No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0140","usgsCitation":"Aycock, R.A., and Haugh, C.J., 2001, Ground-water hydrology and water-quality data for wells, springs, and surface-water sites in the Bradley-Brumalow creeks area near Arnold Air Force Base, Tennessee, September to December 1999: U.S. Geological Survey Open-File Report 2001-40, iv, 49 p., https://doi.org/10.3133/ofr0140.","productDescription":"iv, 49 p.","costCenters":[],"links":[{"id":160888,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":390528,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_37346.htm"},{"id":2746,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr01-040/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Tennessee","otherGeospatial":"Bradley-Brumalow Creeks area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -86.1386489868164,\n 35.294952147406576\n ],\n [\n -85.98037719726562,\n 35.294952147406576\n ],\n [\n -85.98037719726562,\n 35.47744667178578\n ],\n [\n -86.1386489868164,\n 35.47744667178578\n ],\n [\n -86.1386489868164,\n 35.294952147406576\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668d0e","contributors":{"authors":[{"text":"Aycock, Robert A.","contributorId":75976,"corporation":false,"usgs":true,"family":"Aycock","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":205337,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haugh, Connor J. 0000-0002-5204-8271 cjhaugh@usgs.gov","orcid":"https://orcid.org/0000-0002-5204-8271","contributorId":3932,"corporation":false,"usgs":true,"family":"Haugh","given":"Connor","email":"cjhaugh@usgs.gov","middleInitial":"J.","affiliations":[{"id":581,"text":"Tennessee Water Science Center","active":true,"usgs":true}],"preferred":true,"id":205336,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":31212,"text":"ofr0135 - 2001 - Hydraulic and mechanical properties affecting ground-water flow and aquifer-system compaction, San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:09:06","indexId":"ofr0135","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","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":"2001-35","title":"Hydraulic and mechanical properties affecting ground-water flow and aquifer-system compaction, San Joaquin Valley, California","docAbstract":"This report summarizes hydraulic and mechanical properties affecting ground-water flow and aquifer-system compaction in the San Joaquin Valley, a broad alluviated intermontane structural trough that constitutes the southern two-thirds of the Central Valley of California. These values will be used to constrain a coupled ground-water flow and aquifer-system compaction model of the western San Joaquin Valley called WESTSIM. A main objective of the WESTSIM model is to evaluate potential future land subsidence that might occur under conditions in which deliveries of imported surface water for agricultural use are reduced and ground-water pumping is increased. Storage values generally are components of the total aquifer-system storage and include inelastic and elastic skeletal storage values of the aquifers and the aquitards that primarily govern the potential amount of land subsidence. Vertical hydraulic conductivity values generally are for discrete thicknesses of sediments, usually aquitards, that primarily govern the rate of land subsidence. The data were compiled from published sources and include results of aquifer tests, stress-strain analyses of borehole extensometer observations, laboratory consolidation tests, and calibrated models of aquifer-system compaction.","language":"ENGLISH","doi":"10.3133/ofr0135","usgsCitation":"Sneed, M., 2001, Hydraulic and mechanical properties affecting ground-water flow and aquifer-system compaction, San Joaquin Valley, California: U.S. Geological Survey Open-File Report 2001-35, 26 p., https://doi.org/10.3133/ofr0135.","productDescription":"26 p.","costCenters":[],"links":[{"id":2745,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr01035","linkFileType":{"id":5,"text":"html"}},{"id":160887,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629b78","contributors":{"authors":[{"text":"Sneed, Michelle 0000-0002-8180-382X micsneed@usgs.gov","orcid":"https://orcid.org/0000-0002-8180-382X","contributorId":155,"corporation":false,"usgs":true,"family":"Sneed","given":"Michelle","email":"micsneed@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":205335,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":31229,"text":"ofr0167 - 2001 - A comparative analysis of hazard models for predicting debris flows in Madison County, Virginia","interactions":[],"lastModifiedDate":"2021-12-01T22:24:22.681164","indexId":"ofr0167","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","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":"2001-67","title":"A comparative analysis of hazard models for predicting debris flows in Madison County, Virginia","docAbstract":"During the rainstorm of June 27, 1995, roughly 330-750 mm of rain fell within a sixteen-hour period, initiating floods and over 600 debris flows in a small area (130 km2) of Madison County, Virginia. Field studies showed that the majority (70%) of these debris flows initiated with a thickness of 0.5 to 3.0 m in colluvium on slopes from 17 o to 41 o (Wieczorek et al., 2000). This paper evaluated and compared the approaches of SINMAP, LISA, and Iverson's (2000) transient response model for slope stability analysis by applying each model to the landslide data from Madison County. Of these three stability models, only Iverson's transient response model evaluated stability conditions as a function of time and depth. Iverson?s model would be the preferred method of the three models to evaluate landslide hazards on a regional scale in areas prone to rain-induced landslides as it considers both the transient and spatial response of pore pressure in its calculation of slope stability. The stability calculation used in SINMAP and LISA is similar and utilizes probability distribution functions for certain parameters. Unlike SINMAP that only considers soil cohesion, internal friction angle and rainfall-rate distributions, LISA allows the use of distributed data for all parameters, so it is the preferred model to evaluate slope stability over SINMAP. Results from all three models suggested similar soil and hydrologic properties for triggering the landslides that occurred during the 1995 storm in Madison County, Virginia. The colluvium probably had cohesion of less than 2KPa. The root-soil system is above the failure plane and consequently root strength and tree surcharge had negligible effect on slope stability. The result that the final location of the water table was near the ground surface is supported by the water budget analysis of the rainstorm conducted by Smith et al. (1996).","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0167","usgsCitation":"Morrissey, M.M., Wieczorek, G.F., and Morgan, B.A., 2001, A comparative analysis of hazard models for predicting debris flows in Madison County, Virginia (Version 1.0): U.S. Geological Survey Open-File Report 2001-67, HTML Document; CD-ROM, https://doi.org/10.3133/ofr0167.","productDescription":"HTML Document; CD-ROM","costCenters":[],"links":[{"id":161344,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":392351,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_37337.htm"},{"id":2799,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/ofr-01-0067/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Virginia","county":"Madison County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -78.5,\n 38.333\n ],\n [\n -78.333,\n 38.333\n ],\n [\n -78.333,\n 38.55\n ],\n [\n -78.5,\n 38.55\n ],\n [\n -78.5,\n 38.333\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4993e4b0b290850ef46c","contributors":{"authors":[{"text":"Morrissey, Meghan M.","contributorId":98765,"corporation":false,"usgs":true,"family":"Morrissey","given":"Meghan","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":205390,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wieczorek, Gerald F.","contributorId":81889,"corporation":false,"usgs":true,"family":"Wieczorek","given":"Gerald","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":205389,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morgan, Benjamin A.","contributorId":32158,"corporation":false,"usgs":true,"family":"Morgan","given":"Benjamin","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":205388,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":31270,"text":"ofr2001135 - 2001 - Basin-centered gas systems of the U.S.","interactions":[],"lastModifiedDate":"2021-11-23T23:24:02.073468","indexId":"ofr2001135","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","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":"2001-135","title":"Basin-centered gas systems of the U.S.","docAbstract":"Basin-center accumulations, a type of continuous accumulation, have spatial dimensions equal to or exceeding those of conventional oil and gas accumulations, but unlike conventional fields, cannot be represented in terms of discrete, countable units delineated by downdip hydrocarbon-water contacts. Common geologic and production characteristics of continuous accumulations include their occurrence downdip from water-saturated rocks, lack of traditional trap or seal, relatively low matrix permeability, abnormal pressures (high or low), local interbedded source rocks, large in-place hydrocarbon volumes, and low recovery factors.\r\n\r\nThe U.S. Geological Survey, in cooperation with the U.S. Department of Energy, National Energy Technology Laboratory, Morgantown, West Virginia, is currently re-evaluating the resource potential of basin-center gas accumulations in the U.S. in light of changing geologic perceptions about these accumulations (such as the role of subtle structures to produce sweet spots), and the availability of new data. Better geologic understanding of basin-center gas accumulations could result in new plays or revised plays relative to those of the U.S. Geological Survey 1995 National Assessment (Gautier and others, 1995).\r\n\r\nFor this study, 33 potential basin-center gas accumulations throughout the U.S. were identified and characterized based on data from the published literature and from well and reservoir databases (Figure 1). 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E.","contributorId":92741,"corporation":false,"usgs":true,"family":"Bartberger","given":"Charles","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":205536,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":31252,"text":"ofr01102 - 2001 - Vegetative resistance to flow in South Florida: Summary of vegetation sampling in Taylor Slough, Everglades National Park, September 1997–July 1998","interactions":[],"lastModifiedDate":"2025-04-23T15:55:32.798402","indexId":"ofr01102","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","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":"2001-102","title":"Vegetative resistance to flow in South Florida: Summary of vegetation sampling in Taylor Slough, Everglades National Park, September 1997–July 1998","docAbstract":"The U.S. Geological Survey is one of many agencies providing scientific support to the effort to restore the South Florida Everglades. In September and November 1997 and July 1998, vegetation was sampled at selected sites in the Everglades as part of a study to quantify vegetative resistance to flow. The objectives of the vegetation sampling are (1) to provide detailed information on species composition, vegetation characteristics, and biomass for quantification of the effect of vegetation on water flow, and (2) to use these data in the future to infer flow resistance from vegetation information. Forty-two vegetation quadrats were sampled in Taylor Slough to determine the number and width of stems and leaves and the biomass of live and dead standing sawgrass, rush, and other plants, and the biomass of dead litter and periphyton. The samples were grouped into ten vegetation classes based on species composition and total biomass minus periphyton biomass.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr01102","productDescription":"vii, 59 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":391837,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_40461.htm"},{"id":160866,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2001/0102/report-thumb.jpg"},{"id":59712,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0102/report.pdf","text":"Report","size":"9 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2001-102"}],"country":"United States","state":"Florida","otherGeospatial":"Everglades National Park, Taylor Slough","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.833,\n 25.167\n ],\n [\n -80.467,\n 25.167\n ],\n [\n -80.467,\n 25.417\n ],\n [\n -80.833,\n 25.417\n ],\n [\n -80.833,\n 25.167\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"Caribbean-Florida Water Science Center
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The calibration of a model of flow, temperature, and water quality in the Tualatin River, Oregon, originally calibrated for the summers of 1991 through 1993, was extended to the summers of 1991 through 1997. The model is now calibrated for a total period of 42 months during the May through October periods of 7 hydrologically distinct years. Based on a modified version of the U.S. Army Corps of Engineers model CE-QUAL-W2, this model provides a good fit to the measured data for streamflow, water temperature, and water quality constituents such as chloride, ammonia, nitrate, total phosphorus, orthophosphate, phytoplankton, and dissolved oxygen. In particular, the model simulates ammonia concentrations and the effects of instream ammonia nitrification very well, which is critical to ongoing efforts to revise ammonia regulations for the Tualatin River. In addition, the model simulates the timing, duration, and relative size of algal blooms with sufficient accuracy to provide important insights for regulators and managers of this river.Efforts to limit the size of algal blooms through phosphorus control measures are apparent in the model simulations, which show this limitation on algal growth. Such measures are largely responsible for avoiding violations of the State of Oregon maximum pH standard of 8.5 in recent years, but they have not yet reduced algal biomass levels below the State of Oregon nuisance phytoplankton growth guideline of 15 ?g/L chlorophyll-a.Most of the dynamics of the instream dissolved oxygen concentrations are captured by the model. About half of the error in the simulated dissolved oxygen concentrations is directly attributable to error in the size of the simulated phytoplankton population. To achieve greater accuracy in simulating dissolved oxygen, therefore, it will be necessary to increase accuracy in the simulation of Tualatin River phytoplankton.Future efforts may include the introduction of multiple algal groups in the model. This model of the Tualatin River continues to be used as a quantitative tool to aid in the management of this important resource.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/wri014041","collaboration":"Prepared in cooperation with the Unified Sewerage Agency of Washington County, Oregon","usgsCitation":"Rounds, S.A., and Wood, T.M., 2001, Modeling water quality in the Tualatin River, Oregon, 1991-1997: U.S. Geological Survey Water-Resources Investigations Report 2001-4041, v, 53 p., https://doi.org/10.3133/wri014041.","productDescription":"v, 53 p.","numberOfPages":"60","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":160731,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri014041.PNG"},{"id":311371,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2001/4041/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Oregon","otherGeospatial":"Tualaltin River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -91.1700439453125,\n 32.55144352864431\n ],\n [\n -91.1700439453125,\n 32.55144352864431\n ],\n [\n -91.16455078125,\n 32.55144352864431\n ],\n [\n -91.16455078125,\n 32.55144352864431\n ],\n [\n -91.1700439453125,\n 32.55144352864431\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -123.57421875,\n 45.00365115687189\n ],\n [\n -123.57421875,\n 45.85176048817254\n ],\n [\n -122.178955078125,\n 45.85176048817254\n ],\n [\n -122.178955078125,\n 45.00365115687189\n ],\n [\n -123.57421875,\n 45.00365115687189\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699763","contributors":{"authors":[{"text":"Rounds, Stewart A. 0000-0002-8540-2206 sarounds@usgs.gov","orcid":"https://orcid.org/0000-0002-8540-2206","contributorId":905,"corporation":false,"usgs":true,"family":"Rounds","given":"Stewart","email":"sarounds@usgs.gov","middleInitial":"A.","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":204329,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, Tamara M. 0000-0001-6057-8080 tmwood@usgs.gov","orcid":"https://orcid.org/0000-0001-6057-8080","contributorId":1164,"corporation":false,"usgs":true,"family":"Wood","given":"Tamara","email":"tmwood@usgs.gov","middleInitial":"M.","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":204330,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":31261,"text":"ofr01117 - 2001 - Magnetotelluric data across the Battle Mountain-Eureka and Carlin trends, north of Cortez, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:09:04","indexId":"ofr01117","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","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":"2001-117","title":"Magnetotelluric data across the Battle Mountain-Eureka and Carlin trends, north of Cortez, Nevada","language":"ENGLISH","doi":"10.3133/ofr01117","usgsCitation":"Williams, J.M., Rodriguez, B.D., and Klein, D.P., 2001, Magnetotelluric data across the Battle Mountain-Eureka and Carlin trends, north of Cortez, Nevada (Version 1.0): U.S. Geological Survey Open-File Report 2001-117, 154 p., https://doi.org/10.3133/ofr01117.","productDescription":"154 p.","costCenters":[],"links":[{"id":160366,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2890,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/ofr-01-0117/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649411","contributors":{"authors":[{"text":"Williams, Jackie M.","contributorId":11217,"corporation":false,"usgs":true,"family":"Williams","given":"Jackie","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":205510,"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":205509,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Klein, Douglas P.","contributorId":50896,"corporation":false,"usgs":true,"family":"Klein","given":"Douglas","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":205511,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":31280,"text":"ofr01158 - 2001 - Laboratory measurements of electrical properties of composite mine dump samples from Colorado and New Mexico","interactions":[],"lastModifiedDate":"2025-01-14T14:27:15.46296","indexId":"ofr01158","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","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":"2001-158","title":"Laboratory measurements of electrical properties of composite mine dump samples from Colorado and New Mexico","docAbstract":"Individual mine waste samples were collected and combined to form one composite sample at each of eight mine dump sites in Colorado and New Mexico. The samples were air-dried and sieved to determine the geochemical composition of their <2mm size fraction. Splits of the samples were then rehydrated and their electrical properties were measured in the US Geological Survey Petrophysical Laboratory, Denver, Colorado (PetLab). The PetLab measurements were done twice: in 1999, using convenient amounts of rehydration water ranging from 5% to 8%; and in 2000, using carefully controlled rehydrations to 5% and 10% water. This report gives geochemical analyses of the <2mm size fraction of the composite samples (Appendix A), PetLab graphs of the 1999 measurements (Appendix B), Petlab graphs of the 2000 measurements (Appendix C), and Cole-Cole models of the PetLab data from the 2000 measurements (Appendix D).","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr01158","usgsCitation":"Anderson, A.L., Campbell, D.L., and Beanland, S., 2001, Laboratory measurements of electrical properties of composite mine dump samples from Colorado and New Mexico (Version 1.0): U.S. Geological Survey Open-File Report 2001-158, 55 p., https://doi.org/10.3133/ofr01158.","productDescription":"55 p.","costCenters":[],"links":[{"id":160189,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2904,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/ofr-01-0158/","linkFileType":{"id":5,"text":"html"}},{"id":391589,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_39549.htm","text":"Leadville, CO area","linkFileType":{"id":5,"text":"html"}},{"id":466183,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_39550.htm","text":"Silverton, CO area","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado","city":"Leadville, Silverton","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.283,\n 39.239\n ],\n [\n -106.197,\n 39.239\n ],\n [\n -106.197,\n 39.267\n ],\n [\n -106.283,\n 39.267\n ],\n [\n -106.283,\n 39.239\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -107.699,\n 37.87805429381186\n ],\n [\n -107.699,\n 37.79022985684327\n ],\n [\n -107.61758505688162,\n 37.79022985684327\n ],\n [\n -107.61758505688162,\n 37.87805429381186\n ],\n [\n -107.699,\n 37.87805429381186\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b44f7","contributors":{"authors":[{"text":"Anderson, Anita L.","contributorId":55482,"corporation":false,"usgs":true,"family":"Anderson","given":"Anita","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":205566,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, David L.","contributorId":95447,"corporation":false,"usgs":true,"family":"Campbell","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":205567,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Beanland, Shay","contributorId":11244,"corporation":false,"usgs":true,"family":"Beanland","given":"Shay","affiliations":[],"preferred":false,"id":205565,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":31294,"text":"ofr2001183 - 2001 - Simple Techniques For Assessing Impacts Of Oil And Gas Operations On Public Lands: A Field Evaluation Of A Photoionization Detector (PID) At A Condensate Release Site, Padre Island National Seashore, Texas","interactions":[],"lastModifiedDate":"2017-02-21T13:30:34","indexId":"ofr2001183","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","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":"2001-183","title":"Simple Techniques For Assessing Impacts Of Oil And Gas Operations On Public Lands: A Field Evaluation Of A Photoionization Detector (PID) At A Condensate Release Site, Padre Island National Seashore, Texas","docAbstract":"Simple, cost-effective techniques are needed for land managers to assess the environmental impacts of oil and gas production activities on public lands, so that sites may be prioritized for remediation or for further, more formal assessment. Field-portable instruments provide real-time data and allow the field investigator to extend an assessment beyond simply locating and mapping obvious disturbances. Field investigators can examine sites for the presence of hydrocarbons in the subsurface using a soil auger and a photoionization detector (PID). The PID measures volatile organic compounds (VOC) in soil gases. This allows detection of hydrocarbons in the shallow subsurface near areas of obvious oil-stained soils, oil in pits, or dead vegetation. Remnants of a condensate release occur in sandy soils at a production site on the Padre Island National Seashore in south Texas. Dead vegetation had been observed by National Park Service personnel in the release area several years prior to our visit. The site is located several miles south of the Malaquite Beach Campground. In early 2001, we sampled soil gases for VOCs in the area believed to have received the condensate. Our purpose in this investigation was: 1) to establish what sampling techniques might be effective in sandy soils with a shallow water and contrast them with techniques used in an earlier study; and 2) delineate the probable area of condensate release. Our field results show that sealing the auger hole with a clear, rigid plastic tube capped at the top end and sampling the soil gas through a small hole in the cap increases the soil VOC gas signature, compared to sampling soil gases in the bottom of an open hole. This sealed-tube sampling method increases the contrast between the VOC levels within a contaminated area and adjacent background areas. The tube allows the PID air pump to draw soil gas from the volume of soil surrounding the open hole below the tube in a zone less influenced by atmospheric air. In an open hole, the VOC readings seem to be strongly dependent on the degree of diffusion and advection of soil gas VOCs into the open hole from the surrounding soil, a process that may vary with soil and wind conditions. Making measurements with the sealed hole does take some additional time (4-7 minutes after the hole is augered) compared to the open-hole technique (1-2 minutes). We used the rigid-plastic tube technique to survey for soil gas VOCs across the entire site, less than ? acre. Condensate has impacted at least 0.28 acres. The impacted area may extend northwest of the surveyed area.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr2001183","usgsCitation":"Otton, J.K., and Zielinski, R.A., 2001, Simple Techniques For Assessing Impacts Of Oil And Gas Operations On Public Lands: A Field Evaluation Of A Photoionization Detector (PID) At A Condensate Release Site, Padre Island National Seashore, Texas: U.S. Geological Survey Open-File Report 2001-183, 27 p., https://doi.org/10.3133/ofr2001183.","productDescription":"27 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":161262,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2931,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/ofr-01-183/","linkFileType":{"id":1,"text":"pdf"}},{"id":12511,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/ofr-01-183/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f3a11","contributors":{"authors":[{"text":"Otton, James K. jkotton@usgs.gov","contributorId":1170,"corporation":false,"usgs":true,"family":"Otton","given":"James","email":"jkotton@usgs.gov","middleInitial":"K.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":205600,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zielinski, Robert A. 0000-0002-4047-5129 rzielinski@usgs.gov","orcid":"https://orcid.org/0000-0002-4047-5129","contributorId":1593,"corporation":false,"usgs":true,"family":"Zielinski","given":"Robert","email":"rzielinski@usgs.gov","middleInitial":"A.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":205601,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":30886,"text":"wri20004262 - 2001 - Factors affecting reservoir and stream-water quality in the Cambridge, Massachusetts, drinking-water source area and implications for source-water protection","interactions":[],"lastModifiedDate":"2022-05-18T18:37:09.153254","indexId":"wri20004262","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2000-4262","title":"Factors affecting reservoir and stream-water quality in the Cambridge, Massachusetts, drinking-water source area and implications for source-water protection","docAbstract":"This report presents the results of a study conducted by the U.S. Geological Survey, in cooperation with the city of Cambridge, Massachusetts, Water Department, to assess reservoir and tributary-stream quality in the Cambridge drinking-water source area, and to use the information gained to help guide the design of a comprehensive water-quality monitoring program for the source area. Assessments of the quality and trophic state of the three primary storage reservoirs, Hobbs Brook Reservoir, Stony Brook Reservoir, and Fresh Pond, were conducted (September 1997-November 1998) to provide baseline information on the state of these resources and to determine the vulnerability of the reservoirs to increased loads of nutrients and other contaminants. The effects of land use, land cover, and other drainage-basin characteristics on sources, transport, and fate of fecal-indicator bacteria, highway deicing chemicals, nutrients, selected metals, and naturally occurring organic compounds in 11 subbasins that contribute water to the reservoirs also was investigated, and the data used to select sampling stations for incorporation into a water-quality monitoring network for the source area.\r\n\r\nAll three reservoirs exhibited thermal and chemical stratification, despite artificial mixing by air hoses in Stony Brook Reservoir and Fresh Pond. The stratification produced anoxic or hypoxic conditions in the deepest parts of the reservoirs and these conditions resulted in the release of ammonia nitrogen orthophosphate phosphorus, and dissolved iron and manganese from the reservoir bed sediments.\r\nConcentrations of sodium and chloride in the reservoirs usually were higher than the amounts recommended by the U.S. Environmental Protection agency for drinking-water sources (20 milligrams per liter for sodium and 250 milligrams per liter for chloride). Maximum measured sodium concentrations were highest in Hobbs Brook Reservoir (113 milligrams per liter), intermediate in Stony Brook Reservoir (62 milligrams per liter), and lowest in Fresh Pond (54 milligrams per liter). Bed sediments in Hobbs Brook and Stony Brook Reservoirs were enriched in iron, manganese, and arsenic relative to those in the impounded lower Charles River in Boston, Massachusetts.\r\n\r\nTrophic state indices, calculated for each reservoir based on nutrient concentrations, water-column transparency, and phytoplankton abundances, indicated that the upper and middle basins of Hobbs Brook Reservoir were moderately to highly productive and likely to produce algal blooms; the lower basin of Hobbs Brook Reservoir and Stony Brook Reservoir were similar and intermediate in productivity, and Fresh Pond was relatively unproductive and unlikely to produce algal blooms. This pattern is likely due to sedimentation of organic and inorganic particles in the three basins of Hobbs Brook Reservoir and in Stony Brook Reservoir. Molar ratios of nitrogen to phosphorus ranged from 55 in Stony Brook Reservoir to 120 in Hobbs Brook Reservoir, indicating that phytoplankton algae in these water bodies may be phosphorus limited and therefore sensitive to small increases in phosphorus loading from the drainage basin. Nitrogen loads were found to be less important than phosphorus to the trophic condition of the reservoirs.\r\nHobbs Brook and Stony Brook, the two principle streams draining the Cambridge drinking-water source area, differed in their relative contributions to many of the estimated constituent loads. The estimated load of fecal coliform bacteria was more than seven times larger for the mainly residential Stony Brook subbasin upstream from Kendal Green, Mass., than it was for the more commercial and industrial Hobbs Brook subbasin, though the drainage areas of the two subbasins differ only by about 20 percent. The State standard for fecal coliform bacteria in streams in the Cambridge drinking-water source area (20 colony forming units per 100 milliliters) was exceeded at all sampling stations.\r\n\r\nEstimated s","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri20004262","usgsCitation":"Waldron, M.C., and Bent, G.C., 2001, Factors affecting reservoir and stream-water quality in the Cambridge, Massachusetts, drinking-water source area and implications for source-water protection: U.S. Geological Survey Water-Resources Investigations Report 2000-4262, v, 89 p., https://doi.org/10.3133/wri20004262.","productDescription":"v, 89 p.","costCenters":[],"links":[{"id":400773,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_37620.htm"},{"id":160992,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2000/4262/report-thumb.jpg"},{"id":95870,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2000/4262/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Massachusetts","city":"Cambridge","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.33,\n 42.3\n ],\n [\n -71,\n 42.3\n ],\n [\n -71,\n 42.433\n ],\n [\n -71.33,\n 42.433\n ],\n [\n -71.33,\n 42.3\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a05e4b07f02db5f87dc","contributors":{"authors":[{"text":"Waldron, Marcus C. mwaldron@usgs.gov","contributorId":1867,"corporation":false,"usgs":true,"family":"Waldron","given":"Marcus","email":"mwaldron@usgs.gov","middleInitial":"C.","affiliations":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true}],"preferred":true,"id":204275,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bent, Gardner C. 0000-0002-5085-3146 gbent@usgs.gov","orcid":"https://orcid.org/0000-0002-5085-3146","contributorId":1864,"corporation":false,"usgs":true,"family":"Bent","given":"Gardner","email":"gbent@usgs.gov","middleInitial":"C.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":204274,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":31196,"text":"ofr00513 - 2001 - National Irrigation Water Quality Program data-synthesis data base","interactions":[],"lastModifiedDate":"2020-02-23T16:56:27","indexId":"ofr00513","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","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":"2000-513","title":"National Irrigation Water Quality Program data-synthesis data base","docAbstract":"Under the National Irrigation Water Quality Program (NIWQP) of the U.S. Department of the Interior, researchers investigated contamination caused by irrigation drainage in 26 areas in the Western United States from 1986 to 1993. From 1992 to 1995, a comprehensive relational data base was built to organize data collected during the 26-area investigations. The data base provided the basis for analysis and synthesis of these data to identify common features of contaminated areas and hence dominant biologic, geologic, climatic, chemical, and physiographic factors that have resulted in contamination of water and biota in irrigated areas in the Western United States. Included in the data base are geologic, hydrologic, climatological, chemical, and cultural data that describe the 26 study areas in 14 Western States. The data base contains information on 1,264 sites from which water and bottom sediment were collected. It also contains chemical data from 6,903 analyses of surface water, 914 analyses of ground water, 707 analyses of inorganic constituents in bottom sediments, 223 analyses of organochlorine pesticides in bottom sediments, 8,217 analyses of inorganic constituents in biota, and 1,088 analyses for organic constituents in biota. The data base is available to the public and can be obtained at the NIWQP homepage http://www.usbr.gov/niwqp as dBase III tables for personal-computer systems or as American Standard Code for Information Exchange structured query language (SQL) command and data files for SQL data bases.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr00513","usgsCitation":"Seiler, R.L., and Skorupa, J.P., 2001, National Irrigation Water Quality Program data-synthesis data base: U.S. Geological Survey Open-File Report 2000-513, iv, 35 p. , https://doi.org/10.3133/ofr00513.","productDescription":"iv, 35 p. ","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":160373,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2708,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr00513/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fc216","contributors":{"authors":[{"text":"Seiler, Ralph L.","contributorId":13609,"corporation":false,"usgs":true,"family":"Seiler","given":"Ralph","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":205297,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Skorupa, Joseph P.","contributorId":54980,"corporation":false,"usgs":true,"family":"Skorupa","given":"Joseph","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":205298,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":30722,"text":"fs03301 - 2001 - U.S. Geological Survey World Wide Web Information","interactions":[{"subject":{"id":30722,"text":"fs03301 - 2001 - U.S. Geological Survey World Wide Web Information","indexId":"fs03301","publicationYear":"2001","noYear":false,"title":"U.S. Geological Survey World Wide Web Information"},"predicate":"SUPERSEDED_BY","object":{"id":53167,"text":"fs05503 - 2003 - U.S. Geological Survey World Wide Web Information","indexId":"fs05503","publicationYear":"2003","noYear":false,"title":"U.S. Geological Survey World Wide Web Information"},"id":1}],"supersededBy":{"id":53167,"text":"fs05503 - 2003 - U.S. Geological Survey World Wide Web Information","indexId":"fs05503","publicationYear":"2003","noYear":false,"title":"U.S. Geological Survey World Wide Web Information"},"lastModifiedDate":"2014-04-03T08:41:19","indexId":"fs03301","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","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":"033-01","title":"U.S. Geological Survey World Wide Web Information","docAbstract":"The U.S. Geological Survey (USGS) invites\nyou to explore an earth science virtual library\nof digital information, publications, and data.\nThe USGS World Wide Web sites offer an\narray of information that reflects scientific\nresearch and monitoring programs conducted\nin the areas of natural hazards, environmental\nresources, and cartography. This list\nprovides gateways to access a cross section of\nthe digital information on the USGS World\nWide Web sites.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs03301","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2001, U.S. Geological Survey World Wide Web Information (Supersedes FS 037-00 & Superseded by FS 055-03): U.S. Geological Survey Fact Sheet 033-01, 2 p., https://doi.org/10.3133/fs03301.","productDescription":"2 p.","numberOfPages":"2","costCenters":[],"links":[{"id":160761,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs03301.jpg"},{"id":285362,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/0033-01/report.pdf"}],"edition":"Supersedes FS 037-00 & Superseded by FS 055-03","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2be4b07f02db612edd","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529229,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30735,"text":"fs05501 - 2001 - Availability Of Ground-Water Data For California, Water Year 2000","interactions":[],"lastModifiedDate":"2012-02-02T00:09:05","indexId":"fs05501","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","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":"055-01","title":"Availability Of Ground-Water Data For California, Water Year 2000","docAbstract":"The Water Resources Division of the U.S. Geological Survey, in cooperation with Federal, State, and local water agencies, obtains a large amount of data pertaining to the ground-water resources of California each water year. These data constitute a valuable database for developing an improved understanding of the water resources of the State. Beginning with the 1985 water year and continuing through 1993, these data were published in a report series entitled ?Water Resources Data for California, Volume 5. Ground-Water Data.? Prior to the introduction of this series, historical ground-water information was published in U.S. Geological Survey Water-Supply Papers.\r\n\r\nIn 1994, the Volume 5 Ground-Water Data report was discontinued, but data continue to be available in our databases. This Fact Sheet serves as an index to ground-water data for water year 2000. The 2-page report contains a map of California showing the number of wells (by county) with available water-level and water-quality data for water year 2000 (fig. 2) and instructions for obtaining this and other ground-water information contained in the databases of the Water Resources Division, California District.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/fs05501","usgsCitation":"Huff, J., 2001, Availability Of Ground-Water Data For California, Water Year 2000: U.S. Geological Survey Fact Sheet 055-01, 2 p. , https://doi.org/10.3133/fs05501.","productDescription":"2 p. ","temporalStart":"1999-10-01","temporalEnd":"2000-09-30","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":122391,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2001/0055/report-thumb.jpg"},{"id":59471,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2001/0055/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db668046","contributors":{"authors":[{"text":"Huff, Julia jahuff@usgs.gov","contributorId":1001,"corporation":false,"usgs":true,"family":"Huff","given":"Julia","email":"jahuff@usgs.gov","affiliations":[],"preferred":true,"id":203809,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30731,"text":"fs05101 - 2001 - United States Antarctic Resource Center (USARC)","interactions":[],"lastModifiedDate":"2012-03-16T17:16:06","indexId":"fs05101","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","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":"051-01","title":"United States Antarctic Resource Center (USARC)","docAbstract":"The U.S. Antarctic Resource Center (USARC) is our Nation?s depository for Antarctic maps, charts, geodetic ground control, satellite images, aerial photographs, publications, slides, and video tapes. These resources are items produced by Antarctic Treaty nations in support of their activities in Antarctica and provided to the USARC in compliance with a standing resolution of the treaty providing for exchange of information. The U.S. Geological Survey (USGS) maintains these materials through an interagency cooperative agreement with the National Science Foundation (NSF), which also supports the USGS Antarctic Mapping Program.\r\n\r\nThe USARC develops and maintains the Antarctic Web site (usarc.usgs.gov) and its supporting data bases, as well as providing access to other online digital data bases, such as the Atlas of Antarctic Resources.","language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs05101","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2001, United States Antarctic Resource Center (USARC): U.S. Geological Survey Fact Sheet 051-01, 2 p. , https://doi.org/10.3133/fs05101.","productDescription":"2 p. ","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":126786,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2001/0051/report-thumb.jpg"},{"id":59468,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2001/0051/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e412f","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529235,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30732,"text":"fs05201 - 2001 - Innovative Partnerships","interactions":[{"subject":{"id":25087,"text":"fs21496 - 1997 - Innovative partnerships","indexId":"fs21496","publicationYear":"1997","noYear":false,"title":"Innovative partnerships"},"predicate":"SUPERSEDED_BY","object":{"id":30732,"text":"fs05201 - 2001 - Innovative Partnerships","indexId":"fs05201","publicationYear":"2001","noYear":false,"title":"Innovative Partnerships"},"id":1}],"lastModifiedDate":"2012-02-29T17:02:31","indexId":"fs05201","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","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":"052-01","title":"Innovative Partnerships","docAbstract":"A major responsibility of the U.S. Geological Survey (USGS) is to ensure geospatial data availability. This includes the cooperative production of digital geospatial data through the National Mapping Program's Innovative Partnerships (IP) initiative, which began in October 1992.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/fs05201","usgsCitation":"Szemraj, J., 2001, Innovative Partnerships: U.S. Geological Survey Fact Sheet 052-01, 2 p. , https://doi.org/10.3133/fs05201.","productDescription":"2 p. ","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":2545,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2001/0052/","linkFileType":{"id":5,"text":"html"}},{"id":126450,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2001/0052/report-thumb.jpg"},{"id":59469,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2001/0052/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee48a","contributors":{"authors":[{"text":"Szemraj, John","contributorId":23186,"corporation":false,"usgs":true,"family":"Szemraj","given":"John","affiliations":[],"preferred":false,"id":203806,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30733,"text":"fs05301 - 2001 - National Water Quality Laboratory - A profile","interactions":[],"lastModifiedDate":"2021-05-28T16:11:21.875224","indexId":"fs05301","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","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":"053-01","title":"National Water Quality Laboratory - A profile","docAbstract":"The U.S. Geological Survey (USGS) National Water Quality Laboratory (NWQL) is a full-service laboratory that specializes in environmental analytical chemistry. The NWQL's primary mission is to support USGS programs requiring environmental analyses that provide consistent methodology for national assessment and trends analysis. The NWQL provides the following: high-quality chemical data; consistent, published, state-of-the-art methodology; extremely low-detection levels; high-volume capability; biological unit for identifying benthic invertebrates; quality assurance for determining long-term water-quality trends; and a professional staff.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs05301","usgsCitation":"Raese, J.W., 2001, National Water Quality Laboratory - A profile: U.S. Geological Survey Fact Sheet 053-01, 6 p., https://doi.org/10.3133/fs05301.","productDescription":"6 p.","costCenters":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true},{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":59470,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2001/0053/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":11564,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://nwql.usgs.gov/Public/FS-053-01.shtml","linkFileType":{"id":5,"text":"html"}},{"id":119231,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2001/0053/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db6986d0","contributors":{"authors":[{"text":"Raese, Jon W. jwraese@usgs.gov","contributorId":183,"corporation":false,"usgs":true,"family":"Raese","given":"Jon","email":"jwraese@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":203807,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30066,"text":"wri014005 - 2001 - Data-collection methods, quality-assurance data, and site considerations for total dissolved gas monitoring, lower Columbia River, Oregon and Washington, 2000","interactions":[],"lastModifiedDate":"2017-02-07T09:12:33","indexId":"wri014005","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4005","title":"Data-collection methods, quality-assurance data, and site considerations for total dissolved gas monitoring, lower Columbia River, Oregon and Washington, 2000","docAbstract":"Excessive total dissolved gas pressure can cause gas-bubble trauma in fish downstream from dams on the Columbia River. In cooperation with the U.S. Army Corps of Engineers, the U.S. Geological Survey collected data on total dissolved gas pressure, barometric pressure, water temperature, and probe depth at eight stations on the lower Columbia River from the John Day forebay (river mile 215.6) to Camas (river mile 121.7) in water year 2000 (October 1, 1999, to September 30, 2000). These data are in the databases of the U.S. Geological Survey and the U.S. Army Corps of Engineers. Methods of data collection, review, and processing, and quality-assurance data are presented in this report.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/wri014005","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers","usgsCitation":"Tanner, D.Q., and Johnston, M.W., 2001, Data-collection methods, quality-assurance data, and site considerations for total dissolved gas monitoring, lower Columbia River, Oregon and Washington, 2000: U.S. Geological Survey Water-Resources Investigations Report 2001-4005, iii, 19 p., https://doi.org/10.3133/wri014005.","productDescription":"iii, 19 p.","numberOfPages":"24","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":160125,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri014005.PNG"},{"id":310705,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2001/4005/report.pdf","text":"Report","size":"690.94 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Lower Columbia River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.48657226562499,\n 45.61403741135093\n ],\n [\n -122.18994140624999,\n 45.644768217751924\n ],\n [\n -121.86035156249999,\n 45.740693395533064\n ],\n [\n -121.53625488281249,\n 45.75985868785574\n ],\n [\n -121.2176513671875,\n 45.729191061299936\n ],\n [\n -121.0638427734375,\n 45.68315803253308\n ],\n [\n -120.7452392578125,\n 45.77135470445036\n ],\n [\n -120.56945800781249,\n 45.786679041363726\n ],\n [\n -120.4046630859375,\n 45.706179285330855\n ],\n [\n -120.45959472656249,\n 45.644768217751924\n ],\n [\n -120.66284179687499,\n 45.66780526567164\n ],\n [\n -120.92651367187499,\n 45.598665689820656\n ],\n [\n -121.19567871093751,\n 45.54867850352087\n ],\n [\n -121.3275146484375,\n 45.65628792636447\n ],\n [\n -121.761474609375,\n 45.63324613981234\n ],\n [\n -122.1844482421875,\n 45.521743896993634\n ],\n [\n -122.76672363281249,\n 45.471688258104614\n ],\n [\n -122.89306640624999,\n 45.706179285330855\n ],\n [\n -122.93701171874999,\n 45.98169518512228\n ],\n [\n -122.9974365234375,\n 46.09609080214316\n ],\n [\n -123.1842041015625,\n 46.145588688591964\n ],\n [\n -123.1622314453125,\n 46.195042108660154\n ],\n [\n -122.92602539062501,\n 46.20264638061019\n ],\n [\n -122.794189453125,\n 46.06560846138691\n ],\n [\n -122.5909423828125,\n 45.775186183521036\n ],\n [\n -122.48657226562499,\n 45.61403741135093\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db674479","contributors":{"authors":[{"text":"Tanner, Dwight Q.","contributorId":93452,"corporation":false,"usgs":true,"family":"Tanner","given":"Dwight","email":"","middleInitial":"Q.","affiliations":[],"preferred":false,"id":202618,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnston, Matthew W. mattj@usgs.gov","contributorId":3066,"corporation":false,"usgs":true,"family":"Johnston","given":"Matthew","email":"mattj@usgs.gov","middleInitial":"W.","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":202617,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":30861,"text":"wri004070 - 2001 - Use of borehole and surface geophysics to investigate ground-water quality near a road-deicing salt-storage facility, Valparaiso, Indiana","interactions":[],"lastModifiedDate":"2019-04-15T09:01:17","indexId":"wri004070","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2000–4070","displayTitle":"Use of borehole and surface geophysics to investigate ground-water quality near a road-deicing salt-storage facility, Valparaiso, Indiana","title":"Use of borehole and surface geophysics to investigate ground-water quality near a road-deicing salt-storage facility, Valparaiso, Indiana","docAbstract":"Borehole and surface geophysics were used to investigate ground-water quality affected by a road-deicing salt-storage facility located near a public water-supply well field. From 1994 through 1998, borehole geophysical logs were made in an existing network of monitoring wells completed near the bottom of a thick sand aquifer. Logs of natural gamma activity indicated a uniform and negligible contribution of clay to the electromagnetic conductivity of the aquifer so that the logs of electromagnetic conductivity primarily measured the amount of dissolved solids in the ground water near the wells. Electromagnetic-conductivity data indicated the presence of a saltwater plume near the bottom of the aquifer. Increases in electromagnetic conductivity, observed from sequential logging of wells, indicated the saltwater plume had moved north about 60 to 100 feet per year between 1994 and 1998. These rates were consistent with estimates of horizontal ground-water flow based on velocity calculations made with hydrologic data from the study area.
Ratios of chloride to bromide concentrations in water samples were used to distinguish sources of chloride in the ground water?whether from road-deicing salt, domestic wastewater, or natural occurrences. Water samples identified with the chloride/bromide ratios as being affected by road-deicing salt had concentrations of dissolved solids, chloride, and sodium many times the background levels for the study area. The largest concentrations were in water from wells near the salt-storage facility?12,400 to 12,800 milligrams per liter (mg/L) dissolved solids, 6,730 to 7,230 mg/L chloride, and 3,690 to 4,400 mg/L sodium.
A conceptual, multi-layer model was developed to describe the vertical extent of the saltwater plume in the vicinity of the monitoring wells. A relation was derived between average borehole electromagnetic conductivity in the screened interval of the wells in the saltwater plume and concentrations of dissolved solids in water samples from those wells. This relation was used in the model to show borehole electromagnetic conductivity in transects of wells as a zone of saline water overlain by zones of brackish water and freshwater. The thickness and altitude of the zones of saline and brackish water decreased with increased distance from the salt-storage facility.
Two surface surveys of terrain electromagnetic conductivity were used to map the horizontal extent of the saltwater plume in areas without monitoring wells. Background values of terrain conductivity were measured in an area where water-quality and borehole geophysical data did not indicate saline or brackish water. Based on a guideline from previous case studies, the boundaries of the saltwater plume were mapped where terrain conductivity was 1.5 times background. The extent of the saltwater plume, based on terrain conductivity, generally was consistent with the available water-quality and borehole electromagnetic-conductivity data and with directions of ground-water flow determined from water-level altitudes.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/wri004070","usgsCitation":"Risch, M., and Robinson, B., 2001, Use of borehole and surface geophysics to investigate ground-water quality near a road-deicing salt-storage facility, Valparaiso, Indiana: U.S. Geological Survey Water-Resources Investigations Report 2000–4070, Report: vi, 63 p., https://doi.org/10.3133/wri004070.","productDescription":"Report: vi, 63 p.","numberOfPages":"71","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":2737,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2000/4070/wri20004070.pdf","text":"Report","size":"4.04 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 2000-4070"},{"id":160294,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2000/4070/coverthb.jpg"}],"country":"United States","state":"Indiana","county":"Porter County","city":"Valparaiso","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-85.9369,39.9272],[-85.9379,39.87],[-85.9541,39.8696],[-85.9518,39.6969],[-85.9523,39.638],[-86.248,39.6335],[-86.3268,39.6318],[-86.3281,39.8526],[-86.328,39.8662],[-86.325,39.8662],[-86.3267,39.9238],[-86.2967,39.9246],[-86.2757,39.925],[-86.2385,39.9259],[-85.9801,39.9269],[-85.9411,39.9272],[-85.9369,39.9272]]]},\"properties\":{\"name\":\"Marion\",\"state\":\"IN\"}}]}","contact":"Director, Indiana Water Science Center
U.S. Geological Survey
5957 Lakeside Blvd.
Indianapolis, IN 46278
Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
OVERVIEW OF ARSENIC IN STREAM SEDIMENTS The overall range of arsenic in the NURE stream sediments was from 0.3 to 44 mg/kg sediment (ppm) As in the sample data set. The mean value was 4.3 ppm with a standard deviation of 4.1 ppm. For comparison, the crustal abundance of arsenic is 1.8 ppm (Taylor, 1964). Shale is higher, with average values of 15 ppm. Coal samples from the entire USGS National Coal Resource Data System coal database (Finkelman, 1994) average 24 ppm arsenic. A study of stream sediments from throughout the U.S. by the USGS NAWQA program reported that the 75th percentile for arsenic in 541 stream sediments was 9.5 ppm (Rice, 1999). Given the relatively low crustal abundance of arsenic, a number of stream-sediment samples in this study may be considered geochemically anomalous in this element.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf2357","usgsCitation":"Goldhaber, M., Irwin, E., Atkins, B., Lee, L., Black, D., Zappia, H., Hatch, J., Pashin, J., Barwick, L., Cartwright, W., Sanzolone, R., Rupert, L., Kolker, A., and Finkelman, R., 2001, Arsenic in stream sediments of northern Alabama: U.S. Geological Survey Miscellaneous Field Studies Map 2357, Sheet 62 by 44 inches (in color)., https://doi.org/10.3133/mf2357.","productDescription":"Sheet 62 by 44 inches (in color).","costCenters":[],"links":[{"id":186819,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6048,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/mf/2001/mf-2357/","linkFileType":{"id":5,"text":"html"}},{"id":110182,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_39183.htm","linkFileType":{"id":5,"text":"html"},"description":"39183"}],"country":"United States","state":"Alabama","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.65966796875,\n 33.22949814144951\n ],\n [\n -86.50634765625,\n 33.22949814144951\n ],\n [\n -86.50634765625,\n 35.11990857099681\n ],\n [\n -88.65966796875,\n 35.11990857099681\n ],\n [\n -88.65966796875,\n 33.22949814144951\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db672ea6","contributors":{"authors":[{"text":"Goldhaber, M. B. 0000-0002-1785-4243","orcid":"https://orcid.org/0000-0002-1785-4243","contributorId":103280,"corporation":false,"usgs":true,"family":"Goldhaber","given":"M. B.","affiliations":[],"preferred":false,"id":265771,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Irwin, Elise","contributorId":26928,"corporation":false,"usgs":true,"family":"Irwin","given":"Elise","affiliations":[],"preferred":false,"id":265760,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Atkins, Brian","contributorId":38422,"corporation":false,"usgs":true,"family":"Atkins","given":"Brian","email":"","affiliations":[],"preferred":false,"id":265761,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lee, Lopaka","contributorId":83167,"corporation":false,"usgs":true,"family":"Lee","given":"Lopaka","email":"","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":false,"id":265769,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Black, D.D.","contributorId":70244,"corporation":false,"usgs":true,"family":"Black","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":265766,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Zappia, Humbert","contributorId":79093,"corporation":false,"usgs":true,"family":"Zappia","given":"Humbert","email":"","affiliations":[],"preferred":false,"id":265767,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Hatch, Joe","contributorId":50204,"corporation":false,"usgs":true,"family":"Hatch","given":"Joe","email":"","affiliations":[],"preferred":false,"id":265764,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Pashin, Jack","contributorId":80144,"corporation":false,"usgs":true,"family":"Pashin","given":"Jack","affiliations":[],"preferred":false,"id":265768,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Barwick, L.H.","contributorId":66961,"corporation":false,"usgs":true,"family":"Barwick","given":"L.H.","email":"","affiliations":[],"preferred":false,"id":265765,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Cartwright, W.E.","contributorId":103140,"corporation":false,"usgs":true,"family":"Cartwright","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":265770,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Sanzolone, Rick","contributorId":45180,"corporation":false,"usgs":true,"family":"Sanzolone","given":"Rick","email":"","affiliations":[],"preferred":false,"id":265762,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Rupert, Leslie","contributorId":45959,"corporation":false,"usgs":true,"family":"Rupert","given":"Leslie","email":"","affiliations":[],"preferred":false,"id":265763,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Kolker, Allan 0000-0002-5768-4533 akolker@usgs.gov","orcid":"https://orcid.org/0000-0002-5768-4533","contributorId":643,"corporation":false,"usgs":true,"family":"Kolker","given":"Allan","email":"akolker@usgs.gov","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":265758,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Finkelman, Robert","contributorId":25036,"corporation":false,"usgs":true,"family":"Finkelman","given":"Robert","affiliations":[],"preferred":false,"id":265759,"contributorType":{"id":1,"text":"Authors"},"rank":14}]}} ,{"id":30912,"text":"wri014065 - 2001 - Herbicide use in the management of roadside vegetation, western Oregon, 1999-2000; effects on the water quality of nearby streams","interactions":[],"lastModifiedDate":"2016-06-09T08:45:05","indexId":"wri014065","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4065","title":"Herbicide use in the management of roadside vegetation, western Oregon, 1999-2000; effects on the water quality of nearby streams","docAbstract":"The Oregon Department of Transportation (ODOT) uses the herbicides Krovar (active ingredients diuron and bromacil), Oust (active ingredient sulfometuron-methyl) and Roundup (active ingredient glyphosate) to control roadside vegetation. The purpose of this study was to assess whether the use of these herbicides could contribute to the load of herbicides carried by Oregon streams.
\nIn spring of 1999, three test plots were constructed on a road shoulder near a crossing of Bull Creek, a small stream near Colton, Oregon, in the Willamette Valley. Simulated rainfall of 0.3 in/hr was applied to the experimental plots 1 day, 1 week, and 2 weeks after herbicide application. The simulated rainfall experiments yielded an upper limit concentration of 1 mg/L (milligram per liter, or parts per million) glyphosate and diuron, and of a few hundred micrograms per liter (µg/L, or parts per billion) of sulfometuron-methyl in runoff from the roadside when rainfall was applied 24 hr after spraying. Concentrations in the ditch itself would be less under natural conditions because of dilution by drainage water from the entire contributing drainage area.
\nThe road shoulder was resprayed at the end of September, and data were collected from late October 1999 through early January 2000, during natural rainfall. Diuron concentrations in the direct runoff from the road shoulder ranged from 1 to 10 µg/L throughout the 3-month sampling period; during the period, concentrations in the roadside ditch decreased from about 10 µg/L in October to about 0.1 µg/L in January, indicating progressive dilution of the roadside herbicide runoff during the fall/winter rainy season. No diuron was detected in Bull Creek downstream from the drainage ditch. A mass balance calculation confirmed that the load to Bull Creek from the drainage ditch was too low to result in detectable concentrations in the stream during October to January.
\nSulfometuron-methyl concentrations in runoff from the road shoulder ranged from 0.1 to 1 µg/L throughout the 3-month sampling period, and in the drainage ditch decreased from about 1 µg/L in October and November to about 0.2 µg/L in January. It was never detected in Bull Creek. Bromacil concentrations were similar to those of diuron. Glyphosate was never detected in fall samples from the road shoulder, the drainage ditch, or the stream.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri014065","collaboration":"Prepared in cooperation with the Oregon Department of Transportation","usgsCitation":"Wood, T.M., 2001, Herbicide use in the management of roadside vegetation, western Oregon, 1999–2000—\nEffects on the water quality of nearby streams: U.S. Geological Survey Water-Resources Investigations\nReport 01–4065, 27 p.","productDescription":"27 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":160300,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2001/4065/coverthb.jpg"},{"id":2878,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2001/4065/wri01-4065.pdf","text":"Report","size":"467 KB","linkFileType":{"id":1,"text":"pdf"},"description":"PDF of report"}],"contact":"Director, Oregon Water Science Center
U.S. Geological Survey
2130 SW 5th Avenue
Portland, Oregon 97201
http://or.water.usgs.gov
As of September 30, 1999, the surface-water data-collection network of Texas (table 1) included 321 continuous-record streamflow stations (D), 20 continuous-record gage-height only stations (G), 24 crest-stage partial-record stations (C), 40 floodhydrograph partial-record stations (H), 25 low-flow partial-record stations (L), 1 continuous-record temperature station (M1), 25 continuous-record temperature and specific conductance stations (M2), 17 continuous-record temperature, specific conductance, dissolved oxygen, and pH stations (M4), 4 daily water-quality stations (Qd), 115 periodic water-quality stations (Qp), 17 reservoir/lake surveys for water quality stations (Qs), 85 continuous or daily reservoircontent stations (R), and 10 daily precipitation stations (Pd). Plate 1 identifies the major river basins in Texas and shows the location of the stations listed in table 1.
Table 1 shows the station number and name, latitude and longitude, type of station, and office responsible for the collection of the data and maintenance of the record. An 8-digit permanent numerical designation for all gaging stations has been adopted on a nationwide basis; stations are numbered and listed in downstream order. In the downstream direction along the main stem, all stations on a tributary entering between two main-stem stations are listed between these two stations. A similar order is followed in listing stations by first rank, second rank, and other ranks of tributaries. The rank of any tributary, with respect to the stream to which it is an immediate tributary, is indicated by an indention in the table. Each indention represents one rank. This downstream order and system of indention shows which gaging stations are on tributaries between any two stations on a main stem and the rank of the tributary on which each gaging station is situated.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f4253","contributors":{"compilers":[{"text":"Gandara, Susan C.","contributorId":178740,"corporation":false,"usgs":true,"family":"Gandara","given":"Susan","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":662860,"contributorType":{"id":3,"text":"Compilers"},"rank":1},{"text":"Barbie, Dana L.","contributorId":64632,"corporation":false,"usgs":true,"family":"Barbie","given":"Dana","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":662861,"contributorType":{"id":3,"text":"Compilers"},"rank":2}]}} ,{"id":33080,"text":"b2184A - 2001 - Potential for deep basin-centered gas accumulation in Hanna Basin, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:09:16","indexId":"b2184A","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2184","chapter":"A","title":"Potential for deep basin-centered gas accumulation in Hanna Basin, Wyoming","docAbstract":"The potential for a continuous-type basin-centered gas accumulation in the Hanna Basin in Carbon County, Wyoming,\r\nis evaluated using geologic and production data including\r\nmud-weight, hydrocarbon-show, formation-test, bottom-hole-temperature, and vitrinite reflectance data from 29 exploratory\r\nwells.\r\nThis limited data set supports the presence of a hypothetical\r\nbasin-centered gas play in the Hanna Basin. Two generalized\r\nstructural cross sections illustrate our interpretations of possible abnormally pressured compartments. Data indicate that a gas-charged, overpressured interval may occur within the Cretaceous Mowry, Frontier, and Niobrara Formations at depths below 10,000 ft along the southern and western margins of the basin. Overpressuring may also occur near the basin center within the Steele Shale and lower Mesaverde Group section at depths below 18,000 to 20,000 ft. However, the deepest wells drilled to date (12,000 to 15,300 ft) have not encountered over-pressure in the basin center. This overpressured zone is likely to be relatively small (probably 20 to 25 miles in diameter) and is probably depleted of gas near major basement reverse faults and outcrops where gas may have escaped. Water may have invaded reservoirs through outcrops and fracture zones along the basin margins, creating an extensive normally pressured zone.\r\nA zone of subnormal pressure also may exist below the water-saturated, normal-pressure zone and above the central zone of overpressure. Subnormal pressures have been interpreted\r\nin the center of the Hanna Basin at depths ranging from 10,000 to 25,000 ft based on indirect evidence including lost-circulation zones. Three wells on the south side of the basin, where the top of the subnormally pressured zone is interpreted to cut across stratigraphic boundaries, tested the Niobrara Formation and recovered gas and oil shows with very low shut-in pressures.","language":"ENGLISH","doi":"10.3133/b2184A","usgsCitation":"Wilson, M.S., Dyman, T.S., and Nuccio, V.F., 2001, Potential for deep basin-centered gas accumulation in Hanna Basin, Wyoming (Version 1.0): U.S. Geological Survey Bulletin 2184, 12 p., https://doi.org/10.3133/b2184A.","productDescription":"12 p.","costCenters":[],"links":[{"id":164283,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3282,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/bul/b2184-a/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6833df","contributors":{"authors":[{"text":"Wilson, Michael S.","contributorId":56270,"corporation":false,"usgs":true,"family":"Wilson","given":"Michael","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":209845,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dyman, Thaddeus S.","contributorId":83971,"corporation":false,"usgs":true,"family":"Dyman","given":"Thaddeus","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":209846,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nuccio, Vito F. vnuccio@usgs.gov","contributorId":853,"corporation":false,"usgs":true,"family":"Nuccio","given":"Vito","email":"vnuccio@usgs.gov","middleInitial":"F.","affiliations":[],"preferred":true,"id":209844,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}