{"pageNumber":"4004","pageRowStart":"100075","pageSize":"25","recordCount":184938,"records":[{"id":44723,"text":"wri944048 - 1994 - Potentiometric-surface map of the Sparta aquifer in Mississippi, October through December 1989","interactions":[],"lastModifiedDate":"2019-08-21T11:24:48","indexId":"wri944048","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-4048","title":"Potentiometric-surface map of the Sparta aquifer in Mississippi, October through December 1989","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri944048","usgsCitation":"Oakley, W.T., and Burt, D.E., 1994, Potentiometric-surface map of the Sparta aquifer in Mississippi, October through December 1989: U.S. Geological Survey Water-Resources Investigations Report 94-4048, 1 Plate: 37.87 x 36.93 inches, https://doi.org/10.3133/wri944048.","productDescription":"1 Plate: 37.87 x 36.93 inches","costCenters":[],"links":[{"id":366788,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4048/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162872,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4048/report-thumb.jpg"}],"country":"United States","state":"Mississippi","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db681e62","contributors":{"authors":[{"text":"Oakley, William T.","contributorId":70815,"corporation":false,"usgs":true,"family":"Oakley","given":"William","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":230321,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burt, David E. Jr.","contributorId":31443,"corporation":false,"usgs":true,"family":"Burt","given":"David","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":230320,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28995,"text":"wri934214 - 1994 - Application of borehole geophysics in the characterization of flow in fractured rocks","interactions":[],"lastModifiedDate":"2020-04-12T14:40:00.241029","indexId":"wri934214","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"93-4214","title":"Application of borehole geophysics in the characterization of flow in fractured rocks","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri934214","usgsCitation":"Paillet, F.L., 1994, Application of borehole geophysics in the characterization of flow in fractured rocks: U.S. Geological Survey Water-Resources Investigations Report 93-4214, iv, 36 p., https://doi.org/10.3133/wri934214.","productDescription":"iv, 36 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":57862,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4214/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118908,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4214/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67aae7","contributors":{"authors":[{"text":"Paillet, Frederick L.","contributorId":63820,"corporation":false,"usgs":true,"family":"Paillet","given":"Frederick","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":200753,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29229,"text":"wri944001 - 1994 - Nonpoint and Point Sources of Nitrogen in Major Watersheds of the United States","interactions":[],"lastModifiedDate":"2012-02-02T00:08:48","indexId":"wri944001","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-4001","title":"Nonpoint and Point Sources of Nitrogen in Major Watersheds of the United States","docAbstract":"Estimates of nonpoint and point sources of nitrogen were made for 107 watersheds located in the U.S. Geological Survey's National Water-Quality Assessment Program study units throughout the conterminous United States. The proportions of nitrogen originating from fertilizer, manure, atmospheric deposition, sewage, and industrial sources were found to vary with climate, hydrologic conditions, land use, population, and physiography. Fertilizer sources of nitrogen are proportionally greater in agricultural areas of the West and the Midwest than in other parts of the Nation. Animal manure contributes large proportions of nitrogen in the South and parts of the Northeast. Atmospheric deposition of nitrogen is generally greatest in areas of greatest precipitation, such as the Northeast. Point sources (sewage and industrial) generally are predominant in watersheds near cities, where they may account for large proportions of the nitrogen in streams. The transport of nitrogen in streams increases as amounts of precipitation and runoff increase and is greatest in the Northeastern United States. Because no single nonpoint nitrogen source is dominant everywhere, approaches to control nitrogen must vary throughout the Nation. Watershed-based approaches to understanding nonpoint and point sources of contamination, as used by the National Water-Quality Assessment Program, will aid water-quality and environmental managers to devise methods to reduce nitrogen pollution.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/wri944001","usgsCitation":"Puckett, L., 1994, Nonpoint and Point Sources of Nitrogen in Major Watersheds of the United States (Revised Mar 1994): U.S. Geological Survey Water-Resources Investigations Report 94-4001, iii, 9 p., https://doi.org/10.3133/wri944001.","productDescription":"iii, 9 p.","costCenters":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"links":[{"id":126693,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4001/report-thumb.jpg"},{"id":11654,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri944001/","linkFileType":{"id":5,"text":"html"}},{"id":58089,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4001/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Revised Mar 1994","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691aed","contributors":{"authors":[{"text":"Puckett, Larry J. lpuckett@usgs.gov","contributorId":31739,"corporation":false,"usgs":true,"family":"Puckett","given":"Larry J.","email":"lpuckett@usgs.gov","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":false,"id":201183,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70187227,"text":"70187227 - 1994 - Precambrian zircons from the Florida basement: A Gondwanan connection","interactions":[],"lastModifiedDate":"2024-01-21T22:46:25.83814","indexId":"70187227","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Precambrian zircons from the Florida basement: A Gondwanan connection","docAbstract":"<div id=\"15575728\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>A Gondwanan origin for the pre-Cretaceous basement of Florida is suggested by U- Pb ages of 515 to 2860 Ma for single zircons separated from subsurface samples of lower Paleozoic sandstone of the Suwannee basin (Alachua County, Florida) and Neoproterozoic Osceola granite (Osceola County, Florida). Forty individual grains analyzed by SHRIMP ion microprobe yielded ages from 515 to 2860 Ma; ages &gt;1000 Ma were predominantly concordant. Two principal populations are evident: (1) 515 to 637 Ma (avg. = 574 Ma;<span>&nbsp;</span><sup>206</sup>Pb/<sup>238</sup>U ages) and (2) 1967 to 2282 Ma (avg. = 2130 Ma;<span>&nbsp;</span><sup>207</sup>Pb/<sup>206</sup>Pb ages). Only six zircons were recovered from the granite; four are Pan-African and two are Archean. For the sandstone, the similarity between the Sm-Nd model age (1245 Ma) and the average of the single zircon ages (1326 Ma) suggests that these zircons are chronologically representative of the aggregate provenance of the sandstone. The two dominant zircon age groupings correspond chronologically to the Pan-African and Birimian or Eburnian (Africa) and to the Brasiliano and Trans-Amazonian (South America) orogenic cycles. The presence of detritus from rocks of these two orogenic cycles clearly places the basement of Florida in Gondwanaland proximal to the West African and/or Trans-Amazonian-San Luis cratons in the early Paleozoic, a location it probably shared with other circum-Atlantic exotic terranes (Avalonian, Cadomian, and/or Carolina).</p></div>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1994)022<0119:PZFTFB>2.3.CO;2","usgsCitation":"Mueller, P.A., Heatherington, A.L., Wooden, J., Shuster, R.D., Nutman, A.P., and Williams, I.S., 1994, Precambrian zircons from the Florida basement: A Gondwanan connection: Geology, v. 22, no. 2, p. 119-122, https://doi.org/10.1130/0091-7613(1994)022<0119:PZFTFB>2.3.CO;2.","productDescription":"4 p.","startPage":"119","endPage":"122","costCenters":[],"links":[{"id":340489,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5901b1c2e4b0c2e071a99bca","contributors":{"authors":[{"text":"Mueller, Paul A.","contributorId":191457,"corporation":false,"usgs":false,"family":"Mueller","given":"Paul","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":693084,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Heatherington, Ann L.","contributorId":191458,"corporation":false,"usgs":false,"family":"Heatherington","given":"Ann","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":693085,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wooden, Joseph L.","contributorId":32209,"corporation":false,"usgs":true,"family":"Wooden","given":"Joseph L.","affiliations":[],"preferred":false,"id":693086,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Shuster, Robert D.","contributorId":191459,"corporation":false,"usgs":false,"family":"Shuster","given":"Robert","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":693087,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Nutman, Allen P.","contributorId":191460,"corporation":false,"usgs":false,"family":"Nutman","given":"Allen","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":693088,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Williams, Ian S.","contributorId":77439,"corporation":false,"usgs":true,"family":"Williams","given":"Ian","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":693089,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":21293,"text":"ofr94278 - 1994 - A dislocation model of the 1994 Northridge, California, earthquake determined from strong ground motions","interactions":[],"lastModifiedDate":"2012-02-02T00:07:59","indexId":"ofr94278","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-278","title":"A dislocation model of the 1994 Northridge, California, earthquake determined from strong ground motions","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr94278","usgsCitation":"Wald, D., and Heaton, T.H., 1994, A dislocation model of the 1994 Northridge, California, earthquake determined from strong ground motions: U.S. Geological Survey Open-File Report 94-278, 53 p. :ill. ;28 cm., https://doi.org/10.3133/ofr94278.","productDescription":"53 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":155304,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0278/report-thumb.jpg"},{"id":50844,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0278/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aed0c","contributors":{"authors":[{"text":"Wald, D.J. 0000-0002-1454-4514","orcid":"https://orcid.org/0000-0002-1454-4514","contributorId":43809,"corporation":false,"usgs":true,"family":"Wald","given":"D.J.","affiliations":[],"preferred":false,"id":184159,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Heaton, T. H.","contributorId":64671,"corporation":false,"usgs":false,"family":"Heaton","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":184160,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44330,"text":"ofr94204 - 1994 - Geologic map of the La Barge Quadrangle, Lincoln and Sublette counties, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:11:01","indexId":"ofr94204","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-204","title":"Geologic map of the La Barge Quadrangle, Lincoln and Sublette counties, Wyoming","language":"ENGLISH","doi":"10.3133/ofr94204","usgsCitation":"Rioux, R., 1994, Geologic map of the La Barge Quadrangle, Lincoln and Sublette counties, Wyoming: U.S. Geological Survey Open-File Report 94-204, 1 map : col. ; 58 x 43 cm., on sheet 74 x 75 cm., https://doi.org/10.3133/ofr94204.","productDescription":"1 map : col. ; 58 x 43 cm., on sheet 74 x 75 cm.","costCenters":[],"links":[{"id":108218,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12475.htm","linkFileType":{"id":5,"text":"html"},"description":"12475"},{"id":168822,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":21560,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0204/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db697158","contributors":{"authors":[{"text":"Rioux, R.L.","contributorId":36541,"corporation":false,"usgs":true,"family":"Rioux","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":229576,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70017753,"text":"70017753 - 1994 - Flood monitoring network in southeastern Louisiana","interactions":[],"lastModifiedDate":"2012-03-12T17:19:20","indexId":"70017753","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Flood monitoring network in southeastern Louisiana","docAbstract":"A flood monitoring network has been established to alert emergency operations personnel and the public about hydrologic conditions in the Amite River Basin. The U.S. Geological Survey (USGS), in cooperation with the Louisiana Office of Emergency Preparedness (LOEP), has installed a real-time data acquisition system to monitor rainfall and river stages in the basin. These data will be transmitted for use by emergency operations personnel to develop flood control and evacuation strategies. The current river stages at selected gaging stations in the basin also will be broadcast by local television and radio stations during a flood. Residents can record the changing river stages on a basin monitoring map, similar to a hurricane tracking map.","largerWorkTitle":"Proceedings - National Conference on Hydraulic Engineering","conferenceTitle":"Proceedings of the 1994 ASCE National Conference on Hydraulic Engineering","conferenceDate":"1 August 1994 through 5 August 1994","conferenceLocation":"Buffalo, NY, USA","language":"English","publisher":"Publ by ASCE","publisherLocation":"New York, NY, United States","issn":"10701559","isbn":"0784400377","usgsCitation":"McCallum, B.E., 1994, Flood monitoring network in southeastern Louisiana, <i>in</i> Proceedings - National Conference on Hydraulic Engineering, no. pt 1, Buffalo, NY, USA, 1 August 1994 through 5 August 1994, p. 346-350.","startPage":"346","endPage":"350","numberOfPages":"5","costCenters":[],"links":[{"id":228395,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"pt 1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a10fbe4b0c8380cd53ea1","contributors":{"authors":[{"text":"McCallum, Brian E. 0000-0002-8935-0343 bemccall@usgs.gov","orcid":"https://orcid.org/0000-0002-8935-0343","contributorId":1591,"corporation":false,"usgs":true,"family":"McCallum","given":"Brian","email":"bemccall@usgs.gov","middleInitial":"E.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":377467,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70017719,"text":"70017719 - 1994 - Rhenium and osmium isotopes in black shales and Ni-Mo-PGE-rich sulfide layers, Yukon Territory, Canada, and Hunan and Guizhou provinces, China","interactions":[],"lastModifiedDate":"2023-12-21T00:57:20.871686","indexId":"70017719","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Rhenium and osmium isotopes in black shales and Ni-Mo-PGE-rich sulfide layers, Yukon Territory, Canada, and Hunan and Guizhou provinces, China","docAbstract":"<p>Rhenium and osmium abundances and osmium isotopic compositions were determined by negative thermal ionization mass spectrometry for samples of Devonian black shale and an associated Ni-enriched sulfide layer from the Yukon Territory, Canada. The same composition information was also obtained for samples of early Cambrian Ni-Mo-rich sulfide layers hosted in black shale in Guizhou and Hunan provinces, China. This study was undertaken to constrain the origin of the PGE enrichment in the sulfide layers.</p><p>Samples of the Ni sulfide layer from the Yukon Territory are highly enriched in Re, Os, and other PGE, with distinctly higher Re/<sup>192</sup>Os but similar Pt/Re, compared to the black shale host. Re-Os isotopic data of the black shale and the sulfide layer are approximately isochronous, and the data plot close to reference isochrons which bracket the depositional age of the enclosing shales. Samples of the Chinese sulfide layers are also highly enriched in Re, Os, and the other PGE. Re/<sup>192</sup>Os are lower than in the Yukon sulfide layer. Re-Os isotopic data for the sulfide layers lie near a reference isochron with an age of 560 Ma, similar to the depositional age of the black shale host. The osmium isotopic data suggest that Re and PGE enrichment of the brecciated sulfide layers in both the Yukon Territory and in southern China may have occurred near the time of sediment deposition or during early diagenesis, during the middle to late Devonian and early Cambrian, respectively.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(94)90463-4","issn":"00167037","usgsCitation":"Horan, M., Morgan, J.W., Grauch, R., Coveney, R., Murowchick, J., and Hulbert, L., 1994, Rhenium and osmium isotopes in black shales and Ni-Mo-PGE-rich sulfide layers, Yukon Territory, Canada, and Hunan and Guizhou provinces, China: Geochimica et Cosmochimica Acta, v. 58, no. 1, p. 257-265, https://doi.org/10.1016/0016-7037(94)90463-4.","productDescription":"9 p.","startPage":"257","endPage":"265","costCenters":[],"links":[{"id":228623,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, China","state":"Guizhou Province, Hunan Province, Yukon Territory","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -137.9354079894031,\n              65.82002289302704\n            ],\n            [\n              -137.9354079894031,\n              64.5420143704358\n            ],\n            [\n              -134.66809723404737,\n              64.5420143704358\n            ],\n            [\n              -134.66809723404737,\n              65.82002289302704\n            ],\n            [\n              -137.9354079894031,\n              65.82002289302704\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              106.35939307834292,\n              28.098681827718266\n            ],\n            [\n              106.35939307834292,\n              27.57651869998071\n            ],\n            [\n              107.08654010288109,\n              27.57651869998071\n            ],\n            [\n              107.08654010288109,\n              28.098681827718266\n            ],\n            [\n              106.35939307834292,\n              28.098681827718266\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              110.27545423220931,\n              29.368381722514187\n            ],\n            [\n              110.27545423220931,\n              28.984973517532836\n            ],\n            [\n              110.84752576222121,\n              28.984973517532836\n            ],\n            [\n              110.84752576222121,\n              29.368381722514187\n            ],\n            [\n              110.27545423220931,\n              29.368381722514187\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"58","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aad32e4b0c8380cd86e58","contributors":{"authors":[{"text":"Horan, M.F.","contributorId":75282,"corporation":false,"usgs":true,"family":"Horan","given":"M.F.","email":"","affiliations":[],"preferred":false,"id":377365,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morgan, J. W.","contributorId":92384,"corporation":false,"usgs":true,"family":"Morgan","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":377367,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grauch, R. I. 0000-0002-1763-0813","orcid":"https://orcid.org/0000-0002-1763-0813","contributorId":107698,"corporation":false,"usgs":true,"family":"Grauch","given":"R. I.","affiliations":[],"preferred":false,"id":377368,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Coveney, R.M. Jr.","contributorId":8861,"corporation":false,"usgs":true,"family":"Coveney","given":"R.M.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":377363,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Murowchick, J.B.","contributorId":45058,"corporation":false,"usgs":true,"family":"Murowchick","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":377364,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hulbert, L.J.","contributorId":91261,"corporation":false,"usgs":true,"family":"Hulbert","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":377366,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70017794,"text":"70017794 - 1994 - Organonitrogen herbicides in the lower Kansas River basin","interactions":[],"lastModifiedDate":"2024-02-15T15:17:36.134163","indexId":"70017794","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2136,"text":"Journal - American Water Works Association","active":true,"publicationSubtype":{"id":10}},"title":"Organonitrogen herbicides in the lower Kansas River basin","docAbstract":"<p>Atrazine, which is not readily removed by conventional treatment, may cause problems for water utilities in agricultural areas.</p><p>To help managers, planners, and regulators determine when and where surface waters are likely to be adversely affected by organonitrogen herbicides, the authors analyzed various data on the distribution of these compounds in the lower Kansas River basin. They found that atrazine was the most frequently detected herbicide, was found in the highest concentrations, and was most likely to exceed the maximum contaminant level. The highest atrazine concentrations in the water were measured where the largest amounts of atrazine had been applied to the land, and median concentrations were higher in spring and summer than in fall and winter. Atrazine and chemically similar herbicides are not effectively removed by traditional water treatment. The Kansas State Board of Agriculture has established a pesticide management area to decrease the amount of atrazine that enters surface water.</p>","language":"English","publisher":"American Water Works Association","doi":"10.1002/j.1551-8833.1994.tb06139.x","issn":"0003150X","usgsCitation":"Stamer, J.K., and Zelt, R.B., 1994, Organonitrogen herbicides in the lower Kansas River basin: Journal - American Water Works Association, v. 86, no. 1, p. 93-104, https://doi.org/10.1002/j.1551-8833.1994.tb06139.x.","productDescription":"12 p.","startPage":"93","endPage":"104","numberOfPages":"12","costCenters":[],"links":[{"id":228999,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"86","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7086e4b0c8380cd760a2","contributors":{"authors":[{"text":"Stamer, John K.","contributorId":104481,"corporation":false,"usgs":true,"family":"Stamer","given":"John","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":377582,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zelt, Ronald B. 0000-0001-9024-855X rbzelt@usgs.gov","orcid":"https://orcid.org/0000-0001-9024-855X","contributorId":300,"corporation":false,"usgs":true,"family":"Zelt","given":"Ronald","email":"rbzelt@usgs.gov","middleInitial":"B.","affiliations":[{"id":464,"text":"Nebraska Water Science Center","active":true,"usgs":true},{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":377581,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70017755,"text":"70017755 - 1994 - Studies of the Reactivity of the Ferrihydrite Surface by Iron Isotopic Exchange and Mössbauer Spectroscopy","interactions":[],"lastModifiedDate":"2023-06-02T13:43:05.166992","indexId":"70017755","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1245,"text":"Clays and Clay Minerals","onlineIssn":"1552-8367","printIssn":"0009-8604","active":true,"publicationSubtype":{"id":10}},"title":"Studies of the Reactivity of the Ferrihydrite Surface by Iron Isotopic Exchange and Mössbauer Spectroscopy","docAbstract":"<p>Two-line ferrihydrite is an important adsorbent of many toxics in natural and anthropogenic systems; however, the specific structural sites responsible for the high adsorption capacity are not well understood. A combination of chemical and spectroscopic techniques have been employed in this study to gain further insight into the structural nature of sites at the ferrihydrite surface. The kinetics of iron isotopic exchange demonstrated that there are at least two types of iron sites in ferrihydrite. One population of sites, referred to as <i>labile</i> sites, approached iron isotopic equilibrium within 24 hr in <sup>59</sup>Fe-NTA solutions, while the second population of sites, referred to as <i>non-labile</i>, exhibited a much slower rate of isotopic exchange. Adsorbed arsenate reduced the degree of exchange by labile sites, indicating that the anion blocked or greatly inhibited the rate of exchange of these sites. Mössbauer spectra were collected from a variety of samples including <sup>56</sup>Fe-ferrihydrite samples with <sup>57</sup>Fe in labile sites, samples containing <sup>57</sup>Fe throughout the structure, and samples with <sup>57</sup>Fe in non-labile sites. The spectra showed characteristic broad doublets signifying poor structural order. Refined fits of the spectra indicated that labile sites have larger quadrupole splitting, hence more local distortion, than non-labile sites. In all cases, the spectra demonstrated some degree of asymmetry, indicating a distribution of Fe environments in ferrihydrite. Overall spectral findings, combined with recent EXAFS results (Waychunas <i>et al.</i>, 1993), indicate that labile sites likely are more reactive (with respect to iron isotopic exchange) because they have fewer neighboring Fe octahedra and are therefore bound less strongly to the ferrihydrite structure. The labile population of sites probably is composed of end sites of the dioctahedral chain structure of 2-line ferrihydrite, which is a subset of the entire population of surface sites. Mössbauer spectra of samples containing adsorbed arsenate indicated that the anion may slightly decrease the distortion of labile sites and stabilized the structure as a whole by bidentate bonding.</p>","language":"English","publisher":"Springer","doi":"10.1346/CCMN.1994.0420104","usgsCitation":"Rea, B.A., Davis, J., and Waychunas, G.A., 1994, Studies of the Reactivity of the Ferrihydrite Surface by Iron Isotopic Exchange and Mössbauer Spectroscopy: Clays and Clay Minerals, v. 42, no. 1, p. 23-34, https://doi.org/10.1346/CCMN.1994.0420104.","productDescription":"12 p.","startPage":"23","endPage":"34","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":228440,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"42","issue":"1","noUsgsAuthors":false,"publicationDate":"2024-02-28","publicationStatus":"PW","scienceBaseUri":"505b9cb1e4b08c986b31d488","contributors":{"authors":[{"text":"Rea, Brigid A.","contributorId":82282,"corporation":false,"usgs":true,"family":"Rea","given":"Brigid","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":377473,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, James A.","contributorId":69289,"corporation":false,"usgs":true,"family":"Davis","given":"James A.","affiliations":[],"preferred":false,"id":377474,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waychunas, Glenn A.","contributorId":189615,"corporation":false,"usgs":false,"family":"Waychunas","given":"Glenn","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":377475,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":21545,"text":"ofr94202 - 1994 - A direct-current resistivity survey near the Marine Corps Logistics Bases at Nebo and Yermo, Barstow, California","interactions":[],"lastModifiedDate":"2012-02-02T00:07:47","indexId":"ofr94202","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-202","title":"A direct-current resistivity survey near the Marine Corps Logistics Bases at Nebo and Yermo, Barstow, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr94202","usgsCitation":"Zohdy, A.A., and Bisdorf, R.J., 1994, A direct-current resistivity survey near the Marine Corps Logistics Bases at Nebo and Yermo, Barstow, California: U.S. Geological Survey Open-File Report 94-202, 155 p. :chiefly ill. (some col.) ;28 cm., https://doi.org/10.3133/ofr94202.","productDescription":"155 p. :chiefly ill. (some col.) ;28 cm.","costCenters":[],"links":[{"id":153974,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0202/report-thumb.jpg"},{"id":51134,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0202/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aeced","contributors":{"authors":[{"text":"Zohdy, Adel A. R.","contributorId":61799,"corporation":false,"usgs":true,"family":"Zohdy","given":"Adel","email":"","middleInitial":"A. R.","affiliations":[],"preferred":false,"id":184632,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bisdorf, Robert J.","contributorId":107277,"corporation":false,"usgs":true,"family":"Bisdorf","given":"Robert","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":184633,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70017793,"text":"70017793 - 1994 - The geochemical evolution of low-molecular-weight organic acids derived from the degradation of petroleum contaminants in groundwater","interactions":[],"lastModifiedDate":"2019-02-27T10:21:00","indexId":"70017793","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"The geochemical evolution of low-molecular-weight organic acids derived from the degradation of petroleum contaminants in groundwater","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id5\" class=\"abstract author\"><div id=\"aep-abstract-sec-id6\"><p>The geochemical evolution of low-molecular-weight organic acids in groundwater downgradient from a crude-oil spill near Bemidji, Minnesota, was studied over a five year period (1986–1990). The organic acids are metabolic intermediates of the degradation of components of the crude oil and are structurally related to hydrocarbon precursors. The concentrations of organic acids, particularly aliphatic acids, increase as the microbial alteration of hydrocarbons progresses. The organic-acid pool changes in composition and concentration over time and in space as the degradation processes shift from Fe(III) reduction to methanogenesis. Over time, the aquifer system evolves into one in which the groundwater contains more oxidized products of hydrocarbon degradation and the reduced forms of iron, manganese, and nitrogen. Laboratory microcosm experiments with aquifer material support the hypothesis that organic acids observed in the groundwater originate from the microbial degradation of aromatic hydrocarbons under anoxic conditions.</p><p>The geochemistry of two other shallow aquifers in coastal plain sediments, one contaminated with creosote waste and the other with gasoline, were compared to the Bemidji site. The geochemical evolution of the low-molecular-weight organic acid pool in these systems is controlled, in part, by the presence of electron acceptors available for microbially mediated electron-transfer reactions. The depletion of electron acceptors in aquifers leads to the accumulation of aliphatic organic acids in anoxic groundwater.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(94)90511-8","issn":"00167037","usgsCitation":"Cozzarelli, I., Baedecker, M., Eganhouse, R., and Goerlitz, D., 1994, The geochemical evolution of low-molecular-weight organic acids derived from the degradation of petroleum contaminants in groundwater: Geochimica et Cosmochimica Acta, v. 58, no. 2, p. 863-877, https://doi.org/10.1016/0016-7037(94)90511-8.","productDescription":"15 p.","startPage":"863","endPage":"877","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":228998,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"58","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bac47e4b08c986b3233b9","contributors":{"authors":[{"text":"Cozzarelli, I.M. 0000-0002-5123-1007","orcid":"https://orcid.org/0000-0002-5123-1007","contributorId":22343,"corporation":false,"usgs":true,"family":"Cozzarelli","given":"I.M.","affiliations":[],"preferred":false,"id":377578,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baedecker, M.J.","contributorId":42702,"corporation":false,"usgs":true,"family":"Baedecker","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":377579,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eganhouse, R.P.","contributorId":67555,"corporation":false,"usgs":true,"family":"Eganhouse","given":"R.P.","email":"","affiliations":[],"preferred":false,"id":377580,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Goerlitz, D.F.","contributorId":8445,"corporation":false,"usgs":true,"family":"Goerlitz","given":"D.F.","affiliations":[],"preferred":false,"id":377577,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":27420,"text":"wri934218 - 1994 - Water quality assessment of Maumelle and Winona reservoir systems, central Arkansas, May 1989-October 1992","interactions":[],"lastModifiedDate":"2022-12-19T19:56:30.478877","indexId":"wri934218","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"93-4218","title":"Water quality assessment of Maumelle and Winona reservoir systems, central Arkansas, May 1989-October 1992","docAbstract":"Water quality of the Maumelle and Winona water supply reservoir systems in central Arkansas, was assessed on the basis of the data collected from May 1989 through October 1992. Water quality relative to: (1) suitability for municipal water supply; (2) other streams and reservoirs within the region; and for the Maumelle reservoir, (3) the ecological trophic condition and sensity to change. The Maumelle reservoir covers 8,900 acres and is relatively shallow (maximum depth is 45 feet). The Winona reservoir covers 1,240 acres and has a maximum depth of 100 feet. \r\n\r\nThe tributary and reservoir water was analyzed for constituents regulated by the U.S. Environmental Protection Agency and the Arkansas Department of Health. In many cases, the concentration of these constituents was at or below detection limits, which was well below the respective maximum contaminant levels used by the Arkansas Department of Health. Total iron and manganese concentrations often exceeded the maximum contaminant level, especially in the bottom of Maumelle. Turbidity levels also exceeded the maximum contaminant level, but this would be expected in the raw water. \r\n\r\nThe water quality of Maumelle and Winona reservoir systems also compared favorably when measured against other regional streams and reservoirs. From these comparisons, it can be considered that the water quality of the major tributaries discharging into the respective reservoirs represents the baseline or pristine condition within the region. Likewise, the water quality of the reservoirs could be considered to represent the baseline condition; Maumelle for a shallow, impounded flood-plain reservoir, and Winona for a deep river valley reservoir.\r\n\r\nData from the Maumelle reservoir system were used to investigate trophic condition using empirical models developed from an 80 lake cross-sectional data set that examined, specified, and parameterized trophic state relations. Observed and predicted values generated from empirical trophic state models compared favorably. The Maumelle reservoir can be considered in a state of oligo-mesotrophic transition. If nutrient inputs can be maintained at current levels, the water quality of the Maumelle reservoir should remain relatively stable. However, increases in phosphorus load may alter the water quality from its present oligo-mesotrophic condition to that of a more eutrophic condition, and this trophic response may be amplified with increases in nitrogen loading.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri934218","usgsCitation":"Green, W.R., 1994, Water quality assessment of Maumelle and Winona reservoir systems, central Arkansas, May 1989-October 1992: U.S. Geological Survey Water-Resources Investigations Report 93-4218, v, 42 p., https://doi.org/10.3133/wri934218.","productDescription":"v, 42 p.","temporalStart":"1989-05-01","temporalEnd":"1992-10-31","costCenters":[{"id":225,"text":"Earth Science Information Center","active":false,"usgs":true}],"links":[{"id":158093,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8807,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri93-4218/","linkFileType":{"id":5,"text":"html"}},{"id":410726,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_49257.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Arkansas","otherGeospatial":"Maumelle and Winona Reservoir systems","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -92.4667,\n              34.9167\n            ],\n            [\n              -93.0833,\n              34.9167\n            ],\n            [\n              -93.0833,\n              34.7833\n            ],\n            [\n              -92.4667,\n              34.7833\n            ],\n            [\n              -92.4667,\n              34.9167\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9b5b","contributors":{"authors":[{"text":"Green, W. Reed","contributorId":87886,"corporation":false,"usgs":true,"family":"Green","given":"W.","email":"","middleInitial":"Reed","affiliations":[],"preferred":false,"id":198085,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70017741,"text":"70017741 - 1994 - Floodflow effects on riparian vegetation in Arizona","interactions":[],"lastModifiedDate":"2012-03-12T17:19:53","indexId":"70017741","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Floodflow effects on riparian vegetation in Arizona","docAbstract":"A relation for estimating changes in the condition of riparian vegetation as a function of stream power was developed for stream channels in central Arizona. Flood and vegetation data were collected from 13 flows at 11 sites. Stream power was computed at cross sections and plotted against the average height of vegetation for each flow. The effect of the flow - no effect, little effect, laid over, or removed - on the riparian vegetation is related to stream power and vegetation height. As vegetation height increases, the magnitude of stream power needed to affect the vegetation also increases. Stream power of about 72 Newton-meters per second per meter squared is needed to lay over 1-meter-high vegetation, and stream power of about 580 Newton-meters per second per meter squared is needed to lay over 5.5-meter-high vegetation. This relation can be used to estimate vegetation conditions at the time of peak floodflow.","largerWorkTitle":"Proceedings - National Conference on Hydraulic Engineering","conferenceTitle":"Proceedings of the 1994 ASCE National Conference on Hydraulic Engineering","conferenceDate":"1 August 1994 through 5 August 1994","conferenceLocation":"Buffalo, NY, USA","language":"English","publisher":"Publ by ASCE","publisherLocation":"New York, NY, United States","issn":"10701559","isbn":"0784400377","usgsCitation":"Phillips, J.V., and Hjalmarson, H., 1994, Floodflow effects on riparian vegetation in Arizona, <i>in</i> Proceedings - National Conference on Hydraulic Engineering, no. pt 1, Buffalo, NY, USA, 1 August 1994 through 5 August 1994, p. 707-711.","startPage":"707","endPage":"711","numberOfPages":"5","costCenters":[],"links":[{"id":228996,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"pt 1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a117fe4b0c8380cd53ff2","contributors":{"authors":[{"text":"Phillips, J. V.","contributorId":40244,"corporation":false,"usgs":true,"family":"Phillips","given":"J.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":377430,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hjalmarson, H. W.","contributorId":95872,"corporation":false,"usgs":true,"family":"Hjalmarson","given":"H. W.","affiliations":[],"preferred":false,"id":377431,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70017765,"text":"70017765 - 1994 - Factors affecting accuracy of slope-area discharge determination of the September 1992 flood in Raven Fork, Western North Carolina","interactions":[],"lastModifiedDate":"2016-11-30T10:13:54","indexId":"70017765","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Factors affecting accuracy of slope-area discharge determination of the September 1992 flood in Raven Fork, Western North Carolina","docAbstract":"For the flood of September 10, 1992, in Raven Fork, Swain County, North Carolina, a peak discharge of 460 cubic meters per second was computed by using the slope-area method. Accuracy of this determination depends on suitability of the selected reach and, in particular, selection of Manning's roughness coefficients, interpretation of the high-water marks, number and placement of cross sections, presence of large expansions or contractions, state-of-flow transitions, and magnitude of the change in water-surface elevation. Some of these factors can contribute to greater uncertainties for measurements in steep mountain streams than for measurements in streams with flatter gradients.","largerWorkTitle":"Proceedings - National Conference on Hydraulic Engineering","conferenceTitle":"Proceedings of the 1994 ASCE National Conference on Hydraulic Engineering","conferenceDate":"1 August 1994 through 5 August 1994","conferenceLocation":"Buffalo, NY, USA","language":"English","publisher":"Publ by ASCE","publisherLocation":"New York, NY, United States","issn":"10701559","isbn":"0784400377","usgsCitation":"Eddins, W.H., and Zembrzuski, T.J., 1994, Factors affecting accuracy of slope-area discharge determination of the September 1992 flood in Raven Fork, Western North Carolina, <i>in</i> Proceedings - National Conference on Hydraulic Engineering, no. pt 1, Buffalo, NY, USA, 1 August 1994 through 5 August 1994, p. 645-649.","startPage":"645","endPage":"649","numberOfPages":"5","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":228624,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Carolina","county":"Swain County","city":"Raven Fork","issue":"pt 1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0e9ae4b0c8380cd5352c","contributors":{"authors":[{"text":"Eddins, W. Harold","contributorId":90056,"corporation":false,"usgs":true,"family":"Eddins","given":"W.","email":"","middleInitial":"Harold","affiliations":[],"preferred":false,"id":377503,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zembrzuski, Thomas J. Jr.","contributorId":37371,"corporation":false,"usgs":true,"family":"Zembrzuski","given":"Thomas","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":377502,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70017739,"text":"70017739 - 1994 - In search of earthquake-related hydrologic and chemical changes along Hayward Fault","interactions":[],"lastModifiedDate":"2023-01-26T12:28:14.387238","indexId":"70017739","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":835,"text":"Applied Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"In search of earthquake-related hydrologic and chemical changes along Hayward Fault","docAbstract":"Flow and chemical measurements have been made about once a month, and more frequently when required, since 1976 at two springs in Alum Rock Park in eastern San Jose, California, and since 1980 at two shallow wells in eastern Oakland in search of earthquake-related changes. All sites are on or near the Hayward Fault and are about 55 km apart. Temperature, electric conductivity, and water level or flow rate were measured in situ with portable instruments. Water samples were collected for later chemical and isotopic analyses in the laboratory. The measured flow rate at one of the springs showed a long-term decrease of about 40% since 1987, when a multi-year drought began in California. It also showed several increases that lasted a few days to a few months with amplitudes of 2.4 to 8.6 times the standard deviations above the background rate. Five of these increases were recorded shortly after nearby earthquakes of magnitude 5.0 or larger, and may have resulted from unclogging of the flow path and increase of permeability caused by strong seismic shaking. Two other flow increases were possibly induced by exceptionally heavy rainfalls. The water in both wells showed seasonal temperature and chemical variations, largely in response to rainfall. In 1980 the water also showed some clear chemical changes unrelated to rainfall that lasted a few months; these changes were followed by a magnitude 4 earthquake 37 km away. The chemical composition at one of the wells and at the springs also showed some longer-term variations that were not correlated with rainfall but possibly correlated with the five earthquakes mentioned above. These correlations suggest a common tectonic origin for the earthquakes and the anomalies. The last variation at the affected well occurred abruptly in 1989, shortly before a magnitude 5.0 earthquake 54 km away. ?? 1993.","language":"English","publisher":"Elsevier","doi":"10.1016/0883-2927(94)90055-8","issn":"08832927","usgsCitation":"King, C., Basler, D., Presser, T.S., Evans, W.C., White, L.D., and Minissale, A., 1994, In search of earthquake-related hydrologic and chemical changes along Hayward Fault: Applied Geochemistry, v. 9, no. 1, p. 83-91, https://doi.org/10.1016/0883-2927(94)90055-8.","productDescription":"9 p.","startPage":"83","endPage":"91","numberOfPages":"9","costCenters":[],"links":[{"id":228994,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Hayward Fault","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.99999800441196,\n              38.34222057686159\n            ],\n            [\n              -122.99999800441196,\n              36.69613467586389\n            ],\n            [\n              -120.6828668099721,\n              36.69613467586389\n            ],\n            [\n              -120.6828668099721,\n              38.34222057686159\n            ],\n            [\n              -122.99999800441196,\n              38.34222057686159\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"9","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3993e4b0c8380cd6197d","contributors":{"authors":[{"text":"King, C.-Y.","contributorId":81225,"corporation":false,"usgs":true,"family":"King","given":"C.-Y.","affiliations":[],"preferred":false,"id":377421,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Basler, D.","contributorId":100136,"corporation":false,"usgs":true,"family":"Basler","given":"D.","email":"","affiliations":[],"preferred":false,"id":377424,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Presser, T. S.","contributorId":93875,"corporation":false,"usgs":true,"family":"Presser","given":"T.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":377422,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Evans, William C.","contributorId":104903,"corporation":false,"usgs":true,"family":"Evans","given":"William","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":377425,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"White, L. D.","contributorId":14330,"corporation":false,"usgs":true,"family":"White","given":"L.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":377420,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Minissale, A.","contributorId":94441,"corporation":false,"usgs":true,"family":"Minissale","given":"A.","email":"","affiliations":[],"preferred":false,"id":377423,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":21396,"text":"ofr9377 - 1994 - Flood characteristics for the New River in the New River Gorge National River, West Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:07:48","indexId":"ofr9377","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"93-77","title":"Flood characteristics for the New River in the New River Gorge National River, West Virginia","docAbstract":"The frequency and magnitude of flooding of the New River in the New River Gorge National River was studied. A steady-state, one-dimensional flow model was applied to the study reach. Rating curves, cross sections, and Manning's roughness coefficients that were used are presented in this report. Manning's roughness coefficients were evaluated by comparing computed elevations (from application of the steady-state, one-dimensional flow model) to rated elevations at U.S. Geological Survey (USGS) streamflow-gaging stations and miscellaneous-rating sites. Manning's roughness coefficients ranged from 0.030 to 0.075 and varied with hydraulic depth. The 2-, 25-, and 100-year flood discharges were esti- mated on the basis of information from flood- insurance studies of Summers County, Fayette County, and the city of Hinton, and flood-frequency analysis of discharge records for the USGS streamflow-gaging stations at Hinton and Thurmond. The 100-year discharge ranged from 107,000 cubic feet per second at Hinton to 150,000 cubic feet per second at Fayette.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Books and Open-File Reports Section [distributor],","doi":"10.3133/ofr9377","usgsCitation":"Wiley, J., and Cunningham, M., 1994, Flood characteristics for the New River in the New River Gorge National River, West Virginia: U.S. Geological Survey Open-File Report 93-77, iv, 96 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr9377.","productDescription":"iv, 96 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":154062,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0077/report-thumb.jpg"},{"id":50965,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0077/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5ef21c","contributors":{"authors":[{"text":"Wiley, J.B.","contributorId":76739,"corporation":false,"usgs":true,"family":"Wiley","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":184354,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cunningham, M.K.","contributorId":86800,"corporation":false,"usgs":true,"family":"Cunningham","given":"M.K.","email":"","affiliations":[],"preferred":false,"id":184355,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44359,"text":"ofr946B - 1994 - Principal facts and field data for gravity data in and adjacent to the Reno 1 degree by 2 degrees quadrangle, Nevada and California","interactions":[],"lastModifiedDate":"2013-09-17T15:18:55","indexId":"ofr946B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-6","chapter":"B","title":"Principal facts and field data for gravity data in and adjacent to the Reno 1 degree by 2 degrees quadrangle, Nevada and California","language":"ENGLISH","doi":"10.3133/ofr946B","collaboration":"The USGS does not support this software or technical questions for the software associated with the publication.","usgsCitation":"Plouff, D., 1994, Principal facts and field data for gravity data in and adjacent to the Reno 1 degree by 2 degrees quadrangle, Nevada and California: U.S. Geological Survey Open-File Report 94-6, 1 computer disk ; 3 1/2 in. + 1 text (i, 16 p. : map ; 28 cm.), https://doi.org/10.3133/ofr946B.","productDescription":"1 computer disk ; 3 1/2 in. + 1 text (i, 16 p. : map ; 28 cm.)","costCenters":[],"links":[{"id":168047,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":277703,"type":{"id":4,"text":"Application Site"},"url":"https://pubs.usgs.gov/of/1994/0006b/application.zip"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668df5","contributors":{"authors":[{"text":"Plouff, Donald","contributorId":94657,"corporation":false,"usgs":true,"family":"Plouff","given":"Donald","email":"","affiliations":[],"preferred":false,"id":229637,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21385,"text":"ofr9439 - 1994 - Data on ground-water quality in the Carson River basin, western Nevada and eastern California, 1987-90","interactions":[],"lastModifiedDate":"2012-02-02T00:07:48","indexId":"ofr9439","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-39","title":"Data on ground-water quality in the Carson River basin, western Nevada and eastern California, 1987-90","docAbstract":"The U.S. Geological Survey collected and analyzed water samples from June 1987 through February 1990 as part of a study of the ground-water quality in the Carson River Basin.  The Carson River Basin is one of seven national pilot projects conducted by the Geological Survey as part of a National Water-Quality Assessment Program.  The data from the sampling program include analyses of 110 different constituents and properties of ground water in 400 separate samplings of 230 domestic, public-supply, irrigation, and shallow monitoring wells and one spring. The water-quality data include: field measurements, major constituents, nutrients, minor constituents, radionuclides, stable isotopes, and synthetic organic compounds.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr9439","usgsCitation":"Whitney, R., 1994, Data on ground-water quality in the Carson River basin, western Nevada and eastern California, 1987-90: U.S. Geological Survey Open-File Report 94-39, iv, 139 p. :maps ;28 cm., https://doi.org/10.3133/ofr9439.","productDescription":"iv, 139 p. :maps ;28 cm.","costCenters":[],"links":[{"id":153983,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0039/report-thumb.jpg"},{"id":50955,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0039/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c83d","contributors":{"authors":[{"text":"Whitney, Rita","contributorId":46573,"corporation":false,"usgs":true,"family":"Whitney","given":"Rita","email":"","affiliations":[],"preferred":false,"id":184331,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":17832,"text":"ofr93372 - 1994 - Water-quality data for the Ohio River from Willow Island Dam to Belleville Dam, West Virginia and Ohio, June-October 1991","interactions":[],"lastModifiedDate":"2012-02-02T00:07:12","indexId":"ofr93372","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"93-372","title":"Water-quality data for the Ohio River from Willow Island Dam to Belleville Dam, West Virginia and Ohio, June-October 1991","docAbstract":"This report contains water-quality data for the Ohio River from river mile 160.6 (1.1 mi upstream from Willow Island Dam) to river mile 203.6 (0.3 mi upstream from Belleville Dam) during the summer of 1991. Water quality was determined by a combi- nation of synoptic field measurements and laboratory analyses. Synoptic sampling consisted of 8 cross-sectional transects and a longitudinal transect with 28 mid-channel stations. Each cross- sectional transect included five vertical profiles of water temperature, dissolved oxygen concen- tration, pH, and specific conductance. Longi- tudinal transect stations were sampled at three depths (near the surface, middle of the water column, and at or near the bottom) for the same characteristics. Sampling was completed in 3 days or less, and was repeated approximately every 2 weeks from June through October 1991. Beginning in August 1991, water samples were collected at selected locations and analyzed for chlorophyll-a and pheophytin concentrations, as measures of phytoplankton biomass and phytoplankton-degradation products, respectively. The depth of light penetration was estimated at all pigment-sampling locations.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr93372","usgsCitation":"Chambers, D., Miller, K.F., Waldron, M., and Falkenburg, C., 1994, Water-quality data for the Ohio River from Willow Island Dam to Belleville Dam, West Virginia and Ohio, June-October 1991: U.S. Geological Survey Open-File Report 93-372, ii, 114 p. :maps ;28 cm., https://doi.org/10.3133/ofr93372.","productDescription":"ii, 114 p. :maps ;28 cm.","costCenters":[],"links":[{"id":149776,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0372/report-thumb.jpg"},{"id":47070,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0372/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faae6","contributors":{"authors":[{"text":"Chambers, D.B.","contributorId":76762,"corporation":false,"usgs":true,"family":"Chambers","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":178047,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, K. F.","contributorId":87153,"corporation":false,"usgs":true,"family":"Miller","given":"K.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":178049,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waldron, M.C.","contributorId":33342,"corporation":false,"usgs":true,"family":"Waldron","given":"M.C.","email":"","affiliations":[],"preferred":false,"id":178046,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Falkenburg, C.W.","contributorId":80298,"corporation":false,"usgs":true,"family":"Falkenburg","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":178048,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70017766,"text":"70017766 - 1994 - Implementation and use of direct-flow connections in a coupled ground-water and surface-water model","interactions":[],"lastModifiedDate":"2024-03-19T00:03:00.091872","indexId":"70017766","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Implementation and use of direct-flow connections in a coupled ground-water and surface-water model","docAbstract":"The U.S. Geological Survey's MODFLOW finite-difference ground-water flow model has been coupled with three surface-water packages - the MODBRANCH, River, and Stream packages - to simulate surface water and its interaction with ground water. Prior to the development of the coupling packages, the only interaction between these modeling packages was that leakage values could be passed between MODFLOW and the three surface-water packages. To facilitate wider and more flexible uses of the models, a computer program was developed and added to MODFLOW to allow direct flows or stages to be passed between any of the packages and MODFLOW. The flows or stages calculated in one package can be set as boundary discharges or stages to be used in another package. Several modeling packages can be used in the same simulation depending upon the level of sophistication needed in the various reaches being modeled. This computer program is especially useful when any of the River, Stream, or MODBRANCH packages are used to model a river flowing directly into or out of wetlands in direct connection with the aquifer and represented in the model as an aquifer block. A field case study is shown to illustrate an application.","language":"English","publisher":"National Groundwater Association","doi":"10.1111/j.1745-6584.1994.tb00621.x","issn":"0017467X","usgsCitation":"Swain, E.D., 1994, Implementation and use of direct-flow connections in a coupled ground-water and surface-water model: Groundwater, v. 32, no. 1, p. 139-144, https://doi.org/10.1111/j.1745-6584.1994.tb00621.x.","productDescription":"6 p.","startPage":"139","endPage":"144","numberOfPages":"6","costCenters":[],"links":[{"id":228625,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"1","noUsgsAuthors":false,"publicationDate":"2005-08-04","publicationStatus":"PW","scienceBaseUri":"505a390be4b0c8380cd617a3","contributors":{"authors":[{"text":"Swain, Eric D. 0000-0001-7168-708X edswain@usgs.gov","orcid":"https://orcid.org/0000-0001-7168-708X","contributorId":1538,"corporation":false,"usgs":true,"family":"Swain","given":"Eric","email":"edswain@usgs.gov","middleInitial":"D.","affiliations":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"preferred":true,"id":377504,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":54514,"text":"wdrFL933A - 1994 - Water resources data, Florida, water year 1993; Volume 3A. Southwest Florida surface water","interactions":[],"lastModifiedDate":"2023-01-27T21:41:02.862215","indexId":"wdrFL933A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"FL-93-3A","title":"Water resources data, Florida, water year 1993; Volume 3A. Southwest Florida surface water","docAbstract":"<p>The Water Resources Division of the U.S. Geological Survey, in cooperation with local, State, and Federal agencies, obtains a large amount of data pertaining to the water resources of Florida each water year. These data, accumulated during many water years, constitute a valuable data base for developing an improved understanding of the water resources of the State. To make these data readily available to interested parties outside the Geological Survey, the data are published annually in this report series entitled \"Water Resources Data - Florida.\"</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrFL933A","collaboration":"Prepared in cooperation with the State of Florida and with other agencies","usgsCitation":"Coffin, J., and Fletcher, W., 1994, Water resources data, Florida, water year 1993; Volume 3A. Southwest Florida surface water: U.S. Geological Survey Water Data Report FL-93-3A, xvi, 245 p., https://doi.org/10.3133/wdrFL933A.","productDescription":"xvi, 245 p.","costCenters":[],"links":[{"id":412420,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1993/fl-93-3-a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174459,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1993/fl-93-3-a/report-thumb.jpg"}],"country":"United 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