{"pageNumber":"1245","pageRowStart":"31100","pageSize":"25","recordCount":46734,"records":[{"id":24556,"text":"ofr97492 - 1997 - National Geochemical Database: Reformatted data from the National Uranium Resource Evaluation (NURE) Hydrogeochemical and Stream Sediment Reconnaissance (HSSR) program","interactions":[],"lastModifiedDate":"2022-06-03T19:49:36.692447","indexId":"ofr97492","displayToPublicDate":"1998-12-01T00:00:00","publicationYear":"1997","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":"97-492","title":"National Geochemical Database: Reformatted data from the National Uranium Resource Evaluation (NURE) Hydrogeochemical and Stream Sediment Reconnaissance (HSSR) program","docAbstract":"The National Uranium Resource Evaluation (NURE) Hydrogeochemical and Stream Sediment Reconnaissance (HSSR) program produced a large amount of geochemical data. To fully understand how these data were generated, it is recommended that you read the History of NURE HSSR Program for a summary of the entire program.\r\n\r\nBy the time the NURE program had ended, the HSSR data consisted of 894 separate data files stored with 47 different formats. Many files contained duplication of data found in other files. The University of Oklahoma's Information Systems Programs of the Energy Resources Institute (ISP) was contracted by the Department of Energy to enhance the accessibility and usefulness of the NURE HSSR data. ISP created a single standard-format master file to replace the 894 original files. ISP converted 817 of the 894 original files before its funding apparently ran out.\r\n\r\nThe ISP-reformatted NURE data files have been released by the USGS on CD-ROM (Lower 48 States, Hoffman and Buttleman, 1994; Alaska, Hoffman and Buttleman, 1996). A description of each NURE database field, derived from a draft NURE HSSR data format manual (unpubl. commun., Stan Moll, ISP, Oct 7, 1988), was included in a readme file on each CD-ROM. That original manual was incomplete and assumed that the reformatting process had gone to completion. A lot of vital information was not included. Efforts to correct that manual and the NURE data revealed a large number of problems and missing data.\r\nAs a result of the frustrating process of cleaning and re-cleaning data from the ISP-reformatted NURE files, a new NURE HSSR data format was developed. This work represents a totally new attempt to reformat the original NURE files into 2 consistent database structures; one for water samples and a second for sediment samples, on a quadrangle by quadrangle basis, from the original NURE files. Although this USGS-reformatted NURE HSSR data format is different than that created by the ISP, many of their ideas were incorporated and expanded in this effort. All of the data from each quadrangle are being examined thoroughly in an attempt to eliminate problems, to combine partial or duplicate records, to convert all coding to a common scheme, and to identify problems even if they can not be solved at this time.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr97492","issn":"0094-9140","usgsCitation":"Smith, S.M., 1997, National Geochemical Database: Reformatted data from the National Uranium Resource Evaluation (NURE) Hydrogeochemical and Stream Sediment Reconnaissance (HSSR) program (Version 1.0: September 11, 1998; Version 1.1: July 29, 1999; Version 1.2: August 7, 2000; Version 1.3: September 11, 2001; Version 1.40: January 13, 2006; Version 1.41: February 23, 2006): U.S. Geological Survey Open-File Report 97-492, HTML Document, https://doi.org/10.3133/ofr97492.","productDescription":"HTML Document","additionalOnlineFiles":"Y","costCenters":[{"id":387,"text":"Mineral Resources 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Resources Science Center","active":true,"usgs":true},{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"preferred":true,"id":192150,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21881,"text":"ofr96580 - 1997 - Hydrologic, sedimentologic, and chemical data describing surficial bed sediments in the navigation pools of the upper Mississippi River, after the flood of 1993","interactions":[],"lastModifiedDate":"2018-10-22T18:43:33","indexId":"ofr96580","displayToPublicDate":"1998-12-01T00:00:00","publicationYear":"1997","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":"96-580","title":"Hydrologic, sedimentologic, and chemical data describing surficial bed sediments in the navigation pools of the upper Mississippi River, after the flood of 1993","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nInformation Services, Open-file Reports Section [distributor],","doi":"10.3133/ofr96580","issn":"0566-8174","usgsCitation":"1997, Hydrologic, sedimentologic, and chemical data describing surficial bed sediments in the navigation pools of the upper Mississippi River, after the flood of 1993: U.S. Geological Survey Open-File Report 96-580, xiii, 237 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr96580.","productDescription":"xiii, 237 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":51369,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0580/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153058,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0580/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e995","contributors":{"editors":[{"text":"Moody, John A. 0000-0003-2609-364X jamoody@usgs.gov","orcid":"https://orcid.org/0000-0003-2609-364X","contributorId":771,"corporation":false,"usgs":true,"family":"Moody","given":"John","email":"jamoody@usgs.gov","middleInitial":"A.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":749277,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":24497,"text":"ofr97534 - 1997 - Progress report on sediment analyses at selected faunal monitoring sites in north-central and northeastern Florida Bay","interactions":[],"lastModifiedDate":"2012-02-02T00:08:06","indexId":"ofr97534","displayToPublicDate":"1998-12-01T00:00:00","publicationYear":"1997","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":"97-534","title":"Progress report on sediment analyses at selected faunal monitoring sites in north-central and northeastern Florida Bay","docAbstract":"Florida Bay is a shallow, subtropical lagoon at the southern tip of the Florida peninsula. The 2200 square kilometer, triangular-shaped area is the site of modern carbonate sediment formation and deposition. The intricate ecosystem of the bay has undergone significant changes as the result of natural influences and human intervention. The purpose of this study is to investigate carbonate sediment characteristics and distribution in conjunction with faunal and floral to determine the substrate preferences of associated fauna and flora. The modern data provide the proxy data for down-core analyses of sediments, fauna and flora in order to document ecosystem changes in the bay. \r\n\r\nSelected sediment samples collected during 1996 from 18 sites in the northeastern and central bay were analyzed for insoluble residues, organic content, total carbonate, and percent of silt and clay sized particles. Insoluble residues range from 0.8% of the sediment in a shell lag to 11.5% with an average of 5.1%. Organic content ranged from a minimum of 1.43% of the sediment to 18.05% with an average of 7.6%. The total carbonate content ranged from 72.56% to 97.81%, averaging 87.98%. The percent silt and clay sized particles ranged from 13.75% to 63.62% for the samples analyzed. The insoluble residue content shows a general trend of decreasing insoluble residues from the northeastern bay toward the southwest. Organic content is variable throughout the bay and does not show a regional trend. Several sites show a trend of higher organic content in the samples collected in February as compared to those collected in July. \r\n\r\nLithologic examination indicated that, in addition to the carbonate mud (less than 63mm), sample components included whole and fragmented mollusks, foraminifers, bryozoans, ostracods, and organic matter. The insoluble residues consisted of quartz sand and silt, clays and siliceous fossils. A component of the insoluble residues may be dust derived from Africa and transported to southern Florida by the prevailing winds.\r\n\r\nThis report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government.","language":"ENGLISH","publisher":"Florida Geological Survey,","doi":"10.3133/ofr97534","issn":"0094-9140","usgsCitation":"Scott, T., Means, G., and Brewster-Wingard, G., 1997, Progress report on sediment analyses at selected faunal monitoring sites in north-central and northeastern Florida Bay: U.S. Geological Survey Open-File Report 97-534, 50 p. :ill. ;28 cm., https://doi.org/10.3133/ofr97534.","productDescription":"50 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":155729,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1583,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pdf/of/ofr97534.html","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65de39","contributors":{"authors":[{"text":"Scott, T.M.","contributorId":66694,"corporation":false,"usgs":true,"family":"Scott","given":"T.M.","email":"","affiliations":[],"preferred":false,"id":192026,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Means, G.H.","contributorId":76348,"corporation":false,"usgs":true,"family":"Means","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":192027,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brewster-Wingard, G. L.","contributorId":102508,"corporation":false,"usgs":true,"family":"Brewster-Wingard","given":"G. L.","affiliations":[],"preferred":false,"id":192028,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":24912,"text":"ofr97269 - 1997 - Proceedings of a workshop on digital mapping techniques; methods for geologic map data capture, management, and publication - June 2 - 5, 1997, Lawrence, Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:08:27","indexId":"ofr97269","displayToPublicDate":"1998-11-01T00:00:00","publicationYear":"1997","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":"97-269","title":"Proceedings of a workshop on digital mapping techniques; methods for geologic map data capture, management, and publication - June 2 - 5, 1997, Lawrence, Kansas","docAbstract":"Introduction: From June 2-5, 1997, selected technical representatives of the USGS and State geological surveys participated in the 'AASG/USGS Digital Mapping Techniques' workshop in Lawrence, Kansas. The workshop was initiated by the AASG/USGS Data Capture Working Group, and was hosted by the Kansas Geological Survey (KGS). With a focus on methods for data capture and digital map production, the goal was to help move the state surveys and the USGS toward development of more cost-effective, flexible, and useful systems for digital mapping and GIS analysis. \r\n","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr97269","issn":"0094-9140","usgsCitation":"Soller, D.R., 1997, Proceedings of a workshop on digital mapping techniques; methods for geologic map data capture, management, and publication - June 2 - 5, 1997, Lawrence, Kansas: U.S. Geological Survey Open-File Report 97-269, vi, 120 :ill., maps; 28 cm., https://doi.org/10.3133/ofr97269.","productDescription":"vi, 120 :ill., maps; 28 cm.","temporalStart":"1997-06-02","temporalEnd":"1997-06-05","costCenters":[],"links":[{"id":157891,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0269/report-thumb.jpg"},{"id":9127,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1997/of97-269/","linkFileType":{"id":5,"text":"html"}},{"id":53889,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0269/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db6605f3","contributors":{"authors":[{"text":"Soller, David R. 0000-0001-6177-8332 drsoller@usgs.gov","orcid":"https://orcid.org/0000-0001-6177-8332","contributorId":2700,"corporation":false,"usgs":true,"family":"Soller","given":"David","email":"drsoller@usgs.gov","middleInitial":"R.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":5061,"text":"National Cooperative Geologic Mapping and Landslide Hazards","active":true,"usgs":true}],"preferred":true,"id":192785,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4985,"text":"fs04097 - 1997 - Organochlorine compounds and trace elements in streambed sediment and fish tissue, South Platte River Basin; Colorado, Nebraska, and Wyoming","interactions":[],"lastModifiedDate":"2017-09-20T16:58:55","indexId":"fs04097","displayToPublicDate":"1998-11-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"040-97","title":"Organochlorine compounds and trace elements in streambed sediment and fish tissue, South Platte River Basin; Colorado, Nebraska, and Wyoming","docAbstract":"<p>Concentration data for organochlorine compounds and trace elements in streambed sediment and fish tissue collected throughout the South Platte River Basin as part of the U.S. Geological Survey's National WaterQuality Assessment (NAWQA) Program were evaluated to determine the following: (1) which organochlorine compounds and trace elements occurred most frequently, (2) whether detection frequencies and concentrations differed among land uses, (3) how measured concentrations related to established standards and guidelines, and (4) whether there was any relation between concentrations in streambed sediment and fish tissue. Streambed sediment and fish tissue were collected at 23 sites, which were selected on the basis of physiography, geology, and land-use characteristics. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs04097","usgsCitation":"Heiny, J.S., 1997, Organochlorine compounds and trace elements in streambed sediment and fish tissue, South Platte River Basin; Colorado, Nebraska, and Wyoming: U.S. Geological Survey Fact Sheet 040-97, 4 p., https://doi.org/10.3133/fs04097.","productDescription":"4 p.","costCenters":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true},{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":118321,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1997/0040/report-thumb.jpg"},{"id":31827,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1997/0040/report.pdf","text":"Report","size":"2.1 MB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 040-97"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68aa52","contributors":{"authors":[{"text":"Heiny, Janet S.","contributorId":93468,"corporation":false,"usgs":true,"family":"Heiny","given":"Janet","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":150241,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24143,"text":"ofr97868 - 1997 - Sidescan sonar and navigation field data collected during R/V Caleta 91-1 cruise (10-14 June,1991)","interactions":[],"lastModifiedDate":"2017-01-18T09:59:17","indexId":"ofr97868","displayToPublicDate":"1998-10-01T00:00:00","publicationYear":"1997","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":"97-868","title":"Sidescan sonar and navigation field data collected during R/V Caleta 91-1 cruise (10-14 June,1991)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr97868","issn":"0094-9140","usgsCitation":"Paskevich, V.F., Twichell, D.C., and Able, K.W., 1997, Sidescan sonar and navigation field data collected during R/V Caleta 91-1 cruise (10-14 June,1991): U.S. Geological Survey Open-File Report 97-868, 2 computer laser optical discs ;4 3/4 in., in pockets in plastic envelope (14 x 14 cm.), https://doi.org/10.3133/ofr97868.","productDescription":"2 computer laser optical discs ;4 3/4 in., in pockets in plastic envelope (14 x 14 cm.)","costCenters":[],"links":[{"id":155852,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":333311,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0868/ofr97868_1.zip","text":"Disc 1","linkFileType":{"id":6,"text":"zip"}},{"id":333312,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0868/ofr97868_2.zip","text":"Disc 2","linkFileType":{"id":6,"text":"zip"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f3dbd","contributors":{"authors":[{"text":"Paskevich, Valerie F.","contributorId":81907,"corporation":false,"usgs":true,"family":"Paskevich","given":"Valerie","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":191396,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Twichell, David C.","contributorId":37730,"corporation":false,"usgs":true,"family":"Twichell","given":"David","email":"","middleInitial":"C.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":191395,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Able, Kenneth W.","contributorId":16448,"corporation":false,"usgs":false,"family":"Able","given":"Kenneth","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":191394,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":21581,"text":"ofr97743B - 1997 - Analytical data of stream-sediment and heavy-mineral-concentrate samples collected from the Buckstock Mountains and surrounding areas, Sleetmute Quadrangle, southwest Alaska","interactions":[],"lastModifiedDate":"2013-03-27T06:59:55","indexId":"ofr97743B","displayToPublicDate":"1998-10-01T00:00:00","publicationYear":"1997","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":"97-743","chapter":"B","title":"Analytical data of stream-sediment and heavy-mineral-concentrate samples collected from the Buckstock Mountains and surrounding areas, Sleetmute Quadrangle, southwest Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey :Branch of Information Services [distributor],","doi":"10.3133/ofr97743B","collaboration":"The USGS does not support this software or technical questions for the software associated with the publication.","usgsCitation":"Gray, J.E., Theodorakos, P.M., Lee, G.K., Hageman, P., and Sutley, S.J., 1997, Analytical data of stream-sediment and heavy-mineral-concentrate samples collected from the Buckstock Mountains and surrounding areas, Sleetmute Quadrangle, southwest Alaska (Diskette version.): U.S. Geological Survey Open-File Report 97-743, 1 computer disk ;3 1/2 in., https://doi.org/10.3133/ofr97743B.","productDescription":"1 computer disk ;3 1/2 in.","costCenters":[],"links":[{"id":153437,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":270232,"type":{"id":4,"text":"Application Site"},"url":"https://pubs.usgs.gov/of/1997/0743b/application.zip"}],"edition":"Diskette version.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67fe3c","contributors":{"authors":[{"text":"Gray, J. E.","contributorId":49363,"corporation":false,"usgs":true,"family":"Gray","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":184755,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Theodorakos, P. M.","contributorId":12500,"corporation":false,"usgs":true,"family":"Theodorakos","given":"P.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":184753,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lee, G. K.","contributorId":76722,"corporation":false,"usgs":true,"family":"Lee","given":"G.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":184756,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hageman, P.O.","contributorId":44033,"corporation":false,"usgs":true,"family":"Hageman","given":"P.O.","email":"","affiliations":[],"preferred":false,"id":184754,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sutley, S. J.","contributorId":91484,"corporation":false,"usgs":true,"family":"Sutley","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":184757,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":24138,"text":"ofr97853 - 1997 - Digital mosaics of the GLORIA sidescan sonar data of the U.S. Atlantic East Coast","interactions":[],"lastModifiedDate":"2017-01-18T09:57:08","indexId":"ofr97853","displayToPublicDate":"1998-10-01T00:00:00","publicationYear":"1997","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":"97-853","title":"Digital mosaics of the GLORIA sidescan sonar data of the U.S. Atlantic East Coast","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr97853","issn":"0094-9140","usgsCitation":"Paskevich, V., 1997, Digital mosaics of the GLORIA sidescan sonar data of the U.S. Atlantic East Coast: U.S. Geological Survey Open-File Report 97-853, 2 computer laser optical disks ;4 3/4 in., https://doi.org/10.3133/ofr97853.","productDescription":"2 computer laser optical disks ;4 3/4 in.","costCenters":[],"links":[{"id":157169,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":333309,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0853/ofr97853_1.zip","text":"Disc 1","linkFileType":{"id":6,"text":"zip"}},{"id":333310,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0853/ofr97853_2.zip","text":"Disc 2","linkFileType":{"id":6,"text":"zip"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65ab83","contributors":{"authors":[{"text":"Paskevich, V.F.","contributorId":96285,"corporation":false,"usgs":true,"family":"Paskevich","given":"V.F.","email":"","affiliations":[],"preferred":false,"id":191386,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26947,"text":"wri974272 - 1997 - Mesocosm experiments to assess factors affecting phosphorus retention and release in an extended Wisconsin wetland","interactions":[],"lastModifiedDate":"2015-10-27T15:54:54","indexId":"wri974272","displayToPublicDate":"1998-10-01T00:00:00","publicationYear":"1997","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":"97-4272","title":"Mesocosm experiments to assess factors affecting phosphorus retention and release in an extended Wisconsin wetland","docAbstract":"<p>Phosphorus retention by wetland sediments and vegetation was investigated in Jackson Creek wetland, an extension of an existing prairie marsh in southeastern Wisconsin. The extended wetland construction was undertaken in 1992-93 to help reduce the phosphorus loading to a downstream eutrophic lake. Two approaches were used to study potential and actual phosphorus retention in the system. Mesocosm experiments of 20-40 days duration indicated that retention of total and dissolved reactive phosphorus in mesocosm cells containing macrophytes and/or sediments was reduced by factors of 2-20 relative to cells containing only water or a copper algicide to suppress metabolic activity. In contrast to the nutrient trapping function, these results show a potential for net phosphorus release that can be associated with increased biological richness. Measurements of water flow and nutrient loads at the wetland's inflow and outflow points demonstrated 9-39% net uptake of phosphorus on an annual scale but frequent occurrences of net phosphorus release over shorter (one-month) time scales. These episodes of release are most likely during the summer months. Thus, the wetland role in phosphorus cycling is not one of a true source or sink, although the annual budget data alone suggest substantial net retention. Effective management of the wetland for its nutrient trapping potential can be hindered by this oversimplification. The system is instead subject to relatively short-term alternation between net import and export. The periodic phosphorus export, although representing a small fraction of net annual import, could be critical for growth of macrophyte and algal communities downstream.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri974272","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Elder, J.F., Manion, B., and Goddard, G.L., 1997, Mesocosm experiments to assess factors affecting phosphorus retention and release in an extended Wisconsin wetland: U.S. Geological Survey Water-Resources Investigations Report 97-4272, vi, 14 p., https://doi.org/10.3133/wri974272.","productDescription":"vi, 14 p.","numberOfPages":"19","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":119103,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1997/4272/report-thumb.jpg"},{"id":55835,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1997/4272/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","county":"Walworth County","otherGeospatial":"Delevan Lake, Jackson Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.57383728027344,\n              42.717759147911806\n            ],\n            [\n              -88.76884460449219,\n              42.62385465855651\n            ],\n            [\n              -88.8079833984375,\n              42.583422001323584\n            ],\n            [\n              -88.76335144042969,\n              42.55763248666914\n            ],\n            [\n              -88.69606018066406,\n              42.54498667313236\n            ],\n            [\n              -88.6164093017578,\n              42.552574468712514\n            ],\n            [\n              -88.56559753417969,\n              42.56623017635374\n            ],\n            [\n              -88.48663330078125,\n              42.628401690377316\n            ],\n            [\n              -88.45848083496094,\n              42.64204079304428\n            ],\n            [\n              -88.44131469726562,\n              42.66325123326261\n            ],\n            [\n              -88.43376159667969,\n              42.68344492725026\n            ],\n            [\n              -88.41316223144531,\n              42.705145830019895\n            ],\n            [\n              -88.4674072265625,\n              42.72835235396481\n            ],\n            [\n              -88.57383728027344,\n              42.717759147911806\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624f47","contributors":{"authors":[{"text":"Elder, J. F.","contributorId":54143,"corporation":false,"usgs":true,"family":"Elder","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":197297,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Manion, B.J.","contributorId":59844,"corporation":false,"usgs":true,"family":"Manion","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":197298,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goddard, G. L.","contributorId":10442,"corporation":false,"usgs":true,"family":"Goddard","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":197296,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":27109,"text":"wri974148 - 1997 - Results of quality-control sampling of water, bed sediment, and tissue in the Western Lake Michigan Drainages study unit of the National Water-Quality Assessment Program","interactions":[],"lastModifiedDate":"2015-10-22T11:09:08","indexId":"wri974148","displayToPublicDate":"1998-10-01T00:00:00","publicationYear":"1997","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":"97-4148","title":"Results of quality-control sampling of water, bed sediment, and tissue in the Western Lake Michigan Drainages study unit of the National Water-Quality Assessment Program","docAbstract":"<p>This report contains the quality control results of the Western Lake Michigan Drainages study unit of the National Water Quality Assessment Program. Quality control samples were collected in the same manner and contemporaneously with environmental samples during the first highintensity study phase in the unit (1992 through 1995) and amounted to approximately 15 percent of all samples collected. The accuracy and precision of hundreds of chemical analyses of surface and ground-water, bed sediment, and tissue was determined through the collection and analysis of field blanks, field replicates and splits, matrix spikes, and surrogates. Despite the several detections of analytes in the field blanks, the concentrations of most constituents in the environmental samples will likely be an order of magnitude or higher than those in the blanks. However, frequent detections, and high concentrations, of dissolved organic carbon (DOC) in several surface and ground-water blanks are probably significant with respect to commonly measured environmental concentrations, and the environmental data will have to be qualified accordingly. The precision of sampling of water on a percent basis, as determined from replicates and splits, was generally proportional to the concentration of the constituents, with constituents present in relatively high concentrations generally having less sampling variability than those with relatively low concentrations. In general, analytes with relatively high variability between replicates were present at concentrations near the reporting limit or were associated with relatively small absolute concentration differences, or both. Precision of replicates compared to that for splits in bed sediment samples was similar, thus eliminating sampling as a major source of variability in analyte concentrations. In the case the phthalates in bed sediment, contamination in either the field or laboratory could have caused the relatively large variability between replicate samples and between split samples.Variability of analyte concentrations in tissue samples was relatively low, being 29 percent or less for all constituents. Recoveries of most laboratory schedule 2001/2010 pesticide spike compounds in surfacewater samples were reasonably good. Low intrinsic method recovery resulted in relatively low recovery forp,p'-DDE, metribuzin, and propargite. In the case of propargite, decomposition with the environmental sample matrices was also indicated. Recoveries of two compounds, cyanazine and thiobencarb, might have been biased high due to interferences. The one laboratory schedule 2050/2051 field matrix pesticide spike indicated numerous operational problems with this method that biased recoveries either low or high. Recoveries of pesticides from both pesticide schedules in field spikes of ground-water samples generally were similar to those of field matrix spikes of surface- water samples. High maximum recoveries were noted for tebuthiuron, disulfoton, DCPA, and permethrin, which indicates the possible presence of interferents in the matrices for these compounds. Problems in the recoveries of pesticides on schedule 2050/2051 from ground-water samples generally were the same as those for surfacewater samples. Recoveries of VOCs in field matrix spikes were reasonable when consideration was given for the use of the micropipettor that delivered only about 80 percent on average of the nominal mass of spiked analytes. Finally, the recoveries of most surrogate compounds in surface and ground-water samples were reasonable. Problems in sample handling (for example, spillage) were likely not the cause of any of the low recoveries of spiked compounds.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri974148","usgsCitation":"Fitzgerald, S., 1997, Results of quality-control sampling of water, bed sediment, and tissue in the Western Lake Michigan Drainages study unit of the National Water-Quality Assessment Program: U.S. Geological Survey Water-Resources Investigations Report 97-4148, vii, 24 p., https://doi.org/10.3133/wri974148.","productDescription":"vii, 24 p.","numberOfPages":"31","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":158993,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1997/4148/report-thumb.jpg"},{"id":55969,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1997/4148/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Michigan, Wisconsin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.429443359375,\n              45.61403741135093\n            ],\n            [\n              -86.66015624999999,\n              46.40756396630067\n            ],\n            [\n              -87.099609375,\n              46.41513877649202\n            ],\n            [\n              -87.51708984375,\n              46.53619267489863\n            ],\n            [\n              -87.71484375,\n              46.626806395355175\n            ],\n            [\n              -88.033447265625,\n              46.7549166192819\n            ],\n            [\n              -88.13232421875,\n              46.7549166192819\n            ],\n            [\n              -88.39599609375,\n              46.76244305208004\n            ],\n            [\n              -88.934326171875,\n              46.604167162931844\n            ],\n            [\n              -89.176025390625,\n              46.52863469527167\n            ],\n            [\n              -89.296875,\n              46.32417161725694\n            ],\n            [\n              -89.84619140625,\n              45.4524242413431\n            ],\n            [\n              -90.142822265625,\n              44.56699093657141\n            ],\n            [\n              -90.274658203125,\n              43.667871610117494\n            ],\n            [\n              -89.84619140625,\n              43.068887774169625\n            ],\n            [\n              -89.47265625,\n              42.819580715795915\n            ],\n            [\n              -88.9013671875,\n              42.69858589169842\n            ],\n            [\n              -88.26416015625,\n              42.601619944327965\n            ],\n            [\n              -87.791748046875,\n              42.48019996901214\n            ],\n            [\n              -87.6708984375,\n              42.827638636242284\n            ],\n            [\n              -87.78076171875,\n              43.1811470593997\n            ],\n            [\n              -87.5390625,\n              44.07969327425713\n            ],\n            [\n              -87.308349609375,\n              44.55916341529184\n            ],\n            [\n              -86.8359375,\n              45.22848059584359\n            ],\n            [\n              -86.781005859375,\n              45.43700828867389\n            ],\n            [\n              -86.737060546875,\n              45.460130637921004\n            ],\n            [\n              -86.429443359375,\n              45.61403741135093\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fa32","contributors":{"authors":[{"text":"Fitzgerald, S.A.","contributorId":94348,"corporation":false,"usgs":true,"family":"Fitzgerald","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":197565,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30356,"text":"wri974032 - 1997 - Geochemistry and microbiology of iron-related well-screen encrustation and aquifer biofouling in Suffolk County, Long Island, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:08:56","indexId":"wri974032","displayToPublicDate":"1998-10-01T00:00:00","publicationYear":"1997","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":"97-4032","title":"Geochemistry and microbiology of iron-related well-screen encrustation and aquifer biofouling in Suffolk County, Long Island, New York","docAbstract":" Iron-related well-screen encrustation and aquifer biofouling has decreased the specific capacity of several production wells in Suffolk County, N.Y., and has forced the Suffolk County Water Authority to adopt a costly well-reconditioning and replacement program. The specific-capacity declines are the result of the precipitation of iron oxyhydroxides and the growth of iron bacteria on the well screens and in the pore spaces of the surrounding formation. Mineralogic and chemical analyses indicate that the inorganic part of the encrusting material consists primarily of amorphous ferric hydroxide (Fe(OH)3 ); minor components of the material include goethite (FeOOH), hematite (Fe2 O 3 ), and quartz (SiO 2 ). The weight percent of ferric hydroxide in the material ranged from 32.3 to 98.6 percent and averaged 64.3 percent. Equilibrium modeling indicated that during pumping the well waters were supersaturated with respect to goethite, hematite, magnetite, and quartz and were under-saturated with respect to ferric hydroxide. Theoretical Eh values computed for the ferrous/ferric-iron redox couple and the oxygen/water redox couple averaged 390 millivolts and 810 millivolts, respectively, indicating that the waters were in a state of redox disequilibrium. The disequilibrium condition arises from the mixing of ground water with a low dissolved-oxygen concentration with oxygenated ground water during operation of the well. The low pH of the ground water contributes to the disequilibrium condition by slowing the rate of iron oxidation after the introduction of oxygen.     Chemical and mineralogical data indicate that most of the encrusting material in the wells was deposited while the wells were shut down, probably in response to the use of treated water of higher pH to keep pump turbines wet while the wells were not in operation; the increased pH of water in the static water column increases the rate of ferrous-iron oxidation and causes the well water to become increasingly saturated with respect to ferric hydroxide. The median half-time of oxidation in samples of untreated ground water (pH 4-5) was 4.19 days, whereas the average half-time of oxidation in treated water (pH 7-8) was 11.9 minutes Equilibrium modeling indicated that treated waters generally were supersaturated with respect to ferric hydroxide, whereas untreated well waters were not.     Field and laboratory data indicate that iron bacteria play an important role in the encrustation and biofouling process in Suffolk County. Filamentous iron bacteria were common in the affected wells. The most common species was Gallionella ferruginea, an effective biofouling agent that prefers water with low, but detectable, dissolved-oxygen concentrations and high dissolved-iron concentrations; this species was more common in biofilm samples from the Magothy aquifer than in those from the upper glacial aquifer. Iron bacteria also were found in sediment cores from several locations in the aquifer and in drilling water. Lignite could act as a carbon source for heterotrophic iron bacteria, which could accelerate the formation of iron-bacteria biofilms in wells screened in some parts of the Magothy aquifer. Iron-bacteria biofilms alter the chemistry of well water by removing iron, manganese, and sulfate from solution and by increasing the pH. Sulfur-reducing bacteria and iron-sulfide mineral phases were observed in some samples of encrusting material, indicating that these bacteria could contribute to well-screen encrustation in some geochemical environments. ","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/wri974032","usgsCitation":"Walter, D.A., 1997, Geochemistry and microbiology of iron-related well-screen encrustation and aquifer biofouling in Suffolk County, Long Island, New York: U.S. Geological Survey Water-Resources Investigations Report 97-4032, v, 37 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri974032.","productDescription":"v, 37 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124353,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1997/4032/report-thumb.jpg"},{"id":59145,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1997/4032/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab75a","contributors":{"authors":[{"text":"Walter, D. A.","contributorId":75179,"corporation":false,"usgs":true,"family":"Walter","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":203109,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29864,"text":"wri974227 - 1997 - Interim results of quality-control sampling of surface water for the Upper Colorado River National Water-Quality Assessment Study Unit, water years 1995-96","interactions":[],"lastModifiedDate":"2012-02-02T00:08:59","indexId":"wri974227","displayToPublicDate":"1998-09-01T00:00:00","publicationYear":"1997","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":"97-4227","title":"Interim results of quality-control sampling of surface water for the Upper Colorado River National Water-Quality Assessment Study Unit, water years 1995-96","docAbstract":"Quality-control samples provide part of the information needed to estimate the bias and variability that result from sample collection, processing, and analysis. Quality-control samples of surface water collected for the Upper Colorado River National Water-Quality Assessment study unit for water years 1995?96 are presented and analyzed in this report. The types of quality-control samples collected include pre-processing split replicates, concurrent replicates, sequential replicates, post-processing split replicates, and field blanks. Analysis of the pre-processing split replicates, concurrent replicates, sequential replicates, and post-processing split replicates is based on differences between analytical results of the environmental samples and analytical results of the quality-control samples. Results of these comparisons indicate that variability introduced by sample collection, processing, and handling is low and will not affect interpretation of the environmental data. The differences for most water-quality constituents is on the order of plus or minus 1 or 2 lowest rounding units. A lowest rounding unit is equivalent to the magnitude of the least significant figure reported for analytical results. The use of lowest rounding units avoids some of the difficulty in comparing differences between pairs of samples when concentrations span orders of magnitude and provides a measure of the practical significance of the effect of variability. Analysis of field-blank quality-control samples indicates that with the exception of chloride and silica, no systematic contamination of samples is apparent. Chloride contamination probably was the result of incomplete rinsing of the dilute cleaning solution from the outlet ports of the decaport sample splitter. Silica contamination seems to have been introduced by the blank water. Sampling and processing procedures for water year 1997 have been modified as a result of these analyses.","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nInformation Services [distributor],","doi":"10.3133/wri974227","usgsCitation":"Spahr, N., and Boulger, R., 1997, Interim results of quality-control sampling of surface water for the Upper Colorado River National Water-Quality Assessment Study Unit, water years 1995-96: U.S. Geological Survey Water-Resources Investigations Report 97-4227, iv, 34 p. :ill., map ;28 cm., https://doi.org/10.3133/wri974227.","productDescription":"iv, 34 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":124964,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_97_4227.jpg"},{"id":2393,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri97-4227","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48afe4b07f02db52f5e4","contributors":{"authors":[{"text":"Spahr, N.E.","contributorId":79476,"corporation":false,"usgs":true,"family":"Spahr","given":"N.E.","email":"","affiliations":[],"preferred":false,"id":202261,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boulger, R.W.","contributorId":86386,"corporation":false,"usgs":true,"family":"Boulger","given":"R.W.","affiliations":[],"preferred":false,"id":202262,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26558,"text":"wri974222 - 1997 - PHREEQCI: A graphical user interface for the geochemical computer program PHREEQC","interactions":[],"lastModifiedDate":"2019-12-05T10:52:44","indexId":"wri974222","displayToPublicDate":"1998-09-01T00:00:00","publicationYear":"1997","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":"97-4222","title":"PHREEQCI: A graphical user interface for the geochemical computer program PHREEQC","docAbstract":"PhreeqcI is a Windows-based graphical user interface for the geochemical computer program PHREEQC. PhreeqcI provides the capability to generate and edit input data files, run simulations, and view text files containing simulation results, all within the framework of a single interface. PHREEQC is a multipurpose geochemical program that can perform speciation, inverse, reaction-path, and 1D advective reaction-transport modeling. Interactive access to all of the capabilities of PHREEQC is available with PhreeqcI. The interface is written in Visual Basic and will run on personal computers under the Windows(3.1), Windows95, and WindowsNT operating systems. ","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri974222","usgsCitation":"Charlton, S.R., Macklin, C.L., and Parkhurst, D.L., 1997, PHREEQCI: A graphical user interface for the geochemical computer program PHREEQC: U.S. Geological Survey Water-Resources Investigations Report 97-4222, 9 p., https://doi.org/10.3133/wri974222.","productDescription":"9 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":122884,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1997/4222/report-thumb.jpg"},{"id":55425,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1997/4222/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689e4d","contributors":{"authors":[{"text":"Charlton, Scott R. 0000-0001-7332-3394 charlton@usgs.gov","orcid":"https://orcid.org/0000-0001-7332-3394","contributorId":1632,"corporation":false,"usgs":true,"family":"Charlton","given":"Scott","email":"charlton@usgs.gov","middleInitial":"R.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":196614,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Macklin, Clifford L.","contributorId":45347,"corporation":false,"usgs":true,"family":"Macklin","given":"Clifford","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":196615,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Parkhurst, David L. 0000-0003-3348-1544 dlpark@usgs.gov","orcid":"https://orcid.org/0000-0003-3348-1544","contributorId":1088,"corporation":false,"usgs":true,"family":"Parkhurst","given":"David","email":"dlpark@usgs.gov","middleInitial":"L.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":196613,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":22005,"text":"ofr97736 - 1997 - Paleontological data from Mud Creek Core 1, southern Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:07:50","indexId":"ofr97736","displayToPublicDate":"1998-09-01T00:00:00","publicationYear":"1997","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":"97-736","title":"Paleontological data from Mud Creek Core 1, southern Florida","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr97736","issn":"0094-9140","usgsCitation":"Willard, D., Brewster-Wingard, G., Fellman, C., and Ishman, S., 1997, Paleontological data from Mud Creek Core 1, southern Florida: U.S. Geological Survey Open-File Report 97-736, 13 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr97736.","productDescription":"13 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":153750,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1179,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pdf/of/ofr97736.html","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689c60","contributors":{"authors":[{"text":"Willard, Debra  A. 0000-0003-4878-0942","orcid":"https://orcid.org/0000-0003-4878-0942","contributorId":85982,"corporation":false,"usgs":true,"family":"Willard","given":"Debra  A.","affiliations":[],"preferred":false,"id":186639,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brewster-Wingard, G. L.","contributorId":102508,"corporation":false,"usgs":true,"family":"Brewster-Wingard","given":"G. L.","affiliations":[],"preferred":false,"id":186640,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fellman, Claire","contributorId":50929,"corporation":false,"usgs":true,"family":"Fellman","given":"Claire","email":"","affiliations":[],"preferred":false,"id":186638,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ishman, S. E.","contributorId":20346,"corporation":false,"usgs":true,"family":"Ishman","given":"S. E.","affiliations":[],"preferred":false,"id":186637,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":21663,"text":"ofr9787 - 1997 - Chemical and textural characteristics of sediments at an EPA reference site for dredged material on the continental slope SW of the Farallon Islands","interactions":[],"lastModifiedDate":"2017-11-05T09:33:34","indexId":"ofr9787","displayToPublicDate":"1998-09-01T00:00:00","publicationYear":"1997","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":"97-87","title":"Chemical and textural characteristics of sediments at an EPA reference site for dredged material on the continental slope SW of the Farallon Islands","docAbstract":"<p>A U.S. Environmental Protection Agency (EPA) reference site for dredged material has been established on the Continental Slope off San Francisco in water depths of 800-1500 m. This site, 35 km southwest of the Farallon Islands, serves as a reference for sediment testing in support of dredging and disposal at the San Francisco Deep Ocean Disposal Site (SF-DODS). An estimated 300 million cubic yards of dredged material from San Francisco Bay are expected to be discharged at this site during the next 50 years. Information from the reference site provides an additional baseline for monitoring environmental changes at the SF-DODS. This study provides sediment data on a suite of heavy metals and organic compounds which make up the EPA list of \"chemicals of concern\" because of their potential toxicity to marine organisms.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr9787","issn":"0566-8174","usgsCitation":"Bothner, M., Gill, P., Boothman, W., Taylor, B., and Karl, H.A., 1997, Chemical and textural characteristics of sediments at an EPA reference site for dredged material on the continental slope SW of the Farallon Islands: U.S. Geological Survey Open-File Report 97-87, v, 51 p., https://doi.org/10.3133/ofr9787.","productDescription":"v, 51 p.","costCenters":[],"links":[{"id":156096,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0087/report-thumb.jpg"},{"id":51209,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0087/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Fallaron Islands","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.4423828125,\n              37.29153547292737\n            ],\n            [\n              -122.3822021484375,\n              37.29153547292737\n            ],\n            [\n              -122.3822021484375,\n              37.95719224376526\n            ],\n            [\n              -123.4423828125,\n              37.95719224376526\n            ],\n            [\n              -123.4423828125,\n              37.29153547292737\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e4765","contributors":{"authors":[{"text":"Bothner, Michael H. mbothner@usgs.gov","contributorId":139855,"corporation":false,"usgs":true,"family":"Bothner","given":"Michael H.","email":"mbothner@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":185152,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gill, P.W.","contributorId":107877,"corporation":false,"usgs":true,"family":"Gill","given":"P.W.","email":"","affiliations":[],"preferred":false,"id":185154,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Boothman, W.S.","contributorId":11794,"corporation":false,"usgs":true,"family":"Boothman","given":"W.S.","email":"","affiliations":[],"preferred":false,"id":185150,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Taylor, B.B.","contributorId":53394,"corporation":false,"usgs":true,"family":"Taylor","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":185151,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Karl, Herman A.","contributorId":80649,"corporation":false,"usgs":true,"family":"Karl","given":"Herman","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":185153,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":23451,"text":"ofr97654 - 1997 - Summary of ground-water data for Tutuila and Aunuu, American Samoa, for July 1985 through September 1996","interactions":[],"lastModifiedDate":"2012-02-02T00:08:18","indexId":"ofr97654","displayToPublicDate":"1998-09-01T00:00:00","publicationYear":"1997","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":"97-654","title":"Summary of ground-water data for Tutuila and Aunuu, American Samoa, for July 1985 through September 1996","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr97654","issn":"0094-9140","usgsCitation":"Izuka, S.K., 1997, Summary of ground-water data for Tutuila and Aunuu, American Samoa, for July 1985 through September 1996: U.S. Geological Survey Open-File Report 97-654, iv, 44 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr97654.","productDescription":"iv, 44 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":157368,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0654/report-thumb.jpg"},{"id":52771,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0654/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6991f3","contributors":{"authors":[{"text":"Izuka, S. K.","contributorId":39818,"corporation":false,"usgs":true,"family":"Izuka","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":190129,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22089,"text":"ofr97715 - 1997 - Quaternary Geology and Liquefaction Susceptibility, San Francisco, California 1:100,000 Quadrangle: A Digital Database","interactions":[],"lastModifiedDate":"2012-02-10T00:10:07","indexId":"ofr97715","displayToPublicDate":"1998-09-01T00:00:00","publicationYear":"1997","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":"97-715","title":"Quaternary Geology and Liquefaction Susceptibility, San Francisco, California 1:100,000 Quadrangle: A Digital Database","docAbstract":"This Open-File report is a digital geologic map database.  This pamphlet serves to introduce and describe the digital data.  There are no paper maps included in the Open-File report.  The report does include, however, PostScript plot files containing the images of the geologic map sheets with explanations, as well as the accompanying text describing the geology of the area.  For those interested in a paper plot of information contained in the database or in obtaining the PostScript plot files, please see the section entitled 'For Those Who Aren't Familiar With Digital Geologic Map Databases' below. This digital map database, compiled from previously unpublished data, and new mapping by the authors, represents the general distribution of surficial deposits in the San Francisco bay region.  Together with the accompanying text file (sf_geo.txt or sf_geo.pdf), it provides current information on Quaternary geology and liquefaction susceptibility of the San Francisco, California, 1:100,000 quadrangle.  The database delineates map units that are identified by general age and lithology following the stratigraphic nomenclature of the U.S. Geological Survey.  The scale of the source maps limits the spatial resolution (scale) of the database to 1:100,000 or smaller.  The content and character of the database, as well as three methods of obtaining the database, are described below. ","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr97715","issn":"0094-9140","usgsCitation":"Knudsen, K.L., Noller, J.S., Sowers, J.M., and Lettis, W.R., 1997, Quaternary Geology and Liquefaction Susceptibility, San Francisco, California 1:100,000 Quadrangle: A Digital Database: U.S. Geological Survey Open-File Report 97-715, Report: 22 p.; 2 Plates - Plate 1: 36.25 x 28 inches, Plate 2: 35.5 x 27.5 inches; Data Files, https://doi.org/10.3133/ofr97715.","productDescription":"Report: 22 p.; 2 Plates - Plate 1: 36.25 x 28 inches, Plate 2: 35.5 x 27.5 inches; Data Files","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":153782,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0715/report-thumb.jpg"},{"id":8143,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1997/of97-715/","linkFileType":{"id":5,"text":"html"}},{"id":51529,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0715/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","projection":"UTM Zone 10","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123,37.5 ], [ -123,38 ], [ -122,38 ], [ -122,37.5 ], [ -123,37.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db63547b","contributors":{"authors":[{"text":"Knudsen, Keith L. 0000-0003-2826-5812 kknudsen@usgs.gov","orcid":"https://orcid.org/0000-0003-2826-5812","contributorId":3758,"corporation":false,"usgs":true,"family":"Knudsen","given":"Keith","email":"kknudsen@usgs.gov","middleInitial":"L.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":187021,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Noller, Jay S.","contributorId":56253,"corporation":false,"usgs":true,"family":"Noller","given":"Jay","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":187023,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sowers, Janet M.","contributorId":51318,"corporation":false,"usgs":true,"family":"Sowers","given":"Janet","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":187022,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lettis, William R.","contributorId":85970,"corporation":false,"usgs":true,"family":"Lettis","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":187024,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":24274,"text":"ofr97402 - 1997 - Characterization of stormwater runoff from the Naval Air Station and Naval Wepons Industrial Reserve Plant, Dallas, Texas, 1994-96","interactions":[],"lastModifiedDate":"2016-08-22T15:41:38","indexId":"ofr97402","displayToPublicDate":"1998-09-01T00:00:00","publicationYear":"1997","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":"97-402","title":"Characterization of stormwater runoff from the Naval Air Station and Naval Wepons Industrial Reserve Plant, Dallas, Texas, 1994-96","docAbstract":"<p>The characterization of stormwater runoff from the Naval Air Station (NAS) and the Naval Weapons Industrial Reserve Plant (NWIRP), Dallas, Texas, is necessary to determine if runoff from the facilities is contributing to off-site contamination of surface waters, A network of five fixed sites and four grab sites was established to collect stormwater-runoff samples from a substantial part of the drainage area of each facility. Fixed sites were instrumented to measure and store precipitation, stage, discharge, and runoff-volume data and to collect flow-weighted composite samples during a storm. Grab and composite samples were collected for six storms at each of the five fixed sites from October 1994 to March 1996. The grab samples were analyzed for about 100 properties and constituents including specific conductance, pH, water temperature, bacteria, trace elements, oil and grease, total phenols, and volatile organic compounds. The composite samples were analyzed for about 220 properties and constituents including specific conductance, pH, chemical oxygen demand, biochemical oxygen demand, major ions, suspended and dissolved solids, nutrients, trace elements, total organic carbon, volatile organic compounds, semivolatile organic compounds, and organochlorine and organophosphorus pesticides. Grab samples were collected for two storms (September 18,1995, and October 2,1995) at each of the four grab sites. The grab samples were analyzed for about 80 constituents including specific conductance, pH, water temperature, trace elements, and volatile organic compounds. Composite samples were collected for two of the six storms sampled at the fixed sites and analyzed for aquatic toxicity. Fathead minnow growth and survival toxicity tests and water flea reproduction and survival toxicity tests were done.</p>\n<p>Median event-mean concentrations computed for 12 selected constituents in samples from NAS and NWIRP fixed sites were compared to median event-mean concentrations for residential, commercial, industrial, and highway land uses within the Dallas-Fort Worth area computed from data collected for the National Pollutant Discharge Elimination System program. NAS and NWIRP median event-mean concentrations also were compared to those for residential and commercial land uses from the Nationwide Urban Runoff Program.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr97402","issn":"0094-9140","usgsCitation":"Raines, T.H., Baldys, S., and Lizarraga, J., 1997, Characterization of stormwater runoff from the Naval Air Station and Naval Wepons Industrial Reserve Plant, Dallas, Texas, 1994-96: U.S. Geological Survey Open-File Report 97-402, iv, 80 p., https://doi.org/10.3133/ofr97402.","productDescription":"iv, 80 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":155029,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0402/report-thumb.jpg"},{"id":53396,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0402/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4d1e","contributors":{"authors":[{"text":"Raines, T. H.","contributorId":88389,"corporation":false,"usgs":true,"family":"Raines","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":191616,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baldys, Stanley sbaldys@usgs.gov","contributorId":3366,"corporation":false,"usgs":true,"family":"Baldys","given":"Stanley","email":"sbaldys@usgs.gov","affiliations":[],"preferred":true,"id":191614,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lizarraga, J.S.","contributorId":17875,"corporation":false,"usgs":true,"family":"Lizarraga","given":"J.S.","affiliations":[],"preferred":false,"id":191615,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":21670,"text":"ofr97245 - 1997 - Chemical data for bottom sediment, lake water, bottom-sediment pore water, and fish in Mountain Creek Lake, Dallas, Texas, 1994-96","interactions":[],"lastModifiedDate":"2016-08-22T15:40:31","indexId":"ofr97245","displayToPublicDate":"1998-09-01T00:00:00","publicationYear":"1997","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":"97-245","title":"Chemical data for bottom sediment, lake water, bottom-sediment pore water, and fish in Mountain Creek Lake, Dallas, Texas, 1994-96","docAbstract":"<p>Mountain Creek Lake is a reservoir adjacent to two U.S. Department of the Navy facilities, the Naval Weapons Industrial Reserve Plant and the Naval Air Station in Dallas, Texas. A Resource Conservation and Recovery Act Facility Investigation found ground-water plumes containing chlorinated solvents on both facilities. These findings led to a U.S. Geological Survey study of Mountain Creek Lake adjacent to both facilities between June 1994 and August 1996. Bottom sediments, lake water, bottom-sediment pore water, and fish were collected for chemical analysis.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr97245","issn":"0566-8174","usgsCitation":"Jones, S., Van Metre, P., Moring, J., Braun, C., Wilson, J., and Mahler, B., 1997, Chemical data for bottom sediment, lake water, bottom-sediment pore water, and fish in Mountain Creek Lake, Dallas, Texas, 1994-96: U.S. Geological Survey Open-File Report 97-245, 127 p., https://doi.org/10.3133/ofr97245.","productDescription":"127 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":51214,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0245/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":154404,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0245/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e3e1b","contributors":{"authors":[{"text":"Jones, S.A.","contributorId":38596,"corporation":false,"usgs":true,"family":"Jones","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":185188,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Metre, P. C.","contributorId":92999,"corporation":false,"usgs":true,"family":"Van Metre","given":"P. C.","affiliations":[],"preferred":false,"id":185191,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moring, J.B.","contributorId":89165,"corporation":false,"usgs":true,"family":"Moring","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":185190,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Braun, C.L.","contributorId":63385,"corporation":false,"usgs":true,"family":"Braun","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":185189,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wilson, J.T.","contributorId":97489,"corporation":false,"usgs":true,"family":"Wilson","given":"J.T.","affiliations":[],"preferred":false,"id":185192,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Mahler, B.J.","contributorId":36888,"corporation":false,"usgs":true,"family":"Mahler","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":185187,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":6634,"text":"fs11697 - 1997 - Agricultural chemicals in Iowa's ground water, 1982-95: What are the trends?","interactions":[],"lastModifiedDate":"2019-12-04T16:28:24","indexId":"fs11697","displayToPublicDate":"1998-09-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"116-97","title":"Agricultural chemicals in Iowa's ground water, 1982-95: What are the trends?","docAbstract":"<p>The Iowa Department of Natural Resources. Geological Survey Bureau: the University of Iowa Hygienic Laboratory; and the U.S. Geological Survey (USGS) have been working together to address this question. As part of the Iowa Ground-Water Monitoring Program (IGWM). water samples have been collected from selected Iowa municipal wells since 1982. An examination of this data identified two trends: (1) concentrations of atrazine in Iowa's ground water generally were decreasing over time, and (2) concentrations of metolachlor generally were increasing. Continuing ground-water sampling can determine if these trends represent long-term changes in chemical concentrations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs11697","usgsCitation":"Koplin, D.W., Hallberg, G., Sneck-Fahrer, D.A., and Libra, R., 1997, Agricultural chemicals in Iowa's ground water, 1982-95: What are the trends?: U.S. Geological Survey Fact Sheet 116-97, 3 p., https://doi.org/10.3133/fs11697.","productDescription":"3 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology 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,{"id":24872,"text":"ofr97865 - 1997 - Data related to contaminant distribution at the Beatty, Nevada and Richland, Washington low-level radioactive waste disposal sites","interactions":[],"lastModifiedDate":"2012-02-02T00:08:24","indexId":"ofr97865","displayToPublicDate":"1998-09-01T00:00:00","publicationYear":"1997","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":"97-865","title":"Data related to contaminant distribution at the Beatty, Nevada and Richland, Washington low-level radioactive waste disposal sites","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr97865","issn":"0094-9140","usgsCitation":"Wilshire, H.G., and Friedman, I., 1997, Data related to contaminant distribution at the Beatty, Nevada and Richland, Washington low-level radioactive waste disposal sites: U.S. Geological Survey Open-File Report 97-865, 30 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr97865.","productDescription":"30 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":157564,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0865/report-thumb.jpg"},{"id":53864,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0865/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b562","contributors":{"authors":[{"text":"Wilshire, H. G.","contributorId":36125,"corporation":false,"usgs":false,"family":"Wilshire","given":"H.","middleInitial":"G.","affiliations":[],"preferred":false,"id":192718,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friedman, Irving","contributorId":90664,"corporation":false,"usgs":true,"family":"Friedman","given":"Irving","email":"","affiliations":[],"preferred":false,"id":192719,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221636,"text":"70221636 - 1997 - Upper Eocene sequence stratigraphy and the Absecon Inlet Formation, New Jersey Coastal Plain","interactions":[],"lastModifiedDate":"2021-06-25T20:32:04.480042","indexId":"70221636","displayToPublicDate":"1998-08-01T15:22:29","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5905,"text":"Proceedings of the Ocean Drilling Program: Scientific Results","active":true,"publicationSubtype":{"id":10}},"title":"Upper Eocene sequence stratigraphy and the Absecon Inlet Formation, New Jersey Coastal Plain","docAbstract":"<p>We evaluate the age, benthic biofacies, and sequence stratigraphy of thick and well-recovered upper Eocene sediments from the New Jersey Coastal Plain. These strata are herein defined as a lithostratigraphic unit and named the Absecon Inlet Formation. The formation is divided into upper and lower portions. At its type locality in the Atlantic City borehole, the lower portion of the Absecon Inlet Formation consists of 171 ft (52 m) of glauconitic silts and silty clays and is assigned to calcareous nannoplankton Zone NP 19/20 (late Eocene). At the ACGS#4 borehole, the type locality for its upper portion, the formation consists of slightly sandy clays and is assigned to Zone NP 21 (late Eocene to earliest Oligocene). The continuous stratigraphic occurrence of <i>Hantkenina</i> spp. in these sediments is evidence of an Eocene age for the upper portion of the Absecon Inlet Formation. Benthic foraminiferal analysis reveals five biofacies in the Absecon Inlet Formation, three of which can be related to paleowater depth: a <i>Siphonina</i> biofacies inhabited water depths of 75 ± 25 m; a <i>Cibicidoides</i> biofacies inhabited water depths of 100 ± 30 m; and a <i>Globobulimina</i> biofacies inhabited water depths of 125 ± 30 m. In addition, a <i>Gyroidinoides</i> biofacies occurs only within transgressive systems tracts. A <i>Bulimina</i> <i>jacksonensis</i> biofacies is believed to be related to a circum-Atlantic paleoceanographic event unrelated to depth changes on the shelf. Gamma-log, lithologic, and faunal/floral data are used to interpret the sequence stratigraphic architecture of the Absecon Inlet Formation. We conclude that the timing of unconformities (sequence boundaries) and maximum flooding surfaces within the Absecon Inlet Formation is consistent with the eustatic record of Exxon and the global δ<sup>18</sup>O record.</p>","language":"English","publisher":"Ocean Drilling Program","doi":"10.2973/odp.proc.sr.150X.331.1997","usgsCitation":"Browning, J.V., Miller, K.G., and Bybell, L.M., 1997, Upper Eocene sequence stratigraphy and the Absecon Inlet Formation, New Jersey Coastal Plain: Proceedings of the Ocean Drilling Program: Scientific Results, v. 150X, p. 243-266, https://doi.org/10.2973/odp.proc.sr.150X.331.1997.","productDescription":"23 p.","startPage":"243","endPage":"266","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":488111,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"http://doi.org/10.2973/odp.proc.sr.150x.331.1997","text":"Publisher Index Page"},{"id":386757,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Jersey","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.99703979492188,\n              40.225024210604964\n            ],\n            [\n              -74.7125244140625,\n              40.143189742924406\n            ],\n            [\n              -75.06546020507812,\n              39.845449231287226\n            ],\n            [\n              -75.06271362304688,\n              39.58558227224178\n            ],\n            [\n              -75.10940551757812,\n              39.23650795487107\n            ],\n            [\n              -74.88693237304688,\n              39.15881700964971\n            ],\n            [\n              -74.99404907226562,\n              38.91561302513129\n            ],\n            [\n              -74.86495971679688,\n              38.91133881927712\n            ],\n            [\n              -74.46258544921875,\n              39.29604824402406\n            ],\n            [\n              -74.20028686523438,\n              39.561235736324825\n            ],\n            [\n              -74.0423583984375,\n              39.774769485295465\n            ],\n            [\n              -73.99703979492188,\n              40.225024210604964\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"150X","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Browning, James V.","contributorId":22635,"corporation":false,"usgs":true,"family":"Browning","given":"James","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":818295,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Kenneth G.","contributorId":14260,"corporation":false,"usgs":true,"family":"Miller","given":"Kenneth","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":818296,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bybell, Laurel M. 0000-0002-4760-7542 lbybell@usgs.gov","orcid":"https://orcid.org/0000-0002-4760-7542","contributorId":1760,"corporation":false,"usgs":true,"family":"Bybell","given":"Laurel","email":"lbybell@usgs.gov","middleInitial":"M.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":818297,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70220144,"text":"70220144 - 1997 - Variations in pore-water quality, mineralogy, and sedimentary texture of clay-silts in the lower Miocene Kirkwood Formation, Atlantic City, New Jersey","interactions":[],"lastModifiedDate":"2021-04-21T14:20:05.203383","indexId":"70220144","displayToPublicDate":"1998-08-01T08:59:47","publicationYear":"1997","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Variations in pore-water quality, mineralogy, and sedimentary texture of clay-silts in the lower Miocene Kirkwood Formation, Atlantic City, New Jersey","docAbstract":"<p>Properties of and pore-water solute chemistry in confining units in the New Jersey Coastal Plain were studied to determine whether leakage of solute-enriched pore water from confining units affects regional aquifer-water chemistry, which ultimately may result in aquifer waters with high sodium and bicarbonate concentrations. Pore-water samples collected from a continuously cored borehole in the lower Miocene Kirkwood Formation at Atlantic City, NJ, were analyzed: 15 samples were obtained from clay-silt confining-unit sediments, and four samples were from silt interbeds in the sand of the major confined aquifer in the region, the Atlantic City 800-ft sand. The samples were analyzed to assess interrelations among mineralogy, texture, fluidretention properties, sediment chemistry, and pore-water chemistry, and to document the scale of variation in these properties. </p><p>Linear regressions were developed to describe the relations of constituents dissolved in 14 pore-water samples collected from the lower confining unit overlying the Atlantic City 800-ft sand and from the silt interbeds in the upper sand unit of the Atlantic City 800-ft sand. The regressions were for concentrations of magnesium and calcium (m = 0.27, R2 = 0.99); concentrations of sodium and the sum of calcium and magnesium (m = 0.17, R<sup>2</sup> = 0.92); concentrations of sulfate and the sum of calcium and magnesium (m = 1.14, R<sup>2</sup> = 0.99); and concentrations of sodium and sulfate (m = 0.14, R<sup>2</sup> = 0.89). The percentage of fine sand was greatest in the shallowest sampled interval, where pore-water concentrations of calcium, magnesium, and sulfate were greatest. </p><p>The pore-water samples were of three distinct water-quality types (hydrogeochemical facies): a calcium-sulfate type, a mixed calcium-sodium-sulfate-chloride-bicarbonate type, and a sodium-sulfate-bicarbonate-chloride type. The first two types were found only in the lower confining unit; the third type was found only in the composite confining unit underlying the Atlantic City 800-ft sand. Each of these hydrogeochemical facies generally is found within distinct intervals over a range of tens of feet in the core. </p><p>Krige estimates of pore-water–constituent variations with depth were made by using only the analytical results for the 14 samples from the lower confining unit overlying the Atlantic City 800-ft sand and the silt interbeds in the upper sand unit of the Atlantic City 800-ft sand. Geostatistical analysis of the pore-water–quality data generally resulted in two types of semivariograms. One semivariogram type best fits concentration trends with depth for calcium, magnesium, strontium, sodium, sulfate, and specific conductance; lithium and chloride may also fit this semivariogram type. The other semivariogram type best fits concentration trends with depth for silica, cation exchange capacity, and dissolved inorganic carbon. The scale of variation of the concentrations and properties is indicated by the maximum lag autocorrelation distance of the theoretical semivariograms (the range) and ranged from 44 to 110 ft (13.4–33.5 m). The scale of variation of pore-water major-ion concentrations of sulfate, chloride, calcium, and magnesium alone is on the order of 65–70 ft (19.8–21.3 m). The semivariograms for all pore-water constituents except silica have significant variance at the smallest lag distance, indicating that the constituent concentration varied over a larger scale than the sampling interval. </p><p>The dominant exchangeable cation in the sediment is calcium. Cation exchange reactions do not appear to be the dominant process in the sediments of the lower confining unit above the Atlantic City 800-ft sand, because a linear correlation exists between the concentration of sodium and the sum of calcium and magnesium concentrations in the pore water; concentrations of all these constituents increase in the upward flow direction, and the ratio of sodium to chloride in the pore water is about 1.0. </p><p>Two significant principal components explained 82.5% of the total variation in pore-water solute chemistry. Principal component 1 represents about 53% of the variation in pore-water quality and includes calcium, magnesium, sulfate, strontium, and lithium. Coupled chemical processes in the confining units, such as incongruent dissolution of carbonate and other mineral phases or redox transformations of sulfur, likely explain the covariance of these constituents. Principal component 2 represents about 30% of the variation and includes sodium, dissolved inorganic carbon, and chloride. Covariance of sodium and chloride probably is caused by the presence of residual seawater.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Leg 150X-Scientific results: Island Beach, Atlantic City and Cape May sites, New Jersey coastal plain","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"Ocean Drilling Project","doi":"10.2973/odp.proc.sr.150X.321.1997","usgsCitation":"Pucci, A., Szabo, Z., and Owens, J., 1997, Variations in pore-water quality, mineralogy, and sedimentary texture of clay-silts in the lower Miocene Kirkwood Formation, Atlantic City, New Jersey, <i>in</i> Leg 150X-Scientific results: Island Beach, Atlantic City and Cape May sites, New Jersey coastal plain, p. 317-341, https://doi.org/10.2973/odp.proc.sr.150X.321.1997.","productDescription":"25 p.","startPage":"317","endPage":"341","costCenters":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"links":[{"id":385249,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Jersey","city":"Atlantic City","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.94073486328125,\n              40.390488829277956\n            ],\n            [\n              -74.4873046875,\n              40.42813291388417\n            ],\n            [\n              -75.27008056640625,\n              39.87391156801293\n            ],\n            [\n              -75.58319091796875,\n              39.631076770083666\n            ],\n            [\n              -74.70703125,\n              39.059716474034666\n            ],\n            [\n              -74.080810546875,\n              39.57817336212527\n            ],\n            [\n              -73.94073486328125,\n              40.390488829277956\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Pucci, A. A.","contributorId":74410,"corporation":false,"usgs":false,"family":"Pucci","given":"A. A.","affiliations":[],"preferred":false,"id":814587,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Szabo, Zoltan 0000-0002-0760-9607 zszabo@usgs.gov","orcid":"https://orcid.org/0000-0002-0760-9607","contributorId":138827,"corporation":false,"usgs":true,"family":"Szabo","given":"Zoltan","email":"zszabo@usgs.gov","affiliations":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"preferred":true,"id":814588,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Owens, James P.","contributorId":9691,"corporation":false,"usgs":true,"family":"Owens","given":"James P.","affiliations":[],"preferred":false,"id":814589,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":6942,"text":"fs19597 - 1997 - Unit-area loads of suspended sediment, suspended solids and total phosphorus from small watersheds in Wisconsin","interactions":[],"lastModifiedDate":"2015-09-28T15:25:18","indexId":"fs19597","displayToPublicDate":"1998-08-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"195-97","title":"Unit-area loads of suspended sediment, suspended solids and total phosphorus from small watersheds in Wisconsin","docAbstract":"<p>Watershed planners in the Wisconsin Department of Natural Resources (WDNR) and in Wisconsin county governments use estimates of loads of total solids and total phosphorus in streams for numerous management purposes. A few examples of these are to establish load reduction goals, to estimate the relative magnitude of nonpoint sources compared to point sources, and to estimate phosphorus loads to lakes. Solids and phosphorus are two of the most common nonpoint contaminants resulting from agricultural activity. Loads can be estimated either by monitoring the water quantity and water quality in a watershed or by modeling those same factors. Monitoring is the most accurate method for load estimation, but it is also time consuming and expensive. A simple method of estimating loads of chemical constituents or suspended solids in a watershed is to use unit-area loads that have been calculated from monitored data to estimate loads in watersheds where monitoring data are not available. A \"unit-area load\" is defined as the mass of a particular constituent transported by a stream, divided by the drainage area of the watershed.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs19597","usgsCitation":"Corsi, S., Graczyk, D., Owens, D., and Bannerman, R.T., 1997, Unit-area loads of suspended sediment, suspended solids and total phosphorus from small watersheds in Wisconsin: U.S. Geological Survey Fact Sheet 195-97, 3 p., https://doi.org/10.3133/fs19597.","productDescription":"3 p.","numberOfPages":"3","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science 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