No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051368","usgsCitation":"Chalmers, A., Nilles, M.A., Krabbenhoft, D.P., and Prestbo, E., 2005, Analysis of mercury wet-deposition data collected with a newly designed sampler, Boston, Massachusetts metropolitan area, 2002-04: U.S. Geological Survey Open-File Report 2005-1368, vi, 17 p., https://doi.org/10.3133/ofr20051368.","productDescription":"vi, 17 p.","onlineOnly":"Y","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":193211,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7112,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1368/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Massachusetts ","city":"Boston","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.246337890625,\n 42.273244264402734\n ],\n [\n -70.8673095703125,\n 42.273244264402734\n ],\n [\n -70.8673095703125,\n 42.48019996901214\n ],\n [\n -71.246337890625,\n 42.48019996901214\n ],\n [\n -71.246337890625,\n 42.273244264402734\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db6802c3","contributors":{"authors":[{"text":"Chalmers, Ann","contributorId":23604,"corporation":false,"usgs":true,"family":"Chalmers","given":"Ann","affiliations":[],"preferred":false,"id":285888,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nilles, Mark A. manilles@usgs.gov","contributorId":3171,"corporation":false,"usgs":true,"family":"Nilles","given":"Mark","email":"manilles@usgs.gov","middleInitial":"A.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true}],"preferred":true,"id":285887,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krabbenhoft, David P. 0000-0003-1964-5020 dpkrabbe@usgs.gov","orcid":"https://orcid.org/0000-0003-1964-5020","contributorId":1658,"corporation":false,"usgs":true,"family":"Krabbenhoft","given":"David","email":"dpkrabbe@usgs.gov","middleInitial":"P.","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true},{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true},{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":285886,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Prestbo, Eric","contributorId":77003,"corporation":false,"usgs":true,"family":"Prestbo","given":"Eric","email":"","affiliations":[],"preferred":false,"id":285889,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":72698,"text":"sir20055180 - 2005 - Quantification of fish habitat in selected reaches of the Marmaton and Marais des Cygnes Rivers, Missouri","interactions":[],"lastModifiedDate":"2018-11-13T10:36:53","indexId":"sir20055180","displayToPublicDate":"2005-11-12T00:00:00","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":"2005-5180","title":"Quantification of fish habitat in selected reaches of the Marmaton and Marais des Cygnes Rivers, Missouri","docAbstract":"The U.S. Geological Survey, in cooperation with the Missouri Department of Conservation, undertook a study to quantify fish habitat by using relations between streamflow and the spatial and temporal distributions of fish habitat at five sites in the Marmaton and Marais des Cygnes Rivers in western Missouri. Twenty-six fish habitat categories were selected for nine species under varying seasonal (spring, summer, and fall), diel (summer day and night), and life-stage (spawning, juvenile, and adult) conditions. Physical habitat characteristics were determined for each category using depth, velocity, and channel substrate criteria. Continuous streamflow data were then combined with the habitat-streamflow relations to compile a habitat time series for each habitat category at each site.\r\n\r\nFish habitat categories were assessed as to their vulnerability to habitat alteration based on critical life stages (spawning and juvenile rearing periods) and susceptibility to habitat limitations from dewatering or high flows. Species categories representing critical life stages with physical habitat limitations represent likely bottlenecks in fish populations. Categories with potential bottlenecks can serve as indicator categories and aid managers when determining the flows necessary for maintaining these habitats under altered flow regimes.\r\n\r\nThe relation between the area of each habitat category and streamflow differed greatly between category, season, and stream reach. No single flow maximized selected habitat area for all categories or even for all species/category within a particular season at a site. However, some similarities were noted among habitat characteristics, including the streamflow range for which habitat availability is maximized and the range of streamflows for which a habitat category area is available at the Marmaton River sites.\r\n\r\nA monthly habitat time series was created for all 26 habitat categories at two Marmaton River sites. A daily habitat time series was created at three Marais des Cygnes River sites for two periods: 1941 through 1963 (pre-regulation) and 1982 through 2003 (post-regulation). The habitat category with the highest median area in spring was paddlefish (Polyodon spathula) with normalized areas of up to 2,000 square meters per 100 meters of stream channel. Flathead catfish (Pylodictis olivaris) habitat area generally was the category area most available in summer and fall. Differences in daily selected habitat area time series between pre- and post-regulation time periods varied by species/category and by site. For instance, whereas there was a decline in the distribution of spring spawning habitat for suckermouth minnow (Phenacobius mirabilis) and slenderhead darter (Percina phoxocephala) from pre- to post-regulation periods at all three sites, the 25 to 75 percentile habitat area substantially increased for paddlefish under post-regulation conditions.\r\n\r\nPotential habitat area for most species was maximized at the Marmaton River sites at flows of about 1 to 10 cubic meters per second, whereas median monthly streamflows ranged from less than 1 to 20 cubic meters per second depending on site and season. Paddlefish habitat was available beginning at higher flows than other categories (4 to 7 cubic meters per second) and also maximized at higher flows (greater than 50 to 100 cubic meters per second). Selected potential habitat area was maximized for most species at the Marais des Cygnes River sites at flows of about 1 to 50 cubic meters per second, whereas median monthly streamflows ranged from 4 to 55 cubic meters per second depending on site and season. \r\n\r\nThe range of streamflows for which selected habitat area was available in summer and fall was substantially less at the channelized Marais des Cygnes River site when compared to the non-channelized sites, and, therefore, the susceptibility of categories to high-flow habitat limitations was greater at this site. The channelized reach was more unifor","language":"ENGLISH","doi":"10.3133/sir20055180","collaboration":"Prepared in cooperation with the Missouri Department of Conservation","usgsCitation":"Heimann, D.C., Richards, J.M., Brewer, S.K., and Norman, R.D., 2005, Quantification of fish habitat in selected reaches of the Marmaton and Marais des Cygnes Rivers, Missouri: U.S. Geological Survey Scientific Investigations Report 2005-5180, vii, 58 p. : ill., col. map ; 28 cm.+ 1 CD-ROM (4 3/4 in.), https://doi.org/10.3133/sir20055180.","productDescription":"vii, 58 p. : ill., col. map ; 28 cm.+ 1 CD-ROM (4 3/4 in.)","temporalStart":"2003-01-01","temporalEnd":"2005-12-31","costCenters":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"links":[{"id":191373,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9283,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5180/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a87e4b07f02db64e947","contributors":{"authors":[{"text":"Heimann, David C. 0000-0003-0450-2545 dheimann@usgs.gov","orcid":"https://orcid.org/0000-0003-0450-2545","contributorId":3822,"corporation":false,"usgs":true,"family":"Heimann","given":"David","email":"dheimann@usgs.gov","middleInitial":"C.","affiliations":[{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true},{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285895,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Richards, Joseph M. 0000-0002-9822-2706 richards@usgs.gov","orcid":"https://orcid.org/0000-0002-9822-2706","contributorId":2370,"corporation":false,"usgs":true,"family":"Richards","given":"Joseph","email":"richards@usgs.gov","middleInitial":"M.","affiliations":[{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285894,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brewer, Shannon K. 0000-0002-1537-3921 skbrewer@usgs.gov","orcid":"https://orcid.org/0000-0002-1537-3921","contributorId":2252,"corporation":false,"usgs":true,"family":"Brewer","given":"Shannon","email":"skbrewer@usgs.gov","middleInitial":"K.","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true},{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":285893,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Norman, Richard D. rnorman@usgs.gov","contributorId":4086,"corporation":false,"usgs":true,"family":"Norman","given":"Richard","email":"rnorman@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":285896,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":72694,"text":"sir20055224 - 2005 - Water-quality trend analysis and sampling design for streams in the Red River of the North Basin, Minnesota, North Dakota, and South Dakota, 1970-2001","interactions":[],"lastModifiedDate":"2018-03-16T12:49:52","indexId":"sir20055224","displayToPublicDate":"2005-11-12T00:00:00","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":"2005-5224","title":"Water-quality trend analysis and sampling design for streams in the Red River of the North Basin, Minnesota, North Dakota, and South Dakota, 1970-2001","docAbstract":"The Bureau of Reclamation is considering several alternatives to meet the future municipal, rural, and industrial water-supply needs in the Red River of the North (Red River) Basin, and an environmental impact statement is being prepared to evaluate the potential effects of the various alternatives on the water quality and aquatic health in the basin in relation to the historical variability of streamflow and constituent concentration. Therefore, a water-quality trend analysis was needed to determine the amount of natural water-quality variability that can be expected to occur in the basin, to determine if significant water-quality changes have occurred as a result of human activities, to explore potential causal mechanisms for water-quality changes, and to establish a baseline from which to monitor future water-quality trends. This report presents the results of a study conducted by the U.S. Geological Survey, in cooperation with the Bureau of Reclamation, to analyze historical water-quality trends in two dissolved major ions, dissolved solids, three nutrients, and two dissolved trace metals for nine streamflow-gaging stations in the basin.
Annual variability in streamflow in the Red River Basin was high during the trend-analysis period (1970-2001). The annual variability affects constituent concentrations in individual tributaries to the Red River and, in turn, affects constituent concentrations in the main stem of the Red River because of the relative streamflow contribution from the tributaries to the main stem. Therefore, an annual concentration anomaly, which is an estimate of the interannual variability in concentration that can be attributed to long-term variability in streamflow, was used to analyze annual streamflow-related variability in constituent concentrations. The concentration trend is an estimate of the long-term systematic changes in concentration that are unrelated to seasonal or long-term variability in streamflow. Concentrations that have both the seasonal and annual variability removed are called standardized concentrations. Numerous changes that could not be attributed to natural streamflow-related variability occurred in the standardized concentrations during the trend-analysis period. During various times from the late 1970's to the mid-1990's, significant increases occurred in standardized dissolved sulfate, dissolved chloride, and dissolved- solids concentrations for eight of the nine stations for which water-quality trends were analyzed. Significant increases also occurred from the early 1980's to the mid-1990's for standardized dissolved nitrite plus nitrate concentrations for the main-stem stations. The increasing concentrations for the main-stem stations indicate the upward trends may have been caused by human activities along the main stem of the Red River. Significant trends for standardized total ammonia plus organic nitrogen concentrations occurred for most stations. The fitted trends for standardized total phosphorus concentrations for one tributary station increased from the late 1970's to the early 1980's and decreased from the early 1980's to the mid-1990's. Small but insignificant increases occurred for two main-stem stations. No trends were detected for standardized dissolved iron or dissolved manganese concentrations. However, the combination of extreme high-frequency variability, few data, and the number of censored values may have disguised the streamflow-related variability for iron.
The time-series model used to detect historical concentration trends also was used to evaluate sampling designs to monitor future water-quality trends. Various sampling designs were evaluated with regard to their sensitivity to detect both annual and seasonal trends during three 4-month seasons. A reasonable overall design for detecting trends for all stations and constituents consisted of eight samples per year, with monthly sampling from April to August and bimonthly sampling from October to February.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055224","usgsCitation":"Vecchia, A.V., 2005, Water-quality trend analysis and sampling design for streams in the Red River of the North Basin, Minnesota, North Dakota, and South Dakota, 1970-2001: U.S. Geological Survey Scientific Investigations Report 2005-5224, v, 54 p., https://doi.org/10.3133/sir20055224.","productDescription":"v, 54 p.","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":193210,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7111,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5224/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -101.33333333333333,46 ], [ -101.33333333333333,49 ], [ -94,49 ], [ -94,46 ], [ -101.33333333333333,46 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e5529","contributors":{"authors":[{"text":"Vecchia, Aldo V. 0000-0002-2661-4401","orcid":"https://orcid.org/0000-0002-2661-4401","contributorId":41810,"corporation":false,"usgs":true,"family":"Vecchia","given":"Aldo","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":285885,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":72696,"text":"fs20053052 - 2005 - Monitoring earthquake shaking in federal buildings","interactions":[],"lastModifiedDate":"2012-02-02T00:13:59","indexId":"fs20053052","displayToPublicDate":"2005-11-12T00:00:00","publicationYear":"2005","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":"2005-3052","title":"Monitoring earthquake shaking in federal buildings","language":"ENGLISH","doi":"10.3133/fs20053052","usgsCitation":"Çelebi, M., and Page, R.A., 2005, Monitoring earthquake shaking in federal buildings: U.S. Geological Survey Fact Sheet 2005-3052, 1 sheet ([2] p.) : col. ill., col. map ; 28 x 18 cm., https://doi.org/10.3133/fs20053052.","productDescription":"1 sheet ([2] p.) : col. ill., col. map ; 28 x 18 cm.","costCenters":[],"links":[{"id":120897,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3052.bmp"},{"id":7113,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3052/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69914a","contributors":{"authors":[{"text":"Çelebi, Mehmet 0000-0002-4769-7357 celebi@usgs.gov","orcid":"https://orcid.org/0000-0002-4769-7357","contributorId":3205,"corporation":false,"usgs":true,"family":"Çelebi","given":"Mehmet","email":"celebi@usgs.gov","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":285890,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Page, Robert A.","contributorId":17207,"corporation":false,"usgs":true,"family":"Page","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":285891,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":72699,"text":"sir20055122 - 2005 - Surface-Water and Ground-Water Resources of Kendall County, Illinois","interactions":[],"lastModifiedDate":"2012-03-08T17:16:17","indexId":"sir20055122","displayToPublicDate":"2005-11-12T00:00:00","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":"2005-5122","title":"Surface-Water and Ground-Water Resources of Kendall County, Illinois","docAbstract":"Water-supply needs in Kendall County, in northern Illinois, are met exclusively from ground water derived from glacial drift aquifers and bedrock aquifers open to Silurian, Ordovician, and Cambrian System units. As a result of population growth in Kendall County and the surrounding area, water use has increased from about 1.2 million gallons per day in 1957 to more than 5 million gallons per day in 2000. The purpose of this report is to characterize the surface-water and ground-water resources of Kendall County. The report presents a compilation of available information on geology, surface-water and ground-water hydrology, water quality, and water use.\r\n\r\nThe Fox River is the primary surface-water body in Kendall County and is used for both wastewater disposal and as a drinking-water supply upstream of the county. Water from the Fox River requires pretreatment for use as drinking water, but the river is a potentially viable additional source of water for the county.\r\n\r\nGlacial drift aquifers capable of yielding sufficient water for municipal supply are expected to be present in northern Kendall County, along the Fox River, and in the Newark Valley and its tributaries. Glacial drift aquifers capable of yielding sufficient water for residential supply are present in most of the county, with the exception of the southeastern portion. Volatile organic compounds and select trace metals and pesticides have been detected at low concentrations in glacial drift aquifers near waste-disposal sites. Agricultural-related constituents have been detected infrequently in glacial drift aquifers near agricultural areas. However, on the basis of the available data, widespread, consistent problems with water quality are not apparent in these aquifers. These aquifers are a viable source for additional water supply, but would require further characterization prior to full development.\r\n\r\nThe shallow bedrock aquifer is composed of the sandstone units of the Ancell Group, the Prairie du Chien Group, the Galena-Platteville dolomite, the Maquoketa Group, and the Silurian dolomite where these units are at the bedrock surface. The availability of water from the shallow bedrock aquifer depends primarily on the geologic unit utilized. The Silurian dolomite, Galena-Platteville dolomite, and Ancell Group can yield sufficient water for residential and municipal supply in at least some parts of the county.\r\n\r\nThe Cambrian-Ordovician aquifer system is composed of the most widespread, productive aquifers in northern Illinois and is used for water supply by a number of municipalities and industrial facilities. Water levels in the aquifer system have declined by as much as 600 feet in Kendall County and the aquifer frequently contains concentrations of radium above established health guidelines.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/sir20055122","collaboration":"In cooperation with the Kendall County Soil and Water Conservation District","usgsCitation":"Kay, R.T., Mills, P., Hogan, J.L., and Arnold, T., 2005, Surface-Water and Ground-Water Resources of Kendall County, Illinois: U.S. Geological Survey Scientific Investigations Report 2005-5122, viii, 92 p., https://doi.org/10.3133/sir20055122.","productDescription":"viii, 92 p.","costCenters":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"links":[{"id":191374,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9843,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://il.water.usgs.gov/pubsearch/reports.cgi/view?series=SIR&number=2005-5122&return_url=%2Fpubsearch%2Freports.cgi%2Fseries%3Fseries%3DSIR%3Bsortby%3Ddate","linkFileType":{"id":5,"text":"html"}},{"id":9844,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://il.water.usgs.gov/pubs/sir2005-5122.pdf","size":"27523","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.66666666666667,41.416666666666664 ], [ -88.66666666666667,41.75 ], [ -88.16666666666667,41.75 ], [ -88.16666666666667,41.416666666666664 ], [ -88.66666666666667,41.416666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db691355","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":285897,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mills, P.C. pcmills@usgs.gov","contributorId":3810,"corporation":false,"usgs":true,"family":"Mills","given":"P.C.","email":"pcmills@usgs.gov","affiliations":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285899,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hogan, Jennifer L.","contributorId":51812,"corporation":false,"usgs":true,"family":"Hogan","given":"Jennifer","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":285900,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Arnold, Terri 0000-0003-1406-6054 tlarnold@usgs.gov","orcid":"https://orcid.org/0000-0003-1406-6054","contributorId":1598,"corporation":false,"usgs":false,"family":"Arnold","given":"Terri","email":"tlarnold@usgs.gov","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true},{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true},{"id":35680,"text":"Illinois-Iowa-Missouri Water Science Center","active":true,"usgs":true}],"preferred":false,"id":285898,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":72691,"text":"sir20055108 - 2005 - Characterization of dissolved and particulate natural organic matter (NOM) in Neversink Reservoir, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:13:59","indexId":"sir20055108","displayToPublicDate":"2005-11-12T00:00:00","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":"2005-5108","title":"Characterization of dissolved and particulate natural organic matter (NOM) in Neversink Reservoir, New York","docAbstract":"Natural organic matter (NOM) was isolated from the water of the Neversink Reservoir, part of the New York City water supply, located in the Catskill Mountains of New York. The NOM was fractionated into the following nine different fractions by the isolation procedure: (1) coarse particulates, (2) fine-particulate organics, (3) solvent-extractable organics, (4) hydrophobic neutrals (HPON fraction), (5) dissolved colloids, (6) bases, (7) hydrophobic acids (HPOA), (8) transphilic acids + neutrals (TPI-A+N), and (9) hydrophilic acids + neutrals (HPI-A+N). Each of these fractions, with exception of the first and the third which were too small for the complete series of analyses, was characterized by elemental, carbohydrate, and amino acid analyses, and by nuclear magnetic resonance and infrared spectrometry. The data obtained from these analyses indicate (1) that the fine-particulate organics and colloids are mainly composed of peptidoglycans, and lipopolysaccharides derived from algal, bacterial, and fungal cell walls, (2) that the HPO-N fraction most likely consists of a mixture of alicyclic terpenes and carbohydrates, (3) that the HPOA fraction consists mainly of lignin components conjugated to carbohydrates, (4) that the TPI-A+N and the HPI-A+N fractions most likely represent complex mixtures of relatively low molecular weight carboxylic acids derived from terpenes, carbohydrates, and peptides, and (5) that the base fraction is composed of free amino acids, browning reaction products, and peptide fragments.","language":"ENGLISH","doi":"10.3133/sir20055108","usgsCitation":"Wershaw, R.L., Leenheer, J.A., and Cox, L.G., 2005, Characterization of dissolved and particulate natural organic matter (NOM) in Neversink Reservoir, New York: U.S. Geological Survey Scientific Investigations Report 2005-5108, 24 p., https://doi.org/10.3133/sir20055108.","productDescription":"24 p.","costCenters":[],"links":[{"id":193149,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7108,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5108/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4dbd","contributors":{"authors":[{"text":"Wershaw, Robert L. rwershaw@usgs.gov","contributorId":4856,"corporation":false,"usgs":true,"family":"Wershaw","given":"Robert","email":"rwershaw@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":285876,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leenheer, Jerry A.","contributorId":72420,"corporation":false,"usgs":true,"family":"Leenheer","given":"Jerry","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":285877,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cox, Larry G. lgcox@usgs.gov","contributorId":3310,"corporation":false,"usgs":true,"family":"Cox","given":"Larry","email":"lgcox@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":285875,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":72703,"text":"sir20055132 - 2005 - 40Ar/39Ar geochronology of hypabyssal igneous rocks in the Maranon Basin of Peru - A record of thermal history, structure, and alteration","interactions":[],"lastModifiedDate":"2012-02-02T00:13:55","indexId":"sir20055132","displayToPublicDate":"2005-11-12T00:00:00","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":"2005-5132","title":"40Ar/39Ar geochronology of hypabyssal igneous rocks in the Maranon Basin of Peru - A record of thermal history, structure, and alteration","docAbstract":"Hypabyssal andesites and dacites from the Balsapuerto Dome in the Mara?on Basin of Peru record the thermal, tectonic, and alteration history of the area. The Mara?on Basin is one of 19 sub-Andean foreland basins. The hypabyssal rocks in the Balsapuerto Dome are one of four known occurrences of subvolcanic rocks along the deformation front in Peru. This dome is a potential petroleum structural trap. Petroleum seeps near the dome indicate that a source for the petroleum is present, but the extent and amount of petroleum development is unknown.\r\n\r\nThe Balsapuerto hypabyssal rocks are plagioclase-, hornblende-, pyroxene-phyric andesites to dacites. Some parts of the dome are pervasively altered to a hydrothermal assemblage of quartz-sericite-pyrite. 40Ar/39Ar geochronology shows that thermal activity related to emplacement of these subvolcanic rocks took place between 12-10 Ma, subsequent to the major periods of Andean folding and faulting, previously assumed to have occurred about 9 Ma. Eleven argon mineral age-spectrum analyses were completed. Argon apparent ages on amphibole range from 12.7 to 11.6 Ma, and the age spectra are simple, which indicates that the ages are very close to emplacement ages. Potassium feldspar yields an argon age spectrum ranging in age from 12.5 to 11.4 Ma, reflecting the period during which the potassium feldspar closed to argon diffusion between the temperature range of 350?C to about 150?C; thus the potassium feldspar age spectrum reflects a cooling profile throughout this temperature range. This age range is consistent with ages of emplacement for the entire igneous complex indicating that an increased thermal state existed in the area for at least 1.0 m.y. Combined with the coexisting hornblende age, this rock cooled from ~580?C to ~150?C in ~1.2 m.y. resulting in an average cooling rate of 358?C /m.y. White mica, or sericite, formed as a later alteration phase associated with quartz- sericite- pyrite and propylitic alteration in some samples. Three age-spectrum analyses on white mica indicate that alteration occurred at 12.5 Ma and again at 11 Ma, and suggest that alteration fluids were present throughout the range of emplacement and as long as 0.5 m.y. afterward.\r\n\r\nBased on these data, emplacement of the intrusive body(ies) began at about 12.7 Ma. The hornblende age range can be interpreted to reflect multiple periods of intrusion from 12.7 to 11.6 Ma or a period of thermal activity and high-temperature cooling during this age range. The potassium feldspar cooling age range supports either interpretation. The white mica ages indicate that at least two periods of hydrothermal activity occurred at 12.5 and 11.0 Ma, throughout the period of emplacement and cooling of the intrusive body below about 150?C. The magmatic and hydrothermal systems were active after the intrusion, with temperatures not reaching 150?C until about 1 m.y. after emplacement. Therefore, the thermal effects associated with emplacement of the intrusion and the associated hydrothermal system were probably high enough to destroy petroleum in the host and source rocks. Thus, the Balsapuerto Dome is not a viable source of petroleum. There is no evidence in the rock samples or thin sections for brittle or ductile deformation suggesting that this body was emplaced in its present location after cessation of Andean thrusting. Andean thrusting had been assumed to end about 9 Ma. However, this new data suggested that the Andean thrusting had ceased by about 12-10 Ma.","language":"ENGLISH","doi":"10.3133/sir20055132","usgsCitation":"Prueher, L., Erlich, R., and Snee, L., 2005, 40Ar/39Ar geochronology of hypabyssal igneous rocks in the Maranon Basin of Peru - A record of thermal history, structure, and alteration (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2005-5132, 41 p., https://doi.org/10.3133/sir20055132.","productDescription":"41 p.","costCenters":[],"links":[{"id":124386,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2005_5132.jpg"},{"id":7115,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5132/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4931e4b0b290850eef7e","contributors":{"authors":[{"text":"Prueher, L.M.","contributorId":8346,"corporation":false,"usgs":true,"family":"Prueher","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":285905,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erlich, R.","contributorId":59683,"corporation":false,"usgs":true,"family":"Erlich","given":"R.","email":"","affiliations":[],"preferred":false,"id":285906,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Snee, L.W.","contributorId":99981,"corporation":false,"usgs":true,"family":"Snee","given":"L.W.","email":"","affiliations":[],"preferred":false,"id":285907,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":72799,"text":"sim2876 - 2005 - Altitude and configuration of the potentiometric surface in part of Lower Oxford, East Nottingham, and West Nottingham Townships, and in part of the Borough of Oxford, Chester County, Pennsylvania, April through June, 2003","interactions":[],"lastModifiedDate":"2012-02-10T00:11:37","indexId":"sim2876","displayToPublicDate":"2005-11-10T00:00:00","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":"2876","title":"Altitude and configuration of the potentiometric surface in part of Lower Oxford, East Nottingham, and West Nottingham Townships, and in part of the Borough of Oxford, Chester County, Pennsylvania, April through June, 2003","language":"ENGLISH","doi":"10.3133/sim2876","usgsCitation":"Mohammad, A., 2005, Altitude and configuration of the potentiometric surface in part of Lower Oxford, East Nottingham, and West Nottingham Townships, and in part of the Borough of Oxford, Chester County, Pennsylvania, April through June, 2003: U.S. Geological Survey Scientific Investigations Map 2876, 1 map ; 51 x 50 cm., on sheet 71 x 97 cm., folded in envelope to 27 x 19 cm., https://doi.org/10.3133/sim2876.","productDescription":"1 map ; 51 x 50 cm., on sheet 71 x 97 cm., folded in envelope to 27 x 19 cm.","costCenters":[],"links":[{"id":101663,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sim/2876/report.pdf","size":"72","linkFileType":{"id":1,"text":"pdf"}},{"id":101664,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/sim/2876/plate-1.pdf","size":"6135","linkFileType":{"id":1,"text":"pdf"}},{"id":192986,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/sim/2876/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.08333333333333,39.733333333333334 ], [ -76.08333333333333,39.83361111111111 ], [ -75.95083333333334,39.83361111111111 ], [ -75.95083333333334,39.733333333333334 ], [ -76.08333333333333,39.733333333333334 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db6872aa","contributors":{"authors":[{"text":"Mohammad, Abdul","contributorId":55405,"corporation":false,"usgs":true,"family":"Mohammad","given":"Abdul","email":"","affiliations":[],"preferred":false,"id":286122,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":72798,"text":"sir20055125 - 2005 - Reconnaissance study of the hydrologic characteristics of the Hassayampa River Canyon Wilderness, central Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:14:02","indexId":"sir20055125","displayToPublicDate":"2005-11-10T00:00:00","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":"2005-5125","title":"Reconnaissance study of the hydrologic characteristics of the Hassayampa River Canyon Wilderness, central Arizona","language":"ENGLISH","doi":"10.3133/sir20055125","usgsCitation":"Fleming, J.B., 2005, Reconnaissance study of the hydrologic characteristics of the Hassayampa River Canyon Wilderness, central Arizona: U.S. Geological Survey Scientific Investigations Report 2005-5125, vii, 22 p. : col. ill., col. maps ; 28 cm., https://doi.org/10.3133/sir20055125.","productDescription":"vii, 22 p. : col. ill., col. maps ; 28 cm.","costCenters":[],"links":[{"id":101662,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5125/report.pdf","size":"7732","linkFileType":{"id":1,"text":"pdf"}},{"id":192985,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/sir/2005/5125/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e756","contributors":{"authors":[{"text":"Fleming, John B.","contributorId":33788,"corporation":false,"usgs":true,"family":"Fleming","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":286121,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":72687,"text":"ofr20051387 - 2005 - Preliminary geologic map of Bainbridge Island, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:13:59","indexId":"ofr20051387","displayToPublicDate":"2005-11-07T00:00:00","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":"2005-1387","title":"Preliminary geologic map of Bainbridge Island, Washington","language":"ENGLISH","doi":"10.3133/ofr20051387","usgsCitation":"Haugerud, R., 2005, Preliminary geologic map of Bainbridge Island, Washington (Version 1.0): U.S. Geological Survey Open-File Report 2005-1387, 1 map, 36 x 45 in.; digital data, https://doi.org/10.3133/ofr20051387.","productDescription":"1 map, 36 x 45 in.; digital data","costCenters":[],"links":[{"id":110584,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74085.htm","linkFileType":{"id":5,"text":"html"},"description":"74085"},{"id":193148,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7107,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1387/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c174","contributors":{"authors":[{"text":"Haugerud, Ralph","contributorId":88402,"corporation":false,"usgs":true,"family":"Haugerud","given":"Ralph","affiliations":[],"preferred":false,"id":285874,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":72683,"text":"sir20055203 - 2005 - Occurrence and distribution of pesticide compounds in surface water of the Santa Ana basin, California, 1998-2001","interactions":[],"lastModifiedDate":"2012-02-02T00:13:58","indexId":"sir20055203","displayToPublicDate":"2005-11-07T00:00:00","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":"2005-5203","title":"Occurrence and distribution of pesticide compounds in surface water of the Santa Ana basin, California, 1998-2001","docAbstract":" A study of the occurrence and distribution of pesticide compounds in surface water of the highly urbanized Santa Ana Basin, California, was done as part of the U.S. Geological Survey's National Water-Quality Assessment Program (NAWQA). One-hundred and forty-eight samples were collected from 23 sites, and analyzed for pesticide compounds during the study period from November 1998 to September 2001. Sixty-six different pesticide compounds were detected at varying frequencies and concentrations, and one or more pesticides were detected in 92 percent of the samples. All pesticide concentrations were below maximum levels permitted in drinking water. However, two compounds-diazinon and diuron-exceeded nonenforceable drinking water health-advisory levels in at least one stream sample, and five compounds exceeded guidelines to protect aquatic life-carbaryl, chlorpyrifos, diazinon, lindane, and malathion. Twenty-two pesticide compounds were detected in at least 25 percent of the samples collected from any one fixed site. These are identified as 'major' pesticide compounds and are emphasized in this report. \r\n\r\n The degree to which pesticides were used in the basin, as well as their physical-chemical properties, are important explanatory factors in stream pesticide occurrence, and most pesticides probably enter streams with urban runoff. Stormflow substantially increases urban runoff, and storm effects on stream pesticide concentrations sometimes persist for several days or weeks after the storm. Water sources other than urban runoff also deliver pesticide compounds to surface water in the basin. For example, atrazine may enter streams in gaining reaches where ground water carries high loads as a result of historical use in the basin. Also, the data suggest that lindane, and perhaps bromacil, are present in treated wastewater, the predominant source of water to streams in the Santa Ana Basin.","language":"ENGLISH","doi":"10.3133/sir20055203","usgsCitation":"Kent, R., Belitz, K., Altmann, A.J., Wright, M.T., and Mendez, G.O., 2005, Occurrence and distribution of pesticide compounds in surface water of the Santa Ana basin, California, 1998-2001: U.S. Geological Survey Scientific Investigations Report 2005-5203, 152 p., https://doi.org/10.3133/sir20055203.","productDescription":"152 p.","costCenters":[],"links":[{"id":191740,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7080,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5203/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696368","contributors":{"authors":[{"text":"Kent, Robert 0000-0003-4174-9467","orcid":"https://orcid.org/0000-0003-4174-9467","contributorId":20005,"corporation":false,"usgs":true,"family":"Kent","given":"Robert","affiliations":[],"preferred":false,"id":285868,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Belitz, Kenneth 0000-0003-4481-2345 kbelitz@usgs.gov","orcid":"https://orcid.org/0000-0003-4481-2345","contributorId":442,"corporation":false,"usgs":true,"family":"Belitz","given":"Kenneth","email":"kbelitz@usgs.gov","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true}],"preferred":true,"id":285864,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Altmann, Andrea J.","contributorId":14904,"corporation":false,"usgs":true,"family":"Altmann","given":"Andrea","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":285867,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wright, Michael T. 0000-0003-0653-6466 mtwright@usgs.gov","orcid":"https://orcid.org/0000-0003-0653-6466","contributorId":1508,"corporation":false,"usgs":true,"family":"Wright","given":"Michael","email":"mtwright@usgs.gov","middleInitial":"T.","affiliations":[],"preferred":false,"id":285866,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mendez, Gregory O. 0000-0002-9955-3726 gomendez@usgs.gov","orcid":"https://orcid.org/0000-0002-9955-3726","contributorId":1489,"corporation":false,"usgs":true,"family":"Mendez","given":"Gregory","email":"gomendez@usgs.gov","middleInitial":"O.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":false,"id":285865,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":72686,"text":"ofr20051382 - 2005 - USGS Headwaters Province project, Idaho, Montana, and Washington - an overview of publications supporting land-use planning in the northern Rocky Mountains","interactions":[],"lastModifiedDate":"2012-02-02T00:13:59","indexId":"ofr20051382","displayToPublicDate":"2005-11-07T00:00:00","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":"2005-1382","title":"USGS Headwaters Province project, Idaho, Montana, and Washington - an overview of publications supporting land-use planning in the northern Rocky Mountains","language":"ENGLISH","doi":"10.3133/ofr20051382","usgsCitation":"Zientek, M.L., and Lund, K., 2005, USGS Headwaters Province project, Idaho, Montana, and Washington - an overview of publications supporting land-use planning in the northern Rocky Mountains (Version 1.0): U.S. Geological Survey Open-File Report 2005-1382, 1 poster, 36 x 84 in., https://doi.org/10.3133/ofr20051382.","productDescription":"1 poster, 36 x 84 in.","costCenters":[],"links":[{"id":193147,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7106,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1382/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611898","contributors":{"authors":[{"text":"Zientek, Michael L. 0000-0002-8522-9626 mzientek@usgs.gov","orcid":"https://orcid.org/0000-0002-8522-9626","contributorId":2420,"corporation":false,"usgs":true,"family":"Zientek","given":"Michael","email":"mzientek@usgs.gov","middleInitial":"L.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":285873,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lund, Karen 0000-0002-4249-3582 klund@usgs.gov","orcid":"https://orcid.org/0000-0002-4249-3582","contributorId":1235,"corporation":false,"usgs":true,"family":"Lund","given":"Karen","email":"klund@usgs.gov","affiliations":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":285872,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":72684,"text":"sir20055242 - 2005 - Assessment of a model of forest dynamics under contrasting climate and disturbance regimes in the Pacific Northwest [FORCLIM]","interactions":[],"lastModifiedDate":"2012-02-02T00:13:58","indexId":"sir20055242","displayToPublicDate":"2005-11-07T00:00:00","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":"2005-5242","title":"Assessment of a model of forest dynamics under contrasting climate and disturbance regimes in the Pacific Northwest [FORCLIM]","docAbstract":"An individual-based model of forest dynamics (FORCLIM) was tested for its ability to simulate forest composition and structure in the Pacific Northwest region of North America. Simulation results across gradients of climate and disturbance were compared to forest survey data from several vegetation zones in western Oregon. Modelled patterns of tree species composition, total basal area and stand height across climate gradients matched those in the forest survey data. However, the density of small stems (<50 cm DBH) was underestimated by the model. Thus actual size-class structure and other density-based parameters of stand structure were not simulated with high accuracy. The addition of partial-stand disturbances at moderate frequencies (<0.01 yr-1) often improved agreement between simulated and actual results. Strengths and weaknesses of the FORCLIM model in simulating forest dynamics and structure in the Pacific Northwest are discussed.","language":"ENGLISH","doi":"10.3133/sir20055242","usgsCitation":"Busing, R.T., and Solomon, A.M., 2005, Assessment of a model of forest dynamics under contrasting climate and disturbance regimes in the Pacific Northwest [FORCLIM]: U.S. Geological Survey Scientific Investigations Report 2005-5242, 23 p., https://doi.org/10.3133/sir20055242.","productDescription":"23 p.","costCenters":[],"links":[{"id":191787,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7081,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5242/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672884","contributors":{"authors":[{"text":"Busing, Richard T.","contributorId":13303,"corporation":false,"usgs":true,"family":"Busing","given":"Richard","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":285869,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Solomon, Allen M.","contributorId":20394,"corporation":false,"usgs":true,"family":"Solomon","given":"Allen","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":285870,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":72681,"text":"ofr20051327 - 2005 - Calculation of area and volume for the south part of Great Salt Lake, Utah","interactions":[],"lastModifiedDate":"2017-02-05T12:53:11","indexId":"ofr20051327","displayToPublicDate":"2005-11-07T00:00:00","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":"2005-1327","title":"Calculation of area and volume for the south part of Great Salt Lake, Utah","docAbstract":"The U.S. Geological Survey, in cooperation with the Utah Department of Natural Resources, Division of Wildlife Resources, collected bathymetric data for the south part of Great Salt Lake during 2002-04 using a single-beam, high-definition fathometer and real-time differential global positioning system. About 7.6 million depth measurements were collected along more than 930 miles (1,690 kilometers) of survey transects. Sound-velocity profiles were obtained in conjunction with the bathymetric data to provide time-of-travel corrections to the depth calculations. Data were processed with commercial hydrographic software and exported into geographic information system (GIS) software for mapping and calculation of area and volume. Area and volume calculations show a maximum area of about 508,000 acres (2,056 square kilometers) and a maximum volume of about 9,257,000 acre-feet (11.42 cubic kilometers) at a water-surface altitude of 4,200 feet (1,280 meters). Minimum water-surface altitude of the south part of Great Salt Lake is just below 4,167 feet (1,279 meters) in the area just south of the Union Pacific railroad causeway halfway between Promontory Point and the western edge of the lake. At this altitude, and continuing up to about 4,176 feet (1,279 meters), the south part of the lake is separated into two areas by a ridge extending from Promontory Point to Hat Island. Calculations for area and volume are based on a low altitude of 4,167 feet (1,279 meters) to a high altitude of 4,200 feet (1,280 meters).
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051327","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources, Division of Wildlife Resources","usgsCitation":"Baskin, R.L., 2005, Calculation of area and volume for the south part of Great Salt Lake, Utah (Version 1.0): U.S. Geological Survey Open-File Report 2005-1327, 6 p., https://doi.org/10.3133/ofr20051327.","productDescription":"6 p.","numberOfPages":"6","costCenters":[],"links":[{"id":193172,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":334781,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/sim2894","text":"Scientific Investigations Map 2894: Bathymetric map of the south part of Great Salt Lake, Utah, 2005"},{"id":7078,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1327/","linkFileType":{"id":5,"text":"html"}},{"id":334780,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2005/1327/PDF/OFR2005-1327.pdf"}],"country":"United States","state":"Utah","otherGeospatial":"Great Salt Lake","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.86749999999999,40.6175 ], [ -112.86749999999999,41.25 ], [ -111.86749999999999,41.25 ], [ -111.86749999999999,40.6175 ], [ -112.86749999999999,40.6175 ] ] ] } } ] }","edition":"Version 1.0","publicComments":"Use with Scientific Investigations Map 2894","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f968a","contributors":{"authors":[{"text":"Baskin, Robert L. 0000-0002-2175-8502 rbaskin@usgs.gov","orcid":"https://orcid.org/0000-0002-2175-8502","contributorId":360,"corporation":false,"usgs":true,"family":"Baskin","given":"Robert","email":"rbaskin@usgs.gov","middleInitial":"L.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285863,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":72680,"text":"sim2894 - 2005 - Bathymetric map of the south part of Great Salt Lake, Utah, 2005","interactions":[],"lastModifiedDate":"2017-02-05T12:53:16","indexId":"sim2894","displayToPublicDate":"2005-11-07T00:00:00","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":"2894","title":"Bathymetric map of the south part of Great Salt Lake, Utah, 2005","docAbstract":"The U.S. Geological Survey, in cooperation with the Utah Department of Natural Resources, Division of Wildlife Resources, collected bathymetric data for the south part of Great Salt Lake during 2002–04 using a single beam, high-definition fathometer and real-time differential global positioning system. Approximately 7.6 million depth readings were collected along more than 1,050 miles of survey transects for construction of this map. Sound velocities were obtained in conjunction with the bathymetric data to provide time-of-travel corrections to the depth calculations. Data were processed with commercial hydrographic software and exported into geographic information system (GIS) software for mapping. Because of the shallow nature of the lake and the limitations of the instrumentation, contours above an altitude of 4,193 feet were digitized from existing USGS 1:24,000 source-scale digital line graph data.
For additional information on methods used to derive the bathymetric contours for this map, please see Baskin, Robert L., 2005, Calculation of area and volume for the south part of Great Salt Lake, Utah, U.S. Geological Survey Open-File Report OFR–2005–1327.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/sim2894","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources, Division of Wildlife Resource","usgsCitation":"Baskin, R.L., and Allen, D.V., 2005, Bathymetric map of the south part of Great Salt Lake, Utah, 2005 (Version 1.0): U.S. Geological Survey Scientific Investigations Map 2894, 1 Map: 31 x 38 in., https://doi.org/10.3133/sim2894.","productDescription":"1 Map: 31 x 38 in.","numberOfPages":"1","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":193173,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":334779,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/ofr20051327","text":"Open-File Report 2005-1327: Calculation of area and volume for the south part of Great Salt Lake, Utah"},{"id":334778,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sim/2005/2894/PDF/SIM2894.pdf","text":"Map"},{"id":7079,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/2005/2894/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Utah","otherGeospatial":"Great Salt Lake","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.86749999999999,40.6175 ], [ -112.86749999999999,41.25 ], [ -111.86749999999999,41.25 ], [ -111.86749999999999,40.6175 ], [ -112.86749999999999,40.6175 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db64073a","contributors":{"authors":[{"text":"Baskin, Robert L. 0000-0002-2175-8502 rbaskin@usgs.gov","orcid":"https://orcid.org/0000-0002-2175-8502","contributorId":360,"corporation":false,"usgs":true,"family":"Baskin","given":"Robert","email":"rbaskin@usgs.gov","middleInitial":"L.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285861,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allen, David V.","contributorId":75989,"corporation":false,"usgs":true,"family":"Allen","given":"David","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":285862,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70175127,"text":"wdrNY051 - 2005 - Water Resources Data New York Water Year 2005, Volume 1: Eastern New York excluding Long Island","interactions":[],"lastModifiedDate":"2017-03-30T15:42:05","indexId":"wdrNY051","displayToPublicDate":"2005-11-06T08:30:00","publicationYear":"2005","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":"NY-05-1","title":"Water Resources Data New York Water Year 2005, Volume 1: Eastern New York excluding Long Island","docAbstract":"Water resources data for the 2005 water year for Eastern New York Excluding Long Island consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and ground-water levels. This volume contains records for water discharge at 145 gaging stations; stage only at 8 gaging stations; stage and contents at 6 gaging stations, and 11 other lakes and reservoirs; water quality at 29 gaging stations and 37 other sites; and water levels at 30 observation wells. Also included are data for 34 crest-stage partial-record stations and 50 miscellaneous-measurement sites. These data together with the data in volumes 2 and 3 represent that part of the National Water Data System operated by the U.S. Geological Survey in cooperation with State, Municipal, and Federal agencies in New York.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNY051","usgsCitation":"U.S. Geological Survey, 2005, Water Resources Data New York Water Year 2005, Volume 1: Eastern New York excluding Long Island: U.S. Geological Survey Water Data Report NY-05-1, Summary: 9 p.; Data: vi, 996 p.; Discontinued sites: 12 p., https://doi.org/10.3133/wdrNY051.","productDescription":"Summary: 9 p.; Data: vi, 996 p.; Discontinued sites: 12 p.","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":326652,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":325850,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/2005/wdr-ny-05-1/troy.disc05.pdf","text":"Discontinued Sites","size":"44.3 KB","linkFileType":{"id":1,"text":"pdf"},"description":"WDR 2005-NY-05-1"},{"id":325848,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/2005/wdr-ny-05-1/rept.sum05.pdf","text":"Summary of Hydrologic Conditions","size":"229 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WDR 2005-NY-05-1"},{"id":325849,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/2005/wdr-ny-05-1/wdrny051.rept.data.pdf","text":"Surface-water, Water-quality, and Ground-water Data ","size":"34.7 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WDR 2005-NY-05-1"}],"country":"United States","state":"New York","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -74.674072265625,\n 45.01141864227728\n ],\n [\n -74.124755859375,\n 45.01141864227728\n ],\n [\n -73.289794921875,\n 45.02695045318546\n ],\n [\n -73.32275390625,\n 44.74673324024678\n ],\n [\n -73.377685546875,\n 44.653024159812\n ],\n [\n -73.355712890625,\n 44.55916341529184\n ],\n [\n -73.30078125,\n 44.4808302785626\n ],\n [\n -73.355712890625,\n 44.315987905196906\n ],\n [\n -73.399658203125,\n 44.190082025040525\n ],\n [\n -73.399658203125,\n 44.11125397357153\n ],\n [\n -73.4326171875,\n 44.01652134387754\n ],\n [\n -73.388671875,\n 43.866218006556394\n ],\n [\n -73.355712890625,\n 43.8028187190472\n ],\n [\n -73.377685546875,\n 43.67581809328344\n ],\n [\n -73.41064453125,\n 43.58834891179792\n ],\n [\n -73.30078125,\n 43.620170616189924\n ],\n [\n -73.245849609375,\n 43.55651037504758\n ],\n [\n -73.2568359375,\n 43.30919109985686\n ],\n [\n -73.30078125,\n 42.74701217318067\n ],\n [\n -73.49853515625,\n 42.10637370579324\n ],\n [\n -73.531494140625,\n 41.32732632036622\n ],\n [\n -73.47656249999999,\n 41.18692242290296\n ],\n [\n -73.443603515625,\n 41.062786068733026\n ],\n [\n -73.465576171875,\n 40.98819156349393\n ],\n [\n -73.553466796875,\n 40.93841495689795\n ],\n [\n -73.619384765625,\n 40.979898069620155\n ],\n [\n -73.740234375,\n 40.91351257612758\n ],\n [\n -74.036865234375,\n 41.02964338716638\n ],\n [\n -74.674072265625,\n 41.343824581185686\n ],\n [\n -74.81689453125,\n 41.43449030894922\n ],\n [\n -74.99267578125,\n 41.541477666790286\n ],\n [\n -75.069580078125,\n 41.590796851056005\n ],\n [\n -75.08056640625,\n 41.672911819602085\n ],\n [\n -75.091552734375,\n 41.77131167976407\n ],\n [\n -75.12451171875,\n 41.84501267270692\n ],\n [\n -75.30029296875,\n 41.88592102814744\n ],\n [\n -75.34423828125,\n 41.95131994679697\n ],\n [\n -75.531005859375,\n 42.01665183556825\n ],\n [\n -75.640869140625,\n 42.19596877629178\n ],\n [\n -75.640869140625,\n 42.391008609205045\n ],\n [\n -75.487060546875,\n 42.66628070564928\n ],\n [\n -75.333251953125,\n 42.85985981506279\n ],\n [\n -75.35522460937499,\n 43.068887774169625\n ],\n [\n -75.498046875,\n 43.197167282501276\n ],\n [\n -76.04736328125,\n 43.691707903073805\n ],\n [\n -76.201171875,\n 43.8028187190472\n ],\n [\n -76.17919921875,\n 43.96119063892024\n ],\n [\n -76.256103515625,\n 44.03232064275084\n ],\n [\n -76.365966796875,\n 44.11914151643737\n ],\n [\n -76.26708984375,\n 44.213709909702054\n ],\n [\n -76.11328125,\n 44.3002644115815\n ],\n [\n -75.95947265625,\n 44.35527821160296\n ],\n [\n -75.816650390625,\n 44.457309801319305\n ],\n [\n -75.65185546874999,\n 44.61393394730626\n ],\n [\n -75.289306640625,\n 44.88701247981298\n ],\n [\n -75.08056640625,\n 44.933696389694674\n ],\n [\n -74.959716796875,\n 45.00365115687189\n ],\n [\n -74.805908203125,\n 45.034714778688624\n ],\n [\n -74.674072265625,\n 45.01141864227728\n ]\n ]\n ]\n }\n }\n ]\n}","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/
No abstract available.
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