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":70625,"text":"fs20053016 - 2005 - Did you feel it? : citizens contribute to earthquake science","interactions":[],"lastModifiedDate":"2015-01-13T09:03:16","indexId":"fs20053016","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":"2005-3016","title":"Did you feel it? : citizens contribute to earthquake science","docAbstract":"Since the early 1990s, the magnitude and location of an earthquake have been available within minutes on the Internet. Now, as a result of work by the U.S. Geological Survey and with the cooperation of various regional seismic networks, people who experience an earthquake can go online and share information about its effects to help create a map of shaking intensities and damage. Such “Community Internet Intensity Maps” (CIIMs) contribute greatly toward the quick assessment of the scope of an earthquake emergency and provide valuable data for earthquake research.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs20053016","usgsCitation":"Wald, D.J., and Dewey, J.W., 2005, Did you feel it? : citizens contribute to earthquake science (Version 1.0): U.S. Geological Survey Fact Sheet 2005-3016, 4 p., https://doi.org/10.3133/fs20053016.","productDescription":"4 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":297150,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs20053016.PNG"},{"id":297149,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2005/3016/pdf/FS-2005-3016.pdf","size":"7.6 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":6807,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3016/","linkFileType":{"id":5,"text":"html"}}],"scale":"100000","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65da14","contributors":{"authors":[{"text":"Wald, David J. 0000-0002-1454-4514 wald@usgs.gov","orcid":"https://orcid.org/0000-0002-1454-4514","contributorId":795,"corporation":false,"usgs":true,"family":"Wald","given":"David","email":"wald@usgs.gov","middleInitial":"J.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":282742,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dewey, James W. 0000-0001-8838-2450 jdewey@usgs.gov","orcid":"https://orcid.org/0000-0001-8838-2450","contributorId":5819,"corporation":false,"usgs":true,"family":"Dewey","given":"James","email":"jdewey@usgs.gov","middleInitial":"W.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":282743,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70156406,"text":"70156406 - 2005 - An online operational rainfall-monitoring resource for epidemic malaria early warning systems in Africa","interactions":[],"lastModifiedDate":"2017-05-22T23:04:13","indexId":"70156406","displayToPublicDate":"2005-06-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2650,"text":"Malaria Journal","active":true,"publicationSubtype":{"id":10}},"title":"An online operational rainfall-monitoring resource for epidemic malaria early warning systems in Africa","docAbstract":"Periodic epidemics of malaria are a major public health problem for many sub-Saharan African countries. Populations in epidemic prone areas have a poorly developed immunity to malaria and the disease remains life threatening to all age groups. The impact of epidemics could be minimized by prediction and improved prevention through timely vector control and deployment of appropriate drugs. Malaria Early Warning Systems are advocated as a means of improving the opportunity for preparedness and timely response.
Rainfall is one of the major factors triggering epidemics in warm semi-arid and desert-fringe areas. Explosive epidemics often occur in these regions after excessive rains and, where these follow periods of drought and poor food security, can be especially severe. Consequently, rainfall monitoring forms one of the essential elements for the development of integrated Malaria Early Warning Systems for sub-Saharan Africa, as outlined by the World Health Organization.
The Roll Back Malaria Technical Resource Network on Prevention and Control of Epidemics recommended that a simple indicator of changes in epidemic risk in regions of marginal transmission, consisting primarily of rainfall anomaly maps, could provide immediate benefit to early warning efforts. In response to these recommendations, the Famine Early Warning Systems Network produced maps that combine information about dekadal rainfall anomalies, and epidemic malaria risk, available via their Africa Data Dissemination Service. These maps were later made available in a format that is directly compatible with HealthMapper, the mapping and surveillance software developed by the WHO's Communicable Disease Surveillance and Response Department. A new monitoring interface has recently been developed at the International Research Institute for Climate Prediction (IRI) that enables the user to gain a more contextual perspective of the current rainfall estimates by comparing them to previous seasons and climatological averages. These resources are available at no cost to the user and are updated on a routine basis.
","language":"English","publisher":"BioMed Central","doi":"10.1186/1475-2875-4-6","usgsCitation":"Grover-Kopec, E., Kawano, M., Klaver, R.W., Blumenthal, B., Ceccato, P., and Connor, S.J., 2005, An online operational rainfall-monitoring resource for epidemic malaria early warning systems in Africa: Malaria Journal, v. 4, no. 6, p. 1-5, https://doi.org/10.1186/1475-2875-4-6.","productDescription":"5 p.","startPage":"1","endPage":"5","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":477660,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1186/1475-2875-4-6","text":"Publisher Index Page"},{"id":307070,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"6","noUsgsAuthors":false,"publicationDate":"2005-01-21","publicationStatus":"PW","scienceBaseUri":"55d6fa2fe4b0518e3546bc1e","contributors":{"authors":[{"text":"Grover-Kopec, Emily","contributorId":146813,"corporation":false,"usgs":false,"family":"Grover-Kopec","given":"Emily","email":"","affiliations":[],"preferred":false,"id":569048,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kawano, Mika","contributorId":146814,"corporation":false,"usgs":false,"family":"Kawano","given":"Mika","email":"","affiliations":[],"preferred":false,"id":569049,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Klaver, Robert W. 0000-0002-3263-9701 bklaver@usgs.gov","orcid":"https://orcid.org/0000-0002-3263-9701","contributorId":3285,"corporation":false,"usgs":true,"family":"Klaver","given":"Robert","email":"bklaver@usgs.gov","middleInitial":"W.","affiliations":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true},{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"preferred":true,"id":569050,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Blumenthal, Benno","contributorId":146815,"corporation":false,"usgs":false,"family":"Blumenthal","given":"Benno","email":"","affiliations":[],"preferred":false,"id":569051,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ceccato, Pietro","contributorId":64126,"corporation":false,"usgs":true,"family":"Ceccato","given":"Pietro","email":"","affiliations":[],"preferred":false,"id":569052,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Connor, Stephen J.","contributorId":104370,"corporation":false,"usgs":true,"family":"Connor","given":"Stephen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":569053,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"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":70616,"text":"ofr20051037 - 2005 - Magnetotelluric data in the Espanola Basin, west of Santa Fe, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:14:03","indexId":"ofr20051037","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":"2005-1037","title":"Magnetotelluric data in the Espanola Basin, west of Santa Fe, New Mexico","language":"ENGLISH","doi":"10.3133/ofr20051037","usgsCitation":"Williams, J.M., and Rodriguez, B.D., 2005, Magnetotelluric data in the Espanola Basin, west of Santa Fe, New Mexico (Version 1.0): U.S. Geological Survey Open-File Report 2005-1037, 263 p., https://doi.org/10.3133/ofr20051037.","productDescription":"263 p.","costCenters":[],"links":[{"id":193333,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6803,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1037/","linkFileType":{"id":5,"text":"html"}}],"scale":"100000","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649441","contributors":{"authors":[{"text":"Williams, Jackie M.","contributorId":11217,"corporation":false,"usgs":true,"family":"Williams","given":"Jackie","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":282728,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rodriguez, Brian D. 0000-0002-2263-611X brod@usgs.gov","orcid":"https://orcid.org/0000-0002-2263-611X","contributorId":836,"corporation":false,"usgs":true,"family":"Rodriguez","given":"Brian","email":"brod@usgs.gov","middleInitial":"D.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":282727,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"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":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":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":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":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":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":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.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs20053046","usgsCitation":"Shulters, M.V., 2005, USGS California Water Science Center water programs in California (Online only): U.S. Geological Survey Fact Sheet 2005-3046, 2 p., https://doi.org/10.3133/fs20053046.","productDescription":"2 p.","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":126296,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3046.jpg"},{"id":6890,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/fs2005-3046/"}],"scale":"24000","country":"United 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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":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}]}} ,{"id":70184413,"text":"70184413 - 2005 - Saline tracer visualized with three-dimensional electrical resistivity tomography: Field-scale spatial moment analysis","interactions":[],"lastModifiedDate":"2018-10-31T10:27:27","indexId":"70184413","displayToPublicDate":"2005-05-24T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Saline tracer visualized with three-dimensional electrical resistivity tomography: Field-scale spatial moment analysis","docAbstract":"Cross-well electrical resistivity tomography (ERT) was used to monitor the migration of a saline tracer in a two-well pumping-injection experiment conducted at the Massachusetts Military Reservation in Cape Cod, Massachusetts. After injecting 2200 mg/L of sodium chloride for 9 hours, ERT data sets were collected from four wells every 6 hours for 20 days. More than 180,000 resistance measurements were collected during the tracer test. Each ERT data set was inverted to produce a sequence of 3-D snapshot maps that track the plume. In addition to the ERT experiment a pumping test and an infiltration test were conducted to estimate horizontal and vertical hydraulic conductivity values. Using modified moment analysis of the electrical conductivity tomograms, the mass, center of mass, and spatial variance of the imaged tracer plume were estimated. Although the tomograms provide valuable insights into field-scale tracer migration behavior and aquifer heterogeneity, standard tomographic inversion and application of Archie's law to convert electrical conductivities to solute concentration results in underestimation of tracer mass. Such underestimation is attributed to (1) reduced measurement sensitivity to electrical conductivity values with distance from the electrodes and (2) spatial smoothing (regularization) from tomographic inversion. The center of mass estimated from the ERT inversions coincided with that given by migration of the tracer plume using 3-D advective-dispersion simulation. The 3-D plumes seen using ERT exhibit greater apparent dispersion than the simulated plumes and greater temporal spreading than observed in field data of concentration breakthrough at the pumping well.
","language":"English","publisher":"Wiley","doi":"10.1029/2004WR003460","usgsCitation":"Singha, K., and Gorelick, S.M., 2005, Saline tracer visualized with three-dimensional electrical resistivity tomography: Field-scale spatial moment analysis: Water Resources Research, v. 41, no. 5, W05023; 17 p. , https://doi.org/10.1029/2004WR003460.","productDescription":"W05023; 17 p. ","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":477662,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2004wr003460","text":"Publisher Index Page"},{"id":337104,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"41","issue":"5","noUsgsAuthors":false,"publicationDate":"2005-05-24","publicationStatus":"PW","scienceBaseUri":"58c1263fe4b014cc3a3d34c2","contributors":{"authors":[{"text":"Singha, Kamini","contributorId":76733,"corporation":false,"usgs":true,"family":"Singha","given":"Kamini","affiliations":[],"preferred":false,"id":681369,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gorelick, Steven M.","contributorId":8784,"corporation":false,"usgs":true,"family":"Gorelick","given":"Steven","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":681370,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70581,"text":"wdrMARI041 - 2005 - Water resources data for Massachusetts and Rhode Island, water year 2004","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"wdrMARI041","displayToPublicDate":"2005-05-20T00:00:00","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":"MA-RI-04-1","title":"Water resources data for Massachusetts and Rhode Island, water year 2004","docAbstract":"This report includes records of stage, discharge, and water quality of streams; contents and elevation of lakes and ponds; and water levels of ground-water wells. This volume contains discharge records for 112 gaging stations; stage records for 2 gaging stations; stage records for 2 ponds; month-end contents of 1 reservoir; precipitation totals at 6 gaging stations; water quality for 21 gaging stations; air temperature at 2 climatological stations; and water levels for 131 observation wells. Locations of these sites are shown in figures 1 and 2. Hydrologic data were collected at many sites that were not involved in the systematic data-collection program; these data are published as miscellaneous discharge measurements, miscellaneous surface-water-quality, and miscellaneous ground-water-quality data. The data in this report represent that part of the National Water Information System (NWIS) operated by the U.S. Geological Survey and cooperating State and Federal agencies in Massachusetts and Rhode Island.","language":"ENGLISH","doi":"10.3133/wdrMARI041","usgsCitation":"Socolow, R., Comeau, L., and Murino, D., 2005, Water resources data for Massachusetts and Rhode Island, water year 2004: U.S. Geological Survey Water Data Report MA-RI-04-1, 326 p. : photographs, https://doi.org/10.3133/wdrMARI041.","productDescription":"326 p. : photographs","costCenters":[],"links":[{"id":185742,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6887,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdr-ma-04/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f400f","contributors":{"authors":[{"text":"Socolow, R.S.","contributorId":17639,"corporation":false,"usgs":true,"family":"Socolow","given":"R.S.","affiliations":[],"preferred":false,"id":282682,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Comeau, L.Y.","contributorId":52254,"corporation":false,"usgs":true,"family":"Comeau","given":"L.Y.","email":"","affiliations":[],"preferred":false,"id":282684,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Murino, Domenic Jr.","contributorId":42649,"corporation":false,"usgs":true,"family":"Murino","given":"Domenic","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":282683,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70568,"text":"ofr20051143 - 2005 - MODFLOW data extractor program","interactions":[],"lastModifiedDate":"2020-01-26T16:52:42","indexId":"ofr20051143","displayToPublicDate":"2005-05-18T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1143","title":"MODFLOW data extractor program","docAbstract":"EXTRACTOR is a program that extracts data from formatted and labeled MODFLOW head or drawdown files or from MODFLOW-GWT concentration or velocity files. The user specifies the number of rows, columns, and layers in the target data file, the desired time step or move number, and the range of rows, columns, and layers for which data should be extracted and written to a new text file. The new text file can then be imported into other data-analysis programs.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051143","usgsCitation":"Zinn, B.A., and Konikow, L.F., 2005, MODFLOW data extractor program: U.S. Geological Survey Open-File Report 2005-1143, 11 p., https://doi.org/10.3133/ofr20051143.","productDescription":"11 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":186575,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6854,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1143/","linkFileType":{"id":5,"text":"html"}}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648c5e","contributors":{"authors":[{"text":"Zinn, Brendan A.","contributorId":102953,"corporation":false,"usgs":true,"family":"Zinn","given":"Brendan","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":282665,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Konikow, Leonard F. 0000-0002-0940-3856 lkonikow@usgs.gov","orcid":"https://orcid.org/0000-0002-0940-3856","contributorId":158,"corporation":false,"usgs":true,"family":"Konikow","given":"Leonard","email":"lkonikow@usgs.gov","middleInitial":"F.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":282664,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70570,"text":"tm12A1 - 2005 - ShakeMap manual: technical manual, user's guide, and software guide","interactions":[],"lastModifiedDate":"2012-02-02T00:13:48","indexId":"tm12A1","displayToPublicDate":"2005-05-18T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":335,"text":"Techniques and Methods","code":"TM","onlineIssn":"2328-7055","printIssn":"2328-7047","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"12-A1","title":"ShakeMap manual: technical manual, user's guide, and software guide","docAbstract":"ShakeMap (http://earthquake.usgs.gov/shakemap) --rapidly, automatically generated shaking and intensity maps--combines instrumental measurements of shaking with information about local geology and earthquake location and magnitude to estimate shaking variations throughout a geographic area. The results are rapidly available via the Web through a variety of map formats, including Geographic Information System (GIS) coverages. These maps have become a valuable tool for emergency response, public information, loss estimation, earthquake planning, and post-earthquake engineering and scientific analyses. With the adoption of ShakeMap as a standard tool for a wide array of users and uses came an impressive demand for up-to-date technical documentation and more general guidelines for users and software developers. This manual is meant to address this need.\r\n\r\nShakeMap, and associated Web and data products, are rapidly evolving as new advances in communications, earthquake science, and user needs drive improvements. As such, this documentation is organic in nature. We will make every effort to keep it current, but undoubtedly necessary changes in operational systems take precedence over producing and making documentation publishable.","language":"ENGLISH","doi":"10.3133/tm12A1","usgsCitation":"Wald, D.J., Worden, B.C., Quitoriano, V., and Pankow, K.L., 2005, ShakeMap manual: technical manual, user's guide, and software guide (Version 1.0): U.S. Geological Survey Techniques and Methods 12-A1, 134 p., https://doi.org/10.3133/tm12A1.","productDescription":"134 p.","costCenters":[],"links":[{"id":124749,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tm_12_a1.gif"},{"id":6856,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/tm/2005/12A01/","linkFileType":{"id":5,"text":"html"}}],"scale":"100000","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f3e62","contributors":{"authors":[{"text":"Wald, David J. 0000-0002-1454-4514 wald@usgs.gov","orcid":"https://orcid.org/0000-0002-1454-4514","contributorId":795,"corporation":false,"usgs":true,"family":"Wald","given":"David","email":"wald@usgs.gov","middleInitial":"J.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":282668,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Worden, Bruce C.","contributorId":43438,"corporation":false,"usgs":true,"family":"Worden","given":"Bruce","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":282670,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Quitoriano, Vincent","contributorId":29514,"corporation":false,"usgs":true,"family":"Quitoriano","given":"Vincent","email":"","affiliations":[],"preferred":false,"id":282669,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pankow, Kris L.","contributorId":79180,"corporation":false,"usgs":true,"family":"Pankow","given":"Kris","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":282671,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70566,"text":"wdrNJ042 - 2005 - Water resources data, New Jersey, water year 2004--volume 2. ground-water data","interactions":[],"lastModifiedDate":"2012-02-02T00:13:48","indexId":"wdrNJ042","displayToPublicDate":"2005-05-18T00:00:00","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-04-2","title":"Water resources data, New Jersey, water year 2004--volume 2. ground-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, contents, and water quality of lakes and reservoirs; and water levels and water quality of ground water. Volume 2 contains a summary of the hydrologic conditions for 2004 water year; a listing of current water resource projects in New Jersey; a bibliography of water-related reports, articles, and fact sheets completed by the Geological Survey in recent years; records of ground-water levels from 196 wells; and a table of discontinued observation wells for which ground-water-level data are available. The locations of the ground-water level sites are shown on figure 4. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating Federal, Sate, and local agencies in New Jersey.","language":"ENGLISH","doi":"10.3133/wdrNJ042","usgsCitation":"Jones, W.D., 2005, Water resources data, New Jersey, water year 2004--volume 2. ground-water data: U.S. Geological Survey Water Data Report NJ-04-2, 249 p., https://doi.org/10.3133/wdrNJ042.","productDescription":"249 p.","costCenters":[],"links":[{"id":186573,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6853,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdr-nj-04-2/","linkFileType":{"id":5,"text":"html"}}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0f3d","contributors":{"authors":[{"text":"Jones, Walter D.","contributorId":106460,"corporation":false,"usgs":true,"family":"Jones","given":"Walter","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":282657,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70574,"text":"sir20045256 - 2005 - Movement of the saltwater interface in the surficial aquifer system in response to hydrologic stresses and water-management practices, Broward County, Florida","interactions":[],"lastModifiedDate":"2023-09-20T22:00:31.013424","indexId":"sir20045256","displayToPublicDate":"2005-05-18T00:00:00","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":"2004-5256","title":"Movement of the saltwater interface in the surficial aquifer system in response to hydrologic stresses and water-management practices, Broward County, Florida","docAbstract":"A study was conducted to evaluate the relation between water-level fluctuations and saltwater intrusion in Broward County, Florida. The objective was achieved through data collection at selected wells in Broward County and through the development of a variable-density ground-water flow model. The numerical model is representative of many locations in Broward County that contain a well field, control structure, canal, the Intracoastal Waterway, and the Atlantic Ocean. The model was used to simulate short-term movement (from tidal fluctuations to monthly changes) and long-term movement (greater than 10 years) of the saltwater interface resulting from changes in rainfall, well-field withdrawals, sea-level rise, and upstream canal stage. The SEAWAT code, which is a combined version of the computer codes, MODFLOW and MT3D, was used to simulate the complex variable-density flow patterns.\r\n\r\nModel results indicated that the canal, control structure, and sea level have major effects on ground-water flow. For periods greater than 10 years, the upstream canal stage controls the movement and location of the saltwater interface. If upstream canal stage is decreased by 1 foot (0.3048 meter), the saltwater interface takes 50 years to move inland and stabilize. If the upstream canal stage is then increased by 1 foot (0.3048 meter), the saltwater interface takes 90 years to move seaward and stabilize. If sea level rises about 48 centimeters over the next 100 year as predicted, then inland movement of the saltwater interface may cause well-field contamination.\r\n\r\nFor periods less than 10 years, simulation results indicated that a 3-year drought with increased well-field withdrawals probably will not have long-term effects on the position of the saltwater interface in the Biscayne aquifer. The saltwater interface returns to its original position in less than 10 years. Model results, however, indicated that the interface location in the lower part of the surficial aquifer system takes longer than 10 years to recover from a drought. Additionally, rainfall seems to have the greatest effect on saltwater interface movement in areas some distance from canals, but the upstream canal stage has the greatest effect on the movement of the saltwater interface near canals.\r\n\r\nField data indicated that saltwater interface movement includes short-term fluctuations caused by tidal fluctuations and long-term seasonal fluctuations. Statistical analyses of daily-averaged data indicated that the saltwater interface moves in response to pumpage, rainfall, and upstream canal stage. In areas near the canal, the saltwater interface is most affected by canal stage because water-management structures control the stage in the upstream part of the canal and allow movement of the saltwater interface. In areas away from the canal, the saltwater interface is most affected by pumpage and rainfall, depending on the location of well fields. Data analyses also revealed that rainfall changes the vertical flow direction in the Biscayne aquifer.\r\n\r\nResults from the study indicated that upstream canal stage substantially affects the long-term position of the saltwater interface in the surficial aquifer system. The saltwater interface moves faster inland than seaward because of changes in upstream canal stage. For short-term problems, such as drought, the threat of saltwater intrusion in the Biscayne aquifer does not appear to be severe if the well-field withdrawal is increased; however, this conclusion is based on the assumption that well-field withdrawals will decrease once the drought is over. Sea-level rise may be a potential threat to the water supply in Broward County as the saltwater interface moves inland toward well fields.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20045256","usgsCitation":"Dausman, A.M., and Langevin, C.D., 2005, Movement of the saltwater interface in the surficial aquifer system in response to hydrologic stresses and water-management practices, Broward County, Florida: U.S. Geological Survey Scientific Investigations Report 2004-5256, viii, 73 p., https://doi.org/10.3133/sir20045256.","productDescription":"viii, 73 p.","costCenters":[{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"links":[{"id":420991,"rank":3,"type":{"id":36,"text":"NGMDB Index 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Alyssa M. adausman@usgs.gov","contributorId":1545,"corporation":false,"usgs":true,"family":"Dausman","given":"Alyssa","email":"adausman@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":false,"id":282677,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Langevin, Christian D. 0000-0001-5610-9759 langevin@usgs.gov","orcid":"https://orcid.org/0000-0001-5610-9759","contributorId":1030,"corporation":false,"usgs":true,"family":"Langevin","given":"Christian","email":"langevin@usgs.gov","middleInitial":"D.","affiliations":[{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"preferred":true,"id":282676,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70567,"text":"sir20055055 - 2005 - Organic wastewater compounds, pharmaceuticals, and coliphage in ground water receiving discharge from onsite wastewater treatment systems near La Pine, Oregon: Occurrence and implications for transport","interactions":[],"lastModifiedDate":"2022-01-03T21:21:45.599003","indexId":"sir20055055","displayToPublicDate":"2005-05-18T00:00:00","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":"2005-5055","title":"Organic wastewater compounds, pharmaceuticals, and coliphage in ground water receiving discharge from onsite wastewater treatment systems near La Pine, Oregon: Occurrence and implications for transport","docAbstract":"The occurrence of organic wastewater compounds (components of 'personal care products' and other common household chemicals), pharmaceuticals (human prescription and nonprescription medical drugs), and coliphage (viruses that infect coliform bacteria, and found in high concentrations in municipal wastewater) in onsite wastewater (septic tank effluent) and in a shallow, unconfined, sandy aquifer that serves as the primary source of drinking water for most residents near La Pine, Oregon, was documented. Samples from two types of observation networks provided basic occurrence data for onsite wastewater and downgradient ground water. One observation network was a group of 28 traditional and innovative (advanced treatment) onsite wastewater treatment systems and associated downgradient drainfield monitoring wells, referred to as the 'innovative systems network'. The drainfield monitoring wells were located adjacent to or under onsite wastewater treatment system drainfield lines. Another observation network, termed the 'transect network', consisted of 31 wells distributed among three transects of temporary, stainless-steel-screened, direct-push monitoring wells installed along three plumes of onsite wastewater. The transect network, by virtue of its design, also provided a basis for increased understanding of the transport of analytes in natural systems. Coliphage were frequently detected in onsite wastewater. Coliphage concentrations in onsite wastewater were highly variable, ranging from less than 1 to 3,000,000 plaque forming units per 100 milliliters. Coliphage were occasionally detected (eight occurrences) at low concentrations in samples from wells located downgradient from onsite wastewater treatment system drainfield lines. However, coliphage concentrations were below method detection limits in replicate or repeat samples collected from the eight sites. The consistent absence of coliphage detections in the replicate or repeat samples is interpreted to indicate that the detections reported for ground-water samples represented low-level field or laboratory contamination, and it would appear that coliphage were effectively attenuated to less than 1 PFU/100 mL over distances of several feet of transport in the La Pine aquifer and (or) overlying unsaturated zone. Organic wastewater compounds were frequently detected in onsite wastewater. Of the 63 organic wastewater compounds in the analytical schedule, 45 were detected in the 21 samples of onsite wastewater. Concentrations of organic wastewater compounds reached a maximum of 1,300 ug/L (p-cresol). Caffeine was detected at concentrations as high as 320 ug/L. Fourteen of the 45 compounds were detected in more than 90 percent of onsite wastewater samples. Fewer (nine) organic wastewater compounds were detected in ground water, despite the presence of nitrate and chloride likely from onsite wastewater sources. The nine organic wastewater compounds that were detected in ground-water samples were acetyl-hexamethyl-tetrahydro-naphthalene (AHTN), caffeine, cholesterol, hexahydrohexamethyl-cyclopentabenzopyran, N,N-diethyl-meta-toluamide (DEET), tetrachloroethene, tris (2-chloroethyl) phosphate, tris (dichloroisopropyl) phosphate, and tributyl phosphate. Frequent detection of household-chemical type organic wastewater compounds in onsite wastewater provides evidence that some of these organic wastewater compounds may be useful indicators of human waste effluent dispersal in some hydrologic environments. The occurrence of organic wastewater compounds in ground water downgradient from onsite wastewater treatment systems demonstrates that a subgroup of organic wastewater compounds is transported in the La Pine aquifer. The consistently low concentrations (generally less than 1 ug/L) of organic wastewater compounds in water samples collected from wells located no more than 19 feet from drainfield lines indicates that the reactivity (sorption, degradation) of this suite of organic waste.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055055","collaboration":"Prepared in cooperation with Oregon Department of Environmental Quality and Deschutes County Environmental Health Division","usgsCitation":"Hinkle, S., Weick, R.J., Johnson, J.M., Cahill, J.D., Smith, S.G., and Rich, B.J., 2005, Organic wastewater compounds, pharmaceuticals, and coliphage in ground water receiving discharge from onsite wastewater treatment systems near La Pine, Oregon: Occurrence and implications for transport (Version 1.1, Revised Jul 2009): U.S. Geological Survey Scientific Investigations Report 2005-5055, vi, 98 p., https://doi.org/10.3133/sir20055055.","productDescription":"vi, 98 p.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":186574,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":393804,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_86816.htm"},{"id":12807,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5055/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Oregon","city":"La Pine","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.6667,\n 43.5417\n ],\n [\n -121.3667,\n 43.5417\n ],\n [\n -121.3667,\n 43.9167\n ],\n [\n -121.6667,\n 43.9167\n ],\n [\n -121.6667,\n 43.5417\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"Version 1.1, Revised Jul 2009","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db691254","contributors":{"authors":[{"text":"Hinkle, Stephen J.","contributorId":78821,"corporation":false,"usgs":true,"family":"Hinkle","given":"Stephen J.","affiliations":[],"preferred":false,"id":282662,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weick, Rodney J.","contributorId":79560,"corporation":false,"usgs":true,"family":"Weick","given":"Rodney","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":282663,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnson, Jill M.","contributorId":55908,"corporation":false,"usgs":true,"family":"Johnson","given":"Jill","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":282660,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cahill, Jeffery D.","contributorId":71630,"corporation":false,"usgs":true,"family":"Cahill","given":"Jeffery","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":282661,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Smith, Steven G. sgsmith@usgs.gov","contributorId":1560,"corporation":false,"usgs":true,"family":"Smith","given":"Steven","email":"sgsmith@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":282658,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Rich, Barbara J.","contributorId":42295,"corporation":false,"usgs":true,"family":"Rich","given":"Barbara","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":282659,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70565,"text":"wdrCA043 - 2005 - Water resources data-California, water year 2004, volume 3. southern central valley basins and The Great Basin from Walker River to Truckee River","interactions":[],"lastModifiedDate":"2012-02-02T00:13:48","indexId":"wdrCA043","displayToPublicDate":"2005-05-18T00:00:00","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":"CA-04-3","title":"Water resources data-California, water year 2004, volume 3. southern central valley basins and The Great Basin from Walker River to Truckee River","docAbstract":"Water-resources data for the 2004 water year for California consist of records of stage, discharge, and water quality of streams, stage and contents in lakes and reservoirs, and water levels and water quality in wells. Volume 3 contains discharge records for 187 gaging stations, stage and contents for 48 lakes and reservoirs, water quality for 35 stations and 14 partial-record stations, and precipitation data for 2 stations. Also included are 1 miscellaneous partial-record site and 1 crest-stage partial-record station. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in California.","language":"ENGLISH","doi":"10.3133/wdrCA043","usgsCitation":"Pope, G., Freeman, L., Rockwell, G., and Brockner, S., 2005, Water resources data-California, water year 2004, volume 3. southern central valley basins and The Great Basin from Walker River to Truckee River: U.S. Geological Survey Water Data Report CA-04-3, 590 p., https://doi.org/10.3133/wdrCA043.","productDescription":"590 p.","costCenters":[],"links":[{"id":186572,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6852,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdr-ca-04-3/","linkFileType":{"id":5,"text":"html"}}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0ae9","contributors":{"authors":[{"text":"Pope, G.L.","contributorId":58692,"corporation":false,"usgs":true,"family":"Pope","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":282655,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Freeman, L.A.","contributorId":86374,"corporation":false,"usgs":true,"family":"Freeman","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":282656,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rockwell, G.L.","contributorId":47408,"corporation":false,"usgs":true,"family":"Rockwell","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":282653,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brockner, S.J.","contributorId":56307,"corporation":false,"usgs":true,"family":"Brockner","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":282654,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70569,"text":"ds120 - 2005 - Concentrations of organic contaminants detected during managed flow conditions, San Joaquin River and Old River, California, 2001","interactions":[],"lastModifiedDate":"2012-03-02T17:16:06","indexId":"ds120","displayToPublicDate":"2005-05-18T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"120","title":"Concentrations of organic contaminants detected during managed flow conditions, San Joaquin River and Old River, California, 2001","docAbstract":"Concentrations of organic contaminants were determined in water samples collected at six surface-water sites located along the San Joaquin and Old Rivers during April through June 2001. Water samples were collected, coincident with salmon smolt caging studies conducted by researchers from the Bodega Marine Laboratory at the University of California at Davis to characterize exposure of the salmon smolt to organic contaminants. Sampling occurred prior to, during, and following the implementation of managed streamflow conditions on the San Joaquin and Old Rivers as part of the Vernalis Adaptive Management Plan. Thirteen pesticides were detected in water samples collected during this study, and at least five pesticides were detected in each sample. The total number of pesticide detections varied little between river systems and between sites, but the maximum concentrations of most pesticides occurred in San Joaquin River samples. The total number of pesticides detected varied little over the three time periods. However, during the period of managed streamflow, the fewest number of pesticides were detected at their absolute maximum concentration. Nine wastewater compounds were detected during this study. Suspended-sediment concentrations were similar for the San Joaquin and Old Rivers except during the period of managed streamflow conditions, when suspended-sediment concentration was higher at sites on the San Joaquin River than at sites on the Old River. Values for water parameters (pH, specific conductance, and hardness) were lowest during the period of managed flows.","language":"ENGLISH","doi":"10.3133/ds120","usgsCitation":"Orlando, J., and Kuivila, K., 2005, Concentrations of organic contaminants detected during managed flow conditions, San Joaquin River and Old River, California, 2001 (Online only): U.S. Geological Survey Data Series 120, 19 p., https://doi.org/10.3133/ds120.","productDescription":"19 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":186649,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6855,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ds120/","linkFileType":{"id":5,"text":"html"}}],"scale":"100000","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b03e4b07f02db698f07","contributors":{"authors":[{"text":"Orlando, James L. 0000-0002-0099-7221","orcid":"https://orcid.org/0000-0002-0099-7221","contributorId":95954,"corporation":false,"usgs":true,"family":"Orlando","given":"James L.","affiliations":[],"preferred":false,"id":282667,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kuivila, Kathryn 0000-0001-7940-489X kkuivila@usgs.gov","orcid":"https://orcid.org/0000-0001-7940-489X","contributorId":1367,"corporation":false,"usgs":true,"family":"Kuivila","given":"Kathryn ","email":"kkuivila@usgs.gov","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":false,"id":282666,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70559,"text":"wdrOH042 - 2005 - Ohio water resources data, water year 2004 : volume 2. St. Lawrence River basin and statewide project data","interactions":[],"lastModifiedDate":"2012-02-02T00:13:48","indexId":"wdrOH042","displayToPublicDate":"2005-05-16T00:00:00","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":"OH-04-2","title":"Ohio water resources data, water year 2004 : volume 2. St. Lawrence River basin and statewide project data","docAbstract":"Water-resources data for the 2004 water year for Ohio consist 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 wells. This report, in two volumes, contains records for water discharge at 137 gaging stations and various partial-record sites; water levels at 243 observation wells and 38 crest-stage gages; and water quality at 18 gaging stations, 34 observation wells, and no partial-record sites. Also included are data from miscellaneous and synoptic sites. Additional water data were collected at various sites not involved in the systematic data-collection program and are published as miscellaneous measurements and analyses. These data represent that part of the National Water Information System collected by the U.S. Geological Survey and cooperating Federal, State, and local agencies in Ohio.","language":"ENGLISH","doi":"10.3133/wdrOH042","usgsCitation":"Shindel, H., Mangus, J., and Frum, S., 2005, Ohio water resources data, water year 2004 : volume 2. St. Lawrence River basin and statewide project data: U.S. Geological Survey Water Data Report OH-04-2, 332 p., https://doi.org/10.3133/wdrOH042.","productDescription":"332 p.","costCenters":[],"links":[{"id":186509,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6850,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdroh04/","linkFileType":{"id":5,"text":"html"}}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691ec3","contributors":{"authors":[{"text":"Shindel, H.L.","contributorId":17652,"corporation":false,"usgs":true,"family":"Shindel","given":"H.L.","affiliations":[],"preferred":false,"id":282649,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mangus, J.P.","contributorId":28301,"corporation":false,"usgs":true,"family":"Mangus","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":282650,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Frum, S.R.","contributorId":84843,"corporation":false,"usgs":true,"family":"Frum","given":"S.R.","email":"","affiliations":[],"preferred":false,"id":282651,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}