No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20051304","usgsCitation":"Thieler, E.R., Himmelstoss, E., Zichichi, J.L., and Miller, T.L., 2005, The Digital Shoreline Analysis System (DSAS) version 3.0, an ArcGIS extension for calculating historic shoreline cange (Online only): U.S. Geological Survey Open-File Report 2005-1304, https://doi.org/10.3133/ofr20051304.","onlineOnly":"Y","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":193112,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7074,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://cmgds.marine.usgs.gov/publications/DSAS/of2005-1304/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e47d","contributors":{"authors":[{"text":"Thieler, E. Robert 0000-0003-4311-9717 rthieler@usgs.gov","orcid":"https://orcid.org/0000-0003-4311-9717","contributorId":2488,"corporation":false,"usgs":true,"family":"Thieler","given":"E.","email":"rthieler@usgs.gov","middleInitial":"Robert","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":285852,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Himmelstoss, Emily A.","contributorId":24736,"corporation":false,"usgs":true,"family":"Himmelstoss","given":"Emily A.","affiliations":[],"preferred":false,"id":285853,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zichichi, Jessica L.","contributorId":49473,"corporation":false,"usgs":true,"family":"Zichichi","given":"Jessica","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":285854,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, Tara L.","contributorId":56302,"corporation":false,"usgs":true,"family":"Miller","given":"Tara","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":285855,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":72675,"text":"ds139 - 2005 - International mineral exploration activities from 1995 through 2004","interactions":[],"lastModifiedDate":"2012-02-02T00:14:02","indexId":"ds139","displayToPublicDate":"2005-11-05T00:00:00","publicationYear":"2005","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":"139","title":"International mineral exploration activities from 1995 through 2004","language":"ENGLISH","doi":"10.3133/ds139","usgsCitation":"Wilburn, D.R., 2005, International mineral exploration activities from 1995 through 2004 (Online only): U.S. Geological Survey Data Series 139, Unpaginated, https://doi.org/10.3133/ds139.","productDescription":"Unpaginated","onlineOnly":"Y","costCenters":[],"links":[{"id":193171,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7077,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/2005/139/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e07ae","contributors":{"authors":[{"text":"Wilburn, David R. 0000-0002-5371-7617 wilburn@usgs.gov","orcid":"https://orcid.org/0000-0002-5371-7617","contributorId":1755,"corporation":false,"usgs":true,"family":"Wilburn","given":"David","email":"wilburn@usgs.gov","middleInitial":"R.","affiliations":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"preferred":true,"id":285860,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":72674,"text":"ofr20051359 - 2005 - Economics of 1998 U.S. Geological Survey's 1002 Area regional assessment: An economic update","interactions":[],"lastModifiedDate":"2021-11-19T22:25:08.741486","indexId":"ofr20051359","displayToPublicDate":"2005-11-05T00:00:00","publicationYear":"2005","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":"2005-1359","title":"Economics of 1998 U.S. Geological Survey's 1002 Area regional assessment: An economic update","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051359","usgsCitation":"Attanasi, E., 2005, Economics of 1998 U.S. Geological Survey's 1002 Area regional assessment: An economic update: U.S. Geological Survey Open-File Report 2005-1359, iv, 10 p., https://doi.org/10.3133/ofr20051359.","productDescription":"iv, 10 p.","costCenters":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":193170,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":391961,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74150.htm"},{"id":7076,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1359/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","otherGeospatial":"Arctic National Wildlife Refuge, North Slope","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -146.4667,\n 69.5658\n ],\n [\n -142.1333,\n 69.5658\n ],\n [\n -142.1333,\n 70.1833\n ],\n [\n -146.4667,\n 70.1833\n ],\n [\n -146.4667,\n 69.5658\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625a08","contributors":{"authors":[{"text":"Attanasi, Emil 0000-0001-6845-7160 attanasi@usgs.gov","orcid":"https://orcid.org/0000-0001-6845-7160","contributorId":1809,"corporation":false,"usgs":true,"family":"Attanasi","given":"Emil","email":"attanasi@usgs.gov","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":285859,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70206450,"text":"70206450 - 2005 - Benthic habitats and the effects of fishing: Linking geology, biology, socioeconomics, and management in fisheries: An introduction","interactions":[],"lastModifiedDate":"2019-11-05T07:28:31","indexId":"70206450","displayToPublicDate":"2005-11-04T14:32:07","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Benthic habitats and the effects of fishing: Linking geology, biology, socioeconomics, and management in fisheries: An introduction","docAbstract":"Fishery resource managers face the challenge of ensuring sustainable fisheries and maintaining healthy, diverse ecosystems. This challenge can be met by advancing the scientific knowledge available to resource managers to evaluate and appropriately manage fishing activities that affect benthic habitats. Government agencies have been working to develop benthic habitat research initiatives focused on the effects of fishing gear and the linkage between biological resources and the geology of benthic habitats. This book provides the broad understanding of the effects of fishing activities on benthic habitats necessary to address the pressing issues of habitat alteration that challenge managers, practitioners, and ocean scientists.
","conferenceTitle":"Proceedings of Symposium on Effects of Fishing Activities on Benthic Habitats: Linking Geology, Biology, Socioeconomics, and Management","conferenceDate":"November 12-14, 2002","conferenceLocation":"Tampa Bay, Florida","language":"English","publisher":"American Fisheries Society","usgsCitation":"Thomas, J.P., and Barnes, P.W., 2005, Benthic habitats and the effects of fishing: Linking geology, biology, socioeconomics, and management in fisheries: An introduction, Proceedings of Symposium on Effects of Fishing Activities on Benthic Habitats: Linking Geology, Biology, Socioeconomics, and Management, v. 41, Tampa Bay, Florida, November 12-14, 2002, p. 3-7.","productDescription":"5 p.","startPage":"3","endPage":"7","costCenters":[],"links":[{"id":368933,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"41","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Thomas, James P.","contributorId":27606,"corporation":false,"usgs":true,"family":"Thomas","given":"James","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":774642,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, Peter W.","contributorId":6042,"corporation":false,"usgs":true,"family":"Barnes","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":774643,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":72661,"text":"sim2888 - 2005 - Geologic map of the northern plains of Mars","interactions":[],"lastModifiedDate":"2015-02-09T13:30:19","indexId":"sim2888","displayToPublicDate":"2005-11-04T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":333,"text":"Scientific Investigations Map","code":"SIM","onlineIssn":"2329-132X","printIssn":"2329-1311","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2888","title":"Geologic map of the northern plains of Mars","docAbstract":"The northern plains of Mars cover nearly a third of the planet and constitute the planet's broadest region of lowlands. Apparently formed early in Mars' history, the northern lowlands served as a repository both for sediments shed from the adjacent ancient highlands and for volcanic flows and deposits from sources within and near the lowlands. Geomorphic evidence for extensive tectonic deformation and reworking of surface materials through release of volatiles occurs throughout the northern plains. In the polar region, Planum Boreum contains evidence for the accumulation of ice and dust, and surrounding dune fields suggest widespread aeolian transport and erosion.
\nThe most recent regional- and global-scale maps describing the geology of the northern plains are largely based on Viking Orbiter image data (Dial, 1984; Witbeck and Underwood, 1984; Scott and Tanaka, 1986; Greeley and Guest, 1987; Tanaka and Scott, 1987; Tanaka and others, 1992a; Rotto and Tanaka, 1995; Crumpler and others, 2001; McGill, 2002). These maps reveal highland, plains, volcanic, and polar units based on morphologic character, albedo, and relative ages using local stratigraphic relations and crater counts.
\nThis geologic map of the northern plains is the first published map that covers a significant part of Mars using topography and image data from both the Mars Global Surveyor and Mars Odyssey missions. The new data provide a fresh perspective on the geology of the region that reveals many previously unrecognizable units, features, and temporal relations. In addition, we adapted and instituted terrestrial mapping methods and stratigraphic conventions that we think result in a clearer and more objective map. We focus on mapping with the intent of reconstructing the history of geologic activity within the northern plains, including deposition, volcanism, erosion, tectonism, impact cratering, and other processes with the aid of comprehensive crater-density determinations. Mapped areas include all plains regions within the northern hemisphere of Mars, as well as an approximately 300-km-wide strip of cratered highland and volcanic regions, which border the plains. Note that not all of the contiguous northern plains are mapped, because some minor parts of Elysium and Amazonis Planitiae lie south of the equator.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sim2888","usgsCitation":"Tanaka, K.L., Skinner, J., and Hare, T.M., 2005, Geologic map of the northern plains of Mars: U.S. Geological Survey Scientific Investigations Map 2888, Map: 57.90 x 42.44 inches; Pamphlet: i, 27 p., https://doi.org/10.3133/sim2888.","productDescription":"Map: 57.90 x 42.44 inches; Pamphlet: i, 27 p.","numberOfPages":"32","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":192788,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sim2888.jpg"},{"id":297868,"rank":101,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/sim/2005/2888/sim2888.pdf","text":"Map","size":"61.1 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Map"},{"id":297869,"rank":102,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sim/2005/2888/sim2888pamphlet.pdf","text":"Pamphlet","size":"2.5 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Pamphlet"},{"id":7066,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/2005/2888/","linkFileType":{"id":5,"text":"html"}}],"otherGeospatial":"Mars","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8493","contributors":{"authors":[{"text":"Tanaka, Kenneth L. ktanaka@usgs.gov","contributorId":610,"corporation":false,"usgs":true,"family":"Tanaka","given":"Kenneth","email":"ktanaka@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":285832,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Skinner, James A. 0000-0002-3644-7010 jskinner@usgs.gov","orcid":"https://orcid.org/0000-0002-3644-7010","contributorId":3187,"corporation":false,"usgs":true,"family":"Skinner","given":"James A.","email":"jskinner@usgs.gov","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":285833,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hare, Trent M. 0000-0001-8842-389X thare@usgs.gov","orcid":"https://orcid.org/0000-0001-8842-389X","contributorId":3188,"corporation":false,"usgs":true,"family":"Hare","given":"Trent","email":"thare@usgs.gov","middleInitial":"M.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":285834,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":72663,"text":"sir20055157 - 2005 - Age and quality of ground water and sources of nitrogen in the surficial aquifers in Pumpkin Creek Valley, western Nebraska, 2000","interactions":[],"lastModifiedDate":"2022-01-05T21:16:12.171314","indexId":"sir20055157","displayToPublicDate":"2005-11-04T00:00:00","publicationYear":"2005","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":"2005-5157","title":"Age and quality of ground water and sources of nitrogen in the surficial aquifers in Pumpkin Creek Valley, western Nebraska, 2000","docAbstract":"Ground water is the source of drinking water for the residents of Pumpkin Creek Valley, western Nebraska. In this largely agricultural area, shallow aquifers potentially are susceptible to nitrate contamination. During the last 10 years, ground-water levels in the North Platte Natural Resources District have declined and contamination has become a major problem for the district. In 2000, the U.S. Geological Survey and the North Platte Natural Resources District began a cooperative study to determine the age and quality of the ground water and the sources of nitrogen in the aquifers in Pumpkin Creek Valley.\r\n\r\nWater samples were collected from 8 surface-water sites, 2 springs, and 88 ground-water sites during May, July, and August 2000. These samples were analyzed for physical properties, nutrients or nitrate, and hydrogen and oxygen isotopes. In addition, a subset of samples was analyzed for any combination of chlorofluorocarbons, tritium, tritium/helium, sulfur-hexafluoride, carbon-14, and nitrogen-15.\r\n\r\nThe apparent age of ground water in the alluvial aquifer typically varied from about 1980 to modern, whereas ground water in the fractured Brule Formation had a median value in the 1970s. The Brule Formation typically contained ground water that ranged from the 1940s to the 1990s, but low-yield wells had apparent ages of 5,000 to 10,000 years before present. Data for oxygen-18 and deuterium indicated that lake-water samples showed the greatest effects from evaporation. Ground-water data showed no substantial evaporative effects and some ground water became isotopically heavier as the water moved downgradient. In addition, the physical and chemical ground-water data indicate that Pumpkin Creek is a gaining stream because little, if any, of its water is lost to the ground-water system.\r\n\r\nThe water-quality type changed from a sodium calcium bicarbonate type near Pumpkin Creek's headwaters to a calcium sodium bicarbonate type near its mouth. Nitrate concentrations were largest in the alluvial system (median = 5 mg/L) and smallest in the surface-water system (median = 1 mg/L). Most nitrate concentrations exceeding the U.S. Environmental Protection Agency maximum contaminant level for drinking water of 10 mg/L as nitrogen were adjacent to irrigated fields and in areas where alluvial sediments are less than 50 ft thick.\r\n\r\nSources of nitrogen in the ground water of the study area included naturally occurring nitrogen, commercial fertilizer, and animal waste. Based on nitrate concentration and delta nitrogen-15, the nitrogen in 65 percent of the water samples appears to have originated from a mixture of commercial fertilizers and animal waste. Some of the smallest nitrate concentrations in the ground-water samples contained some of the largest delta nitrogen-15 values (greater than 10 per mil), which suggests animal waste as the likely source. Commercial fertilizers were the likely source of most of the nitrogen in water samples with nitrate concentrations that exceeded 10 mg/L. The source of the nitrogen in water samples with nitrate concentrations exceeding 10 mg/L, but with delta nitrogen-15 values close to 10 per mil, could not be determined.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055157","usgsCitation":"Steele, G.V., Cannia, J.C., Sibray, S., and McGuire, V., 2005, Age and quality of ground water and sources of nitrogen in the surficial aquifers in Pumpkin Creek Valley, western Nebraska, 2000: U.S. Geological Survey Scientific Investigations Report 2005-5157, 68 p., https://doi.org/10.3133/sir20055157.","productDescription":"68 p.","costCenters":[],"links":[{"id":192831,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":393936,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75455.htm"},{"id":7068,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5157/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Nebraska","otherGeospatial":"Pumpkin Creek Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -104.0525,\n 41.3922\n ],\n [\n -102.9358,\n 41.3922\n ],\n [\n -102.9358,\n 41.8289\n ],\n [\n -104.0525,\n 41.8289\n ],\n [\n -104.0525,\n 41.3922\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db689549","contributors":{"authors":[{"text":"Steele, G. V.","contributorId":62543,"corporation":false,"usgs":true,"family":"Steele","given":"G.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":285838,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cannia, J. C.","contributorId":105258,"corporation":false,"usgs":true,"family":"Cannia","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":285841,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sibray, S. S.","contributorId":63048,"corporation":false,"usgs":true,"family":"Sibray","given":"S. S.","affiliations":[],"preferred":false,"id":285839,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McGuire, V. L. 0000-0002-3962-4158","orcid":"https://orcid.org/0000-0002-3962-4158","contributorId":94702,"corporation":false,"usgs":true,"family":"McGuire","given":"V. L.","affiliations":[],"preferred":false,"id":285840,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":72666,"text":"sir20055221 - 2005 - Baseline water-quality characteristics of the Alaska Army National Guard Stewart River Training Area near Nome, Alaska","interactions":[],"lastModifiedDate":"2016-06-20T15:26:49","indexId":"sir20055221","displayToPublicDate":"2005-11-04T00:00:00","publicationYear":"2005","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":"2005-5221","title":"Baseline water-quality characteristics of the Alaska Army National Guard Stewart River Training Area near Nome, Alaska","docAbstract":"The Alaska Army National Guard Stewart River Training Area is approximately 23 miles north of Nome on the Seward Peninsula in northwest Alaska. The Stewart River Training Area encompasses much of the Stewart River Basin and a small part of the Snake River Basin. Hydrologic, water-quality, and physical-habitat data were collected at seven surface-water sites within the Stewart River Training Area during the summer runoff months (late-May to early-September) in 2004. Two of the sampling sites selected for this study were on the main stem Stewart River, one at the upstream boundary and one at the downstream boundary of the training area. Continuous hydrologic, precipitation, and water temperature data were collected at these two sites throughout the summer of 2004. Three pond sites, along the upper, middle, and lower reaches of the Stewart River within the training area, were each sampled twice during the summer of 2004 for analysis of water-quality constituents. Two tributaries to the Snake River Basin, Goldbottom Creek and North Fork Snake River, within the Stewart River Training Area boundary, also were sampled twice during the summer of 2004. Water-quality data collected from the Stewart River at the upstream and downstream study sites indicate similar constituent concentrations. Concentrations of most water-quality constituents collected during the summer of 2004 did not exceed standards for drinking water or recreational contact. Analysis of trace-element concentrations in bed sediment samples indicate the threshold effect concentration (below which no adverse effects on organisms is expected) was exceeded for arsenic, chromium, and nickel concentrations at all sample sites within the Stewart River Training Area and cadmium, copper, zinc, and lead concentrations were found to exceed the threshold effect concentration in varying degrees at the sample sites. The probable effect concentration (above which toxic effects on organisms is likely) was exceeded by arsenic concentrations at all sites except the lower pond site. Chromium and nickel concentrations exceeded the probable effect concentration at the upstream Stewart River site and at the North Fork Snake River site.
","language":"English","doi":"10.3133/sir20055221","issn":"2328-031X","usgsCitation":"Eash, J.D., 2005, Baseline water-quality characteristics of the Alaska Army National Guard Stewart River Training Area near Nome, Alaska (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5221, 54 p., https://doi.org/10.3133/sir20055221.","productDescription":"54 p.","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":192880,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7070,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5221/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db68774f","contributors":{"authors":[{"text":"Eash, Josh D.","contributorId":100933,"corporation":false,"usgs":true,"family":"Eash","given":"Josh","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":285845,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":72665,"text":"sir20055212 - 2005 - Instream flow characterization of upper Salmon River basin streams, central Idaho, 2004","interactions":[],"lastModifiedDate":"2014-05-05T14:43:08","indexId":"sir20055212","displayToPublicDate":"2005-11-04T00:00:00","publicationYear":"2005","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":"2005-5212","title":"Instream flow characterization of upper Salmon River basin streams, central Idaho, 2004","docAbstract":"Anadromous fish populations in the Columbia River Basin have plummeted in the last 100 years. This severe decline led to Federal listing of Chinook salmon (Oncorhynchus tshawytscha) and steelhead trout (Oncorhynchus mykiss) stocks as endangered or threatened under the Endangered Species Act (ESA) in the 1990s. Historically, the upper Salmon River Basin (upstream of the confluence with the Pahsimeroi River) in Idaho provided migration corridors and significant habitat for these ESA-listed species, in addition to the ESA-listed bull trout (Salvelinus confluentus). Human development has modified the original streamflow conditions in many streams in the upper Salmon River Basin. Summer streamflow modifications resulting from irrigation practices, have directly affected quantity and quality of fish habitat and also have affected migration and (or) access to suitable spawning and rearing habitat for these fish.
\nAs a result of these ESA listings and Action 149 of the Federal Columbia River Power System Biological Opinion of 2000, the Bureau of Reclamation was tasked to conduct streamflow characterization studies in the upper Salmon River Basin to clearly define habitat requirements for effective species management and habitat restoration. These studies include collection of habitat and streamflow information for the Physical Habitat Simulation System model, a widely applied method to determine relations between habitat and discharge requirements for various fish species and life stages. Model results can be used by resource managers to guide habitat restoration efforts by evaluating potential fish habitat and passage improvements by increasing streamflow.
\nIn 2004, instream flow characterization studies were completed on Salmon River and Beaver, Pole, Champion, Iron, Thompson, and Squaw Creeks. Continuous streamflow data were recorded upstream of all diversions on Salmon River and Pole, Iron, Thompson, and Squaw Creeks. In addition, natural summer streamflows were estimated for each study site using regional regression equations.
\nThis report describes Physical Habitat Simulation System modeling results for bull trout, Chinook salmon, and steelhead trout during summer streamflows. Habitat/discharge relations were summarized for adult and spawning life stages at each study site. Adult fish passage and discharge relations were evaluated at specific transects identified as a potential low-streamflow passage barrier at each study site.
\nContinuous summer water temperature data for selected study sites were summarized and compared with Idaho Water Quality Standards and various water temperature requirements of targeted fish species. Continuous summer water temperature data recorded in 2003 and streamflow relations were evaluated for Fourth of July Creek using the Stream Segment Temperature model that simulates mean and maximum daily water temperatures with changes in streamflow.
\nResults of these habitat studies can be used to prioritize and direct cost-effective actions to improve fish habitat for ESA-listed anadromous and native fish species in the basin. These actions may include acquiring water during critical low-flow periods by leasing or modifying irrigation delivery systems to minimize out-of-stream diversions.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055212","collaboration":"Prepared in cooperation with the Bureau of Reclamation","usgsCitation":"Maret, T.R., Hortness, J., and Ott, D.S., 2005, Instream flow characterization of upper Salmon River basin streams, central Idaho, 2004: U.S. Geological Survey Scientific Investigations Report 2005-5212, Report: ix, 122 p.; Data files, https://doi.org/10.3133/sir20055212.","productDescription":"Report: ix, 122 p.; Data files","numberOfPages":"135","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":192832,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir20055212.PNG"},{"id":7069,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5212/","linkFileType":{"id":5,"text":"html"}},{"id":286895,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5212/pdf/sir20055212.pdf"},{"id":286896,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/sir/2005/5212/data/"}],"scale":"40000","projection":"Transverse Mercator Projection","country":"United States","state":"Idaho","otherGeospatial":"Salmon River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.0,44.0 ], [ -115.0,44.75 ], [ -114.0,44.75 ], [ -114.0,44.0 ], [ -115.0,44.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aefe4b07f02db69148f","contributors":{"authors":[{"text":"Maret, Terry R. trmaret@usgs.gov","contributorId":953,"corporation":false,"usgs":true,"family":"Maret","given":"Terry","email":"trmaret@usgs.gov","middleInitial":"R.","affiliations":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285842,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hortness, Jon 0000-0002-9809-2876 hortness@usgs.gov","orcid":"https://orcid.org/0000-0002-9809-2876","contributorId":3601,"corporation":false,"usgs":true,"family":"Hortness","given":"Jon","email":"hortness@usgs.gov","affiliations":[],"preferred":true,"id":285844,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ott, Douglas S. dott@usgs.gov","contributorId":3552,"corporation":false,"usgs":true,"family":"Ott","given":"Douglas","email":"dott@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":285843,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":72662,"text":"sir20055100 - 2005 - Regionalized equations for bankfull-discharge and channel characteristics of streams in New York State—Hydrologic Region 6 in the Southern Tier of New York","interactions":[],"lastModifiedDate":"2017-04-14T13:11:32","indexId":"sir20055100","displayToPublicDate":"2005-11-04T00:00:00","publicationYear":"2005","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":"2005-5100","title":"Regionalized equations for bankfull-discharge and channel characteristics of streams in New York State—Hydrologic Region 6 in the Southern Tier of New York","docAbstract":"Equations that relate bankfull discharge and channel characteristics (width, depth, and cross-sectional area) to drainage-area size at gaged sites are needed to define bankfull discharge and channel dimensions at ungaged sites and to provide information for watershed assessments, stream-channel classification, and the design of stream-restoration projects. Such equations are most accurate if derived from streams within an area of uniform hydrologic, climatic, and physiographic conditions and applied only within that region. In New York State, eight hydrologic regions were previously defined on the basis of similar high-flow (flood) characteristics. This report presents drainage areas and associated bankfull characteristics (discharge and channel dimensions) for surveyed streams in southwestern New York (Region 6).
Stream-survey data and discharge records from 11 active (currently gaged) sites and 3 inactive (discontinued) sites were used in regression analyses to relate bankfull discharge and bankfull channel width, depth, and cross-sectional area to the size of the drainage area. The resulting equations are:
(1) bankfull discharge, in cubic feet per second = 48.0*(drainage area, in square miles)0.842;
(2) bankfull channel width, in feet = 16.9*(drainage area, in square miles)0.419;
(3) bankfull channel depth, in feet = 1.04*(drainage area, in square miles)0.244; and
(4) bankfull channel cross-sectional area, in square feet = 17.6*(drainage area, in square miles)0.662.
The coefficient of determination (R2) for these four equations were 0.90, 0.79, 0.64, and 0.89, respectively. The high correlation coefficients for bankfull discharge and cross-sectional area indicate that much of the variation in these variables is explained by the size of the drainage area. The smaller correlation coefficients for bankfull channel width and depth indicate that other factors also affect these relations. Recurrence intervals for the estimated bankfull discharge of each stream ranged from 1.01 to 2.35 years; the mean recurrence interval was 1.54 years. The 14 surveyed streams were classified by Rosgen stream type; most were C-type reaches, with occasional B-type reaches. The Region 6 equation (curve) for bankfull discharge was compared with equations previously developed for four other large areas in New York State and southeastern Pennsylvania. The differences among results indicate that, although the equations need to be refined by region before being applied by water-resources managers to local planning and design efforts, similar regions have similar relations between bankfull discharge and channel characteristics.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055100","collaboration":"Prepared in cooperation with the New York State Department of Environmental Conservation, New York State Department of Transportation, and New York City Department of Environmental Protection","usgsCitation":"Mulvihill, C., Ernst, A., and Baldigo, B.P., 2005, Regionalized equations for bankfull-discharge and channel characteristics of streams in New York State—Hydrologic Region 6 in the Southern Tier of New York: U.S. Geological Survey Scientific Investigations Report 2005-5100, iv, 14 p., https://doi.org/10.3133/sir20055100.","productDescription":"iv, 14 p.","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":339596,"rank":5,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/sir20075189","text":"Scientific Investigations Report 2007-5189","linkHelpText":"- Regionalized Equations for Bankfull Discharge and Channel Characteristics of Streams in New York State—Hydrologic Regions 1 and 2 in the Adirondack Region of Northern New York"},{"id":339126,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/sir20065075","text":"Scientific Investigations Report 2006-5075","linkHelpText":"- Regionalized Equations for Bankfull-Discharge and Channel Characteristics of Streams in New York State—Hydrologic Region 7 in Western New York"},{"id":339594,"rank":7,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/sir20095144","text":"Scientific Investigations Report 2009-5144","linkHelpText":"- Bankfull Discharge and Channel Characteristics of Streams in New York State"},{"id":339595,"rank":6,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/sir20075227","text":"Scientific Investigations Report 2007-5227","linkHelpText":"- Regionalized Equations for Bankfull-Discharge and Channel Characteristics of Streams in New York State—Hydrologic Region 3 East of the Hudson River"},{"id":339597,"rank":3,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/sir20045247 ","text":"Scientific Investigations Report 2004-5247","linkHelpText":"- Regionalized Equations for Bankfull-Discharge and Channel Characteristics of Streams in New York State—Hydrologic Region 5 in Central New York"},{"id":192789,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/sir/2005/5100/coverthb.jpg"},{"id":7067,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5100/pdf/sir2005-5100.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"contact":"Director, New York Water Science Center
U.S. Geological Survey
425 Jordan Rd
Troy, NY 12180
(518) 285-5695
http://ny.water.usgs.gov
The gravity method was the first geophysical technique to be used in oil and gas exploration. Despite being eclipsed by seismology, it has continued to be an important and sometimes crucial constraint in a number of exploration areas. In oil exploration the gravity method is particularly applicable in salt provinces, overthrust and foothills belts, underexplored basins, and targets of interest that underlie high-velocity zones. The gravity method is used frequently in mining applications to map subsurface geology and to directly calculate ore reserves for some massive sulfide orebodies. There is also a modest increase in the use of gravity techniques in specialized investigations for shallow targets.
Gravimeters have undergone continuous improvement during the past 25 years, particularly in their ability to function in a dynamic environment. This and the advent of global positioning systems (GPS) have led to a marked improvement in the quality of marine gravity and have transformed airborne gravity from a regional technique to a prospect-level exploration tool that is particularly applicable in remote areas or transition zones that are otherwise inaccessible. Recently, moving-platform gravity gradiometers have become available and promise to play an important role in future exploration.
Data reduction, filtering, and visualization, together with low-cost, powerful personal computers and color graphics, have transformed the interpretation of gravity data. The state of the art is illustrated with three case histories: 3D modeling of gravity data to map aquifers in the Albuquerque Basin, the use of marine gravity gradiometry combined with 3D seismic data to map salt keels in the Gulf of Mexico, and the use of airborne gravity gradiometry in exploration for kimberlites in Canada.
","language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/1.2133785","usgsCitation":"Nabighian, M., Ander, M.E., Grauch, V.J., LaFehr, T., Li, Y., Pearson, W.C., Peirce, J., Phillips, J., and Ruder, M., 2005, Historical development of the gravity method in exploration: Geophysics, v. 70, no. 6, p. 63ND-89ND, https://doi.org/10.1190/1.2133785.","productDescription":"27 p.","startPage":"63ND","endPage":"89ND","costCenters":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":371273,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"70","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Nabighian, M.N.","contributorId":62724,"corporation":false,"usgs":true,"family":"Nabighian","given":"M.N.","email":"","affiliations":[],"preferred":false,"id":779514,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ander, M. E.","contributorId":221660,"corporation":false,"usgs":false,"family":"Ander","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":779515,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grauch, V. J. S. 0000-0002-0761-3489 tien@usgs.gov","orcid":"https://orcid.org/0000-0002-0761-3489","contributorId":886,"corporation":false,"usgs":true,"family":"Grauch","given":"V.","email":"tien@usgs.gov","middleInitial":"J. S.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":779516,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"LaFehr, T.R.","contributorId":16641,"corporation":false,"usgs":true,"family":"LaFehr","given":"T.R.","affiliations":[],"preferred":false,"id":779517,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Li, Y.","contributorId":221662,"corporation":false,"usgs":false,"family":"Li","given":"Y.","email":"","affiliations":[],"preferred":false,"id":779518,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Pearson, W. C.","contributorId":221661,"corporation":false,"usgs":false,"family":"Pearson","given":"W.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":779519,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Peirce, J.W.","contributorId":21756,"corporation":false,"usgs":true,"family":"Peirce","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":779520,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Phillips, J. D. 0000-0002-6459-2821","orcid":"https://orcid.org/0000-0002-6459-2821","contributorId":22366,"corporation":false,"usgs":true,"family":"Phillips","given":"J. D.","affiliations":[],"preferred":false,"id":779521,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Ruder, M.E.","contributorId":55634,"corporation":false,"usgs":true,"family":"Ruder","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":779522,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":72657,"text":"ofr20051259 - 2005 - Historical late-winter and spring snowpack depth and equivalent water-content data for Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:14:02","indexId":"ofr20051259","displayToPublicDate":"2005-11-03T00:00:00","publicationYear":"2005","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":"2005-1259","title":"Historical late-winter and spring snowpack depth and equivalent water-content data for Maine","language":"ENGLISH","doi":"10.3133/ofr20051259","usgsCitation":"Hodgkins, G.A., Dudley, R.W., and Loiselle, M.C., 2005, Historical late-winter and spring snowpack depth and equivalent water-content data for Maine: U.S. Geological Survey Open-File Report 2005-1259, 87 p., https://doi.org/10.3133/ofr20051259.","productDescription":"87 p.","costCenters":[],"links":[{"id":192742,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7063,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1259/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62ee12","contributors":{"authors":[{"text":"Hodgkins, Glenn A. 0000-0002-4916-5565 gahodgki@usgs.gov","orcid":"https://orcid.org/0000-0002-4916-5565","contributorId":2020,"corporation":false,"usgs":true,"family":"Hodgkins","given":"Glenn","email":"gahodgki@usgs.gov","middleInitial":"A.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285816,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dudley, Robert W. 0000-0002-0934-0568 rwdudley@usgs.gov","orcid":"https://orcid.org/0000-0002-0934-0568","contributorId":2223,"corporation":false,"usgs":true,"family":"Dudley","given":"Robert","email":"rwdudley@usgs.gov","middleInitial":"W.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285817,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Loiselle, Marc C.","contributorId":90350,"corporation":false,"usgs":true,"family":"Loiselle","given":"Marc","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":285818,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":72658,"text":"ds143 - 2005 - Bacteriological water quality in the Lake Pontchartrain basin, Louisiana, following Hurricanes Katrina and Rita, September 2005","interactions":[],"lastModifiedDate":"2022-04-07T11:21:22.023313","indexId":"ds143","displayToPublicDate":"2005-11-03T00:00:00","publicationYear":"2005","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":"143","title":"Bacteriological water quality in the Lake Pontchartrain basin, Louisiana, following Hurricanes Katrina and Rita, September 2005","docAbstract":"The U.S. Geological Survey (USGS), in collaboration with the Louisiana Department of Environmental Quality, monitored bacteriological quality of water at 22 sites in and around Lake Pontchartrain, La., for three consecutive weeks beginning September 13, 2005, following hurricanes Katrina and Rita and the associated flooding. Samples were collected and analyzed by USGS personnel from the USGS Louisiana Water Science Center and the USGS Ohio Water Microbiology Laboratory. Fecal-indicator bacteria (Escherichia coli, enterococci, and fecal coliform) concentrations ranged from the detection limit to 36,000 colony-forming units per 100 milliliters. Data are presented in tabular form and as plots of data in the context of available historical data and water-quality standards and criteria for each site sampled. Quality-control data were reviewed to ensure that methods performed as expected in a mobile laboratory setting.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ds143","usgsCitation":"Stoeckel, D.M., Bushon, R.N., Demcheck, D.K., Skrobialowski, S.C., Kephart, C.M., Bertke, E.E., Mailot, B.E., Mize, S.V., and Fendick, R., 2005, Bacteriological water quality in the Lake Pontchartrain basin, Louisiana, following Hurricanes Katrina and Rita, September 2005: U.S. Geological Survey Data Series 143, 21 p., https://doi.org/10.3133/ds143.","productDescription":"21 p.","costCenters":[{"id":509,"text":"Office of the Associate Director for Water","active":true,"usgs":true},{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"links":[{"id":192787,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7064,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/2005/143/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Louisiana","otherGeospatial":"Lake Pontchartrain basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90.83333333333333,30 ], [ -90.83333333333333,31 ], [ -90.16666666666667,31 ], [ -90.16666666666667,30 ], [ -90.83333333333333,30 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ab05","contributors":{"authors":[{"text":"Stoeckel, Donald M.","contributorId":78384,"corporation":false,"usgs":true,"family":"Stoeckel","given":"Donald","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":285827,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bushon, Rebecca N. rnbushon@usgs.gov","contributorId":2304,"corporation":false,"usgs":true,"family":"Bushon","given":"Rebecca","email":"rnbushon@usgs.gov","middleInitial":"N.","affiliations":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285823,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Demcheck, Dennis K. 0000-0003-2981-078X ddemchec@usgs.gov","orcid":"https://orcid.org/0000-0003-2981-078X","contributorId":3273,"corporation":false,"usgs":true,"family":"Demcheck","given":"Dennis","email":"ddemchec@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":285826,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Skrobialowski, Stanley C. 0000-0001-8627-0279 sski@usgs.gov","orcid":"https://orcid.org/0000-0001-8627-0279","contributorId":1402,"corporation":false,"usgs":true,"family":"Skrobialowski","given":"Stanley","email":"sski@usgs.gov","middleInitial":"C.","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true}],"preferred":true,"id":285820,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kephart, Christopher M. 0000-0002-3369-5596 ckephart@usgs.gov","orcid":"https://orcid.org/0000-0002-3369-5596","contributorId":1932,"corporation":false,"usgs":true,"family":"Kephart","given":"Christopher","email":"ckephart@usgs.gov","middleInitial":"M.","affiliations":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285821,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bertke, Erin E. eebertke@usgs.gov","contributorId":1934,"corporation":false,"usgs":true,"family":"Bertke","given":"Erin","email":"eebertke@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":285822,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Mailot, Brian E. bemailot@usgs.gov","contributorId":2569,"corporation":false,"usgs":true,"family":"Mailot","given":"Brian","email":"bemailot@usgs.gov","middleInitial":"E.","affiliations":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285824,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Mize, Scott V. 0000-0001-6751-5568 svmize@usgs.gov","orcid":"https://orcid.org/0000-0001-6751-5568","contributorId":2997,"corporation":false,"usgs":true,"family":"Mize","given":"Scott","email":"svmize@usgs.gov","middleInitial":"V.","affiliations":[{"id":369,"text":"Louisiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285825,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Fendick, Robert B. Jr. rfendick@usgs.gov","contributorId":1313,"corporation":false,"usgs":true,"family":"Fendick","given":"Robert B.","suffix":"Jr.","email":"rfendick@usgs.gov","affiliations":[{"id":369,"text":"Louisiana Water Science Center","active":true,"usgs":true}],"preferred":false,"id":285819,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":72655,"text":"sir20055172 - 2005 - A computer program for predicting recharge with a master recession curve","interactions":[],"lastModifiedDate":"2020-01-26T16:57:19","indexId":"sir20055172","displayToPublicDate":"2005-11-03T00:00:00","publicationYear":"2005","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":"2005-5172","title":"A computer program for predicting recharge with a master recession curve","docAbstract":"Water-table fluctuations occur in unconfined aquifers owing to ground-water recharge following precipitation and infiltration, and ground-water discharge to streams between storm events. Ground-water recharge can be estimated from well hydrograph data using the water-table fluctuation (WTF) principle, which states that recharge is equal to the product of the water-table rise and the specific yield of the subsurface porous medium. The water-table rise, however, must be expressed relative to the water level that would have occurred in the absence of recharge. This requires a means for estimating the recession pattern of the water-table at the site. For a given site there is often a characteristic relation between the water-table elevation and the water-table decline rate following a recharge event. A computer program was written which extracts the relation between decline rate and water-table elevation from well hydrograph data and uses it to construct a master recession curve (MRC). The MRC is a characteristic water-table recession hydrograph, representing the average behavior for a declining water-table at that site. The program then calculates recharge using the WTF method by comparing the measured well hydrograph with the hydrograph predicted by the MRC and multiplying the difference at each time step by the specific yield. This approach can be used to estimate recharge in a continuous fashion from long-term well records. Presented here is a description of the code including the WTF theory and instructions for running it to estimate recharge with continuous well hydrograph data.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055172","usgsCitation":"Heppner, C.S., and Nimmo, J.R., 2005, A computer program for predicting recharge with a master recession curve: U.S. Geological Survey Scientific Investigations Report 2005-5172, 10 p., https://doi.org/10.3133/sir20055172.","productDescription":"10 p.","onlineOnly":"Y","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":192696,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7061,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5172/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db624762","contributors":{"authors":[{"text":"Heppner, Christopher S.","contributorId":93776,"corporation":false,"usgs":true,"family":"Heppner","given":"Christopher","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":285813,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nimmo, John R. 0000-0001-8191-1727 jrnimmo@usgs.gov","orcid":"https://orcid.org/0000-0001-8191-1727","contributorId":757,"corporation":false,"usgs":true,"family":"Nimmo","given":"John","email":"jrnimmo@usgs.gov","middleInitial":"R.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":285812,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":72656,"text":"sir20055135 - 2005 - Changes in the magnitude of annual and monthly streamflows in New England, 1902-2002","interactions":[],"lastModifiedDate":"2023-04-07T18:24:58.416718","indexId":"sir20055135","displayToPublicDate":"2005-11-03T00:00:00","publicationYear":"2005","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":"2005-5135","title":"Changes in the magnitude of annual and monthly streamflows in New England, 1902-2002","docAbstract":"Selected annual and monthly streamflow statistics for 27 streamflow-gaging stations in New England were computed and tested for changes over time. These 27 stations were considered to be free of substantial human influences such as regulation, diversion, and land use-changes and have an average of 71 years of record. The longest streamflow record extended from 1902 to 2002.\r\n\r\nMarch mean streamflows increased significantly over time (Mann-Kendall test, p < 0.1) at 14 streamflow-gaging stations in northern New England, primarily in northern or mountainous sections of Maine, New Hampshire, and Vermont. March mean flows increased by 76 to 185 percent at the seven stations with the longest continuous records in areas of New England with the largest seasonal snowpack depths. These streamflow-gaging stations had continuous records from the late 1920's and the early 1930s through 2002. May mean streamflows significantly decreased at 10 stations in northern or mountainous sections of Maine and New Hampshire. May mean flows decreased by 9 to 46 percent at the seven stations with the longest continuous records. Despite the fact that March percentage increases were much larger than May percentage decreases, March streamflow increases (in cubic feet per second) were smaller than May decreases, except at one streamflow-gaging station. Increased March and April air temperatures over time may have caused earlier snowmelt and thus increased streamflows in March and decreased streamflows in May.\r\n\r\nThere were no significant changes over time in annual mean streamflows at the 27 stations; however, there were significant increases over time in various annual percentile streamflows (minimum, 25th percentile, median, 75th percentile, or maximum flows) at 22 of the stations. This indicates that flows increased over time at many streams in New England, but the increase was not enough to have caused significant changes in annual mean flows. October mean streamflows increased significantly at five stations in western New England. December minimum streamflows increased significantly at 13 stations in northern and southern New England.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055135","usgsCitation":"Hodgkins, G.A., and Dudley, R.W., 2005, Changes in the magnitude of annual and monthly streamflows in New England, 1902-2002: U.S. Geological Survey Scientific Investigations Report 2005-5135, iv, 37 p., https://doi.org/10.3133/sir20055135.","productDescription":"iv, 37 p.","costCenters":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true}],"links":[{"id":7062,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5135/","linkFileType":{"id":5,"text":"html"}},{"id":415446,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75459.htm","linkFileType":{"id":5,"text":"html"}},{"id":192741,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Connecticut, Maine, Massachusetts, New Hampshire, Rhode Island, Vermont","otherGeospatial":"New England","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -73.58379408161542,\n 40.945827638378546\n ],\n [\n -66.66599541743656,\n 40.945827638378546\n ],\n [\n -66.66599541743656,\n 47.53906208761606\n ],\n [\n -73.58379408161542,\n 47.53906208761606\n ],\n [\n -73.58379408161542,\n 40.945827638378546\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a3498","contributors":{"authors":[{"text":"Hodgkins, Glenn A. 0000-0002-4916-5565 gahodgki@usgs.gov","orcid":"https://orcid.org/0000-0002-4916-5565","contributorId":2020,"corporation":false,"usgs":true,"family":"Hodgkins","given":"Glenn","email":"gahodgki@usgs.gov","middleInitial":"A.","affiliations":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285814,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dudley, Robert W. 0000-0002-0934-0568 rwdudley@usgs.gov","orcid":"https://orcid.org/0000-0002-0934-0568","contributorId":2223,"corporation":false,"usgs":true,"family":"Dudley","given":"Robert","email":"rwdudley@usgs.gov","middleInitial":"W.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285815,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70238572,"text":"70238572 - 2005 - Coordinating NEHRP Post-Earthquake Investigations: Exercising the Plan","interactions":[],"lastModifiedDate":"2022-11-29T20:27:29.708001","indexId":"70238572","displayToPublicDate":"2005-11-01T14:23:36","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1436,"text":"Earthquake Spectra","active":true,"publicationSubtype":{"id":10}},"title":"Coordinating NEHRP Post-Earthquake Investigations: Exercising the Plan","docAbstract":"Three exercises of The Plan to Coordinate NEHRP Post-Earthquake Investigations were developed and implemented in late 2003 and early 2004 in order to test the Plan itself via realistic scenarios, and for the NEHRP agencies to learn how to coordinate post-earthquake investigations. The exercises were selected to cover a range of seismic activity and consequences, and were based on scenario events: (1) a Hayward Fault Mw 7 event without foreshocks; (2) a New Madrid seismic zone Mw 7 event with foreshocks, and (3) a Puerto Rico Mw 8 subduction event on the Puerto Rican Trench accompanied by a tsunami affecting the eastern seaboard of the United States. Each exercise consisted of a four-hour telephone conference call with a Web-based electronic link and post-exercise evaluations fed back to participants. Evaluation of the exercises found the Plan to be adequate, with implementation of the Plan by the NEHRP agencies improving with each exercise. Based on the exercises, recommendations were provided that a Plan coordinator should be designated within USGS, an annual exercise of the Plan should be conducted in different regions of the United States, a permanent NEHRP electronic link should be created, and coordination of post-earthquake data collection, preservation, archiving, and dissemination should be greatly improved.
","language":"English","publisher":"SAGE Publishing","doi":"10.1193/1.2087707","usgsCitation":"Holzer, T.L., Scawthorn, C., and Rojahn, C., 2005, Coordinating NEHRP Post-Earthquake Investigations: Exercising the Plan: Earthquake Spectra, v. 21, no. 4, p. 1043-1062, https://doi.org/10.1193/1.2087707.","productDescription":"20 p.","startPage":"1043","endPage":"1062","costCenters":[],"links":[{"id":409815,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"4","noUsgsAuthors":false,"publicationDate":"2005-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Holzer, Thomas L. tholzer@usgs.gov","contributorId":2829,"corporation":false,"usgs":true,"family":"Holzer","given":"Thomas","email":"tholzer@usgs.gov","middleInitial":"L.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":857952,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scawthorn, Charles","contributorId":65755,"corporation":false,"usgs":true,"family":"Scawthorn","given":"Charles","affiliations":[],"preferred":false,"id":857953,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rojahn, Christopher","contributorId":41482,"corporation":false,"usgs":true,"family":"Rojahn","given":"Christopher","email":"","affiliations":[],"preferred":true,"id":857954,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70238382,"text":"70238382 - 2005 - Correction to “Waveform inversion of volcano-seismic signals assuming possible source geometries”","interactions":[],"lastModifiedDate":"2022-11-18T17:45:05.189096","indexId":"70238382","displayToPublicDate":"2005-11-01T11:35:17","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Correction to “Waveform inversion of volcano-seismic signals assuming possible source geometries”","docAbstract":"No abstract available.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2005GL024848","usgsCitation":"Nakano, M., and Kumagai, H., 2005, Correction to “Waveform inversion of volcano-seismic signals assuming possible source geometries”: Geophysical Research Letters, v. 32, no. 21, L21312, 1 p., https://doi.org/10.1029/2005GL024848.","productDescription":"L21312, 1 p.","costCenters":[],"links":[{"id":477635,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2005gl024848","text":"Publisher Index Page"},{"id":409457,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"21","noUsgsAuthors":false,"publicationDate":"2005-11-11","publicationStatus":"PW","contributors":{"authors":[{"text":"Nakano, Masaru","contributorId":174115,"corporation":false,"usgs":true,"family":"Nakano","given":"Masaru","email":"","affiliations":[{"id":379,"text":"Menlo Park Science Center","active":false,"usgs":true}],"preferred":false,"id":857295,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kumagai, Hiroyuki","contributorId":71337,"corporation":false,"usgs":false,"family":"Kumagai","given":"Hiroyuki","email":"","affiliations":[],"preferred":false,"id":857296,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70238381,"text":"70238381 - 2005 - Correction to “A hypothesis for delayed dynamic earthquake triggering”","interactions":[],"lastModifiedDate":"2022-11-18T17:29:45.895627","indexId":"70238381","displayToPublicDate":"2005-11-01T11:23:23","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Correction to “A hypothesis for delayed dynamic earthquake triggering”","docAbstract":"No abstract available.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2005GL024781","usgsCitation":"Parsons, T., 2005, Correction to “A hypothesis for delayed dynamic earthquake triggering”: Geophysical Research Letters, v. 32, no. 21, L21310, 1 p., https://doi.org/10.1029/2005GL024781.","productDescription":"L21310, 1 p.","costCenters":[],"links":[{"id":409456,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"21","noUsgsAuthors":false,"publicationDate":"2005-11-09","publicationStatus":"PW","contributors":{"authors":[{"text":"Parsons, Tom 0000-0002-0582-4338","orcid":"https://orcid.org/0000-0002-0582-4338","contributorId":22056,"corporation":false,"usgs":true,"family":"Parsons","given":"Tom","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":857294,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70164302,"text":"70164302 - 2005 - A multi-disciplinary approach to the removal of emerging contaminants in municipal wastewater treatment plans in New York State, 2003-2004","interactions":[],"lastModifiedDate":"2018-10-22T08:27:26","indexId":"70164302","displayToPublicDate":"2005-11-01T11:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"A multi-disciplinary approach to the removal of emerging contaminants in municipal wastewater treatment plans in New York State, 2003-2004","docAbstract":"Across the United States, there is a rapidly growing awareness of the occurrence and the toxicological impacts of natural and synthetic trace compounds in the environment. These trace compounds, referred to as emerging contaminants (ECs), are reported to cause a range of negative impacts in the environment, such as adverse effects on biota in receiving streams and interference with the normal functions of the endocrine system, which controls growth and development in living organisms.
\nWastewater treatment plants (WWTPs) have been identified as a key collection point for ECs in the water cycle and potentially an ideal location at which to treat to remove them, thereby mitigating their release into the environment (Figure 1). This presents wastewater industry professionals with both a significant opportunity and a tremendous challenge: to identify cost effective treatment processes that can remove or reduce these contaminants before they are released into the environment.
\nAlthough WWTPs have been identified as strategic focal points and potential treatment locations for the removal of ECs from the environment, little is known about the nature, variability, transport and fate of this class of compounds in typical wastewaters and treatment facilities in the United States. Furthermore few studies have been performed to monitor or understand the capability of conventional or innovative wastewater treatment processes to remove or reduce the concentrations of a wide variety of ECs at wastewater facilities.
\nThis study was designed to provide baseline information on this topic. While other studies have examined the occurrence of a limited number of representative contaminants in the environment (generally five to 10 compounds), this study is unique in that it provides information on a comprehensive list of ECs (63 ECs in total, Contaminant List in Appendix A, not included here) in the wastewater collection and treatment systems for four diverse communities over a two-year period. (It should be noted that the study is ongoing and additional data are pending but only 18 months of data are presented in this paper).
\nThe study was conducted in two phases. Phase 1 was designed to provide information concerning the general character and concentration of ECs commonly detected in wastewaters, the variability over a prolonged period of time, the transport and fate of ECs through typical wastewater treatment plants operating with a range of conventional technologies and the impact of WWTP discharges on receiving streams. It also provided guidance in understanding the capability of distinct wastewater treatment processes or technologies to reduce or remove ECs.
\nThe second phase of the study focused on one of the most common wastewater treatment processes operated in the United States, the Activated Sludge process. Using four controlled parallel activated sludge pilots, a more detailed assessment of the impact of Sludge Retention Time (SRT) on the reduction or removal of ECs was performed.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Water Environment Federation’s WEFTEC 78th Annual Technical Exhibition and Conference, conference proceedings","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Water Environment Federation’s WEFTEC 78th Annual Technical Exhibition and Conference","conferenceDate":"Oct. 29 - Nov. 2, 2005","conferenceLocation":"Washington, DC","language":"English","publisher":"Water Environment Federation","publisherLocation":"Washington, DC","doi":"10.1061/40927(243)136","usgsCitation":"Philips, P.J., Stinson, B., Zaugg, S.D., Furlong, E.T., Kolpin, D.W., Esposito, K., Bodniewicz, B., Pape, R., and Anderson, J., 2005, A multi-disciplinary approach to the removal of emerging contaminants in municipal wastewater treatment plans in New York State, 2003-2004, in Water Environment Federation’s WEFTEC 78th Annual Technical Exhibition and Conference, conference proceedings, Washington, DC, Oct. 29 - Nov. 2, 2005, p. 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Review info: Modeling community structure in freshwater ecosystems. Edited by Sovan Lek, Michele Scardi, Piet F.M. Verdonschot, Jean-Pierre Descy, and Young-Seuk Park, 2005. ISBN: 3-540-23940-5, 518 pp.
","language":"English","publisher":"Ecological Society of America","doi":"10.1890/0012-9658(2005)86[3132:ANNAEC]2.0.CO;2","usgsCitation":"DeAngelis, D., 2005, Artificial neural networks and ecological communities (Book Review: Modelling community structure in freshwater ecosystems): Ecology, v. 86, p. 3132-3133, https://doi.org/10.1890/0012-9658(2005)86[3132:ANNAEC]2.0.CO;2.","productDescription":"2 p.","startPage":"3132","endPage":"3133","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"links":[{"id":313883,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"86","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568e48e3e4b0e7a44bc4188a","contributors":{"authors":[{"text":"DeAngelis, Donald L. 0000-0002-1570-4057 don_deangelis@usgs.gov","orcid":"https://orcid.org/0000-0002-1570-4057","contributorId":147289,"corporation":false,"usgs":true,"family":"DeAngelis","given":"Donald L.","email":"don_deangelis@usgs.gov","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"preferred":false,"id":587725,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70184410,"text":"70184410 - 2005 - Effect of the oxidation rate and Fe(II) state on microbial nitrate-dependent Fe(III) mineral formation","interactions":[],"lastModifiedDate":"2017-03-08T13:39:18","indexId":"70184410","displayToPublicDate":"2005-11-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":850,"text":"Applied and Environmental Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Effect of the oxidation rate and Fe(II) state on microbial nitrate-dependent Fe(III) mineral formation","docAbstract":"A nitrate-dependent Fe(II)-oxidizing bacterium was isolated and used to evaluate whether Fe(II) chemical form or oxidation rate had an effect on the mineralogy of biogenic Fe(III) (hydr)oxides resulting from nitrate-dependent Fe(II) oxidation. The isolate (designated FW33AN) had 99% 16S rRNA sequence similarity to Klebsiella oxytoca. FW33AN produced Fe(III) (hydr)oxides by oxidation of soluble Fe(II) [Fe(II)sol] or FeS under nitrate-reducing conditions. Based on X-ray diffraction (XRD) analysis, Fe(III) (hydr)oxide produced by oxidation of FeS was shown to be amorphous, while oxidation of Fe(II)sol yielded goethite. The rate of Fe(II) oxidation was then manipulated by incubating various cell concentrations of FW33AN with Fe(II)sol and nitrate. Characterization of products revealed that as Fe(II) oxidation rates slowed, a stronger goethite signal was observed by XRD and a larger proportion of Fe(III) was in the crystalline fraction. Since the mineralogy of Fe(III) (hydr)oxides may control the extent of subsequent Fe(III) reduction, the variables we identify here may have an effect on the biogeochemical cycling of Fe in anoxic ecosystems.
","language":"English","publisher":"American Society for Microbiology","doi":"10.1128/AEM.71.11.7172-7177.2005","usgsCitation":"Senko, J.M., Dewers, T.A., and Krumholz, L.R., 2005, Effect of the oxidation rate and Fe(II) state on microbial nitrate-dependent Fe(III) mineral formation: Applied and Environmental Microbiology, v. 71, no. 11, p. 7172-7177, https://doi.org/10.1128/AEM.71.11.7172-7177.2005.","productDescription":"6 p. ","startPage":"7172","endPage":"7177","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":477638,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://www.ncbi.nlm.nih.gov/pmc/articles/1287677","text":"External Repository"},{"id":337101,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"71","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58c1263de4b014cc3a3d34b2","contributors":{"authors":[{"text":"Senko, John M.","contributorId":187692,"corporation":false,"usgs":false,"family":"Senko","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":681359,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dewers, Thomas A.","contributorId":187693,"corporation":false,"usgs":false,"family":"Dewers","given":"Thomas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":681360,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krumholz, Lee R.","contributorId":187679,"corporation":false,"usgs":false,"family":"Krumholz","given":"Lee","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":681361,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}