguments, and petro- \ngraphic observations indicate that calcite and silica are precipitated in \nthe aquifer. Petrographic evidence and thermodynamic arguments sug- \ngest that olivine, pyroxene, plagioclase, pyrite, and anhydrite are being \nweathered from the aquifer framework. Large amounts of sodium, \nchloride, and sulfate, relative to their concentration in the igneous rock, \nare being removed from the aquifer. Release of fluids from inclusions \nin the igneous rocks and initial flushing of grain boundaries and pores \nof detrital marine sediments in interbeds are believed to be a major \nsource of these solutes. Identification and quantification of reactions \ncontrolling solute concentrations in ground water in the eastern plain \nindicate that the aquifer is not a large mixing vessel that simply stores \nand transmits water and solutes but is undergoing diagenesis and is \nboth a source and a sink for solutes.\nEvaluation of solute concentrations and stable-isotope ratios of \nhydrogen, oxygen, carbon, and sulfur along groundwater flowpaths that \ntransect irrigated areas suggests that irrigation water may have altered \nsolute concentrations and isotope ratios in the eastern Snake River Plain \naquifer system. The changes, however, have been small because of the \nsimilarity of solute concentrations and ratios in applied irrigation water \nand in native ground water, and because of rapid movement and large \ndispersivity of the aquifer.\nReactions controlling solutes in the western Snake River basin are \nbelieved to be similar to those in the eastern basin but, because of dif- \nferent hydrologic conditions, a definitive analysis could not be made.\nThe regional geothermal system that underlies the Snake River Plain \ncontains total dissolved solids similar to those in the overlying Snake \nRiver Plain aquifer system but contains higher concentrations of sodium, \nbicarbonate, silica, fluoride, sulfate, chloride, arsenic, boron, and lithium,\nand lower concentrations of calcium, magnesium, and hydrogen. These \nsolutes are believed to be derived from reactions similar to those in the \nSnake River Plain aquifer system, except that ion exchange and hydrol- \nysis play a role in controlling solute concentrations in the geothermal \nsystem.\nGeothermometry calculations of selected ground-water samples from \nknown geothermal areas throughout the basin suggest that the geother- \nmal system is large in areal extent but has relatively low temperatures. \nApproximately half of the silica-quartz calculated water temperatures \nare greater than 90 °C. Radiocarbon dating of geothermal water in the \nSalmon Falls and Bruneau-Grand View areas in the south central part \nof the Snake River basin suggests that residence time of the geother- \nmal water is about 17,700 years.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp1408D","usgsCitation":"Wood, W., and Low, W.H., 1988, Solute geochemistry of the Snake River plain regional aquifer system, Idaho and eastern Oregon: U.S. Geological Survey Professional Paper 1408, vi, 79 p., https://doi.org/10.3133/pp1408D.","productDescription":"vi, 79 p.","numberOfPages":"91","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":123112,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1408d/report-thumb.jpg"},{"id":64929,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1408d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho;Oregon","otherGeospatial":"Snake River Plain","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.0,42.0 ], [ -111.0,45.0 ], [ -117.0,45.0 ], [ -117.0,42.0 ], [ -111.0,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49efe4b07f02db5ed9fc","contributors":{"authors":[{"text":"Wood, Warren W.","contributorId":47770,"corporation":false,"usgs":false,"family":"Wood","given":"Warren W.","affiliations":[{"id":6601,"text":"Michigan State University","active":true,"usgs":false}],"preferred":false,"id":219842,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Low, Walton H.","contributorId":92672,"corporation":false,"usgs":true,"family":"Low","given":"Walton","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":219843,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":42028,"text":"ofr88506 - 1988 - Aeromagnetic map of the Vulcan area, San Bernardino County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:06","indexId":"ofr88506","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"88-506","title":"Aeromagnetic map of the Vulcan area, San Bernardino County, California","language":"ENGLISH","doi":"10.3133/ofr88506","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1988, Aeromagnetic map of the Vulcan area, San Bernardino County, California: U.S. Geological Survey Open-File Report 88-506, 1 map :photocopy ;sheet 58 x 65 cm., https://doi.org/10.3133/ofr88506.","productDescription":"1 map :photocopy ;sheet 58 x 65 cm.","costCenters":[],"links":[{"id":136862,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79781,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1988/0506/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae7e4b07f02db68c142","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":530779,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29223,"text":"wri874129 - 1988 - Flood-carrying capacities and changes in channels of the Lower Puyallup, White, and Carbon Rivers in western Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:48","indexId":"wri874129","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4129","title":"Flood-carrying capacities and changes in channels of the Lower Puyallup, White, and Carbon Rivers in western Washington","docAbstract":"The flood-carrying capacity of the Puyallup River 's leveed channel from its mouth to the city of Puyallup exceeds the 100-yr-flood discharge at most locations. Upstream from the city of Puyallup the flood-carrying capacity also is less than the 100-yr flood at many locations. In King County the flood-carrying capacity would be greater than the 100-year flood nearly everywhere if the levees were in a good state of repair. The flood-carrying capacity of the leveed Carbon River channel is less than the 100-yr flood at numerous locations. Changes between 1976-77 and 1984 in average channel cross-section elevations for the Puyallup and Carbon Rivers were less than 1 ft at more than one-half of 90 surveyed cross sections and were more than 2 ft at only 5 of them. Changes in average elevations for the White River downstream of the inflow from Lake Tapps rose approximately 2 ft or more at 5 of the 10 surveyed cross sections, but decreased 2 ft or more at nearly one-half of 29 cross sections upstream of the reach. Differences between computed 100-yr floodwater-surface elevations for 1976-77 and 1984 channels are similar to changes in average cross-section elevations. Dense growths of streambank vegetation could increase 100-yr floodwater surface elevations by 1.2 ft. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874129","usgsCitation":"Prych, E., 1988, Flood-carrying capacities and changes in channels of the Lower Puyallup, White, and Carbon Rivers in western Washington: U.S. Geological Survey Water-Resources Investigations Report 87-4129, v, 69 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874129.","productDescription":"v, 69 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123373,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4129/report-thumb.jpg"},{"id":58076,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4129/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7512","contributors":{"authors":[{"text":"Prych, E. A.","contributorId":36163,"corporation":false,"usgs":true,"family":"Prych","given":"E. A.","affiliations":[],"preferred":false,"id":201174,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29761,"text":"wri884142 - 1988 - Geohydrology of the Flathead Indian Reservation, northwestern Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri884142","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4142","title":"Geohydrology of the Flathead Indian Reservation, northwestern Montana","docAbstract":"The geohydrology of the Flathead Indian Reservation was studied to provide information needed to formulate groundwater development plans. Bedrock in the area consists predominantly of slightly metamorphosed carbonate and fine-grained clasitc rocks of the Precambrian Belt Supergroup. Valley-fill deposits consist of alluvium of Holocene age; glacial and glaciolacustrine boulders, cobbles, gravel, sand, silt, and clay of Pleistocene age; and siltstone, fine-grained sandstone, and coal of probable Tertiary age. Most wells in the reservation are completed in valley-fill aquifers--for which well discharge ranges from 0.5 to 1,600 gal/minute and transmissivity ranges from 3.2 to 45,600 sq ft/day. Groundwater flow follows the trend of the respective valleys. Water level in valley-fill aquifers fluctuates seasonally in response to recharge from streams and irrigation canals and discharge from wells. Recharge to valley-fill aquifers occurs by direct infiltration of snowmelt and rainfall, leakage from streams and irrigation canals, subsurface inflow, and irrigation return flow. Discharge from the valley-fill aquifers occurs through evaporation, transpiration by plants, withdrawals from wells, leakage to rivers and streams, and subsurface outflow. Water in bedrock is available from fracture zones of secondary permeability; discharge from wells completed in bedrock ranges from 2.5 to 40 gal/min. Water from wells and springs is calcium bicarbonate or sodium bicarbonate type and contained dissolved-solids concentrations of 42 to 1,100 mg/L. All dissolved constituents in most samples were within Federal drinking water standards. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884142","usgsCitation":"Slagle, S., 1988, Geohydrology of the Flathead Indian Reservation, northwestern Montana: U.S. Geological Survey Water-Resources Investigations Report 88-4142, vi, 152 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884142.","productDescription":"vi, 152 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119684,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4142/report-thumb.jpg"},{"id":58556,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4142/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58557,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4142/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58558,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4142/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a89bc","contributors":{"authors":[{"text":"Slagle, S.E.","contributorId":25602,"corporation":false,"usgs":true,"family":"Slagle","given":"S.E.","email":"","affiliations":[],"preferred":false,"id":202076,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29379,"text":"wri874152 - 1988 - Simulated water-level and water-quality changes in the bolson-fill aquifer, Post Headquarters area, White Sands Missile Range, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:55","indexId":"wri874152","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4152","title":"Simulated water-level and water-quality changes in the bolson-fill aquifer, Post Headquarters area, White Sands Missile Range, New Mexico","docAbstract":"The quantity of freshwater available in the Post Headquarters well field, White Sand Missile Range, New Mexico, is limited and its quality is threatened by saltwater enroachment. A three-dimensional, finite-difference, groundwater flow model and a cross-sectional, density-dependent solute-transport model were constructed to simulate possible future water level declines and water quality changes in the Post Headquarters well field. A six-layer flow model was constructed using hydraulic-conductivity values in the upper 600 ft of saturated aquifer ranging from 0.1 to 10 ft/day, specific yield of 0.15, and average recharge of about 1,590 acre-ft/yr. Water levels simulated by the model closely matched measured water levels for 1948-82. Possible future water level changes for 1983-2017 were simulated using rates of groundwater withdrawal of 1,033 and 2 ,066 acre-ft/year and wastewater return flow of 0 or 30% of the groundwater withdrawal rate. The cross-sectional solute-transport model indicated that the freshwater zone is about 1,500 to 2,000 ft thick beneath the well field. Transient simulations show that solutes probably will move laterally toward the well field rather than from beneath the well field. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874152","usgsCitation":"Risser, D.W., 1988, Simulated water-level and water-quality changes in the bolson-fill aquifer, Post Headquarters area, White Sands Missile Range, New Mexico: U.S. Geological Survey Water-Resources Investigations Report 87-4152, viii, 71 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874152.","productDescription":"viii, 71 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159752,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4152/report-thumb.jpg"},{"id":58224,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4152/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f30c2","contributors":{"authors":[{"text":"Risser, D. W.","contributorId":48211,"corporation":false,"usgs":true,"family":"Risser","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":201434,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29116,"text":"wri874018 - 1988 - Streamflow characteristics of the Missouri River basin, Wyoming, through 1984","interactions":[],"lastModifiedDate":"2012-02-02T00:08:53","indexId":"wri874018","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4018","title":"Streamflow characteristics of the Missouri River basin, Wyoming, through 1984","docAbstract":"Streamflow characteristics as of 1984 for the Missouri River Basin, Wyoming, based on data from 204 streamflow-gaging stations are summarized. The streamflow characteristics reported include mean monthly and mean annual streamflow; duration of daily mean flow; and magnitude and probability of instantaneous peak flow, annual low flow, and annual high flow. Recurrence intervals of 2, 5, 10, 20, or 50, and 100 yr are determined for the peak-flow, low-flow, and high-flow characteristics. Annual low-flow and high-flow characteristics are also listed for various numbers of consecutive days. A station description, tables of streamflow characteristics, and graphs of mean monthly streamflow and duration of daily mean streamflow are presented for each station. Streamflow characteristics for periods before and after dam construction or transbasin diversion are presented for six stations. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874018","usgsCitation":"Peterson, D.A., 1988, Streamflow characteristics of the Missouri River basin, Wyoming, through 1984: U.S. Geological Survey Water-Resources Investigations Report 87-4018, iii, 431 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874018.","productDescription":"iii, 431 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159524,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4018/report-thumb.jpg"},{"id":57985,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4018/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57986,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4018/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4e18","contributors":{"authors":[{"text":"Peterson, D. A.","contributorId":6453,"corporation":false,"usgs":true,"family":"Peterson","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200971,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29899,"text":"wri884060 - 1988 - Surface-water quality of the Cedar River basin, Iowa-Minnesota, with emphasis on the occurrence and transport of herbicides, May 1984 through November 1985","interactions":[],"lastModifiedDate":"2022-09-15T18:46:53.281508","indexId":"wri884060","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4060","title":"Surface-water quality of the Cedar River basin, Iowa-Minnesota, with emphasis on the occurrence and transport of herbicides, May 1984 through November 1985","docAbstract":"<p>The surface-water quality in the Cedar River basin was evaluated by analyzing the occurrence, distribution, and transport of common inorganic constituents and selected trace inorganic and organic constituents, with emphasis on herbicides. The surface-water quality of the Cedar River basin was monitored from May 1984 through November 1985. Depth integrated surface-water samples generally were collected monthly at six stations for a considerable range of river discharge. Samples were analyzed for concentrations of common inorganic constituents in the dissolved phase and for concentrations of primary nutrients, trace elements, organic carbon, and herbicides in the dissolved and the dissolved plus suspended phases.</p>\n<p>Water in the Cedar River was determined to be a calcium bicarbonate type; suspended-sediment concentrations ranged from 3 to 676 milligrams per liter. Concentrations of dissolved fluoride, dissolved nitrite plus nitrate, dissolved arsenic, dissolved lead, and dissolved mercury were less than those of the U.S. Environmental Protection Agency's drinking-water standards for public water supplies.</p>\n<p>Generally, herbicides were detected only in the dissolved phase, which indicates that herbicides are not being adsorbed on the suspended sediment. However, the lack of detection of adsorbed herbicides also may indicate a need for re-examination of traditionally acceptable methods of treating water samples at the sampling site, separating sediment and water, and extracting organic compounds from sediment. The largest concentrations of several dissolved herbicides were detected after application on agricultural areas in the spring and early summer in both wet and dry periods. However, dissolved atrazine concentrations also increased in the winter during periods of high streamflow resulting from snow melt. The maximum concentration of dissolved herbicides detected at all sampling sites during the study were: alachlor, 21 micrograms per liter; atrazine, 16 micrograms per liter; cyanazine, 8.7 micrograms per liter; metolachlor, 11.0 micrograms per liter; and metribuzin, 3.0 micrograms per liter.</p>\n<p>Herbicides can be transported from agricultural areas to the river by overland flow, drainage from agricultural areas conveyed by tile drains, and ground water. Hydrograph separation for 10 locations in the Cedar River basin indicates that the ground-water contribution varies within the basin and probably ranges from 56 to 80 percent of the annual river discharge. The predominance of ground-water contribution, the persistent detection of dissolved atrazine even during base flow, and the variety of dissolved herbicides detected in the river during the dry spring of 1985 indicate that some herbicides are being transported to the river by ground water. Atrazine transported to the Cedar River was estimated to be about 1.4 to 4.0 percent of that applied, depending on the assumed application rate. The large river discharge in June 1984, which was predominantly overland flow, contained about 70 percent of the atrazine transported to the river during 1984.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884060","collaboration":"Prepared in cooperation with the University of Iowa Hygienic Laboratory","usgsCitation":"Squillace, P.J., and Engberg, R., 1988, Surface-water quality of the Cedar River basin, Iowa-Minnesota, with emphasis on the occurrence and transport of herbicides, May 1984 through November 1985: U.S. Geological Survey Water-Resources Investigations Report 88-4060, vi, 81 p., https://doi.org/10.3133/wri884060.","productDescription":"vi, 81 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":159821,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4060/report-thumb.jpg"},{"id":58715,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4060/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":406779,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_46982.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Iowa, Minnesota","otherGeospatial":"Cedar River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.351318359375,\n              41.281934557995356\n            ],\n            [\n              -91.2469482421875,\n              41.393294288784865\n            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J.","contributorId":8878,"corporation":false,"usgs":true,"family":"Squillace","given":"P.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":202319,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Engberg, R. A.","contributorId":104876,"corporation":false,"usgs":true,"family":"Engberg","given":"R. A.","affiliations":[],"preferred":false,"id":202320,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28780,"text":"wri874203 - 1988 - Extension of streamflow and dissolved-solids records at selected sites in the Colorado River basin, Arizona, California, Colorado, Nevada, New Mexico, Utah, and Wyoming, 1940-83","interactions":[],"lastModifiedDate":"2012-02-02T00:08:53","indexId":"wri874203","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4203","title":"Extension of streamflow and dissolved-solids records at selected sites in the Colorado River basin, Arizona, California, Colorado, Nevada, New Mexico, Utah, and Wyoming, 1940-83","docAbstract":"Monthly streamflow and dissolved-solids concentration were estimated for periods prior to the initiation of data collection at selected sites in the Colorado River basin. Techniques used for this record extension included simple and weighted least-squares regression. Streamflow records were extended at 5 sites and dissolved-solids records were extended at 13 sites. Records were extended back through 1941 to provide a completely concurrent data set for all sites. Standard errors were 5 to 74% for monthly streamflow and 3 to 27% for monthly, flow-weighted dissolved-solids concentration. The extended records at all sites were consistent with records from the historical period. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874203","usgsCitation":"Mueller, D., and Liebermann, T., 1988, Extension of streamflow and dissolved-solids records at selected sites in the Colorado River basin, Arizona, California, Colorado, Nevada, New Mexico, Utah, and Wyoming, 1940-83: U.S. Geological Survey Water-Resources Investigations Report 87-4203, v, 74 p. :ill., map ;28 cm., https://doi.org/10.3133/wri874203.","productDescription":"v, 74 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":123439,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4203/report-thumb.jpg"},{"id":57659,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4203/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae734","contributors":{"authors":[{"text":"Mueller, D. K.","contributorId":93525,"corporation":false,"usgs":true,"family":"Mueller","given":"D. K.","affiliations":[],"preferred":false,"id":200383,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Liebermann, T.D.","contributorId":23569,"corporation":false,"usgs":true,"family":"Liebermann","given":"T.D.","email":"","affiliations":[],"preferred":false,"id":200382,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28779,"text":"wri874069 - 1988 - Estimation of natural dissolved-solids discharge in the Upper Colorado River basin, Western United States","interactions":[],"lastModifiedDate":"2012-02-02T00:08:53","indexId":"wri874069","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4069","title":"Estimation of natural dissolved-solids discharge in the Upper Colorado River basin, Western United States","docAbstract":"A statistical method was developed to estimate monthly natural dissolved-solids discharge at selected sites in the Upper Colorado River Basin. Natural dissolved-solids discharge was defined as the rate of inorganic-solute flow past a specific site that would have occurred if there had been no water-resources development in the basin upstream from the site. The method used weighted least-squares regression to fit a model of dissolved-solids discharge as a function of streamflow and several variables representing development. After the model had been calibrated for an individual site, the development variables were assigned a value of zero to yield the relation between dissolved-solids discharge and streamflow for conditions of no upstream development. Natural dissolved-solids discharge was calculated using this relation and estimates of natural streamflow provided by the U.S. Bureau of Reclamation. Limitations of the method included lack of data to verify estimates of the natural dissolved-solids discharge and to represent all the effects of development adequately. However, model statistics indicated a good fit to historical data. Also, the estimates of natural dissolved-solids-discharge had the expected monthly distribution and were consistent between upstream and downstream sites. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874069","usgsCitation":"Mueller, D., and Osen, L., 1988, Estimation of natural dissolved-solids discharge in the Upper Colorado River basin, Western United States: U.S. Geological Survey Water-Resources Investigations Report 87-4069, v, 62 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874069.","productDescription":"v, 62 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124085,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4069/report-thumb.jpg"},{"id":57658,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4069/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9a05","contributors":{"authors":[{"text":"Mueller, D. K.","contributorId":93525,"corporation":false,"usgs":true,"family":"Mueller","given":"D. K.","affiliations":[],"preferred":false,"id":200381,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Osen, L.L.","contributorId":46993,"corporation":false,"usgs":true,"family":"Osen","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":200380,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28714,"text":"wri874202 - 1988 - Nomenclature of regional hydrogeologic units of the Southeastern Coastal Plain aquifer system","interactions":[],"lastModifiedDate":"2012-02-02T00:08:53","indexId":"wri874202","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4202","title":"Nomenclature of regional hydrogeologic units of the Southeastern Coastal Plain aquifer system","docAbstract":"Clastic sediments of the Southeastern Coastal Plain aquifer system can be divided into four regional aquifers separated by three regional confining units. The four regional aquifers have been named for major rivers that cut across their outcrop areas and expose the aquifer materials. From youngest to oldest, the aquifers are called the Chickasawhay River, Pearl River, Chattahoochee River, and Black Warrior River aquifers, and the regional confining units separating them are given the same name as the aquifer they overlie. Most of the regional hydrogeologic units are subdivided within each of the four States that comprise the study area. Correlation of regional units is good with hydrogeologic units delineated by a similar regional study to the west and southwest. Because of complexity created by a major geologic structure to the northeast of the study area and dramatic facies change from clastic to carbonate strata to the southeast, correlation of regional hydrogeologic units is poor in these directions. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874202","usgsCitation":"Miller, J.A., and Renken, R., 1988, Nomenclature of regional hydrogeologic units of the Southeastern Coastal Plain aquifer system: U.S. Geological Survey Water-Resources Investigations Report 87-4202, iv, 21 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874202.","productDescription":"iv, 21 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122697,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4202/report-thumb.jpg"},{"id":57547,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4202/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db6970e9","contributors":{"authors":[{"text":"Miller, J. A.","contributorId":77101,"corporation":false,"usgs":false,"family":"Miller","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200274,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Renken, R.A.","contributorId":99161,"corporation":false,"usgs":true,"family":"Renken","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":200275,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29755,"text":"wri874256 - 1988 - Sedimentation in Lake Tuscaloosa, Alabama, 1982-86","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri874256","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4256","title":"Sedimentation in Lake Tuscaloosa, Alabama, 1982-86","docAbstract":"Lake Tuscaloosa, created in 1969 by the impoundment of North River, provides the primary water supply for Tuscaloosa, Alabama , and surrounding areas. This report describes the rate of sedimentation in the lake from its principal tributaries. The rate of sediment deposition in the lake is low. The maximum sediment deposition from 1982 to 1986 at 17 lake cross sections was about 3.5 feet (or 0.9 foot per year) at a cross section that received drainage from Brush Creek basin. Brush Creek is an unmined basin with steep overland and channel slopes. At 15 of the 17 cross sections, the maximum sediment deposition was less than 2 feet (or 0.5 foot per year). Scour and fill processes (redistribution of the sediment) appear to be taking place at many of the cross sections. (Author 's abstract)","language":"ENGLISH","doi":"10.3133/wri874256","usgsCitation":"Slack, L.J., and Pritchett, J., 1988, Sedimentation in Lake Tuscaloosa, Alabama, 1982-86: U.S. Geological Survey Water-Resources Investigations Report 87-4256, v, 24 p. :ill., map ;28 cm., https://doi.org/10.3133/wri874256.","productDescription":"v, 24 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":159315,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4256/report-thumb.jpg"},{"id":58550,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4256/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f1df6","contributors":{"authors":[{"text":"Slack, L. J.","contributorId":44157,"corporation":false,"usgs":true,"family":"Slack","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":202063,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pritchett, J.L.","contributorId":65510,"corporation":false,"usgs":true,"family":"Pritchett","given":"J.L.","affiliations":[],"preferred":false,"id":202064,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28766,"text":"wri874058 - 1988 - Geohydrology and numerical model analysis of ground-water flow in the Goose Lake Basin, Oregon and California","interactions":[],"lastModifiedDate":"2017-02-07T08:15:50","indexId":"wri874058","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4058","title":"Geohydrology and numerical model analysis of ground-water flow in the Goose Lake Basin, Oregon and California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874058","usgsCitation":"Morgan, D.S., 1988, Geohydrology and numerical model analysis of ground-water flow in the Goose Lake Basin, Oregon and California: U.S. Geological Survey Water-Resources Investigations Report 87-4058, ix, 92 p. :ill., maps (1 col.) ;28 cm., https://doi.org/10.3133/wri874058.","productDescription":"ix, 92 p. :ill., maps (1 col.) ;28 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":119041,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4058/report-thumb.jpg"},{"id":57632,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4058/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57633,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4058/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8cd2","contributors":{"authors":[{"text":"Morgan, D. S.","contributorId":19184,"corporation":false,"usgs":true,"family":"Morgan","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":200360,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30430,"text":"wri854327 - 1988 - Rainfall-runoff relationships of the Hop Brook basin, Manchester, Connecticut","interactions":[],"lastModifiedDate":"2012-02-02T00:08:56","indexId":"wri854327","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"85-4327","title":"Rainfall-runoff relationships of the Hop Brook basin, Manchester, Connecticut","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey ;\r\nWestern Distribution Branch,","doi":"10.3133/wri854327","usgsCitation":"Weiss, L., 1988, Rainfall-runoff relationships of the Hop Brook basin, Manchester, Connecticut: U.S. Geological Survey Water-Resources Investigations Report 85-4327, v, 22 p. :ill., 1 map ;28 cm., https://doi.org/10.3133/wri854327.","productDescription":"v, 22 p. :ill., 1 map ;28 cm.","costCenters":[],"links":[{"id":159747,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4327/report-thumb.jpg"},{"id":59208,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4327/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59209,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4327/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64960d","contributors":{"authors":[{"text":"Weiss, L.A.","contributorId":95098,"corporation":false,"usgs":true,"family":"Weiss","given":"L.A.","affiliations":[],"preferred":false,"id":203236,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29990,"text":"wri884025 - 1988 - Distribution of gases in the unsaturated zone at a low-level radioactive-waste disposal site near Sheffield, Illinois","interactions":[],"lastModifiedDate":"2018-01-30T21:06:02","indexId":"wri884025","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4025","title":"Distribution of gases in the unsaturated zone at a low-level radioactive-waste disposal site near Sheffield, Illinois","docAbstract":"The unsaturated zone is a medium that provides pneumatic communication for the movement of gases from wastes buried in landfills to the atmosphere, biota, and groundwater. Gases in unsaturated glacial and eolian deposits near a waste-disposal trench at the low-level radioactive-waste disposal site near Sheffield, Bureau County, Illinois, were identified, and the spatial and temporal distributions of the partial pressures of those gases were determined for the period January 1984 through January 1986. Methods for the collection and analyses of the gases are described, as are geologic and hydrologic characteristics of the unsaturated zone that affect gas transport. The identified gases, which are of natural and of waste origin, include nitrogen, oxygen, and argon, carbon dioxide, methane, propane, butane, tritiated water vapor, 14carbon dioxide, and 222 radon. Concentrations of methane and 14carbon dioxide originated at the waste, as shown by partial-pressure gradients of the gases; 14carbon dioxide partial pressures exceeded natural background partial pressures by factors greater than 1 million at some locations. Variations in partial pressures of oxygen and carbon dioxide were seasonal among piezometers because of increased root and soil-microbe respiration during summer. Variations in methane and 14carbon dioxide partial pressures were apparently related to discrete releases from waste sources at unpredictable intervals of time. No greater than background partial pressures for tritiated water vapor or 222 radon were measured. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884025","usgsCitation":"Striegl, R.G., 1988, Distribution of gases in the unsaturated zone at a low-level radioactive-waste disposal site near Sheffield, Illinois: U.S. Geological Survey Water-Resources Investigations Report 88-4025, vii, 69 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884025.","productDescription":"vii, 69 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":58798,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4025/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":2446,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://il.water.usgs.gov/pubsearch/reports.cgi/view?series=WRIR&number=88-4025","linkFileType":{"id":5,"text":"html"}},{"id":124097,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4025/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db64111d","contributors":{"authors":[{"text":"Striegl, Robert G. 0000-0002-8251-4659 rstriegl@usgs.gov","orcid":"https://orcid.org/0000-0002-8251-4659","contributorId":1630,"corporation":false,"usgs":true,"family":"Striegl","given":"Robert","email":"rstriegl@usgs.gov","middleInitial":"G.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":36183,"text":"Hydro-Ecological Interactions Branch","active":true,"usgs":true}],"preferred":false,"id":202489,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29187,"text":"wri884161 - 1988 - Relation of trihalomethane-formation potential to water-quality and physical characteristics of small water-supply lakes, eastern Kansas","interactions":[],"lastModifiedDate":"2022-12-28T21:03:18.102914","indexId":"wri884161","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4161","title":"Relation of trihalomethane-formation potential to water-quality and physical characteristics of small water-supply lakes, eastern Kansas","docAbstract":"<p>The formation of carcinogenic trihalomethanes during the treatment of public surface water supplies has become a potentially serious problem. The U. S. Geological Survey, in cooperation with the Kansas Department of Health and Environment , investigated the potential for trihalomethane formation in water from 15 small, public water supply lakes in eastern Kansas from April 1984 through April 1986 in order to define the principal factors that affect or control the potential for trihalomethane formation during the water treatment process. Relations of mean concentrations of trihalomethane-formation potential to selected water quality and lake and watershed physical characteristics were investigated using correlation and regression analysis. Statistically significant, direct relations were developed between trihalomethanes produced in unfiltered and filtered lake water and mean concentrations of total and dissolved organic carbon. Correlation coefficients for these relations ranged from 0.86 to 0.93. Mean values of maximum depth of lake were shown to have statistically significant inverse relations to mean concentrations of trihalomethane-formation potential and total and dissolved organic carbon. Correlation coefficients for these relations ranged from -0.76 to -0.81.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884161","usgsCitation":"Pope, L.M., Arruda, J.A., and Fromm, C.H., 1988, Relation of trihalomethane-formation potential to water-quality and physical characteristics of small water-supply lakes, eastern Kansas: U.S. Geological Survey Water-Resources Investigations Report 88-4161, v, 46 p., https://doi.org/10.3133/wri884161.","productDescription":"v, 46 p.","costCenters":[],"links":[{"id":58053,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4161/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":411144,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47068.htm","linkFileType":{"id":5,"text":"html"}},{"id":159407,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4161/report-thumb.jpg"}],"country":"United States","state":"Kansas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -97.4667,\n              40\n            ],\n            [\n              -97.4667,\n              37\n            ],\n            [\n              -94.6194,\n              37\n            ],\n            [\n              -94.6194,\n              40\n            ],\n            [\n              -97.4667,\n              40\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8209","contributors":{"authors":[{"text":"Pope, L. M.","contributorId":71939,"corporation":false,"usgs":true,"family":"Pope","given":"L.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":201110,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Arruda, J. A.","contributorId":70809,"corporation":false,"usgs":true,"family":"Arruda","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":201109,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fromm, C. H.","contributorId":44586,"corporation":false,"usgs":true,"family":"Fromm","given":"C.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":201108,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30077,"text":"wri874189 - 1988 - Predicted effects of underground mine flooding at tract C-b in Piceance Basin, northwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:54","indexId":"wri874189","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4189","title":"Predicted effects of underground mine flooding at tract C-b in Piceance Basin, northwestern Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874189","usgsCitation":"Taylor, O., 1988, Predicted effects of underground mine flooding at tract C-b in Piceance Basin, northwestern Colorado: U.S. Geological Survey Water-Resources Investigations Report 87-4189, iii, 16 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874189.","productDescription":"iii, 16 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159508,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4189/report-thumb.jpg"},{"id":58887,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4189/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ecd2","contributors":{"authors":[{"text":"Taylor, O.J.","contributorId":71584,"corporation":false,"usgs":true,"family":"Taylor","given":"O.J.","email":"","affiliations":[],"preferred":false,"id":202637,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29722,"text":"wri884006 - 1988 - Ground-water hydrology of Marshall County, West Virginia, with emphasis on the effects of longwall coal mining","interactions":[],"lastModifiedDate":"2023-01-09T21:37:24.228504","indexId":"wri884006","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4006","title":"Ground-water hydrology of Marshall County, West Virginia, with emphasis on the effects of longwall coal mining","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884006","usgsCitation":"Shultz, R., 1988, Ground-water hydrology of Marshall County, West Virginia, with emphasis on the effects of longwall coal mining: U.S. Geological Survey Water-Resources Investigations Report 88-4006, ix, 139 p., https://doi.org/10.3133/wri884006.","productDescription":"ix, 139 p.","costCenters":[],"links":[{"id":119488,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4006/report-thumb.jpg"},{"id":58534,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4006/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":110252,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_46937.htm","linkFileType":{"id":5,"text":"html"},"description":"46937"}],"country":"United States","state":"West Virginia","county":"Marshall County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -80.5192,\n              40.0319\n            ],\n            [\n              -80.8667,\n              40.0319\n            ],\n            [\n              -80.8667,\n              39.72\n            ],\n            [\n              -80.5192,\n              39.72\n            ],\n            [\n              -80.5192,\n              40.0319\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae0be","contributors":{"authors":[{"text":"Shultz, R.A.","contributorId":27442,"corporation":false,"usgs":true,"family":"Shultz","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":202014,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28759,"text":"wri884080 - 1988 - Geohydrology and susceptibility of major aquifers to surface contamination in Alabama; area 13","interactions":[],"lastModifiedDate":"2012-02-02T00:08:46","indexId":"wri884080","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4080","title":"Geohydrology and susceptibility of major aquifers to surface contamination in Alabama; area 13","docAbstract":"The geohydrology and susceptibility to surface contamination of the major aquifers in Area 13--Baldwin and Mobile Counties Alabama--are described. Within this area are two major aquifers. The Pliocene-Miocene aquifer occurs throughout the study area. The Alluvial-Coastal aquifer is found near the major rivers and coastal areas and overlies the Pliocene-Miocene aquifer. There is no continuous confining unit between these two aquifers, thus , they are hydraulically connected and act as a single hydrologic unit. The entire study area is susceptible to surface contamination. The sediments are highly permeable, which allows rapid infiltration of water. Areas around some of the large pumping centers are highly susceptible to contamination, not only because of permeable sediments and flat terrain, but also because of depressions created in the potentiometric surface by large withdrawals of water from the aquifers. These depressions act as funnels to direct groundwater flow toward pumping centers; this increases the possibility of a contaminant migrating into the groundwater system. Other areas of high susceptibility are regions characterized by flat terrain and highly permeable soils, which increase the rate of infiltration from the surface. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884080","usgsCitation":"Mooty, W., 1988, Geohydrology and susceptibility of major aquifers to surface contamination in Alabama; area 13: U.S. Geological Survey Water-Resources Investigations Report 88-4080, iv, 29 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/wri884080.","productDescription":"iv, 29 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":124239,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4080/report-thumb.jpg"},{"id":57627,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4080/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57628,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4080/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8bf2","contributors":{"authors":[{"text":"Mooty, W. S.","contributorId":55837,"corporation":false,"usgs":true,"family":"Mooty","given":"W. S.","affiliations":[],"preferred":false,"id":200351,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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