Historical trends in streamflow, sedimentation, and sediment chemistry of the Wolf River were examined for a 6-mile reach that flows through the southern part of the Menominee Indian Reservation and the northern part of Shawano County, Wis. Trends were examined in the context of effects from dams, climate, and land-cover change. Annual flood peaks and mean monthly flow for the Wolf River were examined for 1907-96 and compared to mean annual and mean monthly precipitation. Analysis of trends in sedimentation (from before about 1850 through 1999) involved collection of cores and elevation data along nine valley transects spanning the Wolf River channel, flood plain, and backwater and impounded areas; radioisotope analyses of impounded sediment cores; and analysis of General Land Office Survey Notes (1853-91). Trends in sediment chemistry were examined by analyzing samples from an impoundment core for minor and trace elements. Annual flood peaks for the Wolf River decreased during 1907-49 but increased during 1950-96, most likely reflecting general changes in upper-atmospheric circulation patterns from more zonal before 1950 to more meridional after 1950. The decrease in flood peaks during 1907-49 may also, in part, be due to forest regrowth. Mean monthly streamflow during 1912-96 increased for the months of February and March but decreased for June and July, suggesting that spring snowmelt occurs earlier in the season than it did in the past. Decreases in early summer flows may be a reflection earlier spring snowmelt and large rainstorms in early spring rather than early summer. These trends also may reflect upper-atmospheric circulation patterns. The Balsam Row Dam impoundment contains up to 10 feet of organic-rich silty clay and has lost much of its storage capacity. Fine sediment has accumulated for 1.8 miles upstream from the Balsam Row Dam. Historical average linear and mass sedimentation rates in the Balsam Row impoundment were 0.09 feet per year and 1.15 pounds per square foot per year for 1927-62 and 0.10 feet per year and 1.04 pounds per square foot per year for 1963-99. Sedimentation in the impoundment was episodic and was associated with large floods, especially the flood-related failure of the Keshena Falls Dam in 1972 and a large flood in 1973. Sand deposition is common in the Wolf River upstream from the impounded reach for 2.5 miles and is caused by the base-level increase associated with the Balsam Row Dam. Some sand deposition also may have been associated with logging and log drives in the late 1800s and the failure of the Keshena Falls Dam. In the upstream 1.5-mile part of the studied reach, the substrate is mainly rocky; however, about 2,000 feet downstream from Keshena Falls, the channel has narrowed and incised since the 1890s, likely related to human alterations associated with logging, log drives, and (or) changes in hydraulics and sediment characteristics associated with completion of the Keshena Falls Dam and head race in 1908. Minor- and trace-element concentrations in sediment from Balsam Row impoundment and other depositional areas along the Wolf River generally reflect background conditions as affected by watershed geology and historical inputs from regional and local atmospheric deposition.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055030","collaboration":"In cooperation with the Menominee Indian Tribe of Wisconsin","usgsCitation":"Fitzpatrick, F.A., 2005, Trends in streamflow, sedimentation, and sediment chemistry for the Wolf River, Menominee Indian Reservation, Wisconsin, 1850-1999: U.S. Geological Survey Scientific Investigations Report 2005-5030, vi, 47 p., https://doi.org/10.3133/sir20055030.","productDescription":"vi, 47 p.","numberOfPages":"55","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1849-12-30","temporalEnd":"1999-01-01","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":191281,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":311329,"rank":101,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5030/pdf/SIR_2005-5030.pdf"},{"id":6843,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5030/","linkFileType":{"id":5,"text":"html"}}],"scale":"100000","country":"United States","state":"Wisconsin","county":"Menominee County","otherGeospatial":"Menominee Indian Reservation","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-88.6399,45.1171],[-88.6109,45.1174],[-88.5598,45.1175],[-88.4836,45.117],[-88.4862,45.0302],[-88.4881,44.9435],[-88.4894,44.8554],[-88.6117,44.8563],[-88.736,44.8561],[-88.7356,44.9429],[-88.7982,44.9432],[-88.8588,44.943],[-88.9516,44.943],[-88.9812,44.9427],[-88.9812,45.0299],[-88.9818,45.118],[-88.9301,45.1182],[-88.8623,45.1175],[-88.8118,45.1177],[-88.7343,45.1172],[-88.6826,45.1174],[-88.6574,45.1172],[-88.6399,45.1171]]]},\"properties\":{\"name\":\"Menominee\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db69606b","contributors":{"authors":[{"text":"Fitzpatrick, Faith A. fafitzpa@usgs.gov","contributorId":1182,"corporation":false,"usgs":true,"family":"Fitzpatrick","given":"Faith","email":"fafitzpa@usgs.gov","middleInitial":"A.","affiliations":[{"id":476,"text":"North Carolina Water Science Center","active":true,"usgs":true}],"preferred":false,"id":282779,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70637,"text":"sir20045241 - 2005 - Remote sensing for environmental site screening and watershed evaluation in Utah Mine lands: East Tintic mountains, Oquirrh mountains, and Tushar mountains","interactions":[],"lastModifiedDate":"2022-12-22T20:08:18.850387","indexId":"sir20045241","displayToPublicDate":"2005-06-02T00:00:00","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":"2004-5241","title":"Remote sensing for environmental site screening and watershed evaluation in Utah Mine lands: East Tintic mountains, Oquirrh mountains, and Tushar mountains","docAbstract":"Imaging spectroscopy-a powerful remote-sensing tool for mapping subtle variations in the composition of minerals, vegetation, and man-made materials on the Earth's surface-was applied in support of environmental assessments and watershed evaluations in several mining districts in the State of Utah. Three areas were studied through the use of Landsat 7 ETM+ and Airborne Visible/Infrared Imaging Spectrometer (AVIRIS) data: (1) the Tintic mining district in the East Tintic Mountains southwest of Provo, (2) the Camp Floyd mining district (including the Mercur mine) and the Stockton (or Rush Valley) mining district in the Oquirrh Mountains south of the Great Salt Lake, and (3) the Tushar Mountains and Antelope Range near Marysvale.
The Landsat 7 ETM+ data were used for initial site screening and the planning of AVIRIS surveys. The AVIRIS data were analyzed to create spectrally defined maps of surface minerals with special emphasis on locating and characterizing rocks and soils with acid-producing potential (APP) and acid-neutralizing potential (ANP). These maps were used by the United States Environmental Protection Agency (USEPA) for three primary purposes: (1) to identify unmined and anthropogenic sources of acid generation in the form of iron sulfide and (or) ferric iron sulfate-bearing minerals such as jarosite and copiapite; (2) to seek evidence for downstream or downwind movement of minerals associated with acid generation, mine waste, and (or) tailings from mines, mill sites, and zones of unmined hydrothermally altered rocks; and (3) to identify carbonate and other acid-buffering minerals that neutralize acidic, potentially metal bearing, solutions and thus mitigate potential environmental effects of acid generation.
Calibrated AVIRIS surface-reflectance data were spectrally analyzed to identify and map selected surface materials. Two maps were produced from each flightline of AVIRIS data: a map of iron-bearing minerals and water having absorption features in the spectral region from 0.35 µm to 1.35 µm and a map of minerals (including clays, sulfates, micas, and carbonates) having absorptions in the spectral region from 1.45 µm to 2.51 µm. Several methods were used to verify the AVIRIS mapping results, including field checking of selected locations with a portable spectrometer, visual inspection of the AVIRIS reflectance spectra, and X-ray diffraction (XRD) analysis of field samples.
The maps of iron-bearing minerals derived from analysis of the visible (VIS) and near-infrared (NIR) regions of the electromagnetic spectrum were shown to be more consistently reliable in indicating the presence of jarosite than were the maps generated from analysis of the short-wave infrared (SWIR) region. When present in abundance, phyllosilicate minerals tend to dominate the SWIR and mask the spectral features of jarosite in that wavelength region. The crystal field absorptions of jarosite in the VIS and NIR spectral regions will commonly be present regardless of whether the Fe-OH absorption feature near 2.27 µm can be detected. For this reason, the VIS and NIR were preferable to the SWIR for the remote spectroscopic identification of jarosite (and other iron-bearing minerals).
Large exposures of unmined hydrothermally altered rocks occur throughout the three study areas. These rocks commonly contain sulfide or sulfate minerals that produce sulfuric acid upon subaerial oxidation. The acid may be introduced into local surface and ground water and thus lower the baseline (that is, the premining) pH for a watershed.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20045241","usgsCitation":"Rockwell, B.W., McDougal, R., and Gent, C.A., 2005, Remote sensing for environmental site screening and watershed evaluation in Utah Mine lands: East Tintic mountains, Oquirrh mountains, and Tushar mountains (Version 1.2): U.S. Geological Survey Scientific Investigations Report 2004-5241, Report: viii, 84 p.; Figures, https://doi.org/10.3133/sir20045241.","productDescription":"Report: viii, 84 p.; Figures","costCenters":[],"links":[{"id":410962,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73988.htm","linkFileType":{"id":5,"text":"html"}},{"id":8924,"rank":3,"type":{"id":25,"text":"Version History"},"url":"https://pubs.usgs.gov/sir/2004/5241/sirHist.html","linkFileType":{"id":5,"text":"html"}},{"id":191808,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6846,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2004/5241/","linkFileType":{"id":5,"text":"html"}},{"id":7886,"rank":2,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/sir/2004/5241/figures.html","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Utah","otherGeospatial":"East Tintic Mountains, Oquirrh Mountains, Tushar Mountains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -113.29022483358571,\n 40.93599326796834\n ],\n [\n -113.29022483358571,\n 37.86776389090204\n ],\n [\n -111.17415878264146,\n 37.86776389090204\n ],\n [\n -111.17415878264146,\n 40.93599326796834\n ],\n [\n -113.29022483358571,\n 40.93599326796834\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","edition":"Version 1.2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bf7d","contributors":{"authors":[{"text":"Rockwell, Barnaby W. 0000-0002-9549-0617 barnabyr@usgs.gov","orcid":"https://orcid.org/0000-0002-9549-0617","contributorId":2195,"corporation":false,"usgs":true,"family":"Rockwell","given":"Barnaby","email":"barnabyr@usgs.gov","middleInitial":"W.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":282792,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McDougal, Robert R.","contributorId":53418,"corporation":false,"usgs":true,"family":"McDougal","given":"Robert R.","affiliations":[],"preferred":false,"id":282794,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gent, Carol A.","contributorId":40646,"corporation":false,"usgs":true,"family":"Gent","given":"Carol","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":282793,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70646,"text":"i2811 - 2005 - Geologic map of Cydonia Mensae - southern Acidalia Planitia, Mars, quadrangles MTM 40007, 40012, 40017, 45007, 45012, and 45017","interactions":[],"lastModifiedDate":"2023-07-05T11:09:20.903456","indexId":"i2811","displayToPublicDate":"2005-06-02T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2811","title":"Geologic map of Cydonia Mensae - southern Acidalia Planitia, Mars, quadrangles MTM 40007, 40012, 40017, 45007, 45012, and 45017","docAbstract":"Cydonia Mensae lie adjacent to the boundary separating the highland terrain of western Arabia Terra from the northern lowlands (the dichotomy boundary), where this boundary is gradational rather than abrupt, as is generally the case. Cydonia Mensae are characterized by abundant knobs and mesas, most of which occur in well defined clusters that commonly are long and narrow. The adjacent lowland of Acidalia Planitia contains abundant troughs that define a crude, very large scale polygonal pattern. This pattern, and the troughs, are similar in size and spacing to those in Utopia Planitia (for example, McGill and Hills, 1992; Hiesinger and Head, 2000). The six 1:500,000-scale quadrangles mapped are MTM 40007, 40012, 40017, 45007, 45012, and 45017, which include northern Cydonia Mensae, part of southern Acidalia Planitia, and a small area of Arabia Terra highlands. These six quadrangles are combined into a single map at 1:1,000,000 scale for this publication. Issues of interest addressed by this mapping include the crustal history implied by the knobs and mesas of Cydonia Mensae, the implications of the gradational dichotomy boundary, the age of the Acidalia plains materials, the origin and age of the giant polygons, the validity of putative shorelines inferred to be present in this area, and the origin of the very abundant small cones and domes, specifically if these imply the past presence of water or ice within the plains materials. Earlier maps (Witbeck and Underwood, 1984; Scott and Tanaka, 1986; Tanaka and others, 2003) that included the area mapped for this study addressed some or all of these issues, but these maps were more regional in coverage and were at smaller scales. In addition, new orbital data from Mars Global Surveyor and Mars Odyssey missions were available only to Tanaka and others (2003). The intent of this present study is to address the issues listed by mapping at a scale large enough to permit greater map detail and to better understand the areal distribution of the materials and features of interest.
","language":"English","publisher":"U.S Geological Survey","doi":"10.3133/i2811","usgsCitation":"McGill, G.E., 2005, Geologic map of Cydonia Mensae - southern Acidalia Planitia, Mars, quadrangles MTM 40007, 40012, 40017, 45007, 45012, and 45017: U.S. Geological Survey IMAP 2811, HTML Document, https://doi.org/10.3133/i2811.","productDescription":"HTML Document","costCenters":[],"links":[{"id":6749,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i2811/","linkFileType":{"id":5,"text":"html"}},{"id":185578,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"5000000","otherGeospatial":"Mars","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a33b1","contributors":{"authors":[{"text":"McGill, George E.","contributorId":47462,"corporation":false,"usgs":true,"family":"McGill","given":"George","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":282813,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70636,"text":"sir20045284 - 2005 - Stream-sediment geochemistry in mining-impacted streams: Prichard, Eagle, and Beaver Creeks, northern Coeur d'Alene mining district, northern Idaho","interactions":[],"lastModifiedDate":"2023-04-18T19:39:08.934673","indexId":"sir20045284","displayToPublicDate":"2005-06-02T00:00:00","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":"2004-5284","title":"Stream-sediment geochemistry in mining-impacted streams: Prichard, Eagle, and Beaver Creeks, northern Coeur d'Alene mining district, northern Idaho","docAbstract":"This report presents the results of one aspect of an integrated watershed-characterization study that was undertaken to assess the impacts of historical mining and milling of silver-lead-zinc ores on water and sediment composition and on aquatic biota in streams draining the northern part of the Coeur d'Alene Mining District in northern Idaho. We present the results of chemical analyses of 62 samples of streambed sediment, 19 samples of suspended sediment, 23 samples of streambank soil, and 29 samples of mine- and mill-related artificial- fill material collected from the drainages of Prichard, Eagle, and Beaver Creeks, all tributaries to the North Fork of the Coeur d'Alene River. All samples were sieved into three grain-size fractions (<0.063, 0.063-0.25, and 0.25-1.0 mm) and analyzed for 40 elements after four-acid digestion by inductively coupled plasma atomic-emission spectrometry and for mercury by continuous-flow cold-vapor atomic-absorption spectrometry in the U.S. Geological Survey laboratory in Denver, Colo.
Historical mining of silver-lead-zinc ores in the headwater reaches of the Prichard Creek, Eagle Creek, and Beaver Creek drainages has resulted in enrichments of lead, zinc, mercury, arsenic, cadmium, silver, copper, cobalt, and, to a lesser extent, iron and manganese in streambed sediment. Using samples collected from the relatively unimpacted West Fork of Eagle Creek as representative of background compositions, streambed sediment in the vicinity of the mines and millsites has Pb and Zn contents of 20 to 100 times background values, decreasing to 2 to 5 times background values at the mouth of the each stream, 15 to 20 km downstream. Lesser enrichments (<10 times background values) of mercury and arsenic also are generally associated with, and decrease downstream from, historical silver-lead-zinc mining in the drainages. However, enrichments of arsenic and, to a lesser extent, mercury also are areally associated with the lode gold deposits along Prichard Creek near Murray, which were not studied here. Metal contents in samples of unfractionated suspended sediment collected during a high-flow event in April 2000 are generally similar to, but slightly higher than, those in the fine (<0.063-mm grain size) fraction of streambed sediment from the same sampling site. Although metal enrichment in streambed sediment typically begins adjacent to the mine portals and their associated mine-waste rock dumps, volumetrically larger inputs of metal-enriched materials were contributed by the ore-concentration millsites and their associated, more finely ground, more metal rich mill-tailings impoundments
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20045284","usgsCitation":"Box, S.E., Wallis, J., Briggs, P.H., and Brown, Z.A., 2005, Stream-sediment geochemistry in mining-impacted streams: Prichard, Eagle, and Beaver Creeks, northern Coeur d'Alene mining district, northern Idaho: U.S. Geological Survey Scientific Investigations Report 2004-5284, Report: v, 62 p.; Data Downloads, https://doi.org/10.3133/sir20045284.","productDescription":"Report: v, 62 p.; Data Downloads","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":191352,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":415938,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_71372.htm","linkFileType":{"id":5,"text":"html"}},{"id":6845,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2004/5284/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Idaho","otherGeospatial":"Prichard, Eagle, and Beaver Creeks","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -115.9869,\n 47.5528\n ],\n [\n -115.7172,\n 47.5528\n ],\n [\n -115.7172,\n 47.701\n ],\n [\n -115.9869,\n 47.701\n ],\n [\n -115.9869,\n 47.5528\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4fe2","contributors":{"authors":[{"text":"Box, Stephen E. 0000-0002-5268-8375 sbox@usgs.gov","orcid":"https://orcid.org/0000-0002-5268-8375","contributorId":1843,"corporation":false,"usgs":true,"family":"Box","given":"Stephen","email":"sbox@usgs.gov","middleInitial":"E.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":282788,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wallis, John C.","contributorId":45755,"corporation":false,"usgs":true,"family":"Wallis","given":"John C.","affiliations":[],"preferred":false,"id":282790,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Briggs, Paul H.","contributorId":30973,"corporation":false,"usgs":true,"family":"Briggs","given":"Paul","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":282789,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brown, Zoe Ann","contributorId":95530,"corporation":false,"usgs":true,"family":"Brown","given":"Zoe","email":"","middleInitial":"Ann","affiliations":[],"preferred":false,"id":282791,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70648,"text":"fs20053063 - 2005 - Availability of ground-water data for California, water year 2004","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"fs20053063","displayToPublicDate":"2005-06-02T00:00:00","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":"2005-3063","title":"Availability of ground-water data for California, water year 2004","language":"ENGLISH","doi":"10.3133/fs20053063","usgsCitation":"Huff, J., 2005, Availability of ground-water data for California, water year 2004: U.S. Geological Survey Fact Sheet 2005-3063, 2 p. : map, https://doi.org/10.3133/fs20053063.","productDescription":"2 p. : map","costCenters":[],"links":[{"id":121143,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3063.bmp"},{"id":6751,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3063/","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d868","contributors":{"authors":[{"text":"Huff, Julia A.","contributorId":23130,"corporation":false,"usgs":true,"family":"Huff","given":"Julia A.","affiliations":[],"preferred":false,"id":282819,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70608,"text":"wdrMS041 - 2005 - Water resources data Mississippi water year 2004","interactions":[],"lastModifiedDate":"2012-02-02T00:14:00","indexId":"wdrMS041","displayToPublicDate":"2005-06-01T00:00:00","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":"MS-04-1","title":"Water resources data Mississippi water year 2004","docAbstract":"Water resources data for this water year for Mississippi consists of records of surface water and ground water in the State. Specifically, it contains: (1) Discharge records for 90 streamflow-gaging stations, stage records for 18 of these gaging stations, discharge records for 97 partial-record stations or miscellaneous streamflow sites, including 6 flood hydrograph partial-record stations, 91 crest-stage partial-record stations and 0 special study and miscellaneous sites; (2) stage only at 1 gaging station; (3) water-quality records for 12 streamflow-gaging stations, 0 stage-only stations, 13 water-quality monitor stations, 0 partial-record stations or miscellaneous sites, 0 short-term study sites, and 26 wells; and (4) water-level records for 19 observation wells. Records obtained from water-resources investigations are also included in special sections of the report. Records included for stream stages are only a small fraction of those obtained during the water year.","language":"ENGLISH","doi":"10.3133/wdrMS041","usgsCitation":"Morris, F., Runner, M., and Storm, J., 2005, Water resources data Mississippi water year 2004 (Online only): U.S. Geological Survey Water Data Report MS-04-1, 300 p., https://doi.org/10.3133/wdrMS041.","productDescription":"300 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":6798,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdr-ms-04-1/","linkFileType":{"id":5,"text":"html"}},{"id":192772,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"100000","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a02e4b07f02db5f80b0","contributors":{"authors":[{"text":"Morris, F. III","contributorId":76395,"corporation":false,"usgs":true,"family":"Morris","given":"F.","suffix":"III","email":"","affiliations":[],"preferred":false,"id":282718,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Runner, M.S.","contributorId":28630,"corporation":false,"usgs":true,"family":"Runner","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":282716,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Storm, J.B.","contributorId":51838,"corporation":false,"usgs":true,"family":"Storm","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":282717,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70185646,"text":"70185646 - 2005 - Environmental issues of petroleum exploration and production: Introduction","interactions":[],"lastModifiedDate":"2018-11-05T10:58:39","indexId":"70185646","displayToPublicDate":"2005-06-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1541,"text":"Environmental Geosciences","active":true,"publicationSubtype":{"id":10}},"title":"Environmental issues of petroleum exploration and production: Introduction","docAbstract":"Energy is the lifeblood of our planet Earth, an essential commod- ity that powers the expanding global economy. Starting in the 1950s, oil and natural gas became the main sources of primary energy for the increasing world population, and this dominance is expected to continue for several more decades (Edwards, 1997; Energy Information Administration (EIA), 2004). In the United States, petroleum production started in 1859 when Drake's well was drilled near Titusville, Pennsylvania, and oil and natural gas currently supply approximately 63% of the energy consumption; forecasts indicate that by 2025, their use will increase by about 40% to 28.3 million bbl/day and to 31.4 tcf/yr (EIA, 2004). The clear benefits of petroleum consumption, however, can carry major environmental impacts that may be regional or global in scale, in- cluding air pollution, global climate change, and oil spills. This vol- ume of Environmental Geosciences, covering environmental impacts of petroleum exploration and production, does not address these major impacts directly because air pollution and global warming are issues related primarily to petroleum and coal uses, and major oil spills are generally attributed to marine petroleum transportation, such as the Exxon Valdez's 1989 spill of 260,000 bbl of oil into Prince William Sound, Alaska. Exploration for and production of petroleum, however, have caused local detrimental impacts to soils, surface and groundwa- ters, and ecosystems in the 36 producing states in the United States (Richter and Kreitler, 1993; Kharaka and Hanor, 2003). These im- pacts arose primarily from the improper disposal of some of the large volumes (presently estimated at 20 billion bbl/yr total pro- duced) of saline water produced with oil and gas, from accidental hydrocarbon and produced-water releases, and from abandoned oil wells that were orphaned or not correctly plugged (Kharaka et al., 1995; Veil et al., 2004). Impacts and ground-surface disturbances, in the order of several acres per well, can also arise from related activities such as site clearance, construction of roads, tank bat- teries, brine pits and pipelines, and other land modifications nec- essary for the drilling of exploration and production wells and construction of production facilities. The cumulative impacts from these operations are high, because a total of about 3.5 million oil.
","language":"English","publisher":"AAPG","usgsCitation":"Kharaka, Y.K., and Dorsey, N.S., 2005, Environmental issues of petroleum exploration and production: Introduction: Environmental Geosciences, v. 12, no. 2, p. 61-63.","productDescription":"3 p. ","startPage":"61","endPage":"63","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338346,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":359151,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://toxics.usgs.gov/pubs/KharakaIntro.PDF"}],"volume":"12","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58da251be4b0543bf7fda802","contributors":{"authors":[{"text":"Kharaka, Yousif K. 0000-0001-9861-8260 ykharaka@usgs.gov","orcid":"https://orcid.org/0000-0001-9861-8260","contributorId":1928,"corporation":false,"usgs":true,"family":"Kharaka","given":"Yousif","email":"ykharaka@usgs.gov","middleInitial":"K.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":686207,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dorsey, Nancy S.","contributorId":189835,"corporation":false,"usgs":false,"family":"Dorsey","given":"Nancy","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":686208,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70184392,"text":"70184392 - 2005 - Ground-water/surface-water responses to global climate simulations, Santa Clara-Calleguas basin, Ventura County, California, 1950-93","interactions":[],"lastModifiedDate":"2018-09-18T10:14:43","indexId":"70184392","displayToPublicDate":"2005-06-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2529,"text":"Journal of the American Water Resources Association","active":true,"publicationSubtype":{"id":10}},"title":"Ground-water/surface-water responses to global climate simulations, Santa Clara-Calleguas basin, Ventura County, California, 1950-93","docAbstract":"Climate variations can play an important, if not always crucial, role in successful conjunctive management of ground water and surface water resources. This will require accurate accounting of the links between variations in climate, recharge, and withdrawal from the resource systems, accurate projection or predictions of the climate variations, and accurate simulation of the responses of the resource systems. To assess linkages and predictability of climate influences on conjunctive management, global climate model (GCM) simulated precipitation rates were used to estimate inflows and outflows from a regional ground water model (RGWM) of the coastal aquifers of the Santa Clara-Calleguas Basin at Ventura, California, for 1950 to 1993. Interannual to interdecadal time scales of the El Niño Southern Oscillation (ENSO) and Pacific Decadal Oscillation (PDO) climate variations are imparted to simulated precipitation variations in the Southern California area and are realistically imparted to the simulated ground water level variations through the climate-driven recharge (and discharge) variations. For example, the simulated average ground water level response at a key observation well in the basin to ENSO variations of tropical Pacific sea surface temperatures is 1.2 m/°C, compared to 0.9 m/°C in observations. This close agreement shows that the GCM-RGWM combination can translate global scale climate variations into realistic local ground water responses. Probability distributions of simulated ground water level excursions above a local water level threshold for potential seawater intrusion compare well to the corresponding distributions from observations and historical RGWM simulations, demonstrating the combination's potential usefulness for water management and planning. Thus the GCM-RGWM combination could be used for planning purposes and — when the GCM forecast skills are adequate — for near term predictions.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1752-1688.2005.tb03752.x","usgsCitation":"Hanson, R.T., and Dettinger, M., 2005, Ground-water/surface-water responses to global climate simulations, Santa Clara-Calleguas basin, Ventura County, California, 1950-93: Journal of the American Water Resources Association, v. 41, no. 3, p. 517-536, https://doi.org/10.1111/j.1752-1688.2005.tb03752.x.","productDescription":"20 p. ","startPage":"517","endPage":"536","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":337070,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","county":"Ventura ","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -119.56970214843749,\n 34.397844946449865\n ],\n [\n -118.72924804687499,\n 33.94335994657882\n ],\n [\n -118.30902099609374,\n 34.30260622622907\n ],\n [\n -118.12774658203125,\n 34.56764471968292\n ],\n [\n -117.73223876953124,\n 35.054732099950705\n ],\n [\n -117.68829345703125,\n 35.21196570103912\n ],\n [\n -118.12774658203125,\n 35.44724605551148\n ],\n [\n -118.86383056640625,\n 35.60371874069731\n ],\n [\n -119.42962646484374,\n 35.67514743608467\n ],\n [\n -119.63836669921875,\n 35.632744348010625\n ],\n [\n -119.6905517578125,\n 34.4069096565206\n ],\n [\n -119.56970214843749,\n 34.397844946449865\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"41","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58c1263fe4b014cc3a3d34c0","contributors":{"authors":[{"text":"Hanson, Randall T. 0000-0002-9819-7141 rthanson@usgs.gov","orcid":"https://orcid.org/0000-0002-9819-7141","contributorId":801,"corporation":false,"usgs":true,"family":"Hanson","given":"Randall","email":"rthanson@usgs.gov","middleInitial":"T.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":681283,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dettinger, Michael D. 0000-0002-7509-7332 mddettin@usgs.gov","orcid":"https://orcid.org/0000-0002-7509-7332","contributorId":146383,"corporation":false,"usgs":true,"family":"Dettinger","given":"Michael D.","email":"mddettin@usgs.gov","affiliations":[],"preferred":false,"id":681284,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70603,"text":"wdrOR041 - 2005 - Water resources data for Oregon, water year 2004","interactions":[],"lastModifiedDate":"2012-02-02T00:14:04","indexId":"wdrOR041","displayToPublicDate":"2005-06-01T00:00:00","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":"OR-04-1","title":"Water resources data for Oregon, water year 2004","docAbstract":"The annual Oregon water data report is one of a series of annual reports that document hydrologic data gathered from the U.S. Geological Survey's surface- and ground-water data-collection networks in each State, Puerto Rico, and the Trust Territories. These records of streamflow, ground-water levels, and quality of water provide the hydrologic information needed by State, local, Tribal, and Federal agencies and the private sector for developing and managing our Nation's land and water resources.\r\n\r\nThis report contains water year 2004 data for both surface and ground water, including discharge records for 209 streamflow-gaging stations, 42 partial-record or miscellaneous streamflow stations, and 9 crest-stage partial-record streamflow stations; stage-only records for 6 gaging stations; stage and content records for 15 lakes and reservoirs; water-level records from 12 long-term observation wells; and water-quality records collected at 133 streamflow-gaging stations and 1 atmospheric deposition station.","language":"ENGLISH","doi":"10.3133/wdrOR041","usgsCitation":"Herrett, T.A., Hess, G.W., House, J.G., Ruppert, G.P., and Courts, M., 2005, Water resources data for Oregon, water year 2004: U.S. Geological Survey Water Data Report OR-04-1, 968 p., https://doi.org/10.3133/wdrOR041.","productDescription":"968 p.","costCenters":[],"links":[{"id":192614,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6796,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/2004/wdr-or-04/","linkFileType":{"id":5,"text":"html"}}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629a04","contributors":{"authors":[{"text":"Herrett, Thomas A. herrett@usgs.gov","contributorId":3505,"corporation":false,"usgs":true,"family":"Herrett","given":"Thomas","email":"herrett@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":282710,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hess, Glenn W.","contributorId":33411,"corporation":false,"usgs":true,"family":"Hess","given":"Glenn","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":282711,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"House, Jon G.","contributorId":85266,"corporation":false,"usgs":true,"family":"House","given":"Jon","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":282713,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ruppert, Gregory P.","contributorId":46616,"corporation":false,"usgs":true,"family":"Ruppert","given":"Gregory","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":282712,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Courts, Mary-Lorraine","contributorId":104151,"corporation":false,"usgs":true,"family":"Courts","given":"Mary-Lorraine","email":"","affiliations":[],"preferred":false,"id":282714,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70609,"text":"sir20055071 - 2005 - Water quality, hydrology, and phosphorus loading to Little St. Germain Lake, Wisconsin, with special emphasis on the effects of winter aeration and ground-water inputs","interactions":[],"lastModifiedDate":"2018-02-06T12:31:05","indexId":"sir20055071","displayToPublicDate":"2005-06-01T00:00:00","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":"2005-5071","title":"Water quality, hydrology, and phosphorus loading to Little St. Germain Lake, Wisconsin, with special emphasis on the effects of winter aeration and ground-water inputs","docAbstract":"Little St. Germain Lake is a 978-acre, multibasin lake in Vilas County, Wisconsin. In the interest of protecting and improving the water quality of the lake, the Little St. Germain Lake District initiated several cooperative studies with the U.S. Geological Survey between 1991 and 2004 to (1) document the water quality and the extent of winter anoxia in the lake, (2) evaluate the success of aerators at eliminating winter anoxia, (3) develop water and nutrient budgets for the lake, and (4) assess how the water quality of the lake should respond to changes in phosphorus loading. This report presents the results of these cooperative studies with special emphasis on the water quality in the lake since 2000, including the effects of winter aeration and the importance of ground-water contributions of phosphorus to the productivity of the lake.
\nMeasurements collected during these studies indicate that the water quality in Little St. Germain Lake was consistently different among basins. The West Bay consistently had the best water quality, the South Bay had intermediate water quality, and the East and Upper East Bays consistently had the worst water quality. The water quality in each of the basins was relatively stable from 1991 to 2000; however, since 2001, the West Bay has changed from oligotrophic to mesotrophic, the South Bay has changed from mesotrophic to eutrophic, and the East and Upper East Bays have changed from eutrophic to eutrophic/hypereutrophic.
\nWinter anoxia frequently occurred throughout most of the lake, except in the West Bay and just below the ice in the East Bay. To eliminate winter anoxia, coarse-bubble line aerators were installed and operated in the Upper East, East, and South Bays. The aerators in the Upper East and South Bays were very successful at eliminating winter anoxia; however, the aerator in the East Bay had little impact on the dissolved oxygen concentrations throughout its basin.
\nDetailed water and phosphorus budgets computed for the lake indicated that inflow from Muskellunge Creek was the major source of phosphorus to the lake and that ground water was the secondary source. Results from a detailed ground-water-flow model indicated that ground water flows into the lake from all sides, except the south sides of the West and Second South Bays. Most of the phosphorus appears to come from natural sources, such as ground water and surface water flowing through relatively undeveloped areas surrounding Little St. Germain Lake and Muskellunge Lake.
\nSeveral empirical water-quality models were used to simulate how the East and Upper East Bays of the lake should respond to reductions in phosphorus loading from Muskellunge Creek. Simulation results indicated that reductions in tributary loading could improve the water quality of the East and Upper East Bays. Improving the water quality of these bays would also improve the water quality of the South and Second South Bays because of the flow of water through the lake. However, even with phosphorus loading from Muskellunge Creek completely eliminated, most of the lake would remain borderline mesotrophic/eutrophic because of the contributions of phosphorus from ground water.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055071","collaboration":"In cooperation with the Little St. Germain Lake District","usgsCitation":"Robertson, D.M., Rose, W., and Saad, D.A., 2005, Water quality, hydrology, and phosphorus loading to Little St. Germain Lake, Wisconsin, with special emphasis on the effects of winter aeration and ground-water inputs: U.S. Geological Survey Scientific Investigations Report 2005-5071, viii, 36 p., https://doi.org/10.3133/sir20055071.","productDescription":"viii, 36 p.","numberOfPages":"46","onlineOnly":"N","additionalOnlineFiles":"Y","temporalStart":"1991-04-01","temporalEnd":"2004-03-31","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":192773,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6799,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5071/","linkFileType":{"id":5,"text":"html"}},{"id":311328,"rank":101,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5071/pdf/SIR_2005-5071.pdf"}],"scale":"100000","country":"United States","state":"Wisconsin","county":"Vilas County","otherGeospatial":"Littel St. Germain Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -89.50561523437499,\n 45.89550409759517\n ],\n [\n -89.50561523437499,\n 45.94064578150488\n ],\n [\n -89.38133239746092,\n 45.94064578150488\n ],\n [\n -89.38133239746092,\n 45.89550409759517\n ],\n [\n -89.50561523437499,\n 45.89550409759517\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd357","contributors":{"authors":[{"text":"Robertson, Dale M. 0000-0001-6799-0596 dzrobert@usgs.gov","orcid":"https://orcid.org/0000-0001-6799-0596","contributorId":150760,"corporation":false,"usgs":true,"family":"Robertson","given":"Dale","email":"dzrobert@usgs.gov","middleInitial":"M.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282719,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rose, William J. wjrose@usgs.gov","contributorId":2182,"corporation":false,"usgs":true,"family":"Rose","given":"William J.","email":"wjrose@usgs.gov","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":282721,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Saad, David A. dasaad@usgs.gov","contributorId":121,"corporation":false,"usgs":true,"family":"Saad","given":"David","email":"dasaad@usgs.gov","middleInitial":"A.","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282720,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70611,"text":"fs20053044 - 2005 - Acoustic doppler velocity monitoring within Main Spring, Barton Springs, Austin, Texas, April-September 2004-enhancing the accuracy of springflow data","interactions":[],"lastModifiedDate":"2017-05-30T10:58:55","indexId":"fs20053044","displayToPublicDate":"2005-06-01T00:00:00","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":"2005-3044","title":"Acoustic doppler velocity monitoring within Main Spring, Barton Springs, Austin, Texas, April-September 2004-enhancing the accuracy of springflow data","docAbstract":"Acoustic Doppler velocity (ADV) meters are sophisticated underwater monitoring instruments that use sound waves to measure water velocity in as many as three directions. In April 2004, an ADV meter was installed inside the principal orifice and discharge point of Main Spring at Barton Springs in Austin, Texas. This instrument collects velocity data that can be used to enhance the accuracy of springflow data and identify previously unrecognized hydrologic patterns.
An accurate record of springflow at Barton Springs is important for several reasons. First, Barton Springs is the only known habitat for the Barton Springs salamander (Eurycea sosorum), a federally-listed endangered species that is dependent on reliable springflow to survive. Determination of sustainable Edwards aquifer yields compatible with the survival of the species is impossible without an accurate springflow record. Second, the 3-acre swimming pool fed by Barton Springs is enjoyed by about 340,000 people per year (2003) and is an important tourist attraction. Third, Barton Springs provides a part of Austin's municipal water supply; water from Barton Springs discharges into Town Lake on the Colorado River about 0.4 mile upstream from one of Austin's three water-supply plants. Fourth, flow in Barton Springs reflects water levels in the Barton Springs segment of the Edwards aquifer, which currently (2005) is designated a sole-source aquifer by the U.S. Environmental Protection Agency.
This report, prepared by the U.S. Geological Survey, briefly summarizes the results of recent ADV-based velocity and springflow data acquisition at Barton Springs and describes an application of velocity monitoring to enhance the accuracy of springflow data.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs20053044","usgsCitation":"Asquith, W., and Gary, M., 2005, Acoustic doppler velocity monitoring within Main Spring, Barton Springs, Austin, Texas, April-September 2004-enhancing the accuracy of springflow data: U.S. Geological Survey Fact Sheet 2005-3044, 4 p., https://doi.org/10.3133/fs20053044.","productDescription":"4 p.","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":121071,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3044.bmp"},{"id":341828,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2005/3044/pdf/FS_2005-3044.pdf","text":"Report","size":"2.14 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":6801,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/fs2005-3044/","linkFileType":{"id":5,"text":"html"}}],"scale":"100000","country":"United States","state":"Texas","city":"Austin","otherGeospatial":"Barton Springs","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -97.78514385223389,\n 30.259030134829775\n ],\n [\n -97.7625274658203,\n 30.259030134829775\n ],\n [\n -97.7625274658203,\n 30.2678890804847\n ],\n [\n -97.78514385223389,\n 30.2678890804847\n ],\n [\n -97.78514385223389,\n 30.259030134829775\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a2b5","contributors":{"authors":[{"text":"Asquith, W.H.","contributorId":87980,"corporation":false,"usgs":true,"family":"Asquith","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":282726,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gary, M.O.","contributorId":12917,"corporation":false,"usgs":true,"family":"Gary","given":"M.O.","email":"","affiliations":[],"preferred":false,"id":282725,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70610,"text":"sir20055061 - 2005 - External quality-assurance results for the National Atmospheric Deposition Program/National Trends Network, 2002-03","interactions":[],"lastModifiedDate":"2012-02-02T00:14:00","indexId":"sir20055061","displayToPublicDate":"2005-06-01T00:00:00","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":"2005-5061","title":"External quality-assurance results for the National Atmospheric Deposition Program/National Trends Network, 2002-03","docAbstract":"Six external quality-assurance programs were operated by the U.S. Geological Survey (USGS) External Quality-Assurance (QA) Project for the National Atmospheric Deposition Program/National Trends Network (NADP/NTN) from 2002 through 2003. Each program measured specific components of the overall error inherent in NADP/NTN wet-deposition measurements.\r\n\r\nThe intersite-comparison program assessed the variability and bias of pH and specific conductance determinations made by NADP/NTN site operators twice per year with respect to accuracy goals. The percentage of site operators that met the pH accuracy goals decreased from 92.0 percent in spring 2002 to 86.3 percent in spring 2003. In these same four intersite-comparison studies, the percentage of site operators that met the accuracy goals for specific conductance ranged from 94.4 to 97.5 percent.\r\n\r\nThe blind-audit program and the sample-handling evaluation (SHE) program evaluated the effects of routine sample handling, processing, and shipping on the chemistry of weekly NADP/NTN samples. The blind-audit program data indicated that the variability introduced by sample handling might be environmentally significant to data users for sodium, potassium, chloride, and hydrogen ion concentrations during 2002. In 2003, the blind-audit program was modified and replaced by the SHE program. The SHE program was designed to control the effects of laboratory-analysis variability. The 2003 SHE data had less overall variability than the 2002 blind-audit data. The SHE data indicated that sample handling buffers the pH of the precipitation samples and, in turn, results in slightly lower conductivity. Otherwise, the SHE data provided error estimates that were not environmentally significant to data users.\r\n\r\nThe field-audit program was designed to evaluate the effects of onsite exposure, sample handling, and shipping on the chemistry of NADP/NTN precipitation samples. Field-audit results indicated that exposure of NADP/NTN wet-deposition samples to onsite conditions tended to neutralize the acidity of the samples by less than 1.0 microequivalent per liter. Onsite exposure of the sampling bucket appeared to slightly increase the concentration of most of the analytes but not to an extent that was environmentally significant to NADP data users.\r\n\r\nAn interlaboratory-comparison program was used to estimate the analytical variability and bias of the NADP Central Analytical Laboratory (CAL) during 2002-03. Bias was identified in the CAL data for calcium, magnesium, sodium, potassium, ammonium, chloride, nitrate, sulfate, hydrogen ion, and specific conductance, but the absolute value of the bias was less than analytical minimum detection limits for all constituents except magnesium, nitrate, sulfate, and specific conductance. Control charts showed that CAL results were within statistical control approximately 90 percent of the time. Data for the analysis of ultrapure deionized-water samples indicated that CAL did not have problems with laboratory contamination.\r\n\r\nDuring 2002-03, the overall variability of data from the NADP/NTN precipitation-monitoring system was estimated using data from three collocated monitoring sites. Measurement differences of constituent concentration and deposition for paired samples from the collocated samplers were evaluated to compute error terms. The medians of the absolute percentage errors (MAEs) for the paired samples generally were larger for cations (approximately 8 to 50 percent) than for anions (approximately 3 to 33 percent). MAEs were approximately 16 to 30 percent for hydrogen-ion concentration, less than 10 percent for specific conductance, less than 5 percent for sample volume, and less than 8 percent for precipitation depth.\r\nThe variability attributed to each component of the sample-collection and analysis processes, as estimated by USGS quality-assurance programs, varied among analytes. Laboratory analysis variability accounted for approximately 2 percent of the","language":"ENGLISH","doi":"10.3133/sir20055061","usgsCitation":"Wetherbee, G.A., Latysh, N.E., and Burke, K.P., 2005, External quality-assurance results for the National Atmospheric Deposition Program/National Trends Network, 2002-03 (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5061, 69 p., https://doi.org/10.3133/sir20055061.","productDescription":"69 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":6800,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir20055061/","linkFileType":{"id":5,"text":"html"}},{"id":192774,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"100000","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e65ff","contributors":{"authors":[{"text":"Wetherbee, Gregory A. 0000-0002-6720-2294 wetherbe@usgs.gov","orcid":"https://orcid.org/0000-0002-6720-2294","contributorId":1044,"corporation":false,"usgs":true,"family":"Wetherbee","given":"Gregory","email":"wetherbe@usgs.gov","middleInitial":"A.","affiliations":[{"id":143,"text":"Branch of Quality Systems","active":true,"usgs":true}],"preferred":true,"id":282722,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Latysh, Natalie E.","contributorId":39860,"corporation":false,"usgs":true,"family":"Latysh","given":"Natalie","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":282723,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Burke, Kevin P.","contributorId":101333,"corporation":false,"usgs":true,"family":"Burke","given":"Kevin","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":282724,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70604,"text":"ofr20041387 - 2005 - Ground-water/surface-water relations along Honey Creek, Washtenaw County, Michigan, 2003","interactions":[],"lastModifiedDate":"2016-10-06T12:08:32","indexId":"ofr20041387","displayToPublicDate":"2005-06-01T00:00:00","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":"2004-1387","title":"Ground-water/surface-water relations along Honey Creek, Washtenaw County, Michigan, 2003","docAbstract":"The U.S. Geological Survey (USGS), in cooperation with the city of Ann Arbor, Mich., investigated the ground-water/ surface-water relations along the lower reaches of Honey Creek, Washtenaw County, Mich., and an unnamed tributary to Honey Creek (the discharge tributary) from June through October 2003. Streamflow in these reaches was artificially high during a naturally low-flow period due to an anthropogenic discharge. Ground-water/surface-water relations were examined by seepage runs (series of streamflow measurements for the computation of streams gains or losses) and measurements of the difference in head between the stream surface and shallow aquifer. Specific conductance and water-temperature measurements were used as ancillary data to help identify gaining and losing reaches. Three seepage runs and four runs in which hydraulic-head differences between the stream and shallow aquifer were measured (piezometer runs) were made during periods of base flow.
Streamflow measurements were made at 18 sites for the seepage runs. Instream piezometers were installed at 16 sites and bank piezometers were installed at 2 sites. Two deeper instream piezometers were installed at site 13 on September 4, 2003 to collect additional data on the ground-water/surface-water relations at that site.
The seepage runs indicate that the main stem of Honey Creek and the discharge tributary in the study area are overall gaining reaches. The seepage runs also indicate that smaller reaches of Honey Creek and the discharge tributary may be losing reaches and that this relation may change over time with changing hydraulic conditions. The piezometer-run measurements support the seepage-run results on the main stem, whereas piezometer-run measurements both support and conflict with seepage-run measurements on the discharge tributary. Seepage runs give an average for the reach, whereas piezometer head-difference measurements are for a specific area around the piezometer. Data that may appear to be conflicting actually may be showing that within a gaining reach there are localized areas that lose streamflow.
The overall gain in streamflow along with specific measurements of head differences, specific conductance, and water temperature indicate that ground water is discharging to Honey Creek and the discharge tributary. Although reaches and areas that lose streamflow have been identified, data collected during this study cannot confirm or disprove that the loss is to the regional ground-water system.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20041387","collaboration":"Prepared in cooperation with the city of Ann Arbor, Michigan","usgsCitation":"Healy, D.F., 2005, Ground-water/surface-water relations along Honey Creek, Washtenaw County, Michigan, 2003: U.S. Geological Survey Open-File Report 2004-1387, iv, 17 p., https://doi.org/10.3133/ofr20041387.","productDescription":"iv, 17 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":192615,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6797,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr2004-1387/","linkFileType":{"id":5,"text":"html"}}],"scale":"100000","country":"United States","state":"Michigan","county":"Washtenaw County","otherGeospatial":"Honey Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -83.858333,\n 42.333333\n ],\n [\n -83.858333,\n 42.25\n ],\n [\n -83.775,\n 42.25\n ],\n [\n -83.775,\n 42.333333\n ],\n [\n -83.858333,\n 42.333333\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a95e4b07f02db659ffd","contributors":{"authors":[{"text":"Healy, Denis F.","contributorId":46514,"corporation":false,"usgs":true,"family":"Healy","given":"Denis","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":282715,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70623,"text":"fs20043067 - 2005 - Ground-water vulnerability to nitrate contamination in the mid-atlantic region","interactions":[],"lastModifiedDate":"2012-02-02T00:14:03","indexId":"fs20043067","displayToPublicDate":"2005-06-01T00:00:00","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":"2004-3067","title":"Ground-water vulnerability to nitrate contamination in the mid-atlantic region","docAbstract":"The U.S. Environmental Protection Agency?s (USEPA) Regional Vulnerability Assessment (ReVA) Program has developed a set of statistical tools to support regional-scale, integrated ecological risk-assessment studies. One of these tools, developed by the U.S. Geological Survey (USGS), is used with available water-quality data obtained from USGS National Water-Quality Assessment (NAWQA) and other studies in association with land cover, geology, soils, and other geographic data to develop logistic-regression equations that predict the vulnerability of ground water to nitrate concentrations exceeding specified thresholds in the Mid-Atlantic Region. The models were developed and applied to produce spatial probability maps showing the likelihood of elevated concentrations of nitrate in the region. These maps can be used to identify areas that currently are at risk and help identify areas where ground water has been affected by human activities. This information can be used by regional and local water managers to protect water supplies and identify land-use planning solutions and monitoring programs in these vulnerable areas.","language":"ENGLISH","doi":"10.3133/fs20043067","usgsCitation":"Greene, E.A., LaMotte, A.E., Cullinan, K., and Smith, E.R., 2005, Ground-water vulnerability to nitrate contamination in the mid-atlantic region: U.S. Geological Survey Fact Sheet 2004-3067, 4 p., https://doi.org/10.3133/fs20043067.","productDescription":"4 p.","costCenters":[],"links":[{"id":6805,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://md.water.usgs.gov/publications/fs-2004-3067/html/","linkFileType":{"id":5,"text":"html"}},{"id":125084,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2004/3067/report-thumb.jpg"},{"id":90526,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2004/3067/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db65556b","contributors":{"authors":[{"text":"Greene, Earl A. 0000-0002-9479-0829 eagreene@usgs.gov","orcid":"https://orcid.org/0000-0002-9479-0829","contributorId":3518,"corporation":false,"usgs":true,"family":"Greene","given":"Earl","email":"eagreene@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":282734,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LaMotte, Andrew E. 0000-0002-1434-6518 alamotte@usgs.gov","orcid":"https://orcid.org/0000-0002-1434-6518","contributorId":2842,"corporation":false,"usgs":true,"family":"LaMotte","given":"Andrew","email":"alamotte@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282733,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cullinan, Kerri-Ann","contributorId":90821,"corporation":false,"usgs":true,"family":"Cullinan","given":"Kerri-Ann","email":"","affiliations":[],"preferred":false,"id":282736,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, Elizabeth R.","contributorId":76023,"corporation":false,"usgs":true,"family":"Smith","given":"Elizabeth","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":282735,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70205404,"text":"70205404 - 2005 - Can nitrogen sequestration explain the unexpected nitrate decline in New Hampshire streams?","interactions":[],"lastModifiedDate":"2019-09-17T12:03:02","indexId":"70205404","displayToPublicDate":"2005-05-31T11:59:17","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1478,"text":"Ecosystems","active":true,"publicationSubtype":{"id":10}},"title":"Can nitrogen sequestration explain the unexpected nitrate decline in New Hampshire streams?","docAbstract":"No abstract available
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Hampshire\",\"nation\":\"USA \"}}]}","volume":"8","issue":"3","noUsgsAuthors":false,"publicationDate":"2005-05-31","publicationStatus":"PW","contributors":{"authors":[{"text":"Huntington, Thomas G. 0000-0002-9427-3530 thunting@usgs.gov","orcid":"https://orcid.org/0000-0002-9427-3530","contributorId":1884,"corporation":false,"usgs":true,"family":"Huntington","given":"Thomas","email":"thunting@usgs.gov","middleInitial":"G.","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":771061,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70596,"text":"sir20055074 - 2005 - Generalized water-level contours, September-October 2000 and March-April 2001, and long-term water-level changes, at the U.S. Air Force Plant 42 and vicinity, Palmdale, California","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"sir20055074","displayToPublicDate":"2005-05-31T00:00:00","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":"2005-5074","title":"Generalized water-level contours, September-October 2000 and March-April 2001, and long-term water-level changes, at the U.S. Air Force Plant 42 and vicinity, Palmdale, California","docAbstract":"Historically, the U.S. Air Force Plant 42 has relied on ground water as the primary source of water owing, in large part, to the scarcity of surface water in the region. Groundwater withdrawal for municipal, industrial, and agricultural use has affected ground-water levels at U.S. Air Force Plant 42, and vicinity. A study to document changes in groundwater gradients and to present historical water-level data was completed by the U.S. Geological Survey in cooperation with the U.S. Air Force. This report presents historical water-level data, hydrographs, and generalized seasonal water-level and water-level contours for September?October 2000 and March?April 2001. The collection and interpretation of ground-water data helps local water districts, military bases, and private citizens gain a better understanding of the ground-water flow systems, and consequently water availability.\r\n\r\n During September?October 2000 and March?April 2001 the U.S. Geological Survey and other agencies made a total of 102 water-level measurements, 46 during September?October 2000 and 56 during March?April 2001. These data document recent conditions and, when compared with historical data, document changes in ground-water levels. Two water-level contour maps were drawn: the first depicts water-level conditions for September?October 2000 map and the second depicts water-level conditions for March?April 2001 map. In general, the water-level contour maps show water-level depressions formed as result of ground-water withdrawal. One hundred sixteen long-term hydrographs, using water-level data from 1915 through 2000, were constructed to show water-level trends in the area. The hydrographs indicate that water-level decline occurred throughout the study area, with the greatest declines south of U.S. Air Force Plant 42.","language":"ENGLISH","doi":"10.3133/sir20055074","usgsCitation":"Christensen, A.H., 2005, Generalized water-level contours, September-October 2000 and March-April 2001, and long-term water-level changes, at the U.S. Air Force Plant 42 and vicinity, Palmdale, California: U.S. Geological Survey Scientific Investigations Report 2005-5074, 131 p., https://doi.org/10.3133/sir20055074.","productDescription":"131 p.","costCenters":[],"links":[{"id":6893,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir20055074/","linkFileType":{"id":5,"text":"html"}},{"id":185922,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aec16","contributors":{"authors":[{"text":"Christensen, Allen H. 0000-0002-7061-5591 ahchrist@usgs.gov","orcid":"https://orcid.org/0000-0002-7061-5591","contributorId":1510,"corporation":false,"usgs":true,"family":"Christensen","given":"Allen","email":"ahchrist@usgs.gov","middleInitial":"H.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282694,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70597,"text":"fs20053041 - 2005 - South Carolina coastal erosion study","interactions":[],"lastModifiedDate":"2016-12-07T08:43:27","indexId":"fs20053041","displayToPublicDate":"2005-05-31T00:00:00","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":"2005-3041","title":"South Carolina coastal erosion study","language":"ENGLISH","doi":"10.3133/fs20053041","usgsCitation":"Denny, J.F., Baldwin, W.E., Schwab, W.C., Warner, J., and DeVoe, M.R., 2005, South Carolina coastal erosion study: U.S. Geological Survey Fact Sheet 2005-3041, 4 p., https://doi.org/10.3133/fs20053041.","productDescription":"4 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":122457,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3041.bmp"},{"id":6894,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3041/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"South Carolina","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.84677124023438,\n 33.89435731090067\n ],\n [\n -82.72705078125,\n 33.28691595686207\n ],\n [\n -82.13104248046875,\n 32.76649095995108\n ],\n [\n -81.18072509765625,\n 33.5093393678006\n ],\n [\n -81.84677124023438,\n 33.89435731090067\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -78.62777709960938,\n 33.91715274008259\n ],\n [\n -78.519287109375,\n 33.82137099133305\n ],\n [\n -78.63876342773438,\n 33.78827853625996\n ],\n [\n -78.71429443359375,\n 33.755173286674825\n ],\n [\n -78.80630493164062,\n 33.69578012931697\n ],\n [\n -78.8543701171875,\n 33.6477787401531\n ],\n [\n -78.92166137695312,\n 33.58945533558725\n ],\n [\n -78.96697998046875,\n 33.50475906922609\n ],\n [\n -79.00405883789061,\n 33.42914915719729\n ],\n [\n -79.0576171875,\n 33.31905344502012\n ],\n [\n -79.07135009765625,\n 33.23639027157906\n ],\n [\n -79.08096313476562,\n 33.169743600216165\n ],\n [\n -79.07958984375,\n 33.10534697199519\n ],\n [\n -79.38720703125,\n 33.151349385342506\n ],\n [\n -79.35150146484375,\n 33.33167564632156\n ],\n [\n -79.31854248046875,\n 33.39590576922804\n ],\n [\n -79.25125122070312,\n 33.527658137677335\n ],\n [\n -79.14138793945312,\n 33.66492516885242\n ],\n [\n -79.0411376953125,\n 33.75288969455201\n ],\n [\n -78.93539428710938,\n 33.831638461142866\n ],\n [\n -78.8104248046875,\n 33.895497227123876\n ],\n [\n -78.7060546875,\n 33.92285064485909\n ],\n [\n -78.64974975585938,\n 33.95133445208438\n ],\n [\n -78.62777709960938,\n 33.91715274008259\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e752f","contributors":{"authors":[{"text":"Denny, Jane F. 0000-0002-3472-618X jdenny@usgs.gov","orcid":"https://orcid.org/0000-0002-3472-618X","contributorId":418,"corporation":false,"usgs":true,"family":"Denny","given":"Jane","email":"jdenny@usgs.gov","middleInitial":"F.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":282696,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baldwin, Wayne E. 0000-0001-5886-0917 wbaldwin@usgs.gov","orcid":"https://orcid.org/0000-0001-5886-0917","contributorId":1321,"corporation":false,"usgs":true,"family":"Baldwin","given":"Wayne","email":"wbaldwin@usgs.gov","middleInitial":"E.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":282697,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schwab, William C. 0000-0001-9274-5154 bschwab@usgs.gov","orcid":"https://orcid.org/0000-0001-9274-5154","contributorId":417,"corporation":false,"usgs":true,"family":"Schwab","given":"William","email":"bschwab@usgs.gov","middleInitial":"C.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":282695,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Warner, John C. 0000-0002-3734-8903 jcwarner@usgs.gov","orcid":"https://orcid.org/0000-0002-3734-8903","contributorId":2681,"corporation":false,"usgs":true,"family":"Warner","given":"John C.","email":"jcwarner@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":282698,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"DeVoe, M. Richard","contributorId":53887,"corporation":false,"usgs":true,"family":"DeVoe","given":"M.","email":"","middleInitial":"Richard","affiliations":[],"preferred":false,"id":282699,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70595,"text":"sir20055090 - 2005 - Inventory of ground-water resources in the Kabul Basin, Afghanistan","interactions":[],"lastModifiedDate":"2021-09-28T15:59:10.570019","indexId":"sir20055090","displayToPublicDate":"2005-05-31T00:00:00","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":"2005-5090","title":"Inventory of ground-water resources in the Kabul Basin, Afghanistan","docAbstract":"In 2004, the U.S. Geological Survey began working with engineers at the Afghanistan Geological Survey to provide hydrologic training and equipment and to apply these tools to build an inventory of water wells in the Kabul Basin of Afghanistan. An inventory of 148 wells now includes information on well location, depth, and access. Water-level and water-quality measurements have been made at most of these wells. A water-level elevation map has been constructed, and general directions of ground-water flow have been defined.\r\n\r\nGround-water flow in the Kabul Basin is primarily through saturated alluvium and other basin-fill sediments. The water-table surface generally mirrors topography, and ground water generally flows in the directions of surface-water discharge. The quality of ground water in the Kabul Basin varies widely. In some areas, ground-water quality is excellent, with low concentrations of dissolved solids and no problematic constituents. In other areas, however, high concentrations of dissolved solids and the presence of some constituents at concentrations deemed harmful to humans and crops render untreated ground water marginal or unsuitable for public supply and/or agricultural use. Of particular concern are elevated concentrations of nitrate, boron, and dissolved solids, and an indication of fecal pollution in some parts of the basin.\r\n\r\nAs Afghanistan emerges from years of conflict, as institutional capacities rejuvenate and grow, and as the need for wise water-management decisions continues, adequate data and a fuller understanding of the ground-water resource in the Kabul Basin will be imperative. The work described in this report represents only a modest beginning in what will be a long-term data-collection and interpretive effort.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055090","usgsCitation":"Broshears, R.E., Chornack, M.P., Mueller, D.K., and Ruddy, B.C., 2005, Inventory of ground-water resources in the Kabul Basin, Afghanistan: U.S. Geological Survey Scientific Investigations Report 2005-5090, 44 p., https://doi.org/10.3133/sir20055090.","productDescription":"44 p.","costCenters":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"links":[{"id":6892,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5090/","linkFileType":{"id":5,"text":"html"}},{"id":185921,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","country":"Afghanistan","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[61.21082,35.65007],[62.23065,35.27066],[62.98466,35.40404],[63.19354,35.85717],[63.9829,36.00796],[64.54648,36.31207],[64.74611,37.11182],[65.58895,37.30522],[65.74563,37.66116],[66.21738,37.39379],[66.51861,37.36278],[67.07578,37.35614],[67.83,37.14499],[68.13556,37.02312],[68.85945,37.34434],[69.19627,37.15114],[69.51879,37.609],[70.11658,37.58822],[70.27057,37.73516],[70.3763,38.1384],[70.80682,38.48628],[71.34813,38.25891],[71.2394,37.95327],[71.54192,37.90577],[71.44869,37.06564],[71.84464,36.73817],[72.19304,36.94829],[72.63689,37.04756],[73.26006,37.49526],[73.9487,37.42157],[74.98,37.41999],[75.15803,37.13303],[74.57589,37.02084],[74.06755,36.83618],[72.92002,36.72001],[71.84629,36.50994],[71.26235,36.07439],[71.49877,35.65056],[71.61308,35.1532],[71.11502,34.73313],[71.15677,34.34891],[70.8818,33.98886],[69.93054,34.02012],[70.32359,33.35853],[69.68715,33.1055],[69.26252,32.50194],[69.31776,31.90141],[68.92668,31.62019],[68.55693,31.71331],[67.79269,31.58293],[67.68339,31.30315],[66.93889,31.30491],[66.38146,30.7389],[66.34647,29.88794],[65.04686,29.47218],[64.35042,29.56003],[64.148,29.34082],[63.55026,29.46833],[62.54986,29.31857],[60.87425,29.82924],[61.78122,30.73585],[61.69931,31.37951],[60.94194,31.54807],[60.86365,32.18292],[60.53608,32.98127],[60.9637,33.52883],[60.52843,33.67645],[60.80319,34.4041],[61.21082,35.65007]]]},\"properties\":{\"name\":\"Afghanistan\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e479de4b07f02db491c7c","contributors":{"authors":[{"text":"Broshears, Robert E.","contributorId":40675,"corporation":false,"usgs":true,"family":"Broshears","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":282692,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chornack, Michael P. mpchorna@usgs.gov","contributorId":2431,"corporation":false,"usgs":true,"family":"Chornack","given":"Michael","email":"mpchorna@usgs.gov","middleInitial":"P.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":282690,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mueller, David K. mueller@usgs.gov","contributorId":1585,"corporation":false,"usgs":true,"family":"Mueller","given":"David","email":"mueller@usgs.gov","middleInitial":"K.","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true}],"preferred":true,"id":282689,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ruddy, Barbara C. bcruddy@usgs.gov","contributorId":4163,"corporation":false,"usgs":true,"family":"Ruddy","given":"Barbara","email":"bcruddy@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":282691,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70598,"text":"wdrNJ041 - 2005 - Water resources data, New Jersey, water year 2004-volume 1. surface-water data","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"wdrNJ041","displayToPublicDate":"2005-05-31T00:00:00","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":"NJ-04-1","title":"Water resources data, New Jersey, water year 2004-volume 1. surface-water data","docAbstract":"Water-resources data for the 2004 water year for New Jersey are presented in three volumes, and consists of records of stage, discharge, and water-quality of streams; stage and contents of lakes and reservoirs; and water levels and water-quality of ground water. Volume 1 contains discharge records for 105 gaging stations; tide summaries at 27 tidal gaging stations; stage and contents at 39 lakes and reservoirs; and diversions from 51 surface-water sources. Also included are stage and discharge for 108 crest-stage partial-record stations, stage-only at 34 tidal crest-stage gages, and discharge for 124 low-flow partial-record stations. Locations of these sites are shown in figures 8-11. Additional discharge measurements were made at 131 miscellaneous sites that are not part of the systematic data-collection program. Discontinued station tables for gaging stations, crest-stage gages, tidal crest-stage and tidal gaging stations show historical coverage. The data in this report represent that part of the National Water Information System (NWIS) data collected by the United States Geological Survey (USGS). Hydrologic conditions are also described for this water year, including stream-flow, precipitation, reservoir conditions, and air temperatures.","language":"ENGLISH","doi":"10.3133/wdrNJ041","usgsCitation":"Centinaro, G., White, B., Hoppe, H., Dudek, J., Protz, A., Reed, T., Shvanda, J., and Watson, A., 2005, Water resources data, New Jersey, water year 2004-volume 1. surface-water data: U.S. Geological Survey Water Data Report NJ-04-1, 412 p., https://doi.org/10.3133/wdrNJ041.","productDescription":"412 p.","costCenters":[],"links":[{"id":6895,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdrnj041/","linkFileType":{"id":5,"text":"html"}},{"id":185990,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0f60","contributors":{"authors":[{"text":"Centinaro, G.L.","contributorId":61892,"corporation":false,"usgs":true,"family":"Centinaro","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":282705,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, B.T.","contributorId":9710,"corporation":false,"usgs":true,"family":"White","given":"B.T.","email":"","affiliations":[],"preferred":false,"id":282700,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hoppe, H.L.","contributorId":36994,"corporation":false,"usgs":true,"family":"Hoppe","given":"H.L.","email":"","affiliations":[],"preferred":false,"id":282704,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dudek, J.F.","contributorId":31818,"corporation":false,"usgs":true,"family":"Dudek","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":282702,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Protz, A.R.","contributorId":97976,"corporation":false,"usgs":true,"family":"Protz","given":"A.R.","affiliations":[],"preferred":false,"id":282707,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Reed, T.J. 0000-0002-9943-4081","orcid":"https://orcid.org/0000-0002-9943-4081","contributorId":15224,"corporation":false,"usgs":true,"family":"Reed","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":282701,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Shvanda, J.C.","contributorId":34999,"corporation":false,"usgs":true,"family":"Shvanda","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":282703,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Watson, A.F.","contributorId":85653,"corporation":false,"usgs":true,"family":"Watson","given":"A.F.","email":"","affiliations":[],"preferred":false,"id":282706,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":70589,"text":"fs20053046 - 2005 - USGS California Water Science Center water programs in California","interactions":[],"lastModifiedDate":"2016-08-17T14:17:51","indexId":"fs20053046","displayToPublicDate":"2005-05-26T00:00:00","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":"2005-3046","title":"USGS California Water Science Center water programs in California","docAbstract":"California is threatened by many natural hazards—fire, floods, landslides, earthquakes. The State is also threatened by longer-term problems, such as hydrologic effects of climate change, and human-induced problems, such as overuse of ground water and degradation of water quality. The threats and problems are intensified by increases in population, which has risen to nearly 36.8 million. For the USGS California Water Science Center, providing scientific information to help address hazards, threats, and hydrologic issues is a top priority. To meet the demands of a growing California, USGS scientific investigations are helping State and local governments improve emergency management, optimize resources, collect contaminant-source and -mobility information, and improve surface- and ground-water quality. USGS hydrologic studies and data collection throughout the State give water managers quantifiable and detailed scientific information that can be used to plan for development and to protect and more efficiently manage resources. The USGS, in cooperation with state, local, and tribal agencies, operates more than 500 instrument stations, which monitor streamflow, ground-water levels, and surface- and ground-water constituents to help protect water supplies and predict the threats of natural hazards. The following are some of the programs implemented by the USGS, in cooperation with other agencies, to obtain and analyze information needed to preserve California's environment and resources.
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\"}}]}","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611954","contributors":{"authors":[{"text":"Shulters, Michael V. shulters@usgs.gov","contributorId":1023,"corporation":false,"usgs":true,"family":"Shulters","given":"Michael","email":"shulters@usgs.gov","middleInitial":"V.","affiliations":[{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"preferred":true,"id":282687,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70590,"text":"sir20055092 - 2005 - Historic and naturalized monthly streamflow for selected sites in the Red River of the North Basin in North Dakota, Minnesota, and South Dakota, 1931-2001","interactions":[],"lastModifiedDate":"2018-03-05T16:09:32","indexId":"sir20055092","displayToPublicDate":"2005-05-26T00:00:00","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":"2005-5092","title":"Historic and naturalized monthly streamflow for selected sites in the Red River of the North Basin in North Dakota, Minnesota, and South Dakota, 1931-2001","docAbstract":"Historic monthly streamflow data were compiled and missing historic and naturalized monthly streamflow data were estimated to develop a database of updated streamflow data for January 1931 through December 2001 (the data-development period) for 35 sites in the Red River of the North Basin. Of the 35 sites, 4 had gaged historic monthly streamflow data for the entire data-development period, 10 had gaged historic monthly streamflow data for part of the data-development period, and 21 had no gaged historic monthly streamflow data. To develop the database, a modified drainage-area ratio method, a maintenance of variance extension type 1 method, and a water-balance method were used to estimate the missing historic monthly streamflow data. Naturalized streamflow for the 35 sites was estimated by eliminating the hydrologic effects of Orwell Dam, Reservation Dam, White Rock Dam, Baldhill Dam, surfacewater withdrawals, and return flows.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055092","usgsCitation":"Emerson, D.G., 2005, Historic and naturalized monthly streamflow for selected sites in the Red River of the North Basin in North Dakota, Minnesota, and South Dakota, 1931-2001 (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5092, vi, 228 p., https://doi.org/10.3133/sir20055092.","productDescription":"vi, 228 p.","numberOfPages":"235","onlineOnly":"Y","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":185832,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6891,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5092/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -100.1,45.96666666666667 ], [ -100.1,49 ], [ -94.43333333333334,49 ], [ -94.43333333333334,45.96666666666667 ], [ -100.1,45.96666666666667 ] ] ] } } ] }","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db691287","contributors":{"authors":[{"text":"Emerson, Douglas G.","contributorId":40579,"corporation":false,"usgs":true,"family":"Emerson","given":"Douglas","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":282688,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70585,"text":"fs20053065 - 2005 - USGS California Water Science Center Streamgage Program","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"fs20053065","displayToPublicDate":"2005-05-25T00:00:00","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":"2005-3065","title":"USGS California Water Science Center Streamgage Program","language":"ENGLISH","doi":"10.3133/fs20053065","usgsCitation":"Shulters, M.V., 2005, USGS California Water Science Center Streamgage Program (Online only): U.S. Geological Survey Fact Sheet 2005-3065, 2 p., https://doi.org/10.3133/fs20053065.","productDescription":"2 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":6889,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/fs2005-3065/","linkFileType":{"id":5,"text":"html"}},{"id":121167,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3065.jpg"}],"scale":"24000","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611a81","contributors":{"authors":[{"text":"Shulters, Michael V. shulters@usgs.gov","contributorId":1023,"corporation":false,"usgs":true,"family":"Shulters","given":"Michael","email":"shulters@usgs.gov","middleInitial":"V.","affiliations":[{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"preferred":true,"id":282686,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70584,"text":"sir20055095 - 2005 - Water quality of streams in the Red River of the North Basin, Minnesota, North Dakota, and South Dakota, 1970-2001","interactions":[],"lastModifiedDate":"2018-03-16T13:36:05","indexId":"sir20055095","displayToPublicDate":"2005-05-25T00:00:00","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":"2005-5095","title":"Water quality of streams in the Red River of the North Basin, Minnesota, North Dakota, and South Dakota, 1970-2001","docAbstract":"Data for the Red River of the North (Red River) Basin in Minnesota, North Dakota, and South Dakota were analyzed to determine whether the water quality of streams in the basin is adequate to meet future needs. For the Red River at Emerson, Manitoba, site, pH values, water temperatures, and dissolved-oxygen concentrations generally were within the criteria established for the protection of aquatic life. Dissolved-solids concentrations ranged from 245 to 1,100 milligrams per liter. Maximum sulfate and chloride concentrations were near, but did not exceed, the established secondary maximum contaminant level. The trace elements considered potentially harmful generally were at concentrations that were less than the established guidelines, standards, and criteria. The concentrations of lead that were detected may have occurred as a result of sample contamination.
For the Red River upstream from Emerson, Manitoba, sites, pH and other field values rarely exceeded the criteria established for the protection of aquatic life. Many constituent concentrations for the Red River below Fargo, N. site exceeded water-quality guidelines, standards, and criteria. However, the trace-element exceedances could be natural or could be related to pollution or sample contamination.
Many of the tributaries in the western part of the Red River Basin had median specific-conductance values that were greater than 1,000 microsiemens per centimeter. Sulfate concentrations occasionally exceeded the established drinking-water standard. Median arsenic concentrations were 6 micrograms per liter or less, and maximum concentrations rarely exceeded the 10-microgram-per-liter drinking-water standard that is scheduled to take effect in 2006. The small concentrations of lead, mercury, and selenium that occasionally were detected may have been a result of sample contamination or other factors. The tributaries in the eastern part of the Red River Basin had median specific-conductance values that were less than 1,000 microsiemens per centimeter.
Concentrations of pesticides that were detected and that had regulatory limits were less than the cited water-quality guidelines, standards, and criteria. Concentrations of compounds that were detected generally were less than the sediment- quality standards and criteria.
The data considered in this report generally provide a good baseline from which to evaluate changes in water-quality conditions. However, because many of the trace elements detected, including lead and mercury, may have been the result of sample contamination, additional data are needed to confirm that trace-element concentrations generally are low. Concentrations of major ions, including sulfate, and specific conductance may continue to approach drinking-water standards during periods of low flow because the streams, particularly those in the western part of the basin, are sustained mostly by ground-water discharge that generally has large dissolved-solids concentrations.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055095","usgsCitation":"Tornes, L.H., 2005, Water quality of streams in the Red River of the North Basin, Minnesota, North Dakota, and South Dakota, 1970-2001: U.S. Geological Survey Scientific Investigations Report 2005-5095, vi, 81 p., https://doi.org/10.3133/sir20055095.","productDescription":"vi, 81 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":185743,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6888,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir20055095/","linkFileType":{"id":5,"text":"html"}},{"id":352611,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5095/pdf/report.pdf"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -101,45.8 ], [ -101,79 ], [ -94.43333333333334,79 ], [ -94.43333333333334,45.8 ], [ -101,45.8 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699125","contributors":{"authors":[{"text":"Tornes, Lan H.","contributorId":70484,"corporation":false,"usgs":true,"family":"Tornes","given":"Lan","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":282685,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}