{"pageNumber":"3063","pageRowStart":"76550","pageSize":"25","recordCount":184785,"records":[{"id":30971,"text":"wri014129 - 2001 - Geochemistry of the Madison and Minnelusa aquifers in the Black Hills area, South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:09:00","indexId":"wri014129","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","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":"2001-4129","title":"Geochemistry of the Madison and Minnelusa aquifers in the Black Hills area, South Dakota","docAbstract":"The Madison and Minnelusa aquifers are two of the most important aquifers in the Black Hills area because of utilization for water supplies and important influences on surface-water resources resulting from large springs and streamflow- loss zones. Examination of geochemical information provides a better understanding of the complex flow systems within these aquifers and interactions between the aquifers.\r\n\r\nMajor-ion chemistry in both aquifers is dominated by calcium and bicarbonate near outcrop areas, with basinward evolution towards various other water types. The most notable differences in major-ion chemistry between the Madison and Minnelusa aquifers are in concentrations of sulfate within the Minnelusa aquifer. Sulfate concentrations increase dramatically near a transition zone where dissolution of anhydrite is actively occurring.\r\n\r\nWater chemistry for the Madison and Minnelusa aquifers is controlled by reactions among calcite, dolomite, and anhydrite. Saturation indices for gypsum, calcite, and dolomite for most samples in both the Madison and Minnelusa aquifers are indicative of the occurrence of dedolomitization. Because water in the Madison aquifer remains undersaturated with respect to gypsum, even at the highest sulfate concentrations, upward leakage into the overlying Minnelusa aquifer has potential to drive increased dissolution of anhydrite in the Minnelusa Formation.\r\n\r\nIsotopic information is used to evaluate ground-water flowpaths, ages, and mixing conditions for the Madison and Minnelusa aquifers. Distinctive patterns exist in the distribution of stable isotopes of oxygen and hydrogen in precipitation for the Black Hills area, with isotopically lighter precipitation generally occurring at higher elevations and latitudes. Distributions of 18O in ground water are consistent with spatial patterns in recharge areas, with isotopically lighter 18O values in the Madison aquifer resulting from generally higher elevation recharge sources, relative to the Minnelusa aquifer.\r\n\r\nThree conceptual models, which are simplifications of lumped-parameter models, are considered for evaluation of mixing conditions and general ground-water ages. For a simple slug-flow model, which assumes no mixing, measured tritium concentrations in ground water can be related through a first-order decay equation to estimated concentrations at the time of recharge. Two simplified mixing models that assume equal proportions of annual recharge over a range of years also are considered. An ?immediate-arrival? model is used to conceptually represent conditions in outcrop areas and a ?time-delay? model is used for locations removed from outcrops, where delay times for earliest arrival of ground water generally would be expected. Because of limitations associated with estimating tritium input and gross simplifying assumptions of equal annual recharge and thorough mixing conditions, the conceptual models are used only for general evaluation of mixing conditions and approximation of age ranges.\r\n\r\nHeadwater springs, which are located in or near outcrop areas, have the highest tritium concentrations, which is consistent with the immediate-arrival mixing model. Tritium concentrations for many wells are very low, or nondetectable, indicating general applicability of the timedelay conceptual model for locations beyond outcrop areas, where artesian conditions generally occur. Concentrations for artesian springs generally are higher than for wells, which indicates generally shorter delay times resulting from preferential flowpaths that typically are associated with artesian springs.\r\n\r\nIn the Rapid City area, a distinct division of isotopic values for the Madison aquifer corresponds with distinguishing 18O signatures for nearby streams, where large streamflow recharge occurs. Previous dye testing in this area documented rapid ground-water flow (timeframe of weeks) from a streamflow loss zone to sites located several miles away. These results are used to ill","language":"ENGLISH","doi":"10.3133/wri014129","usgsCitation":"Naus, C.A., Driscoll, D.G., and Carter, J.M., 2001, Geochemistry of the Madison and Minnelusa aquifers in the Black Hills area, South Dakota: U.S. Geological Survey Water-Resources Investigations Report 2001-4129, 118 p. , https://doi.org/10.3133/wri014129.","productDescription":"118 p. ","costCenters":[],"links":[{"id":159967,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2950,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri014129/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ee4b07f02db6aa096","contributors":{"authors":[{"text":"Naus, Cheryl A.","contributorId":82749,"corporation":false,"usgs":true,"family":"Naus","given":"Cheryl","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":204487,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Driscoll, Daniel G. dgdrisco@usgs.gov","contributorId":1558,"corporation":false,"usgs":true,"family":"Driscoll","given":"Daniel","email":"dgdrisco@usgs.gov","middleInitial":"G.","affiliations":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":204486,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carter, Janet M. 0000-0002-6376-3473 jmcarter@usgs.gov","orcid":"https://orcid.org/0000-0002-6376-3473","contributorId":339,"corporation":false,"usgs":true,"family":"Carter","given":"Janet","email":"jmcarter@usgs.gov","middleInitial":"M.","affiliations":[{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true},{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":false,"id":204485,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30701,"text":"fs06801 - 2001 - Reconnaissance for trace metals in bed sediment, Wright Patman Lake, near Texarkana, Texas","interactions":[],"lastModifiedDate":"2017-01-12T12:34:10","indexId":"fs06801","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","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":"068-01","title":"Reconnaissance for trace metals in bed sediment, Wright Patman Lake, near Texarkana, Texas","docAbstract":"<p>Many contaminants can be introduced into the environment by urban and industrial activities. The drainage area of Wright Patman Lake is influenced by these activities. Among the contaminants associated with urban and industrial activities are trace metals such as arsenic, lead, mercury, and zinc. These contaminants are relatively insoluble in water and commonly are found in stream, lake, and reservoir bottom sediment, especially the clays and silts within the sediment.</p><p>Wright Patman Lake serves as the major potable water supply for the city of Texarkana and surrounding communities. Texarkana, located in the northeastern corner of Texas and the southwestern corner of Arkansas, had a population of about 56,000 in 1998, which reflects an increase of about 3.4 percent from the 1990 census (Ramos, 1999). </p><p>Texarkana Water Utilities, which manages the water-treatment facilities for Texarkana, proposes to dredge the lake bed near the water intake in the Elliot Creek arm of Wright Patman Lake. It is possible that arsenic, lead, mercury, and other trace metals might be released into the water if the bed sediment is disturbed. Bed sediment in the Elliot Creek arm of the lake, in particular, could contain trace metals because of its proximity to Red River Army Depot and because industrial land use is prevalent in the headwaters of Elliot Creek.</p><p>The U.S. Geological Survey (USGS), in cooperation with Reconnaissance for Trace Metals in Bed Sediment, Wright Patman Lake, Near Texarkana, Texas In cooperation with the Texarkana Water Utilities conducted a reconnaissance of Wright Patman Lake to collect bed-sediment samples for analysis of trace metals. This report presents trace metal concentrations in bed-sediment samples collected at six sites along the Elliot Creek arm of the lake, one site each in two adjacent arms, and one site near the dam on June 16, 1999 (fig. 1). One bed-sediment sample was collected at each of the nine sites, and one sediment core was collected at each of two of the sites. Trace metal concentrations are compared to sediment-quality guidelines for the protection of aquatic life and to screening levels based on historical trace metal concentrations in bed sediment of Texas reservoirs.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs06801","collaboration":"In cooperation with the Texarkana Water Utilities","usgsCitation":"McKee, P.W., 2001, Reconnaissance for trace metals in bed sediment, Wright Patman Lake, near Texarkana, Texas: U.S. Geological Survey Fact Sheet 068-01, HTML Document; Report: 6 p., https://doi.org/10.3133/fs06801.","productDescription":"HTML Document; Report: 6 p.","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":119301,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_068_01.bmp"},{"id":333086,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2001/fs-068-01/pdf/FS_068-01.pdf","text":"Report","size":"823 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":3075,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/fs-068-01/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Texas","otherGeospatial":"Wright Patman Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.1,\n              33.4\n            ],\n            [\n              -94.1,\n              33.2\n            ],\n            [\n              -94.3,\n              33.2\n            ],\n            [\n              -94.3,\n              33.4\n            ],\n            [\n              -94.1,\n              33.4\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db6440f4","contributors":{"authors":[{"text":"McKee, Paul W.","contributorId":88792,"corporation":false,"usgs":true,"family":"McKee","given":"Paul","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":203755,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31433,"text":"ofr01386 - 2001 - Selected laboratory evaluations of the whole-water sample-splitting capabilities of a prototype fourteen-liter Teflon churn splitter","interactions":[],"lastModifiedDate":"2012-02-02T00:09:13","indexId":"ofr01386","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","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":"2001-386","title":"Selected laboratory evaluations of the whole-water sample-splitting capabilities of a prototype fourteen-liter Teflon churn splitter","docAbstract":"A prototype 14-L Teflon? churn splitter was evaluated for whole-water sample-splitting capabilities over a range of sediment concentratons and grain sizes as well as for potential chemical contamination from both organic and inorganic constituents. These evaluations represent a 'best-case' scenario because they were performed in the controlled environment of a laboratory, and used monomineralic silica sand slurries of known concentration made up in deionized water. Further, all splitting was performed by a single operator, and all the requisite concentration analyses were performed by a single laboratory.\u000B\u000BThe prototype Teflon? churn splitter did not appear to supply significant concentrations of either organic or inorganic contaminants at current U.S. Geological Survey (USGS) National Water Quality Laboratory detection and reporting limits when test samples were prepared using current USGS protocols. As with the polyethylene equivalent of the prototype Teflon? churn, the maximum usable whole-water suspended sediment concentration for the prototype churn appears to lie between 1,000 and 10,000 milligrams per liter (mg/L). Further, the maximum grain-size limit appears to lie between 125- and 250-microns (m). Tests to determine the efficacy of the valve baffle indicate that it must be retained to facilitate representative whole-water subsampling. ","language":"ENGLISH","doi":"10.3133/ofr01386","usgsCitation":"Horowitz, A.J., Smith, J., and Elrick, K.A., 2001, Selected laboratory evaluations of the whole-water sample-splitting capabilities of a prototype fourteen-liter Teflon churn splitter: U.S. Geological Survey Open-File Report 2001-386, 12 p. , https://doi.org/10.3133/ofr01386.","productDescription":"12 p. ","costCenters":[],"links":[{"id":161481,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2568,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/ofr01-386/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478ee4b07f02db489dec","contributors":{"authors":[{"text":"Horowitz, A. J.","contributorId":102066,"corporation":false,"usgs":true,"family":"Horowitz","given":"A.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":205976,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, J.J.","contributorId":106175,"corporation":false,"usgs":true,"family":"Smith","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":205977,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Elrick, K. A.","contributorId":98731,"corporation":false,"usgs":true,"family":"Elrick","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":205975,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30708,"text":"fs08101 - 2001 - Water budget for the Nueces Estuary, Texas, May-October 1998","interactions":[],"lastModifiedDate":"2017-01-12T16:49:53","indexId":"fs08101","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","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":"081-01","title":"Water budget for the Nueces Estuary, Texas, May-October 1998","docAbstract":"<p>The Texas Water Development Board (TWDB), Texas Parks and Wildlife Department (TPWD), and Texas Natural Resource Conservation Commission (TNRCC) are charged by the Texas Legislature with determining freshwater inflows required to maintain the ecological health of streams, bays, and estuaries in Texas. To determine required inflows, the three agencies collect data and conduct studies on the needs for freshwater inflows to Texas estuaries.</p><p>The U.S. Geological Survey (USGS), in cooperation with the TWDB, conducted a study in the Nueces estuary (fig. 1) during May–October 1998 to provide water-budget data for calibration of a TWDB model that will be used to estimate the effects of different freshwater inflow volumes on circulation and salinity in the estuary. The water budget (inflows and outflows) for the Nueces estuary was estimated by using (1) data collected during this study, (2) data collected at two upstream streamflow-gaging stations previous to this study, and (3) evaporation and return-flow data obtained from other agencies. This fact sheet describes the data-collection methods and the results of the water-budget estimates for the Nueces estuary.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs08101","collaboration":"In cooperation with the Texas Water Development Board","usgsCitation":"Ockerman, D., 2001, Water budget for the Nueces Estuary, Texas, May-October 1998: U.S. Geological Survey Fact Sheet 081-01, HTML Document; Report: 6 p. , https://doi.org/10.3133/fs08101.","productDescription":"HTML Document; Report: 6 p. ","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":123176,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_081_01.bmp"},{"id":333155,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/fs-081-01/pdf/FS_081-01.pdf","text":"Report","size":"701 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":3079,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/fs-081-01/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Texas","otherGeospatial":"Nueces Estuary","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.3,\n              27.75\n            ],\n            [\n              -97.3,\n              28\n            ],\n            [\n              -97.7,\n              28\n            ],\n            [\n              -97.7,\n              27.75\n            ],\n            [\n              -97.3,\n              27.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa2f9","contributors":{"authors":[{"text":"Ockerman, D.J.","contributorId":38979,"corporation":false,"usgs":true,"family":"Ockerman","given":"D.J.","affiliations":[],"preferred":false,"id":203766,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31438,"text":"ofr01453 - 2001 - Rb-Sr whole-rock and mineral ages, K-Ar, 40Ar/39Ar, and U-Pb mineral ages, and strontium, lead, neodymium, and oxygen isotopic compositions for granitic rocks from the Salinian composite terrane, California","interactions":[],"lastModifiedDate":"2021-10-04T20:28:41.925263","indexId":"ofr01453","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","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":"2001-453","title":"Rb-Sr whole-rock and mineral ages, K-Ar, 40Ar/39Ar, and U-Pb mineral ages, and strontium, lead, neodymium, and oxygen isotopic compositions for granitic rocks from the Salinian composite terrane, California","docAbstract":"<p>This report summarizes new and published age and isotopic data for whole-rocks and minerals from granitic rocks in the Salinian composite terrane, California. Rubidium-strontium whole-rock ages of plutons are in two groups, Early Cretaceous (122 to 100 Ma) and Late Cretaceous (95 to 82 Ma). Early Cretaceous plutons occur in all granitic rock exposures from Bodega Head in the north to those from the Santa Lucia and Gabilan Ranges in the central part of the terrane. Late Cretaceous plutons have been identified in the Point Reyes Peninsula, the Santa Lucia and the Gabilan Ranges, and in the La Panza Range in the southern part of the terrane. Ranges of initial values of isotopic compositions are <sup>87</sup>Sr/<sup>86</sup>Sr, 0.7046-0.7147, δ<sup>18</sup>O, +8.5 to +12.5 per mil, <sup>206</sup>Pb/<sup>204</sup>Pb, 18.901-19.860, <sup>207</sup>Pb/<sup>204</sup>Pb, 15.618-15.814, <sup>208</sup>Pb/<sup>204</sup>Pb, 38.569- 39.493, and εNd, +0.9 to -8.6.</p>\n<br/>\n<p>The initial <sup>87</sup>Sr/<sup>86</sup>Sr=0.706 isopleth is identified in the northern Gabilan Range and in the Ben Lomond area of the Santa Cruz Mountains, in Montara Mountain, in Bodega Head, and to the west of the Farallon Islands on the Cordell Bank. This isotopic boundary is offset about 95 miles (160km) by right-lateral displacements along the San Gregorio-Hosgri and San Andreas fault systems.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr01453","usgsCitation":"Kistler, R.W., and Champion, D., 2001, Rb-Sr whole-rock and mineral ages, K-Ar, 40Ar/39Ar, and U-Pb mineral ages, and strontium, lead, neodymium, and oxygen isotopic compositions for granitic rocks from the Salinian composite terrane, California: U.S. Geological Survey Open-File Report 2001-453, 80 p., https://doi.org/10.3133/ofr01453.","productDescription":"80 p.","numberOfPages":"80","costCenters":[],"links":[{"id":59781,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0453/pdf/of01-453.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":390209,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_45592.htm"},{"id":282380,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr01453.jpg"},{"id":2571,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/0453/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","otherGeospatial":"Bodega Head, Gabilan Range, La Panza Range, Montara Mountain, Point Reyes Peninsula, Santa Cruz Mountains, Santa Lucia Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.5,\n              34.7750\n            ],\n            [\n              -119,\n              34.7750\n            ],\n            [\n              -119,\n              38.167\n            ],\n            [\n              -123.5,\n              38.167\n            ],\n            [\n              -123.5,\n              34.7750\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a55e4b07f02db62ce7e","contributors":{"authors":[{"text":"Kistler, R. W.","contributorId":36112,"corporation":false,"usgs":true,"family":"Kistler","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":205991,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Champion, D.E.","contributorId":70402,"corporation":false,"usgs":true,"family":"Champion","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":205992,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30702,"text":"fs07001 - 2001 - Water-quality monitoring of Sweetwater Reservoir","interactions":[],"lastModifiedDate":"2012-02-02T00:09:14","indexId":"fs07001","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","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":"070-01","title":"Water-quality monitoring of Sweetwater Reservoir","docAbstract":"Sweetwater Authority is concerned with the quality of water it provides to its customers. Results from the water-quality monitoring study that the USGS is conducting in the Sweetwater watershed show that the contaminant concentrations in bed sediments, water, and air are reflected in increased urbanization. The bed sediments show the most dramatic evidence of this impact with a sharp increase of persistent organic chemical concentrations over the past 65 years. Water quality is also affected by urbanization in the form of chemicals in the runoff water and deposition of airborne chemicals. The concentrations of the detected organic chemicals in Sweetwater and Loveland Reservoirs are all well below the guidance limits set by State and Federal agencies to protect human health. Many of these compounds are detected only because of the sensitive analytical methods used. This monitoring program provides the Sweetwater Authority with information on what monitored chemicals are present in the reservoirs, and at what concentrations. With this information, the Authority can assess the associated risks, and consider future water treatment and remediation. These results also help focus and support future efforts by Sweetwater Authority to protect the watershed.","language":"ENGLISH","doi":"10.3133/fs07001","usgsCitation":"Majewski, M., 2001, Water-quality monitoring of Sweetwater Reservoir: U.S. Geological Survey Fact Sheet 070-01, 4 p. , https://doi.org/10.3133/fs07001.","productDescription":"4 p. ","costCenters":[],"links":[{"id":124802,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_070_01.bmp"},{"id":3076,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/FS/fs-070-01/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa851","contributors":{"authors":[{"text":"Majewski, Michael","contributorId":74792,"corporation":false,"usgs":true,"family":"Majewski","given":"Michael","affiliations":[],"preferred":false,"id":203756,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31431,"text":"ofr01377 - 2001 - Shallow ground-water quality in an agricultural area of the lower coastal plain of South Carolina, 1997","interactions":[],"lastModifiedDate":"2016-12-07T15:06:53","indexId":"ofr01377","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","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":"2001-377","title":"Shallow ground-water quality in an agricultural area of the lower coastal plain of South Carolina, 1997","docAbstract":"Ground-water-quality samples were collected from 30 shallow monitoring wells located in agricultural areas of the lower Coastal Plain of South Carolina during the summer of 1997 as part of the U.S. Geological Survey National Water-Quality Assessment Program in the Santee River Basin and Coastal Drainages study unit. The wells were completed in sand to clayey sand sediments of the surficial aquifer and sampled one time for selected field properties, and nutrient, major ion, and pesticide concentrations. This report contains the results of the sampling effort.","language":"ENGLISH","doi":"10.3133/ofr01377","usgsCitation":"Reuber, E.J., 2001, Shallow ground-water quality in an agricultural area of the lower coastal plain of South Carolina, 1997: U.S. Geological Survey Open-File Report 2001-377, 13 p. , https://doi.org/10.3133/ofr01377.","productDescription":"13 p. ","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":161453,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2001/0377/report-thumb.jpg"},{"id":59778,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0377/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":2567,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr01377/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"South Carolina","otherGeospatial":"Lower Coastal Plain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.71307373046874,\n              35.67068501330236\n            ],\n            [\n              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,{"id":31418,"text":"ofr0138 - 2001 - Selected hydrologic data for Little Cottonwood Creek, Salt Lake County, Utah, September 1998","interactions":[],"lastModifiedDate":"2020-02-19T06:10:38","indexId":"ofr0138","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","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":"2001-38","title":"Selected hydrologic data for Little Cottonwood Creek, Salt Lake County, Utah, September 1998","docAbstract":"<p><span>Metals enter Little Cottonwood Creek in Salt Lake County, Utah, in drainage water that discharges from inactive mines in the watershed (fig. 1). As part of a study to evaluate the effects of this mine drainage on water quality, a sodium chloride tracer was injected into Little Cottonwood Creek during September 17-18, 1998. The purpose of the injection was to quantify stream discharge; to identify inflows, both those observable and those dispersed in the subsurface; and ultimately, to determine which areas within the watershed contribute the most metals to Little Cottonwood Creek. The purpose of this report is to make these data available to agencies responsible for managing the area’ s water resources and to supplement interpretive reports for this study.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0138","collaboration":"Prepared in cooperation with the U.S. Department of Agriculture, U.S. Forest Service","usgsCitation":"Gerner, L.J., Rossi, F.J., and Kimball, B., 2001, Selected hydrologic data for Little Cottonwood Creek, Salt Lake County, Utah, September 1998: U.S. Geological Survey Open-File Report 2001-38, 2 Sheets: 43.00 x 27.50 inches and 43.00 x 27.00 inches, https://doi.org/10.3133/ofr0138.","productDescription":"2 Sheets: 43.00 x 27.50 inches and 43.00 x 27.00 inches","costCenters":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":340282,"rank":2,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/2001/0038/ofr0138_sheet1.pdf","text":"OFR 01–38 Sheet 1","size":"375 KB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 01–38 Sheet 1"},{"id":340283,"rank":3,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/2001/0038/ofr0138_sheet2.pdf","text":"OFR 01–38 Sheet 2","size":"241 KB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 01–38 Sheet 2"},{"id":160845,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2001/0038/coverthb.jpg"}],"country":"United States","state":"Utah","county":"Salt Lake 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Lake\",\"state\":\"UT\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8ba2","contributors":{"authors":[{"text":"Gerner, L. J.","contributorId":72008,"corporation":false,"usgs":true,"family":"Gerner","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":205945,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rossi, F. J.","contributorId":57113,"corporation":false,"usgs":true,"family":"Rossi","given":"F.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":205944,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kimball, B.K.","contributorId":15668,"corporation":false,"usgs":true,"family":"Kimball","given":"B.K.","email":"","affiliations":[],"preferred":false,"id":205943,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":31419,"text":"ofr01202 - 2001 - Impacts of climate change on landscapes of the eastern Sierra Nevada and western Great Basin","interactions":[],"lastModifiedDate":"2023-06-27T14:23:30.648176","indexId":"ofr01202","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","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":"2001-202","title":"Impacts of climate change on landscapes of the eastern Sierra Nevada and western Great Basin","docAbstract":"This effort was developed under a U.S. Geological Survey (USGS) initiative to sponsor science workshops focusing on various of multidiscipline, multiprogram themes in the arid Southwest. The intent was to use the workshops to explore leading edge questions, as well as to provide better communication and collaboration between USGS and other organizations and agencies. The workshop topics fall within the broad areas of landscape science of the Southwest, ecosystem studies, climatic variation, land use associated with degradation of habitat and soils, and surficial processes in relation to the environment.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr01202","usgsCitation":"Jayko, A.S., and Millar, C.I., 2001, Impacts of climate change on landscapes of the eastern Sierra Nevada and western Great Basin: U.S. Geological Survey Open-File Report 2001-202, v, 35 p., https://doi.org/10.3133/ofr01202.","productDescription":"v, 35 p.","numberOfPages":"39","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":282570,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":59774,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0202/pdf/of01-202.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":2558,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/0202/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","otherGeospatial":"Great Basin, Sierra Nevada","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123.18,34.36 ], [ -123.18,44.89 ], [ -110.37,44.89 ], [ -110.37,34.36 ], [ -123.18,34.36 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a05e4b07f02db5f8629","contributors":{"authors":[{"text":"Jayko, A. S. 0000-0002-7378-0330","orcid":"https://orcid.org/0000-0002-7378-0330","contributorId":18011,"corporation":false,"usgs":true,"family":"Jayko","given":"A.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":205946,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Millar, C. I.","contributorId":47165,"corporation":false,"usgs":true,"family":"Millar","given":"C.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":205947,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":31424,"text":"ofr01348 - 2001 - Columbium (niobium) recycling in the United States in 1998","interactions":[],"lastModifiedDate":"2012-02-02T00:09:13","indexId":"ofr01348","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","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":"2001-348","title":"Columbium (niobium) recycling in the United States in 1998","docAbstract":"This report describes the flow of columbium in the United States in 1998 with emphasis on the extent to which columbium (niobium) was recycled/reused. Columbium was mostly recycled from products of columbium-bearing steels and superalloys; little was recovered from products specifically for their columbium content. In 1998, about 1,800 metric tons of columbium was recycled/reused, with about 55% derived from old scrap. The columbium recycling rate was calculated to be 22%, and columbium scrap recycling efficiency, 50%.","language":"ENGLISH","doi":"10.3133/ofr01348","usgsCitation":"Cunningham, L.D., 2001, Columbium (niobium) recycling in the United States in 1998: U.S. Geological Survey Open-File Report 2001-348, 12 p., https://doi.org/10.3133/ofr01348.","productDescription":"12 p.","costCenters":[],"links":[{"id":161263,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2560,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/openfile/of01-348/ ","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae767","contributors":{"authors":[{"text":"Cunningham, Larry D.","contributorId":62649,"corporation":false,"usgs":true,"family":"Cunningham","given":"Larry","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":205960,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30703,"text":"fs07201 - 2001 - Effects of oil and gas production on Lake Meredith sediments, 1964-99","interactions":[],"lastModifiedDate":"2016-09-09T13:09:12","indexId":"fs07201","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","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":"072-01","title":"Effects of oil and gas production on Lake Meredith sediments, 1964-99","docAbstract":"<p>Lake Meredith lies on the dry and windswept High Plains of the Texas Panhandle and is a popular recreation area for the region. Oil and gas exploration and extraction have been ongoing at Lake Meredith National Recreation Area since about 1930. More than 250 wells, including those abandoned or relocated, are within the boundaries of the recreation area. Oil and gas wells in the watershed of Lake Meredith number in the thousands.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs07201","usgsCitation":"Mahler, B., and Van Metre, P., 2001, Effects of oil and gas production on Lake Meredith sediments, 1964-99: U.S. Geological Survey Fact Sheet 072-01, 6 p., https://doi.org/10.3133/fs07201.","productDescription":"6 p.","numberOfPages":"6","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":119302,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs07201.PNG"},{"id":3077,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/fs07201/","linkFileType":{"id":5,"text":"html"}},{"id":328444,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/fs07201/pdf/FS_072-01.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611ae3","contributors":{"authors":[{"text":"Mahler, Barbara 0000-0002-9150-9552 bjmahler@usgs.gov","orcid":"https://orcid.org/0000-0002-9150-9552","contributorId":1249,"corporation":false,"usgs":true,"family":"Mahler","given":"Barbara","email":"bjmahler@usgs.gov","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":203757,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Metre, Peter C.","contributorId":34104,"corporation":false,"usgs":true,"family":"Van Metre","given":"Peter C.","affiliations":[],"preferred":false,"id":203758,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":31425,"text":"ofr01349 - 2001 - Tantalum recycling in the United States in 1998","interactions":[],"lastModifiedDate":"2012-02-02T00:09:13","indexId":"ofr01349","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","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":"2001-349","title":"Tantalum recycling in the United States in 1998","docAbstract":"This report describes the flow of tantalum in the United States in 1998 with emphasis on the extent to which tantalum was recycled/reused. Tantalum was mostly recycled from new scrap that was generated during the manufacture of tantalum-related electronic components and new and old scrap products of tantalum-containing cemented carbides and superalloys. In 1998, about 210 metric tons of tantalum was recycled/reused, with about 43% derived from old scrap. The tantalum recycling rate was calculated to be 21%, and tantalum scrap recycling efficiency, 35%.","language":"ENGLISH","doi":"10.3133/ofr01349","usgsCitation":"Cunningham, L.D., 2001, Tantalum recycling in the United States in 1998: U.S. Geological Survey Open-File Report 2001-349, 12 p., https://doi.org/10.3133/ofr01349.","productDescription":"12 p.","costCenters":[],"links":[{"id":161264,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2561,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/openfile/of01-349/ ","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686736","contributors":{"authors":[{"text":"Cunningham, Larry D.","contributorId":62649,"corporation":false,"usgs":true,"family":"Cunningham","given":"Larry","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":205961,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31430,"text":"ofr01374 - 2001 - A guide to potential soil carbon sequestration: Land-use management for mitigation of greenhouse gas emissions","interactions":[],"lastModifiedDate":"2022-12-15T19:42:53.741152","indexId":"ofr01374","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","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":"2001-374","title":"A guide to potential soil carbon sequestration: Land-use management for mitigation of greenhouse gas emissions","docAbstract":"Terrestrial carbon sequestration has a potential role in reducing the recent increase in atmospheric carbon dioxide (CO2) that is, in part, contributing to global warming. Because the most stable long-term surface reservoir for carbon is the soil, changes in agriculture and forestry can potentially reduce atmospheric CO2 through increased soil-carbon storage. If local governments and regional planning agencies are to effect changes in land-use management that could mitigate the impacts of increased greenhouse gas (GHG) emissions, it is essential to know how carbon is cycled and distributed on the landscape. Only then can a cost/benefit analysis be applied to carbon sequestration as a potential land-use management tool for mitigation of GHG emissions. \r\n\r\nFor the past several years, the U.S. Geological Survey (USGS) has been researching the role of terrestrial carbon in the global carbon cycle. Data from these investigations now allow the USGS to begin to (1) 'map' carbon at national, regional, and local scales; (2) calculate present carbon storage at land surface; and (3) identify those areas having the greatest potential to sequester carbon.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr01374","usgsCitation":"Markewich, H.W., and Buell, G.R., 2001, A guide to potential soil carbon sequestration: Land-use management for mitigation of greenhouse gas emissions: U.S. Geological Survey Open-File Report 2001-374, 4 p., https://doi.org/10.3133/ofr01374.","productDescription":"4 p.","costCenters":[],"links":[{"id":410560,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_43719.htm","linkFileType":{"id":5,"text":"html"}},{"id":161452,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2566,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/openfile/of01-374/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"North Carolina","county":"Mitchell County, Yancey County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -80.48600054457992,\n              36.51996654528013\n            ],\n            [\n              -83.62386313718575,\n              36.51996654528013\n            ],\n            [\n              -83.62386313718575,\n              35.05523711139929\n            ],\n            [\n              -80.48600054457992,\n              35.05523711139929\n            ],\n            [\n              -80.48600054457992,\n              36.51996654528013\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae505","contributors":{"authors":[{"text":"Markewich, H. W.","contributorId":31426,"corporation":false,"usgs":true,"family":"Markewich","given":"H.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":205969,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buell, G. R.","contributorId":57103,"corporation":false,"usgs":true,"family":"Buell","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":205970,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30700,"text":"fs06701 - 2001 - PCBs in tissue of fish from the Spokane River, Washington, 1999","interactions":[],"lastModifiedDate":"2012-11-25T18:17:22","indexId":"fs06701","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","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":"067-01","title":"PCBs in tissue of fish from the Spokane River, Washington, 1999","docAbstract":"Several studies over the past 6 years have indicated that elevated concentrations of polychlorinated biphenyls (PCBs) in the Spokane River, Washington, are a potential hazard to human and aquatic health. To help address these concerns, fish were collected from the Spokane River in 1999 and analyzed for PCBs for a cooperative study by the U.S. Geological Survey (as part of the National Water-Quality Assessment Program) and the Washington State Department of Ecology. This Fact Sheet summarizes comparisons of PCB concentrations in fish tissue recommended by national criteria with concentrations in fish tissue analyzed for this 1999 cooperative study and for previous studies.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs06701","collaboration":"Prepared in cooperation with Washington State Department of Ecology","usgsCitation":"MacCoy, D.E., 2001, PCBs in tissue of fish from the Spokane River, Washington, 1999: U.S. Geological Survey Fact Sheet 067-01, 6 p., https://doi.org/10.3133/fs06701.","productDescription":"6 p.","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":121981,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2001/0067/report-thumb.jpg"},{"id":59457,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2001/0067/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","projection":"Albers Equal-Area Conic","country":"United States","state":"Washington;Idaho;Montana","city":"Spokane;Post Falls","otherGeospatial":"Spokane River;Northern Rockies Intermontane Basins;Nine Mile Dam;Upriver Dam","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.783,47.245 ], [ -117.783,47.9979 ], [ -116.3794,47.9979 ], [ -116.3794,47.245 ], [ -117.783,47.245 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689eb1","contributors":{"authors":[{"text":"MacCoy, Dorene E. 0000-0001-6810-4728 demaccoy@usgs.gov","orcid":"https://orcid.org/0000-0001-6810-4728","contributorId":948,"corporation":false,"usgs":true,"family":"MacCoy","given":"Dorene","email":"demaccoy@usgs.gov","middleInitial":"E.","affiliations":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"preferred":true,"id":203754,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30748,"text":"fs09201 - 2001 - Streamflow information for the Jacks Fork and Current River in the Ozark National Scenic Riverways, south-central Missouri","interactions":[],"lastModifiedDate":"2019-06-18T15:28:45","indexId":"fs09201","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","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":"092-01","displayTitle":"Streamflow Information for the Jacks Fork and Current River in the Ozark National Scenic Riverways, South-Central Missouri","title":"Streamflow information for the Jacks Fork and Current River in the Ozark National Scenic Riverways, south-central Missouri","docAbstract":"<p>The U.S. Geological Survey (USGS), in cooperation with the National Park Service (NPS), has been collecting streamflow information on the Current River and one of its tributaries, the Jacks Fork, for 78 years. Both rivers are located in south-central Missouri in an area with large springs, streams, caves, and rugged countryside. Outdoor activities, such as camping, floating, fishing, hunting, and hiking, are numerous. Part of both the Jacks Fork and the Current River are in the Ozark National Scenic Riverways (ONSR), which is administrated by the NPS. The Jacks Fork and Current River were the Nation’s first congressionally designated scenic riverways.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs09201","usgsCitation":"Wilson, G.L., 2001, Streamflow information for the Jacks Fork and Current River in the Ozark National Scenic Riverways, south-central Missouri: U.S. Geological Survey Fact Sheet 092-01, 4 p., https://doi.org/10.3133/fs09201.","productDescription":"4 p.","numberOfPages":"4","costCenters":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"links":[{"id":59476,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2001/0092/fs09201.pdf","text":"Report","size":"535 kB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 092–01"},{"id":119496,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2001/0092/coverthb.jpg"}],"contact":"<p>Director,&nbsp;<a href=\"https://www.usgs.gov/centers/cm-water\" data-mce-href=\"https://www.usgs.gov/centers/cm-water\">Central Midwest Water Science Center</a><br>U.S. Geological Survey<br>1400 Independence Road<br>Rolla, MO 65401</p>","tableOfContents":"<ul><li>Introduction</li><li>Springs</li><li>Rivers</li><li>Flow Variation</li><li>Low Flow</li><li>High Flow</li><li>Information on the Internet</li><li>References Cited</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4da0","contributors":{"authors":[{"text":"Wilson, Gary L. gwilson@usgs.gov","contributorId":3078,"corporation":false,"usgs":true,"family":"Wilson","given":"Gary","email":"gwilson@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":203838,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31429,"text":"ofr01363 - 2001 - Spectral induced polarization measurements at the Carlisle mine dump, New Mexico","interactions":[],"lastModifiedDate":"2021-11-23T19:47:47.285885","indexId":"ofr01363","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","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":"2001-363","title":"Spectral induced polarization measurements at the Carlisle mine dump, New Mexico","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr01363","usgsCitation":"Campbell, D.L., and Beanland, S., 2001, Spectral induced polarization measurements at the Carlisle mine dump, New Mexico: U.S. Geological Survey Open-File Report 2001-363, 11 p., https://doi.org/10.3133/ofr01363.","productDescription":"11 p.","costCenters":[],"links":[{"id":392059,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_43481.htm"},{"id":161451,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2565,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/ofr-01-0363/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New Mexico","otherGeospatial":"Carlisle mine dump","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.973,\n              32.847\n            ],\n            [\n              -108.962,\n              32.847\n            ],\n            [\n              -108.962,\n              32.856\n            ],\n            [\n              -108.973,\n              32.856\n            ],\n            [\n              -108.973,\n              32.847\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e5ced","contributors":{"authors":[{"text":"Campbell, David L.","contributorId":95447,"corporation":false,"usgs":true,"family":"Campbell","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":205968,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beanland, Shay","contributorId":11244,"corporation":false,"usgs":true,"family":"Beanland","given":"Shay","affiliations":[],"preferred":false,"id":205967,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":31420,"text":"ofr01250 - 2001 - Hydrogeologic data for the Big River–Mishnock River stream-aquifer system, central Rhode Island","interactions":[],"lastModifiedDate":"2022-01-20T19:11:04.187945","indexId":"ofr01250","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","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":"2001-250","title":"Hydrogeologic data for the Big River–Mishnock River stream-aquifer system, central Rhode Island","docAbstract":"Hydrogeology, ground-water development alternatives, and water quality in the Big\u001FMishnock stream-aquifer system in central Rhode Island are being investigated as part of a long-term cooperative program between the Rhode Island Water Resources Board and the U.S. Geological Survey to evaluate the ground-water resources throughout Rhode Island. The study area includes the Big River drainage basin and that portion of the Mishnock River drainage basin upstream from the Mishnock River at State Route 3. This report presents geologic data and hydrologic and water-quality data for ground and surface water.\r \rGround-water data were collected from July 1996 through September 1998 from a network of observation wells consisting of existing wells and wells installed for this study, which provided a broad distribution of data-collection sites throughout the study area. Streambed piezometers were used to obtain differences in head data between surface-water levels and ground-water levels to help evaluate stream-aquifer interactions throughout the study area. The types of data presented include monthly ground-water levels, average daily ground-water withdrawals, drawdown data from aquifer tests, and water-quality data. Historical water-level data from other wells within the study area also are presented in this report.\r \rSurface-water data were obtained from a network consisting of surface-water impoundments, such as ponds and reservoirs, existing and newly established partial-record stream-discharge sites, and synoptic surface-water-quality sites. Water levels were collected monthly from the surface-water impoundments. Stream-discharge measurements were made at partial-record sites to provide measurements of inflow, outflow, and internal flow throughout the study area. Specific conductance was measured monthly at partial-record sites during the study, and also during the fall and spring of 1997 and 1998 at 41 synoptic sites throughout the study area.\r \rGeneral geologic data, such as estimates of depth to bedrock and depth to water table, as well as indications of underlying geologic structure, were obtained from geophysical surveys. Site-specific geologic data were collected during the drilling of observation wells and test holes. These data include depth to bedrock or refusal, depth to water table, and lithologic information.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr01250","usgsCitation":"Craft, P.A., 2001, Hydrogeologic data for the Big River–Mishnock River stream-aquifer system, central Rhode Island: U.S. Geological Survey Open-File Report 2001-250, 104 p., https://doi.org/10.3133/ofr01250.","productDescription":"104 p.","costCenters":[],"links":[{"id":161231,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":394601,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_46474.htm"},{"id":2559,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr01250","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Rhode Island","otherGeospatial":"Big River–Mishnock River stream-aquifer system","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.6944,\n              41.5833\n            ],\n            [\n              -71.5439,\n              41.5833\n            ],\n            [\n              -71.5439,\n              41.6958\n            ],\n            [\n              -71.6944,\n              41.6958\n            ],\n            [\n              -71.6944,\n              41.5833\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628afc","contributors":{"authors":[{"text":"Craft, P. A.","contributorId":102105,"corporation":false,"usgs":true,"family":"Craft","given":"P.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":205948,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31439,"text":"ofr01454 - 2001 - Methods of analysis by the U.S. Geological Survey Organic Geochemistry Research Group—Determination of glyphosate, aminomethylphosphonic acid, and glufonsinate in water using online solid-phase extraction and high-performance liquid chromatography/mass spectrometry","interactions":[],"lastModifiedDate":"2020-02-16T11:40:21","indexId":"ofr01454","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","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":"2001-454","displayTitle":"Methods of Analysis by the U.S. Geological Survey Organic Geochemistry Research Group—Determination of Glyphosate, Aminomethylphosphonic Acid, and Glufosinate in Water Using Online Solid-Phase Extraction and High-Performance Liquid Chromatography/Mass Spectrometry","title":"Methods of analysis by the U.S. Geological Survey Organic Geochemistry Research Group—Determination of glyphosate, aminomethylphosphonic acid, and glufonsinate in water using online solid-phase extraction and high-performance liquid chromatography/mass spectrometry","docAbstract":"<p>An analytical method for the determination of glyphosate, its principal degradation compound, aminomethylphosphonic acid (AMPA), and glufosinate in water with varying matrices has been developed. Four different sample matrices fortified at 0.2 and 2.0 μg/L (micrograms per liter) were analyzed using precolumn derivatization with 9-fluorenylmethylchloroformate (FMOC). After derivatization, cleanup and concentration were accomplished using automated online solid-phase extraction followed by elution with the mobile phase allowing for direct injection into a liquid chromatograph/mass spectrometer (LC/MS). Analytical conditions for MS detection were optimized, and quantitation was carried out using the following representative ions: 390 and 168 for glyphosate; 332, 110, and 136 for AMPA; and 402, 180, and 206 for glufosinate. Matrix effects were minimized by utilizing standard addition for quantification and an isotope-labeled glyphosate (2-<sup>13</sup>C,<sup>15</sup>N) as the internal standard. Method detection limits (MDLs) were 0.084 μg/L for glyphosate, 0.078 μg/L for AMPA, and 0.057 μg/L for glufosinate. The method reporting limits (MRLs) were set at 0.1 μg/L for all three compounds. The mean recovery values ranged from 88.0 to 128.7 percent, and relative standard deviation values ranged from 5.6 to 32.6 percent.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr01454","usgsCitation":"Lee, E., Strahan, A., and Thurman, E., 2001, Methods of analysis by the U.S. Geological Survey Organic Geochemistry Research Group—Determination of glyphosate, aminomethylphosphonic acid, and glufonsinate in water using online solid-phase extraction and high-performance liquid chromatography/mass spectrometry: U.S. Geological Survey Open-File Report 2001-454, iv, 13 p., https://doi.org/10.3133/ofr01454.","productDescription":"iv, 13 p.","numberOfPages":"18","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":161425,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":360148,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0454/ofr20010454.pdf","text":"Report","size":"403 kB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2001–0454"}],"contact":"<p><a href=\"mailto:%20dc_ks@usgs.gov\" data-mce-href=\"mailto:%20dc_ks@usgs.gov\">Director</a>, <a href=\"https://www.usgs.gov/centers/kswsc\" data-mce-href=\"https://www.usgs.gov/centers/kswsc\">Kansas Water Science Center</a><br>U.S. Geological Survey<br>1217 Biltmore Drive<br>Lawrence, KS 66049</p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Determination of Glyphosate, Aminomethylphosphonic Acid, and Glufosinate in Water</li><li>Discussion</li><li>Conclusions</li><li>References Cited</li><li>Appendices</li></ul>","publishingServiceCenter":{"id":4,"text":"Rolla PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bc6e","contributors":{"authors":[{"text":"Lee, E.A.","contributorId":48608,"corporation":false,"usgs":true,"family":"Lee","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":205994,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Strahan, A.P.","contributorId":6902,"corporation":false,"usgs":true,"family":"Strahan","given":"A.P.","affiliations":[],"preferred":false,"id":205993,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thurman, E.M.","contributorId":102864,"corporation":false,"usgs":true,"family":"Thurman","given":"E.M.","affiliations":[],"preferred":false,"id":205995,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":31434,"text":"ofr2001393 - 2001 - Thickness and geometry of Cenozoic deposits in California Wash area, Nevada, based on gravity and seismic-reflection data","interactions":[],"lastModifiedDate":"2012-02-10T00:10:09","indexId":"ofr2001393","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","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":"2001-393","title":"Thickness and geometry of Cenozoic deposits in California Wash area, Nevada, based on gravity and seismic-reflection data","docAbstract":"Gravity and seismic-reflection data provide insights into the subsurface stratigraphy and structure of the California Wash area of southern Nevada. This area is part of the Lower Colorado flow system and stratigraphic and structural data are important inputs into developing the hydrogeologic framework. These data indicate that the basin beneath California Wash reaches depths of 2-3 km. The eastern margin of the basin coincides with a system of young (Quaternary and late Tertiary) faults, although both seismic and gravity data indicate that the major basin-bounding fault is 2-3 km west of the mapped young faults. Dry Lake Valley, the adjacent valley to the west, is characterized by thinner basin fill. The basin configuration beneath both California Wash and Dry Lake Valleys based on the inversion of gravity data is unconstrained because of the lack of gravity stations north of 36030?. Broad aeromagnetic anomalies beneath pre-Cenozoic basement in the Muddy Mountains and Arrow Canyon Range reflect Precambrian basement at depths of ~ 5 km. These rocks are probably barriers to ground-water flow,except where fractured.","language":"ENGLISH","doi":"10.3133/ofr2001393","usgsCitation":"Langenheim, V., Miller, J.J., Page, W.R., and Grow, J.A., 2001, Thickness and geometry of Cenozoic deposits in California Wash area, Nevada, based on gravity and seismic-reflection data: U.S. Geological Survey Open-File Report 2001-393, 27 p., https://doi.org/10.3133/ofr2001393.","productDescription":"27 p.","costCenters":[{"id":647,"text":"Western Earth Surface Processes","active":false,"usgs":true}],"links":[{"id":161482,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8870,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/of01-393/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c596","contributors":{"authors":[{"text":"Langenheim, V.E. 0000-0003-2170-5213","orcid":"https://orcid.org/0000-0003-2170-5213","contributorId":54956,"corporation":false,"usgs":true,"family":"Langenheim","given":"V.E.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":205980,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, J. J.","contributorId":54588,"corporation":false,"usgs":true,"family":"Miller","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":205979,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Page, W. R.","contributorId":73619,"corporation":false,"usgs":true,"family":"Page","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":205981,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Grow, J. A.","contributorId":27858,"corporation":false,"usgs":true,"family":"Grow","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":205978,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":30982,"text":"wri014273 - 2001 - Quality-assurance data, comparison to water-quality standards, and site considerations for total dissolved gas and water temperature, lower Columbia River, Oregon and Washington, 2001","interactions":[],"lastModifiedDate":"2017-02-07T09:13:41","indexId":"wri014273","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","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":"2001-4273","title":"Quality-assurance data, comparison to water-quality standards, and site considerations for total dissolved gas and water temperature, lower Columbia River, Oregon and Washington, 2001","docAbstract":"<h1>Significant Findings</h1>\n<ul>\n<li>For eight monitoring sites, in water year 2001, an average of 99.3% of the total-dissolved-gas data were received in real time and passed quality-assurance checks.</li>\n<li>After 2 to 3 weeks of deployment in the river, most comparisons of field total-dissolved-gas sensors with a secondary standard (another calibrated total-dissolved-gas sensor) were within 1%.</li>\n<li>The only exceedances of Oregon water-quality standards for total dissolved gas occurred on May 23 and 24, 2001, at the Camas, Washington, station.</li>\n<li>At the forebay of the John Day Dam, temporary increases in water temperature and total dissolved gas occurred on hot afternoons during periods of low wind. These increases were not observed at the John Day tailwater station.</li>\n<li>At Camas, Washington, daily variations of total dissolved gas were probably due to the production of oxygen by aquatic plants and to water-temperature variations on warm, sunny days.</li>\n<li>During spill over Bonneville Dam in water year 2001, the site on the Oregon side of the Columbia River, Warrendale, measured larger total-dissolved-gas levels than the site directly across on the Washington side at Skamania.</li>\n<li>Apparently, streamflow through generating facilities on the north side of the dam forced supersaturated water from the spill bays over to the Oregon side of the river.</li>\n<li>At times in July and August 2001, the total-dissolved-gas probe at Warrendale could not be positioned below the minimum compensation depth because the river was too shallow at that location. Consequently, degassing at probe depth may have occurred, and total dissolved gas may have been larger in locations with greater depths.</li>\n</ul>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/wri014273","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers","usgsCitation":"Suggested citation: Tanner, D.Q., and Bragg, H.M., 2001, Quality-assurance data, comparison to water-quality\nstandards, and site considerations for total dissolved gas and water temperature, lower Columbia River, Oregon\nand Washington, 2001: U.S. Geological Survey Water-Resources Investigations Report 01–4273, 14 p.","productDescription":"14 p. ","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":159988,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2976,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2001/4273/wri01-4273.pdf","text":"Report","size":"1.5 MB","linkFileType":{"id":1,"text":"pdf"},"description":"PDF of report"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Lower Columbia River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.48657226562499,\n              45.61403741135093\n            ],\n            [\n              -122.18994140624999,\n              45.644768217751924\n            ],\n            [\n              -121.86035156249999,\n              45.740693395533064\n            ],\n            [\n              -121.53625488281249,\n              45.75985868785574\n            ],\n            [\n              -121.2176513671875,\n              45.729191061299936\n            ],\n            [\n              -121.0638427734375,\n              45.68315803253308\n            ],\n            [\n              -120.7452392578125,\n              45.77135470445036\n            ],\n            [\n              -120.56945800781249,\n              45.786679041363726\n            ],\n            [\n              -120.4046630859375,\n              45.706179285330855\n            ],\n            [\n              -120.45959472656249,\n              45.644768217751924\n            ],\n            [\n              -120.66284179687499,\n              45.66780526567164\n            ],\n            [\n              -120.92651367187499,\n              45.598665689820656\n            ],\n            [\n              -121.19567871093751,\n              45.54867850352087\n            ],\n            [\n              -121.3275146484375,\n              45.65628792636447\n            ],\n            [\n              -121.761474609375,\n              45.63324613981234\n            ],\n            [\n              -122.1844482421875,\n              45.521743896993634\n            ],\n            [\n              -122.76672363281249,\n              45.471688258104614\n            ],\n            [\n              -122.89306640624999,\n              45.706179285330855\n            ],\n            [\n              -122.93701171874999,\n              45.98169518512228\n            ],\n            [\n              -122.9974365234375,\n              46.09609080214316\n            ],\n            [\n              -123.1842041015625,\n              46.145588688591964\n            ],\n            [\n              -123.1622314453125,\n              46.195042108660154\n            ],\n            [\n              -122.92602539062501,\n              46.20264638061019\n            ],\n            [\n              -122.794189453125,\n              46.06560846138691\n            ],\n            [\n              -122.5909423828125,\n              45.775186183521036\n            ],\n            [\n              -122.48657226562499,\n              45.61403741135093\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"mailto:dc_or@usgs.gov\">Director, </a>Oregon Water Science Center<br />U.S. Geological Survey<br />2130 SW 5th Avenue<br />Portland, Oregon 97201<br /><a href=\"http://or.water.usgs.gov\" target=\"_blank\">http://or.water.usgs.gov </a></p>","tableOfContents":"<ul>\n<li>Introduction</li>\n<li>Methods of Data Collection</li>\n<li>Summary of Data Completeness and Quality</li>\n<li>Quality-Assurance Data</li>\n<li>Effects of Spill on Total Dissolved Gas</li>\n<li>Comparison of Total Dissolved Gas and Temperature to Water-Quality Standards</li>\n<li>Site-Specific Considerations</li>\n<li>References Cited</li>\n</ul>","publishedDate":"2002-03-06","noUsgsAuthors":false,"publicationDate":"2002-03-06","publicationStatus":"PW","scienceBaseUri":"4f4e4a8ae4b07f02db651468","contributors":{"authors":[{"text":"Tanner, Dwight Q.","contributorId":93452,"corporation":false,"usgs":true,"family":"Tanner","given":"Dwight","email":"","middleInitial":"Q.","affiliations":[],"preferred":false,"id":204518,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bragg, Heather M. hmbragg@usgs.gov","contributorId":428,"corporation":false,"usgs":true,"family":"Bragg","given":"Heather M.","email":"hmbragg@usgs.gov","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":204517,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":69371,"text":"i2749 - 2001 - Geologic map of the Winona Quadrangle, Shannon County, Missouri","interactions":[],"lastModifiedDate":"2012-02-10T00:11:32","indexId":"i2749","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2749","subseriesTitle":"GIS","title":"Geologic map of the Winona Quadrangle, Shannon County, Missouri","docAbstract":"The bedrock exposed in the Winona Quadrangle, Missouri, comprises Mesoproterozoic aged volcanic rocks overlain by Late Cambrian and Early Ordovician aged dolomite, sandstone, and chert. The sedimentary rocks are nearly flat-lying except where they drape around knobs of  the volcanic rocks or where they are adjacent to faults. The carbonates are karstified and the area contains numerous sinkholes, springs, caves, and losing-streams. \r\n\r\nThis map is one of several being produced under the U.S. Geological Survey National Cooperative Geologic Mapping Program to provide geologic data applicable to land-use problems in the Ozarks of south-central Missouri.  Ongoing and potential industrial and agricultural development in the Ozarks region has presented issues of ground-water quality in karst areas.  A National Park in this region (Ozark National Scenic Riverways, Missouri ) is concerned about the effects of activities in areas outside of their stewardship on the water resources that define the heart of this Park. This task applies geologic mapping and karst investigations to address issues surrounding competing land use in south-central Missouri. This task keeps geologists from the USGS associated with the park and allows the Parks to utilize USGS expertise and aid the NPS on how to effectively use geologic maps for Park management. For more information see:  http://geology.er.usgs.gov/eespteam/Karst/index.html","language":"ENGLISH","doi":"10.3133/i2749","usgsCitation":"Orndorff, R.C., and Harrison, R., 2001, Geologic map of the Winona Quadrangle, Shannon County, Missouri (Online version 1.0): U.S. Geological Survey IMAP 2749, Sheet 53 by 33 1/2 inch (in color, https://doi.org/10.3133/i2749.","productDescription":"Sheet 53 by 33 1/2 inch (in color","costCenters":[],"links":[{"id":110278,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_49739.htm","linkFileType":{"id":5,"text":"html"},"description":"49739"},{"id":191159,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6320,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i2749/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -91.36749999999999,37 ], [ -91.36749999999999,37.1175 ], [ -91.25,37.1175 ], [ -91.25,37 ], [ -91.36749999999999,37 ] ] ] } } ] }","edition":"Online version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db6889a0","contributors":{"authors":[{"text":"Orndorff, R. C.","contributorId":17613,"corporation":false,"usgs":true,"family":"Orndorff","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":280261,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harrison, R.W.","contributorId":32188,"corporation":false,"usgs":true,"family":"Harrison","given":"R.W.","affiliations":[],"preferred":false,"id":280262,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":31435,"text":"ofr01399 - 2001 - Initial findings; national survey of MTBE, other ether oxygenates, and other VOCs in community drinking-water sources","interactions":[],"lastModifiedDate":"2012-02-02T00:09:13","indexId":"ofr01399","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","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":"2001-399","title":"Initial findings; national survey of MTBE, other ether oxygenates, and other VOCs in community drinking-water sources","language":"ENGLISH","doi":"10.3133/ofr01399","usgsCitation":"Rowe, B.L., Grady, S., Zogorski, J.S., Koch, B., and Tratnyek, P., 2001, Initial findings; national survey of MTBE, other ether oxygenates, and other VOCs in community drinking-water sources: U.S. Geological Survey Open-File Report 2001-399, 1 poster : col. ill., col. map ; 62 x 91 cm., https://doi.org/10.3133/ofr01399.","productDescription":"1 poster : col. ill., col. map ; 62 x 91 cm.","costCenters":[],"links":[{"id":161483,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":59780,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2001/0399/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a02e4b07f02db5f809a","contributors":{"authors":[{"text":"Rowe, Barbara L. blrowe@usgs.gov","contributorId":2673,"corporation":false,"usgs":true,"family":"Rowe","given":"Barbara","email":"blrowe@usgs.gov","middleInitial":"L.","affiliations":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":205983,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grady, Stephen","contributorId":66314,"corporation":false,"usgs":true,"family":"Grady","given":"Stephen","affiliations":[],"preferred":false,"id":205985,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zogorski, John S. jszogors@usgs.gov","contributorId":189,"corporation":false,"usgs":true,"family":"Zogorski","given":"John","email":"jszogors@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":205982,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Koch, Bart","contributorId":22813,"corporation":false,"usgs":true,"family":"Koch","given":"Bart","email":"","affiliations":[],"preferred":false,"id":205984,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Tratnyek, Paul","contributorId":83173,"corporation":false,"usgs":true,"family":"Tratnyek","given":"Paul","affiliations":[],"preferred":false,"id":205986,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":30976,"text":"wri014201 - 2001 - The search for reliable aqueous solubility (Sw) and octanol-water partition coefficient (Kow) data for hydrophobic organic compounds; DDT and DDE as a case study","interactions":[],"lastModifiedDate":"2020-03-22T11:29:39","indexId":"wri014201","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","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":"2001-4201","title":"The search for reliable aqueous solubility (Sw) and octanol-water partition coefficient (Kow) data for hydrophobic organic compounds; DDT and DDE as a case study","docAbstract":"<p>The accurate determination of an organic contaminant’s physico-chemical properties is essential for predicting its environmental impact and fate. Approximately 700 publications (1944–2001) were reviewed and all known aqueous solubilities (S<sub>w</sub>) and octanol-water partition coefficients (K<sub>ow</sub>) for the organochlorine pesticide, DDT, and its persistent metabolite, DDE were compiled and examined. Two problems are evident with the available database: 1) egregious errors in reporting data and references, and 2) poor data quality and/or inadequate documentation of procedures. The published literature (particularly the collative literature such as compilation articles and handbooks) is characterized by a preponderance of unnecessary data duplication. Numerous data and citation errors are also present in the literature. The percentage of original S<sub>w</sub><span>&nbsp;</span>and K<sub>ow</sub><span>&nbsp;</span>data in compilations has decreased with time, and in the most recent publications (1994–97) it composes only 6–26 percent of the reported data. The variability of original DDT/DDE S<sub>w</sub><span>&nbsp;</span>and K<sub>ow</sub><span>&nbsp;</span>data spans 2–4 orders of magnitude, and there is little indication that the uncertainty in these properties has declined over the last 5 decades. A criteria-based evaluation of DDT/DDE S<sub>w</sub><span>&nbsp;</span>and K<sub>ow</sub><span>&nbsp;</span>data sources shows that 95–100 percent of the database literature is of poor or unevaluatable quality. The accuracy and reliability of the vast majority of the data are unknown due to inadequate documentation of the methods of determination used by the authors. [For example, estimates of precision have been reported for only 20 percent of experimental S<sub>w</sub><span>&nbsp;</span>data and 10 percent of experimental K<sub>ow</sub><span>&nbsp;</span>data.] Computational methods for estimating these parameters have been increasingly substituted for direct or indirect experimental determination despite the fact that the data used for model development and validation may be of unknown reliability. Because of the prevalence of errors, the lack of methodological documentation, and unsatisfactory data quality, the reliability of the DDT/ DDE S<sub>w</sub><span>&nbsp;</span>and K<sub>ow</sub><span>&nbsp;</span>database is questionable. The nature and extent of the errors documented in this study are probably indicative of a more general problem in the literature of hydrophobic organic compounds. Under these circumstances, estimation of critical environmental parameters on the basis of S<sub>w</sub><span>&nbsp;</span>and K<sub>ow</sub><span>&nbsp;</span>(for example, bioconcentration factors, equilibrium partition coefficients) is inadvisable because it will likely lead to incorrect environmental risk assessments. The current state of the database indicates that much greater efforts are needed to: 1) halt the proliferation of erroneous data and references, 2) initiate a coordinated program to develop improved methods of property determination, 3) establish and maintain consistent reporting requirements for physico-chemical property data, and 4) create a mechanism for archiving reliable data for widespread use in the scientific/regulatory community.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri014201","usgsCitation":"Pontolillo, J., and Eganhouse, R., 2001, The search for reliable aqueous solubility (Sw) and octanol-water partition coefficient (Kow) data for hydrophobic organic compounds; DDT and DDE as a case study: U.S. Geological Survey Water-Resources Investigations Report 2001-4201, 51 p. , https://doi.org/10.3133/wri014201.","productDescription":"51 p. ","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":159985,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2954,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri014201","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640d38","contributors":{"authors":[{"text":"Pontolillo, James jpontoli@usgs.gov","contributorId":2033,"corporation":false,"usgs":true,"family":"Pontolillo","given":"James","email":"jpontoli@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":204499,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eganhouse, R.P.","contributorId":67555,"corporation":false,"usgs":true,"family":"Eganhouse","given":"R.P.","email":"","affiliations":[],"preferred":false,"id":204500,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":31423,"text":"ofr01345 - 2001 - Investigation of dioxin concentrations in the lower Roanoke River basin, North Carolina, February 26-March 7, 2001","interactions":[],"lastModifiedDate":"2022-10-07T21:37:54.847592","indexId":"ofr01345","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","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":"2001-345","title":"Investigation of dioxin concentrations in the lower Roanoke River basin, North Carolina, February 26-March 7, 2001","docAbstract":"Dioxin is a toxic chemical that, when present in the environment, can cause cancer and birth defects in humans. Dioxin is of particular concern because concentrations of dioxin that were released into the environment many years ago remain a contributing factor to current exposure. Dioxin exposure often occurs in surface-water systems downstream from contaminated sites and is detrimental to aquatic life. For these reasons and because the U.S. Geological Survey has expertise in conducting high-volume dioxin sampling, the U.S. Environmental Protection Agency and the State of North Carolina asked the U.S. Geological Survey to collect water samples in the lower Roanoke River to be analyzed for the presence of dioxin.\r\n\r\nWater quality of the lower Roanoke River Basin in North Carolina was assessed at eight sites during February 26-March 7, 2001. Water- quality samples were collected for analysis of suspended-sediment and dioxin concentrations; high-volume (750-liter) water samples were collected for dioxin analysis. Discharge measurements were made at or near the high-volume sampling sites. Suspended-sediment sampling and water-quality measurements of specific conductance, pH, water temperature, and dissolved-oxygen concentrations made at each sampling site included multidepth measurements at two cross-section transects and hourly measurements at the point of high-volume sampling. Multidepth measurements were made near the surface, mid-depth, and near the bottom of the water column. These values were averaged for each cross section.\r\n\r\nDuring the sampling period, all sites sampled had dioxin concentrations above detection limits (1 part per quintillion) for both suspended and dissolved dioxin. Suspended dioxin ranged from 5.1 to 900 femtograms per liter, and dissolved dioxin values ranged from 0.31 to 41 femtograms per liter. Suspended-sediment concentrations ranged from 1.1 to 14 milligrams per liter. Specific conductance values ranges from 111 to 340 microsiemens per centimeter at 25 degrees Celsius. The range of pH values at the sampling sites was from 6.6 to 7.7. Water temperatures ranged from 8.9 to 13 degrees Celsius. Dissolved-oxygen concentrations ranged from 7.3 to 10.9 milligrams per liter.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr01345","usgsCitation":"Miller, K.F., and Walters, D.A., 2001, Investigation of dioxin concentrations in the lower Roanoke River basin, North Carolina, February 26-March 7, 2001: U.S. Geological Survey Open-File Report 2001-345, iv, 18 p., https://doi.org/10.3133/ofr01345.","productDescription":"iv, 18 p.","costCenters":[],"links":[{"id":408139,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_45798.htm","linkFileType":{"id":5,"text":"html"}},{"id":59777,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0345/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":161234,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2001/0345/report-thumb.jpg"}],"country":"United States","state":"North Carolina","otherGeospatial":"lower Roanoke River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.9,\n              35.808\n            ],\n            [\n              -76.682,\n              35.808\n            ],\n            [\n              -76.682,\n              36.056\n            ],\n            [\n              -76.9,\n              36.056\n            ],\n            [\n              -76.9,\n              35.808\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4880e4b07f02db51635c","contributors":{"authors":[{"text":"Miller, K. F.","contributorId":87153,"corporation":false,"usgs":true,"family":"Miller","given":"K.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":205959,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walters, D. A.","contributorId":21994,"corporation":false,"usgs":true,"family":"Walters","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":205958,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":31432,"text":"ofr01379 - 2001 - Water-quality, bed-sediment, and biological data (October 1999 through September 2000) and statistical summaries of data for streams in the upper Clark Fork basin, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:09:13","indexId":"ofr01379","displayToPublicDate":"2002-02-01T00:00:00","publicationYear":"2001","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":"2001-379","title":"Water-quality, bed-sediment, and biological data (October 1999 through September 2000) and statistical summaries of data for streams in the upper Clark Fork basin, Montana","language":"ENGLISH","doi":"10.3133/ofr01379","usgsCitation":"Dodge, K.A., Hornberger, M.I., and David, C.P., 2001, Water-quality, bed-sediment, and biological data (October 1999 through September 2000) and statistical summaries of data for streams in the upper Clark Fork basin, Montana: U.S. Geological Survey Open-File Report 2001-379, 95 p., https://doi.org/10.3133/ofr01379.","productDescription":"95 p.","costCenters":[],"links":[{"id":161480,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2001/0379/report-thumb.jpg"},{"id":59779,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0379/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e538b","contributors":{"authors":[{"text":"Dodge, K. A.","contributorId":40615,"corporation":false,"usgs":true,"family":"Dodge","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":205973,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hornberger, Michelle I. 0000-0002-7787-3446","orcid":"https://orcid.org/0000-0002-7787-3446","contributorId":23574,"corporation":false,"usgs":true,"family":"Hornberger","given":"Michelle","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":205972,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"David, C. P. C.","contributorId":76343,"corporation":false,"usgs":true,"family":"David","given":"C.","email":"","middleInitial":"P. C.","affiliations":[],"preferred":false,"id":205974,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}