{"pageNumber":"409","pageRowStart":"10200","pageSize":"25","recordCount":36991,"records":[{"id":31960,"text":"ofr96199 - 1996 - Plan for assessment of the occurrence, status, and distribution of volatile organic compounds in aquifers of the United States","interactions":[],"lastModifiedDate":"2012-02-02T00:09:17","indexId":"ofr96199","displayToPublicDate":"1996-12-01T00:00:00","publicationYear":"1996","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":"96-199","title":"Plan for assessment of the occurrence, status, and distribution of volatile organic compounds in aquifers of the United States","docAbstract":"The occurrence of volatile organic compounds (VOCs) in water is of national concern because of their relatively high aqueous solubility, mobility, and persistence, because many are known or suspected carcinogens, because of their widespread use, and because they have been found in drinking-water supplies. Because of this national concern, VOCs were selected for National investigation (hereafter termed "National Synthesis") by the U.S. Geological Survey's National Water-Quality Assessment (NAWQA) Program in 1994. The broad goals of this National Synthesis are to: (1) describe current water- quality conditions with respect to VOCs; (2) define trends, or lack of trends, in VOCs in surface and ground water; and (3) identify, describe, and explain causal relations among the occurrence and distribution of VOCs in surface water and ground water, and natural and human factors. The National Synthesis of VOCs in ground water has three objectives: (1) to describe their occurrence, status, and distribution; (2) to determine relations among VOCs in shallow ground water and natural and human factors; and (3) to determine, compare, and contrast the occurrence, transformation, transport, and fate of selected VOCs in the hydrologic cycle for several regionally or nationally important aquifer systems. The description of VOC occurrence, status, and distribution in ground water focuses on major aquifers of the United States. Occurrence describes the presence or absence of VOCs, their frequency of occurrence, and their ranges of concentrations. Status compares the concentrations of VOCs detected in relation to water-quality regulations or advisories, such as Maximum Contaminant Levels, Proposed Maximum Contaminant Levels, Maximum Contaminant Level Goals, and Health Advisories. Distribution describes the variability of VOCs in ground water, areally and by depth. This report describes the study design for conducting such an assessment. The assessment focuses on aquifers, or parts of aquifers, that are currently used or have the potential to be used as sources of water supplies, using data collected as part of local, State, and Federal ground-water monitoring programs since 1985. Assessment by aquifer and comparison of results among aquifers will be completed for those aquifers for which adequate spatial or depth-related data are available. Assessment of VOCs in aquifers also will be completed at regional and national scales. A set of criteria for well-network design, well construction, sample-collection methods, and methods of laboratory analysis must be met before VOC data are used for assessment. An appropriate well-network design will provide a generally unbiased, random, equal-area distribution of sampling sites throughout the aquifer, or part of the aquifer, of interest. Well-construction information must be sufficient to ensure that the hydrogeologic unit (or units) represented by the water level measured and the hydrologic unit (or units) contributing water to the well are known. In addition, the well construction and pumping equipment in the well need to be of a type that are not likely to affect concentrations of VOCs in the water sample. VOC data will be considered suitable for use in the occurrence assessment if nationally accepted methods for collection and analysis were used and if the quantitation level for VOC analytes was less than about 5 micrograms per liter; laboratory analysis was done by a laboratory certified by the U.S. Environ- mental Protection Agency; and the sample was collected from untreated (raw) water at or near the well head before being held in a pressure tank or holding tank.","language":"ENGLISH","doi":"10.3133/ofr96199","usgsCitation":"Lapham, W., and Tadayon, S., 1996, Plan for assessment of the occurrence, status, and distribution of volatile organic compounds in aquifers of the United States: U.S. Geological Survey Open-File Report 96-199, 44 p. , https://doi.org/10.3133/ofr96199.","productDescription":"44 p. ","costCenters":[],"links":[{"id":163449,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0199/report-thumb.jpg"},{"id":60117,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0199/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6856b2","contributors":{"authors":[{"text":"Lapham, W.W.","contributorId":36583,"corporation":false,"usgs":true,"family":"Lapham","given":"W.W.","email":"","affiliations":[],"preferred":false,"id":207366,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tadayon, Saeid stadayon@usgs.gov","contributorId":2928,"corporation":false,"usgs":true,"family":"Tadayon","given":"Saeid","email":"stadayon@usgs.gov","affiliations":[],"preferred":true,"id":207365,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24703,"text":"ofr96349 - 1996 - Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1994 through March 1996","interactions":[],"lastModifiedDate":"2012-02-02T00:08:23","indexId":"ofr96349","displayToPublicDate":"1996-12-01T00:00:00","publicationYear":"1996","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":"96-349","title":"Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1994 through March 1996","docAbstract":"This report describes the status of ground-water resources at U.S. Navy Support Facility, Diego Garcia. Data presented are from January 1994 through March 1996, with a focus on data from January through March 1996 (first quarter of 1996). A complete database of ground-water withdrawals and chloride-concentration records since 1985 is maintained by the U.S. Geological Survey. Cumulative rainfall for January through March 1996 was about 30 inches, which is 9 percent less than the mean cumulative rainfall of about 33 inches for January through March. The period January through February is the end of the annual wet season, while March marks the start of the annual dry season. Ground-water withdrawal during January through March 1996 averaged 970,300 gallons per day. Withdrawal for the same 3 months in 1995 averaged 894,600 gallons per day. With- drawal patterns during the first quarter of 1996 did not change significantly since 1991, with the Cantonment and Air Operations areas supplying about 99 percent of total islandwide pumpage. At the end of March 1996, the chloride concentration of water from the elevated tanks at Cantonment and Air Operations were 47 and 80 milligrams per liter, respectively. The chloride data from all five production areas showed no significant upward or downward trends throughout the first quarter of 1996. Potable levels of chloride concentrations have been maintained by adjusting individual pumping rates, and also because of the absence of long-term droughts. Chloride concentration of ground water in monitoring wells at Cantonment and Air Operations also showed no significant trends throughout the first quarter of 1996. Chloride concentrations have been about the same since the last quarter of 1995. A fuel-pipeline leak at Air Operations in May 1991 decreased total islandwide withdrawals by 15 percent. This lost pumping capacity is being offset by increased pumpage at Cantonment. Six wells do not contribute to the water supply because they are being used to hydraulically divert fuel migration away from water-supply wells by a program of ground-water withdrawal and injection.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr96349","issn":"0094-9140","usgsCitation":"Torikai, J., 1996, Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1994 through March 1996: U.S. Geological Survey Open-File Report 96-349, v, 43 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr96349.","productDescription":"v, 43 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":157560,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0349/report-thumb.jpg"},{"id":53736,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0349/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e486fe4b07f02db50ca07","contributors":{"authors":[{"text":"Torikai, J.D.","contributorId":93926,"corporation":false,"usgs":true,"family":"Torikai","given":"J.D.","affiliations":[],"preferred":false,"id":192406,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24745,"text":"ofr96204 - 1996 - U.S. Geological Survey National Computer Technology Meeting; programs and abstracts, Rancho Mirage, California May 19-23, 1996","interactions":[],"lastModifiedDate":"2016-03-21T14:16:59","indexId":"ofr96204","displayToPublicDate":"1996-12-01T00:00:00","publicationYear":"1996","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":"96-204","title":"U.S. Geological Survey National Computer Technology Meeting; programs and abstracts, Rancho Mirage, California May 19-23, 1996","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr96204","issn":"0094-9140","usgsCitation":"1996, U.S. Geological Survey National Computer Technology Meeting; programs and abstracts, Rancho Mirage, California May 19-23, 1996: U.S. Geological Survey Open-File Report 96-204, xiv, 65 p., https://doi.org/10.3133/ofr96204.","productDescription":"xiv, 65 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":158185,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0204/report-thumb.jpg"},{"id":53776,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0204/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696219","contributors":{"compilers":[{"text":"Shank, Kim L.","contributorId":167698,"corporation":false,"usgs":false,"family":"Shank","given":"Kim","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":623165,"contributorType":{"id":3,"text":"Compilers"},"rank":1}]}}
,{"id":21833,"text":"ofr9690 - 1996 - Geology of Upper Cretaceous and Paleocene gas-bearing rocks, Wind River Basin, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:07:49","indexId":"ofr9690","displayToPublicDate":"1996-11-01T00:00:00","publicationYear":"1996","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":"96-90","title":"Geology of Upper Cretaceous and Paleocene gas-bearing rocks, Wind River Basin, Wyoming","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr9690","issn":"0566-8174","usgsCitation":"Johnson, R.C., Finn, T., Keefer, W.R., and Szmajter, R., 1996, Geology of Upper Cretaceous and Paleocene gas-bearing rocks, Wind River Basin, Wyoming: U.S. Geological Survey Open-File Report 96-90, 120 p., 3 over-size sheets, :ill., maps ;28 cm., https://doi.org/10.3133/ofr9690.","productDescription":"120 p., 3 over-size sheets, :ill., maps ;28 cm.","costCenters":[],"links":[{"id":153578,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0090/report-thumb.jpg"},{"id":19388,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0090/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19389,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0090/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19390,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0090/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":51321,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0090/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683acb","contributors":{"authors":[{"text":"Johnson, R. C. 0000-0002-6197-5165","orcid":"https://orcid.org/0000-0002-6197-5165","contributorId":101621,"corporation":false,"usgs":true,"family":"Johnson","given":"R.","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":185886,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Finn, T.M. 0000-0001-6396-9351","orcid":"https://orcid.org/0000-0001-6396-9351","contributorId":65495,"corporation":false,"usgs":true,"family":"Finn","given":"T.M.","affiliations":[],"preferred":false,"id":185884,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Keefer, W. R.","contributorId":21538,"corporation":false,"usgs":true,"family":"Keefer","given":"W.","middleInitial":"R.","affiliations":[],"preferred":false,"id":185883,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Szmajter, R.J.","contributorId":87573,"corporation":false,"usgs":true,"family":"Szmajter","given":"R.J.","affiliations":[],"preferred":false,"id":185885,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":24713,"text":"ofr9619 - 1996 - DECCON software to decompress NOAA IMGMAP compressed imagery and convert to common image file formats","interactions":[],"lastModifiedDate":"2012-02-02T00:08:24","indexId":"ofr9619","displayToPublicDate":"1996-11-01T00:00:00","publicationYear":"1996","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":"96-19","title":"DECCON software to decompress NOAA IMGMAP compressed imagery and convert to common image file formats","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr9619","issn":"0094-9140","usgsCitation":"Townsley, B., and Stumpf, R., 1996, DECCON software to decompress NOAA IMGMAP compressed imagery and convert to common image file formats: U.S. Geological Survey Open-File Report 96-19, ii, 19 p. ;28 cm., https://doi.org/10.3133/ofr9619.","productDescription":"ii, 19 p. ;28 cm.","costCenters":[],"links":[{"id":157521,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0019/report-thumb.jpg"},{"id":53744,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0019/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ead3","contributors":{"authors":[{"text":"Townsley, Bill","contributorId":63422,"corporation":false,"usgs":true,"family":"Townsley","given":"Bill","email":"","affiliations":[],"preferred":false,"id":192420,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stumpf, Rick","contributorId":92295,"corporation":false,"usgs":true,"family":"Stumpf","given":"Rick","affiliations":[],"preferred":false,"id":192421,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24781,"text":"ofr96260 - 1996 - Earthquakes, minerals, and me with the USGS, 1942-1995","interactions":[],"lastModifiedDate":"2012-02-02T00:08:11","indexId":"ofr96260","displayToPublicDate":"1996-11-01T00:00:00","publicationYear":"1996","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":"96-260","title":"Earthquakes, minerals, and me with the USGS, 1942-1995","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96260","issn":"0094-9140","usgsCitation":"Wallace, R.E., and Scott, S., 1996, Earthquakes, minerals, and me with the USGS, 1942-1995: U.S. Geological Survey Open-File Report 96-260, vi, 201 p.; 28 cm.; available in print, djvu, and pdf formats, https://doi.org/10.3133/ofr96260.","productDescription":"vi, 201 p.; 28 cm.; available in print, djvu, and pdf formats","costCenters":[{"id":648,"text":"Western Earthquake Hazards","active":false,"usgs":true}],"links":[{"id":1812,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://quake.wr.usgs.gov/research/history/","linkFileType":{"id":5,"text":"html"}},{"id":156111,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9327,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1996/of96-260/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db62939b","contributors":{"authors":[{"text":"Wallace, Robert E.","contributorId":15570,"corporation":false,"usgs":true,"family":"Wallace","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":192556,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, Stanley","contributorId":76350,"corporation":false,"usgs":true,"family":"Scott","given":"Stanley","email":"","affiliations":[],"preferred":false,"id":192557,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21834,"text":"ofr9639 - 1996 - Geology, alteration, and rock and water chemistry of the Iron, Alum, and Bitter Creek areas, upper Alamosa River, southwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:07:49","indexId":"ofr9639","displayToPublicDate":"1996-11-01T00:00:00","publicationYear":"1996","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":"96-39","title":"Geology, alteration, and rock and water chemistry of the Iron, Alum, and Bitter Creek areas, upper Alamosa River, southwestern Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr9639","issn":"0566-8174","usgsCitation":"Bove, D.J., Wilson, A., Barry, T., Hon, K., Kurtz, J., Van Loenen, R.E., and Calkin, W., 1996, Geology, alteration, and rock and water chemistry of the Iron, Alum, and Bitter Creek areas, upper Alamosa River, southwestern Colorado: U.S. Geological Survey Open-File Report 96-39, 34 p., 10 over-size sheets, iii, 34 leaves :ill., maps ;28 cm., https://doi.org/10.3133/ofr9639.","productDescription":"34 p., 10 over-size sheets, iii, 34 leaves :ill., maps ;28 cm.","costCenters":[],"links":[{"id":153596,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0039/report-thumb.jpg"},{"id":19391,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0039/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19392,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0039/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19393,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0039/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19394,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0039/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19395,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0039/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19396,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0039/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19397,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0039/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19398,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0039/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19399,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0039/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19400,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0039/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":51322,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0039/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c73c","contributors":{"authors":[{"text":"Bove, Dana J. dbove@usgs.gov","contributorId":4855,"corporation":false,"usgs":true,"family":"Bove","given":"Dana","email":"dbove@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":185887,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, A.B. 0000-0002-9737-2614","orcid":"https://orcid.org/0000-0002-9737-2614","contributorId":63818,"corporation":false,"usgs":true,"family":"Wilson","given":"A.B.","affiliations":[],"preferred":false,"id":185890,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barry, T.H.","contributorId":69844,"corporation":false,"usgs":true,"family":"Barry","given":"T.H.","email":"","affiliations":[],"preferred":false,"id":185891,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hon, Ken","contributorId":19163,"corporation":false,"usgs":true,"family":"Hon","given":"Ken","affiliations":[],"preferred":false,"id":185888,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kurtz, Jeffrey","contributorId":32401,"corporation":false,"usgs":true,"family":"Kurtz","given":"Jeffrey","affiliations":[],"preferred":false,"id":185889,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Van Loenen, R. E.","contributorId":99130,"corporation":false,"usgs":true,"family":"Van Loenen","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":185893,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Calkin, W.S.","contributorId":92537,"corporation":false,"usgs":true,"family":"Calkin","given":"W.S.","email":"","affiliations":[],"preferred":false,"id":185892,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":21685,"text":"ofr96129 - 1996 - Comparison of estimated and observed stormwater runoff for fifteen watersheds in west-central Florida, using five common design techniques","interactions":[],"lastModifiedDate":"2012-02-02T00:07:59","indexId":"ofr96129","displayToPublicDate":"1996-11-01T00:00:00","publicationYear":"1996","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":"96-129","title":"Comparison of estimated and observed stormwater runoff for fifteen watersheds in west-central Florida, using five common design techniques","docAbstract":"Hydrologists use several traditional techniques for estimating peak discharges and runoff volumes from ungaged watersheds. However, applying these techniques to watersheds in west-central Florida requires that empirical relationships be extrapolated beyond tested ranges. As a result there is some uncertainty as to their accuracy. Sixty-six storms in 15 west-central Florida watersheds were modeled using (1) the rational method, (2) the U.S. Geological Survey regional regression equations, (3) the Natural Resources Conservation Service (formerly the Soil Conservation Service) TR-20 model, (4) the Army Corps of Engineers HEC-1 model, and (5) the Environmental Protection Agency SWMM model. The watersheds ranged between fully developed urban and undeveloped natural watersheds. Peak discharges and runoff volumes were estimated using standard or recommended methods for determining input parameters. All model runs were uncalibrated and the selection of input parameters was not influenced by observed data. The rational method, only used to calculate peak discharges, overestimated 45 storms, underestimated 20 storms and estimated the same discharge for 1 storm. The mean estimation error for all storms indicates the method overestimates the peak discharges. Estimation errors were generally smaller in the urban watersheds and larger in the natural watersheds. The U.S. Geological Survey regression equations provide peak discharges for storms of specific recurrence intervals. Therefore, direct comparison with observed data was limited to sixteen observed storms that had precipitation equivalent to specific recurrence intervals. The mean estimation error for all storms indicates the method overestimates both peak discharges and runoff volumes. Estimation errors were smallest for the larger natural watersheds in Sarasota County, and largest for the small watersheds located in the eastern part of the study area. The Natural Resources Conservation Service TR-20 model, overestimated peak discharges for 45 storms and underestimated 21 storms, and overestimated runoff volumes for 44 storms and underestimated 22 storms. The mean estimation error for all storms modeled indicates that the model overestimates peak discharges and runoff volumes. The smaller estimation errors in both peak discharges and runoff volumes were for storms occurring in the urban watersheds, and the larger errors were for storms occurring in the natural watersheds. The HEC-1 model overestimated peak discharge rates for 55 storms and underestimated 11 storms. Runoff volumes were overestimated for 44 storms and underestimated for 22 storms using the Army Corps of Engineers HEC-1 model. The mean estimation error for all the storms modeled indicates that the model overestimates peak discharge rates and runoff volumes. Generally, the smaller estimation errors in peak discharges were for storms occurring in the urban watersheds, and the larger errors were for storms occurring in the natural watersheds. Estimation errors in runoff volumes; however, were smallest for the 3 natural watersheds located in the southernmost part of Sarasota County. The Environmental Protection Agency Storm Water Management model produced similar peak discharges and runoff volumes when using both the Green-Ampt and Horton infiltration methods. Estimated peak discharge and runoff volume data calculated with the Horton method was only slightly higher than those calculated with the Green-Ampt method. The mean estimation error for all the storms modeled indicates the model using the Green-Ampt infiltration method overestimates peak discharges and slightly underestimates runoff volumes. Using the Horton infiltration method, the model overestimates both peak discharges and runoff volumes. The smaller estimation errors in both peak discharges and runoff volumes were for storms occurring in the five natural watersheds in Sarasota County with the least amount of impervious cover and the lowest slopes. The largest er","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-file Reports Section [distributor],","doi":"10.3133/ofr96129","issn":"0566-8174","usgsCitation":"Trommer, J., Loper, J., Hammett, K., and Bowman, G., 1996, Comparison of estimated and observed stormwater runoff for fifteen watersheds in west-central Florida, using five common design techniques: U.S. Geological Survey Open-File Report 96-129, viii, 120 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr96129.","productDescription":"viii, 120 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":154904,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1291,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr96-129/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae35f","contributors":{"authors":[{"text":"Trommer, J.T.","contributorId":28248,"corporation":false,"usgs":true,"family":"Trommer","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":185248,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Loper, J.E.","contributorId":19965,"corporation":false,"usgs":true,"family":"Loper","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":185247,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hammett, K.M.","contributorId":59006,"corporation":false,"usgs":true,"family":"Hammett","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":185250,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bowman, Georgia","contributorId":44184,"corporation":false,"usgs":true,"family":"Bowman","given":"Georgia","email":"","affiliations":[],"preferred":false,"id":185249,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":21780,"text":"ofr96262 - 1996 - Faults, lineaments, and earthquake epicenters digital map of the Pahute Mesa 30' x 60' quadrangle, Nevada","interactions":[],"lastModifiedDate":"2022-07-15T17:53:11.688486","indexId":"ofr96262","displayToPublicDate":"1996-11-01T00:00:00","publicationYear":"1996","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":"96-262","title":"Faults, lineaments, and earthquake epicenters digital map of the Pahute Mesa 30' x 60' quadrangle, Nevada","docAbstract":"<p>This map database, identified as Faults, lineaments, and earthquake epicenters digital map of the Pahute Mesa 30' X 60' quadrangle, Nevada, has been approved for release and publication by the Director of the USGS. Although this database has been subjected to rigorous review and is substantially complete, the USGS reserves the right to revise the data pursuant to further analysis and review. Furthermore, it is released on condition that neither the USGS nor the United States Government may be held liable for any damages resulting from its authorized or unauthorized use. This digital map compilation incorporates fault, air photo lineament, and earthquake epicenter data from within the Pahute Mesa 30' by 60' quadrangle, southern Nye County, Nevada (fig. 1). The compilation contributes to the U.S. Department of Energy's Yucca Mountain Project, established to determine whether or not the Yucca Mountain site is suitable for the disposal of high-level nuclear waste. Studies of local and regional faulting and earthquake activity, including the features depicted in this compilation, are carried out to help characterize seismic hazards and tectonic processes that may be relevant to the future stability of Yucca Mountain. The Yucca Mountain site is located in the central part of the Beatty 30' by 60' quadrangle approximately 15 km south of the south edge of the Pahute Mesa quadrangle (fig. 1). The U.S. Geological Survey participates in studies of the Yucca Mountain site under Interagency Agreement DE-AI08-78ET44802. The map compilation is only available on line as a digital database in ARC/INFO ASCII (Generate) and export formats. The database can be downloaded via 'anonymous ftp' from a USGS system named greenwood.cr.usgs.gov (136.177.48.5). The files are located in a directory named /pub/open-file-reports/ofr-96-0262. This directory contains a text document named 'README.1 ST' that contains database technical and explanatory documentation, including instructions for uncompressing the bundled (tar) file. In displaying the compilation it is important to note that the map data set is considered accurate when depicted at a scale of about 1:100,000; displaying the compilation at scales significantly larger than this may result in distortions and (or) mislocations of the data.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96262","usgsCitation":"Minor, S., Vick, G.S., Carr, M.D., and Wahl, R.R., 1996, Faults, lineaments, and earthquake epicenters digital map of the Pahute Mesa 30' x 60' quadrangle, Nevada: U.S. Geological Survey Open-File Report 96-262, 13 p., https://doi.org/10.3133/ofr96262.","productDescription":"13 p.","costCenters":[],"links":[{"id":403844,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22971.htm","linkFileType":{"id":5,"text":"html"}},{"id":51280,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0262/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":1203,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1996/ofr-96-0262/","linkFileType":{"id":5,"text":"html"}},{"id":154785,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0262/report-thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Pahute Mesa 30' X 60' quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117,\n              37.5\n            ],\n            [\n              -116,\n              37.5\n            ],\n            [\n              -116,\n              37\n            ],\n            [\n              -117,\n              37\n            ],\n            [\n              -117,\n              37.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f72ba","contributors":{"authors":[{"text":"Minor, S.A.","contributorId":65047,"corporation":false,"usgs":true,"family":"Minor","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":185651,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vick, G. S.","contributorId":100010,"corporation":false,"usgs":true,"family":"Vick","given":"G.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":185652,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carr, M. D.","contributorId":51767,"corporation":false,"usgs":true,"family":"Carr","given":"M.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":185650,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wahl, R. R.","contributorId":27462,"corporation":false,"usgs":true,"family":"Wahl","given":"R.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":185649,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":23444,"text":"ofr96142 - 1996 - Use of an ultra-clean sampling technique with inductively coupled plasma-mass spectrometry to determine trace-element concentrations in water from the Kirkwood-Cohansey Aquifer system, coastal plain, New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:08:10","indexId":"ofr96142","displayToPublicDate":"1996-11-01T00:00:00","publicationYear":"1996","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":"96-142","title":"Use of an ultra-clean sampling technique with inductively coupled plasma-mass spectrometry to determine trace-element concentrations in water from the Kirkwood-Cohansey Aquifer system, coastal plain, New Jersey","docAbstract":"Water samples were collected during 1993 from 22 public supply wells screened in the Kirkwood-Cohansey aquifer system; concentrations of 18 trace elements were determined primarily by using inductively coupled plasma-mass spectrometry (ICP-MS) techniques, though graphite furnace atomic adsorption, hydride generation, and cold- vapor flameless atomic adsorption techniques were used for thallium, arsenic, and mercury, respectively, at the U.S. Geological Survey (USGS) National Water Quality Laboratory (NWQL). In addition, laboratory measurements of alkalinity and turbidity were made. The ground-water samples were collected by using ultra-clean sampling protocols developed by the USGS for collecting ground-water samples in areas with water containing low concentrations of trace elements. This technique is based on recently gained experience in sampling surface water for these elements. Field parameters (water temperature, specific conductance, pH, and dissolved-oxygen concentration) were monitored prior to sample collection. Three equipment blanks were collected to ensure that low-level trace-element contamination did not occur during sample collection. One split sample and a commercially- prepared reference standard were submitted to the NWQL o evaluate laboratory precision and accuracy, respectively. Trace-element concentrations in 10 sample splits and one equipment blank were also determined at the Rutgers University Chemistry Department laboratory. Results of the ICP-MS analyses and cold vapor flameless atomic absorption indicated that five trace elements-- cobalt, copper, lead, mercury, and nickel--were detectable in low concentrations (&lt;0.1-29 mg/L) in most of the samples from the 22 wells, and four elements--aluminum, barium, manganese and zinc--were detected in higher concentrations than the other elements (30-710 mg/L for aluminum; 4-180 mg/L for barium, manganese, and zinc). The remaining nine trace elements were present in concentrations consistently lower than the minimum reporting limit. Turbidity was low (less than 1 nephelometric turbidity unit (NTU)), indicating that the trace-element concentrations were present in the dissolved phase and ideally would be reproducible in the absence of highly variable concentrations of particulates. The concentration of lead in one sample exceeded the U.S. Environmental Protection Agency (USEPA) action level of 15 mg/L; concentrations ranged from &lt;1 to 16 mg/L. Mercury was frequently detected; concentrations ranged from &lt;0.1 to 1.1 mg/L but did not exceed the USEPA maximum contaminant level. Results of analyses of the equipment blanks indicated that samples collected by using the new ultra-clean sampling protocols were free of low-level (&lt; 1mg/L) trace-element contamination. The analysis of the split sample sent to the NWQL had a difference of 5 percent or less for all constituents except aluminum, for which the analysis had a difference of 10 percent. Results of ICP-MS analyses of split water samples sent to the Rutgers University Chemistry Department laboratory were, in general, in good agreement (within 10 percent) with those of the NWQL. Results of the analysis of the commercial standard agreed (within 5 percent) with the known concentrations of the trace elements. The quality-assurance data (three blanks, one split sample, and one standard), although not statistically evaluated because of the small data set, indicate that the measured trace-element concentrations are precise and accurate and that the samples were free of contamination at the microgram-per-liter level of contamination.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S., Earth Science Information Center, Books and Open-File Reports Section [distributor],","doi":"10.3133/ofr96142","issn":"0094-9140","usgsCitation":"Ivahnenko, T., Szabo, Z., and Hall, G., 1996, Use of an ultra-clean sampling technique with inductively coupled plasma-mass spectrometry to determine trace-element concentrations in water from the Kirkwood-Cohansey Aquifer system, coastal plain, New Jersey: U.S. Geological Survey Open-File Report 96-142, v, 37 p. :map ;28 cm., https://doi.org/10.3133/ofr96142.","productDescription":"v, 37 p. :map ;28 cm.","costCenters":[],"links":[{"id":156103,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0142/report-thumb.jpg"},{"id":52764,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0142/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604d0a","contributors":{"authors":[{"text":"Ivahnenko, Tamara 0000-0002-1124-7688 ivahnenk@usgs.gov","orcid":"https://orcid.org/0000-0002-1124-7688","contributorId":93524,"corporation":false,"usgs":true,"family":"Ivahnenko","given":"Tamara","email":"ivahnenk@usgs.gov","affiliations":[],"preferred":false,"id":190118,"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":2240,"corporation":false,"usgs":true,"family":"Szabo","given":"Zoltan","email":"zszabo@usgs.gov","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":false,"id":190116,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hall, G.S.","contributorId":8889,"corporation":false,"usgs":true,"family":"Hall","given":"G.S.","email":"","affiliations":[],"preferred":false,"id":190117,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":24629,"text":"ofr96207 - 1996 - Selected geohydrologic data from a regional aquifer-system analysis of the Northern Rocky Mountains intermontane basins in Idaho","interactions":[],"lastModifiedDate":"2013-11-15T13:33:35","indexId":"ofr96207","displayToPublicDate":"1996-11-01T00:00:00","publicationYear":"1996","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":"96-207","title":"Selected geohydrologic data from a regional aquifer-system analysis of the Northern Rocky Mountains intermontane basins in Idaho","docAbstract":"The U.S. Geological Survey began a regional aquifer-system analysis of the Northern Rocky Mountains of northern and central Idaho and western Montana in 1990. The analysis helped establish a regional framework of information for aquifers in about 70 ntermontane basins in an area of 80,000 square miles. In many areas, ground water is the only suitable source of supply, yet little information is available about this resource. Selected geohydrologic data from 1,004 wells in 19 intermontane basins in Idaho were compiled as part of the regional analysis. Data consist of basin name and well number, altitude of land surface, date of well construction, geologic unit, depth of well, diameter of casing, type of finish, top of open interval, primary use of water, date of water level measurement, water level, discharge, specific capacity, source of discharge data, type of log available, date of water-quality constituent measurement, specific conductance, pH, and temperature. A similar report for intermontane basins in Montana has been published by the U.S. Geologcial Survey in Montana. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96207","usgsCitation":"Stone, M., Parliman, D., and Schaefer, J., 1996, Selected geohydrologic data from a regional aquifer-system analysis of the Northern Rocky Mountains intermontane basins in Idaho: U.S. Geological Survey Open-File Report 96-207, iii, 30 p., https://doi.org/10.3133/ofr96207.","productDescription":"iii, 30 p.","numberOfPages":"33","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":157874,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0207/report-thumb.jpg"},{"id":53671,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0207/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","otherGeospatial":"Northern Rocky Mountains Intermontane Basins","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.24,41.99 ], [ -117.24,49.0 ], [ -111.04,49.0 ], [ -111.04,41.99 ], [ -117.24,41.99 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa58d","contributors":{"authors":[{"text":"Stone, M.A.","contributorId":9665,"corporation":false,"usgs":true,"family":"Stone","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":192282,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parliman, D. J.","contributorId":64220,"corporation":false,"usgs":true,"family":"Parliman","given":"D. J.","affiliations":[],"preferred":false,"id":192283,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schaefer, J.L.","contributorId":106160,"corporation":false,"usgs":true,"family":"Schaefer","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":192284,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":24555,"text":"ofr96314 - 1996 - Surface-water quantity and quality data, Rocky Flats environmental technology site near Denver Colorado, water years 1994-95","interactions":[],"lastModifiedDate":"2012-02-02T00:08:00","indexId":"ofr96314","displayToPublicDate":"1996-11-01T00:00:00","publicationYear":"1996","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":"96-314","title":"Surface-water quantity and quality data, Rocky Flats environmental technology site near Denver Colorado, water years 1994-95","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nInformation Services [distributor],","doi":"10.3133/ofr96314","issn":"0094-9140","usgsCitation":"Smith, M., Unruh, J., and Thompson, C., 1996, Surface-water quantity and quality data, Rocky Flats environmental technology site near Denver Colorado, water years 1994-95: U.S. Geological Survey Open-File Report 96-314, iv, 88 p. :ill. ;1996., https://doi.org/10.3133/ofr96314.","productDescription":"iv, 88 p. :ill. ;1996.","costCenters":[],"links":[{"id":155093,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0314/report-thumb.jpg"},{"id":53606,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0314/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a58e","contributors":{"authors":[{"text":"Smith, M.E.","contributorId":104525,"corporation":false,"usgs":true,"family":"Smith","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":192148,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Unruh, J.W.","contributorId":105756,"corporation":false,"usgs":true,"family":"Unruh","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":192149,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thompson, C.H.","contributorId":85987,"corporation":false,"usgs":true,"family":"Thompson","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":192147,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":31938,"text":"ofr95755 - 1996 - Quality-assurance plan for water-resources activities of the U.S. Geological Survey in Idaho","interactions":[],"lastModifiedDate":"2013-11-15T13:22:42","indexId":"ofr95755","displayToPublicDate":"1996-11-01T00:00:00","publicationYear":"1996","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":"95-755","title":"Quality-assurance plan for water-resources activities of the U.S. Geological Survey in Idaho","docAbstract":"To ensure continued confidence in its products, the Water Resources Division of the U.S. Geological Survey implemented a policy that all its scientific work be performed in accordance with a centrally managed quality-assurance program. This report establishes and documents a formal policy for current (1995) quality assurance within the Idaho District of the U.S. Geological Survey. Quality assurance is formalized by describing district  organization and operational responsibilities, documenting the district quality-assurance policies, and describing district functions. The districts conducts its work through offices in Boise, Idaho Falls, Twin Falls, Sandpoint, and at the Idaho National Engineering Laboratory. Data-collection programs and interpretive studies are conducted by two operating units, and operational and technical assistance is provided by three support units: (1) Administrative Services advisors provide guidance on various personnel issues and budget functions, (2) computer and reports advisors provide guidance in their fields, and (3) discipline specialists provide technical advice and assistance to the district and to chiefs of various projects. The district's quality-assurance plan is based on an overall policy that provides a framework for defining the precision and accuracy of collected data. The plan is supported by a series of quality-assurance policy statements that describe responsibilities for specific operations in the district's program. The operations are program planning; project planning; project implementation; review and remediation; data collection; equipment calibration and maintenance; data processing and storage; data analysis, synthesis, and interpretation; report preparation and processing; and training. Activities of the district are systematically conducted under a hierarchy of supervision an management that is designed to ensure conformance with Water Resources Division goals quality assurance. The district quality-assurance plan does not describe detailed technical activities that are commonly termed \"quality-control procedures.\" Instead, it focuses on current policies, operations, and responsibilities that are implemented at the management level. Contents of the plan will be reviewed annually and updated as programs and operations change.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95755","usgsCitation":"Packard, F.A., 1996, Quality-assurance plan for water-resources activities of the U.S. Geological Survey in Idaho: U.S. Geological Survey Open-File Report 95-755, iii, 22 p., https://doi.org/10.3133/ofr95755.","productDescription":"iii, 22 p.","numberOfPages":"25","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":161370,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0755/report-thumb.jpg"},{"id":60093,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0755/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.24,41.99 ], [ -117.24,49.0 ], [ -111.04,49.0 ], [ -111.04,41.99 ], [ -117.24,41.99 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a87e4b07f02db64eb96","contributors":{"authors":[{"text":"Packard, F. A.","contributorId":71164,"corporation":false,"usgs":true,"family":"Packard","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":207307,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22862,"text":"ofr95729 - 1996 - Reconnaissance of volatile organic compounds in the subsurface at Rutgers University, Busch Campus, Piscataway Township, New Jersey","interactions":[],"lastModifiedDate":"2019-09-26T08:16:26","indexId":"ofr95729","displayToPublicDate":"1996-11-01T00:00:00","publicationYear":"1996","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":"95-729","title":"Reconnaissance of volatile organic compounds in the subsurface at Rutgers University, Busch Campus, Piscataway Township, New Jersey","docAbstract":"During 1991-92, the U.S. Geological Survey conducted a hydrogeologic reconnaissance at a site near the Rutgers University, Busch Campus, Chemical Engineering building, C-Wing. Results of analyses of the soil-gas samples, which were collected at 43 locations, indicated the presence of volatile organic compounds, primarily carbon tetrachloride, near the C-Wing building and about 550 feet downgradient from and southwest of the C-Wing building. Concentrations of the compound in soil-gas samples were highest (2.1 ug/L (micrograms per liter)) along the southwestern wall of the C-Wing building. Ground-water samples were collected at depths as great as 55 feet from five wells and piezometers near the C-Wing building. Samples collected along the southwestern wall of the building also contained the highest concentrations of volatile organic compounds. Concentrations of carbon tetrachloride in the ground-water samples ranged from &lt; 0.35 ug/L to 3,400 ug/L, and concentrations of tetrachloro- ethylene ranged from &lt; 0.28 ug/L to 85 ug/L. Ground-water samples collected at depths of 55 feet or more from two wells located on the Rutgers University Golf Course about 2,400 feet down- gradient from the C-Wing building contained concentrations of tetrachloroethylene as great as 17.7 ug/L. Water levels measured in six wells and six piezometers indicated that the general flow direction in the shallow part of the aquifer is to the southwest of the C-Wing building. An electrical-resistivity survey was conducted by azimuthal resistivity techniques. The results of the survey were consistent with field measurements, and the dominant vertical fractures near the Busch Campus trend northeast. An electromagnetic survey was ineffective as a result of cultural interferences and could not be used to determine the hydrogeologic characteristics of the site.","language":"English","publisher":"U.S. Geological Survey ","publisherLocation":"Reston, VA","doi":"10.3133/ofr95729","issn":"0094-9140","usgsCitation":"DePaul, V.T., 1996, Reconnaissance of volatile organic compounds in the subsurface at Rutgers University, Busch Campus, Piscataway Township, New Jersey: U.S. Geological Survey Open-File Report 95-729, Report: v, 26 p. , https://doi.org/10.3133/ofr95729.","productDescription":"Report: v, 26 p. 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,{"id":24272,"text":"ofr95691 - 1996 - Digital representation of the Montana state geologic map: A contribution to the Interior Columbia River Basin Ecosystem Management Project","interactions":[],"lastModifiedDate":"2021-09-08T22:02:10.285621","indexId":"ofr95691","displayToPublicDate":"1996-11-01T00:00:00","publicationYear":"1996","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":"95-691","title":"Digital representation of the Montana state geologic map: A contribution to the Interior Columbia River Basin Ecosystem Management Project","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95691","issn":"0094-9140","usgsCitation":"Raines, G.L., and Johnson, B., 1996, Digital 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a94e4b07f02db658958","contributors":{"authors":[{"text":"Raines, G. L.","contributorId":90720,"corporation":false,"usgs":true,"family":"Raines","given":"G.","middleInitial":"L.","affiliations":[],"preferred":false,"id":191611,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, B. R.","contributorId":73995,"corporation":false,"usgs":true,"family":"Johnson","given":"B. R.","affiliations":[],"preferred":false,"id":191610,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23504,"text":"ofr96266 - 1996 - Some facts about aftershocks to large earthquakes in California","interactions":[],"lastModifiedDate":"2014-03-18T13:09:45","indexId":"ofr96266","displayToPublicDate":"1996-11-01T00:00:00","publicationYear":"1996","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":"96-266","title":"Some facts about aftershocks to large earthquakes in California","docAbstract":"<p>Earthquakes occur in clusters. After one earthquake happens, we usually see others at nearby (or identical) locations. To talk about this phenomenon, seismologists coined three terms foreshock , mainshock , and aftershock. In any cluster of earthquakes, the one with the largest magnitude is called the mainshock; earthquakes that occur before the mainshock are called foreshocks while those that occur after the mainshock are called aftershocks. A mainshock will be redefined as a foreshock if a subsequent event in the cluster has a larger magnitude.</p>\n<br/>\n<p>Aftershock sequences follow predictable patterns. That is, a sequence of aftershocks follows certain global patterns as a group, but the individual earthquakes comprising the group are random and unpredictable. This relationship between the pattern of a group and the randomness (stochastic nature) of the individuals has a close parallel in actuarial statistics. We can describe the pattern that aftershock sequences tend to follow with well-constrained equations. However, we must keep in mind that the actual aftershocks are only probabilistically described by these equations. Once the parameters in these equations have been estimated, we can determine the probability of aftershocks occurring in various space, time and magnitude ranges as described below.</p>\n<br/>\n<p>Clustering of earthquakes usually occurs near the location of the mainshock. The stress on the mainshock's fault changes drastically during the mainshock and that fault produces most of the aftershocks. This causes a change in the regional stress, the size of which decreases rapidly with distance from the mainshock. Sometimes the change in stress caused by the mainshock is great enough to trigger aftershocks on other, nearby faults. While there is no hard \"cutoff\" distance beyond which an earthquake is totally incapable of triggering an aftershock, the vast majority of aftershocks are located close to the mainshock. As a rule of thumb, we consider earthquakes to be aftershocks if they are located within a characteristic distance from the mainshock. This distance is usually taken to be one or two times the length of the fault rupture associated with the mainshock. For example, if the mainshock ruptured a 100 km length of a fault, subsequent earthquakes up to 100-200 km away from the mainshock rupture would be considered aftershocks. The fault rupture length was approximately 15 km in the 1994 Northridge earthquake, and 430 km in the great 1906 earthquake.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96266","issn":"0094-9140","usgsCitation":"Jones, L.M., and Reasenberg, P.A., 1996, Some facts about aftershocks to large earthquakes in California: U.S. Geological Survey Open-File Report 96-266, 4 p., https://doi.org/10.3133/ofr96266.","productDescription":"4 p.","numberOfPages":"4","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":284169,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1570,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1996/0266/","linkFileType":{"id":5,"text":"html"}},{"id":52793,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0266/pdf/of96-266.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.41,32.53 ], [ -124.41,42.01 ], [ -114.13,42.01 ], [ -114.13,32.53 ], [ -124.41,32.53 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e9e4b07f02db5e933f","contributors":{"authors":[{"text":"Jones, Lucile M. jones@usgs.gov","contributorId":1014,"corporation":false,"usgs":true,"family":"Jones","given":"Lucile","email":"jones@usgs.gov","middleInitial":"M.","affiliations":[{"id":508,"text":"Office of the AD Hazards","active":true,"usgs":true}],"preferred":true,"id":190215,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reasenberg, Paul A.","contributorId":35760,"corporation":false,"usgs":true,"family":"Reasenberg","given":"Paul","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":190216,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24119,"text":"ofr9626 - 1996 - Preliminary geologic map of the Paleozoic rocks in the Wildcat Wash SE and Wildcat Wash SW quadrangles, Lincoln and Clark counties, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:08:12","indexId":"ofr9626","displayToPublicDate":"1996-11-01T00:00:00","publicationYear":"1996","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":"96-26","title":"Preliminary geologic map of the Paleozoic rocks in the Wildcat Wash SE and Wildcat Wash SW quadrangles, Lincoln and Clark counties, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr9626","issn":"0094-9140","usgsCitation":"Page, W.R., and Pampeyan, E., 1996, Preliminary geologic map of the Paleozoic rocks in the Wildcat Wash SE and Wildcat Wash SW quadrangles, Lincoln and Clark counties, Nevada: U.S. Geological Survey Open-File Report 96-26, 18 p., 2 over-size sheets, 17 leaves :ill. (some col.), maps ;28 cm., https://doi.org/10.3133/ofr9626.","productDescription":"18 p., 2 over-size sheets, 17 leaves :ill. (some col.), maps ;28 cm.","costCenters":[],"links":[{"id":156227,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0026/report-thumb.jpg"},{"id":53271,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0026/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53272,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0026/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53273,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0026/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ae49","contributors":{"authors":[{"text":"Page, W. R.","contributorId":73619,"corporation":false,"usgs":true,"family":"Page","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":191349,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pampeyan, E. H.","contributorId":14493,"corporation":false,"usgs":true,"family":"Pampeyan","given":"E. H.","affiliations":[],"preferred":false,"id":191348,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24271,"text":"ofr95686 - 1996 - Digital National Uranium Resource Evaluation (NURE) geochemistry for the Pacific Northwest: A contribution to the Interior Columbia River Basin Ecosystem Management Project","interactions":[],"lastModifiedDate":"2021-09-09T11:52:06.486039","indexId":"ofr95686","displayToPublicDate":"1996-11-01T00:00:00","publicationYear":"1996","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":"95-686","title":"Digital National Uranium Resource Evaluation (NURE) geochemistry for the Pacific Northwest: A contribution to the Interior Columbia River Basin Ecosystem Management Project","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95686","issn":"0094-9140","usgsCitation":"Raines, G.L., and Smith, C.L., 1996, Digital National Uranium Resource Evaluation (NURE) geochemistry for the Pacific Northwest: A contribution to the Interior Columbia River Basin Ecosystem Management Project: U.S. Geological Survey Open-File Report 95-686, 22 p., https://doi.org/10.3133/ofr95686.","productDescription":"22 p.","costCenters":[],"links":[{"id":155012,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":388962,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23432.htm"},{"id":1656,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/of95-686/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Idaho, Montana, Oregon, Washington, Wyoming","otherGeospatial":"Pacific northwest","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.3470,\n              41.3830\n            ],\n            [\n              -103.305,\n              41.3830\n            ],\n            [\n              -103.305,\n              49.5640\n            ],\n            [\n              -120.3470,\n              49.5640\n            ],\n            [\n              -120.3470,\n              41.3830\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b45f0","contributors":{"authors":[{"text":"Raines, Gary L.","contributorId":48162,"corporation":false,"usgs":true,"family":"Raines","given":"Gary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":191608,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Cole L.","contributorId":70757,"corporation":false,"usgs":true,"family":"Smith","given":"Cole","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":191609,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23698,"text":"ofr96301 - 1996 - Neural network technique for merging radar and visible band images","interactions":[],"lastModifiedDate":"2012-02-02T00:08:10","indexId":"ofr96301","displayToPublicDate":"1996-11-01T00:00:00","publicationYear":"1996","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":"96-301","title":"Neural network technique for merging radar and visible band images","language":"ENGLISH","publisher":"U.S. Geological Survey, National Mapping Division,","doi":"10.3133/ofr96301","issn":"0094-9140","usgsCitation":"Lemeshewsky, G., 1996, Neural network technique for merging radar and visible band images: U.S. Geological Survey Open-File Report 96-301, 14 p. :ill. ;28 cm., https://doi.org/10.3133/ofr96301.","productDescription":"14 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":156309,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0301/report-thumb.jpg"},{"id":52946,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0301/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697b42","contributors":{"authors":[{"text":"Lemeshewsky, George","contributorId":97134,"corporation":false,"usgs":true,"family":"Lemeshewsky","given":"George","affiliations":[],"preferred":false,"id":190563,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23485,"text":"ofr95690 - 1996 - Digital representation of the Idaho State geologic map; a contribution to the Interior Columbia River basin ecosystem management project","interactions":[],"lastModifiedDate":"2021-09-08T12:09:12.454516","indexId":"ofr95690","displayToPublicDate":"1996-11-01T00:00:00","publicationYear":"1996","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":"95-690","title":"Digital representation of the Idaho State geologic map; a contribution to the Interior Columbia River basin ecosystem management project","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95690","issn":"0094-9140","usgsCitation":"Johnson, B., and Raines, G.L., 1996, Digital representation of the Idaho State geologic map; a contribution to the Interior Columbia River basin ecosystem management project: U.S. Geological Survey Open-File Report 95-690, 24 p., https://doi.org/10.3133/ofr95690.","productDescription":"24 p.","costCenters":[],"links":[{"id":156873,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1795,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/of95-690/","linkFileType":{"id":5,"text":"html"}},{"id":388907,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_33354.htm"}],"country":"United States","state":"Idaho, Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.0480,\n              49\n            ],\n            [\n              -117.2410,\n              49\n            ],\n            [\n              -117.2410,\n              42\n            ],\n            [\n              -111.0480,\n              42\n            ],\n            [\n              -111.0480,\n              49\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a95e4b07f02db659e39","contributors":{"authors":[{"text":"Johnson, B. R.","contributorId":73995,"corporation":false,"usgs":true,"family":"Johnson","given":"B. R.","affiliations":[],"preferred":false,"id":190185,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Raines, G. L.","contributorId":90720,"corporation":false,"usgs":true,"family":"Raines","given":"G.","middleInitial":"L.","affiliations":[],"preferred":false,"id":190186,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23872,"text":"ofr96318 - 1996 - Simulation of water quality for Salt Creek in northeastern Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:08:12","indexId":"ofr96318","displayToPublicDate":"1996-11-01T00:00:00","publicationYear":"1996","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":"96-318","title":"Simulation of water quality for Salt Creek in northeastern Illinois","docAbstract":"Water-quality processes in the Salt Creek watershed in northeastern Illinois were simulated with a computer model. Selected waste-load scenarios for 7-day, 10-year low-flow conditions were simulated in the stream system. The model development involved the calibration of the U.S. Environmental Protection Agency QUAL2E model to water-quality constituent concentration data collected by the Illinois Environmental Protection Agency (IEPA) for a diel survey on August 29-30, 1995, and the verification of this model with water-quality constituent concentration data collected by the IEPA for a diel survey on June 27-28, 1995. In-stream measurements of sediment oxygen demand rates and carbonaceous biochemical oxygen demand (CBOD) decay rates by the IEPA and traveltime and reaeration-rate coefficients by the U.S. Geological Survey facilitated the development of a model for simulation of water quality in the Salt Creek watershed. In general, the verification of the calibrated model increased confidence in the utility of the model for water-quality planning in the Salt Creek watershed. However, the model was adjusted to better simulate constituent concentrations measured during the June 27-28, 1995, diel survey.\r\nTwo versions of the QUAL2E model were utilized to simulate dissolved oxygen (DO) concentrations in the Salt Creek watershed for selected effluent discharge and concentration scenarios for water-quality planning: (1) the QUAL2E model calibrated to the August 29-30, 1995, diel survey, and (2) the QUAL2E model adjusted to the June 27-28, 1995, diel survey. The results of these simulations indicated that the QUAL2E model adjusted to the June 27-28, 1995, diel survey simulates reliable information for water-quality planning. The results of these simulations also indicated that to maintain DO concentrations greater than 5 milligrams per liter (mg/L) throughout most of Salt Creek for 7-day, 10-year low-flow conditions, the sewage-treatment plants (STP's) must discharge effluent with CBOD and total ammonia as nitrogen concentrations substantially below the permit limits. If the STP's discharge effluent with CBOD and total ammonia as nitrogen concentrations at the permit limits for 7-day, 10-year low-flow conditions, DO concentrations less than 5 mg/L are expected for all of Salt Creek downstream from Fullerton Avenue (river mile 23.1).","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nInformation Services [distributor],","doi":"10.3133/ofr96318","issn":"0094-9140","usgsCitation":"Melching, C.S., and Chang, T., 1996, Simulation of water quality for Salt Creek in northeastern Illinois: U.S. Geological Survey Open-File Report 96-318, viii, 136 p. :ill. ;28 cm., https://doi.org/10.3133/ofr96318.","productDescription":"viii, 136 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":1591,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://il.water.usgs.gov/pubsearch/reports.cgi/view?series=OFR&number=96-318","linkFileType":{"id":5,"text":"html"}},{"id":156999,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0318/report-thumb.jpg"},{"id":53087,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0318/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478fe4b07f02db48a1f3","contributors":{"authors":[{"text":"Melching, Charles S.","contributorId":8135,"corporation":false,"usgs":true,"family":"Melching","given":"Charles","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":190891,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chang, T.J.","contributorId":85224,"corporation":false,"usgs":true,"family":"Chang","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":190892,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23636,"text":"ofr96343 - 1996 - Base-flow data for the Little West Fork Basin, Fort Campbell, Tennessee and Kentucky, 1993 and 1994","interactions":[],"lastModifiedDate":"2012-02-02T00:08:01","indexId":"ofr96343","displayToPublicDate":"1996-11-01T00:00:00","publicationYear":"1996","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":"96-343","title":"Base-flow data for the Little West Fork Basin, Fort Campbell, Tennessee and Kentucky, 1993 and 1994","docAbstract":"Base-flow data were collected from selected sites within the Little West Fork Red River basin during high and low base-flow conditions in order to support a study of the source and movement of ground water that supplies the Fort Campbell Military Reservation. Stream and spring discharge, water temperature, and specific-conductance data were collected during low base-flow conditions from 64 sites on September 1 and 13, 1993, and from 64 sites on March 17 and 18, 1994. Discharge was greater during high base-flow conditions than low base-flow conditions. Major tributaries on the south side of the study area consistently had lower flow than the tributaries on the north side. Discharge data were used to categorize stream reaches and sub-basins. Stream reaches were categorized as gaining or losing, wet, dry, or unobserved for each base-flow measurement period. More dry stream reaches occurred during the two low base-flow periods than during the high base-flow period. Sub-basin areas with surplus or deficient flow were also defined. Many areas of deficient flow occurred near the headwaters of the Little West Fork basin under all base-flow conditions. Fewer areas of deficient flow occurred near the mouth of the basin. The flow per square mile for each major tributary basin in the study area was also calculated. The values of flow per square mile for the tributary basins in the northern part of the study area were greater than those for the tributary basins in the southern part of the study area under all base-flow conditions.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr96343","issn":"0094-9140","usgsCitation":"Ladd, D., 1996, Base-flow data for the Little West Fork Basin, Fort Campbell, Tennessee and Kentucky, 1993 and 1994 (Supercedes OFR 95-724): U.S. Geological Survey Open-File Report 96-343, iv, 28 p. :ill. ;28 cm., https://doi.org/10.3133/ofr96343.","productDescription":"iv, 28 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":154897,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1682,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr96-343","linkFileType":{"id":5,"text":"html"}}],"edition":"Supercedes OFR 95-724","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648883","contributors":{"authors":[{"text":"Ladd, D.E.","contributorId":34956,"corporation":false,"usgs":true,"family":"Ladd","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":190463,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24273,"text":"ofr95684 - 1996 - Digital representation of the Washington state geologic map: a contribution to the Interior Columbia River Basin Ecosystem Management Project","interactions":[],"lastModifiedDate":"2012-02-02T00:08:00","indexId":"ofr95684","displayToPublicDate":"1996-11-01T00:00:00","publicationYear":"1996","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":"95-684","title":"Digital representation of the Washington state geologic map: a contribution to the Interior Columbia River Basin Ecosystem Management Project","docAbstract":"This report describes the digital representation of the Washington state geologic map (Hunting and others, 1961). This report contains an explantion of why the data were prepared, a description of the digital data, and information on obtaining the digital files. This report is one in a series of digital maps, data files, and reports generated by the U.S. Geological Survey to provide geologic process and mineral resource information to the Interior Columbia Basin Ecosystem Management Project (ICBEMP). The various digital maps and data files are being used in a geographic information system (GIS)-based ecosystem assessment including an analysis of diverse questions relating to past, present, and future conditions within the general area of the Columbia River Basin east of the Cascade Mountains.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr95684","issn":"0094-9140","usgsCitation":"Raines, G.L., and Johnson, B.R., 1996, Digital representation of the Washington state geologic map: a contribution to the Interior Columbia River Basin Ecosystem Management Project: U.S. Geological Survey Open-File Report 95-684, 22 p. , https://doi.org/10.3133/ofr95684.","productDescription":"22 p. ","costCenters":[{"id":658,"text":"Western Mineral Resources","active":false,"usgs":true}],"links":[{"id":155028,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7852,"rank":9999,"type":{"id":23,"text":"Spatial Data"},"url":"https://pubs.usgs.gov/of/1995/of95-684/wafaults.e00.z"},{"id":7851,"rank":9999,"type":{"id":23,"text":"Spatial Data"},"url":"https://pubs.usgs.gov/of/1995/of95-684/wageol.e00.z"},{"id":7850,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/of95-684/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a94e4b07f02db65945d","contributors":{"authors":[{"text":"Raines, Gary L.","contributorId":48162,"corporation":false,"usgs":true,"family":"Raines","given":"Gary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":191612,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Bruce R.","contributorId":100009,"corporation":false,"usgs":true,"family":"Johnson","given":"Bruce","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":191613,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21874,"text":"ofr96218 - 1996 - Hydrologic and water-quality data for the Weldon Spring Ordnance Works, St. Charles County, Missouri, 1992-95","interactions":[],"lastModifiedDate":"2012-02-02T00:07:47","indexId":"ofr96218","displayToPublicDate":"1996-11-01T00:00:00","publicationYear":"1996","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":"96-218","title":"Hydrologic and water-quality data for the Weldon Spring Ordnance Works, St. Charles County, Missouri, 1992-95","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nInformation Services [distributor],","doi":"10.3133/ofr96218","issn":"0566-8174","usgsCitation":"Schumacher, J., Merten, L., Hockanson, E.A., and DeRusseau, S., 1996, Hydrologic and water-quality data for the Weldon Spring Ordnance Works, St. Charles County, Missouri, 1992-95: U.S. Geological Survey Open-File Report 96-218, iv, 101 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr96218.","productDescription":"iv, 101 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":154125,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0218/report-thumb.jpg"},{"id":51363,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0218/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6116e2","contributors":{"authors":[{"text":"Schumacher, John G. jschu@usgs.gov","contributorId":2055,"corporation":false,"usgs":true,"family":"Schumacher","given":"John G.","email":"jschu@usgs.gov","affiliations":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"preferred":true,"id":186072,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Merten, L.M.","contributorId":74775,"corporation":false,"usgs":true,"family":"Merten","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":186075,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hockanson, E. A.","contributorId":39405,"corporation":false,"usgs":true,"family":"Hockanson","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":186074,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"DeRusseau, S.N.","contributorId":31784,"corporation":false,"usgs":true,"family":"DeRusseau","given":"S.N.","affiliations":[],"preferred":false,"id":186073,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":22613,"text":"ofr96202 - 1996 - Peak-flow frequency estimates through 1994 for gaged streams in South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:07:58","indexId":"ofr96202","displayToPublicDate":"1996-11-01T00:00:00","publicationYear":"1996","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":"96-202","title":"Peak-flow frequency estimates through 1994 for gaged streams in South Dakota","docAbstract":"Annual peak-flow data are listed for 250 continuous-record and crest-stage gaging stations in South Dakota. Peak-flow frequency estimates for selected recurrence intervals ranging from 2 to 500 years are given for 234 of these 250 stations. The log-Pearson Type III procedure was used to compute the frequency relations for the 234 stations, which in 1994 included 105 active and 129 inactive stations. The log-Pearson Type III procedure is recommended by the Hydrology Subcommittee of the Interagency Advisory Committee on Water Data, 1982, &quot;Guidelines for Determining Flood Flow Frequency.&quot;No peak-flow frequency estimates are given for 16 of the 250 stations because: (1) of extreme variability in data set; (2) more than 20 percent of years had no flow; (3) annual peak flows represent large outflow from a spring; (4) of insufficient peak-flow record subsequent to reservoir regulation; and (5) peak-flow records were combined with records from nearby stations.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr96202","issn":"0094-9140","usgsCitation":"Burr, M., and Korkow, K., 1996, Peak-flow frequency estimates through 1994 for gaged streams in South Dakota: U.S. Geological Survey Open-File Report 96-202, x, 407 p. :maps ;28 cm., https://doi.org/10.3133/ofr96202.","productDescription":"x, 407 p. :maps ;28 cm.","costCenters":[],"links":[{"id":155370,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0202/report-thumb.jpg"},{"id":52083,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0202/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c6c2","contributors":{"authors":[{"text":"Burr, M.J.","contributorId":34541,"corporation":false,"usgs":true,"family":"Burr","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":188566,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Korkow, K.L.","contributorId":70797,"corporation":false,"usgs":true,"family":"Korkow","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":188567,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}