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No abstract available.

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A.","contributorId":279873,"corporation":false,"usgs":false,"family":"Walker","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":835632,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":75733,"text":"wdrND052 - 2006 - Water resources data--North Dakota, water year 2005, Volume 2. Ground water","interactions":[],"lastModifiedDate":"2018-03-21T14:34:30","indexId":"wdrND052","displayToPublicDate":"2006-03-20T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"ND-05-2","title":"Water resources data--North Dakota, water year 2005, Volume 2. Ground water","docAbstract":"

Water-resources data for the 2005 water year for North Dakota consists of records of discharge, stage, and water quality for streams; contents, stage, and water quality for lakes and reservoirs; and water levels and water quality for ground-water wells. Volume 2 contains water-level records for 115 ground-water wells and water-quality records for 71 monitoring wells. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating Federal, State, and local agencies in North Dakota.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrND052","usgsCitation":"Robinson, S., and Rosenkranz, D., 2006, Water resources data--North Dakota, water year 2005, Volume 2. Ground water (Online only): U.S. Geological Survey Water Data Report ND-05-2, 104 p., https://doi.org/10.3133/wdrND052.","productDescription":"104 p.","numberOfPages":"104","onlineOnly":"Y","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":192826,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7033,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/2005/wdr-nd-05-2/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104,46 ], [ -104,49 ], [ -97.5,49 ], [ -97.5,46 ], [ -104,46 ] ] ] } } ] }","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60eb15","contributors":{"authors":[{"text":"Robinson, S.M.","contributorId":79162,"corporation":false,"usgs":true,"family":"Robinson","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":286946,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosenkranz, D.R.","contributorId":20024,"corporation":false,"usgs":true,"family":"Rosenkranz","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":286945,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":75753,"text":"ofr20051367 - 2006 - A Preliminary Investigation of The Structure of Southern Yucca Flat, Massachusetts Mountain, and CP Basin, Nevada Test Site, Nevada, Based on Geophysical Modeling","interactions":[],"lastModifiedDate":"2012-02-10T00:11:37","indexId":"ofr20051367","displayToPublicDate":"2006-03-20T00:00:00","publicationYear":"2006","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":"2005-1367","title":"A Preliminary Investigation of The Structure of Southern Yucca Flat, Massachusetts Mountain, and CP Basin, Nevada Test Site, Nevada, Based on Geophysical Modeling","docAbstract":"New gravity and magnetic data collected in the vicinity of Massachusetts Mountain and CP basin (Nevada Test Site, NV) provides a more complex view of the structural relationships present in the vicinity of CP basin than previous geologic models, helps define the position and extent of structures in southern Yucca Flat and CP basin, and better constrains the configuration of the basement structure separating CP basin and Frenchman Flat. The density and gravity modeling indicates that CP basin is a shallow, oval-shaped basin which trends north-northeast and contains ~800 m of basin-filling rocks and sediment at its deepest point in the northeast. CP basin is separated from the deeper Frenchman Flat basin by a subsurface ridge that may represent a Tertiary erosion surface at the top of the Paleozoic strata. The magnetic modeling indicates that the Cane Spring fault appears to merge with faults in northwest Massachusetts Mountain, rather than cut through to Yucca Flat basin and that the basin is downed-dropped relative to Massachusetts Mountain.\r\n\r\nThe magnetic modeling indicates volcanic units within Yucca Flat basin are down-dropped on the west and supports the interpretations of Phelps and KcKee (1999). The magnetic data indicate that the only faults that appear to be through-going from Yucca Flat into either Frenchman Flat or CP basin are the faults that bound the CP hogback. In general, the north-trending faults present along the length of Yucca Flat bend, merge, and disappear before reaching CP hogback and Massachusetts Mountain or French Peak.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr20051367","collaboration":"Prepared in cooperation with the U. S. Department of Energy, National Nuclear Security Administration, Nevada Site Office, Office of Environmental Management, under Interagency Agreement DE-AI52-01NV13944 Identification and /or Statement of Cooperation","usgsCitation":"Phelps, G., Justet, L., Moring, B.C., and Roberts, C.W., 2006, A Preliminary Investigation of The Structure of Southern Yucca Flat, Massachusetts Mountain, and CP Basin, Nevada Test Site, Nevada, Based on Geophysical Modeling (Version 1.1, Revised Mar 2008): U.S. Geological Survey Open-File Report 2005-1367, 36 p., https://doi.org/10.3133/ofr20051367.","productDescription":"36 p.","numberOfPages":"36","costCenters":[{"id":314,"text":"Geophysics Unit of Menlo Park, CA (GUMP)","active":false,"usgs":true}],"links":[{"id":192828,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7035,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1367/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.36749999999999,36.6175 ], [ -116.36749999999999,37.25 ], [ -115.86749999999999,37.25 ], [ -115.86749999999999,36.6175 ], [ -116.36749999999999,36.6175 ] ] ] } } ] }","edition":"Version 1.1, Revised Mar 2008","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4964e4b0b290850ef1e5","contributors":{"authors":[{"text":"Phelps, Geoffrey A.","contributorId":17262,"corporation":false,"usgs":true,"family":"Phelps","given":"Geoffrey A.","affiliations":[],"preferred":false,"id":286952,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Justet, Leigh ljustet@usgs.gov","contributorId":3367,"corporation":false,"usgs":true,"family":"Justet","given":"Leigh","email":"ljustet@usgs.gov","affiliations":[],"preferred":true,"id":286951,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moring, Barry C. 0000-0001-6797-9258 moring@usgs.gov","orcid":"https://orcid.org/0000-0001-6797-9258","contributorId":2794,"corporation":false,"usgs":true,"family":"Moring","given":"Barry","email":"moring@usgs.gov","middleInitial":"C.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":286950,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Roberts, Carter W.","contributorId":45282,"corporation":false,"usgs":true,"family":"Roberts","given":"Carter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":286953,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":75743,"text":"ofr20051313 - 2006 - Preliminary gravity inversion model of basins east of Yucca Flat, Nevada Test Site, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:14:01","indexId":"ofr20051313","displayToPublicDate":"2006-03-20T00:00:00","publicationYear":"2006","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":"2005-1313","title":"Preliminary gravity inversion model of basins east of Yucca Flat, Nevada Test Site, Nevada","language":"ENGLISH","doi":"10.3133/ofr20051313","usgsCitation":"Phelps, G., Roberts, C.W., and Moring, B.C., 2006, Preliminary gravity inversion model of basins east of Yucca Flat, Nevada Test Site, Nevada (Version 1.0): U.S. Geological Survey Open-File Report 2005-1313, 21 p., https://doi.org/10.3133/ofr20051313.","productDescription":"21 p.","numberOfPages":"21","costCenters":[],"links":[{"id":192827,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7034,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1313/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db673450","contributors":{"authors":[{"text":"Phelps, Geoffrey A.","contributorId":17262,"corporation":false,"usgs":true,"family":"Phelps","given":"Geoffrey A.","affiliations":[],"preferred":false,"id":286948,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roberts, Carter W.","contributorId":45282,"corporation":false,"usgs":true,"family":"Roberts","given":"Carter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":286949,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moring, Barry C. 0000-0001-6797-9258 moring@usgs.gov","orcid":"https://orcid.org/0000-0001-6797-9258","contributorId":2794,"corporation":false,"usgs":true,"family":"Moring","given":"Barry","email":"moring@usgs.gov","middleInitial":"C.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":286947,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":75613,"text":"sir20055235 - 2006 - A cyclostratigraphic and borehole-geophysical approach to development of a three-dimensional conceptual hydrogeologic model of the karstic Biscayne aquifer, southeastern Florida","interactions":[],"lastModifiedDate":"2020-03-27T06:47:15","indexId":"sir20055235","displayToPublicDate":"2006-03-18T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5235","title":"A cyclostratigraphic and borehole-geophysical approach to development of a three-dimensional conceptual hydrogeologic model of the karstic Biscayne aquifer, southeastern Florida","docAbstract":"

A fundamental problem in the simulation of karst ground-water flow and solute transport is how best to represent aquifer heterogeneity as defined by the spatial distribution of porosity, permeability, and storage. Combined analyses of cyclostratigraphy, including lithofacies and depositional environments, and borehole-geophysical logs, has improved the conceptualization of porosity, permeability, and storage within the triple-porosity karstic Biscayne aquifer in an approximately 95-square-mile study area of Miami-Dade County in southeastern Florida. The triple porosity of the Biscayne aquifer is principally: (1) matrix of interparticle and separate-vug porosity, providing much of the storage, and under dynamic conditions, diffuse-carbonate flow; (2) touching-vug porosity creating stratiform ground-water flow passageways; and (3) less common conduit porosity composed mainly of bedding-plane vugs, thin solution pipes, and cavernous vugs. These three conduit porosity types are all pathways for conduit ground-water flow.

To develop an accurate three-dimensional conceptual hydrogeologic model of the Biscayne aquifer in the study area, a detailed analysis of data was conducted that include continuously drilled cores, digital borehole images, borehole-fluid conductivity and temperature logs, and borehole-flowmeter measurements from 25 wells that fully penetrate the Biscayne aquifer. Six depositional environments for major lithologic components of the Biscayne aquifer--the Tamiami Formation, Fort Thompson Formation, and Miami Limestone--include: (1) middle ramp, (2) platform margin-to-outer platform, (3) open-marine platform interior, (4) restricted platform interior, (5) brackish platform interior, and (6) freshwater terrestrial environments. High-frequency cycles form the fundamental building blocks of the rocks composing the Biscayne aquifer. Vertical lithofacies successions, which have stacking patterns that reoccur, fit within the high-frequency cycles. Upward-shallowing subtidal cycles, upward-shallowing paralic cycles, and aggradational subtidal cycles define three types of ideal high-frequency cycles that occur within the Fort Thompson Formation and Miami Limestone. Based on vertical cycle patterns, high-frequency cycles group into two cycle sets: an older progradational cycle set and an overlying younger aggradational cycle.


A primary observation is that a predictable vertical pattern of porosity and permeability commonly exists within the three ideal cycles because the porosity and permeability relate directly to lithofacies. Sixteen major lithofacies of the Fort Thompson Formation and Miami Limestone have been assigned to one of three pore classes (I, II, and III). Touching-vug porosity and conduit porosity characterize pore class I, which commonly comprises the lower part of upward-shallowing cycles within the Fort Thompson Formation and an upper aggradational cycle of the Miami Limestone. Matrix porosity distinguishes pore class II, which commonly occurs in the upper part of the upward-shallowing subtidal cycles and middle part of the upward-shallowing paralic cycles. Micrite-dominated, leaky, low-permeability lithologies are characteristic of pore class III, which commonly caps upward-shallowing paralic cycles and occurs throughout much of a lower aggradational cycle of the Miami Limestone. These relations among lithofacies, cyclicity, and aquifer attributes (porosity, permeability, and storage) are crucial features of the architecture of a three-dimensional conceptual hydrogeologic model of the karstic Biscayne aquifer. This study shows that development of these relations is critical to producing a realistic cycle-based karstic aquifer framework for the Biscayne aquifer and for karst aquifers within other platform carbonates.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055235","usgsCitation":"Cunningham, K.J., Wacker, M.A., Robinson, E., Dixon, J.F., and Wingard, G.L., 2006, A cyclostratigraphic and borehole-geophysical approach to development of a three-dimensional conceptual hydrogeologic model of the karstic Biscayne aquifer, southeastern Florida: U.S. Geological Survey Scientific Investigations Report 2005-5235, Report: vi, 69 p.; Database, https://doi.org/10.3133/sir20055235.","productDescription":"Report: vi, 69 p.; Database","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"links":[{"id":121176,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2005_5235.jpg"},{"id":7015,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5235/","linkFileType":{"id":5,"text":"html"}},{"id":110631,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75769.htm","linkFileType":{"id":5,"text":"html"},"description":"75769"}],"country":"United States","state":"Florida","otherGeospatial":"Biscayne National Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.584716796875,\n 25.363882272740256\n ],\n [\n -80.85937499999999,\n 25.06569718553588\n ],\n [\n -80.17822265625,\n 25.21488107113259\n ],\n [\n -80.1507568359375,\n 25.903703303407667\n ],\n [\n -80.57922363281249,\n 25.849336891707605\n ],\n [\n -80.584716796875,\n 25.363882272740256\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af44f","contributors":{"authors":[{"text":"Cunningham, Kevin J. 0000-0002-2179-8686 kcunning@usgs.gov","orcid":"https://orcid.org/0000-0002-2179-8686","contributorId":1689,"corporation":false,"usgs":true,"family":"Cunningham","given":"Kevin","email":"kcunning@usgs.gov","middleInitial":"J.","affiliations":[{"id":269,"text":"FLWSC-Ft. Lauderdale","active":true,"usgs":true}],"preferred":true,"id":286913,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wacker, Michael A. mwacker@usgs.gov","contributorId":2162,"corporation":false,"usgs":true,"family":"Wacker","given":"Michael","email":"mwacker@usgs.gov","middleInitial":"A.","affiliations":[{"id":269,"text":"FLWSC-Ft. Lauderdale","active":true,"usgs":true}],"preferred":true,"id":286915,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Robinson, Edward","contributorId":99633,"corporation":false,"usgs":true,"family":"Robinson","given":"Edward","affiliations":[],"preferred":false,"id":286917,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dixon, Joann F. 0000-0001-9200-6407 jdixon@usgs.gov","orcid":"https://orcid.org/0000-0001-9200-6407","contributorId":1756,"corporation":false,"usgs":true,"family":"Dixon","given":"Joann","email":"jdixon@usgs.gov","middleInitial":"F.","affiliations":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true},{"id":5051,"text":"FLWSC-Orlando","active":true,"usgs":true},{"id":269,"text":"FLWSC-Ft. Lauderdale","active":true,"usgs":true}],"preferred":true,"id":286914,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wingard, G. Lynn 0000-0002-3833-5207 lwingard@usgs.gov","orcid":"https://orcid.org/0000-0002-3833-5207","contributorId":605,"corporation":false,"usgs":true,"family":"Wingard","given":"G.","email":"lwingard@usgs.gov","middleInitial":"Lynn","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":286916,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":75683,"text":"ofr20061069 - 2006 - Oregon geology — Parent of the soil, foundation for the vine","interactions":[],"lastModifiedDate":"2022-01-25T22:54:32.796484","indexId":"ofr20061069","displayToPublicDate":"2006-03-18T00:00:00","publicationYear":"2006","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":"2006-1069","title":"Oregon geology — Parent of the soil, foundation for the vine","docAbstract":"This presentation describes USGS geologic mapping in western Oregon, geologic map products, a thumbnail sketch of geologic history, a discussion of new mapping in progress in northwest Oregon, a tour of northwest Oregon geologic units, their relation to new American Viticultural Areas, and online sources of information.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061069","usgsCitation":"Wells, R., 2006, Oregon geology — Parent of the soil, foundation for the vine (Version 1.0): U.S. Geological Survey Open-File Report 2006-1069, 39 p., https://doi.org/10.3133/ofr20061069.","productDescription":"39 p.","numberOfPages":"39","costCenters":[],"links":[{"id":192783,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7028,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1069/","linkFileType":{"id":5,"text":"html"}},{"id":394853,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75776.htm"}],"country":"United States","state":"Oregon, Washington","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -124.5,\n 43\n ],\n [\n -120,\n 43\n ],\n [\n -120,\n 49\n ],\n [\n -124.5,\n 49\n ],\n [\n -124.5,\n 43\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e480ae4b07f02db4d2b96","contributors":{"authors":[{"text":"Wells, Ray 0000-0002-7796-0160","orcid":"https://orcid.org/0000-0002-7796-0160","contributorId":71260,"corporation":false,"usgs":true,"family":"Wells","given":"Ray","affiliations":[],"preferred":false,"id":286929,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":75643,"text":"sir20055199 - 2006 - Trends in streamflow on the Humboldt River between Elko and Imlay, Nevada, 1950-99","interactions":[],"lastModifiedDate":"2012-02-02T00:14:01","indexId":"sir20055199","displayToPublicDate":"2006-03-18T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5199","title":"Trends in streamflow on the Humboldt River between Elko and Imlay, Nevada, 1950-99","language":"ENGLISH","doi":"10.3133/sir20055199","usgsCitation":"Prudic, D.E., Niswonger, R., and Plume, R.W., 2006, Trends in streamflow on the Humboldt River between Elko and Imlay, Nevada, 1950-99 (Online only, Version 1.0): U.S. Geological Survey Scientific Investigations Report 2005-5199, x, 58 p.: ill., https://doi.org/10.3133/sir20055199.","productDescription":"x, 58 p.: ill.","numberOfPages":"68","onlineOnly":"Y","costCenters":[],"links":[{"id":192691,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7024,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5199/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only, Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db626066","contributors":{"authors":[{"text":"Prudic, David E. deprudic@usgs.gov","contributorId":3430,"corporation":false,"usgs":true,"family":"Prudic","given":"David","email":"deprudic@usgs.gov","middleInitial":"E.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":286921,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Niswonger, Richard G.","contributorId":45402,"corporation":false,"usgs":true,"family":"Niswonger","given":"Richard G.","affiliations":[],"preferred":false,"id":286922,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Plume, Russell W. rwplume@usgs.gov","contributorId":2303,"corporation":false,"usgs":true,"family":"Plume","given":"Russell","email":"rwplume@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":286920,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":75663,"text":"sir20055259 - 2006 - Predicting the vulnerability of streams to episodic acidification and potential effects on aquatic biota in Shenandoah National Park, Virginia","interactions":[],"lastModifiedDate":"2017-01-19T14:53:52","indexId":"sir20055259","displayToPublicDate":"2006-03-18T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5259","title":"Predicting the vulnerability of streams to episodic acidification and potential effects on aquatic biota in Shenandoah National Park, Virginia","docAbstract":"

Acidic deposition is one of the most serious environmental problems affecting Shenandoah National Park in north-central Virginia. The park is the third most contaminated park in the National Park System because of the deposition of acid rain. Acid rain affects headwater streams in the park by temporarily reducing the acid-neutralizing capacity (ANC) of the water, a process termed episodic acidification. In turn, the increase in acidic components in streamwater can have deleterious effects on the aquatic biota.

Although acidic deposition to the park is relatively uniform across its land area, the water-quality response of streamwater during rain events varies substantially. This response is a function of the underlying geology and topographic attributes of watersheds.

Geologic and topographic data for the park's 231 watersheds are readily available; however, long-term (years and tens of years) measurements of streamwater ANC and accompanying discharge are not and would be prohibitively expensive to collect. Modeled predictions of the vulnerability of the park's streams to episodic acidification are an alternative to long-term water-quality monitoring. These predictions can aid park officials in making management decisions.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Richmond, VA","doi":"10.3133/sir20055259","collaboration":"Prepared in cooperation with National Park Service","usgsCitation":"Rice, K.C., Deviney, F.A., Hornberger, G., and Webb, J., 2006, Predicting the vulnerability of streams to episodic acidification and potential effects on aquatic biota in Shenandoah National Park, Virginia: U.S. Geological Survey Scientific Investigations Report 2005-5259, vii, 51 p., https://doi.org/10.3133/sir20055259.","productDescription":"vii, 51 p.","numberOfPages":"61","costCenters":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"links":[{"id":192733,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":333049,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5259/sir05_5259.pdf"},{"id":7026,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5259/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Virginia","otherGeospatial":"Shenandoah National Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -78.20068359374999,\n 38.6275996886131\n ],\n [\n -78.1512451171875,\n 38.7283759182398\n ],\n [\n -78.12103271484375,\n 38.76693348394693\n ],\n [\n -78.1182861328125,\n 38.86109762182888\n ],\n [\n -78.19244384765625,\n 38.92522904714054\n ],\n [\n -78.25286865234375,\n 38.86965182408357\n ],\n [\n -78.24188232421875,\n 38.83756825896614\n ],\n [\n -78.30230712890624,\n 38.841846903808985\n ],\n [\n -78.3929443359375,\n 38.77121637244273\n ],\n [\n -78.4259033203125,\n 38.713375686254714\n ],\n [\n -78.3984375,\n 38.638327308061875\n ],\n [\n -78.4918212890625,\n 38.55031345037904\n ],\n [\n -78.5577392578125,\n 38.567495358827344\n ],\n [\n -78.59344482421875,\n 38.51378825951165\n ],\n [\n -78.55224609374999,\n 38.436379603\n ],\n [\n -78.607177734375,\n 38.41271038284709\n ],\n [\n -78.71429443359375,\n 38.33088431959971\n ],\n [\n -78.80218505859375,\n 38.272688535980976\n ],\n [\n -78.826904296875,\n 38.21012996629426\n ],\n [\n -78.82965087890625,\n 38.13239618602294\n ],\n [\n -78.82415771484375,\n 38.07404145941957\n ],\n [\n -78.70330810546875,\n 38.1237539824224\n ],\n [\n -78.695068359375,\n 38.201496974020806\n ],\n [\n -78.56597900390625,\n 38.28131307922966\n ],\n [\n -78.45611572265625,\n 38.34381037525605\n ],\n [\n -78.37921142578125,\n 38.371808917147554\n ],\n [\n -78.3544921875,\n 38.44498466889473\n ],\n [\n -78.31054687499999,\n 38.50948995925553\n ],\n [\n -78.23638916015625,\n 38.55031345037904\n ],\n [\n -78.23638916015625,\n 38.59326051987162\n ],\n [\n -78.20068359374999,\n 38.6275996886131\n ]\n ]\n ]\n }\n }\n ]\n}\n","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e7ec","contributors":{"authors":[{"text":"Rice, Karen C. 0000-0002-9356-5443 kcrice@usgs.gov","orcid":"https://orcid.org/0000-0002-9356-5443","contributorId":1998,"corporation":false,"usgs":true,"family":"Rice","given":"Karen","email":"kcrice@usgs.gov","middleInitial":"C.","affiliations":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"preferred":false,"id":286927,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Deviney, Frank A.","contributorId":22447,"corporation":false,"usgs":true,"family":"Deviney","given":"Frank","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":286924,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hornberger, George M.","contributorId":63894,"corporation":false,"usgs":true,"family":"Hornberger","given":"George M.","affiliations":[],"preferred":false,"id":286925,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Webb, James R.","contributorId":74431,"corporation":false,"usgs":true,"family":"Webb","given":"James R.","affiliations":[],"preferred":false,"id":286926,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":75723,"text":"sir20055278 - 2006 - Geophysical framework based on analysis of aeromagnetic and gravity data, upper and middle Verde River watershed, Yavapai County, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:14:01","indexId":"sir20055278","displayToPublicDate":"2006-03-18T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5278","title":"Geophysical framework based on analysis of aeromagnetic and gravity data, upper and middle Verde River watershed, Yavapai County, Arizona","language":"ENGLISH","doi":"10.3133/sir20055278","usgsCitation":"Langenheim, V., DeWitt, E., and Wirt, L., 2006, Geophysical framework based on analysis of aeromagnetic and gravity data, upper and middle Verde River watershed, Yavapai County, Arizona (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2005-5278, iv, 25 p. report: ill., maps; 1 plate, 33 x 25 in., https://doi.org/10.3133/sir20055278.","productDescription":"iv, 25 p. report: ill., maps; 1 plate, 33 x 25 in.","numberOfPages":"29","costCenters":[],"links":[{"id":192825,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7032,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5278/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c160","contributors":{"authors":[{"text":"Langenheim, Vicki E. 0000-0003-2170-5213","orcid":"https://orcid.org/0000-0003-2170-5213","contributorId":69662,"corporation":false,"usgs":true,"family":"Langenheim","given":"Vicki E.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":286944,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeWitt, Ed","contributorId":65081,"corporation":false,"usgs":true,"family":"DeWitt","given":"Ed","affiliations":[],"preferred":false,"id":286943,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wirt, Laurie","contributorId":13204,"corporation":false,"usgs":true,"family":"Wirt","given":"Laurie","affiliations":[],"preferred":false,"id":286942,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":75673,"text":"ofr20061045 - 2006 - Geology, hydrology, and water quality of the glacial drift aquifer in the vicinity of the Nelson landfill near Yorkville, Illinois","interactions":[],"lastModifiedDate":"2019-03-20T10:47:05","indexId":"ofr20061045","displayToPublicDate":"2006-03-18T00:00:00","publicationYear":"2006","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":"2006-1045","displayTitle":"Geology, Hydrology, and Water Quality of the Glacial Drift Aquifer in the Vicinity of the Nelson Landfill near Yorkville, Illinois","title":"Geology, hydrology, and water quality of the glacial drift aquifer in the vicinity of the Nelson landfill near Yorkville, Illinois","docAbstract":"

The geologic and hydrologic characteristics of the sand-and-gravel deposits that compose the glacial drift aquifer in the vicinity of the Nelson Landfill site in Yorkville, Illinois indicate that the aquifer could be developed as a source of public water supply. The geology of these deposits within the Newark Bedrock Valley is complex, however, and a detailed investigation of their water bearing and transmitting properties will be required to successfully locate high-capacity wells.

Volatile organic compounds, pesticides, and cyanide were not detected in ground water during this investigation. Metals and nitrogen compounds were not detected at concentrations above their Maximum Contaminant Level. Iron, manganese, and aluminum were detected at concentrations above their Secondary Maximum Con-taminant Level and various constituents were detected at concentrations above background levels downgradient of the landfill. Nitrate and ammonia, presumably derived from agricultural practices, also were detected in samples from locations hydraulically upgradient of the landfill.

Oxidation-reduction conditions in the aquifer become more reducing with depth. This change is reflected by a change in the type of nitrogen compound detected and the concentration of dissolved oxygen and iron in the glacial drift aquifer. Concentrations of some of the major ions and metals may be affected by dissolution of carbonate minerals in the aquifer and perhaps road salts.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20061045","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency and the United City of Yorkville, Illinois","usgsCitation":"Kay, R.T., 2006, Geology, hydrology, and water quality of the glacial drift aquifer in the vicinity of the Nelson landfill near Yorkville, Illinois (Online only): U.S. Geological Survey Open-File Report 2006-1045, v, 32 p., https://doi.org/10.3133/ofr20061045.","productDescription":"v, 32 p.","numberOfPages":"38","onlineOnly":"Y","costCenters":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"links":[{"id":192734,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":362136,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2006/1045/pdf/ofr20061045.pdf","text":"Report","size":"1.59 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2006–1045"},{"id":7027,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1045/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89,41 ], [ -89,42 ], [ -88,42 ], [ -88,41 ], [ -89,41 ] ] ] } } ] }","edition":"Online only","contact":"

Director, Central Midwest Water Science Center
U.S. Geological Survey
405 North Goodwin
Urbana, IL 61801

","tableOfContents":"","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db6886da","contributors":{"authors":[{"text":"Kay, Robert T. 0000-0002-6281-8997 rtkay@usgs.gov","orcid":"https://orcid.org/0000-0002-6281-8997","contributorId":1122,"corporation":false,"usgs":true,"family":"Kay","given":"Robert","email":"rtkay@usgs.gov","middleInitial":"T.","affiliations":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"preferred":true,"id":286928,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":75603,"text":"ofr20061047 - 2006 - Field comparison of optical and Clark cell dissolved oxygen sensors in the Tualatin River, Oregon, 2005","interactions":[],"lastModifiedDate":"2012-02-02T00:13:49","indexId":"ofr20061047","displayToPublicDate":"2006-03-18T00:00:00","publicationYear":"2006","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":"2006-1047","title":"Field comparison of optical and Clark cell dissolved oxygen sensors in the Tualatin River, Oregon, 2005","language":"ENGLISH","doi":"10.3133/ofr20061047","usgsCitation":"Johnston, M.W., and Williams, J.S., 2006, Field comparison of optical and Clark cell dissolved oxygen sensors in the Tualatin River, Oregon, 2005 (Online only): U.S. Geological Survey Open-File Report 2006-1047, 15 p., https://doi.org/10.3133/ofr20061047.","productDescription":"15 p.","numberOfPages":"15","onlineOnly":"Y","costCenters":[],"links":[{"id":186341,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7014,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1047/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fce4b07f02db5f5a7f","contributors":{"authors":[{"text":"Johnston, Matthew W. mattj@usgs.gov","contributorId":3066,"corporation":false,"usgs":true,"family":"Johnston","given":"Matthew","email":"mattj@usgs.gov","middleInitial":"W.","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":286912,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, John S. johnw@usgs.gov","contributorId":329,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"johnw@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":286911,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":75653,"text":"sir20065002 - 2006 - Low-flow analysis and selected flow statistics representative of 1930-2002 for streamflow-gaging stations in or near West Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:14:01","indexId":"sir20065002","displayToPublicDate":"2006-03-18T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5002","title":"Low-flow analysis and selected flow statistics representative of 1930-2002 for streamflow-gaging stations in or near West Virginia","docAbstract":"Five time periods between 1930 and 2002 are identified as having distinct patterns of annual minimum daily mean flows (minimum flows). Average minimum flows increased around 1970 at many streamflow-gaging stations in West Virginia. Before 1930, however, there might have been a period of minimum flows greater than any period identified between 1930 and 2002. The effects of climate variability are probably the principal causes of the differences among the five time periods. \r\n\r\nComparisons of selected streamflow statistics are made between values computed for the five identified time periods and values computed for the 1930-2002 interval for 15 streamflow-gaging stations. The average difference between statistics computed for the five time periods and the 1930-2002 interval decreases with increasing magnitude of the low-flow statistic. The greatest individual-station absolute difference was 582.5 percent greater for the 7-day 10-year low flow computed for 1970-1979 compared to the value computed for 1930-2002. The hydrologically based low flows indicate approximately equal or smaller absolute differences than biologically based low flows. The average 1-day 3-year biologically based low flow (1B3) and 4-day 3-year biologically based low flow (4B3) are less than the average 1-day 10-year hydrologically based low flow (1Q10) and 7-day 10-year hydrologic-based low flow (7Q10) respectively, and range between 28.5 percent less and 13.6 percent greater. Seasonally, the average difference between low-flow statistics computed for the five time periods and 1930-2002 is not consistent between magnitudes of low-flow statistics, and the greatest difference is for the summer (July 1-September 30) and fall (October 1-December 31) for the same time period as the greatest difference determined in the annual analysis. The greatest average difference between 1B3 and 4B3 compared to 1Q10 and 7Q10, respectively, is in the spring (April 1-June 30), ranging between 11.6 and 102.3 percent greater. \r\n\r\nStatistics computed for the individual station's record period may not represent the statistics computed for the period 1930 to 2002 because (1) station records are available predominantly after about 1970 when minimum flows were greater than the average between 1930 and 2002 and (2) some short-term station records are mostly during dry periods, whereas others are mostly during wet periods. A criterion-based sampling of the individual station's record periods at stations was taken to reduce the effects of statistics computed for the entire record periods not representing the statistics computed for 1930-2002. The criterion used to sample the entire record periods is based on a comparison between the regional minimum flows and the minimum flows at the stations. Criterion-based sampling of the available record periods was superior to record-extension techniques for this study because more stations were selected and areal distribution of stations was more widespread. Principal component and correlation analyses of the minimum flows at 20 stations in or near West Virginia identify three regions of the State encompassing stations with similar patterns of minimum flows: the Lower Appalachian Plateaus, the Upper Appalachian Plateaus, and the Eastern Panhandle. All record periods of 10 years or greater between 1930 and 2002 where the average of the regional minimum flows are nearly equal to the average for 1930-2002 are determined as representative of 1930-2002. Selected statistics are presented for the longest representative record period that matches the record period for 77 stations in West Virginia and 40 stations near West Virginia. These statistics can be used to develop equations for estimating flow in ungaged stream locations. \r\n\r\n","language":"ENGLISH","doi":"10.3133/sir20065002","usgsCitation":"Wiley, J.B., 2006, Low-flow analysis and selected flow statistics representative of 1930-2002 for streamflow-gaging stations in or near West Virginia: U.S. Geological Survey Scientific Investigations Report 2006-5002, vi, 190 p., https://doi.org/10.3133/sir20065002.","productDescription":"vi, 190 p.","numberOfPages":"196","costCenters":[],"links":[{"id":192692,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7025,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5002/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a75e4b07f02db644a1f","contributors":{"authors":[{"text":"Wiley, Jeffrey B.","contributorId":59746,"corporation":false,"usgs":true,"family":"Wiley","given":"Jeffrey","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":286923,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":75713,"text":"wdrIL051 - 2006 - Water Resources Data for Illinois - Water Year 2005 (Includes Historical Data)","interactions":[],"lastModifiedDate":"2012-03-08T17:16:18","indexId":"wdrIL051","displayToPublicDate":"2006-03-18T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"IL-05-1","title":"Water Resources Data for Illinois - Water Year 2005 (Includes Historical Data)","docAbstract":"This annual Water-Data Report for Illinois contains current water year (Oct. 1, 2004, to Sept. 30, 2005) and historical data of discharge, stage, water quality and biology of streams; stage of lakes and reservoirs; levels and quality of ground water; and records of precipitation, air temperature, dew point, solar radiation, and wind speed. The current year's (2005) data provided in this report include (1) discharge for 182 surface-water gaging stations and for 9 crest-stage partial-record stations; (2) stage for 33 surface-water gaging stations; (3) water-quality records for 10 surface-water stations; (4) sediment-discharge records for 14 surface-water stations; (5) water-level records for 98 ground-water wells; (6) water-quality records for 17 ground-water wells; (7) precipitation records for 48 rain gages; (8) records of air temperature, dew point, solar radiation and wind speed for 1 meteorological station; and (9) biological records for 6 sample sites. Also included are miscellaneous data collected at various sites not in the systematic data-collection network.\r\n\r\nData were collected and compiled as a part of the National Water Information System (NWIS) maintained by the U.S. Geological Survey in cooperation with Federal, State, and local agencies.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/wdrIL051","collaboration":"Prepared in cooperation with the State of Illinois and with other agencies","usgsCitation":"LaTour, J., Weldon, E., Dupre, D., and Halfar, T., 2006, Water Resources Data for Illinois - Water Year 2005 (Includes Historical Data): U.S. Geological Survey Water Data Report IL-05-1, Available online and on CD-ROM; PDF Report: 2144 p., https://doi.org/10.3133/wdrIL051.","productDescription":"Available online and on CD-ROM; PDF Report: 2144 p.","numberOfPages":"2144","onlineOnly":"N","additionalOnlineFiles":"Y","temporalStart":"2004-10-01","temporalEnd":"2005-09-30","costCenters":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"links":[{"id":192824,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7031,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/2005/wdr-il-05/start.htm","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -91.5,36.916666666666664 ], [ -91.5,42.5 ], [ -87.5,42.5 ], [ -87.5,36.916666666666664 ], [ -91.5,36.916666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcebb","contributors":{"authors":[{"text":"LaTour, J.K.","contributorId":30257,"corporation":false,"usgs":true,"family":"LaTour","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":286939,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weldon, E.A.","contributorId":66345,"corporation":false,"usgs":true,"family":"Weldon","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":286940,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dupre, D.H.","contributorId":89237,"corporation":false,"usgs":true,"family":"Dupre","given":"D.H.","email":"","affiliations":[],"preferred":false,"id":286941,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Halfar, T.M.","contributorId":9729,"corporation":false,"usgs":true,"family":"Halfar","given":"T.M.","email":"","affiliations":[],"preferred":false,"id":286938,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":75693,"text":"ofr20061028 - 2006 - Calibration of PS09, PS10, and PS11 trans-Alaska pipeline system strong-motion instruments, with acceleration, velocity, and displacement records of the Denali fault earthquake, 03 November 2002","interactions":[],"lastModifiedDate":"2012-02-02T00:14:01","indexId":"ofr20061028","displayToPublicDate":"2006-03-18T00:00:00","publicationYear":"2006","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":"2006-1028","title":"Calibration of PS09, PS10, and PS11 trans-Alaska pipeline system strong-motion instruments, with acceleration, velocity, and displacement records of the Denali fault earthquake, 03 November 2002","docAbstract":"In September, 2003, the Alyeska Pipeline Service Company (APSC) and the U.S. Geological Survey (USGS) embarked on a joint effort to extract, test, and calibrate the accelerometers, amplifiers, and bandpass filters from the earthquake monitoring systems (EMS) at Pump Stations 09, 10, and 11 of the Trans-Alaska Pipeline System (TAPS). These were the three closest strong-motion seismographs to the Denali fault when it ruptured in the MW 7.9 earthquake of 03 November 2002 (22:12:41 UTC). The surface rupture is only 3.0 km from PS10 and 55.5 km from PS09 but PS11 is 124.2 km away from a small rupture splay and 126.9 km from the main trace. Here we briefly describe precision calibration results for all three instruments. Included with this report is a link to the seismograms reprocessed using these new calibrations: \r\n\r\nhttp://nsmp.wr.usgs.gov/data_sets/20021103_2212_taps.html \r\n\r\nCalibration information in this paper applies at the time of the Denali fault earthquake (03 November 2002), but not necessarily at other times because equipment at these stations is changed by APSC personnel at irregular intervals. In particular, the equipment at PS09, PS10, and PS11 was changed by our joint crew in September, 2003, so that we could perform these calibrations. The equipment stayed the same from at least the time of the earthquake until that retrieval, and these calibrations apply for that interval. ","language":"ENGLISH","doi":"10.3133/ofr20061028","usgsCitation":"Evans, J.R., Jensen, E.G., Sell, R., Stephens, C.D., Nyman, D.J., Hamilton, R.C., and Hager, W.C., 2006, Calibration of PS09, PS10, and PS11 trans-Alaska pipeline system strong-motion instruments, with acceleration, velocity, and displacement records of the Denali fault earthquake, 03 November 2002 (Version 1.0): U.S. Geological Survey Open-File Report 2006-1028, 55 p.: ill.; seismograms, https://doi.org/10.3133/ofr20061028.","productDescription":"55 p.: ill.; seismograms","numberOfPages":"55","costCenters":[],"links":[{"id":192784,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7029,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1028/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f954e","contributors":{"authors":[{"text":"Evans, John R. jrevans@usgs.gov","contributorId":529,"corporation":false,"usgs":true,"family":"Evans","given":"John","email":"jrevans@usgs.gov","middleInitial":"R.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":286930,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jensen, E. 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2006 - The Rabaul Volcano Observatory real-time GPS upgrade","interactions":[],"lastModifiedDate":"2012-02-02T00:14:01","indexId":"ofr20051232","displayToPublicDate":"2006-03-18T00:00:00","publicationYear":"2006","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":"2005-1232","title":"The Rabaul Volcano Observatory real-time GPS upgrade","language":"ENGLISH","doi":"10.3133/ofr20051232","usgsCitation":"Endo, E., 2006, The Rabaul Volcano Observatory real-time GPS upgrade: U.S. Geological Survey Open-File Report 2005-1232, 65 p., https://doi.org/10.3133/ofr20051232.","productDescription":"65 p.","numberOfPages":"65","costCenters":[],"links":[{"id":192785,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7030,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1232/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ace4","contributors":{"authors":[{"text":"Endo, Eliot","contributorId":6958,"corporation":false,"usgs":true,"family":"Endo","given":"Eliot","email":"","affiliations":[],"preferred":false,"id":286937,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":75623,"text":"sir20055279 - 2006 - Water quality and possible sources of nitrogen and bacteria to rock and travertine creeks, Chickasaw National Recreation Area, Oklahoma, 2004","interactions":[],"lastModifiedDate":"2012-02-02T00:13:49","indexId":"sir20055279","displayToPublicDate":"2006-03-18T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5279","title":"Water quality and possible sources of nitrogen and bacteria to rock and travertine creeks, Chickasaw National Recreation Area, Oklahoma, 2004","language":"ENGLISH","doi":"10.3133/sir20055279","usgsCitation":"Becker, C., 2006, Water quality and possible sources of nitrogen and bacteria to rock and travertine creeks, Chickasaw National Recreation Area, Oklahoma, 2004: U.S. Geological Survey Scientific Investigations Report 2005-5279, iv, 24 p., https://doi.org/10.3133/sir20055279.","productDescription":"iv, 24 p.","numberOfPages":"28","costCenters":[],"links":[{"id":7016,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5279/","linkFileType":{"id":5,"text":"html"}},{"id":186342,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9b72","contributors":{"authors":[{"text":"Becker, Carol 0000-0001-6652-4542 cjbecker@usgs.gov","orcid":"https://orcid.org/0000-0001-6652-4542","contributorId":2489,"corporation":false,"usgs":true,"family":"Becker","given":"Carol","email":"cjbecker@usgs.gov","affiliations":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"preferred":true,"id":286918,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70140091,"text":"70140091 - 2006 - Impacts on water quality and biota from natural acid rock drainage in Colorado's Lake Creek watershed","interactions":[],"lastModifiedDate":"2016-07-14T13:49:16","indexId":"70140091","displayToPublicDate":"2006-03-16T13:15:00","publicationYear":"2006","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Impacts on water quality and biota from natural acid rock drainage in Colorado's Lake Creek watershed","docAbstract":"

Colorado's Lake Creek watershed hosts natural acid rock drainage that significantly impacts surface water, streambed sediment, and aquatic life. The source of the ARD is a group of iron-rich springs that emerge from intensely hydrothermally altered, unexploited, low-grade porphyry copper mineralization in the Grizzly Peak Caldera. Source water chemistry includes pH of 2.5 and dissolved metal concentrations of up to 277 mg/L aluminum, 498 mg/L iron, and 10 mg/L copper. From the hydrothermally altered area downstream for 27 kilometers to Twin Lakes Reservoir, metal concentrations in streambed sediment are elevated and the watershed experiences locally severe adverse impacts to aquatic life due to the acidic, metal-laden water. The water and sediment quality of Twin Lakes Reservoir is sufficiently improved that the reservoir supports a trout fishery, and remnants of upstream ARD are negligible.

","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings from the Seventh International Conference on Acid Rock Drainage","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Seventh International Conference on Acid Rock Drainage","conferenceDate":"March 26, 2006","conferenceLocation":"St. Louis, MO","language":"English","publisher":"American Society of Mining and Reclamation","publisherLocation":"Lexington, KY","usgsCitation":"Bird, D., Sares, M.A., Policky, G.A., Schmidt, T., and Church, S.E., 2006, Impacts on water quality and biota from natural acid rock drainage in Colorado's Lake Creek watershed, in Proceedings from the Seventh International Conference on Acid Rock Drainage, St. Louis, MO, March 26, 2006, p. 158-126.","productDescription":"29 p.","startPage":"158","endPage":"126","numberOfPages":"29","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":297721,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.061279296875,\n 36.99377838872517\n ],\n [\n -109.061279296875,\n 41.0130657870063\n ],\n [\n -102.041015625,\n 41.0130657870063\n ],\n [\n -102.041015625,\n 36.99377838872517\n ],\n [\n -109.061279296875,\n 36.99377838872517\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54dd2bd1e4b08de9379b34f3","contributors":{"authors":[{"text":"Bird, D.A.","contributorId":53989,"corporation":false,"usgs":true,"family":"Bird","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":539777,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sares, Matthew A.","contributorId":139021,"corporation":false,"usgs":false,"family":"Sares","given":"Matthew","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":539778,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Policky, Greg A.","contributorId":139022,"corporation":false,"usgs":false,"family":"Policky","given":"Greg","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":539779,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Schmidt, Travis S. 0000-0003-1400-0637 tschmidt@usgs.gov","orcid":"https://orcid.org/0000-0003-1400-0637","contributorId":1300,"corporation":false,"usgs":true,"family":"Schmidt","given":"Travis S.","email":"tschmidt@usgs.gov","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":685,"text":"Wyoming-Montana Water Science Center","active":false,"usgs":true},{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true},{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":539780,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Church, Stan E. schurch@usgs.gov","contributorId":803,"corporation":false,"usgs":true,"family":"Church","given":"Stan","email":"schurch@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":false,"id":539781,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70176793,"text":"70176793 - 2006 - Source parameters of microearthquakes at Mount St Helens (USA)","interactions":[],"lastModifiedDate":"2016-10-05T17:13:11","indexId":"70176793","displayToPublicDate":"2006-03-16T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1803,"text":"Geophysical Journal International","active":true,"publicationSubtype":{"id":10}},"title":"Source parameters of microearthquakes at Mount St Helens (USA)","docAbstract":"

We estimate the source parameters for a selection of microearthquakes that occurred at Mount St Helens in the period 1995–1998. Excluding the activity of 2004 September, this time period includes the most intense episode of earthquake activity since the last dome-building eruption in 1986 October. 200 seismograms were processed to obtain seismic moments, source radii, stress drops and average fault slip. The source parameters were determined from the spectral analysis of P waves, after correction for attenuation and site effects. In particular, P-wave quality (Qp) and site (S) factors have been previously calculated in the frequency ranges 2–7 Hz and 18–30 Hz. Because it was impossible to perform corrections for Qp and S over the whole spectrum we applied a new approach, based on the notion of ‘holed spectrum’, to estimate spectral parameters. The term ‘holed spectrum’ indicates a spectrum lacking corrected spectral amplitude values at certain frequencies. We carried out a statistical study to verify that dealing with the ‘holed spectrum’ does not lead to significant differences in the estimates of spectral parameters. We also investigated the dependence of spectral parameters (low-frequency level, corner frequency and high-frequency decay) on the bandwidth of spectral hole, and defined the threshold values for three different spectral models. Displacement ‘holed spectra’, corrected by attenuation and site response, are then used to determine spectral parameters in order to calculate seismic source parameters. Seismic moments range from 1017 to 1019 dyne-cm, source dimensions from 100 to 350 m, and average fault slip from 0.003 to 0.1 cm. Self-similarity seems to break down in that stress drops are very low (0.1–1 bars). We postulate that seismicity is associated with a brittle shear failure mechanism occurring in a highly heterogeneous material under a relatively low stress regime.

","language":"English","publisher":"The Royal Astronomical Society","doi":"10.1111/j.1365-246X.2006.03025.x","usgsCitation":"Tusa, G., Brancato, A., Gresta, S., and Malone, S.D., 2006, Source parameters of microearthquakes at Mount St Helens (USA): Geophysical Journal International, v. 166, no. 3, p. 1193-1223, https://doi.org/10.1111/j.1365-246X.2006.03025.x.","productDescription":"31 p.","startPage":"1193","endPage":"1223","costCenters":[],"links":[{"id":477337,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1365-246x.2006.03025.x","text":"Publisher Index Page"},{"id":329356,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Mount St. Helens","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.4,\n 46.1\n ],\n [\n -122.4,\n 46.3\n ],\n [\n -122,\n 46.3\n ],\n [\n -122,\n 46.1\n ],\n [\n -122.4,\n 46.1\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"166","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57fe8d33e4b0824b2d14b0e9","contributors":{"authors":[{"text":"Tusa, Giuseppina","contributorId":175170,"corporation":false,"usgs":false,"family":"Tusa","given":"Giuseppina","email":"","affiliations":[],"preferred":false,"id":650329,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brancato, Alfonso","contributorId":175171,"corporation":false,"usgs":false,"family":"Brancato","given":"Alfonso","email":"","affiliations":[],"preferred":false,"id":650330,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gresta, Stefano","contributorId":175172,"corporation":false,"usgs":false,"family":"Gresta","given":"Stefano","email":"","affiliations":[],"preferred":false,"id":650331,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Malone, Stephen D.","contributorId":68135,"corporation":false,"usgs":true,"family":"Malone","given":"Stephen","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":650332,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":75583,"text":"fs20053140 - 2006 - Effects of post-wildfire sedimentation on leopard frog habitat in Saguaro National Park","interactions":[],"lastModifiedDate":"2012-02-02T00:13:49","indexId":"fs20053140","displayToPublicDate":"2006-03-16T00:00:00","publicationYear":"2006","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":"2005-3140","title":"Effects of post-wildfire sedimentation on leopard frog habitat in Saguaro National Park","language":"ENGLISH","doi":"10.3133/fs20053140","usgsCitation":"Parker, J.T., 2006, Effects of post-wildfire sedimentation on leopard frog habitat in Saguaro National Park (Version 1.0): U.S. Geological Survey Fact Sheet 2005-3140, 4 p., https://doi.org/10.3133/fs20053140.","productDescription":"4 p.","numberOfPages":"4","costCenters":[],"links":[{"id":121175,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3140.jpg"},{"id":7012,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3140/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611a64","contributors":{"authors":[{"text":"Parker, John T.C.","contributorId":18766,"corporation":false,"usgs":true,"family":"Parker","given":"John","email":"","middleInitial":"T.C.","affiliations":[],"preferred":false,"id":286905,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70171565,"text":"70171565 - 2006 - Endocrine disrupting chemicals research program of the U.S. Environmental Protection Agency: summary of a peer-review report","interactions":[],"lastModifiedDate":"2016-06-03T16:47:26","indexId":"70171565","displayToPublicDate":"2006-03-15T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1542,"text":"Environmental Health Perspectives","active":true,"publicationSubtype":{"id":10}},"title":"Endocrine disrupting chemicals research program of the U.S. Environmental Protection Agency: summary of a peer-review report","docAbstract":"

At the request of the U.S. Environmental Protection Agency (EPA) Office of Research and Development, a subcommittee of the Board of Scientific Counselors Executive Committee conducted an independent and open peer review of the Endocrine Disrupting Chemicals Research Program (EDC Research Program) of the U.S. EPA. The subcommittee was charged with reviewing the design, relevance, progress, scientific leadership, and resources of the program. The subcommittee found that the long-term goals and science questions in the EDC Program are appropriate and represent an understandable and solid framework for setting research priorities, representing a combination of problem-driven and core research. Long-term goal (LTG) 1, dealing with the underlying science surrounding endocrine disruptors, provides a solid scientific foundation for conducting risk assessments and making risk management decisions. LTG 2, dealing with defining the extent of the impact of endocrine-disrupting chemicals (EDCs), has shown greater progress on ecologic effects of EDCs compared with that on human health effects. LTG 3, which involves support of the Endocrine Disruptor Screening and Testing Program of the U.S. EPA, has two mammalian tests already through a validation program and soon available for use. Despite good progress, we recommend that the U.S. EPA a) strengthen their expertise in wildlife toxicology, b) expedite validation of the Endocrine Disruptors Screening and Testing Advisory Committee tests, c) continue dependable funding for the EDC Research Program, d) take a leadership role in the application of “omics” technologies to address many of the science questions critical for evaluating environmental and human health effects of EDCs, and e) continue to sponsor multidisciplinary intramural research and interagency collaborations.

","language":"English","publisher":"NCBI","doi":"10.1289/ehp.8875","usgsCitation":"Harding, A.K., Daston, G.P., Boyd, G.R., Lucier, G.W., Safe, S.H., Stewart, J., Tillitt, D.E., and Van Der Kraak, G., 2006, Endocrine disrupting chemicals research program of the U.S. Environmental Protection Agency: summary of a peer-review report: Environmental Health Perspectives, v. 114, no. 8, p. 1276-1282, https://doi.org/10.1289/ehp.8875.","productDescription":"7 p.","startPage":"1276","endPage":"1282","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":477338,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1289/ehp.8875","text":"Publisher Index Page"},{"id":322156,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"114","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5752aa30e4b053f0edd13e3a","contributors":{"authors":[{"text":"Harding, Anna K.","contributorId":170035,"corporation":false,"usgs":false,"family":"Harding","given":"Anna","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":631821,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Daston, George P.","contributorId":170020,"corporation":false,"usgs":false,"family":"Daston","given":"George","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":631822,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Boyd, Glen R.","contributorId":170036,"corporation":false,"usgs":false,"family":"Boyd","given":"Glen","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":631823,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lucier, George W.","contributorId":170037,"corporation":false,"usgs":false,"family":"Lucier","given":"George","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":631824,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Safe, Stephen H.","contributorId":170038,"corporation":false,"usgs":false,"family":"Safe","given":"Stephen","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":631825,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Stewart, Juarine","contributorId":170039,"corporation":false,"usgs":false,"family":"Stewart","given":"Juarine","email":"","affiliations":[],"preferred":false,"id":631826,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Tillitt, Donald E. 0000-0002-8278-3955 dtillitt@usgs.gov","orcid":"https://orcid.org/0000-0002-8278-3955","contributorId":1875,"corporation":false,"usgs":true,"family":"Tillitt","given":"Donald","email":"dtillitt@usgs.gov","middleInitial":"E.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":631827,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Van Der Kraak, Glen","contributorId":170040,"corporation":false,"usgs":false,"family":"Van Der Kraak","given":"Glen","email":"","affiliations":[],"preferred":false,"id":631828,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":75573,"text":"fs20053099 - 2006 - Age-dating ground water beneath Tinker Air Force Base, Midwest City, Oklahoma, 2003-04","interactions":[],"lastModifiedDate":"2020-01-26T16:17:26","indexId":"fs20053099","displayToPublicDate":"2006-03-14T00:00:00","publicationYear":"2006","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":"2005-3099","title":"Age-dating ground water beneath Tinker Air Force Base, Midwest City, Oklahoma, 2003-04","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs20053099","usgsCitation":"Christenson, S., Parkhurst, D., Hunt, A.G., and Athay, D., 2006, Age-dating ground water beneath Tinker Air Force Base, Midwest City, Oklahoma, 2003-04: U.S. Geological Survey Fact Sheet 2005-3099, 4 p., https://doi.org/10.3133/fs20053099.","productDescription":"4 p.","numberOfPages":"4","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":120965,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3099.jpg"},{"id":7516,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3099/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Oklahoma ","city":"Midwest City","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -97.44461059570312,\n 35.38513141280172\n ],\n [\n -97.34161376953125,\n 35.38513141280172\n ],\n [\n -97.34161376953125,\n 35.48247900534352\n ],\n [\n -97.44461059570312,\n 35.48247900534352\n ],\n [\n -97.44461059570312,\n 35.38513141280172\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db689477","contributors":{"authors":[{"text":"Christenson, Scott","contributorId":59128,"corporation":false,"usgs":true,"family":"Christenson","given":"Scott","affiliations":[],"preferred":false,"id":286904,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parkhurst, David","contributorId":33588,"corporation":false,"usgs":true,"family":"Parkhurst","given":"David","affiliations":[],"preferred":false,"id":286902,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hunt, Andrew G. 0000-0002-3810-8610 ahunt@usgs.gov","orcid":"https://orcid.org/0000-0002-3810-8610","contributorId":1582,"corporation":false,"usgs":true,"family":"Hunt","given":"Andrew","email":"ahunt@usgs.gov","middleInitial":"G.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":286901,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Athay, Denae","contributorId":48449,"corporation":false,"usgs":true,"family":"Athay","given":"Denae","email":"","affiliations":[],"preferred":false,"id":286903,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":75563,"text":"fs20063031 - 2006 - Assessment of undiscovered petroleum resources of northern Afghanistan, 2006","interactions":[],"lastModifiedDate":"2021-09-29T11:49:17.989593","indexId":"fs20063031","displayToPublicDate":"2006-03-14T00:00:00","publicationYear":"2006","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":"2006-3031","title":"Assessment of undiscovered petroleum resources of northern Afghanistan, 2006","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs20063031","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2006, Assessment of undiscovered petroleum resources of northern Afghanistan, 2006 (Version 1.0): U.S. Geological Survey Fact Sheet 2006-3031, 2 p., https://doi.org/10.3133/fs20063031.","productDescription":"2 p.","numberOfPages":"2","costCenters":[],"links":[{"id":126249,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3031.jpg"},{"id":7515,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2006/3031/","linkFileType":{"id":5,"text":"html"}}],"country":"Afghanistan","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[61.21082,35.65007],[62.23065,35.27066],[62.98466,35.40404],[63.19354,35.85717],[63.9829,36.00796],[64.54648,36.31207],[64.74611,37.11182],[65.58895,37.30522],[65.74563,37.66116],[66.21738,37.39379],[66.51861,37.36278],[67.07578,37.35614],[67.83,37.14499],[68.13556,37.02312],[68.85945,37.34434],[69.19627,37.15114],[69.51879,37.609],[70.11658,37.58822],[70.27057,37.73516],[70.3763,38.1384],[70.80682,38.48628],[71.34813,38.25891],[71.2394,37.95327],[71.54192,37.90577],[71.44869,37.06564],[71.84464,36.73817],[72.19304,36.94829],[72.63689,37.04756],[73.26006,37.49526],[73.9487,37.42157],[74.98,37.41999],[75.15803,37.13303],[74.57589,37.02084],[74.06755,36.83618],[72.92002,36.72001],[71.84629,36.50994],[71.26235,36.07439],[71.49877,35.65056],[71.61308,35.1532],[71.11502,34.73313],[71.15677,34.34891],[70.8818,33.98886],[69.93054,34.02012],[70.32359,33.35853],[69.68715,33.1055],[69.26252,32.50194],[69.31776,31.90141],[68.92668,31.62019],[68.55693,31.71331],[67.79269,31.58293],[67.68339,31.30315],[66.93889,31.30491],[66.38146,30.7389],[66.34647,29.88794],[65.04686,29.47218],[64.35042,29.56003],[64.148,29.34082],[63.55026,29.46833],[62.54986,29.31857],[60.87425,29.82924],[61.78122,30.73585],[61.69931,31.37951],[60.94194,31.54807],[60.86365,32.18292],[60.53608,32.98127],[60.9637,33.52883],[60.52843,33.67645],[60.80319,34.4041],[61.21082,35.65007]]]},\"properties\":{\"name\":\"Afghanistan\"}}]}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d8b5","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534770,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":75493,"text":"ds150 - 2006 - Ground-water-quality data in Pennsylvania: A compilation of computerized [electronic] databases, 1979-2004","interactions":[],"lastModifiedDate":"2017-07-06T17:46:30","indexId":"ds150","displayToPublicDate":"2006-03-13T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"150","title":"Ground-water-quality data in Pennsylvania: A compilation of computerized [electronic] databases, 1979-2004","docAbstract":"

This study, by the U.S. Geological Survey (USGS) in cooperation with the Pennsylvania Department of Environmental Protection (PADEP), provides a compilation of ground-water-quality data for a 25-year period (January 1, 1979, through August 11, 2004) based on water samples from wells. The data are from eight source agencies唯orough of Carroll Valley, Chester County Health Department, Pennsylvania Department of Environmental Protection-Ambient and Fixed Station Network, Montgomery County Health Department, Pennsylvania Drinking Water Information System, Pennsylvania Department of Agriculture, Susquehanna River Basin Commission, and the U.S. Geological Survey. The ground-water-quality data from the different source agencies varied in type and number of analyses; however, the analyses are represented by 12 major analyte groups:biological (bacteria and viruses), fungicides, herbicides, insecticides, major ions, minor ions (including trace elements), nutrients (dominantly nitrate and nitrite as nitrogen), pesticides, radiochemicals (dominantly radon or radium), volatile organic compounds, wastewater compounds, and water characteristics (dominantly field pH, field specific conductance, and hardness).

A summary map shows the areal distribution of wells with ground-water-quality data statewide and by major watersheds and source agency. Maps of 35 watersheds within Pennsylvania are used to display the areal distribution of water-quality information. Additional maps emphasize the areal distribution with respect to 13 major geolithologic units in Pennsylvania and concentration ranges of nitrate (as nitrogen). Summary data tables by source agency provide information on the number of wells and samples collected for each of the 35 watersheds and analyte groups. 

The number of wells sampled for ground-water-quality data varies considerably across Pennsylvania. Of the 8,012 wells sampled, the greatest concentration of wells are in the southeast (Berks, Bucks, Chester, Delaware, Lancaster, Montgomery, and Philadelphia Counties), in the vicinity of Pittsburgh, and in the northwest (Erie County). The number of wells sampled is relatively sparse in south-central (Adams, Cambria, Cumberland, and Franklin Counties), central (Centre, Indiana, and Snyder Counties), and north-central (Bradford, Potter, and Tioga Counties) Pennsylvania. Little to no data are available for approximately one-third of the state. Water characteristics and nutrients were the most frequently sampled major analyte groups; approximately 21,000 samples were collected for each group. Major and minor ions were the next most-frequently sampled major analyte groups; approximately 17,000 and 12,000 samples were collected, respectively. For the remaining eight major analyte groups, the number of samples collected ranged from a low of 307 samples (wastewater compounds) to a high of approximately 3,000 samples (biological).

The number of samples that exceeded a maximum contaminant level (MCL) or secondary maximum contaminant level (SMCL) by major analyte group also varied. Of the 2,988 samples in the biological analyte group, 53 percent had water that exceeded an MCL. Almost 2,500 samples were collected and analyzed for volatile organic compounds; 14 percent exceeded an MCL. Other major analyte groups that frequently exceeded MCLs or SMCLs included major ions (17,465 samples and a 33.9 percent exceedence), minor ions (11,905 samples and a 17.1 percent exceedence), and water characteristics (21,183 samples and a 20.3 percent exceedence). Samples collected and analyzed for fungicides, herbicides, insecticides, and pesticides (4,062 samples), radiochemicals (1,628 samples), wastewater compounds (307 samples), and nutrients (20,822 samples) had the lowest exceedences of 0.3, 8.4, 0.0, and 8.8 percent, respectively.

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