The data described in this report were collected in the U. S. Geological Survey (USGS) Priority Ecosystems Science project investigating \"Forcing Effects on Flow Structure in Vegetated Wetlands of the Everglades.\" Data collected at five locations in Shark River Slough, Everglades National Park, during the 2002-2003 wet season are documented in the report. Methods used to process the data are described. Daily mean flow velocities, water temperatures, and specific conductance values are presented in the appendices. The quality-checked and edited data have been compiled and stored on the USGS South Florida Information Access (SOFIA) website http://sofia.usgs.gov.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20041233","usgsCitation":"Riscassi, A.L., and Schaffranek, R.W., 2004, Flow velocity, water temperature, and conductivity in Shark River Slough, Everglades National Park, Florida: June 2002–July 2003: U.S. Geological Survey Open-File Report 2004-1233, 64 p., https://doi.org/10.3133/ofr20041233.","productDescription":"64 p.","costCenters":[],"links":[{"id":183525,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":394217,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_69889.htm"},{"id":6003,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr20041233/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Florida","otherGeospatial":"Everglades National Park, Shark River Slough","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.8961,\n 25.4967\n ],\n [\n -80.6147,\n 25.4967\n ],\n [\n -80.6147,\n 25.7617\n ],\n [\n -80.8961,\n 25.7617\n ],\n [\n -80.8961,\n 25.4967\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de821","contributors":{"authors":[{"text":"Riscassi, Ami L.","contributorId":24399,"corporation":false,"usgs":true,"family":"Riscassi","given":"Ami","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":257718,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schaffranek, Raymond W.","contributorId":86314,"corporation":false,"usgs":true,"family":"Schaffranek","given":"Raymond","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":257719,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":58104,"text":"ofr20041353 - 2004 - Dynamics of the physical environment at the USS Arizona memorial: 2002-2004","interactions":[],"lastModifiedDate":"2023-03-22T20:45:22.500744","indexId":"ofr20041353","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2004-1353","title":"Dynamics of the physical environment at the USS Arizona memorial: 2002-2004","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20041353","usgsCitation":"Storlazzi, C., Russell, M.A., Owens, M.D., Field, M.E., and Murphy, L.E., 2004, Dynamics of the physical environment at the USS Arizona memorial: 2002-2004 (Version 1.0): U.S. Geological Survey Open-File Report 2004-1353, 28 p., https://doi.org/10.3133/ofr20041353.","productDescription":"28 p.","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":181222,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414578,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_69080.htm","linkFileType":{"id":5,"text":"html"}},{"id":5716,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1353/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Hawaii","otherGeospatial":"USS Arizona Memorial","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -157.95033963540192,\n 21.365229540959703\n ],\n [\n -157.95033963540192,\n 21.364365122627703\n ],\n [\n -157.94948215103528,\n 21.364365122627703\n ],\n [\n -157.94948215103528,\n 21.365229540959703\n ],\n [\n -157.95033963540192,\n 21.365229540959703\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a59e4b07f02db62fe2d","contributors":{"authors":[{"text":"Storlazzi, Curt D. 0000-0001-8057-4490","orcid":"https://orcid.org/0000-0001-8057-4490","contributorId":77889,"corporation":false,"usgs":true,"family":"Storlazzi","given":"Curt D.","affiliations":[],"preferred":false,"id":258330,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Russell, Matthew A.","contributorId":74814,"corporation":false,"usgs":true,"family":"Russell","given":"Matthew","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":258329,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Owens, Marshall D.","contributorId":32238,"corporation":false,"usgs":true,"family":"Owens","given":"Marshall","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":258327,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Field, Michael E. mfield@usgs.gov","contributorId":2101,"corporation":false,"usgs":true,"family":"Field","given":"Michael","email":"mfield@usgs.gov","middleInitial":"E.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":258326,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Murphy, Larry E.","contributorId":57942,"corporation":false,"usgs":true,"family":"Murphy","given":"Larry","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":258328,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":58050,"text":"ofr20041347 - 2004 - Rainfall, runoff, and water-quality data for the urban storm-water program in the Albuquerque, New Mexico, metropolitan area, water year 2002","interactions":[],"lastModifiedDate":"2025-06-05T18:34:13.933998","indexId":"ofr20041347","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2004-1347","title":"Rainfall, runoff, and water-quality data for the urban storm-water program in the Albuquerque, New Mexico, metropolitan area, water year 2002","docAbstract":"Urbanization has dramatically increased precipitation runoff to the system of drainage channels and natural stream channels in the Albuquerque, New Mexico, metropolitan area. Rainfall and runoff data are important for planning and designing future storm-water conveyance channels in newly developing areas. Storm-water quality also is monitored in accordance with the National Pollutant Discharge Elimination System mandated by the U.S. Environmental Protection Agency. The Albuquerque Metropolitan Arroyo Flood Control Authority, the City of Albuquerque, and the U.S. Geological Survey began a cooperative program to collect hydrologic data to help assess the quality and quantity of surface-water resources in the Albuquerque area. This report presents water-quality, streamflow, and rainfall data collected from October 1, 2001, to September 30, 2002 (water year 2002). Also provided is a station analysis for each of the 20 streamflow-gaging sites and 41 rainfall-gaging sites, which includes a description of monitoring equipment, problems associated with data collection during the year, and other information used to compute streamflow discharges or rainfall records. A hydrographic comparison shows the effects that the largest drainage channel in the metropolitan area, the North Floodway Channel, has on total flow in the Rio Grande.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20041347","collaboration":"Prepared in cooperation with the Albuquerque Metropolitan Arroyo Flood Control Authority and the City of Albuquerque","usgsCitation":"Kelly, T., Romero, O., and Turner, E., 2004, Rainfall, runoff, and water-quality data for the urban storm-water program in the Albuquerque, New Mexico, metropolitan area, water year 2002: U.S. Geological Survey Open-File Report 2004-1347, iv, 119 p., https://doi.org/10.3133/ofr20041347.","productDescription":"iv, 119 p.","costCenters":[],"links":[{"id":183996,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2004/1347/report-thumb.jpg"},{"id":489805,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2004/1347/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Mexico","city":"Albuquerque","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -107.0159062021065,\n 35.40557093842378\n ],\n [\n -107.0159062021065,\n 34.77880064470824\n ],\n [\n -106.13498380427245,\n 34.77880064470824\n ],\n [\n -106.13498380427245,\n 35.40557093842378\n ],\n [\n -107.0159062021065,\n 35.40557093842378\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6496f4","contributors":{"authors":[{"text":"Kelly, Todd","contributorId":89168,"corporation":false,"usgs":true,"family":"Kelly","given":"Todd","email":"","affiliations":[],"preferred":false,"id":258219,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Romero, Orlando","contributorId":92335,"corporation":false,"usgs":true,"family":"Romero","given":"Orlando","affiliations":[],"preferred":false,"id":258220,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Turner, Eric","contributorId":101145,"corporation":false,"usgs":true,"family":"Turner","given":"Eric","email":"","affiliations":[],"preferred":false,"id":258221,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":58048,"text":"ofr20041334 - 2004 - NADM Conceptual Model 1.0 -- A Conceptual Model for Geologic Map Information","interactions":[],"lastModifiedDate":"2012-02-02T00:12:15","indexId":"ofr20041334","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2004-1334","title":"NADM Conceptual Model 1.0 -- A Conceptual Model for Geologic Map Information","docAbstract":"Executive Summary -- The NADM Data Model Design Team was established in 1999 by the North American Geologic Map Data Model Steering Committee (NADMSC) with the purpose of drafting a geologic map data model for consideration as a standard for developing interoperable geologic map-centered databases by state, provincial, and federal geological surveys. The model is designed to be a technology-neutral conceptual model that can form the basis for a web-based interchange format using evolving information technology (e.g., XML, RDF, OWL), and guide implementation of geoscience databases in a common conceptual framework. The intended purpose is to allow geologic information sharing between geologic map data providers and users, independent of local information system implementation. \r\nThe model emphasizes geoscience concepts and relationships related to information presented on geologic maps. Design has been guided by an informal requirements analysis, documentation of existing databases, technology developments, and other standardization efforts in the geoscience and computer-science communities. \r\nA key aspect of the model is the notion that representation of the conceptual framework (ontology) that underlies geologic map data must be part of the model, because this framework changes with time and understanding, and varies between information providers. The top level of the model distinguishes geologic concepts, geologic representation concepts, and metadata. The geologic representation part of the model provides a framework for representing the ontology that underlies geologic map data through a controlled vocabulary, and for establishing the relationships between this vocabulary and a geologic map visualization or portrayal. Top-level geologic classes in the model are Earth material (substance), geologic unit (parts of the Earth), geologic age, geologic structure, fossil, geologic process, geologic relation, and geologic event.","language":"ENGLISH","doi":"10.3133/ofr20041334","usgsCitation":"North American Geologic Map Data Model (NADM) Steering Committee Data Model Design Team, 2004, NADM Conceptual Model 1.0 -- A Conceptual Model for Geologic Map Information: U.S. Geological Survey Open-File Report 2004-1334, 60 p., https://doi.org/10.3133/ofr20041334.","productDescription":"60 p.","costCenters":[],"links":[{"id":5978,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1334/","linkFileType":{"id":5,"text":"html"}},{"id":183917,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b492d","contributors":{"authors":[{"text":"North American Geologic Map Data Model (NADM) Steering Committee Data Model Design Team","contributorId":127896,"corporation":true,"usgs":false,"organization":"North American Geologic Map Data Model (NADM) Steering Committee Data Model Design Team","id":533190,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":58025,"text":"ofr20041277 - 2004 - Stream habitat and water-quality information for sites in the Buffalo River Basin and nearby basins of Arkansas, 2001-2002","interactions":[],"lastModifiedDate":"2012-02-02T00:12:31","indexId":"ofr20041277","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2004-1277","title":"Stream habitat and water-quality information for sites in the Buffalo River Basin and nearby basins of Arkansas, 2001-2002","docAbstract":"The Buffalo River lies in north-central Arkansas and is a tributary of the White River. Stream-habitat and water-quality information are presented for 52 sites in the Buffalo River Basin and adjacent areas of the White River Basin. The information was collected during the summers of 2001 and 2002 to supplement fish community sampling during the same time period.","language":"ENGLISH","doi":"10.3133/ofr20041277","usgsCitation":"Petersen, J., 2004, Stream habitat and water-quality information for sites in the Buffalo River Basin and nearby basins of Arkansas, 2001-2002: U.S. Geological Survey Open-File Report 2004-1277, 16 p., https://doi.org/10.3133/ofr20041277.","productDescription":"16 p.","costCenters":[],"links":[{"id":183450,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5955,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr2004-1277/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a54ab","contributors":{"authors":[{"text":"Petersen, James C. petersen@usgs.gov","contributorId":2437,"corporation":false,"usgs":true,"family":"Petersen","given":"James C.","email":"petersen@usgs.gov","affiliations":[{"id":129,"text":"Arkansas Water Science Center","active":true,"usgs":true}],"preferred":false,"id":258167,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":58024,"text":"ofr20041294 - 2004 - The Memphis, Shelby County, Tennessee, seismic hazard maps","interactions":[],"lastModifiedDate":"2012-02-02T00:12:31","indexId":"ofr20041294","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2004-1294","title":"The Memphis, Shelby County, Tennessee, seismic hazard maps","language":"ENGLISH","doi":"10.3133/ofr20041294","usgsCitation":"Cramer, C.H., Gomberg, J.S., Schweig, E.S., Waldron, B.A., and Tucker, K., 2004, The Memphis, Shelby County, Tennessee, seismic hazard maps (Version 1.0): U.S. Geological Survey Open-File Report 2004-1294, 41 p., https://doi.org/10.3133/ofr20041294.","productDescription":"41 p.","costCenters":[],"links":[{"id":183449,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5954,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1294/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f1418","contributors":{"authors":[{"text":"Cramer, Chris H.","contributorId":32196,"corporation":false,"usgs":true,"family":"Cramer","given":"Chris","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":258164,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gomberg, Joan S. 0000-0002-0134-2606 gomberg@usgs.gov","orcid":"https://orcid.org/0000-0002-0134-2606","contributorId":1269,"corporation":false,"usgs":true,"family":"Gomberg","given":"Joan","email":"gomberg@usgs.gov","middleInitial":"S.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":258162,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schweig, Eugene S. 0000-0003-3669-9741 schweig@usgs.gov","orcid":"https://orcid.org/0000-0003-3669-9741","contributorId":1271,"corporation":false,"usgs":true,"family":"Schweig","given":"Eugene","email":"schweig@usgs.gov","middleInitial":"S.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":258163,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Waldron, Brian A.","contributorId":96767,"corporation":false,"usgs":true,"family":"Waldron","given":"Brian","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":258166,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Tucker, Kathleen","contributorId":65921,"corporation":false,"usgs":true,"family":"Tucker","given":"Kathleen","affiliations":[],"preferred":false,"id":258165,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":57948,"text":"ofr20041342 - 2004 - Lead isotopic compositions of common arsenical pesticides used in New England","interactions":[],"lastModifiedDate":"2012-02-02T00:12:00","indexId":"ofr20041342","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2004-1342","title":"Lead isotopic compositions of common arsenical pesticides used in New England","docAbstract":"The three most important arsenical pesticides and herbicides that were extensively used on apple, blueberry, and potato crops in New England from mid-1800s to recent times are lead arsenate, calcium arsenate, and sodium arsenate. Lead arsenate was probably the most heavily used of the arsenical pesticides until it was banned in 1988. Other metal-arsenic pesticides were also used but in lesser amounts. A recent report identified areas in New England where arsenical pesticides were used extensively (Robinson and Ayuso, 2004). On the basis of factor analysis of metal concentrations in stream sediment samples, a positive correlation with pesticide use was shown in regions having stream sediment sample populations that contained concentrations of high arsenic and lead. Lead isotope compositions of stream sediments from areas with heavy use of the pesticides could not be entirely explained by lead originating from rock sulfides and their weathering products. An industrial lead contribution (mostly from atmospheric deposition of lead) was suggested in general to explain the lead isotopic distributions of the stream sediments that could not be accounted for by the natural lead in the environment. We concluded that when agricultural land previously contaminated with arsenical pesticides is urbanized, pesticide residues in the soils and stream sediments could be released into the groundwater. No lead isotopic data characterizing the compositions of pesticides were available for comparison. \r\n\r\nWe have determined the lead isotopic compositions of commonly used pesticides in New England, such as lead arsenate, sodium metaarsenite, and calcium arsenate, in order to assist in future isotopic comparisons and to better establish anthropogenic sources of Pb and As. New data are also presented for copper acetoarsenite (or Paris green), methyl arsonic acid and methane arsonic acid, as well as for arsanilic acid, all of which are used as feed additives to promote swine and poultry growth. The new data characterize these anthropogenic sources. The data show that the arsenical pesticides have similar compositions: 208Pb/207Pb = 2.3839-2.4721, 206Pb/207Pb = 1.1035-1.2010, and 206Pb/204Pb = 17.070-18.759 and, more importantly, that the pesticides overlap the composition of the stream sediments that represent the areas with the most extensive agricultural use. Copper acetoarsenite (Paris green), arsenic oxide, methyl arsonic acid, methane arsonic acid, and arsanilic acid were also analyzed and have lead isotope compositions that range widely. An important source of arsenic and metals to most of the stream sediment samples in New England appears to be weathering products from rocks and industrial lead, but the extensive use of arsenical pesticides and herbicides up to about the 1960s can also be a significant anthropogenic source in agricultural regions.","language":"ENGLISH","doi":"10.3133/ofr20041342","usgsCitation":"Ayuso, R., Foley, N., Robinson, G., Wandless, G., and Dillingham, J., 2004, Lead isotopic compositions of common arsenical pesticides used in New England (Version 1.0; Online only): U.S. Geological Survey Open-File Report 2004-1342, 14 p., https://doi.org/10.3133/ofr20041342.","productDescription":"14 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":5907,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1342/","linkFileType":{"id":5,"text":"html"}},{"id":181952,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Version 1.0; Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688a95","contributors":{"authors":[{"text":"Ayuso, Robert","contributorId":96350,"corporation":false,"usgs":true,"family":"Ayuso","given":"Robert","email":"","affiliations":[],"preferred":false,"id":257974,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foley, Nora","contributorId":9342,"corporation":false,"usgs":true,"family":"Foley","given":"Nora","affiliations":[],"preferred":false,"id":257970,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Robinson, Gilpin Jr. grobinso@usgs.gov","contributorId":23625,"corporation":false,"usgs":true,"family":"Robinson","given":"Gilpin","suffix":"Jr.","email":"grobinso@usgs.gov","affiliations":[],"preferred":false,"id":257971,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wandless, Gregory","contributorId":77233,"corporation":false,"usgs":true,"family":"Wandless","given":"Gregory","affiliations":[],"preferred":false,"id":257973,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dillingham, Jeremy","contributorId":49451,"corporation":false,"usgs":true,"family":"Dillingham","given":"Jeremy","email":"","affiliations":[],"preferred":false,"id":257972,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":57947,"text":"ofr20041336 - 2004 - Lime kiln dust as a potential raw material in portland cement manufacturing","interactions":[],"lastModifiedDate":"2012-02-02T00:12:00","indexId":"ofr20041336","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2004-1336","title":"Lime kiln dust as a potential raw material in portland cement manufacturing","docAbstract":"In the United States, the manufacture of portland cement involves burning in a rotary kiln a finely ground proportional mix of raw materials. The raw material mix provides the required chemical combination of calcium, silicon, aluminum, iron, and small amounts of other ingredients. The majority of calcium is supplied in the form of calcium carbonate usually from limestone. Other sources including waste materials or byproducts from other industries can be used to supply calcium (or lime, CaO), provided they have sufficiently high CaO content, have low magnesia content (less than 5 percent), and are competitive with limestone in terms of cost and adequacy of supply. In the United States, the lime industry produces large amounts of lime kiln dust (LKD), which is collected by dust control systems. This LKD may be a supplemental source of calcium for cement plants, if the lime and cement plants are located near enough to each other to make the arrangement economical.","language":"ENGLISH","doi":"10.3133/ofr20041336","usgsCitation":"Miller, M.M., and Callaghan, R.M., 2004, Lime kiln dust as a potential raw material in portland cement manufacturing (Version 1.0; Online only): U.S. Geological Survey Open-File Report 2004-1336, 9 p., https://doi.org/10.3133/ofr20041336.","productDescription":"9 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":181951,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5906,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1336/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0; Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a52ef","contributors":{"authors":[{"text":"Miller, M. Michael mmiller1@usgs.gov","contributorId":2018,"corporation":false,"usgs":true,"family":"Miller","given":"M.","email":"mmiller1@usgs.gov","middleInitial":"Michael","affiliations":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true},{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":257969,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Callaghan, Robert M. rcallaghan@usgs.gov","contributorId":475,"corporation":false,"usgs":true,"family":"Callaghan","given":"Robert","email":"rcallaghan@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":257968,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":57899,"text":"ofr20041296 - 2004 - A summary of the scientific literature on the effects of fire on the concentration of nutrients in surface waters","interactions":[],"lastModifiedDate":"2012-02-02T00:12:14","indexId":"ofr20041296","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2004-1296","title":"A summary of the scientific literature on the effects of fire on the concentration of nutrients in surface waters","docAbstract":"This paper provides a detailed review of the chemical changes that occur in soil during a fire, the pathways by which nutrients are transferred from soil to surface-water bodies following a fire, and the temporal and spatial effects of fires on the concentration of nutrients in surface-water bodies during and following a fire that have been reported in the scientific literature. Thirty-nine papers from the scientific literature that represent studies that (1) were done in a variety of environments (savannas, grasslands, temperate forests, alpine forests, and so forth); (2) had a range of sampling frequency and duration, such as during and immediately following a fire (from the start of fire to 1 year later), short-term sampling (from end of fire to 3 years later), and long term-sampling (sampling for greater than 3 years following a fire); and (3) incorporated watersheds with various burn intensities, severities, and histories were reviewed and summarized. The review of the scientific literature has revealed that measurable effects of fires on streamwater quality are most likely to occur if the fire was severe enough to burn large amounts of organic matter, if windy conditions were present during the fire, if heavy rain occurred following the fire, and if the fire occurred in a watershed with steep slopes and soils with little cation-exchange capacity. Measurable effects of fires on lake- and reservoir-water quality are most likely to occur if, in addition to the factors listed for streams, the lake or reservoir is oligotrophic or mesotrophic and the residence time of water in the lake or reservoir is short relative to the length of time elevated concentrations of nutrients occur in runoff. Knowledge of whether a lake or reservoir is nitrogen or phosphorus limited is important because eutrophication of nitrogen-limited lakes may occur following a fire due to increasing nitrogen:phosphorus ratios caused by prolonged increases of nitrogen concentrations, especially nitrate.","language":"ENGLISH","doi":"10.3133/ofr20041296","usgsCitation":"Ranalli, A.J., 2004, A summary of the scientific literature on the effects of fire on the concentration of nutrients in surface waters (Online Only): U.S. Geological Survey Open-File Report 2004-1296, 23 p., https://doi.org/10.3133/ofr20041296.","productDescription":"23 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":5857,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr2004-1296/","linkFileType":{"id":5,"text":"html"}},{"id":185204,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Online Only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a5f2f","contributors":{"authors":[{"text":"Ranalli, Anthony J. tranalli@usgs.gov","contributorId":1195,"corporation":false,"usgs":true,"family":"Ranalli","given":"Anthony","email":"tranalli@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":257916,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":57811,"text":"ofr20041283 - 2004 - Proceedings of the twentieth annual meeting of the Society for Organic Petrology","interactions":[],"lastModifiedDate":"2022-06-15T19:52:33.975934","indexId":"ofr20041283","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2004-1283","title":"Proceedings of the twentieth annual meeting of the Society for Organic Petrology","docAbstract":"The Society for Organic Petrology (TSOP; pronounced \"Tee'-sop\") was established in 1984 to consolidate and foster the organizational activities of scientists and engineers involved with coal petrology, kerogen petrology, organic geochemistry, and related disciplines. The following report, \"Proceedings of the Twentieth Annual Meeting of The Society for Organic Petrology\" (ISSN 1060-7250), features technical talks, poster presentations, business meetings, short courses, and field trips from the Fall 2003 annual meeting held in Washington, D.C.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20041283","usgsCitation":"2004, Proceedings of the twentieth annual meeting of the Society for Organic Petrology (Version 1.0): U.S. Geological Survey Open-File Report 2004-1283, 126 p., https://doi.org/10.3133/ofr20041283.","productDescription":"126 p.","costCenters":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":184709,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":402235,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_68866.htm","linkFileType":{"id":5,"text":"html"}},{"id":5789,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1283/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db660372","contributors":{"compilers":[{"text":"Karlsen, Alex W.","contributorId":78789,"corporation":false,"usgs":true,"family":"Karlsen","given":"Alex W.","affiliations":[],"preferred":false,"id":727899,"contributorType":{"id":3,"text":"Compilers"},"rank":1}],"editors":[{"text":"Bragg, Linda J.","contributorId":103717,"corporation":false,"usgs":true,"family":"Bragg","given":"Linda","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":727894,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Lentz, Erika E. elentz@usgs.gov","contributorId":167611,"corporation":false,"usgs":true,"family":"Lentz","given":"Erika","email":"elentz@usgs.gov","middleInitial":"E.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":727895,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Warwick, Peter D. 0000-0002-3152-7783 pwarwick@usgs.gov","orcid":"https://orcid.org/0000-0002-3152-7783","contributorId":762,"corporation":false,"usgs":true,"family":"Warwick","given":"Peter","email":"pwarwick@usgs.gov","middleInitial":"D.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":727896,"contributorType":{"id":2,"text":"Editors"},"rank":3},{"text":"Finkelman, Robert B.","contributorId":38138,"corporation":false,"usgs":false,"family":"Finkelman","given":"Robert B.","affiliations":[{"id":6643,"text":"University of California - Berkeley","active":true,"usgs":false}],"preferred":false,"id":727897,"contributorType":{"id":2,"text":"Editors"},"rank":4},{"text":"Trippi, Michael H. 0000-0002-1398-3427 mtrippi@usgs.gov","orcid":"https://orcid.org/0000-0002-1398-3427","contributorId":941,"corporation":false,"usgs":true,"family":"Trippi","given":"Michael","email":"mtrippi@usgs.gov","middleInitial":"H.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":727898,"contributorType":{"id":2,"text":"Editors"},"rank":5}]}} ,{"id":57804,"text":"ofr20041201 - 2004 - Hydraulic conductivity of near-surface alluvium in the vicinity of Cattlemans Detention Basin, South Lake Tahoe, California","interactions":[],"lastModifiedDate":"2012-02-02T00:12:21","indexId":"ofr20041201","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2004-1201","title":"Hydraulic conductivity of near-surface alluvium in the vicinity of Cattlemans Detention Basin, South Lake Tahoe, California","docAbstract":"Cattlemans detention basin, South Lake Tahoe, California is designed to capture and reduce urban runoff and pollutants originating from developed areas before entering Cold Creek, which is tributary to Trout Creek and to Lake Tahoe. The effectiveness of the basin in reducing sediment and nutrient loads currently is being assessed with a five-year study. Hydraulic conductivity of the alluvium near the detention basin is needed to estimate ground-water flow and subsurface nutrient transport. Hydraulic conductivity was estimated using slug tests in 27 monitoring wells that surround the detention basin. For each test, water was poured rapidly into a well, changes in water-level were monitored, and the observed changes were analyzed using the Bouwer and Rice method. Each well was tested one to four times. A total of 24 wells were tested more than once. Of the 24 wells, the differences among the tests were within 10 percent of the average. Estimated hydraulic conductivities of basin alluvium range from 0.5 to 70 feet per day with an average of 17.8 feet per day. This range is consistent with the sandy alluvial deposits observed in the area of Cattlemans detention basin.","language":"ENGLISH","doi":"10.3133/ofr20041201","usgsCitation":"Green, J.M., Henkelman, K.K., and Caskey, R.M., 2004, Hydraulic conductivity of near-surface alluvium in the vicinity of Cattlemans Detention Basin, South Lake Tahoe, California: U.S. Geological Survey Open-File Report 2004-1201, 18 p., https://doi.org/10.3133/ofr20041201.","productDescription":"18 p.","costCenters":[],"links":[{"id":5764,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr2004-1201/","linkFileType":{"id":5,"text":"html"}},{"id":184119,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a2f1","contributors":{"authors":[{"text":"Green, Jena M.","contributorId":77597,"corporation":false,"usgs":true,"family":"Green","given":"Jena","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":257839,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Henkelman, Katherine K.","contributorId":26751,"corporation":false,"usgs":true,"family":"Henkelman","given":"Katherine","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":257837,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Caskey, Rachel M.","contributorId":74817,"corporation":false,"usgs":true,"family":"Caskey","given":"Rachel","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":257838,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":57778,"text":"ofr20041250 - 2004 - Flood of June 4-5, 2002, in the Maquoketa River Basin, east-central Iowa","interactions":[],"lastModifiedDate":"2016-02-01T12:58:46","indexId":"ofr20041250","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2004","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":"2004-1250","title":"Flood of June 4-5, 2002, in the Maquoketa River Basin, east-central Iowa","docAbstract":"Severe flooding occurred on June 4-5, 2002, in the Maquoketa River Basin in Delaware, Dubuque, Jackson, and Jones Counties, following thunderstorm activity over east-central Iowa. The rain gage at Cascade, Iowa, recorded a 14-hour rainfall of 6.0 inches at noon on June 4. Radar indications estimated as much as 8 to 10 inches of rain fell in the upper-middle part of the Maquoketa River Basin. Peak discharges on the Maquoketa River at Monticello of 47,500 cubic feet per second (recurrence interval estimated to be greater than 500 years as computed using flood-estimation equations developed by the U.S. Geological Survey), and at the Maquoketa River near Maquoketa streamflow-gaging station of 47,900 cubic feet per second (recurrence interval about 50 years), were determined for the flood. The peak discharge of the 2002 flood is nearly equal that of the 1944 flood (48,000 cubic feet per second), the largest flood on record in the Maquoketa River Basin. The 2002 flood is the largest known flood in the North Fork Maquoketa River Basin. A peak discharge of 22,600 cubic feet per second (recurrence interval about 110 years) was determined for the flood at the North Fork Maquoketa River near Fulton gaging station. Information about the basin and flood history, the 2002 thunderstorms and associated flooding, and a profile of high-water marks are presented for selected reaches along the Maquoketa and North Fork Maquoketa Rivers.
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\"}}]}","edition":"3rd Edition","tableOfContents":"Abstract
Introduction
Acknowledgments
Basin Description
Flood History
Flood of June 15, 1925
Flood of June 27, 1944
Flood of June 13, 1947
Flood of June 4-5, 2002
Storm Description
Flood Description
Flood Profile
Summary
References
Appendix: Temporary Bench Marks and Reference Points
The Comprehensive Everglades Restoration Plan (CERP) lists restoration of the timing, quantity, and quality of the natural flow of freshwater as one its primary goals. Before restoration can occur, however, the baseline conditions of the environment prior to significant human alteration must be established and the range of variation within the natural system must be determined. In addition, the response of the system to human alterations during the 20th century should be evaluated. Resource managers can use this information to establish targets and performance measures for restoration and to predict the system's response to changes invoked by restoration.
The objectives of the U.S. Geological Survey’s Ecosystem History of Biscayne Bay research project are to examine historical changes in the Biscayne Bay ecosystem at selected sites on a decadal-centennial scale and to correlate these changes with natural events and anthropogenic alterations in the South Florida region. Specific emphasis is being placed on historical changes to (1) amount, timing, and sources of freshwater influx and the resulting effects on salinity and water quality; (2) shoreline and sub-aquatic vegetation; and (3) the relationship between sea-level change, onshore vegetation, and salinity.
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Submarine ground-water discharge (SGD) has recently been recognized as a phenomenon that can strongly influence coastal water and geochemical budgets and drive ecosystem change. For example, the discharge of nutrient-enriched ground water into coastal waters may contribute significantly to eutrophication and blooms of harmful algae. Similarly, the quantity of SGD can also directly affect the availability of fresh water to coastal communities, impact fragile coastal ecosystems such as estuaries and coral reefs, and influence geomorphology of shoreline features.
Moore raised awareness of the global importance of SGD and much effort has been devoted to developing new tracer techniques and methods for the identification and quantification of SGD. Because the discharge of coastal ground water commonly occurs as diffuse seepage rather than focused discharge through identifiable springs, assessing SGD has remained difficult for both oceanographers and hydrologists. Through national and international research programs, Burnett, Moore, Charette, and others have developed a rigorous, systematic approach for quantifying SGD using a wide assortment of tracers and methods. Intercalibration experiments, such as those conducted in coastal waters off Australia, Brazil, and Long Island, NY, demonstrate that careful measurements can accurately quantify SGD, confirm some of the driving mechanisms (e.g. climatic and tidal forcing), and constrain the spatial and temporal scales at which these mechanisms operate. Now that approaches for rigorously quantifying SGD are becoming better established, scientists can now begin to investigate the wide variety of coastal processes affected by SGD.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20041226","usgsCitation":"Swarzenski, P.W., Bratton, J.F., and Crusius, J., 2004, Submarine ground-water discharge and its role in coastal processes and ecosystems: U.S. Geological Survey Open-File 2004–1226, 4 p., https://doi.org/10.3133/ofr20041226.","productDescription":"4 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":185309,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2004/1226/coverthb.jpg"},{"id":362212,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2004/1226/ofr20041226.pdf","text":"Report","size":"812 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.74951171875,\n 25.54244147012483\n ],\n [\n -82.33154296875,\n 27.68352808378776\n ],\n [\n -82.529296875,\n 29.32472016151103\n ],\n [\n -83.6279296875,\n 30.20211367909724\n ],\n [\n -83.95751953125,\n 29.516110386062277\n ],\n [\n -82.96875,\n 28.748396571187406\n ],\n [\n -83.0126953125,\n 27.664068965384516\n ],\n [\n -81.97998046875,\n 25.740529092773226\n ],\n [\n -80.92529296875,\n 24.78673454198888\n ],\n [\n -79.716796875,\n 24.986058021167594\n ],\n [\n -79.6728515625,\n 27.196014383173306\n ],\n [\n -80.96923828125,\n 30.637912028341123\n ],\n [\n -78.31054687499999,\n 33.5963189611327\n ],\n [\n -76.552734375,\n 34.488447837809304\n ],\n [\n -74.77294921875,\n 35.96022296929667\n ],\n [\n -75.21240234375,\n 37.33522435930639\n ],\n [\n -74.02587890625,\n 39.53793974517628\n ],\n [\n -72.97119140625,\n 40.43022363450862\n ],\n [\n -71.54296874999999,\n 40.68063802521456\n ],\n [\n -70.51025390625,\n 41.1455697310095\n ],\n [\n -69.67529296875,\n 41.178653972331674\n ],\n [\n -69.76318359375,\n 42.17968819665961\n ],\n [\n -71.1474609375,\n 42.293564192170095\n ],\n [\n -73.49853515625,\n 41.42625319507269\n ],\n [\n -74.6630859375,\n 40.44694705960048\n ],\n [\n -75.08056640625,\n 39.58875727696545\n ],\n [\n -76.09130859375,\n 39.8928799002948\n ],\n [\n -77.18994140625,\n 38.238180119798635\n ],\n [\n -76.75048828125,\n 36.66841891894786\n ],\n [\n -77.2119140625,\n 35.28150065789119\n ],\n [\n -79.47509765625,\n 33.706062655101206\n ],\n [\n -81.298828125,\n 32.24997445586331\n ],\n [\n -82.08984375,\n 30.939924331023445\n ],\n [\n -81.23291015625,\n 28.246327971048842\n ],\n [\n -80.2001953125,\n 26.745610382199022\n ],\n [\n -80.74951171875,\n 25.54244147012483\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"Caribbean-Florida Water Science Center
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The Iowa ground-water-quality monitoring program has been conducted cooperatively since 1982 by the Iowa Department of Natural Resources, Iowa Geological Survey; the University of Iowa Hygienic Laboratory; and the U.S. Geological Survey. The original objectives of the program were to provide baseline ground-water-quality data throughout the State for the major aquifers and to address any new areas of water-quality concern. Since the program began, the emphasis and objectives of the program have changed several times. As of 1992, greater emphasis has been placed on determining trends in ground-water quality and correlating water quality with possible contributing factors such as location, land use, aquifer, aquifer depth, and precipitation.
\nFrom 1997 through 2002, a total of 471 samples of untreated water have been collected from 154 municipal wells throughout Iowa. The samples, collected from six different aquifers, consisted of 192 alluvial aquifer samples (36 wells), 79 Pleistocene aquifer samples (16 wells), 52 Cretaceous aquifer samples (35 wells), 48 Carboniferous aquifer samples (30 wells), 54 Silurian-Devonian aquifer samples (19 wells), and 46 Cambrian-Ordovician aquifer samples (18 wells).
\nSome samples had concentrations greater than or equal to the respective Maximum Contaminant Levels for drinking water established by the U.S. Environmental Protection Agency. Of 471 samples analyzed, 19 samples had concentrations greater than or equal to the Maximum Contaminant Level for sulfate; 31 samples had concentrations greater than or equal to the Maximum Contaminant Level for nitrite plus nitrate; 257 samples had concentrations greater than or equal to the Secondary Maximum Contaminant Level for iron; and 249 samples had concentrations greater than or equal to the Secondary Maximum Contaminant Level for manganese. Of the 443 samples analyzed for pesticides, 87 samples had concentrations greater than or equal to the respective minimum reporting levels for the parent compounds, 30 samples had concentrations greater than or equal to the respective minimum reporting levels for pesticide metabolites, and 26 samples had detectable concentrations (censored values) less than the minimum reporting levels. Concentrations of alachlor, atrazine, cyanazine, and metolachlor accounted for about 90 percent of the samples equal to or exceeding the respective minimum reporting levels for pesticides. No samples had pesticide concentrations greater than the respective Maximum Contaminant or Health Advisory Levels.
\nThe compact disc included with this report has information about water-quality properties and concentrations of dissolved solids, major ions, nutrients, trace elements, radionuclides, total organic carbon, pesticides, and synthetic organic compounds for water years 1997 through 2002.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20041048","collaboration":"Prepared in cooperation with the Iowa Department of Natural Resources, Iowa Geological Survey, and the University of Iowa Hygienic Laboratory","usgsCitation":"Littin, G.R., 2004, Quality of ground water for selected municipal water supplies in Iowa, 1997–2002 water years: U.S. Geological Survey Open-File Report 2004-1048, Report: vi, 36 p.; Appendixes, https://doi.org/10.3133/ofr20041048.","productDescription":"Report: vi, 36 p.; Appendixes","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":423450,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_69893.htm","linkFileType":{"id":5,"text":"html"}},{"id":5797,"rank":4,"type":{"id":15,"text":"Index 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U.S. Geological Survey
400 South Clinton Street, Suite 269
Iowa City, IA 52240
Preface
Abstract
Introduction
Purpose and Scope
Description of Iowa Ground-Water Quality Monitoring Program
Municipal Wells
Sample Collection and Analysis
Description of Aquifers
Alluvial Aquifers
Pleistocene Aquifers
Cretaceous Aquifers
Carboniferous Aquifers
Silurian-Devonian Aquifers
Cambrian-Ordovician Aquifers
Precambrian Aquifer
Quality of Ground Water
Sulfate
Nitrite Plus Nitrate
Arsenic
Iron
Manganese
Alachlor, Atrazine, Cyanazine, and Metolachlor
Organization of the Water-Quality Data on the Compact Disc
Summary
References Cited
Supplemental Information
No abstract available.
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