The Volcano Hazards Program of the U.S. Geological Survey (USGS) is part of the Geologic Hazards Assessments subactivity as funded by Congressional appropriation. Investigations are carried out in the Geology and Hydrology Disciplines of the USGS and with cooperators at the Alaska Division of Geological and Geophysical Surveys, University of Alaska Fairbanks Geophysical Institute, University of Hawaii Hilo, University of Utah, and University of Washington Geophysics Program. This report lists publications from all these institutions.
\nThis report contains only published papers and maps; numerous abstracts produced for presentations at scientific meetings have not been included. Publications are included based on date of publication with no attempt to assign them to Fiscal Year.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02492","usgsCitation":"Nathenson, M., 2002, Publications of the Volcano Hazards Program 2001: U.S. Geological Survey Open-File Report 2002-492, Report: PDF, 9 p.; Report: TXT, https://doi.org/10.3133/ofr02492.","productDescription":"Report: PDF, 9 p.; Report: TXT","numberOfPages":"9","additionalOnlineFiles":"Y","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":176319,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02492.jpg"},{"id":4389,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0492/","linkFileType":{"id":5,"text":"html"}},{"id":283919,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0492/pdf/of02-492.pdf"},{"id":283920,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0492/of02-492.txt"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a90e4b07f02db655e9f","contributors":{"authors":[{"text":"Nathenson, Manuel 0000-0002-5216-984X mnathnsn@usgs.gov","orcid":"https://orcid.org/0000-0002-5216-984X","contributorId":1358,"corporation":false,"usgs":true,"family":"Nathenson","given":"Manuel","email":"mnathnsn@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":241896,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":50582,"text":"ofr02488 - 2002 - Water quality and aquatic toxicity data of 2002 spring thaw conditions in the upper Animas River watershed, Silverton, Colorado","interactions":[],"lastModifiedDate":"2016-12-05T11:13:10","indexId":"ofr02488","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","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":"2002-488","title":"Water quality and aquatic toxicity data of 2002 spring thaw conditions in the upper Animas River watershed, Silverton, Colorado","docAbstract":"This report presents hydrologic, water-quality, and biologic toxicity data collected during the annual spring thaw of 2002 in the upper Animas River watershed near Silverton, Colorado. The spring-thaw runoff is a concern because elevated concentrations of iron oxyhydroxides can contain sorbed trace metals that are potentially toxic to aquatic life. Water chemistry of streams draining the San Juan Mountains is affected by natural acid drainage and weathering of hydrothermal altered volcanic rocks and by more than a century of mining activities. The timing of the spring-thaw sampling effort was determined by reviewing historical climate and stream-flow hydrographs and current weather conditions. Twenty-one water-quality samples were collected between 11:00 AM March 27, 2002 and 6:00 PM March 30, 2002 to characterize water chemistry at the A-72 gage on the upper Animas River below Silverton. Analyses of unfiltered water at the A-72 gage showed a relation between turbidity and total-recoverable iron concentrations, and showed diurnal patterns. Copper and lead concentrations were related to iron concentrations, indicating that these elements are probably sorbed to colloidal iron material. Calcium, strontium, and sulfate concentrations showed overall decreasing trends due to dilution, but the loads of those constituents increased over the sampling period. Nine water-quality samples were collected near the confluence of Mineral Creek with the Animas River, the confluence of Cement Creek with the Animas River, and on the upper Animas River above the confluence with Cement Creek (three samples at each site). A total of six bulk water-toxicity samples were collected before, during, and after the spring thaw from the Animas River at the A-72 gage site. Toxicity tests conducted with the bulk water samples on amphipods did not show strong differences in toxicity among the three sampling periods; however, toxicity of river water to fathead minnows showed a decreasing trend during the course of the study.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02488","usgsCitation":"Fey, D., Wirt, L., Besser, J., and Wright, W.G., 2002, Water quality and aquatic toxicity data of 2002 spring thaw conditions in the upper Animas River watershed, Silverton, Colorado: U.S. Geological Survey Open-File Report 2002-488, ii, 31 p., https://doi.org/10.3133/ofr02488.","productDescription":"ii, 31 p.","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":176229,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4387,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-488","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado","city":"Silverton","otherGeospatial":"Upper Animas River Watershed","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -108.468017578125,\n 37.06394430056685\n ],\n [\n -108.468017578125,\n 37.87485339352928\n ],\n [\n -107.105712890625,\n 37.87485339352928\n ],\n [\n -107.105712890625,\n 37.06394430056685\n ],\n [\n -108.468017578125,\n 37.06394430056685\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9bb7","contributors":{"authors":[{"text":"Fey, D.L.","contributorId":44537,"corporation":false,"usgs":true,"family":"Fey","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":241892,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wirt, L.","contributorId":80342,"corporation":false,"usgs":true,"family":"Wirt","given":"L.","email":"","affiliations":[],"preferred":false,"id":241893,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Besser, J.M.","contributorId":91569,"corporation":false,"usgs":true,"family":"Besser","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":241894,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wright, W. G.","contributorId":19582,"corporation":false,"usgs":true,"family":"Wright","given":"W.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":241891,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":50515,"text":"ofr02337 - 2002 - Method of analysis and quality-assurance practices by the U.S. Geological Survey Organic Geochemistry Research Group: Determination of geosmin and methylisoborneol in water using solid-phase microextraction and gas chromatography/mass spectrometry","interactions":[],"lastModifiedDate":"2024-07-31T14:14:19.055171","indexId":"ofr02337","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","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":"2002-337","title":"Method of analysis and quality-assurance practices by the U.S. Geological Survey Organic Geochemistry Research Group: Determination of geosmin and methylisoborneol in water using solid-phase microextraction and gas chromatography/mass spectrometry","docAbstract":"A method for the determination of two common odor-causing compounds in water, geosmin and 2-methylisoborneol, was modified and verified by the U.S. Geological Survey's Organic Geochemistry Research Group in Lawrence, Kansas. The optimized method involves the extraction of odor-causing compounds from filtered water samples using a divinylbenzene-carboxen-polydimethylsiloxane cross-link coated solid-phase microextraction (SPME) fiber. Detection of the compounds is accomplished using capillary-column gas chromatography/mass spectrometry (GC/MS). Precision and accuracy were demonstrated using reagent-water, surface-water, and ground-water samples.
The mean accuracies as percentages of the true compound concentrations from water samples spiked at 10 and 35 nanograms per liter ranged from 60 to 123 percent for geosmin and from 90 to 96 percent for 2-methylisoborneol. Method detection limits were 1.9 nanograms per liter for geosmin and 2.0 nanograms per liter for 2-methylisoborneol in 45-milliliter samples. Typically, concentrations of 30 and 10 nanograms per liter of geosmin and 2-methylisoborneol, respectively, can be detected by the general public. The calibration range for the method is equivalent to concentrations from 5 to 100 nanograms per liter without dilution. The method is valuable for acquiring information about the production and fate of these odor-causing compounds in water.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02337","usgsCitation":"Zimmerman, L., Ziegler, A., and Thurman, E., 2002, Method of analysis and quality-assurance practices by the U.S. Geological Survey Organic Geochemistry Research Group: Determination of geosmin and methylisoborneol in water using solid-phase microextraction and gas chromatography/mass spectrometry: U.S. Geological Survey Open-File Report 2002-337, iv, 12 p., https://doi.org/10.3133/ofr02337.","productDescription":"iv, 12 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":176542,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2002/0337/report-thumb.jpg"},{"id":431707,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0337/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db627397","contributors":{"authors":[{"text":"Zimmerman, L.R.","contributorId":28624,"corporation":false,"usgs":true,"family":"Zimmerman","given":"L.R.","email":"","affiliations":[],"preferred":false,"id":241653,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ziegler, A.C.","contributorId":74398,"corporation":false,"usgs":true,"family":"Ziegler","given":"A.C.","email":"","affiliations":[],"preferred":false,"id":241654,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thurman, E.M.","contributorId":102864,"corporation":false,"usgs":true,"family":"Thurman","given":"E.M.","affiliations":[],"preferred":false,"id":241655,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":44934,"text":"wri20024292 - 2002 - Estimates of median flows for streams on the Kansas surface water register","interactions":[{"subject":{"id":44934,"text":"wri20024292 - 2002 - Estimates of median flows for streams on the Kansas surface water register","indexId":"wri20024292","publicationYear":"2002","noYear":false,"displayTitle":"Estimates of Median Flows for Streams on the Kansas Surface Water Register","title":"Estimates of median flows for streams on the Kansas surface water register"},"predicate":"SUPERSEDED_BY","object":{"id":55232,"text":"sir20045032 - 2004 - Estimates of median flows for streams on the 1999 Kansas Surface Water Register","indexId":"sir20045032","publicationYear":"2004","noYear":false,"title":"Estimates of median flows for streams on the 1999 Kansas Surface Water Register"},"id":1}],"supersededBy":{"id":55232,"text":"sir20045032 - 2004 - Estimates of median flows for streams on the 1999 Kansas Surface Water Register","indexId":"sir20045032","publicationYear":"2004","noYear":false,"title":"Estimates of median flows for streams on the 1999 Kansas Surface Water Register"},"lastModifiedDate":"2019-05-28T10:09:50","indexId":"wri20024292","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","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":"2002-4292","displayTitle":"Estimates of Median Flows for Streams on the Kansas Surface Water Register","title":"Estimates of median flows for streams on the Kansas surface water register","docAbstract":"The Kansas State Legislature, by enacting Kansas Statute KSA 82a-2001 et. seq., mandated the criteria for determining which Kansas stream segments would be subject to classification by the State. One criterion for the selection as a classified stream segment is based on the statistic of median flow being equal to or greater than 1 cubic foot per second. As specified by KSA 82a-2001 et. seq., median flows were determined from U.S. Geological Survey streamflow-gaging-station data by using the most-recent 10-years of gaged data (KSA) for each streamflow-gaging station. Median flows also were determined by using gaged data from the entire period of record (all-available hydrology, AAH).
Least-squares multiple regression techniques were used, along with Tobit analyses, to develop equations for estimating median flows for uncontrolled stream segments. The drainage area of the uncontrolled gaging stations used in the regression analyses ranged from 2.06 to 12,004 square miles. A logarithmic transformation of the data was needed to develop the best linear relation for computing median flows. In the regression analyses, the significant climatic and basin characteristics, in order of importance, were drainage area, mean annual precipitation, mean basin permeability, and mean basin slope. Tobit analyses of KSA data yielded a root mean square error of 0.285 logarithmic units, and the best equations using Tobit analyses of AAH data had a root mean square error of 0.247 logarithmic units.
These equations and an interpolation procedure were used to compute median flows for the uncontrolled stream segments on the Kansas Surface Water Register. Measured median flows from gaging stations were incorporated into the regression-estimated median flows along the stream segments where available. The segments that were uncontrolled were interpolated using gaged data weighted according to the drainage area and the bias between the regression-estimated and gaged flow information. On controlled reaches of Kansas streams, the median flow information was interpolated between gaging stations using only gaged data weighted by drainage area.
Of the 2,232 total stream segments on the Kansas Surface Water Register, 30 percent of the segments had an estimated median streamflow of less than 1 cubic foot per second when the KSA analysis was used. When the AAH analysis was used, 40 percent of the segments had an estimated median streamflow of less than 1 cubic foot per second.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri20024292","collaboration":"Prepared in cooperation with the Kansas Department of Health and Environment","usgsCitation":"Perry, C.A., Wolock, D.M., and Artman, J.C., 2002, Estimates of median flows for streams on the Kansas surface water register (Superseded by SIR 2004-5032): U.S. Geological Survey Water-Resources Investigations Report 2002-4292, vi, 107 p., https://doi.org/10.3133/wri20024292.","productDescription":"vi, 107 p.","numberOfPages":"114","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":360235,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4292/wrir20024292.pdf","text":"Report","size":"29.0 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRIR 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U.S. Geological Survey
1217 Biltmore Drive
Lawrence, KS 66049
We describe a laboratory investigation into the effect of turbulent hydrodynamic stresses on clam larvae in the settlement phase of the recruitment process. A two-component laser-Doppler anemometer (LDA) was used to measure time histories of the instantaneous turbulence structure at potential recruitment sites within reconstructed beds of the adult Asian clam, Potamocorbula amurensis. Measurements were made for two flow speeds over beds with three different clam densities and two different clam heights. We analyze the statistical effect of the turbulence on the larval flux to the bed and on the probability of successful anchoring to the substrate. It is shown that the anchoring probability depends on the nature of the instantaneous stress events rather than on mean stresses. The instantaneous turbulence structure near the bed is altered by the flow rate and the spacing and height of adult clams living in the substrate. The ability to anchor quickly is therefore extremely important, since the time sequence of episodic turbulent stress events influences larval settlement success. The probability of successful larval settlement is predicted to decrease as the spacing between adults decreases, implying that the hydrodynamics impose negative feedback on clam bed aggregation dynamics.
","language":"English","publisher":"Association for the Sciences of Limnology and Oceanography","doi":"10.4319/lo.2002.47.4.1137","usgsCitation":"Crimaldi, J.P., Thompson, J.K., Rosman, J.H., Lowe, R.J., and Koseff, J.R., 2002, Hydrodynamics of larval settlement: The influence of turbulent stress events at potential recruitment sites: Limnology and Oceanography, v. 47, no. 4, p. 1137-1151, https://doi.org/10.4319/lo.2002.47.4.1137.","productDescription":"15 p.","startPage":"1137","endPage":"1151","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":478598,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.4319/lo.2002.47.4.1137","text":"Publisher Index Page"},{"id":314347,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"47","issue":"4","noUsgsAuthors":false,"publicationDate":"2002-07-11","publicationStatus":"PW","scienceBaseUri":"5698d4cde4b0fbd3f7fa4c44","contributors":{"authors":[{"text":"Crimaldi, John P.","contributorId":58918,"corporation":false,"usgs":true,"family":"Crimaldi","given":"John","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":588729,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, Janet K. 0000-0002-1528-8452 jthompso@usgs.gov","orcid":"https://orcid.org/0000-0002-1528-8452","contributorId":1009,"corporation":false,"usgs":true,"family":"Thompson","given":"Janet","email":"jthompso@usgs.gov","middleInitial":"K.","affiliations":[{"id":36183,"text":"Hydro-Ecological Interactions Branch","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":588730,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rosman, Johanna H.","contributorId":152264,"corporation":false,"usgs":false,"family":"Rosman","given":"Johanna","email":"","middleInitial":"H.","affiliations":[{"id":6986,"text":"Stanford University","active":true,"usgs":false}],"preferred":false,"id":588731,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lowe, Ryan J.","contributorId":152265,"corporation":false,"usgs":false,"family":"Lowe","given":"Ryan","email":"","middleInitial":"J.","affiliations":[{"id":6986,"text":"Stanford University","active":true,"usgs":false}],"preferred":false,"id":588732,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Koseff, Jeffrey R.","contributorId":37915,"corporation":false,"usgs":false,"family":"Koseff","given":"Jeffrey","email":"","middleInitial":"R.","affiliations":[{"id":6986,"text":"Stanford University","active":true,"usgs":false}],"preferred":false,"id":588733,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":50573,"text":"ofr02465 - 2002 - A bibliography of terrain modeling (geomorphometry), the quantitative representation of topography: Supplement 4.0","interactions":[],"lastModifiedDate":"2023-06-23T16:51:47.889016","indexId":"ofr02465","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","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":"2002-465","title":"A bibliography of terrain modeling (geomorphometry), the quantitative representation of topography: Supplement 4.0","docAbstract":"Terrain modeling, the practice of ground-surface quantification, is an amalgam of Earth science, mathematics, engineering, and computer science. The discipline is known variously as geomorphometry (or simply morphometry), terrain analysis, and quantitative geomorphology. It continues to grow through myriad applications to hydrology, geohazards mapping, tectonics, sea-floor and planetary exploration, and other fields. Dating nominally to the co-founders of academic geography, Alexander von Humboldt (1808, 1817) and Carl Ritter (1826, 1828), the field was revolutionized late in the 20th Century by the computer manipulation of spatial arrays of terrain heights, or digital elevation models (DEMs), which can quantify and portray ground-surface form over large areas (Maune, 2001). Morphometric procedures are implemented routinely by commercial geographic information systems (GIS) as well as specialized software (Harvey and Eash, 1996; Köthe and others, 1996; ESRI, 1997; Drzewiecki et al., 1999; Dikau and Saurer, 1999; Djokic and Maidment, 2000; Wilson and Gallant, 2000; Breuer, 2001; Guth, 2001; Eastman, 2002). The new Earth Surface edition of the Journal of Geophysical Research, specializing in surficial processes, is the latest of many publication venues for terrain modeling.
\nThis is the fourth update of a bibliography and introduction to terrain modeling (Pike, 1993, 1995, 1996, 1999) designed to collect the diverse, scattered literature on surface measurement as a resource for the research community. The use of DEMs in science and technology continues to accelerate and diversify (Pike, 2000a). New work appears so frequently that a sampling must suffice to represent the vast literature. This report adds 1636 entries to the 4374 in the four earlier publications1. Forty-eight additional entries correct dead Internet links and other errors found in the prior listings. Chronicling the history of terrain modeling, many entries in this report predate the 1999 supplement. Coverage is representative from about 1800 through early–mid 2002. Papers increasingly are published exclusively or in duplicate on the Internet's World Wide Web; the dates given here for Web addresses (URLs) that lack a print publication indicate a Web site's last update or my last access of it. The bibliography is arranged alphabetically and thus is not readily summarized. This introduction cites about 500 entries, a third of them grouped under 24 morphometric topics, as a guide to the listing's contents. Continuing the practice of previous bibliographies in the series to provide more information on a few applications (see summary of past topics in Pike, 2000a), this report elaborates further on topographic data, putative new parameters, tectonic geomorphology/neo-orometry, biogeography, ice-cap morphometry, results from the Mars Global DEM, landslide-hazard mapping, terrain modeling as physics, Hack's law, and broad-scale computer visualization. The literature of some of these subjects is large, and none of the summaries is intended to more than introduce the topic and comment on some of the current contributions of terrain modeling. Closing the essay is a discussion of pre-1900 papers that trace the evolution of ridge-line and watercourse quantification by descriptive geometry, as well as comments on some new books and an on-line bulletin board.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02465","usgsCitation":"Pike, R.J., 2002, A bibliography of terrain modeling (geomorphometry), the quantitative representation of topography: Supplement 4.0: U.S. Geological Survey Open-File Report 2002-465, 158 p., https://doi.org/10.3133/ofr02465.","productDescription":"158 p.","numberOfPages":"158","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":176704,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02465.jpg"},{"id":283911,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0465/pdf/of02-465.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":283912,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0465/of02-465.txt"},{"id":4381,"rank":4,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0465/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4975e4b0b290850ef30e","contributors":{"authors":[{"text":"Pike, Richard J. rpike@usgs.gov","contributorId":5753,"corporation":false,"usgs":true,"family":"Pike","given":"Richard","email":"rpike@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":241872,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44961,"text":"wri024186 - 2002 - Guidance on the use of passive-vapor-diffusion samplers to detect volatile organic compounds in ground-water-discharge areas, and example applications in New England","interactions":[],"lastModifiedDate":"2020-02-19T19:29:25","indexId":"wri024186","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","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":"2002-4186","title":"Guidance on the use of passive-vapor-diffusion samplers to detect volatile organic compounds in ground-water-discharge areas, and example applications in New England","docAbstract":"Polyethylene-membrane passive-vapor-diffusion samplers, or PVD samplers, have been shown to be an effective and economical reconnaissance tool for detecting and identifying volatile organic compounds (VOCs) in bottom sediments of surface-water bodies in areas of ground-water discharge. The PVD samplers consist of an empty glass vial enclosed in two layers of polyethylene membrane tubing. When samplers are placed in contaminated sediments, the air in the vial equilibrates with VOCs in pore water. Analysis of the vapor indicates the presence or absence of VOCs and the likely magnitude of concentrations in pore water.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri024186","usgsCitation":"Church, P.E., Vroblesky, D.A., and Lyford, F.P., 2002, Guidance on the use of passive-vapor-diffusion samplers to detect volatile organic compounds in ground-water-discharge areas, and example applications in New England: U.S. Geological Survey Water-Resources Investigations Report 2002-4186, vii, 79 p., https://doi.org/10.3133/wri024186.","productDescription":"vii, 79 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":162077,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3835,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024186/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Maine, Vermont, New Hampshire, Massachusetts, Pennsylvania, New York, Maryland, New Jersey, Rhode Island, Virginia, Delaware, Connecticut, West Virginia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -76.025390625,\n 36.56260003738545\n ],\n [\n -75.5859375,\n 37.09023980307208\n ],\n [\n -75.2783203125,\n 37.996162679728116\n ],\n [\n -75.05859375,\n 38.8225909761771\n ],\n [\n -74.0478515625,\n 40.01078714046552\n ],\n [\n -73.4326171875,\n 40.51379915504413\n ],\n [\n -72.50976562499999,\n 40.78054143186033\n ],\n [\n -71.19140625,\n 41.21172151054787\n ],\n [\n -70.0048828125,\n 41.47566020027821\n ],\n [\n -69.9609375,\n 41.83682786072714\n ],\n [\n -70.13671875,\n 42.32606244456202\n ],\n [\n -70.5322265625,\n 42.68243539838623\n ],\n [\n -70.4443359375,\n 43.13306116240612\n ],\n [\n -69.0380859375,\n 44.02442151965934\n ],\n [\n -67.3681640625,\n 44.5278427984555\n ],\n [\n -66.97265625,\n 44.99588261816546\n ],\n [\n -67.7197265625,\n 45.89000815866184\n ],\n [\n -67.8076171875,\n 47.100044694025215\n ],\n [\n -68.2470703125,\n 47.368594345213374\n ],\n [\n -68.9501953125,\n 47.27922900257082\n ],\n [\n -69.169921875,\n 47.45780853075031\n ],\n [\n -70.09277343749999,\n 46.558860303117164\n ],\n [\n -70.4443359375,\n 45.706179285330855\n ],\n [\n -71.806640625,\n 45.213003555993964\n ],\n [\n -74.3115234375,\n 45.1510532655634\n ],\n [\n -75.41015624999999,\n 44.74673324024678\n ],\n [\n -76.0693359375,\n 44.24519901522129\n ],\n [\n -77.16796875,\n 43.866218006556394\n ],\n [\n -79.189453125,\n 43.389081939117496\n ],\n [\n -79.27734374999999,\n 42.87596410238256\n ],\n [\n -80.595703125,\n 42.22851735620852\n ],\n [\n -80.595703125,\n 40.54720023441049\n ],\n [\n -81.298828125,\n 39.639537564366684\n ],\n [\n -82.08984375,\n 38.92522904714054\n ],\n [\n -82.6171875,\n 38.47939467327645\n ],\n [\n -82.177734375,\n 37.579412513438385\n ],\n [\n -83.3642578125,\n 36.70365959719456\n ],\n [\n -76.025390625,\n 36.56260003738545\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db654c01","contributors":{"authors":[{"text":"Church, Peter E.","contributorId":99178,"corporation":false,"usgs":true,"family":"Church","given":"Peter","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":230777,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vroblesky, Don A. vroblesk@usgs.gov","contributorId":413,"corporation":false,"usgs":true,"family":"Vroblesky","given":"Don","email":"vroblesk@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":230775,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lyford, Forest P.","contributorId":43334,"corporation":false,"usgs":true,"family":"Lyford","given":"Forest","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":230776,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":39980,"text":"wri024094 - 2002 - Hydrology of the Black Hills area, South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:10:35","indexId":"wri024094","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","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":"2002-4094","title":"Hydrology of the Black Hills area, South Dakota","docAbstract":"The Black Hills Hydrology Study was initiated in 1990 to assess the quantity, quality, and distribution of surface water and ground water in the Black Hills area of South Dakota. This report summarizes the hydrology of the Black Hills area and the results of this long-term study.The Black Hills area of South Dakota and Wyoming is an important recharge area for several regional, bedrock aquifer systems and various local aquifers; thus, the study focused on describing the hydrologic significance of selected bedrock aquifers. The major aquifers in the Black Hills area are the Deadwood, Madison, Minnelusa, Minnekahta, and Inyan Kara aquifers. The highest priority was placed on the Madison and Minnelusa aquifers, which are used extensively and heavily influence the surface-water resources of the area.Within this report, the hydrogeologic framework of the area, including climate, geology, ground water, and surface water, is discussed. Hydrologic processes and characteristics for ground water and surface water are presented. For ground water, water-level trends and comparisons and water-quality characteristics are presented. For surface water, streamflow characteristics, responses to precipitation, annual yields and yield efficiencies, and water-quality characteristics are presented. Hydrologic budgets are presented for ground water, surface water, and the combined ground-water/surface-water system. A summary of study findings regarding the complex flow systems within the Madison and Minnelusa aquifers also is presented.","language":"ENGLISH","doi":"10.3133/wri024094","usgsCitation":"Driscoll, D.G., Carter, J., Williamson, J., and Putnam, L., 2002, Hydrology of the Black Hills area, South Dakota: U.S. Geological Survey Water-Resources Investigations Report 2002-4094, 150 p. : ill. (some col.), maps (some col.) ; 28 cm., https://doi.org/10.3133/wri024094.","productDescription":"150 p. : ill. (some col.), maps (some col.) ; 28 cm.","costCenters":[],"links":[{"id":173297,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3669,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024094","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47b0e4b07f02db49cbe0","contributors":{"authors":[{"text":"Driscoll, Daniel G. dgdrisco@usgs.gov","contributorId":1558,"corporation":false,"usgs":true,"family":"Driscoll","given":"Daniel","email":"dgdrisco@usgs.gov","middleInitial":"G.","affiliations":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":222732,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carter, Janet M. 0000-0002-6376-3473","orcid":"https://orcid.org/0000-0002-6376-3473","contributorId":40660,"corporation":false,"usgs":true,"family":"Carter","given":"Janet M.","affiliations":[{"id":501,"text":"Office of Science Quality and Integrity","active":true,"usgs":true},{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":222735,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Williamson, Joyce jewillia@usgs.gov","contributorId":23612,"corporation":false,"usgs":true,"family":"Williamson","given":"Joyce","email":"jewillia@usgs.gov","affiliations":[],"preferred":false,"id":222733,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Putnam, Larry","contributorId":31456,"corporation":false,"usgs":true,"family":"Putnam","given":"Larry","affiliations":[],"preferred":false,"id":222734,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":44650,"text":"wri024278 - 2002 - Simulation of reservoir storage and firm yields of three surface-water supplies, Ipswich River Basin, Massachusetts","interactions":[],"lastModifiedDate":"2025-07-23T13:17:24.384486","indexId":"wri024278","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","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":"2002-4278","title":"Simulation of reservoir storage and firm yields of three surface-water supplies, Ipswich River Basin, Massachusetts","docAbstract":"A Hydrologic Simulation Program FORTRAN (HSPF) model previously developed for the Ipswich River Basin was modified to simulate the hydrologic response and firm yields of the water-supply systems of Lynn, Peabody, and Salem-Beverly. The updated model, expanded to include a portion of the Saugus River Basin that supplies water to Lynn, simulated reservoir system storage over a 35-year period (1961-95) under permitted withdrawals and hypothetical restrictions designed to maintain seasonally varied streamflow for aquatic habitat. A firm yield was calculated for each system and each withdrawal restriction by altering demands until the system failed. This is considered the maximum withdrawal rate that satisfies demands, but depletes reservoir storage. Simulations indicate that, under the permitted withdrawals, Lynn and Salem-Beverly were able to meet demands and generally have their reservoir system recover to full capacity during most years; reservoir storage averaged 83 and 82 percent of capacity, respectively. The firm yields for the Lynn and Salem-Beverly systems were 11.4 and 12.2 million gallons per day (Mgal/d), respectively, or 8 and 21 percent more than average 1998-2000 demands, respectively. Under permitted withdrawals and average 1998-2000 demands, the Peabody system failed in all years; thus Peabody purchased water to meet demands. The firm yield for the Peabody system is 3.70 Mgal/d, or 37 percent less than the average 1998-2000 demand. Simulations that limit withdrawals to levels recommended by the Ipswich River Fisheries Restoration Task Group (IRFRTG) indicate that under average 1998-2000 demands, reservoir storage was depleted in each of the three systems. Reservoir storage under average 1998-2000 demands and IRFRTG-recommended streamflow requirements averaged 15, 22, and 71 percent of capacity for the Lynn, Peabody, Salem-Beverly systems, respectively. The firm-yield estimates under the IRFRTG-recommended streamflow requirements were 6.02, 1.94, and 7.69 Mgal/d or 43, 64, and 34 percent less than the average 1998-2000 demands for the Lynn, Peabody, and Salem-Beverly systems, respectively. Simulations that limit withdrawals from the Saugus River to a less stringent set of restrictions (based on an Instream Flow Incremental Methodology study) than those previously simulated indicate that the firm yield of the Lynn system is about 31 percent less than the average 1998-2000 withdrawals (7.31 Mgal/d).","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri024278","usgsCitation":"Zarriello, P.J., 2002, Simulation of reservoir storage and firm yields of three surface-water supplies, Ipswich River Basin, Massachusetts: U.S. Geological Survey Water-Resources Investigations Report 2002-4278, 58 p., https://doi.org/10.3133/wri024278.","productDescription":"58 p.","costCenters":[],"links":[{"id":169130,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3758,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri02-4278/index.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Massachusetts","otherGeospatial":"Ipswich River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -70.80079238887427,\n 42.791573181324765\n ],\n [\n -71.33162209596102,\n 42.791573181324765\n ],\n [\n -71.33162209596102,\n 42.47218348466947\n ],\n [\n -70.80079238887427,\n 42.47218348466947\n ],\n [\n -70.80079238887427,\n 42.791573181324765\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f2217","contributors":{"authors":[{"text":"Zarriello, Phillip J. 0000-0001-9598-9904 pzarriel@usgs.gov","orcid":"https://orcid.org/0000-0001-9598-9904","contributorId":1868,"corporation":false,"usgs":true,"family":"Zarriello","given":"Phillip","email":"pzarriel@usgs.gov","middleInitial":"J.","affiliations":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230200,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44956,"text":"wri024168 - 2002 - The National Flood Frequency Program, version 3 : a computer program for estimating magnitude and frequency of floods for ungaged sites","interactions":[],"lastModifiedDate":"2012-02-02T00:10:12","indexId":"wri024168","displayToPublicDate":"2003-01-01T00:00:00","publicationYear":"2002","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":"2002-4168","title":"The National Flood Frequency Program, version 3 : a computer program for estimating magnitude and frequency of floods for ungaged sites","docAbstract":"For many years, the U.S. Geological Survey (USGS) has been developing regional regression equations for estimating flood magnitude and frequency at ungaged sites. These regression equations are used to transfer flood characteristics from gaged to ungaged sites through the use of watershed and climatic characteristics as explanatory or predictor variables. Generally, these equations have been developed on a Statewide or metropolitan-area basis as part of cooperative study programs with specific State Departments of Transportation. \r\n\r\nIn 1994, the USGS released a computer program titled the National Flood Frequency Program (NFF), which compiled all the USGS available regression equations for estimating the magnitude and frequency of floods in the United States and Puerto Rico. NFF was developed in cooperation with the Federal Highway Administration and the Federal Emergency Management Agency. Since the initial release of NFF, the USGS has produced new equations for many areas of the Nation. A new version of NFF has been developed that incorporates these new equations and provides additional functionality and ease of use. \r\n\r\nNFF version 3 provides regression-equation estimates of flood-peak discharges for unregulated rural and urban watersheds, flood-frequency plots, and plots of typical flood hydrographs for selected recurrence intervals. The Program also provides weighting techniques to improve estimates of flood-peak discharges for gaging stations and ungaged sites. The information provided by NFF should be useful to engineers and hydrologists for planning and design applications. \r\n\r\nThis report describes the flood-regionalization techniques used in NFF and provides guidance on the applicability and limitations of the techniques. The NFF software and the documentation for the regression equations included in NFF are available at http://water.usgs.gov/software/nff.html.","language":"ENGLISH","doi":"10.3133/wri024168","usgsCitation":"Ries, K., and Crouse, M.Y., 2002, The National Flood Frequency Program, version 3 : a computer program for estimating magnitude and frequency of floods for ungaged sites: U.S. Geological Survey Water-Resources Investigations Report 2002-4168, 53 p., https://doi.org/10.3133/wri024168.","productDescription":"53 p.","costCenters":[],"links":[{"id":3830,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024168/","linkFileType":{"id":5,"text":"html"}},{"id":162264,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b1ab","contributors":{"authors":[{"text":"Ries, Kernell G. III kries@usgs.gov","contributorId":1913,"corporation":false,"usgs":true,"family":"Ries","given":"Kernell G.","suffix":"III","email":"kries@usgs.gov","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":false,"id":230766,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crouse, Michele Y.","contributorId":93540,"corporation":false,"usgs":true,"family":"Crouse","given":"Michele","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":230767,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70205408,"text":"70205408 - 2002 - Historical trend in ice thickness on the Piscataquis River in central Maine.","interactions":[],"lastModifiedDate":"2019-09-19T11:28:00","indexId":"70205408","displayToPublicDate":"2002-12-31T12:50:11","publicationYear":"2002","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"title":"Historical trend in ice thickness on the Piscataquis River in central Maine.","docAbstract":"We analyzed a long-term record of ice thickness on the Piscataquis River in central Maine to determine whether there were temporal trends that were associated with climate warming. Trends in ice thickness were compared and correlated with regional time series of winter air temperature, heating degree days (HDD) , date of river ice-out, seasonal center-of-volume date (SCVD) (date on which half of the stream runoff volume during the period 1 Jan and 31 May has occurred), water temperature, and lake ice-out date. All of these variables except lake ice-out date showed significant temporal trends during the 20th century. Average ice thickness around 28 Feb. decreased by about 23 cm from 1912 to 2001. Over the period 1900 to 1999, winter air temperature increased by 1.7 ˚C and HDD decreased by about 7.5%. Final ice-out date on the Piscataquis River occurred earlier (advanced), by 0.23 days yr–1 over the period 1931 to 2002. The SCVD advanced by 0.11 days yr–1 over the period 1903 to 2001. Ice thickness was significantly correlated with winter air temperature, HDD, river ice-out, and SCVD (P-value < 0.01). These systematic temporal trends in multiple hydrologic indicator variables indicate a coherent response to climate forcing.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the 59th Eastern Snow Conference, June 5-7, 2002, Stowe, VT","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"U. S. Army Corps of Engineers","isbn":"9780920081242","usgsCitation":"Huntington, T.G., Dudley, R.W., and Hodgkins, G.A., 2002, Historical trend in ice thickness on the Piscataquis River in central Maine., in Proceedings of the 59th Eastern Snow Conference, June 5-7, 2002, Stowe, VT, p. 299-312.","productDescription":"14 p.","startPage":"299","endPage":"312","costCenters":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"links":[{"id":367484,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":367544,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.easternsnow.org/esc-2002"}],"country":"United States","state":"Maine","otherGeospatial":"Piscataquis River","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Huntington, Thomas G. 0000-0002-9427-3530 thunting@usgs.gov","orcid":"https://orcid.org/0000-0002-9427-3530","contributorId":1884,"corporation":false,"usgs":true,"family":"Huntington","given":"Thomas","email":"thunting@usgs.gov","middleInitial":"G.","affiliations":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":771071,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dudley, Robert W. 0000-0002-0934-0568 rwdudley@usgs.gov","orcid":"https://orcid.org/0000-0002-0934-0568","contributorId":2223,"corporation":false,"usgs":true,"family":"Dudley","given":"Robert","email":"rwdudley@usgs.gov","middleInitial":"W.","affiliations":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":771072,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hodgkins, Glenn A. 0000-0002-4916-5565 gahodgki@usgs.gov","orcid":"https://orcid.org/0000-0002-4916-5565","contributorId":2020,"corporation":false,"usgs":true,"family":"Hodgkins","given":"Glenn","email":"gahodgki@usgs.gov","middleInitial":"A.","affiliations":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":771073,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70258391,"text":"70258391 - 2002 - A flood early warning system for southern Africa","interactions":[],"lastModifiedDate":"2024-09-16T16:01:36.017257","indexId":"70258391","displayToPublicDate":"2002-12-01T10:50:48","publicationYear":"2002","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"A flood early warning system for southern Africa","docAbstract":"Sizeable areas of the Southern African Region experienced widespread flooding in 2000. Deployment of hydrologic models can help reduce the human and economic losses in the regions by providing improved monitoring and forecast information to guide relief activities. In this study, we describe a hydrologic model developed for wide-area flood risk monitoring for the Southern African region. The model is forced by daily estimates of rainfall and evapotranspiration derived from remotely sensed data and assimilation fields. Model predictive skills were verified with data observed stream flow data from locations within the Limpopo basin. The model performed well in simulating the timing and magnitude of the stream flow during a recent episode of flooding in Mozambique in 2000.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Integrated remote sensing at the global, regional, and local scale","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"ISPRS","usgsCitation":"Artan, G.A., Restrepo, M., Asante, K., and Verdin, J., 2002, A flood early warning system for southern Africa, in Integrated remote sensing at the global, regional, and local scale, 6 p.","productDescription":"6 p.","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":434782,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":434781,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.isprs.org/proceedings/XXXIV/part1/","linkFileType":{"id":5,"text":"html"}}],"country":"Mozambique, South Africa","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n 29.34290288445743,\n -22.135533223295766\n ],\n [\n 33.01976593609842,\n -25.466081059632074\n ],\n [\n 35.141784383325216,\n -24.541722931066573\n ],\n [\n 32.295674877395356,\n -21.527094949254916\n ],\n [\n 31.312481654135553,\n -22.34841955234407\n ],\n [\n 29.34290288445743,\n -22.135533223295766\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Artan, Guleid A. 0000-0001-8409-6182 gartan@usgs.gov","orcid":"https://orcid.org/0000-0001-8409-6182","contributorId":2938,"corporation":false,"usgs":true,"family":"Artan","given":"Guleid","email":"gartan@usgs.gov","middleInitial":"A.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":913174,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Restrepo, Miguel","contributorId":344204,"corporation":false,"usgs":true,"family":"Restrepo","given":"Miguel","email":"","affiliations":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"preferred":true,"id":913175,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Asante, Kwabena 0000-0001-5408-1852","orcid":"https://orcid.org/0000-0001-5408-1852","contributorId":344205,"corporation":false,"usgs":true,"family":"Asante","given":"Kwabena","affiliations":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"preferred":true,"id":913176,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Verdin, James 0000-0003-0238-9657 verdin@usgs.gov","orcid":"https://orcid.org/0000-0003-0238-9657","contributorId":145830,"corporation":false,"usgs":true,"family":"Verdin","given":"James","email":"verdin@usgs.gov","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":913177,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70261392,"text":"70261392 - 2002 - Methods and tools for the development of hydrologically conditioned elevation data and derivatives for national applications","interactions":[],"lastModifiedDate":"2024-12-06T16:44:52.847531","indexId":"70261392","displayToPublicDate":"2002-12-01T10:40:53","publicationYear":"2002","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Methods and tools for the development of hydrologically conditioned elevation data and derivatives for national applications","docAbstract":"The National Elevation Dataset (NED) contains the best publicly available elevation data merged into a seamless dataset for the entire United States. In some cases these data contain unwanted artifacts, limiting the quality of standard hydrologic derivatives. The Elevation Derivatives for National Applications (EDNA) project is an interagency effort with the goal of developing a more hydrologically correct version of the NED. This improved NED will be used in the systematic derivation of standard hydrologic derivatives. Methods and tools have recently been developed to facilitate the semiautomatic creation of a hydrologically conditioned NED and hydrologically improved derivatives.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Hydrologic modeling for the 21st Century, Second Federal Interagency Hydrologic Modeling Conference","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Second Federal Interagency Hydrologic Modeling Conference, 2nd, , 28 July 1 - 1 August, 2002","conferenceDate":"July 28-August 1, 2002","conferenceLocation":"Las Vegas, NV","language":"English","publisher":"United States Interagency Advisory Committee on Water Data, the Subcommittee on Hydrology","usgsCitation":"Kost, J.R., Verdin, K.L., Worstell, B.B., and Kelly, G.G., 2002, Methods and tools for the development of hydrologically conditioned elevation data and derivatives for national applications, in Hydrologic modeling for the 21st Century, Second Federal Interagency Hydrologic Modeling Conference, Las Vegas, NV, July 28-August 1, 2002, 12 p.","productDescription":"12 p.","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":464889,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Kost, Jay R. jkost@usgs.gov","contributorId":3931,"corporation":false,"usgs":true,"family":"Kost","given":"Jay","email":"jkost@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":920471,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Verdin, Kristine L. 0000-0002-6114-4660 kverdin@usgs.gov","orcid":"https://orcid.org/0000-0002-6114-4660","contributorId":3070,"corporation":false,"usgs":true,"family":"Verdin","given":"Kristine","email":"kverdin@usgs.gov","middleInitial":"L.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true},{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"preferred":true,"id":920472,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Worstell, Bruce B. 0000-0001-8927-3336 worstell@usgs.gov","orcid":"https://orcid.org/0000-0001-8927-3336","contributorId":1815,"corporation":false,"usgs":true,"family":"Worstell","given":"Bruce","email":"worstell@usgs.gov","middleInitial":"B.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":920473,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kelly, Glenn G.","contributorId":342745,"corporation":false,"usgs":true,"family":"Kelly","given":"Glenn","email":"","middleInitial":"G.","affiliations":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"preferred":false,"id":920474,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":39984,"text":"wri014241 - 2002 - Hydrologic characteristics of selected alluvial aquifers in the North Platte Natural Resources District, western Nebraska","interactions":[],"lastModifiedDate":"2012-02-02T00:10:35","indexId":"wri014241","displayToPublicDate":"2002-12-01T00:00:00","publicationYear":"2002","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":"2001-4241","title":"Hydrologic characteristics of selected alluvial aquifers in the North Platte Natural Resources District, western Nebraska","language":"ENGLISH","doi":"10.3133/wri014241","usgsCitation":"Steele, G.V., Cannia, J.C., and Scripter, K.G., 2002, Hydrologic characteristics of selected alluvial aquifers in the North Platte Natural Resources District, western Nebraska: U.S. Geological Survey Water-Resources Investigations Report 2001-4241, 24 p. : ill., map ; 28 cm., https://doi.org/10.3133/wri014241.","productDescription":"24 p. : ill., map ; 28 cm.","costCenters":[],"links":[{"id":122055,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2001/4241/report-thumb.jpg"},{"id":67746,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2001/4241/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db61165b","contributors":{"authors":[{"text":"Steele, Gregory V. gvsteele@usgs.gov","contributorId":783,"corporation":false,"usgs":true,"family":"Steele","given":"Gregory","email":"gvsteele@usgs.gov","middleInitial":"V.","affiliations":[{"id":464,"text":"Nebraska Water Science Center","active":true,"usgs":true}],"preferred":true,"id":222746,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cannia, James C.","contributorId":94356,"corporation":false,"usgs":true,"family":"Cannia","given":"James","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":222748,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Scripter, Kimberly G.","contributorId":32226,"corporation":false,"usgs":true,"family":"Scripter","given":"Kimberly","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":222747,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":45094,"text":"wri024209 - 2002 - Assessment of possible sources of microbiological contamination and water-quality characteristics of the Jacks Fork, Ozark National Scenic Riverways, Missouri — Phase II","interactions":[],"lastModifiedDate":"2022-01-21T20:28:56.459901","indexId":"wri024209","displayToPublicDate":"2002-12-01T00:00:00","publicationYear":"2002","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":"2002-4209","displayTitle":"Assessment of Possible Sources of Microbiological Contamination and Water-Quality Characteristics of the Jacks Fork, Ozark National Scenic Riverways, Missouri — Phase II","title":"Assessment of possible sources of microbiological contamination and water-quality characteristics of the Jacks Fork, Ozark National Scenic Riverways, Missouri — Phase II","docAbstract":"In 1998, an 8-mile reach of the Jacks Fork was included on Missouri's list of impaired waters as required by Section 303(d) of the Federal Clean Water Act. The identified pollutant on the Jacks Fork was fecal coliform bacteria. Potential sources of fecal contamination to the Jacks Fork include a wastewater treatment plant; campground pit-toilet or septic-system effluent; a large commercial, cross-country horseback trail riding facility; canoeists, boaters, and tubers; and cows.
The U.S. Geological Survey, in cooperation with the National Park Service, conducted a study to better understand the extent and sources of microbiological contamination within the Jacks Fork from Alley Spring to the mouth, which includes the 8-mile 303(d) reach. Identification of the sources would provide the National Park Service and the State of Missouri with the information needed to craft a solution of abatement, regulation, prevention, and mitigation with the end result being the removal of the Jacks Fork from the 303(d) list. Fifteen sites were sampled from November 1999 through December 2000. An additional site was sampled one time. Samples were collected mostly during base-flow conditions during a variety of nonrecreational and recreational season river uses. Samples were analyzed for selected fecal indicator bacteria, physical properties, nutrients, and wastewater organic compounds.
During the sampling period, the whole-body-contact recreation standard for fecal coliform (200 colonies per 100 milliliters of sample) was exceeded at three sites on August 10, 2000, and also at one site on May 11, June 7, and October 3, 2000. Fecal coliform densities and instantaneous loads generally increased from background concentrations at the Eminence site, peaked about 2 river miles downstream, and then decreased until the most downstream site sampled. Generally, the largest densities and loads at sites downstream from Eminence not related to wet-weather flow were observed during a trail ride held August 6 to 12, 2000.
A 24-hour sample collection effort was conducted the weekend of July 15 and 16, 2000, to investigate the effect that large numbers of swimmers, canoeists, and tubers had on fecal coliform densities in the Jacks Fork. Five or six samples were collected at six sites between Saturday morning and the following Sunday afternoon. No fecal coliform density at any of the sites sampled exceeded the whole-body-contact recreation standard.
Because bacteria survive longer in stream-bed sediments than in water, a source of bacteria in the water column could be from resuspension of accumulated bacteria from streambed sediments. Water and streambed-sediment samples were collected at three sites on August 3, 2000, 1 week before a trail ride and again at three sites on August 8, 2000, during a trail ride.
Sixty-five Escherichia coli isolates obtained from water samples collected at 9 sites and 23 Escherichia coli isolates obtained from stream-bed-sediment samples collected at 5 sites were submitted for ribotyping analysis. Samples were collected in 2000 during a variety of nonrecreational and recreational season river uses, including trail rides, canoeing, tubing, and swimming. Of the 65 isolates from water samples, 40 percent were identified as originating from sewage, 29 percent from horse, 11 percent from cow, and 20 percent from an unknown source. Of the 23 isolates from streambed-sediment samples, 39 percent were identified as originating from sewage, 35 percent from horse, 13 percent from cow, and 13 percent from unknown sources.
Analysis of physical property (dissolved oxygen, pH, specific conductance, and temperature) and nutrient (dissolved nitrite plus nitrate and total phosphorus) data indicated that overall few statistically significant differences occurred among the main stem sites of the Jacks Fork. A significant increase in total phosphorus concentrations did occur at site 75 immediately downstream from the Eminence Wastewater Treatment Plant, but the effect diminished quickly downstream. Unlike fecal coliform bacteria, most variations in physical property values or nutrient concentrations were related to seasonal changes, time of day the sample was collected, or hydrologic conditions and not to certain recreational activities.
Trace quantities of wastewater organic compounds were detected in all waters sampled for these constituents. Two of the compounds were detected in associated laboratory blanks, and other detected compounds have sources other than sewage effluent. The best indicators of municipal or domestic sewage effluent were the non-ionic detergent metabolites (nonylphenol monoethoxylate, octylphenol monoethoxylate, and para-nonylphenol), phenol, and caffeine; but possible sources of these compounds, which were detected in one or more of the samples, could be the numerous campers, swimmers, and canoeists that were present when the samples were collected.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri024209","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Davis, J., and Richards, J.M., 2002, Assessment of possible sources of microbiological contamination and water-quality characteristics of the Jacks Fork, Ozark National Scenic Riverways, Missouri — Phase II: U.S. Geological Survey Water-Resources Investigations Report 2002-4209, iv, 43 p., https://doi.org/10.3133/wri024209.","productDescription":"iv, 43 p.","numberOfPages":"45","costCenters":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"links":[{"id":135357,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2002/4209/coverthb.jpg"},{"id":360412,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4209/wrir20024209.pdf","text":"Report","size":"1.77 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRIR 2002–4209"},{"id":394690,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_53968.htm"}],"country":"United States","state":"Missouri","otherGeospatial":"Jacks Fork, Ozark National Scenic Riverways","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -91.45,\n 37.1447\n ],\n [\n -91.2719,\n 37.1447\n ],\n [\n -91.2719,\n 37.1917\n ],\n [\n -91.45,\n 37.1917\n ],\n [\n -91.45,\n 37.1447\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"Director, Central Midwest Water Science Center
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The recent discovery of pharmaceuticals in streams across the United States (Kolpin and others, 2002) has raised the visibility and need for monitoring of antibiotics in the environment. Possible sources of antibiotics and other pharmaceuticals in streams may include fish hatcheries. This fact sheet presents the results from a preliminary study of fish hatcheries across the United States for the occurrence and concentration of antibiotics present in fish hatchery water. The study examines both sufonamides and tetracyclines. Sulfonamides are synthetic compounds, and tetracyclines are naturally occurring compounds. The use of antibiotics added to specially formulated feed is a common practice in fish hatcheries to treat and prevent bacterial infections in large fish populations. U.S. Food and Drug Administration (FDA) approved antibiotics are oxytetracycline-HCI, sulfamerazine, and a combination drug containing ormetoprim and sulfadiamethoxine (U.S. Food and Drug Administration, 2003). During January 2001–June 2002, the U.S. Geological Survey (USGS) Organic Geochemistry Research Laboratory (OGRL), Lawrence, Kansas, cooperatively collected water samples from 13 fish hatcheries across the United States (fig. 1) with the assistance of hatchery operators. A method for the analysis of antibiotics was developed and used to identify and quantify these compounds in fish hatchery water (Lindsey and others, 2001). This study was completed to determine if trace levels of antibiotics [approximately 1 microgram per liter (μg/L) or 1 part per billion or greater occurred] in which water associated with fish hatcheries, which are a potential source of these compounds in surface water.
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U.S. Geological Survey
1217 Biltmore Drive
Lawrence, KS 66049
Acidic waters containing elevated concentrations of dissolved metals have contaminated the regional aquifer in the Pinal Creek Basin, which is in Gila County, Arizona, about 100 kilometers east of Phoenix. The aquifer is made up of two geologic units: unconsolidated stream alluvium and consolidated basin fill. To better understand how contaminants are transported through these units, a better understanding of the distribution of hydraulic conductivity and processes that affect it within the aquifer is needed.
\nSlug tests were done in September 1997 and October 1998 on 9 wells finished in the basin fill and 14 wells finished in the stream alluvium. Data from the tests were analyzed by using either the Bouwer and Rice (1976) method, or by using an extension to the method developed by Springer and Gellhar (1991). Both methods are applicable for unconfined aquifers and partially penetrating wells. The results of the analyses show wide variability within and between the two geologic units. Hydraulic conductivity estimates ranged from 0.5 to 250 meters per day for the basin fill and from 3 to 200 meters per day for the stream alluvium. Results of the slug tests also show a correlation coefficient of 0.83 between the hydraulic conductivity and the pH of the ground water. The areas of highest hydraulic conductivity coincide with the areas of lowest pH, and the areas of lowest hydraulic conductivity coincide with the areas of highest pH, suggesting that the acidic water is increasing the hydraulic conductivity of the aquifer by dissolution of carbonate minerals.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Tucson, AZ","doi":"10.3133/wri024205","usgsCitation":"Angeroth, C.E., 2002, Characterization of hydraulic conductivity of the alluvium and basin fill, Pinal Creek Basin near Globe, Arizona: U.S. Geological Survey Water-Resources Investigations Report 2002-4205, iv, 25 p., https://doi.org/10.3133/wri024205.","productDescription":"iv, 25 p.","numberOfPages":"30","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":288422,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4205/report.pdf"},{"id":288423,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","country":"United States","state":"Arizona","city":"Globe","otherGeospatial":"Pinal Creek Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.0,33.25 ], [ -111.0,33.583333 ], [ -110.75,33.583333 ], [ -110.75,33.25 ], [ -111.0,33.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4e4d","contributors":{"authors":[{"text":"Angeroth, Cory E. 0000-0002-2915-6418 angeroth@usgs.gov","orcid":"https://orcid.org/0000-0002-2915-6418","contributorId":2105,"corporation":false,"usgs":true,"family":"Angeroth","given":"Cory","email":"angeroth@usgs.gov","middleInitial":"E.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":222670,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44692,"text":"fs14102 - 2002 - Effects of wildfire on the hydrology of Frijoles and Capulin canyons in and near Bandelier National Monument, New Mexico","interactions":[],"lastModifiedDate":"2019-03-12T10:38:23","indexId":"fs14102","displayToPublicDate":"2002-12-01T00:00:00","publicationYear":"2002","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":"141-02","displayTitle":"Effects of Wildfire on the Hydrology of Frijoles and Capulin Canyons in and near Bandelier National Monument, New Mexico","title":"Effects of wildfire on the hydrology of Frijoles and Capulin canyons in and near Bandelier National Monument, New Mexico","docAbstract":"In June 1977, the La Mesa wildfire burned 15,270 acres in and near Frijoles Canyon in Bandelier National Monument (BNM) and the adjacent Santa Fe National Forest, New Mexico. In April 1996, the Dome wildfire in BNM burned 16,516 acres in and near Capulin Canyon and the surrounding Dome Wilderness area. Both Frijoles and Capulin Canyon watersheds are characterized by archeological artifacts that could be affected by increased runoff and accelerated rates of erosion, which typically occur after a fire. In response to this concern, the U.S. Geological Survey (USGS), in cooperation with the National Park Service, conducted a study to monitor and document the wildfire effects on streamflow after the 1996 Dome fire.
","language":"English","publisher":"U.S. Geological Survey ","publisherLocation":"Reston, VA","doi":"10.3133/fs14102","usgsCitation":"Veenhuis, J.E., and Bowman, P.R., 2002, Effects of wildfire on the hydrology of Frijoles and Capulin canyons in and near Bandelier National Monument, New Mexico: U.S. Geological Survey Fact Sheet 141-02, 4 p., https://doi.org/10.3133/fs14102.","productDescription":"4 p.","costCenters":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"links":[{"id":122575,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2002/0141/report-thumb.jpg"},{"id":359786,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2002/0141/fs14102.pdf","text":"Report","size":"1.69 MB","linkFileType":{"id":1,"text":"pdf"}}],"contact":"Director, New Mexico Water Science Center
U.S. Geological Survey
6700 Edith Blvd NE
Albuquerque, NM 87113
Microbial activity is responsible for the transformation of at least one third of the elements in the periodic table. These transformations are the result of assimilatory, dissimilatory, or detoxification processes and form the cornerstones of many biogeochemical cycles. Arsenic and selenium are two elements whose roles in microbial ecology have only recently been recognized. Known as \"essential toxins\", they are required in trace amounts for growth and metabolism but are toxic at elevated concentrations. Arsenic is used as an osmolite in some marine organisms while selenium is required as selenocysteine (i.e. the twenty-first amino acid) or as a ligand to metal in some enzymes (e.g. FeNiSe hydrogenase). Arsenic resistance involves a small-molecular-weight arsenate reductase (ArsC). The use of arsenic and selenium oxyanions for energy is widespread in prokaryotes with representative organisms from the Crenarchaeota, thermophilic bacteria, low and high G+C gram-positive bacteria, and Proteobacteria. Recent studies have shown that both elements are actively cycled and play a significant role in carbon mineralization in certain environments. The occurrence of multiple mechanisms involving different enzymes for arsenic and selenium transformation indicates several different evolutionary pathways (e.g. convergence and lateral gene transfer) and underscores the environmental significance and selective impact in microbial evolution of these two elements.
","language":"English","publisher":"Springer","doi":"10.1007/s10123-002-0091-y","usgsCitation":"Stolz, J., Basu, P., and Oremland, R., 2002, Microbial transformation of elements: The case of arsenic and selenium: International Microbiology , v. 5, no. 4, p. 201-207, https://doi.org/10.1007/s10123-002-0091-y.","productDescription":"7 p.","startPage":"201","endPage":"207","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":478604,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://revistes.iec.cat/index.php/IM/article/view/9383","text":"External Repository"},{"id":338374,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58da251ce4b0543bf7fda816","contributors":{"authors":[{"text":"Stolz, J.","contributorId":189866,"corporation":false,"usgs":false,"family":"Stolz","given":"J.","affiliations":[],"preferred":false,"id":686295,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Basu, P.","contributorId":35527,"corporation":false,"usgs":true,"family":"Basu","given":"P.","email":"","affiliations":[],"preferred":false,"id":686296,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Oremland, R.","contributorId":26831,"corporation":false,"usgs":true,"family":"Oremland","given":"R.","email":"","affiliations":[],"preferred":false,"id":686297,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70185177,"text":"70185177 - 2002 - Comparison of formation and fluid-column logs in a heterogeneous basalt aquifer","interactions":[],"lastModifiedDate":"2018-11-26T08:53:16","indexId":"70185177","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Comparison of formation and fluid-column logs in a heterogeneous basalt aquifer","docAbstract":"Deep observation boreholes in the vicinity of active production wells in Honolulu, Hawaii, exhibit the anomalous condition that fluid-column electrical conductivity logs and apparent profiles of pore-water electrical conductivity derived from induction conductivity logs are nearly identical if a formation factor of 12.5 is assumed. This condition is documented in three boreholes where fluid-column logs clearly indicate the presence of strong borehole flow induced by withdrawal from partially penetrating water-supply wells. This result appears to contradict the basic principles of conductivity-log interpretation. Flow conditions in one of these boreholes was investigated in detail by obtaining flow profiles under two water production conditions using the electromagnetic flowmeter. The flow-log interpretation demonstrates that the fluid-column log resembles the induction log because the amount of inflow to the borehole increases systematically upward through the transition zone between deeper salt water and shallower fresh water. This condition allows the properties of the fluid column to approximate the properties of water entering the borehole as soon as the upflow stream encounters that producing zone. Because this condition occurs in all three boreholes investigated, the similarity of induction and fluid-column logs is probably not a coincidence, and may relate to aquifer response under the influence of pumping from production wells.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.2002.tb02544.x","usgsCitation":"Paillet, F., Williams, J., Oki, D., and Knutson, K.D., 2002, Comparison of formation and fluid-column logs in a heterogeneous basalt aquifer: Groundwater, v. 40, no. 6, p. 577-585, https://doi.org/10.1111/j.1745-6584.2002.tb02544.x.","productDescription":"9 p. ","startPage":"577","endPage":"585","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":337682,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"40","issue":"6","noUsgsAuthors":false,"publicationDate":"2005-12-13","publicationStatus":"PW","scienceBaseUri":"58ca52d4e4b0849ce97c86ec","contributors":{"authors":[{"text":"Paillet, F.L.","contributorId":189369,"corporation":false,"usgs":false,"family":"Paillet","given":"F.L.","email":"","affiliations":[],"preferred":false,"id":684616,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, J.H.","contributorId":29482,"corporation":false,"usgs":true,"family":"Williams","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":684617,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Oki, D.S.","contributorId":75184,"corporation":false,"usgs":true,"family":"Oki","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":684618,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Knutson, K. D.","contributorId":31790,"corporation":false,"usgs":true,"family":"Knutson","given":"K.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":684619,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":51126,"text":"ofr02324 - 2002 - Digital soils survey map of the Patagonia Mountains, Arizona","interactions":[],"lastModifiedDate":"2014-03-13T13:04:19","indexId":"ofr02324","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-324","title":"Digital soils survey map of the Patagonia Mountains, Arizona","docAbstract":"The ‘Soil Survey of Santa Cruz and Parts of Cochise\n and Pima Counties, Arizona,' a product of the USDA’s\n Soil Conservation Service and the Forest Service in\n cooperation with the Arizona Agricultural Experiment\n Station, released in 1979, was created according to\n the site conditions in 1971, when soil scientists\n identified soils types on aerial photographs. The\n scale at which these maps were published is 1:20,000.
\nThese soil maps were automated for incorporation into\n the hydrologic modeling within a GIS. The aerial photos\n onto which the soils units were drawn had not been\n orthoganalized, and contained distortion. A total of 15\n maps composed the study area. These maps were scanned\n into TIFF format using an 8-bit black and white drum\n scanner at 100 dpi. The images were imported into ERDAS\n IMAGINE and the white borders were removed through\n subset decollaring processes. Five CD-ROM’s containing\n Digital Orthophoto Quarter Quads (DOQQ’s) were used to\n register and rectify the scanned soils maps. Polygonal\n data was then attributed according to the datasets.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02324","usgsCitation":"Norman, L., Wissler, C., Guertin, D.P., and Gray, F., 2002, Digital soils survey map of the Patagonia Mountains, Arizona: U.S. Geological Survey Open-File Report 2002-324, Report: 24 p.; Readme; Metadata; Dataset; Legend; Map: JPG format, https://doi.org/10.3133/ofr02324.","productDescription":"Report: 24 p.; Readme; Metadata; Dataset; Legend; Map: JPG format","additionalOnlineFiles":"Y","costCenters":[{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"links":[{"id":179138,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02324.jpg"},{"id":4513,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0324/","linkFileType":{"id":5,"text":"html"}},{"id":283898,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/2002/0324/00readme.txt"},{"id":283899,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2002/0324/scs_soil.met"},{"id":283900,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0324/pdf/scs_soil.pdf"},{"id":283901,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2002/0324/scs_soil.e00"},{"id":283902,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2002/0324/scs_soil.avl"},{"id":283903,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2002/0324/images/scs_soil.jpg"}],"scale":"35000","projection":"Universal Transverse Mercator","datum":"North American Datum of 1983","country":"United States","state":"Arizona","otherGeospatial":"Patagonia Mountains","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.864671,31.348635 ], [ -110.864671,31.536392 ], [ -110.642353,31.536392 ], [ -110.642353,31.348635 ], [ -110.864671,31.348635 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651835","contributors":{"authors":[{"text":"Norman, Laura","contributorId":90382,"corporation":false,"usgs":true,"family":"Norman","given":"Laura","affiliations":[],"preferred":false,"id":242995,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wissler, Craig","contributorId":16912,"corporation":false,"usgs":true,"family":"Wissler","given":"Craig","affiliations":[],"preferred":false,"id":242993,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Guertin, D. Phillip","contributorId":46062,"corporation":false,"usgs":false,"family":"Guertin","given":"D.","email":"","middleInitial":"Phillip","affiliations":[{"id":12625,"text":"School of Natural Resources and the Environment, University of Arizona, Tucson, AZ, 85721, USA","active":true,"usgs":false}],"preferred":false,"id":242994,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gray, Floyd 0000-0002-0223-8966 fgray@usgs.gov","orcid":"https://orcid.org/0000-0002-0223-8966","contributorId":603,"corporation":false,"usgs":true,"family":"Gray","given":"Floyd","email":"fgray@usgs.gov","affiliations":[{"id":662,"text":"Western Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":242992,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ]}