This report presents the results of the U.S. Geological Survey's analytical evaluation program for seven standard reference samples -- T-155 (trace constituents), M-148 (major constituents), N-59 (nutrient constituents), N-60 (nutrient constituents), P-31 (low ionic strength constituents), GWT-4 (ground-water trace constituents), and Hg- 27 (mercury) -- which were distributed in September 1998 to 162 laboratories enrolled in the U.S. Geological Survey sponsored interlaboratory testing program. Analytical data that were received from 136 of the laboratories were evaluated with respect to overall laboratory performance and relative laboratory performance for each analyte in the seven reference samples. Results of these evaluations are presented in tabular form. Also presented are tables and graphs summarizing the analytical data provided by each laboratory for each analyte in the seven standard reference samples. The most probable value for each analyte was determined using nonparametric statistics.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr9972","usgsCitation":"Farrar, J.W., 1999, Results of the U.S. Geological Survey's Analytical Evaluation Program for standard reference samples: T-155 (trace constituents), M-148 (major constituents), N-59 (nutrient constituents), N-60 (nutrient constituents), P-31 (low ionic strength constituents), GWT-4 (ground-water trace constituents) and Hg-27 (Mercury) distributed in September 1998: U.S. Geological Survey Open-File Report 99-72, iii, 143 p., https://doi.org/10.3133/ofr9972.","productDescription":"iii, 143 p.","costCenters":[],"links":[{"id":345731,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0072/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162032,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0072/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db60556b","contributors":{"authors":[{"text":"Farrar, Jerry W.","contributorId":102067,"corporation":false,"usgs":true,"family":"Farrar","given":"Jerry","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":241127,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24320,"text":"ofr99607 - 1999 - Hydrologic data for the Columbia/Eagle Bluffs Wetland Complex, Columbia, Missouri-1993-96","interactions":[],"lastModifiedDate":"2022-04-26T23:05:57.413823","indexId":"ofr99607","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1999","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":"99-607","title":"Hydrologic data for the Columbia/Eagle Bluffs Wetland Complex, Columbia, Missouri-1993-96","docAbstract":"The U.S. Geological Survey, in cooperation with the Missouri Department of Conservation and the city of Columbia, Missouri, collected hydrologic data from September 1993 through October 1996 as part of a hydrologic characterization of the Columbia/Eagle Bluffs Wetland Complex. The wetland complex was constructed in the Missouri River alluvial plain adjacent to the Columbia municipal supply wells. Part of the wetland complex was designed to treat sewage effluent from Columbia, with the treated effluent being used as the primary water source for wetland management practices on the Eagle Bluffs Wildlife Area. This report presents hydrologic data and the procedures used to collect the data, which include water-quality analyses of samples collected quarterly from 28 wells and 2 surface-water sites. Four additional wells were incorporated into the monitoring network in November 1994 and also were sampled quarterly. Data from these 4 wells also are included.
Water samples were analyzed for specific conductance, pH, temperature, dissolved oxygen, bacteria, alkalinity, major cations and anions, nutrients, trace elements, and total and dissolved organic carbon. Dissolved nitrite plus nitrate as nitrogen concentrations were equal to or less than 5.2 milligrams per liter for all ground-water samples and were equal to or less than 2.7 milligrams per liter in surface-water samples. Dissolved phosphorous concentrations ranged from less than 0.01 to 2.2 milligrams per liter in the ground-water samples, and from less than 0.01 to 0.19 milli-grams per liter in the surface-water samples. Fecal coliform bacteria counts ranged from less than 1 to 39 colonies per 100 milliliters for ground-water samples, and from 1 to greater than 6,000 colonies per 100 milliliters for surface-water samples. Fecal streptococcus bacteria counts ranged from less than 1 to 92 colonies per 100 milliliters for ground-water samples, and from 2 to greater than 10,000 colonies per 100 milliliters for surface-water samples. Samples for well USGS-6 had dissolved arsenic concentrations that exceeded 50 micrograms per liter. Dissolved manganese concentrations exceeded 50 micrograms per liter at least once for each site except for USGS-9S. Dissolved iron concentrations exceeded 300 micro-grams per liter at least once for 28 of 34 sites.
Samples from 8 of the 32 wells and both surface-water sites were analyzed for base/neutral/ acid semi-volatile organic compounds, selected pesticides, selected organochlorine compounds, and purgeable volatile organic compounds. All but one of the organic compounds detected in the samples collected from the monitoring wells or surface-water sites were pesticides. Atrazine was detected consistently at both surface-water sites. Other frequently detected pesticides include metolachlor, diazinon, chlorpyrifos, prometon, and simazine.
Following the 1993 Missouri River flood samples of residual flood water and flood-deposited sediments were collected from the Columbia/ Eagle Bluffs Wetland Complex. A brief description of the flooding and damage to the study area is presented. Methods of collection of the four residual flood water and the four flood-deposited sediment samples, as well as the analytical results of these samples, are included in this report. Data from two continuous water-level recorders and from quarterly water-level measurements in wells also are included.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr99607","collaboration":"Prepared in cooperation with the Missouri Department of Conservation and the City of Columbia","usgsCitation":"Richards, J.M., 1999, Hydrologic data for the Columbia/Eagle Bluffs Wetland Complex, Columbia, Missouri-1993-96: U.S. Geological Survey Open-File Report 99-607, iii, 91 p., https://doi.org/10.3133/ofr99607.","productDescription":"iii, 91 p.","costCenters":[],"links":[{"id":399723,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0607/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156176,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0607/report-thumb.jpg"}],"country":"United States","state":"Missouri","city":"Columbia","otherGeospatial":"Columbia/Eagle Bluffs Wetland Complex","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -92.4667,\n 38.8194\n ],\n [\n -92.3844,\n 38.8194\n ],\n [\n -92.3844,\n 38.9056\n ],\n [\n -92.4667,\n 38.9056\n ],\n [\n -92.4667,\n 38.8194\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60eb3d","contributors":{"authors":[{"text":"Richards, Joseph M. 0000-0002-9822-2706 richards@usgs.gov","orcid":"https://orcid.org/0000-0002-9822-2706","contributorId":2370,"corporation":false,"usgs":true,"family":"Richards","given":"Joseph","email":"richards@usgs.gov","middleInitial":"M.","affiliations":[{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":191688,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":50160,"text":"ofr98629 - 1999 - A temporal and spatial analysis of ground-water levels for effective monitoring in Huron County, Michigan","interactions":[],"lastModifiedDate":"2016-10-06T16:05:48","indexId":"ofr98629","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1999","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":"98-629","title":"A temporal and spatial analysis of ground-water levels for effective monitoring in Huron County, Michigan","docAbstract":"Quarterly water-level measurements were analyzed to assess the effectiveness of a monitoring network of 26 wells in Huron County, Michigan. Trends were identified as constant levels and autoregressive components were computed at all wells on the basis of data collected from 1993 to 1997, using structural time series analysis. Fixed seasonal components were identified at 22 wells and outliers were identified at 23 wells. The 95- percent confidence intervals were forecast for water-levels during the first and second quarters of 1998. Intervals in the first quarter were consistent with 92.3 percent of the measured values. In the second quarter, measured values were within the forecast intervals only 65.4 percent of the time. Unusually low precipitation during the second quarter is thought to have contributed to the reduced reliability of the second-quarter forecasts.
Spatial interrelations among wells were investigated on the basis of the autoregressive components, which were filtered to create a set of innovation sequences that were temporally uncorrelated. The empirical covariance among the innovation sequences indicated both positive and negative spatial interrelations. The negative covariance components are considered to be physically implausible and to have resulted from random sampling error. Graphical modeling, a form of multivariate analysis, was used to model the covariance structure. Results indicate that only 29 of the 325 possible partial correlations among the water-level innovations were statistically significant. The model covariance matrix, corresponding to the model partial correlation structure, contained only positive elements. This model covariance was sequentially partitioned to compute a set of partial covariance matrices that were used to rank the effectiveness of the 26 monitoring wells from greatest to least. Results, for example, indicate that about 50 percent of the uncertainty of the water-level innovations currently monitored by the 26- well network could be described by the 6 most effective wells.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/ofr98629","collaboration":"Prepared in cooperation with Huron County, Michigan","usgsCitation":"Holtschlag, D.J., and Sweat, M., 1999, A temporal and spatial analysis of ground-water levels for effective monitoring in Huron County, Michigan: U.S. Geological Survey Open-File Report 98-629, ii, 24 p., https://doi.org/10.3133/ofr98629.","productDescription":"ii, 24 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":175412,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr98629.JPG"},{"id":7902,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://mi.water.usgs.gov/reports/Holtschlag12.html","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Michigan","county":"Huron 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David J. 0000-0001-5185-4928 dholtschlag@usgs.gov","orcid":"https://orcid.org/0000-0001-5185-4928","contributorId":5447,"corporation":false,"usgs":true,"family":"Holtschlag","given":"David","email":"dholtschlag@usgs.gov","middleInitial":"J.","affiliations":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"preferred":true,"id":240870,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sweat, M.J.","contributorId":90786,"corporation":false,"usgs":true,"family":"Sweat","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":240871,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":23734,"text":"ofr99346 - 1999 - An evaluation of alternative chemical classifications of sandstones","interactions":[],"lastModifiedDate":"2017-03-09T15:01:40","indexId":"ofr99346","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1999","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":"99-346","title":"An evaluation of alternative chemical classifications of sandstones","docAbstract":"Chemical classification of sandstone is worth attempting because modern analytical methods are producing extensive data sets on rock composition. Previous compilations and statistical studies have demonstrated the application of chemical data to problems in sandstone petrology, but classification has been largely ignored. Chemical data has value for classification, but the limitations of using chemical data for classification must be identified. Consideration of the processes of sandstone formation permits formulation of classification guidelines and systems for classification. Alternative systems for chemical classification can be then evaluated for their power to identify major types of sandstones and to facilitate genetic interpretation.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr99346","issn":"0094-9140","usgsCitation":"Lindsey, D.A., 1999, An evaluation of alternative chemical classifications of sandstones: U.S. Geological Survey Open-File Report 99-346, 28 cm, https://doi.org/10.3133/ofr99346.","productDescription":"28 cm","costCenters":[],"links":[{"id":156799,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0346/report-thumb.jpg"},{"id":52974,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0346/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":1749,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1999/ofr-99-0346/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db6849e9","contributors":{"authors":[{"text":"Lindsey, D. A.","contributorId":49814,"corporation":false,"usgs":true,"family":"Lindsey","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":190621,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23832,"text":"ofr99361S - 1999 - Manual del McVCO 1999","interactions":[],"lastModifiedDate":"2014-06-02T09:52:18","indexId":"ofr99361S","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1999","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":"99-361","chapter":"S","title":"Manual del McVCO 1999","docAbstract":"El McVCO es un generador de frecuencias basado en un microcontrolador que reemplaza al oscilador controlado por voltaje (VCO) utilizado en telemetría analógica de datos sísmicas. Acepta señales de baja potencia desde un sismómetro y produce una señal subportadora modulada en frecuencia adecuada para enlaces telefónicos o vía radio a un lugar remoto de recolección de datos. La frecuencia de la subportadora y la ganancia pueden ser seleccionadas mediante un interruptor. Tiene la opción de poder operar con dos canales para la observación con ganancia alta y baja.\n\nEl McVCO fue diseñado con el propósito de mejorar la telemetría analógica de las señales dentro de la Pacific Northwest Seismograph Network (PNSN) (Red Sismográfica del Noroeste del Pacífico). Su desarrollo recibió el respaldo del Programa de Geofísica de la Universidad de Washington y del \"Volcano Hazards and Earthquake Hazards programs of the United States Geological Survey (USGS) (Programa de Investigaciones de Riesgos Volcánicos y Programa de Investigaciones de Riesgos Sísmicos de los EEUU). Cientos de instrumentos se han construido e instalado. Además de utilizarlo el PNSN, el McVCO es usado por el Observatorio Vulcanológico de Alaska para monitorear los volcanes aleutianos y por el USGS Volcano Disaster Assistance Program (Programa de Ayuda en las Catástrofes Volcánicas del USGS) para responder a crisis volcánicas en otros países.\n\nEste manual cubre el funcionamiento del McVCO, es una referencia técnica para aquellos que necesitan saber con más detalle cómo funciona el McVCO, y cubre una serie de temas que requieren un trato explícito o que derivan del despliegue del instrumento.","language":"Spanish","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr99361S","issn":"0094-9140","collaboration":"This report is also available in English at OFR 99-361.","usgsCitation":"McChesney, P., 1999, Manual del McVCO 1999: U.S. Geological Survey Open-File Report 99-361, 57 p., https://doi.org/10.3133/ofr99361S.","productDescription":"57 p.","numberOfPages":"57","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":156547,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr99361S.jpg"},{"id":1571,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1999/0361s/","linkFileType":{"id":5,"text":"html"}},{"id":284906,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0361s/pdf/OF99-361s.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64aea1","contributors":{"authors":[{"text":"McChesney, P.J.","contributorId":29470,"corporation":false,"usgs":true,"family":"McChesney","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":190822,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24278,"text":"ofr99269 - 1999 - Water-level data for the Albuquerque Basin and adjacent areas, New Mexico, period of record through 1998","interactions":[],"lastModifiedDate":"2019-03-08T09:28:40","indexId":"ofr99269","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1999","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":"99-269","displayTitle":"Water-Level Data for the Albuquerque Basin and Adjacent Areas, New Mexico, Period of Record through 1998","title":"Water-level data for the Albuquerque Basin and adjacent areas, New Mexico, period of record through 1998","docAbstract":"The Albuquerque Basin, located in central New Mexico, is about \r\n100 miles long and 25 to 40 miles wide. The basin is defined \r\nas the extent of Cenozoic deposits that encompass the structural \r\nRio Grande Rift within the basin. Drinking-water supplies \r\nthroughout the Albuquerque Basin are obtained solely from ground-\r\nwater resources. The population of the basin grew from 419,000 in \r\n1980 to 563,600 in 1990, a 34-percent increase, and resulted in \r\nincreases in water demand and ground-water pumpage. From April \r\n1982 through September 1983, a network of wells was established \r\nto monitor changes in ground-water levels throughout the Albuquerque \r\nBasin. Water-level data are currently (1998) collected at 88 \r\nwells and piezometers. This report includes water-level data from \r\nmost of these sites for the period of record through 1998. Data \r\ncollection at sites 6, 21, 27-29, 31, 35, 56-60, 77, 87, and 88 was \r\ninterrupted due to construction or limited access, and does not \r\nextend through the reporting period. Data are currently \r\ncollected annually at sites 11 and 56-60; semiannually at sites \r\n1-10, 78, and 85; quarterly at sites 12-55, 67-77, 79, 80, 82-84, \r\n87, and 88; and monthly at sites 61-63, 81, and 86. Water levels \r\nare recorded hourly at sites 64-66.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr99269","issn":"0094-9140","collaboration":"Prepared in cooperation with the City of Albuquerque","usgsCitation":"Rankin, D.R., 1999, Water-level data for the Albuquerque Basin and adjacent areas, New Mexico, period of record through 1998: U.S. Geological Survey Open-File Report 99-269, iv, 27 p., https://doi.org/10.3133/ofr99269.","productDescription":"iv, 27 p.","numberOfPages":"33","costCenters":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"links":[{"id":155039,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0269/report-thumb.jpg"},{"id":95511,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0269/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"contact":"Director, New Mexico Water Science Center
U.S. Geological Survey
6700 Edith Blvd NE
Albuquerque, NM 87113
It is now well documented that impoundment of natural waters, with inundation of terrestrial area, results in enhanced conversion of inorganic mercury to methylmercury, a form that is toxic and bioaccumulates to a greater extent than inorganic mercury. Concentrations of mercury, methylmercury, and other water-quality constituents are reported from water sampled from flood-control impoundments and natural (unimpounded) waters of the Red River of the North Basin from 1997-99.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Mounds View, MN","doi":"10.3133/ofr99273A","issn":"0094-9140","collaboration":"Prepared in cooperation with the Red River Watershed Management Board and the Minnesota Pollution Control Agency","usgsCitation":"Brigham, M.E., Olson, M.L., and DeWild, J.F., 1999, Mercury, methylmercury, and other water-quality data from flood-control impoundments and natural waters of the Red River of the North Basin, Minnesota, 1997-99: U.S. Geological Survey Open-File Report 99-273, iii, 34 p., https://doi.org/10.3133/ofr99273A.","productDescription":"iii, 34 p.","numberOfPages":"37","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":155192,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0273a/report-thumb.jpg"},{"id":52049,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0273a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","otherGeospatial":"Red River of the North Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -95.44097900390625,\n 48.99463598353408\n ],\n [\n -95.4052734375,\n 48.95858066440977\n ],\n [\n -95.4327392578125,\n 48.927913136732556\n ],\n [\n -95.44921875,\n 48.90625412315376\n ],\n [\n -95.4766845703125,\n 48.88819777098229\n ],\n [\n -95.4876708984375,\n 48.855679899769\n ],\n [\n -95.49316406249999,\n 48.832181625698475\n ],\n [\n -95.42999267578125,\n 48.81590713080018\n 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Minerals-related permits on national forests, 1967 to 1998","interactions":[{"subject":{"id":32273,"text":"ofr99414B - 1999 - Geologic datasets for weights-of-evidence analysis in northeast Washington: 3. Minerals-related permits on national forests, 1967-1998","indexId":"ofr99414B","publicationYear":"1999","noYear":false,"chapter":"B","title":"Geologic datasets for weights-of-evidence analysis in northeast Washington: 3. Minerals-related permits on national forests, 1967-1998"},"predicate":"IS_PART_OF","object":{"id":22524,"text":"ofr99414A - 1999 - Geologic datasets for weights of evidence analysis in northeast Washington: 3. Minerals-related permits on national forests, 1967 to 1998","indexId":"ofr99414A","publicationYear":"1999","noYear":false,"chapter":"A","title":"Geologic datasets for weights of evidence analysis in northeast Washington: 3. 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Permits for these activities require filing at the Forest Service a Notice of Intention (Notice) to conduct mineral exploration activities and (or) a Plan of Operation (Plan). A Plan of Operation is required is significant activities are anticipated. This compilation of Notices and Plans for the Colville, Kaniksu, Okanogan, and Wenatchee National Forests between 1967 and 1998 is intended for use in combination with geologic and economic information to predict future mineral-related activities in the region.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr99414A","issn":"0094-9140","usgsCitation":"Boleneus, D., 1999, Geologic datasets for weights of evidence analysis in northeast Washington: 3. Minerals-related permits on national forests, 1967 to 1998: U.S. Geological Survey Open-File Report 99-414, Report: PDF, 32 p.; Report: DOC; Readme; Metadata; Data files; Location map, https://doi.org/10.3133/ofr99414A.","productDescription":"Report: PDF, 32 p.; Report: DOC; Readme; Metadata; Data files; Location map","numberOfPages":"32","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":285017,"rank":6,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr99414A.jpg"},{"id":154340,"rank":1,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/1999/0414a/of99-414.doc"},{"id":1302,"rank":7,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1999/0414a/","linkFileType":{"id":5,"text":"html"}},{"id":52029,"rank":8,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0414a/pdf/of99-414.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":285013,"rank":5,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/1999/0414a/readme.txt"},{"id":285014,"rank":3,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/1999/0414a/of99-414.met"},{"id":285015,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/1999/0414a/of99-414.xls"},{"id":285016,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1999/0414a/images/of99-414.jpg","text":"Plate 1"}],"country":"United States","state":"Washington","otherGeospatial":"Colville National Forest, Kaniksu National Forest, Okanogan National Forest, Wenatchee National Forest","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -121.25,47.25 ], [ -121.25,49.0 ], [ -117.0,49.0 ], [ -117.0,47.25 ], [ -121.25,47.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e92e","contributors":{"authors":[{"text":"Boleneus, D. 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This \r\nsimulation was done by the U.S. Geological Survey in cooperation \r\nwith the U.S. Department of the Army, U.S. Army Air Defense \r\nArtillery Center and Fort Bliss, El Paso, Texas. The U.S. \r\nEnvironmental Protection Agency-developed Hydrologic Evaluation of \r\nLandfill Performance (HELP) and Multimedia Exposure Assessment \r\n(MULTIMED) computer models were used to simulate the production of \r\nleachate by a landfill and transport of landfill leachate to \r\nthe water table. Model input data files used with and output files \r\ngenerated by the HELP and MULTIMED models are provided in ASCII \r\nformat on a 3.5-inch 1.44-megabyte IBM-PC compatible floppy disk.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr98397","issn":"0094-9140","usgsCitation":"Abeyta, C.G., and Frenzel, P.F., 1999, Model input and output files for the simulation of time of arrival of landfill leachate at the water table, Municipal Solid Waste Landfill Facility, U.S. Army Air Defense Artillery Center and Fort Bliss, El Paso County, Texas (Supplement to WRI 97–4036): U.S. Geological Survey Open-File Report 98-397, iv, 4 leaves ;28 cm. +1 computer disk (3 1/2 in.), https://doi.org/10.3133/ofr98397.","productDescription":"iv, 4 leaves ;28 cm. +1 computer disk (3 1/2 in.)","costCenters":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"links":[{"id":155349,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Supplement to WRI 97–4036","contact":"Director, New Mexico Water Science Center
U.S. Geological Survey
6700 Edith Blvd NE
Albuquerque, NM 87113
The Planning Team for the U.S. Geological Survey (USGS) National Water-Quality Assessment (NAWQA) Program defines a successful NAWQA Program as one that makes a balanced contribution to study-unit issues, national issues, and to the pursuit of scientific knowledge. Using this criterion, NAWQA has been a success. The program has provided important new knowledge and understanding of scientific processes, and insights into the occurrence and distribution of contaminants that have been key to local and national policy decisions. Most of the basic design characteristics of NAWQA's first decade (1991-2000), hereafter called cycle I) remain appropriate as the program enters its second decade (cycle II) in 2001. In cycle II, the program has the opportunity to build on its successful base and to evolve to take advantage of the knowledge generated in cycle I. In addition to this expected evolution, NAWQA must also make some changes to compensate for the fact that program funding has not kept pace with inflation.
\nAn important theme for the second cycle of NAWQA will be the integration of knowledge across scales and across disciplines. The question that drove the NAWQA design in the first cycle was \"How is water quality related to land use?\" Cycle II will build upon what was learned in cycle I and use land-use and water-quality gradients to identify and understand potential sources of various constituents and the processes affecting transport and fate of those constituents and their effects on receptors. The understanding we gain from applying this approach will be relevant to the interests of policymakers, regulatory agencies, and resource managers.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr99470","issn":"0094-9140","collaboration":"National Water-Quality Assessment Program","usgsCitation":"U.S. Geological Survey, Mallard, G.E., Armbruster, J.T., Broshears, R.E., Evenson, E.J., Luoma, S.N., Phillips, P., and Prince, K.R., 1999, Recommendations for Cycle II of National Water-Quality Assessment (NAWQA) Program: U.S. Geological Survey Open-File Report 99-470, iv, 52 p., https://doi.org/10.3133/ofr99470.","productDescription":"iv, 52 p.","numberOfPages":"58","costCenters":[],"links":[{"id":153819,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0470/report-thumb.jpg"},{"id":279462,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0470/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db64492c","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":128240,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":529089,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mallard, Gail E.","contributorId":46556,"corporation":false,"usgs":true,"family":"Mallard","given":"Gail","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":187068,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Armbruster, Jeffrey T.","contributorId":37707,"corporation":false,"usgs":true,"family":"Armbruster","given":"Jeffrey","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":187066,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Broshears, Robert E.","contributorId":40675,"corporation":false,"usgs":true,"family":"Broshears","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":187067,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Evenson, Eric J. eevenson@usgs.gov","contributorId":4072,"corporation":false,"usgs":true,"family":"Evenson","given":"Eric","email":"eevenson@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":187065,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Luoma, Samuel N. 0000-0001-5443-5091 snluoma@usgs.gov","orcid":"https://orcid.org/0000-0001-5443-5091","contributorId":2287,"corporation":false,"usgs":true,"family":"Luoma","given":"Samuel","email":"snluoma@usgs.gov","middleInitial":"N.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":187064,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Phillips, Patrick J. pjphilli@usgs.gov","contributorId":856,"corporation":false,"usgs":true,"family":"Phillips","given":"Patrick J.","email":"pjphilli@usgs.gov","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":false,"id":187062,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Prince, Keith R. krprince@usgs.gov","contributorId":1413,"corporation":false,"usgs":true,"family":"Prince","given":"Keith","email":"krprince@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":187063,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":50332,"text":"ofr99147A - 1999 - Chemical composition of weathered and unweathered strata of the Meade Peak Phosphatic Shale Member of the Permian Phosphoria Formation-A. Measured sections A and B, central part of Rasmussen Ridge, Caribou County, Idaho","interactions":[],"lastModifiedDate":"2012-05-17T01:01:41","indexId":"ofr99147A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1999","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":"99-147","chapter":"A","title":"Chemical composition of weathered and unweathered strata of the Meade Peak Phosphatic Shale Member of the Permian Phosphoria Formation-A. Measured sections A and B, central part of Rasmussen Ridge, Caribou County, Idaho","language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr99147A","usgsCitation":"Herring, J., Desborough, G.A., Wilson, S., Tysdal, R.G., Grauch, R., and Gunter, M.E., 1999, Chemical composition of weathered and unweathered strata of the Meade Peak Phosphatic Shale Member of the Permian Phosphoria Formation-A. Measured sections A and B, central part of Rasmussen Ridge, Caribou County, Idaho: U.S. Geological Survey Open-File Report 99-147, 24 p., https://doi.org/10.3133/ofr99147A.","productDescription":"24 p.","costCenters":[],"links":[{"id":256869,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0147a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":258735,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0147a/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e3fc0","contributors":{"authors":[{"text":"Herring, J. R.","contributorId":43348,"corporation":false,"usgs":true,"family":"Herring","given":"J. R.","affiliations":[],"preferred":false,"id":241220,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Desborough, G. A.","contributorId":34527,"corporation":false,"usgs":true,"family":"Desborough","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":241219,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilson, S. A. 0000-0002-9468-0005","orcid":"https://orcid.org/0000-0002-9468-0005","contributorId":23561,"corporation":false,"usgs":true,"family":"Wilson","given":"S. A.","affiliations":[],"preferred":false,"id":241218,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tysdal, R. G.","contributorId":8823,"corporation":false,"usgs":true,"family":"Tysdal","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":241217,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Grauch, R. I. 0000-0002-1763-0813","orcid":"https://orcid.org/0000-0002-1763-0813","contributorId":107698,"corporation":false,"usgs":true,"family":"Grauch","given":"R. I.","affiliations":[],"preferred":false,"id":241222,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gunter, M. E.","contributorId":104937,"corporation":false,"usgs":true,"family":"Gunter","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":241221,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":50339,"text":"ofr99455 - 1999 - Near Field Receiving Water Monitoring of Trace Metals in Clams (Macoma balthica) and sediments near the Palo Alto and San Jose/Sunnyvale Water Quality Control Plants in South San Francisco Bay","interactions":[],"lastModifiedDate":"2012-02-02T00:10:25","indexId":"ofr99455","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1999","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":"99-455","title":"Near Field Receiving Water Monitoring of Trace Metals in Clams (Macoma balthica) and sediments near the Palo Alto and San Jose/Sunnyvale Water Quality Control Plants in South San Francisco Bay","language":"ENGLISH","doi":"10.3133/ofr99455","usgsCitation":"Wellise, C., Luoma, S., Cain, D., Brown, C., Hornberger, M., and Bouse, R., 1999, Near Field Receiving Water Monitoring of Trace Metals in Clams (Macoma balthica) and sediments near the Palo Alto and San Jose/Sunnyvale Water Quality Control Plants in South San Francisco Bay: U.S. Geological Survey Open-File Report 99-455, 101 p., https://doi.org/10.3133/ofr99455.","productDescription":"101 p.","costCenters":[],"links":[{"id":170388,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db697ff4","contributors":{"authors":[{"text":"Wellise, C.J.","contributorId":50203,"corporation":false,"usgs":true,"family":"Wellise","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":241235,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Luoma, S. 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