{"pageNumber":"4287","pageRowStart":"107150","pageSize":"25","recordCount":165901,"records":[{"id":31896,"text":"ofr87495C - 1987 - Palinspastic paleogeographic map of the Paleogene sequence of the Circum-Borneo region, Southeast Asia","interactions":[],"lastModifiedDate":"2012-03-02T17:16:06","indexId":"ofr87495C","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1987","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":"87-495","chapter":"C","title":"Palinspastic paleogeographic map of the Paleogene sequence of the Circum-Borneo region, Southeast Asia","language":"ENGLISH","doi":"10.3133/ofr87495C","usgsCitation":"Robinson, K., 1987, Palinspastic paleogeographic map of the Paleogene sequence of the Circum-Borneo region, Southeast Asia: U.S. Geological Survey Open-File Report 87-495, 1 over-size sheet, scale 1:2,000,000 (1 inch = about 32 miles) , https://doi.org/10.3133/ofr87495C.","productDescription":"1 over-size sheet, scale 1:2,000,000 (1 inch = about 32 miles) ","costCenters":[],"links":[{"id":161319,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":21245,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0495c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":21246,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0495c/plate-1-preview.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"200000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db6899fb","contributors":{"authors":[{"text":"Robinson, Keith","contributorId":80277,"corporation":false,"usgs":true,"family":"Robinson","given":"Keith","affiliations":[],"preferred":false,"id":207185,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":31897,"text":"ofr87495D - 1987 - Palinspastic thickness map of the Neogene sequence of the Circum-Borneo region, Southeast Asia","interactions":[],"lastModifiedDate":"2012-03-02T17:16:06","indexId":"ofr87495D","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1987","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":"87-495","chapter":"D","title":"Palinspastic thickness map of the Neogene sequence of the Circum-Borneo region, Southeast Asia","language":"ENGLISH","doi":"10.3133/ofr87495D","usgsCitation":"Robinson, K., 1987, Palinspastic thickness map of the Neogene sequence of the Circum-Borneo region, Southeast Asia: U.S. Geological Survey Open-File Report 87-495, 1 over-size sheet, scale 1:2,000,000 (1 inch = about 32 miles). , https://doi.org/10.3133/ofr87495D.","productDescription":"1 over-size sheet, scale 1:2,000,000 (1 inch = about 32 miles). ","costCenters":[],"links":[{"id":161339,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":21247,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0495d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":21248,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0495d/plate-1-preview.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"200000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689a09","contributors":{"authors":[{"text":"Robinson, Keith","contributorId":80277,"corporation":false,"usgs":true,"family":"Robinson","given":"Keith","affiliations":[],"preferred":false,"id":207186,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":31898,"text":"ofr87495E - 1987 - Palinspastic paleogeographic map of the Neogene sequence of the Circum-Borneo region, Southeast Asia","interactions":[],"lastModifiedDate":"2012-03-02T17:16:06","indexId":"ofr87495E","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1987","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":"87-495","chapter":"E","title":"Palinspastic paleogeographic map of the Neogene sequence of the Circum-Borneo region, Southeast Asia","language":"ENGLISH","doi":"10.3133/ofr87495E","usgsCitation":"Robinson, K., 1987, Palinspastic paleogeographic map of the Neogene sequence of the Circum-Borneo region, Southeast Asia: U.S. Geological Survey Open-File Report 87-495, 1 over-size sheet, scale 1:2,000,000 (1 inch = about 32 miles)., https://doi.org/10.3133/ofr87495E.","productDescription":"1 over-size sheet, scale 1:2,000,000 (1 inch = about 32 miles).","costCenters":[],"links":[{"id":161210,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":21249,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0495e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"200000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b08e4b07f02db69b9b2","contributors":{"authors":[{"text":"Robinson, Keith","contributorId":80277,"corporation":false,"usgs":true,"family":"Robinson","given":"Keith","affiliations":[],"preferred":false,"id":207187,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":31894,"text":"ofr87495A - 1987 - Thickness map of the petroliferous Tertiary sequence of the Circum-Borneo region, Southeast Asia","interactions":[],"lastModifiedDate":"2012-03-02T17:16:06","indexId":"ofr87495A","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1987","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":"87-495","chapter":"A","title":"Thickness map of the petroliferous Tertiary sequence of the Circum-Borneo region, Southeast Asia","language":"ENGLISH","doi":"10.3133/ofr87495A","usgsCitation":"Robinson, K., and DuBois, E., 1987, Thickness map of the petroliferous Tertiary sequence of the Circum-Borneo region, Southeast Asia: U.S. Geological Survey Open-File Report 87-495, 1 over-size sheet, scale 1:2,000,000 (1 inch = about 32 miles). , https://doi.org/10.3133/ofr87495A.","productDescription":"1 over-size sheet, scale 1:2,000,000 (1 inch = about 32 miles). ","costCenters":[],"links":[{"id":160258,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":21242,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0495a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":21243,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0495a/plate-1-preview.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"200000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a55e4b07f02db62cea1","contributors":{"authors":[{"text":"Robinson, Keith","contributorId":80277,"corporation":false,"usgs":true,"family":"Robinson","given":"Keith","affiliations":[],"preferred":false,"id":207183,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DuBois, E.P.","contributorId":70644,"corporation":false,"usgs":true,"family":"DuBois","given":"E.P.","email":"","affiliations":[],"preferred":false,"id":207182,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":31895,"text":"ofr87495B - 1987 - Palinspastic thickness map of the Paleogene sequence of the Circum-Borneo region, Southeast Asia","interactions":[],"lastModifiedDate":"2012-03-02T17:16:06","indexId":"ofr87495B","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1987","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":"87-495","chapter":"B","title":"Palinspastic thickness map of the Paleogene sequence of the Circum-Borneo region, Southeast Asia","language":"ENGLISH","doi":"10.3133/ofr87495B","usgsCitation":"Robinson, K., 1987, Palinspastic thickness map of the Paleogene sequence of the Circum-Borneo region, Southeast Asia: U.S. Geological Survey Open-File Report 87-495, 1 over-size sheet, scale 1:2,000,000 (1 inch = about 32 miles). , https://doi.org/10.3133/ofr87495B.","productDescription":"1 over-size sheet, scale 1:2,000,000 (1 inch = about 32 miles). ","costCenters":[],"links":[{"id":160259,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":21244,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0495b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"200000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db689895","contributors":{"authors":[{"text":"Robinson, Keith","contributorId":80277,"corporation":false,"usgs":true,"family":"Robinson","given":"Keith","affiliations":[],"preferred":false,"id":207184,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":33521,"text":"b1639 - 1987 - The Morgan Hill, California, earthquake of April 24, 1984","interactions":[{"subject":{"id":7352,"text":"ofr84498A - 1984 - The Morgan Hill, California earthquake of April 24, 1984; a preliminary report; Volume I","indexId":"ofr84498A","publicationYear":"1984","noYear":false,"chapter":"A","title":"The Morgan Hill, California earthquake of April 24, 1984; a preliminary report; Volume I"},"predicate":"SUPERSEDED_BY","object":{"id":33521,"text":"b1639 - 1987 - The Morgan Hill, California, earthquake of April 24, 1984","indexId":"b1639","publicationYear":"1987","noYear":false,"title":"The Morgan Hill, California, earthquake of April 24, 1984"},"id":1},{"subject":{"id":17400,"text":"ofr84498B - 1984 - The Morgan Hill, California earthquake of April 24, 1984; a preliminary report; Volume II","indexId":"ofr84498B","publicationYear":"1984","noYear":false,"chapter":"B","title":"The Morgan Hill, California earthquake of April 24, 1984; a preliminary report; Volume II"},"predicate":"SUPERSEDED_BY","object":{"id":33521,"text":"b1639 - 1987 - The Morgan Hill, California, earthquake of April 24, 1984","indexId":"b1639","publicationYear":"1987","noYear":false,"title":"The Morgan Hill, California, earthquake of April 24, 1984"},"id":2}],"lastModifiedDate":"2018-10-01T19:13:22","indexId":"b1639","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1639","title":"The Morgan Hill, California, earthquake of April 24, 1984","docAbstract":"The\nMorgan\nHill\nearthquake,\na\nmoderate-size\n(M_g=6.1,\nML\n=6.2,\nM=6.2)\nevent,\nwas\nfelt\nthroughout\ncentral\nCalifornia\non\nApril\n24,\n1984.\nThe\nepicenter\nof\nthe\nearthquake\nwas\nlocated\nnear\nHalls\nValley\nsouthwest\nof\nMount\nHamilton,\nand\nthe\nevent\nis\npresumed\nto\nhave\noccurred\non\nthe\nCalaveras\nfault.\nDamage,\nhowever,\nwas\nconcentrated\nnear\nthe\nsouth\nend\nof\nthe\nAnderson\nReservoir\nand\nin\nthe\ntown\nof\nMorgan\nHill.\nA\npreliminary\nassessment\nby\nthe\nCalifornia\nOffice\nof\nEmergency\nServices\nestimated\ndamage\nto\nprivate\nproperty\nat\n$7.0\nmillion\nand\nto\nlocal-government\nfacilities\nat\n$0.5\nmillion,\nfor\na\ntotal\nof\n$7.5\nmillion\nin\ndamage.\nAcknowledgments.--!\nappreciate\nthe\nhelpful\nsuggestions\nof\nJoseph\nI.\nZiony\nand\nRobert\nD.\nBrown,\nJr.\nThese\nstudies\nwere\naided\nby\nthe\ngenerous\ncooperation\nof\nthe\nmany\nlandowners\nwho\npermitted\naccess\nto\ntheir\nproperties.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, DC","doi":"10.3133/b1639","usgsCitation":"1987, The Morgan Hill, California, earthquake of April 24, 1984: U.S. Geological Survey Bulletin 1639, Report: iii, 256 p.; Plate: 31.50 inches x 36.50 inches, https://doi.org/10.3133/b1639.","productDescription":"Report: iii, 256 p.; Plate: 31.50 inches x 36.50 inches","costCenters":[],"links":[{"id":61423,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1639/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61424,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1639/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166599,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1639/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"California","city":"Morgan Hill","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -121.75,37.25 ], [ -121.75,37.375 ], [ -121.625,37.375 ], [ -121.625,37.25 ], [ -121.75,37.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b395","contributors":{"editors":[{"text":"Hoose, Seena N.","contributorId":21867,"corporation":false,"usgs":true,"family":"Hoose","given":"Seena N.","affiliations":[],"preferred":false,"id":747035,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}} ,{"id":4666,"text":"twri03B2_spanish - 1987 - Introduccion a la hidraulica de aguas subterraneas : un texto programado para auto-ensenanza","interactions":[],"lastModifiedDate":"2013-12-20T14:29:10","indexId":"twri03B2_spanish","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1987","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":"03-B2","title":"Introduccion a la hidraulica de aguas subterraneas : un texto programado para auto-ensenanza","docAbstract":"Este ' texto programado esta diseflado para ayudarle a comprender la teoria de la hidniulica de \naguas subterraneas por medio de la auto-enseflanza. \nLa instrucci6n programada es un enfoque a una \nmateria, un metodo de aprender;que no elimina el \nesfuerzo mental del proceso de aprendizaje. Algunas secciones de este programa necesitan solamente ser leidas; otras tendrian que ser elaboradas \ncon lapiz y papel. Algunas preguntas pueden ser \ncontestadas directamente; otras requieren calculos. A medida que se avanza en el texto, tendra que \nconsultar frecuentemente textos o referencias sobre \nmatematicas, mecanica de fluidos e hidrologia. \nEn cada una de las ocho partes del texto, inicie \nel programa de instrucci6n leyendo la Secci6n 1. \nElija una respuesta a la pregunta al final de la secci6n y dirijase a la nueva secci6n indicada al lado \nde la respuesta escogida. Si su respuesta fue \ncorrecta, pase a la secci6n que contiene materia \nnueva y otra pregunta, y proceda tal como en la \nSecci6n 1. Si su respuesta no fue correcta, dirijase \na la secci6n que contiene explicaciones adicionales \nsobre el tema anterior y que le indica volver a la \npregunta inicial e intentar de nuevo. \nEn este caso, valdra Ia pena repasar el material \nde la secci6n anterior. Continue de esta man era en \nel programa hasta que llegue a Ia secci6n que indica \nel final de la parte. Observe que aunque las secciones \nestan en orden numerico en cada una de las ocho \npartes, por lo general, usted no procedeni en secuencia numerica (Secci6n 1 ala Secci6n 2, etc.) de principia a fin.","language":"Spanish","publisher":"U.S Government Printing Office","publisherLocation":"Washington","doi":"10.3133/twri03B2_spanish","issn":"0565-596X","usgsCitation":"Bennett, G.D., 1987, Introduccion a la hidraulica de aguas subterraneas : un texto programado para auto-ensenanza: U.S. Geological Survey Techniques of Water-Resources Investigations 03-B2, xi, 167 p., https://doi.org/10.3133/twri03B2_spanish.","productDescription":"xi, 167 p.","numberOfPages":"178","costCenters":[],"links":[{"id":139516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/4666/report-thumb.jpg"},{"id":279836,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/4666/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49c2e4b07f02db5d3d4b","contributors":{"authors":[{"text":"Bennett, Gordon D.","contributorId":18740,"corporation":false,"usgs":true,"family":"Bennett","given":"Gordon","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":149589,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":12000,"text":"ofr87575 - 1987 - Data on the distribution and abundance of submersed aquatic vegetation in the tidal Potomac River and estuary, Maryland, Virginia, and the District of Columbia, 1986","interactions":[],"lastModifiedDate":"2014-05-21T14:06:02","indexId":"ofr87575","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1987","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":"87-575","title":"Data on the distribution and abundance of submersed aquatic vegetation in the tidal Potomac River and estuary, Maryland, Virginia, and the District of Columbia, 1986","docAbstract":"This report summarizes data on the distribution and abundance of submersed aquatic vegetation collected in the tidal Potomac River and Estuary during 1986. Plant species were identified and dry weight determined for selected sites sampled in spring and fall. The percentage of each plant species was determined in areas of high plant density in the fall. Water quality characteristics measured include temperature, specific conductance, dissolved oxygen, pH, and transparency as indicated by Secchi depth. Maps were made of the distribution of submersed aquatic vegetation based on transect samples and a complete shoreline survey.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr87575","usgsCitation":"Rybicki, N.B., Anderson, R.T., Shapiro, J., Johnson, K.L., and Schulman, C., 1987, Data on the distribution and abundance of submersed aquatic vegetation in the tidal Potomac River and estuary, Maryland, Virginia, and the District of Columbia, 1986: U.S. Geological Survey Open-File Report 87-575, iv, 82 p., https://doi.org/10.3133/ofr87575.","productDescription":"iv, 82 p.","costCenters":[],"links":[{"id":287513,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287512,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0575/report.pdf"}],"country":"United States","state":"District of Columbia;Maryl;Virginia","otherGeospatial":"Potomac River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.5,38.0 ], [ -77.5,39.0 ], [ -76.5,39.0 ], [ -76.5,38.0 ], [ -77.5,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c831","contributors":{"authors":[{"text":"Rybicki, N. B.","contributorId":97504,"corporation":false,"usgs":true,"family":"Rybicki","given":"N.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":164603,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, R. T.","contributorId":17614,"corporation":false,"usgs":true,"family":"Anderson","given":"R.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":164600,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shapiro, J.M.","contributorId":47376,"corporation":false,"usgs":true,"family":"Shapiro","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":164601,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Johnson, K. L.","contributorId":75543,"corporation":false,"usgs":true,"family":"Johnson","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":164602,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schulman, C.L.","contributorId":103285,"corporation":false,"usgs":true,"family":"Schulman","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":164604,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":14055,"text":"ofr86301 - 1987 - Evapotranspiration and microclimate at a low-level radioactive-waste disposal site in northwestern Illinois","interactions":[{"subject":{"id":14055,"text":"ofr86301 - 1987 - Evapotranspiration and microclimate at a low-level radioactive-waste disposal site in northwestern Illinois","indexId":"ofr86301","publicationYear":"1987","noYear":false,"title":"Evapotranspiration and microclimate at a low-level radioactive-waste disposal site in northwestern Illinois"},"predicate":"SUPERSEDED_BY","object":{"id":1816,"text":"wsp2327 - 1989 - Evapotranspiration and microclimate at a low-level radioactive-waste disposal site in northwestern Illinois","indexId":"wsp2327","publicationYear":"1989","noYear":false,"title":"Evapotranspiration and microclimate at a low-level radioactive-waste disposal site in northwestern Illinois"},"id":1}],"supersededBy":{"id":1816,"text":"wsp2327 - 1989 - Evapotranspiration and microclimate at a low-level radioactive-waste disposal site in northwestern Illinois","indexId":"wsp2327","publicationYear":"1989","noYear":false,"title":"Evapotranspiration and microclimate at a low-level radioactive-waste disposal site in northwestern Illinois"},"lastModifiedDate":"2021-02-03T22:02:33.215354","indexId":"ofr86301","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"86-301","title":"Evapotranspiration and microclimate at a low-level radioactive-waste disposal site in northwestern Illinois","docAbstract":"From July 1982 through June 1984, a study was made of the microclimate and evapotranspiration at a low-level radioactive-waste disposal site near Sheffield, Bureau County, Illinois. Vegetation at the site consists of mixed pasture grasses, primarily brome (Bromus inermis) and red clover (Trifoleum pratense). Three methods were used to estimate evapotranspiration: (1) an energy-budget with the Bowen ratio, (2) an aerodynamic-profile, and (3) a soil-based water-budget. For the aerodynamic-profile method, sensible-heat flux was estimated by a profile equation and evapotranspiration was then calculated as the residual in the energy-balance equation. Estimates by the energy-budget and aerodynamic-profile methods were computed from hourly data, then summed by days and months. Yearly estimates for March through November, by these methods, were quite close--648 and 626 millimeters, respectively. Daily estimates range up to a maximum of about 6 millimeters. The water-budget method produced only monthly estimates based on weekly or biweekly soil-moisture content measurements. The yearly evapotranspiration estimated by this method (which actually included only the months of April through October) was 655 millimeters. The March-through-November average for the three methods of 657 millimeters was equivalent to 70 percent of precipitation.\r\nContinuous measurements were made of incoming and reflected shortwave radiation, incoming and emitted longwave radiation, net radiation, soil-heat flux, soil temperature, horizontal windspeed, and wet- and dry-bulb air temperature. Windspeed and air temperature were measured at heights of 0.5 and 2.0 meters (and also at 1.0 meter after September 1983). Soil-moisture content of the soil zone was measured with a gamma-attenuation gage.\r\n\r\nAnnual precipitation (938 millimeters) and average temperature (10.8 degrees Celsius) were virtually identical to long-term averages from nearby National Weather Service stations. Solar radiation averaged 65 percent of that normally expected under clear skies. Net radiation averaged 70.1 watts per square meter and was highest in July and negative during some winter months. Wind direction varied but was predominately out of the south-southeast. Wind speed at the 2-meter height averaged 3.5 meters per second and was slightly higher in winter months than the rest of the year. The amount of water stored within the soil zone was greatest in early spring and least in late summer.\r\n\r\nSeasonal and diurnal trends in evapotranspiration rates mirrored those in net radiation; July was usually the month with the highest rate. The ratio of sensible- to latent-heat fluxes (commonly called the Bowen ratio) for the 2-year period was 0.38, as averaged from the three methods. Monthly Bowen ratios fluctuated somewhat but averaged about 0.35 for late spring through summer. In fall, the ratio declined to zero or to slightly negative values. When the ratio was negative, the latent-heat flux was slightly greater than the net radiation because of additional energy supplied by the cooling soil and air.\r\n\r\nEvapotranspiration calculated by the three methods averaged 75 percent of potential evapotranspiration, as estimated by the Penman equation. There was no apparent seasonal trend in the relation between actual and potential evapotranspiration rates.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr86301","usgsCitation":"Healy, R.W., DeVries, M., and Sturrock, A., 1987, Evapotranspiration and microclimate at a low-level radioactive-waste disposal site in northwestern Illinois: U.S. Geological Survey Open-File Report 86-301, viii, 88 p., https://doi.org/10.3133/ofr86301.","productDescription":"viii, 88 p.","costCenters":[],"links":[{"id":382927,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0301/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147248,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0301/report-thumb.jpg"}],"country":"United States","state":"Illinois","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -91.01074218749999,\n 40.74725696280421\n ],\n [\n -88.9453125,\n 40.74725696280421\n ],\n [\n -88.9453125,\n 42.58544425738491\n ],\n [\n -91.01074218749999,\n 42.58544425738491\n ],\n [\n -91.01074218749999,\n 40.74725696280421\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9ba5","contributors":{"authors":[{"text":"Healy, R. W.","contributorId":89872,"corporation":false,"usgs":true,"family":"Healy","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":168859,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeVries, M.P.","contributorId":39760,"corporation":false,"usgs":true,"family":"DeVries","given":"M.P.","email":"","affiliations":[],"preferred":false,"id":168858,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sturrock, A.M.","contributorId":25947,"corporation":false,"usgs":true,"family":"Sturrock","given":"A.M.","affiliations":[],"preferred":false,"id":168857,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":26440,"text":"wri874116 - 1987 - Relation of water chemistry of the Edwards aquifer to hydrogeology and land use, San Antonio Region, Texas","interactions":[],"lastModifiedDate":"2016-08-10T11:49:14","indexId":"wri874116","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4116","title":"Relation of water chemistry of the Edwards aquifer to hydrogeology and land use, San Antonio Region, Texas","docAbstract":"

Water-chemistry data from the Edwards aquifer for 1976-85, consisting of nearly 1,500 chemical analyses from 280 wells and 3 springs, were used to statistically evaluate relations among ground-water chemistry, hydrogeology, and land use. Five land uses associated with sampled wells were classified on the basis of published information and field surveys. Four major subareas of the aquifer were defined to reflect the relative susceptibility of ground water to contamination originating from human activities using hydrogeologic and tritium data.

\n

Water from an agricultural area over the unconfined zone of the aquifer had the largest median concentration of nitrite plus nitrate. Large nitrite plus nitrate concentrations were spatially associated with large tritium concentrations and nitrogen isotopic ratios characteristic of streamflow recharge. Detections of fecal-coliform bacteria were associated mainly with water from wells completed in the unconfined zone.

\n

Most of the occurrences of tetrachloroethylene, l,2-(trans)-dichloroethylene, trichlorofluoromethane, 1,1,1-trichloroethane, and 2,4-D in ground water were associated with wells completed in the unconfined zone of the aquifer. Fatty acids detected in water from some wells may commonly be present naturally in ground water.

\n

The percentage of samples in which arsenic, barium, lead, and zinc were detected was similar among subareas; the samples were from the freshwater parts of the aquifer. Large lead and zinc concentrations were associated with volumes of pumpage less than 1,000 gallons.

\n

In general, the quality of ground water in the freshwater parts of the aquifer (north of the \"bad-water\" line) is suitable for all uses including human consumption. Two areas that are exceptions are: (1) Northeast of Garner Field in Uvalde, Texas, where PCE (tetrachloroethylene) has been detected in groundwater samples, and (2) north-central Bexar County near the former West Avenue landfill where PCE and benzene have been detected in ground-water samples. Concentrations of these organic compounds in water from many wells in the two areas exceed the maximum contaminant level for human consumption set by the U.S. Environmental Protection Agency.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri874116","usgsCitation":"Buszka, P.M., 1987, Relation of water chemistry of the Edwards aquifer to hydrogeology and land use, San Antonio Region, Texas: U.S. Geological Survey Water-Resources Investigations Report 87-4116, Report: vi, 100 p.; 16 Plates, https://doi.org/10.3133/wri874116.","productDescription":"Report: vi, 100 p.; 16 Plates","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":55255,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55258,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55259,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55260,"rank":415,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55257,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158130,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4116/report-thumb.jpg"},{"id":110243,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_46783.htm","linkFileType":{"id":5,"text":"html"},"description":"46783"},{"id":55261,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4116/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55245,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55246,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55247,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55248,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55249,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55250,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55251,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55252,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55253,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55254,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55256,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db6349f6","contributors":{"authors":[{"text":"Buszka, Paul M. 0000-0001-8218-826X pmbuszka@usgs.gov","orcid":"https://orcid.org/0000-0001-8218-826X","contributorId":1786,"corporation":false,"usgs":true,"family":"Buszka","given":"Paul","email":"pmbuszka@usgs.gov","middleInitial":"M.","affiliations":[{"id":27231,"text":"Indiana-Kentucky Water Science Center","active":true,"usgs":true},{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":196396,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":41938,"text":"ofr87336 - 1987 - Aeromagnetic map of the Goshute area, northeastern Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"ofr87336","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-336","title":"Aeromagnetic map of the Goshute area, northeastern Nevada","language":"ENGLISH","doi":"10.3133/ofr87336","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1987, Aeromagnetic map of the Goshute area, northeastern Nevada: U.S. Geological Survey Open-File Report 87-336, 1 map :photocopy ;140 x 73 cm., on sheet 150 x 77 cm., https://doi.org/10.3133/ofr87336.","productDescription":"1 map :photocopy ;140 x 73 cm., on sheet 150 x 77 cm.","costCenters":[],"links":[{"id":172748,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":21241,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0336/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db694084","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":530718,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":65745,"text":"i1865 - 1987 - Mineral resource assessment of the Republic of Costa Rica","interactions":[],"lastModifiedDate":"2012-02-10T00:11:02","indexId":"i1865","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"1865","subseriesTitle":"NONE","title":"Mineral resource assessment of the Republic of Costa Rica","language":"ENGLISH","doi":"10.3133/i1865","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1987, Mineral resource assessment of the Republic of Costa Rica: U.S. Geological Survey IMAP 1865, 1 atlas (75 p.) :ill. (chiefly col.), col. maps ;82 cm., https://doi.org/10.3133/i1865.","productDescription":"1 atlas (75 p.) :ill. (chiefly col.), col. maps ;82 cm.","costCenters":[],"links":[{"id":251397,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1865/report.pdf","size":"258080","linkFileType":{"id":1,"text":"pdf"}},{"id":252253,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1865/report-thumb.jpg"}],"scale":"500000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -86,8 ], [ -86,11.25 ], [ -82.5,11.25 ], [ -82.5,8 ], [ -86,8 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c238","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":534108,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":42384,"text":"ofr87114 - 1987 - Selected ground-water data in the upper Mongaup River basin, Sullivan County, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:05:04","indexId":"ofr87114","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-114","title":"Selected ground-water data in the upper Mongaup River basin, Sullivan County, New York","docAbstract":"A set of four adjoining 7.5-minute quadrangle sheets that together depict the upper Mongaup River Basin in Sullivan County , N.Y., at 1:24,000 scale show the location, well yield, depth, water use, ownership, and date of ownership of wells, test holes , and springs. Most wells that tap stratified-drift deposits have high yields (50 to 300 gal/min) and are used for public supply. Bedrock wells have smaller yields and are generally used for domestic supply. The data were compiled from a previous U.S. Geological Survey, countywide, groundwater resources report and from unpublished data. (USGS)","language":"ENGLISH","doi":"10.3133/ofr87114","usgsCitation":"Wolcott, S.W., 1987, Selected ground-water data in the upper Mongaup River basin, Sullivan County, New York: U.S. Geological Survey Open-File Report 87-114, 4 maps ;58 x 44 cm., on sheet 69 x 48 cm., folded in envelope 34 x 25 cm., https://doi.org/10.3133/ofr87114.","productDescription":"4 maps ;58 x 44 cm., on sheet 69 x 48 cm., folded in envelope 34 x 25 cm.","costCenters":[],"links":[{"id":136518,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":80149,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0114/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80150,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0114/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80151,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0114/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80152,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0114/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f96da","contributors":{"authors":[{"text":"Wolcott, Stephen W.","contributorId":93458,"corporation":false,"usgs":true,"family":"Wolcott","given":"Stephen","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":226379,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":14118,"text":"ofr87247 - 1987 - National and regional trends in water-well drilling in the United States, 1964-84","interactions":[],"lastModifiedDate":"2019-11-27T10:19:05","indexId":"ofr87247","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-247","title":"National and regional trends in water-well drilling in the United States, 1964-84","docAbstract":"

Information on national and regional water well drilling activity is important for water resource planning and management and for water related equipment marketing. A study was conducted to analyze drilling trends on the basis of data for selected years from 1964 through 1984. The study focused primarily on the years 1964 and 1980-84, but also included data from 1960. Approximately 397,000 water wells were drilled in the United States in 1984. Seven states--Florida, Texas, New York, Michigan, North Carolina, Virginia, and Ohio--accounted for 39% of all the wells drilled in the United States in 1984. Florida led the nation in drilling activity with 45,600 new wells. The 1984 national drilling total was 2.6% > the total for 1980 (387,000) and 8.5% < the total for 1964 (434,000). However, these moderate differences do not reflect substantial year-to-year fluctuations that may have occurred during that 20-yr period. Qualitative comparisons suggest that drilling activity for a given year is closely related to the number of housing starts for that year. If so, there may have been peaks in drilling activity in 1972 and 1977-78 (corresponding to peaks in housing starts) that are not identified in this study because of a lack of available well drilling data for those years. Well drilling data for 1964 and the 1980-84 period probably represent a low to moderate level of drilling activity, and, if compared to earlier data, suggest that there has been no substantial growth or decline in the water well industry as a whole since the 1940's. (Author's abstract)

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr87247","usgsCitation":"Hindall, S.M., and Eberle, M., 1987, National and regional trends in water-well drilling in the United States, 1964-84: U.S. Geological Survey Open-File Report 87-247, iv, 25 p. , https://doi.org/10.3133/ofr87247.","productDescription":"iv, 25 p. 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]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698401","contributors":{"authors":[{"text":"Hindall, S. M.","contributorId":59414,"corporation":false,"usgs":true,"family":"Hindall","given":"S.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":168951,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eberle, Michael","contributorId":39770,"corporation":false,"usgs":true,"family":"Eberle","given":"Michael","email":"","affiliations":[],"preferred":false,"id":168950,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":26757,"text":"wri874084 - 1987 - Movement of ground water in coal-bearing rocks near Fishtrap Lake in Pike County, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:08:33","indexId":"wri874084","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4084","title":"Movement of ground water in coal-bearing rocks near Fishtrap Lake in Pike County, Kentucky","docAbstract":"Eight test holes were core-drilled from various altitudes in a typical coal-bearing sequence rocks of Pennsylvania age in Pike County, eastern Kentucky. Vertical fractures were common in cores from shallow depths, but became less common or absent toward the bottom of two test holes drilled 400 and 291 ft deep. Most fractures readily injected water, and near the bottoms of the two deep holes, coal beds accepted water in the non-fractured rocks. Rhodamin-WT dye was injected in a 61-ft deep ridge-top well on October 24, 1985 and was detected in varying concentrations in water samples taken from all down-gradient piezometers at the study site on November 7, 1985. The presence of dye in down-gradient piezometers indicated that groundwater in the Eastern Kentucky coal field can move from areas of higher head to areas of lower head. The movement probably occurs in a stair-step fashion through a complex system of near-vertical fractures, and laterally through permeable rocks, which probably are the coal beds. This suggests that land uses on ridges could affect the quality of water from wells or springs at lower altitudes on hillsides or in the valley bottoms even though separated by a thick interval of rocks that include beds of low primary permeability. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874084","usgsCitation":"Davis, R.W., 1987, Movement of ground water in coal-bearing rocks near Fishtrap Lake in Pike County, Kentucky: U.S. Geological Survey Water-Resources Investigations Report 87-4084, iv, 24 p. :ill. ;28 cm., https://doi.org/10.3133/wri874084.","productDescription":"iv, 24 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":126418,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4084/report-thumb.jpg"},{"id":55647,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4084/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db641027","contributors":{"authors":[{"text":"Davis, R. W.","contributorId":93459,"corporation":false,"usgs":true,"family":"Davis","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":196949,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26446,"text":"wri834127 - 1987 - Pesticide data for selected Wyoming streams, 1976-78","interactions":[],"lastModifiedDate":"2017-01-09T10:55:12","indexId":"wri834127","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4127","title":"Pesticide data for selected Wyoming streams, 1976-78","docAbstract":"

In 1976, the U.S. Geological Survey, in cooperation with the Wyoming Department of Agriculture, started a monitoring program to determine pesticide concentrations in Wyoming streams. This program was incorporated into the water-quality data-collection system already in operation. Samples were collected at 20 sites for analysis of various insecticides, herbicides, polychlorinated biphenyls, and polychlorinated napthalenes.\\

The results through 1978 revealed small concentrations of pesticides in water and bottom-material samples were DDE (39 percent of the concentrations equal to or greater than the minimum reported concentrations of the analytical methods), DDD (20 percent), dieldrin (21 percent), and polychlorinated biphenyls (29 percent). The herbicides most commonly found in water samples were 2,4-D (29 percent of the concentrations equal to or greater than the minimum reported concentrations of the analytical method) and picloram (23 percent). Most concentrations were significantly less than concentrations thought to be harmful to freshwater aquatic life based on available toxicity data. However for some pesticides, U.S. Environmental Protection Agency water-quality criteria for freshwater aquatic life are based on bioaccumulation factors that result in criteria concentrations less than the minimum reported concentrations of the analytical methods. It is not known if certain pesticides were present at concentrations less than the minimum reported concentrations that exceeded these criteria.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Cheyenne, WY","doi":"10.3133/wri834127","collaboration":"Prepared in cooperation with the Wyoming Department of Agriculture","usgsCitation":"Butler, D.L., 1987, Pesticide data for selected Wyoming streams, 1976-78: U.S. Geological Survey Water-Resources Investigations Report 83-4127, v, 41 p., https://doi.org/10.3133/wri834127.","productDescription":"v, 41 p.","numberOfPages":"46","costCenters":[],"links":[{"id":122841,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4127/report-thumb.jpg"},{"id":55269,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4127/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wyoming","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688398","contributors":{"authors":[{"text":"Butler, David L.","contributorId":12843,"corporation":false,"usgs":true,"family":"Butler","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":196404,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26824,"text":"wri864173 - 1987 - Geohydrologic reconnaissance of a ground-water contamination problem in the Argonne Road area near Spokane, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:30","indexId":"wri864173","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"86-4173","title":"Geohydrologic reconnaissance of a ground-water contamination problem in the Argonne Road area near Spokane, Washington","docAbstract":"Three domestic wells that withdraw groundwater from an alluvium-filled trough cut into granite were found to be contaminated with the organic solvents tetrachloroethene, trichloroethene, 1,1,1-trichloroethane, and 1 ,2-trans-dichloroethene. The suspected source of contamination is a nearby septic-tank sludge disposal area. There is concern that the affected aquifer is tributary to the Spokane aquifer, which has been accorded ' sole source ' status by the U.S. Environmental Protection Agency. Preliminary estimates suggest that groundwater in the area is moving toward the Spokane aquifer and that the transit time may range from 2.5 to 25 years. Because of longitudinal dispersion, however, the plume of contaminants may move at a faster rate than the ambient groundwater and may arrive at given destinations more quickly than calculated above. A literature search has indicated that the dissolved solute phase of the contaminants will not be significantly affected by sorption, volatilization, chemical activity, or biodegradation. Because of the preliminary nature of the investigation, many questions relating to the extent of contamination remain unanswered. A list of suggested additional studies to answer those questions and to refine and confirm the findings of this investigation is presented. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864173","usgsCitation":"Dion, N.P., 1987, Geohydrologic reconnaissance of a ground-water contamination problem in the Argonne Road area near Spokane, Washington: U.S. Geological Survey Water-Resources Investigations Report 86-4173, v, 37 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri864173.","productDescription":"v, 37 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124095,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4173/report-thumb.jpg"},{"id":55705,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4173/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8e23","contributors":{"authors":[{"text":"Dion, N. P.","contributorId":33302,"corporation":false,"usgs":true,"family":"Dion","given":"N.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":197069,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29118,"text":"wri864016 - 1987 - Water quality of Fremont Lake and New Fork Lakes, western Wyoming: A progress report","interactions":[],"lastModifiedDate":"2022-12-19T20:09:14.384152","indexId":"wri864016","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"86-4016","title":"Water quality of Fremont Lake and New Fork Lakes, western Wyoming: A progress report","docAbstract":"

Fremont Lake and New Fork Lakes in the New Fork River drainage of western Wyoming were selected for a comprehensive study of hydrologic processes affecting mountain lakes in the Rocky Mountains. Information is needed about lakes in this area to assess their response to existing and planned development. The concerns include regional issues such as acid precipitation from gas-sweetening plants, coal-fired powerplants, and smelters, as well as local issues, such as shoreline development and raising outlet control structures. Onsite measurements indicated strong thermal stratification in the lakes during the summer. Isothermal conditions occurred during December 1983 and May 1984. Mean phytoplankton concentrations were less than 5,000 cells/ml, and chlorophyll a concentrations were weakly correlated with phytoplankton concentrations. Zooplankton concentrations were small, less than 6 organisms/L. The numbers of benthic invertebrates/unit area in Fremont Lake were extremely small. The lake waters and inflow and outflow streams were chemically dilute solutions. Mean dissolved-solids concentrations were 13 mg/L in Fremont Lake and 24 mg/L in New Fork Lakes. Calcium and bicarbonate were the predominant ions. Concentrations of phosphorus and nitrogen usually were less than detection limits. Trace-metals concentrations in the lakes were similar to those in precipitation and generally were small. Dissolved organic-carbon concentrations were about 1 mg/L. Concentrations of fulvic and humic acids were relatively large in the inlet of Fremont Lake during the spring. Pine Creek has deposited 800 metric tons of sediment, on an annual average, to the delta of Fremont Lake. Most sediment is deposited during spring runoff.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864016","usgsCitation":"Peterson, D.A., Averett, R., and Mora, K.L., 1987, Water quality of Fremont Lake and New Fork Lakes, western Wyoming: A progress report: U.S. Geological Survey Water-Resources Investigations Report 86-4016, vi, 55 p., https://doi.org/10.3133/wri864016.","productDescription":"vi, 55 p.","costCenters":[],"links":[{"id":410729,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36486.htm","linkFileType":{"id":5,"text":"html"}},{"id":57988,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4016/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159526,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4016/report-thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Fremont Lake and New Fork Lakes","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -109.75,\n 43.117\n ],\n [\n -110,\n 43.117\n ],\n [\n -110,\n 42.875\n ],\n [\n -109.75,\n 42.875\n ],\n [\n -109.75,\n 43.117\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a02e4b07f02db5f8110","contributors":{"authors":[{"text":"Peterson, D. 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L.","contributorId":55008,"corporation":false,"usgs":true,"family":"Mora","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":200975,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":20113,"text":"ofr87404 - 1987 - Sedimentary basin models documented on computer diskettes for USGS bulletin 1810 the muPETROL expert system for classifying world sedimentary basins","interactions":[],"lastModifiedDate":"2012-02-02T00:07:37","indexId":"ofr87404","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-404","title":"Sedimentary basin models documented on computer diskettes for USGS bulletin 1810 the muPETROL expert system for classifying world sedimentary basins","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87404","usgsCitation":"Miller, B., 1987, Sedimentary basin models documented on computer diskettes for USGS bulletin 1810 the muPETROL expert system for classifying world sedimentary basins: U.S. Geological Survey Open-File Report 87-404, 5 p. ;28 cm., https://doi.org/10.3133/ofr87404.","productDescription":"5 p. ;28 cm.","costCenters":[],"links":[{"id":152269,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0404/report-thumb.jpg"},{"id":49657,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0404/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd71dfe4b0b29085107f3b","contributors":{"authors":[{"text":"Miller, B.M.","contributorId":73232,"corporation":false,"usgs":true,"family":"Miller","given":"B.M.","email":"","affiliations":[],"preferred":false,"id":182088,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":65323,"text":"i1869 - 1987 - Controlled photomosaic of part of the Kasei Valles Region of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:20","indexId":"i1869","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"1869","subseriesTitle":"NONE","title":"Controlled photomosaic of part of the Kasei Valles Region of Mars","language":"ENGLISH","doi":"10.3133/i1869","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1987, Controlled photomosaic of part of the Kasei Valles Region of Mars: U.S. Geological Survey IMAP 1869, 1 remote-sensing image ;61 x 57 cm., on sheet 96 x 65 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1869.","productDescription":"1 remote-sensing image ;61 x 57 cm., on sheet 96 x 65 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":189359,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":100893,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1869/plate-1.pdf","size":"7858","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a81d","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":533710,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26448,"text":"wri874026 - 1987 - Sediment discharge in Rock Creek and the effect of sedimentation rate on the proposed Rock Creek Reservoir, northwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:27","indexId":"wri874026","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4026","title":"Sediment discharge in Rock Creek and the effect of sedimentation rate on the proposed Rock Creek Reservoir, northwestern Colorado","docAbstract":"Sediment data collected from 1976 to 1985 and stream discharge data collected from 1952 to 1980 at gaging station 09060500, Rock Creek near Toponas, Colorado, were used to determine total sediment discharge into the proposed Rock Creek Reservoir. Suspended sediment discharge and bedload discharge were related to stream discharge by using logarithmic regression relations. Mean annual suspended sediment discharge was estimated to be 309 tons/yr, and mean annual bedload discharge was estimated to be 428 tons/yr in Rock Creek at the Toponas gaging station for the 1953 through 1980 water years. The mean annual total sediment discharge into the proposed reservoir was estimated to be 768 tons/yr, which includes 10% addition to the suspended sediment discharge calculated for the Toponas gaging station to account for suspended sediment discharge from Horse Creek. This rate of mean annual total sediment discharge would decrease the long-term water storage capacity of the proposed reservoir by < 1% after 100 years. Suspended sediment discharge/unit-drainage-basin area at gaging station 09060550, Rock Creek at Crater, located about 5 mi downstream for the proposed reservoir site, was equivalent to suspended-sediment discharge/unit-drainage-basin area at the Toponas gaging station during 1985. Long-term sediment data collection at the Crater gaging station could be used for detecting changes in suspended sediment discharge in Rock Creek at the proposed reservoir site. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874026","usgsCitation":"Butler, D.L., 1987, Sediment discharge in Rock Creek and the effect of sedimentation rate on the proposed Rock Creek Reservoir, northwestern Colorado: U.S. Geological Survey Water-Resources Investigations Report 87-4026, iv, 23 p. :ill., map ;28 cm., https://doi.org/10.3133/wri874026.","productDescription":"iv, 23 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":157897,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4026/report-thumb.jpg"},{"id":55271,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4026/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fc037","contributors":{"authors":[{"text":"Butler, D. L.","contributorId":36967,"corporation":false,"usgs":true,"family":"Butler","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":196408,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29121,"text":"wri864199 - 1987 - Description and comparison of selected models for hydrologic analysis of ground-water flow, St. Joseph River basin, Indiana","interactions":[],"lastModifiedDate":"2022-01-31T19:42:22.790964","indexId":"wri864199","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"86-4199","title":"Description and comparison of selected models for hydrologic analysis of ground-water flow, St. Joseph River basin, Indiana","docAbstract":"

The Indiana Department of Natural Resources (IDNR) is developing water-management policies designed to assess the effects of irrigation and other water uses on water supply in the basin. In support of this effort, the USGS, in cooperation with IDNR, began a study to evaluate appropriate methods for analyzing the effects of pumping on ground-water levels and streamflow in the basin 's glacial aquifer systems. Four analytical models describe drawdown for a nonleaky, confined aquifer and fully penetrating well; a leaky, confined aquifer and fully penetrating well; a leaky, confined aquifer and partially penetrating well; and an unconfined aquifer and partially penetrating well. Analytical equations, simplifying assumptions, and methods of application are described for each model. In addition to these four models, several other analytical models were used to predict the effects of ground-water pumping on water levels in the aquifer and on streamflow in local areas with up to two pumping wells. Analytical models for a variety of other hydrogeologic conditions are cited. A digital ground-water flow model was used to describe how a numerical model can be applied to a glacial aquifer system. The numerical model was used to predict the effects of six pumping plans in 46.5 sq mi area with as many as 150 wells. Water budgets for the six pumping plans were used to estimate the effect of pumping on streamflow reduction. Results of the analytical and numerical models indicate that, in general, the glacial aquifers in the basin are highly permeable. Radial hydraulic conductivity calculated by the analytical models ranged from 280 to 600 ft/day, compared to 210 and 360 ft/day used in the numerical model. Maximum seasonal pumping for irrigation produced maximum calculated drawdown of only one-fourth of available drawdown and reduced streamflow by as much as 21%. Analytical models are useful in estimating aquifer properties and predicting local effects of pumping in areas with simple lithology and boundary conditions and with few pumping wells. Numerical models are useful in regional areas with complex hydrogeology with many pumping wells and provide detailed water budgets useful for estimating the sources of water in pumping simulations. Numerical models are useful in constructing flow nets. The choice of which type of model to use is also based on the nature and scope of questions to be answered and on the degree of accuracy required.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/wri864199","collaboration":"Indiana Department of Natural Resources","usgsCitation":"Peters, J.G., 1987, Description and comparison of selected models for hydrologic analysis of ground-water flow, St. Joseph River basin, Indiana: U.S. Geological Survey Water-Resources Investigations Report 86-4199, xii, 125 p., https://doi.org/10.3133/wri864199.","productDescription":"xii, 125 p.","numberOfPages":"138","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":395170,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36620.htm"},{"id":126646,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4199/report-thumb.jpg"},{"id":57991,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4199/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Indiana, Michigan","county":"Elkhart, Kosciusko, Lagrange, Noble, Saint Joseph, Steuben, Berrien, Branch, Calhoun, cass, Hillsdale, Kalamazoo, Saint Joseph, Van Buren,","otherGeospatial":"Saint Jospeh River Basin","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-85.7663,42.4196],[-85.5421,42.4195],[-85.5328,42.4194],[-85.4172,42.4199],[-85.3091,42.4185],[-85.2979,42.4188],[-85.0736,42.4211],[-85.0667,42.4215],[-84.9561,42.4221],[-84.8375,42.4215],[-84.83,42.421],[-84.7207,42.4209],[-84.7195,42.2464],[-84.7144,42.1586],[-84.7116,42.0709],[-84.5948,42.0715],[-84.3666,42.0734],[-84.3623,41.7082],[-84.3989,41.7074],[-84.4979,41.705],[-84.6319,41.7018],[-84.6756,41.7007],[-84.8067,41.6958],[-84.8064,41.5598],[-84.8063,41.5303],[-84.8554,41.53],[-84.969,41.5287],[-85.0819,41.5282],[-85.1947,41.5276],[-85.1939,41.4395],[-85.1943,41.3519],[-85.1935,41.2643],[-85.309,41.265],[-85.3096,41.265],[-85.4245,41.2655],[-85.5387,41.2664],[-85.5384,41.295],[-85.6527,41.2949],[-85.6518,41.2668],[-85.6522,41.1787],[-85.6876,41.179],[-85.6856,41.0896],[-85.6849,41.0465],[-85.9457,41.0424],[-86.017,41.0414],[-86.0179,41.0863],[-86.0758,41.0851],[-86.0777,41.1736],[-86.0539,41.1735],[-86.0574,41.3033],[-86.059,41.4336],[-86.059,41.4367],[-86.0594,41.4644],[-86.0593,41.474],[-86.0593,41.479],[-86.0789,41.479],[-86.0979,41.4791],[-86.1181,41.4792],[-86.1273,41.4792],[-86.1421,41.4792],[-86.1562,41.4793],[-86.234,41.479],[-86.3063,41.4787],[-86.3302,41.4778],[-86.3492,41.4778],[-86.378,41.4774],[-86.4356,41.4765],[-86.4559,41.4765],[-86.4645,41.4765],[-86.4669,41.4765],[-86.4669,41.4616],[-86.4669,41.4339],[-86.5245,41.4339],[-86.5245,41.5201],[-86.5012,41.5206],[-86.5,41.5287],[-86.4982,41.531],[-86.4982,41.5669],[-86.4865,41.5769],[-86.4871,41.649],[-86.5068,41.6499],[-86.5264,41.6499],[-86.5264,41.6572],[-86.5258,41.6731],[-86.5252,41.7085],[-86.524,41.7603],[-86.5284,41.7603],[-86.6391,41.7606],[-86.7387,41.7608],[-86.7677,41.7608],[-86.7814,41.7609],[-86.8262,41.7609],[-86.8182,41.7641],[-86.7758,41.7864],[-86.7482,41.8037],[-86.7285,41.8147],[-86.7064,41.8265],[-86.6886,41.8402],[-86.6418,41.8761],[-86.6122,41.9006],[-86.6092,41.9029],[-86.5956,41.9202],[-86.5833,41.9374],[-86.5698,41.9647],[-86.5667,41.9711],[-86.5636,41.9829],[-86.563,41.9842],[-86.5402,42.0274],[-86.5136,42.0701],[-86.5112,42.0737],[-86.5025,42.0864],[-86.4895,42.1046],[-86.4883,42.1137],[-86.474,42.1287],[-86.4555,42.1441],[-86.4418,42.1591],[-86.4381,42.1632],[-86.4158,42.1836],[-86.3904,42.2127],[-86.3637,42.2453],[-86.3625,42.2467],[-86.3544,42.2612],[-86.3401,42.2807],[-86.3388,42.2821],[-86.327,42.3034],[-86.3133,42.332],[-86.3039,42.3507],[-86.2877,42.3906],[-86.2814,42.4065],[-86.2745,42.4201],[-86.2248,42.4191],[-85.995,42.4193],[-85.8975,42.4185],[-85.7663,42.4196]]]},\"properties\":{\"name\":\"Elkhart\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d2c4","contributors":{"authors":[{"text":"Peters, J. G.","contributorId":56216,"corporation":false,"usgs":true,"family":"Peters","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":200980,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11833,"text":"ofr87115 - 1987 - Activities of the U.S. Geological Survey, status of Idaho projects, fiscal year 1986","interactions":[],"lastModifiedDate":"2012-02-02T00:06:41","indexId":"ofr87115","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-115","title":"Activities of the U.S. Geological Survey, status of Idaho projects, fiscal year 1986","language":"ENGLISH","publisher":"U.S. Geological Survey, WRD,","doi":"10.3133/ofr87115","usgsCitation":"Channel, L.K., 1987, Activities of the U.S. Geological Survey, status of Idaho projects, fiscal year 1986: U.S. Geological Survey Open-File Report 87-115, ii, 60 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr87115.","productDescription":"ii, 60 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":145779,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0115/report-thumb.jpg"},{"id":39735,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0115/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2c5d","contributors":{"authors":[{"text":"Channel, L. 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The major aquifers in the study area are the Nanafalia, Eutaw, Gordo, and Coker aquifers of Tertiary and Cretaceous age. The recharge areas for one or more of these aquifers are in each of the five counties. East aquifer is a source of public water supply in one or more of the five counties. All recharge areas for the major aquifers are susceptible to contamination from the surface. However, large parts of the recharge areas are in rural settings that are used for timberlands, farms, and pastures, and are several miles from pumping centers; therefore, these areas are not highly susceptible to contamination. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874113","usgsCitation":"DeJarnette, S., and Crownover, J., 1987, Geohydrology and susceptibility of major aquifers to surface contamination in Alabama; area 6: U.S. Geological Survey Water-Resources Investigations Report 87-4113, v, 27 p. :ill. 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