Delavan Lake is a eutrophic, recreational lake in a densely populated area of southeastern Wisconsin. Sewage effluent and septic tank drainage were diverted out of the drainage basin of the lake to improve its water quality in 1981. The worst known blue-green algal bloom occurred in the lake in the summer of 1983. A comprehensive hydrologic and water-quality investigation was started in October 1983 to determine why the water quality in the lake apparently had not improved after cessation of influxes of waste waters. This report describes the hydrology and water quality of Delavan Lake and its drainage basin during the 1984 and 1985 water years.
\nAll major external inputs and outputs of phosphorus and nitrogen to the lake were measured to assess the importance of each source. Internal loading of phosphorus was calculated as a residual of a mass-balance budget. The in-lake phosphorus mass during the 2-year study shows a gradual declining trend that suggests an improving lake condition but also could be due to a random phosphorus decline. Future monitoring will be needed to determine whether the decline in phosphorus has indeed occurred as a result of waste-water diversion.
\nContinuous streamflow and water-quality monitoring in the subbasins of the Delavan Lake watershed showed a wide range of annual phosphorus and nitrogen yields during the study. Jackson Creek tributary, which predominantly drains the city of Elkhorn, had the highest average yields of phosphorus (838 pounds per square mile) and Kjeldahl nitrogen (3,600 pounds per square mile). These yields were almost three times those found in the Jackson Creek basin, which has the largest livestock population. The other major tributary, Delavan Lake tributary 2, had much lower average annual yields of phosphorus (53.1 pounds per square mile) and Kjeldahl nitrogen (550 pounds per square mile). The lower yields in this tributary result from significantly reduced runoff caused by storage and evapotranspiration in a large pond that is surrounded by a wetland in the stream's basin.
\nExternal loading of phosphorus and nitrogen were sufficient to cause eutrophic conditions. Internal loading of phosphorus was more than two times the external phosphorus supply. Most of the internal loading occurred when the hypolimnion was anoxic during summer. Internal loading of phosphorus during the 1985 water year was significantly reduced from that of 1984 because of a shorter anoxic period.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri874168","collaboration":"Prepared in cooperation with the Delevan Lake Sanitary District","usgsCitation":"Field, S.J., and Duerk, M., 1988, Hydrology and water quality of Delavan Lake in southeastern Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 87-4168, vi, 107 p., https://doi.org/10.3133/wri874168.","productDescription":"vi, 107 p.","numberOfPages":"112","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":55950,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4168/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123372,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4168/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","otherGeospatial":"Delevan Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.53675842285156,\n 42.74449090412214\n ],\n [\n -88.72695922851562,\n 42.597070956721446\n ],\n [\n -88.71253967285156,\n 42.54751604081074\n ],\n [\n -88.6328887939453,\n 42.54144538620976\n ],\n [\n -88.58894348144531,\n 42.55763248666914\n ],\n [\n -88.53813171386719,\n 42.60465241823049\n ],\n [\n -88.48663330078125,\n 42.627896481020855\n ],\n [\n -88.45916748046875,\n 42.63042248679955\n ],\n [\n -88.43170166015625,\n 42.63698962207662\n ],\n [\n -88.41522216796875,\n 42.6450712987999\n ],\n [\n -88.39462280273438,\n 42.67082463742399\n ],\n [\n -88.38363647460938,\n 42.69303463329987\n ],\n [\n -88.44612121582031,\n 42.72532590823042\n ],\n [\n -88.53675842285156,\n 42.74449090412214\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604c0c","contributors":{"authors":[{"text":"Field, S. J.","contributorId":50540,"corporation":false,"usgs":true,"family":"Field","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":197529,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Duerk, M.D.","contributorId":18806,"corporation":false,"usgs":true,"family":"Duerk","given":"M.D.","affiliations":[],"preferred":false,"id":197528,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":26239,"text":"wri874239 - 1988 - A water-resources appraisal of the Mount Shasta area in northern California, 1985","interactions":[],"lastModifiedDate":"2016-09-14T12:35:25","indexId":"wri874239","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":"87-4239","title":"A water-resources appraisal of the Mount Shasta area in northern California, 1985","docAbstract":"Present Mount Shasta, California, area hydrologic characteristics were documented to compare future changes due to land use or volcanic activity. Lower flanks of Mount Shasta consist of broad aprons of pyroclastic-flow, debris flow, and fluvial deposits, with incised channels on upper parts of the mountain. Data include glacial areas and volumes, streamflow, sediment concentrations, temperature, and water chemistry of groundwater and springs. Many springs issue from fractures in lava and lava tubes around Mount Shasta and serve as sources of water for nearby towns. Groundwater levels fluctuate as much as 27 ft. Water sampled from wells meets U.S. Environmental Protection Agency drinking water standards. Streamflow is affected by snowfield and glacial melt and precipitation, with some streams showing diurnal variations related to daily air temperature changes. Only four streams have sufficient streamflow to travel more than about 6 mi from the summit; differences in low flows are attributed to groundwater stored in materials that compose the mountain and alluvial fans and the rain shadow effect on precipitation in northwest areas of the mountain. Most streamflow is ephemeral and percolates into channel beds on alluvial fans. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874239","usgsCitation":"Blodgett, J.C., Poeschel, K., and Thornton, J., 1988, A water-resources appraisal of the Mount Shasta area in northern California, 1985: U.S. Geological Survey Water-Resources Investigations Report 87-4239, v, 46 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874239.","productDescription":"v, 46 p. :ill., maps ;28 cm.","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":55040,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4239/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":126681,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4239/report-thumb.jpg"},{"id":55039,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4239/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d9f","contributors":{"authors":[{"text":"Blodgett, J. C.","contributorId":32154,"corporation":false,"usgs":true,"family":"Blodgett","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":196040,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poeschel, K.R.","contributorId":98715,"corporation":false,"usgs":true,"family":"Poeschel","given":"K.R.","affiliations":[],"preferred":false,"id":196042,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thornton, J.L.","contributorId":41460,"corporation":false,"usgs":true,"family":"Thornton","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":196041,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":4705,"text":"twri06A1 - 1988 - A modular three-dimensional finite-difference ground-water flow model","interactions":[{"subject":{"id":20038,"text":"ofr83875 - 1984 - A modular three-dimensional finite-difference ground-water flow model","indexId":"ofr83875","publicationYear":"1984","noYear":false,"title":"A modular three-dimensional finite-difference ground-water flow model"},"predicate":"SUPERSEDED_BY","object":{"id":4705,"text":"twri06A1 - 1988 - A modular three-dimensional finite-difference ground-water flow model","indexId":"twri06A1","publicationYear":"1988","noYear":false,"title":"A modular three-dimensional finite-difference ground-water flow model"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:31","indexId":"twri06A1","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"06-A1","title":"A modular three-dimensional finite-difference ground-water flow model","docAbstract":"This report presents a finite-difference model and its associated modular computer program. The model simulates flow in three dimensions. The report includes detailed explanations of physical and mathematical concepts on which the model is based and an explanation of how those concepts are incorporated in the modular structure of the computer program. The modular structure consists of a Main Program and a series of highly independent subroutines called 'modules.' The modules are grouped into 'packages.' Each package deals with a specific feature of the hydrologic system which is to be simulated, such as flow from rivers or flow into drains, or with a specific method of solving linear equations which describe the flow system, such as the Strongly Implicit Procedure or Slice-Successive Overrelaxation. \r\n\r\nThe division of the program into modules permits the user to examine specific hydrologic features of the model independently. This also facilita development of additional capabilities because new packages can be added to the program without modifying the existing packages. The input and output systems of the computer program are also designed to permit maximum flexibility. \r\n\r\nGround-water flow within the aquifer is simulated using a block-centered finite-difference approach. Layers can be simulated as confined, unconfined, or a combination of confined and unconfined. Flow associated with external stresses, such as wells, areal recharge, evapotranspiration, drains, and streams, can also be simulated. The finite-difference equations can be solved using either the Strongly Implicit Procedure or Slice-Successive Overrelaxation. \r\n\r\nThe program is written in FORTRAN 77 and will run without modification on most computers that have a FORTRAN 77 compiler. For each program ,module, this report includes a narrative description, a flow chart, a list of variables, and a module listing.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/twri06A1","issn":"0565-596X","usgsCitation":"McDonald, M.G., and Harbaugh, A.W., 1988, A modular three-dimensional finite-difference ground-water flow model: U.S. Geological Survey Techniques of Water-Resources Investigations 06-A1, 586 p. :ill. ;28 cm., https://doi.org/10.3133/twri06A1.","productDescription":"586 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":139143,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":295,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri6a1/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae07b","contributors":{"authors":[{"text":"McDonald, Michael G.","contributorId":47352,"corporation":false,"usgs":true,"family":"McDonald","given":"Michael","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":149652,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harbaugh, Arlen W. harbaugh@usgs.gov","contributorId":426,"corporation":false,"usgs":true,"family":"Harbaugh","given":"Arlen","email":"harbaugh@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":149651,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27106,"text":"wri874034 - 1988 - Hydrogeology, aquifer characteristics, and ground-water flow of the surficial aquifer system, Broward County, Florida","interactions":[],"lastModifiedDate":"2022-01-10T12:39:00.489015","indexId":"wri874034","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":"87-4034","title":"Hydrogeology, aquifer characteristics, and ground-water flow of the surficial aquifer system, Broward County, Florida","docAbstract":"The surficial aquifer system, in which an unconfined groundwater flow system exists, comprises the sediments from land surface to the intermediate confining unit (formerly called the Floridan aquiclude) in Broward County, Florida. These sediments have hydraulic conductivities that range more than seven orders of magnitude from about 0.001 ft/d to more than 10,000 ft/d. The sediments are grouped into (1) the Biscayne aquifer, (2) a semiconfining unit, (3) a gray limestone aquifer in west Broward County, and (4) basal sand or clayey sand. The system is about 160 ft thick in west Broward County and more than 350 ft thick in east Broward. Transmissivities, locally variable, show a clear areal trend from greater than 300,000 sq ft/day in southeast Broward County to less than 75,000 sq ft/day in the northwest part of the county. Very high transmissivity is associated with the Biscayne aquifer. Transmissivity of the gray limestone aquifer ranged from about 20,000 to 88,000 sq ft/day. Topography, water levels, geologic framework, and water quality in west Broward County suggest past and present groundwater movement is south or southeast. Drainage and urban development have greatly altered circulation patterns in east Broward County , eliminating the original coastal groundwater ridge, causing rapid surface runoff and short groundwater flow paths, and saltwater intrusion. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri874034","collaboration":"Prepared in cooperation with the South Florida Water Management District","usgsCitation":"Fish, J., 1988, Hydrogeology, aquifer characteristics, and ground-water flow of the surficial aquifer system, Broward County, Florida: U.S. Geological Survey Water-Resources Investigations Report 87-4034, vi, 92 p., https://doi.org/10.3133/wri874034.","productDescription":"vi, 92 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science 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Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrVA871","usgsCitation":"Prugh, B., Easton, F., and Lynch, D.D., 1988, Water resources data for Virginia, water year 1987: U.S. Geological Survey Water Data Report VA-87-1, xiv, 441 p., https://doi.org/10.3133/wdrVA871.","productDescription":"xiv, 441 p.","costCenters":[],"links":[{"id":380815,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1987/va-87-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":184397,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1987/va-87-1/report-thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc80d","contributors":{"authors":[{"text":"Prugh, B.J.","contributorId":88811,"corporation":false,"usgs":true,"family":"Prugh","given":"B.J.","affiliations":[],"preferred":false,"id":256726,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Easton, F.J.","contributorId":61096,"corporation":false,"usgs":true,"family":"Easton","given":"F.J.","email":"","affiliations":[],"preferred":false,"id":256725,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lynch, D. D.","contributorId":12075,"corporation":false,"usgs":true,"family":"Lynch","given":"D.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":256724,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":27177,"text":"wri884040 - 1988 - Geohydrology of the Navajo sandstone in western Kane, southwestern Garfield, and southeastern Iron counties, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:08:26","indexId":"wri884040","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":"88-4040","title":"Geohydrology of the Navajo sandstone in western Kane, southwestern Garfield, and southeastern Iron counties, Utah","docAbstract":"The upper Navajo and Lamb Point aquifers in the Navajo Sandstone are the principal source of water for the city of Kanab, irrigation, stock, and for rural homes in the study area. Well logs and outcrop descriptions indicate the Navajo Sandstone consists of the Lamb Point Tongue and an unnamed upper member that are separated by the Tenney Canyon Tongue of the Kayenta Formation. The main Kayenta Formation underlies the Lamb Point Tongue. The Lamb Point Tongue and the upper member of the Navajo Sandstone are saturated and hydraulically connected through the Tenney Canyon Tongue. Available data indicate that precipitation percolates to the groundwater reservoir where the Navajo Sandstone crops out. Estimates of the rate of recharge at the outcrop range from 0.1 to as much as 2.8 in/yr. Water level data indicate that water moves from the upper member of the Navajo Sandstone, through the Tenney Canyon Tongue, and into the Lamb Point Tongue. Lateral flow is generally from the outcrop areas toward the incised canyons formed by tributaries of Kanab Creek and Johnson Wash. Direction and rate of groundwater movement and the location and character of the natural hydrologic boundaries in the northern part of the area where the Navajo Sandstone is buried cannot be determined conclusively without additional water level data. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884040","usgsCitation":"Freethey, G., 1988, Geohydrology of the Navajo sandstone in western Kane, southwestern Garfield, and southeastern Iron counties, Utah: U.S. Geological Survey Water-Resources Investigations Report 88-4040, v, 43 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884040.","productDescription":"v, 43 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118738,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4040/report-thumb.jpg"},{"id":56053,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4040/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56054,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4040/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56052,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4040/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8932","contributors":{"authors":[{"text":"Freethey, G. W.","contributorId":105714,"corporation":false,"usgs":true,"family":"Freethey","given":"G. W.","affiliations":[],"preferred":false,"id":197695,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4687,"text":"twri02D2 - 1988 - Application of seismic-refraction techniques to hydrologic studies","interactions":[{"subject":{"id":13950,"text":"ofr84746 - 1986 - Application of seismic-refraction techniques to hydrologic studies","indexId":"ofr84746","publicationYear":"1986","noYear":false,"title":"Application of seismic-refraction techniques to hydrologic studies"},"predicate":"SUPERSEDED_BY","object":{"id":4687,"text":"twri02D2 - 1988 - Application of seismic-refraction techniques to hydrologic studies","indexId":"twri02D2","publicationYear":"1988","noYear":false,"title":"Application of seismic-refraction techniques to hydrologic studies"},"id":1}],"lastModifiedDate":"2019-10-15T07:46:19","indexId":"twri02D2","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"02-D2","title":"Application of seismic-refraction techniques to hydrologic studies","docAbstract":"During the past 30 years, seismic-refraction methods have been used extensively in petroleum, mineral, and engineering investigations and to some extent for hydrologic applications. Recent advances in equipment, sound sources, and computer interpretation techniques make seismic refraction a highly effective and economical means of obtaining subsurface data in hydrologic studies. Aquifers that can be defined by one or more high-seismic-velocity surface, such as (1) alluvial or glacial deposits in consolidated rock valleys, (2) limestone or sandstone underlain by metamorphic or igneous rock, or (3) saturated unconsolidated deposits overlain by unsaturated unconsolidated deposits, are ideally suited for seismic-refraction methods. These methods allow economical collection of subsurface data, provide the basis for more efficient collection of data by test drilling or aquifer tests, and result in improved hydrologic studies. This manual briefly reviews the basics of seismic-refraction theory and principles. It emphasizes the use of these techniques in hydrologic investigations and describes the planning, equipment, field procedures, and interpretation techniques needed for this type of study. Further-more, examples of the use of seismic-refraction techniques in a wide variety of hydrologic studies are presented.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/twri02D2","issn":"0565-596X","usgsCitation":"Haeni, F., 1988, Application of seismic-refraction techniques to hydrologic studies: U.S. Geological Survey Techniques of Water-Resources Investigations 02-D2, x, 86 p. , https://doi.org/10.3133/twri02D2.","productDescription":"x, 86 p. ","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"links":[{"id":139165,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":247,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri2d2/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a89a","contributors":{"authors":[{"text":"Haeni, F.P.","contributorId":87105,"corporation":false,"usgs":true,"family":"Haeni","given":"F.P.","affiliations":[],"preferred":false,"id":149624,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26372,"text":"wri884000 - 1988 - Simulation of five ground-water withdrawal projections for the Black Mesa area, Navajo and Hopi Indian Reservations, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:08:32","indexId":"wri884000","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":"88-4000","title":"Simulation of five ground-water withdrawal projections for the Black Mesa area, Navajo and Hopi Indian Reservations, Arizona","docAbstract":"The N Aquifer is the main source of water in the 5,400 sq mi Black Mesa area in the Navajo and Hopi Indian Reservations in northeastern Arizona. Water in the aquifer is under confined conditions in the central 3,300 sq mi of the area. Maximum saturated thickness is about 1,050 ft. Annual groundwater withdrawals from 1972 through 1986 averaged 5,480 acre-ft and included 3,820 acre-ft used to operate a coal mine on Black Mesa. As a result, water levels have declined in a large part of the aquifer. The coal company has applied for a permanent permit under the Surface Mining Control and Reclamation Act of 1977. An existing mathematical model of the aquifer in the Black Mesa area was converted to a newer model program and recalibrated by using revised estimates of selected aquifer parameters and a finer spatial grid. The model was used to simulate four groundwater withdrawal alternatives that combined the existing and proposed mining plans with projected constant or increasing pumpage for nearby communities. A fifth alternative combined increasing community pumpage with no mine withdrawals and was used as a basis for comparison. Simulated water levels for the year 2031 in the coal-lease area are projected to be 60 ft lower than in 1985 for the proposed mining plan combined with growing community pumpage and > 100 ft lower than predevelopment water levels over an area of 1,660 sq mi. Groundwater would rise to within 100 ft of predevelopment levels < 10 yr after mine withdrawals cease. Withdrawals at the mine were a minor factor in determining simulated water levels at most communities in the study area. Water levels at Tuba City were not affected by mine pumpage in any projection. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884000","usgsCitation":"Brown, J.G., and Eychaner, J., 1988, Simulation of five ground-water withdrawal projections for the Black Mesa area, Navajo and Hopi Indian Reservations, Arizona: U.S. Geological Survey Water-Resources Investigations Report 88-4000, v, 51 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884000.","productDescription":"v, 51 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158085,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4000/report-thumb.jpg"},{"id":55166,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4000/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db64857d","contributors":{"authors":[{"text":"Brown, J. G.","contributorId":28263,"corporation":false,"usgs":true,"family":"Brown","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":196274,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eychaner, J.H.","contributorId":34511,"corporation":false,"usgs":true,"family":"Eychaner","given":"J.H.","affiliations":[],"preferred":false,"id":196275,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":55725,"text":"wdrNJ872 - 1988 - Water resources data for New Jersey, water year 1987, volume 2, Delaware River basin and tributaries to Delaware Bay","interactions":[],"lastModifiedDate":"2019-09-24T11:54:11","indexId":"wdrNJ872","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NJ-87-2","title":"Water resources data for New Jersey, water year 1987, volume 2, Delaware River basin and tributaries to Delaware Bay","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNJ872","usgsCitation":"Bauersfeld, W., Moshinsky, E., Pustay, E., and Jones, W., 1988, Water resources data for New Jersey, water year 1987, volume 2, Delaware River basin and tributaries to Delaware Bay: U.S. Geological Survey Water Data Report NJ-87-2, 199 p., https://doi.org/10.3133/wdrNJ872.","productDescription":"199 p.","costCenters":[],"links":[{"id":174165,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1987/nj-87-2/report-thumb.jpg"},{"id":367671,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1987/nj-87-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New 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Jersey\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f26b5","contributors":{"authors":[{"text":"Bauersfeld, W.R.","contributorId":72451,"corporation":false,"usgs":true,"family":"Bauersfeld","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":254129,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moshinsky, E.W.","contributorId":104972,"corporation":false,"usgs":true,"family":"Moshinsky","given":"E.W.","email":"","affiliations":[],"preferred":false,"id":254130,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pustay, E.A.","contributorId":62604,"corporation":false,"usgs":true,"family":"Pustay","given":"E.A.","affiliations":[],"preferred":false,"id":254127,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jones, W.D.","contributorId":68384,"corporation":false,"usgs":true,"family":"Jones","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":254128,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":19032,"text":"ofr88157 - 1988 - U.S. Geological Survey ground-water studies in Utah","interactions":[],"lastModifiedDate":"2017-08-31T15:56:34","indexId":"ofr88157","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":"88-157","title":"U.S. Geological Survey ground-water studies in Utah","docAbstract":"Ground water is an important natural resource in Utah. In the basins west of the Wasatch Front, and in many other parts of Utah, ground water is the primary source of water. In many of the basins of the western desert and in parts of the Colorado Plateau, ground water is the only reliable source of water. Along the Wasatch Front to the north and south of Salt Lake City, in the Uinta Basin, and in the Sevier River drainage, surface water is the primary source of water.
Ground-water sources supply about 20 percent of all water used in Utah and about 63 percent of the water for public supply. Of the total amount of ground water used, 44 percent is for irrigation, 35 percent is for public supply, 11 percent is for industry, 5 percent is for rural domestic supplies, and 5 percent is for livestock. The major issues related to ground water in Utah are:
-Development of additional ground-water supplies while protecting existing water rights and minimizing effects on water levels, water quality, and streamflow, and
-Protection of ground-water resources from contamination by pollutants from various types of land-use and waste-disposal practices.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr88157","usgsCitation":"Gates, J., 1988, U.S. Geological Survey ground-water studies in Utah: U.S. Geological Survey Open-File Report 88-157, 2 p., https://doi.org/10.3133/ofr88157.","productDescription":"2 p.","numberOfPages":"2","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":48444,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0157/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151506,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0157/report-thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db6126b9","contributors":{"authors":[{"text":"Gates, Joseph S.","contributorId":21647,"corporation":false,"usgs":true,"family":"Gates","given":"Joseph S.","affiliations":[],"preferred":false,"id":180183,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":65367,"text":"i1913 - 1988 - Controlled photomosaic of part of the Nilosyrtis Mensae region of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:15","indexId":"i1913","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1913","subseriesTitle":"NONE","title":"Controlled photomosaic of part of the Nilosyrtis Mensae region of Mars","language":"ENGLISH","doi":"10.3133/i1913","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1988, Controlled photomosaic of part of the Nilosyrtis Mensae region of Mars: U.S. Geological Survey IMAP 1913, 1 remote sensing image ;61 x 52 cm., on sheet 96 x 59 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1913.","productDescription":"1 remote sensing image ;61 x 52 cm., on sheet 96 x 59 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190163,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":100925,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1913/plate-1.pdf","size":"6116","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db689011","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological 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included in the National Water Data Exchange Program","docAbstract":"Stations were selected to monitor water discharge and water quality of streams in eastern Montana. This report describes the stations and indicates the availability of hydrologic data through 1985. Included are stations that are operated by organizations that do not belong to the National Water Data Exchange (NAWDEX) program operated by the U.S. Geological Survey. Each station description contains a narration of the station 's history including location, drainage area, elevation, operator, period of record, type of equipment and instruments used at the station, and data availability. The data collected at each station have been identified according to type: water discharge, chemical quality, and suspended sediment. Descriptions are provided for 113 stations. These data have potential uses in characterizing small hydrologic basins, as well as other uses. A map of eastern Montana shows the location of the stations selected. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87770","usgsCitation":"Groskinsky Link, B.L., and Cary, L.E., 1988, Station descriptions and availability of discharge and water-quality data through 1985 for eastern Montana stream sites not included in the National Water Data Exchange Program: U.S. Geological Survey Open-File Report 87-770, iii, 79 p. :map ;28 cm., https://doi.org/10.3133/ofr87770.","productDescription":"iii, 79 p. :map ;28 cm.","costCenters":[],"links":[{"id":146833,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0770/report-thumb.jpg"},{"id":42588,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0770/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e3f13","contributors":{"authors":[{"text":"Groskinsky Link, B. L.","contributorId":99566,"corporation":false,"usgs":true,"family":"Groskinsky Link","given":"B.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":168636,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cary, L. E.","contributorId":47369,"corporation":false,"usgs":true,"family":"Cary","given":"L.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":168635,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":65368,"text":"i1914 - 1988 - Controlled photomosaic of part of the Nilosyrtis Mensae region of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:15","indexId":"i1914","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1914","subseriesTitle":"NONE","title":"Controlled photomosaic of part of the Nilosyrtis Mensae region of Mars","language":"ENGLISH","doi":"10.3133/i1914","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1988, Controlled photomosaic of part of the Nilosyrtis Mensae region of Mars: U.S. Geological Survey IMAP 1914, 1 remote sensing image ;61 x 49 cm., on sheet 96 x 56 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1914.","productDescription":"1 remote sensing image ;61 x 49 cm., on sheet 96 x 56 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":190164,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":100926,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1914/plate-1.pdf","size":"5866","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db688ef6","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":533755,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":65369,"text":"i1915 - 1988 - Controlled photomosaic of part of the Nilosyrtis Mensae region of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:17","indexId":"i1915","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1915","subseriesTitle":"NONE","title":"Controlled photomosaic of part of the Nilosyrtis Mensae region of Mars","language":"ENGLISH","doi":"10.3133/i1915","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1988, Controlled photomosaic of part of the Nilosyrtis Mensae region of Mars: U.S. Geological Survey IMAP 1915, 1 remote sensing image ;61 x 49 cm., on sheet 95 x 56 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1915.","productDescription":"1 remote sensing image ;61 x 49 cm., on sheet 95 x 56 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":189656,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":100927,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1915/plate-1.pdf","size":"5988","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db688f39","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":533756,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":65370,"text":"i1916 - 1988 - Controlled photomosaic of part of the Nilosyrtis Mensae region of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:17","indexId":"i1916","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1916","subseriesTitle":"NONE","title":"Controlled photomosaic of part of the Nilosyrtis Mensae region of Mars","language":"ENGLISH","doi":"10.3133/i1916","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1988, Controlled photomosaic of part of the Nilosyrtis Mensae region of Mars: U.S. Geological Survey IMAP 1916, 1 remote sensing image ;62 x 49 cm., on sheet 96 x 56 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1916.","productDescription":"1 remote sensing image ;62 x 49 cm., on sheet 96 x 56 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":189657,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":100928,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1916/plate-1.pdf","size":"5075","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db688f3c","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":533757,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":66542,"text":"i1875 - 1988 - Subsurface geology of Paleozoic, Mesozoic, and Cenozoic units in southeast Missouri","interactions":[],"lastModifiedDate":"2016-08-23T09:34:53","indexId":"i1875","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1875","title":"Subsurface geology of Paleozoic, Mesozoic, and Cenozoic units in southeast Missouri","docAbstract":"The U.S. Geological Survey is conducting a regional water-resources investigation of the Gulf Costal Plain, which includes all of the Mississippi Alluvial Plain of southeastern Missouri, locally known as the southeast lowlands. The purpose of the regional study is to describe and evaluate the major aquifer systems in sediments of Tertiary and younger age in parts of 10 states (Grubb, 1984). In the southeast lowlands of Missouri, the sub-surface stratigraphy and structural configuration of geologic units need to be described in detail to define the major aquifer syustems in the area. The purpose of this report is to describe the subsurface geologic framework for Paleozoic, Mesozoic, and Cenozoic units in the southeast lowlands of Missouri and to correlate these units to those in adjecent States using geophysical and geologic methods (index map). Geophysical logs of wells were used to determine which units are aquifers or confining beds. The drilling of the U.S. Geological Survey test well 1-X in New Madrid County, Missouri, and the subsequent interpretation of geohydrologic data from the well have provided valuable information used in the preparation of this report.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/i1875","usgsCitation":"Mesko, T.O., 1988, Subsurface geology of Paleozoic, Mesozoic, and Cenozoic units in southeast Missouri: U.S. Geological Survey IMAP 1875, 2 Plates: 40.79 x 54.10 inches and 36.42 x 18.93 inches, https://doi.org/10.3133/i1875.","productDescription":"2 Plates: 40.79 x 54.10 inches and 36.42 x 18.93 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":187893,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/i1875.GIF"},{"id":327511,"rank":701,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1875/plate-1.pdf"},{"id":327512,"rank":702,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1875/plate-2.pdf"},{"id":107160,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9963.htm","linkFileType":{"id":5,"text":"html"},"description":"9963"}],"scale":"500000","country":"United States","state":"Missouri","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -89.50561523437499,\n 37.309014074275915\n ],\n [\n -89.36279296875,\n 37.00255267215955\n ],\n [\n -89.329833984375,\n 37.142803443716836\n ],\n [\n -89.12109375,\n 37.06394430056685\n ],\n [\n -88.978271484375,\n 36.87962060502676\n ],\n [\n -88.978271484375,\n 36.641977814705946\n ],\n [\n -89.066162109375,\n 36.421282443649496\n ],\n [\n -89.329833984375,\n 36.25313319699069\n ],\n [\n -89.50561523437499,\n 35.96022296929667\n ],\n [\n -89.6044921875,\n 35.85343961959182\n ],\n [\n -89.80224609374999,\n 35.7286770448517\n ],\n [\n -90.5712890625,\n 35.71975793933433\n ],\n [\n -90.59326171875,\n 36.491973470593685\n ],\n [\n -90.37353515625,\n 36.69485094156225\n ],\n [\n -90.19775390625,\n 36.730079507078415\n ],\n [\n -90.02197265625,\n 37.03763967977139\n ],\n [\n -89.98901367187499,\n 37.16031654673677\n ],\n [\n -89.835205078125,\n 37.26530995561875\n ],\n [\n -89.593505859375,\n 37.32648861334206\n ],\n [\n -89.50561523437499,\n 37.309014074275915\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699a12","contributors":{"authors":[{"text":"Mesko, T. O.","contributorId":83934,"corporation":false,"usgs":true,"family":"Mesko","given":"T.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":274685,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":19275,"text":"ofr88114 - 1988 - National water-information clearinghouse activities; ground-water perspective","interactions":[],"lastModifiedDate":"2012-02-02T00:07:32","indexId":"ofr88114","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":"88-114","title":"National water-information clearinghouse activities; ground-water perspective","docAbstract":"The US Geological Survey (USGS) has functioned for many years as an informal clearinghouse for water resources information, enabling users to access groundwater information effectively. Water resources clearinghouse activities of the USGS are conducted through several separate computerized water information programs that are involved in the collection, storage, retrieval, and distribution of different types of water information. The following USGS programs perform water information clearinghouse functions and provide the framework for a formalized National Water-Information Clearinghouse: (1) The National Water Data Exchange--a nationwide confederation of more than 300 Federal, State, local, government, academic, and private water-oriented organizations that work together to improve access to water data; (2) the Water Resources Scientific Information Center--acquires, abstracts, and indexes the major water-resources-related literature of the world, and provides this information to the water resources community; (3) the Information Transfer Program--develops innovative approaches to transfer information and technology developed within the USGS to audiences in the public and private sectors; (4) the Hydrologic Information Unit--provides responses to a variety of requests, both technical and lay-oriented, for water resources information , and helps efforts to conduct water resources research; (5) the Water Data Storage and Retrieval System--maintains accessible computerized files of hydrologic data collected nationwide, by the USGS and other governmental agencies, from stream gaging stations, groundwater observation wells, and surface- and groundwater quality sampling sites; (6) the Office of Water Data Coordination--coordinate the water data acquisition activities of all agencies of the Federal Government, and is responsible for the planning, design, and inter-agency coordination of a national water data and information network; and (7) the Water Resources Research Institute Program--coordinates and evaluates activities performed by a variety of groundwater contamination studies ranging from field investigations to analysis of socioeconomic issues. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88114","usgsCitation":"Haupt, C., and Jensen, R., 1988, National water-information clearinghouse activities; ground-water perspective: U.S. Geological Survey Open-File Report 88-114, 2 p. :ill. ;28 cm., https://doi.org/10.3133/ofr88114.","productDescription":"2 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":151295,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0114/report-thumb.jpg"},{"id":48737,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0114/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db69802c","contributors":{"authors":[{"text":"Haupt, C.A.","contributorId":87570,"corporation":false,"usgs":true,"family":"Haupt","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":180603,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jensen, R.A.","contributorId":71570,"corporation":false,"usgs":true,"family":"Jensen","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":180602,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":19277,"text":"ofr88140 - 1988 - U.S. Geological Survey ground-water studies in Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:07:32","indexId":"ofr88140","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":"88-140","title":"U.S. Geological Survey ground-water studies in Oklahoma","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88140","usgsCitation":"Havens, J., 1988, U.S. Geological Survey ground-water studies in Oklahoma: U.S. Geological Survey Open-File Report 88-140, 2 p . :ill. ;28 cm., https://doi.org/10.3133/ofr88140.","productDescription":"2 p . :ill. ;28 cm.","costCenters":[],"links":[{"id":151297,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0140/report-thumb.jpg"},{"id":48739,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0140/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db612764","contributors":{"authors":[{"text":"Havens, J.S.","contributorId":12043,"corporation":false,"usgs":true,"family":"Havens","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":180605,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":19442,"text":"ofr88310 - 1988 - Water quality of runoff to the Clarksville Memorial Hospital drainage well and of Mobley Spring, Clarksville, Tennessee, February and March, 1988","interactions":[],"lastModifiedDate":"2012-02-02T00:07:42","indexId":"ofr88310","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":"88-310","title":"Water quality of runoff to the Clarksville Memorial Hospital drainage well and of Mobley Spring, Clarksville, Tennessee, February and March, 1988","docAbstract":"A drainage well and a spring in Clarksville, Tennessee, have been instrumented to collect storm related data in order to define the types and concentrations of water quality characteristics in stormwater runoff and in the receiving groundwater basin. Water quality samples of storm runoff at the drainage well at Clarksville Memorial Hospital and of nearby Mobley Spring were collected during four storms and during normal flow conditions during February and March 1988. Samples were analyzed for major inorganic water quality constituents, selected trace metals, and organics. Several samples from the drainage well and the spring had trace-metals concentrations that exceeded maximum contaminant levels for State drinking-water standards. Organic compounds including phenols, polynuclear aromatic hydrocarbons, and other base-neutral extractable organic substance are present in samples from both the drainage well and spring. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88310","usgsCitation":"Hoos, A., 1988, Water quality of runoff to the Clarksville Memorial Hospital drainage well and of Mobley Spring, Clarksville, Tennessee, February and March, 1988: U.S. Geological Survey Open-File Report 88-310, iv, 26 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr88310.","productDescription":"iv, 26 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":1107,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr_88-310","linkFileType":{"id":5,"text":"html"}},{"id":153458,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f996f","contributors":{"authors":[{"text":"Hoos, A.B.","contributorId":23572,"corporation":false,"usgs":true,"family":"Hoos","given":"A.B.","affiliations":[],"preferred":false,"id":180911,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55819,"text":"wdrNM871 - 1988 - Water resources data, New Mexico, water year 1987","interactions":[],"lastModifiedDate":"2013-07-12T13:33:54","indexId":"wdrNM871","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NM-87-1","title":"Water resources data, New Mexico, water year 1987","docAbstract":"Water resources data for the 198, water year for New Mexico consist of records of discharge and water quality of streams; stage, contents and water quality of lakes and reservoirs; and water levels and water quality in wells and springs. This report contains discharge records for 165 gaging stations; stage and contents for 25 lakes and reservoirs; water quality for 67 gaging stations and 180 wells; and water levels at 100 observation wells. Also included are 108 crest-stage partial-record stations. Additional water data were collected at various sites) not involved in the systematic data collect-ion program, and are published as miscellaneous measurements. Also, one seepage investigation is published this year. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in New Mexico.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrNM871","usgsCitation":"Beal, L.V., and Gold, R., 1988, Water resources data, New Mexico, water year 1987: U.S. Geological Survey Water Data Report NM-87-1, 464 p., https://doi.org/10.3133/wdrNM871.","productDescription":"464 p.","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":185371,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":270298,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1987/nm-87-1/report.pdf"}],"country":"United States","state":"New Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0502,31.3322 ], [ -109.0502,37.0003 ], [ -103.002,37.0003 ], [ -103.002,31.3322 ], [ -109.0502,31.3322 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0f52","contributors":{"authors":[{"text":"Beal, Linda V.","contributorId":26367,"corporation":false,"usgs":true,"family":"Beal","given":"Linda","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":254318,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gold, Robert L.","contributorId":78324,"corporation":false,"usgs":true,"family":"Gold","given":"Robert L.","affiliations":[],"preferred":false,"id":254319,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":55724,"text":"wdrNJ871 - 1988 - Water resources data for New Jersey, water year 1987, volume 1, Atlantic slope basins, Hudson River to Cape May","interactions":[],"lastModifiedDate":"2020-12-22T18:30:32.124531","indexId":"wdrNJ871","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NJ-87-1","title":"Water resources data for New Jersey, water year 1987, volume 1, Atlantic slope basins, Hudson River to Cape May","docAbstract":"No abstract available.
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