{"pageNumber":"1781","pageRowStart":"44500","pageSize":"25","recordCount":68937,"records":[{"id":17139,"text":"ofr9152 - 1991 - Geohydrology and evaluation of water-resource potential of the Upper Floridan aquifer in the Albany area, southwestern Georgia","interactions":[{"subject":{"id":17139,"text":"ofr9152 - 1991 - Geohydrology and evaluation of water-resource potential of the Upper Floridan aquifer in the Albany area, southwestern Georgia","indexId":"ofr9152","publicationYear":"1991","noYear":false,"title":"Geohydrology and evaluation of water-resource potential of the Upper Floridan aquifer in the Albany area, southwestern Georgia"},"predicate":"SUPERSEDED_BY","object":{"id":59,"text":"wsp2391 - 1993 - Geohydrology and evaluation of water-resource potential of the upper Floridan Aquifer in the Albany area, southwestern Georgia","indexId":"wsp2391","publicationYear":"1993","noYear":false,"title":"Geohydrology and evaluation of water-resource potential of the upper Floridan Aquifer in the Albany area, southwestern Georgia"},"id":1}],"supersededBy":{"id":59,"text":"wsp2391 - 1993 - Geohydrology and evaluation of water-resource potential of the upper Floridan Aquifer in the Albany area, southwestern Georgia","indexId":"wsp2391","publicationYear":"1993","noYear":false,"title":"Geohydrology and evaluation of water-resource potential of the upper Floridan Aquifer in the Albany area, southwestern Georgia"},"lastModifiedDate":"2022-04-06T18:17:18.108896","indexId":"ofr9152","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-52","title":"Geohydrology and evaluation of water-resource potential of the Upper Floridan aquifer in the Albany area, southwestern Georgia","docAbstract":"<p>In the Albany area of southwestern Georgia, the Upper Floridan aquifer lies entirely within the Dougherty Plain district of the Coastal Plain physiographic province, and consists of the Ocala Limestone of late Eocene age. The aquifer is divided throughout most of the study area into an upper and a lower lithologic unit, which creates an upper and a lower water-bearing zone. The lower water-bearing zone consists of alternating layers of sandy limestone and medium-brown, recrystallized dolomitic limestone, and ranges in thickness from about 50 to 100 feet. It is highly fractured, and exhibits well-developed permeability by solution features that are responsible for transmitting most of the ground water in the aquifer. Transmissivity of the lower water-bearing zone ranges from about 90,000 to 178,000 feet squared per day. The upper water-bearing zone is a finely crystallized-to-oolitic, locally dolomitic limestone having an average thickness of about 60 feet. Transmissivities in the upper water-bearing zone are considerably less than those in the lower water-bearing zone. The Upper Floridan aquifer is overlain by about 20 to 120 feet of undifferentiated overburden consisting of fine-to-coarse quartz sand and noncalcareous clay. A clay zone about 10 to 30 feet thick may be continuous throughout the southwestern part of the Albany area, and where present, causes confinement of the Upper Floridan aquifer and creates perched ground water after periods of heavy rainfall. The Upper Floridan aquifer is confined below by the Lisbon Formation, a mostly dolomitic limestone that contains trace amounts of glauconite. The Lisbon Formation is at least 50 feet thick in the study area, and acts as an impermeable base to the Upper Floridan aquifer. The quality of ground-water in the Upper Floridan aquifer is suitable for most uses; wells generally yield water of the hard, calcium-bicarbonate type that generally meets the U.S. Environmental Protection Agency's Primary or Secondary Drinking Water Regulations.</p><p>The water-resource potential of the Upper Floridan aquifer was evaluated by compiling results of test drilling and aquifer testing in the study area, and by conducting computer simulations of the ground-water-flow system under the seasonal-low conditions of November 1985, and under conditions of pumping within a 12square-mile area located southwest of Albany. Results of test drilling, aquifer testing, and water-quality analyses indicate that, in the area southwest of Albany, geohydrologic conditions in the Upper Floridan aquifer, undifferentiated overburden, and Lisbon Formation were favorable for the aquifer to provide a large quantity of water without having adverse effects on the ground-water system. The confinement of the Upper Floridan aquifer by the undifferentiated overburden and the rural setting of the area of potential development decreases the likelihood that chemical constituents will enter the aquifer during development of the ground-water resources.</p><p>Computer simulations of ground-water flow in the Upper Floridan aquifer, incorporating conditions for regional flow across model boundaries, leakage from rivers and other surface-water features, and vertical leakage from the undifferentiated overburden, were conducted by using a finite-element model for groundwater flow in two dimensions. Comparison of computed and measured water levels in the Upper Floridan aquifer for November 1985 at 74 locations indicated that computed water levels generally were within 5 feet of the measured values, which is the accuracy to which measured water levels were known. Water-level altitudes ranged from about 260 feet to 130 feet above sea level in the study area during calibration. Aquifer discharge to the Flint River downstream from the Lake Worth dam was computed by the calibrated model to be about 1 billion gallons per day; about 300 million gallons per day greater than was measured for similar low-flow conditions. The excess computed discharge was attributed partially to stream withdrawals for industrial use, non-reported use, and channel evaporation, but mostly to increased gradients and increased flow from the aquifer to the river than existed during calibration.</p><p>Results from the calibrated finite-element model indicate that ground-water flow is dominated by inflow from regional-flow components to the west, north, and east of the study area, and by outflow to the Flint River downstream from the Lake Worth dam. Simulation results indicated that directions of ground-water flow were not changed appreciably by pumping at the November 1985 rates. However, vertical leakage from the undifferentiated overburden caused local deviations in the regional flow pattern.</p><p>A sensitivity analysis that was performed on 18 hydrologic factors affecting the flow system in the Upper Floridan aquifer showed that computed water levels changed the most (were the most sensitive) in response to changes in hydraulic conductivity of the aquifer, vertical leakage coefficient and water level in the undifferentiated overburden, and stage of the Flint River downstream from the Lake Worth dam. Computed water levels were least sensitive to changes in well pumpage, flow across the northern boundary and from Lake Worth, the boundary coefficient for the Flint River downstream from the Lake Worth dam, and flow from Cooleewahee Creek.</p><p>Simulations of six pumping scenarios in the area of potential development southwest of Albany showed that the Upper Floridan aquifer is capable of providing at least 72 million gallons per day from five locations (14.4 million gallons per day each) within this area without causing adverse affects on the flow system. The 72million-gallon-per-day scenario yielded a maximum drawdown of about 9.4 feet, which placed the water level in the Upper Floridan aquifer about 50 feet above the top of the lower water-bearing zone. Hence, the likelihood of aquifer dewatering, well interference, or sinkhole development from pumping as much as 72 million gallons per day from within the area of potential development is small. All pumping scenarios showed that about 81 percent of the ground-water pumpage was derived from regional flow that would have discharged to the Flint River downstream from the Lake Worth dam. The dominant ground-water-flow direction toward the Flint River was not changed and no induced recharge from the Flint River entered the potential-development area. Induced recharge from the undifferentiated overburden contributed to about 1.5 percent of the total volume pumped during the simulations.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr9152","collaboration":"Prepared in cooperation with City of Albany Water, Gas, and Light Commission","usgsCitation":"Torak, L.J., Davis, G.S., Strain, G.A., and Herndon, J.G., 1991, Geohydrology and evaluation of water-resource potential of the Upper Floridan aquifer in the Albany area, southwestern Georgia: U.S. Geological Survey Open-File Report 91-52, vii, 86 p., https://doi.org/10.3133/ofr9152.","productDescription":"vii, 86 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science 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,{"id":20111,"text":"ofr91204 - 1991 - Potentiometric surface of the upper Floridan Aquifer, in the Albany area, Georgia, October, 1990","interactions":[],"lastModifiedDate":"2019-11-26T11:49:44","indexId":"ofr91204","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-204","title":"Potentiometric surface of the upper Floridan Aquifer, in the Albany area, Georgia, October, 1990","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr91204","usgsCitation":"Milby, B.J., 1991, Potentiometric surface of the upper Floridan Aquifer, in the Albany area, Georgia, October, 1990: U.S. Geological Survey Open-File Report 91-204, iii, 2 p. , https://doi.org/10.3133/ofr91204.","productDescription":"iii, 2 p. ","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":369656,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1991/0204/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152267,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1991/0204/report-thumb.jpg"}],"country":"United States","state":"Georgia","city":"Albany","otherGeospatial":"Upper Floridan Aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.63043212890625,\n              31.31140838620163\n            ],\n            [\n              -84.63043212890625,\n              31.92885480180959\n            ],\n            [\n              -83.69384765625,\n              31.92885480180959\n            ],\n            [\n              -83.69384765625,\n              31.31140838620163\n            ],\n            [\n              -84.63043212890625,\n              31.31140838620163\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682ca5","contributors":{"authors":[{"text":"Milby, Barbara J.","contributorId":17255,"corporation":false,"usgs":true,"family":"Milby","given":"Barbara","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":182085,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20427,"text":"ofr91206 - 1991 - Potentiometric surface of the upper Floridan aquifer, in Georgia, and adjacent parts of Alabama, Florida, and South Carolina, May-June 1990","interactions":[],"lastModifiedDate":"2022-08-31T18:42:47.922803","indexId":"ofr91206","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-206","title":"Potentiometric surface of the upper Floridan aquifer, in Georgia, and adjacent parts of Alabama, Florida, and South Carolina, May-June 1990","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr91206","usgsCitation":"Peck, M., 1991, Potentiometric surface of the upper Floridan aquifer, in Georgia, and adjacent parts of Alabama, Florida, and South Carolina, May-June 1990: U.S. Geological Survey Open-File Report 91-206, iii, 3 p., https://doi.org/10.3133/ofr91206.","productDescription":"iii, 3 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":406013,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18088.htm","linkFileType":{"id":5,"text":"html"}},{"id":49968,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1991/0206/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152119,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1991/0206/report-thumb.jpg"}],"country":"United States","state":"Alabama, Florida, Georgia, South Carolina","otherGeospatial":"upper Floridan aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -85.58349609375,\n              29.954934549656144\n            ],\n            [\n              -85.58349609375,\n              33.50475906922609\n            ],\n            [\n              -80.44189453125,\n              33.50475906922609\n            ],\n            [\n              -80.44189453125,\n              29.954934549656144\n            ],\n            [\n              -85.58349609375,\n              29.954934549656144\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682c9b","contributors":{"authors":[{"text":"Peck, Michael F. mfpeck@usgs.gov","contributorId":1467,"corporation":false,"usgs":true,"family":"Peck","given":"Michael F.","email":"mfpeck@usgs.gov","affiliations":[],"preferred":false,"id":182631,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56,"text":"wsp2380 - 1991 - Geochemical relations and distribution of selected trace elements in ground water of the northern part of the western San Joaquin Valley, California","interactions":[{"subject":{"id":17129,"text":"ofr90108 - 1991 - Geochemical relations and distribution of selected trace elements in ground water of the northern part of the western San Joaquin Valley, California","indexId":"ofr90108","publicationYear":"1991","noYear":false,"title":"Geochemical relations and distribution of selected trace elements in ground water of the northern part of the western San Joaquin Valley, California"},"predicate":"SUPERSEDED_BY","object":{"id":56,"text":"wsp2380 - 1991 - Geochemical relations and distribution of selected trace elements in ground water of the northern part of the western San Joaquin Valley, California","indexId":"wsp2380","publicationYear":"1991","noYear":false,"title":"Geochemical relations and distribution of selected trace elements in ground water of the northern part of the western San Joaquin Valley, California"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:11","indexId":"wsp2380","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"2380","title":"Geochemical relations and distribution of selected trace elements in ground water of the northern part of the western San Joaquin Valley, California","docAbstract":"Water samples were collected from 44 wells in the northern part of the western San Joaquin Valley, California, between March and July 1985 to assess the geochemical relations and distribution of major ions and selected trace-element concentrations in ground water of the area. The ground-waterflow system consists of a semiconfined zone and a confined zone separated by a regionally extensive clay bed. \r\n\r\nThe data show that the areal and vertical distribution of ground-water chemistry in the ground-water-flow system has been affected by different agricultural and natural sources of recharge and the source and redox status of the sediments. Tritium and stable-isotope data indicate extensive infiltration of the semiconfined zone by post-1952 irrigation water originating as runoff from the Sierra Nevada. Tritium concentrations greater than 2 tritium units in most samples from the confined zone indicate that the post-1952 water also has infiltrated to wells completed in this zone. Stable-isotope data indicate that ground water from the semiconfined zone, characterized by the enriched oxygen-18 that is indicative of a Coast Ranges source, occurs in many wells in the confined zone. Movement of water from the semiconfined zone to the confined zone likely is taking place by downward flow through the many wells that perforate the confining clay bed. \r\n\r\nTrace-element concentrations in the semiconfined and confined zones generally are similar. In contrast, concentrations were significantly different between ground water from Coast Ranges sediments and ground water from Sierra Nevada sediments in both zones. Ground water from Coast Ranges sediments contains significantly higher concentrations of nitrate, boron, and selenium than water from Sierra Nevada sediments. Ground water from Sierra Nevada sediments was significantly higher in arsenic, molybdenum, and manganese than ground water from Coast Ranges sediments. These differences result from a combination of variable availability of the constituents and redox controls on mobility. \r\n\r\nSelenium, the only priority pollutant to exceed the U.S. Environmental Protection Agency's drinking-water standard, equaled or exceeded the standard of 10 micrograms per liter in water from two wells completed in the semiconfined zone and one well in the confined zone. The conservative nature of selenium behavior in the oxidized Coast Ranges deposits is shown by the high correlation (r=0.88) between selenium concentrations and specific conductance in water from these deposits in the semiconfined zone. High selenium concentrations in both zones are spatially related to the location of Coast Ranges streams that have high selenium concentrations and that were historical sources of recharge to the zones. \r\n\r\nPrincipal-component analysis confirmed the association of boron, chromium, lithium, and selenium, and the association of arsenic, iron, manganese, and molybdenum to sediments in the study area. The analysis indicated that the first group is associated with Coast Ranges sediments and the second with Sierra Nevada sediments.","language":"ENGLISH","publisher":"U.S. G.P.O. ;\r\nBooks and Open-File Reports Section, U.S. Geological Survey [distributor],","doi":"10.3133/wsp2380","usgsCitation":"Dubrovsky, N.M., Neil, J.M., Welker, M.C., and Evenson, K.D., 1991, Geochemical relations and distribution of selected trace elements in ground water of the northern part of the western San Joaquin Valley, California: U.S. Geological Survey Water Supply Paper 2380, vii, 51 p. :ill. (some col.) ;28 cm., https://doi.org/10.3133/wsp2380.","productDescription":"vii, 51 p. :ill. (some col.) ;28 cm.","costCenters":[],"links":[{"id":137549,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2380/report-thumb.jpg"},{"id":24691,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2380/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db697f1a","contributors":{"authors":[{"text":"Dubrovsky, Neil M. 0000-0001-7786-1149 nmdubrov@usgs.gov","orcid":"https://orcid.org/0000-0001-7786-1149","contributorId":1799,"corporation":false,"usgs":true,"family":"Dubrovsky","given":"Neil","email":"nmdubrov@usgs.gov","middleInitial":"M.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":141886,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Neil, John M.","contributorId":13957,"corporation":false,"usgs":false,"family":"Neil","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":141887,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Welker, Mary C.","contributorId":98703,"corporation":false,"usgs":true,"family":"Welker","given":"Mary","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":141889,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Evenson, Kristin D.","contributorId":42943,"corporation":false,"usgs":true,"family":"Evenson","given":"Kristin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":141888,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":29561,"text":"wri914040 - 1991 - The computer program estimate trend (ESTREND), a system for the detection of trends in water-quality data","interactions":[],"lastModifiedDate":"2012-02-02T00:09:02","indexId":"wri914040","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-4040","title":"The computer program estimate trend (ESTREND), a system for the detection of trends in water-quality data","docAbstract":"Computerized statistical and graphical procedures were developed for use in U.S. Geological Survey (USGS) investigations of trend in stream water-quality data. These procedures, identified as EStimate TREND (ESTREND), are described in this paper to assist USGS investigators involved in multiple-station studies of water-quality trends. Additional discussion focuses on certain statistical and operational decisions required in multiple-station analysis of trends. The statistical methods used in ESTREND overcome common statistical problems encountered by conventional statistical trend techniques in the analysis of water-quality data. The problems include data that are non-normal and seasonally varying and water-quality records with missing values, 'less-than' (censored) values, and outliers, all of which adversely affect the performance of conventional statistical techniques. Parametric and nonparametric statistical trend tests are used in ESTREND. A nonparametric method, the Seasonal Kendall test, is used for data that have few less-than values or data that have been censored at only one reporting limit. A parametric test for trend involving a maximum likelihood estimation method is used for data that have been censored at multiple reporting limits. The Seasonal Kendall test for uncensored data allows for the removal of flow variability in water-quality data which improves the performance of the statistical trend tests. Menu-driven procedures in ESTREND allow the user to easily retrieve water-quality data, analyze data for trend, and view tabular and graphical results of analyses.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri914040","usgsCitation":"Schertz, T.L., Alexander, R.B., and Ohe, D.J., 1991, The computer program estimate trend (ESTREND), a system for the detection of trends in water-quality data: U.S. Geological Survey Water-Resources Investigations Report 91-4040, v, 63 p. :ill. ;28 cm., https://doi.org/10.3133/wri914040.","productDescription":"v, 63 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":2386,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri914040/","linkFileType":{"id":5,"text":"html"}},{"id":160461,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648714","contributors":{"authors":[{"text":"Schertz, Terry L. tschertz@usgs.gov","contributorId":188,"corporation":false,"usgs":true,"family":"Schertz","given":"Terry","email":"tschertz@usgs.gov","middleInitial":"L.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":201718,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alexander, Richard B. 0000-0001-9166-0626 ralex@usgs.gov","orcid":"https://orcid.org/0000-0001-9166-0626","contributorId":541,"corporation":false,"usgs":true,"family":"Alexander","given":"Richard","email":"ralex@usgs.gov","middleInitial":"B.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true}],"preferred":true,"id":201719,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ohe, Dane J. djohe@usgs.gov","contributorId":5446,"corporation":false,"usgs":true,"family":"Ohe","given":"Dane","email":"djohe@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":201720,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":29117,"text":"wri884192 - 1991 - Streamflow recharge to the Madison Limestone and the Casper Formation in the Glenrock area, east-central Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:53","indexId":"wri884192","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"88-4192","title":"Streamflow recharge to the Madison Limestone and the Casper Formation in the Glenrock area, east-central Wyoming","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri884192","usgsCitation":"Peterson, D.A., 1991, Streamflow recharge to the Madison Limestone and the Casper Formation in the Glenrock area, east-central Wyoming: U.S. Geological Survey Water-Resources Investigations Report 88-4192, iv, 18 p. :ill. ;28 cm., https://doi.org/10.3133/wri884192.","productDescription":"iv, 18 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":159525,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4192/report-thumb.jpg"},{"id":57987,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4192/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d57","contributors":{"authors":[{"text":"Peterson, D. A.","contributorId":6453,"corporation":false,"usgs":true,"family":"Peterson","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200972,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29340,"text":"wri914120 - 1991 - Hydrologic provinces of Michigan","interactions":[],"lastModifiedDate":"2017-01-23T11:55:09","indexId":"wri914120","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-4120","title":"Hydrologic provinces of Michigan","docAbstract":"<p>This report presents the results of a study by the U.S. Geological Survey, in cooperation with the Michigan Department of Natural Resources, Geological Survey Division, to describe the statewide hydrologic variations in Michigan's water resources. Twelve hydrologic provinces, which are based on similarities in aquifer lithology, yield, recharge, and ground-water- and surface-water-quality data, are described. The definition of statewide hydrologic characteristics and the delineation of hydrologic provinces improves the understanding of Michigan's water resources and provides a firm basis for realistic water-manangement decisions. </p><p>The 12 provinces identified areas where bedrock aquifers provide most of the potable ground water (five provinces), where glacial-deposit aquifers provide most of the potable ground water (three provinces), and where problems with water quantity and (or) quality have limited the use of ground water as a water supply (four provinces). Subprovinces are defined on the basis of regional surface-water flow directions toward each of the Great Lakes. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/wri914120","collaboration":"Prepared in cooperation with the Michigan Department of Natural Resources, Geological Survey Division","usgsCitation":"Rheaume, S.J., 1991, Hydrologic provinces of Michigan: U.S. Geological Survey Water-Resources Investigations Report 91-4120, Document: viii, 73 p.; Plate: 24.78 x 30.34 inches, https://doi.org/10.3133/wri914120.","productDescription":"Document: viii, 73 p.; Plate: 24.78 x 30.34 inches","costCenters":[{"id":382,"text":"Michigan Water Science 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,{"id":27706,"text":"wri914171 - 1991 - Flood hazards of distributary-flow areas in southwestern Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:08:37","indexId":"wri914171","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-4171","title":"Flood hazards of distributary-flow areas in southwestern Arizona","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri914171","usgsCitation":"Hjalmarson, H., and Kemna, S., 1991, Flood hazards of distributary-flow areas in southwestern Arizona: U.S. Geological Survey Water-Resources Investigations Report 91-4171, x, 58 p. :ill. ;28 cm., https://doi.org/10.3133/wri914171.","productDescription":"x, 58 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":120174,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4171/report-thumb.jpg"},{"id":56552,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4171/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5ef177","contributors":{"authors":[{"text":"Hjalmarson, H. W.","contributorId":95872,"corporation":false,"usgs":true,"family":"Hjalmarson","given":"H. W.","affiliations":[],"preferred":false,"id":198567,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kemna, S.P.","contributorId":95921,"corporation":false,"usgs":true,"family":"Kemna","given":"S.P.","email":"","affiliations":[],"preferred":false,"id":198568,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27681,"text":"wri904146 - 1991 - Preliminary geologic and hydrologic evaluation of a small watershed near Plains, Georgia","interactions":[],"lastModifiedDate":"2020-04-30T17:45:48.848533","indexId":"wri904146","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"90-4146","title":"Preliminary geologic and hydrologic evaluation of a small watershed near Plains, Georgia","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri904146","usgsCitation":"Hicks, D., McConnell, J.B., and Asmussen, L.E., 1991, Preliminary geologic and hydrologic evaluation of a small watershed near Plains, Georgia: U.S. Geological Survey Water-Resources Investigations Report 90-4146, iv, 30 p. , https://doi.org/10.3133/wri904146.","productDescription":"iv, 30 p. ","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":56534,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4146/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159009,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4146/report-thumb.jpg"}],"country":"United States","state":"Georgia","city":"Plains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.47113037109375,\n              31.962066108310047\n            ],\n            [\n              -84.3585205078125,\n              31.962066108310047\n            ],\n            [\n              -84.3585205078125,\n              32.05522664981892\n            ],\n            [\n              -84.47113037109375,\n              32.05522664981892\n            ],\n            [\n              -84.47113037109375,\n              31.962066108310047\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c2f9","contributors":{"authors":[{"text":"Hicks, D.W.","contributorId":61795,"corporation":false,"usgs":true,"family":"Hicks","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":198526,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McConnell, James B.","contributorId":28224,"corporation":false,"usgs":true,"family":"McConnell","given":"James","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":198525,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Asmussen, Loris E.","contributorId":62248,"corporation":false,"usgs":true,"family":"Asmussen","given":"Loris","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":198527,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26700,"text":"wri894192 - 1991 - Evaluation of the Bidahochi and San Andres-Glorieta aquifers on parts of the Zuni Indian reservation, McKinley and Cibola Counties, New Mexico","interactions":[],"lastModifiedDate":"2023-03-07T21:40:33.777602","indexId":"wri894192","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"89-4192","title":"Evaluation of the Bidahochi and San Andres-Glorieta aquifers on parts of the Zuni Indian reservation, McKinley and Cibola Counties, New Mexico","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri894192","usgsCitation":"Crouch, T.M., 1991, Evaluation of the Bidahochi and San Andres-Glorieta aquifers on parts of the Zuni Indian reservation, McKinley and Cibola Counties, New Mexico: U.S. Geological Survey Water-Resources Investigations Report 89-4192, vi, 48 p., https://doi.org/10.3133/wri894192.","productDescription":"vi, 48 p.","costCenters":[],"links":[{"id":413792,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47271.htm","linkFileType":{"id":5,"text":"html"}},{"id":55571,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4192/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119070,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4192/report-thumb.jpg"}],"country":"United States","state":"New Mexico","county":"Cibola County, McKinley County","otherGeospatial":"Bidahochi and San Andres-Glorieta aquifers","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -109.05,\n              35.1667\n            ],\n            [\n              -109.05,\n              34.85\n            ],\n            [\n              -108.25,\n              34.85\n            ],\n            [\n              -108.25,\n              35.1667\n            ],\n            [\n              -109.05,\n              35.1667\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faa80","contributors":{"authors":[{"text":"Crouch, T. M.","contributorId":106163,"corporation":false,"usgs":true,"family":"Crouch","given":"T.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":196850,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28537,"text":"wri894106 - 1991 - Techniques for computing discharge at four Navigation Dams on the Illinois and Des Plaines Rivers in Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:08:48","indexId":"wri894106","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"89-4106","title":"Techniques for computing discharge at four Navigation Dams on the Illinois and Des Plaines Rivers in Illinois","docAbstract":"Techniques for computing discharge are developed for Brandon Road Dam on the Des Plaines River and for Dresden Island, Marseilles, and Starved Rock Dams on the Illinois River. At Brandon Road Dam, streamflow is regulated by the operation of Tainter gates and headgates. At Dresden Island, Marseilles, and Starved Rock Dams, only Tainter gates are operated to regulate streamflow. The locks at all dams are equipped with culvert valves that are used to fill and empty the lock. The techniques facilitate determination of discharge at locations along the upper Illinois Waterway where no streamflow-gaging stations exist. The techniques are also useful for computing low flows when the water-surface slope between control structures on the river approaches zero and traditional methods of determining discharge based on slope are unsatisfactory.\r\nTwo techniques can be used to compute discharge at the dams--gate ratings and tailwater ratings . A gate ratingdescribes the relation between discharge, gate opening, tailwater stage, and headwater stage. A tailwater rating describes the relation between tailwater stage and discharge.\r\n\r\nGate ratings for Tainter gates at Dresden Island, Marseilles, and Starved Rock Dams are based on a total of 78 measurements of discharge that range from 569 to 86,400 cubic feet per second. Flood hydrographs developed from the gate ratings and Lockmaster records of gate opening and stage compare closely with streamflow records published for nearby streamflow-gaging stations. Additional measurements are needed to verify gate ratings for Tainter gates and headgates at Brandon Road Dam after the dam rehabilitation is completed. Extensive leakage past deteriorated headgates and sluice gates contributed to uncertainty in the ratings developed for this dam.\r\n\r\nA useful tailwater rating is developed for Marseilles Dam. Tailwater ratings for Dresden Island Dam and Starved Rock Dam are of limited use because of varying downstream channel-storage conditions. A tailwater rating could not be developed for Brandon Road Dam because its tailwater pool is substantially affected by the headwater pool of Dresden Island Dam.","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri894106","usgsCitation":"Mades, D.M., Weiss, L.S., and Gray, J.R., 1991, Techniques for computing discharge at four Navigation Dams on the Illinois and Des Plaines Rivers in Illinois: U.S. Geological Survey Water-Resources Investigations Report 89-4106, vi, 58 p. :ill. ;28 cm., https://doi.org/10.3133/wri894106.","productDescription":"vi, 58 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":2336,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://il.water.usgs.gov/pubsearch/reports.cgi/view?series=WRIR&number=89-4106","linkFileType":{"id":5,"text":"html"}},{"id":159073,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4106/report-thumb.jpg"},{"id":57350,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4106/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db69998d","contributors":{"authors":[{"text":"Mades, Dean M.","contributorId":102888,"corporation":false,"usgs":true,"family":"Mades","given":"Dean","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":199985,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weiss, Linda S. lsweiss@usgs.gov","contributorId":2955,"corporation":false,"usgs":true,"family":"Weiss","given":"Linda","email":"lsweiss@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":199984,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gray, John R. 0000-0002-8817-3701 jrgray@usgs.gov","orcid":"https://orcid.org/0000-0002-8817-3701","contributorId":1158,"corporation":false,"usgs":true,"family":"Gray","given":"John","email":"jrgray@usgs.gov","middleInitial":"R.","affiliations":[{"id":5058,"text":"Office of the Chief Scientist for Water","active":true,"usgs":true}],"preferred":true,"id":199983,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":28655,"text":"wri894057 - 1991 - Adequacy of available hydrogeologic data for evaluation of declining ground-water levels in the Fort Rock Basin, south-central Oregon","interactions":[],"lastModifiedDate":"2017-02-07T08:23:34","indexId":"wri894057","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"89-4057","title":"Adequacy of available hydrogeologic data for evaluation of declining ground-water levels in the Fort Rock Basin, south-central Oregon","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri894057","usgsCitation":"McFarland, W.D., and Ryals, G., 1991, Adequacy of available hydrogeologic data for evaluation of declining ground-water levels in the Fort Rock Basin, south-central Oregon: U.S. Geological Survey Water-Resources Investigations Report 89-4057, vii, 47 p. :ill., maps (1 col.) ;28 cm., https://doi.org/10.3133/wri894057.","productDescription":"vii, 47 p. :ill., maps (1 col.) ;28 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":126839,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4057/report-thumb.jpg"},{"id":57497,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1989/4057/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57498,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4057/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699665","contributors":{"authors":[{"text":"McFarland, W. D.","contributorId":57099,"corporation":false,"usgs":true,"family":"McFarland","given":"W.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":200180,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ryals, G.N.","contributorId":47374,"corporation":false,"usgs":true,"family":"Ryals","given":"G.N.","email":"","affiliations":[],"preferred":false,"id":200179,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29480,"text":"wri904098 - 1991 - An Axisymmetric finite-difference flow model to simulate drawdown in and around a pumped well","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri904098","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"90-4098","title":"An Axisymmetric finite-difference flow model to simulate drawdown in and around a pumped well","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri904098","usgsCitation":"Rutledge, A.T., 1991, An Axisymmetric finite-difference flow model to simulate drawdown in and around a pumped well: U.S. Geological Survey Water-Resources Investigations Report 90-4098, vi, 33 p. :ill. ;28 cm., https://doi.org/10.3133/wri904098.","productDescription":"vi, 33 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":122256,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4098/report-thumb.jpg"},{"id":58324,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4098/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686549","contributors":{"authors":[{"text":"Rutledge, A. T.","contributorId":38532,"corporation":false,"usgs":true,"family":"Rutledge","given":"A.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":201590,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18170,"text":"ofr91501 - 1991 - Directory of member organizations of the National Water Data Exchange (NAWDEX)","interactions":[{"subject":{"id":18169,"text":"ofr90141 - 1990 - Directory of member organizations of the National Water Data Exchange (NAWDEX)","indexId":"ofr90141","publicationYear":"1990","noYear":false,"title":"Directory of member organizations of the National Water Data Exchange (NAWDEX)"},"predicate":"SUPERSEDED_BY","object":{"id":18170,"text":"ofr91501 - 1991 - Directory of member organizations of the National Water Data Exchange (NAWDEX)","indexId":"ofr91501","publicationYear":"1991","noYear":false,"title":"Directory of member organizations of the National Water Data Exchange (NAWDEX)"},"id":1},{"subject":{"id":18170,"text":"ofr91501 - 1991 - Directory of member organizations of the National Water Data Exchange (NAWDEX)","indexId":"ofr91501","publicationYear":"1991","noYear":false,"title":"Directory of member organizations of the National Water Data Exchange (NAWDEX)"},"predicate":"SUPERSEDED_BY","object":{"id":18172,"text":"ofr93138 - 1993 - Directory of member organizations of the National Water Data Exchange (NAWDEX)","indexId":"ofr93138","publicationYear":"1993","noYear":false,"title":"Directory of member organizations of the National Water Data Exchange (NAWDEX)"},"id":2}],"supersededBy":{"id":18172,"text":"ofr93138 - 1993 - Directory of member organizations of the National Water Data Exchange (NAWDEX)","indexId":"ofr93138","publicationYear":"1993","noYear":false,"title":"Directory of member organizations of the National Water Data Exchange (NAWDEX)"},"lastModifiedDate":"2025-07-28T15:44:16.486733","indexId":"ofr91501","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-501","title":"Directory of member organizations of the National Water Data Exchange (NAWDEX)","docAbstract":"<p>The National Water Data Exchange (NAWDEX) is a national confederation of water-oriented organizations working together to improve access to water data. It consists of member organizations from all sectors of the water-data community. This Directory provides the names, addresses, and telephone numbers of all NAWDEX member organizations and thier designated NAWDEX representatives.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr91501","usgsCitation":"Blackwell, C.D., 1991, Directory of member organizations of the National Water Data Exchange (NAWDEX): U.S. Geological Survey Open-File Report 91-501, xi, 103 p., https://doi.org/10.3133/ofr91501.","productDescription":"xi, 103 p.","costCenters":[],"links":[{"id":493006,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1991/0501/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149839,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1991/0501/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ab5a","contributors":{"authors":[{"text":"Blackwell, Cassandra D.","contributorId":25562,"corporation":false,"usgs":true,"family":"Blackwell","given":"Cassandra","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":178652,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67366,"text":"i2161A - 1991 - Isopleth maps showing regional variations in pH of stream water and ground water in relation to geologic setting and known mineral deposits, Glens Falls 1° x 2° quadrangle, New York, Vermont, and New Hampshire","interactions":[],"lastModifiedDate":"2021-10-06T21:33:39.428612","indexId":"i2161A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"2161","chapter":"A","title":"Isopleth maps showing regional variations in pH of stream water and ground water in relation to geologic setting and known mineral deposits, Glens Falls 1° x 2° quadrangle, New York, Vermont, and New Hampshire","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i2161A","usgsCitation":"Watts, K.C., 1991, Isopleth maps showing regional variations in pH of stream water and ground water in relation to geologic setting and known mineral deposits, Glens Falls 1° x 2° quadrangle, New York, Vermont, and New Hampshire: U.S. Geological Survey IMAP 2161, 1 Plate: 42.49 × 32.89 inches, https://doi.org/10.3133/i2161A.","productDescription":"1 Plate: 42.49 × 32.89 inches","costCenters":[],"links":[{"id":256384,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/2161a/report-thumb.jpg"},{"id":256383,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/2161a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":256382,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2161a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":390305,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10152.htm"}],"scale":"500000","country":"United States","state":"New Hampshire, New York, Vermont","otherGeospatial":"Glens Falls 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -74,43 ], [ -74,44 ], [ -72,44 ], [ -72,43 ], [ -74,43 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696bc4","contributors":{"authors":[{"text":"Watts, K. C.","contributorId":49344,"corporation":false,"usgs":true,"family":"Watts","given":"K.","middleInitial":"C.","affiliations":[],"preferred":false,"id":276062,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20009,"text":"ofr91537 - 1991 - Documentation of model input and output values for the simulation of ground-water flow in Carson Valley, Douglas County, Nevada, and Alpine County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:07:34","indexId":"ofr91537","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-537","title":"Documentation of model input and output values for the simulation of ground-water flow in Carson Valley, Douglas County, Nevada, and Alpine County, California","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr91537","usgsCitation":"Maurer, D.K., 1991, Documentation of model input and output values for the simulation of ground-water flow in Carson Valley, Douglas County, Nevada, and Alpine County, California: U.S. Geological Survey Open-File Report 91-537, iii, 5 p. ;28 cm. +1 computer disk 5 1/4., https://doi.org/10.3133/ofr91537.","productDescription":"iii, 5 p. ;28 cm. +1 computer disk 5 1/4.","costCenters":[],"links":[{"id":152522,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1991/0537/report-thumb.jpg"},{"id":49539,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1991/0537/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db636208","contributors":{"authors":[{"text":"Maurer, Douglas K. dkmaurer@usgs.gov","contributorId":2308,"corporation":false,"usgs":true,"family":"Maurer","given":"Douglas","email":"dkmaurer@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":181893,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65949,"text":"i2133 - 1991 - Topographic map of the Phoenicis Lacus Southwest Quadrangle (MC-17 SW) of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:10","indexId":"i2133","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"2133","subseriesTitle":"NONE","title":"Topographic map of the Phoenicis Lacus Southwest Quadrangle (MC-17 SW) of Mars","language":"ENGLISH","doi":"10.3133/i2133","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1991, Topographic map of the Phoenicis Lacus Southwest Quadrangle (MC-17 SW) of Mars: U.S. Geological Survey IMAP 2133, 1 map ;43 x 59 cm., on sheet 81 x 66 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2133.","productDescription":"1 map ;43 x 59 cm., on sheet 81 x 66 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":252258,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/2133/report-thumb.jpg"},{"id":251412,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/2133/report.pdf","size":"29","linkFileType":{"id":1,"text":"pdf"}},{"id":251413,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2133/plate-1.pdf","size":"2644","linkFileType":{"id":1,"text":"pdf"}}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629c31","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":534302,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20420,"text":"ofr91498 - 1991 - Sediments, nutrients, and oxygen-demanding substances in the Minnesota River: Selected water-quality data, 1989-90","interactions":[],"lastModifiedDate":"2018-03-19T10:45:34","indexId":"ofr91498","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-498","title":"Sediments, nutrients, and oxygen-demanding substances in the Minnesota River: Selected water-quality data, 1989-90","docAbstract":"<p>This report presents selected physical and chemical data collected by the U.S. Geological Survey for the Minnesota River Assessment Project, a four-year interagency study coordinated by the Minnesota Pollution Control Agency. 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,{"id":18983,"text":"ofr91236 - 1991 - Listings of model input values for the simulation of ground-water flow in the San Andres-Glorieta aquifer in the Acoma Embayment and eastern Zuni Uplift, west-central New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:07:30","indexId":"ofr91236","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-236","title":"Listings of model input values for the simulation of ground-water flow in the San Andres-Glorieta aquifer in the Acoma Embayment and eastern Zuni Uplift, west-central New Mexico","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nAvailable from U.S. Geological Survey Books and Open-File Reports,","doi":"10.3133/ofr91236","usgsCitation":"Frenzel, P.F., 1991, Listings of model input values for the simulation of ground-water flow in the San Andres-Glorieta aquifer in the Acoma Embayment and eastern Zuni Uplift, west-central New Mexico: U.S. Geological Survey Open-File Report 91-236, 2 computer disks ;5 1/4 in. +1 booklet (iii, 7p. ; 28 cm.), https://doi.org/10.3133/ofr91236.","productDescription":"2 computer disks ;5 1/4 in. +1 booklet (iii, 7p. ; 28 cm.)","costCenters":[],"links":[{"id":151795,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1991/0236/report-thumb.jpg"},{"id":48391,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1991/0236/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4ed9","contributors":{"authors":[{"text":"Frenzel, Peter F.","contributorId":59442,"corporation":false,"usgs":true,"family":"Frenzel","given":"Peter","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":180090,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30541,"text":"wri904189 - 1991 - Ground-water levels and tritium concentrations at the Maxey Flats Low-Level Radioactive Waste Disposal Site near Morehead, Kentucky, June 1984 to April 1989","interactions":[],"lastModifiedDate":"2012-02-02T00:09:08","indexId":"wri904189","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"90-4189","title":"Ground-water levels and tritium concentrations at the Maxey Flats Low-Level Radioactive Waste Disposal Site near Morehead, Kentucky, June 1984 to April 1989","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri904189","usgsCitation":"Wilson, K.S., and Lyons, B., 1991, Ground-water levels and tritium concentrations at the Maxey Flats Low-Level Radioactive Waste Disposal Site near Morehead, Kentucky, June 1984 to April 1989: U.S. Geological Survey Water-Resources Investigations Report 90-4189, v, 217 p. (one folded) :ill. ;28 cm., https://doi.org/10.3133/wri904189.","productDescription":"v, 217 p. (one folded) :ill. ;28 cm.","costCenters":[],"links":[{"id":126366,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4189/report-thumb.jpg"},{"id":59316,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1990/4189/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59317,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4189/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db6681fd","contributors":{"authors":[{"text":"Wilson, K. S.","contributorId":41042,"corporation":false,"usgs":true,"family":"Wilson","given":"K.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":203428,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lyons, B.E.","contributorId":92710,"corporation":false,"usgs":true,"family":"Lyons","given":"B.E.","email":"","affiliations":[],"preferred":false,"id":203429,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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