Floodflows on natural-flow streams in Massachusetts with drainage areas between 0.25 square miles and 260 square miles may be estimated from drainage area, main-channel slope, mean basin elevation, and the area of swamps, lakes, and ponds. Multiple-regression techniques were used to define the relationship between a suite of basin and climatic characteristics and flood peaks in three flood-frequency regions at a total of 95 sites. Station flood-frequency data were computed following guidelines in Bulletin I7A of the U.S. Water Resources Council. The frequency analyses are based upon weighted skew values, and adjustments for high and low outliers, and historic peak data. Regression equations for estimation of peak discharges for 0.5, 0.2, 0.1, 0.04, 0.02, and 0.01 exceedance probabilities are provided for ungaged sites. An improved sample of flood peaks and gaging stations and the definition of three flood-frequency regions reduced the standard error of estimate by about 5 percent over those for the 1977 relations. Included in this analysis were the synthetic flood-frequency data at eight sites computed using historic climatic data and 10 parameters optimized by calibration of the U.S. Geological Survey's rainfall-runoff model with storm data observed over II years. The equations are applicable to streams unaffected by regulation where the usable manmade storage is less than 4.5 million cubic feet per square mile, or by diversions or urbanization. The equations are restricted to sites where the basin indices are within a specified range outside of eastern Plymouth, Barnstable, Dukes or Nantucket Counties. In these areas, the available data do not adequately define the influence of high infiltration and storage capacities of drainage basins on floodflows.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648677","contributors":{"authors":[{"text":"Wandle, S. William Jr.","contributorId":99562,"corporation":false,"usgs":true,"family":"Wandle","given":"S.","suffix":"Jr.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":163363,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11564,"text":"ofr82566 - 1982 - Reconnaissance of stream biota and physical and chemical water quality in areas of selected land use in the coal-mining region, southwestern Indiana, 1979-80","interactions":[],"lastModifiedDate":"2012-02-02T00:06:42","indexId":"ofr82566","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-566","title":"Reconnaissance of stream biota and physical and chemical water quality in areas of selected land use in the coal-mining region, southwestern Indiana, 1979-80","docAbstract":"To help meet the goals of the Surface-Mining Control and Reclamation Act of 1977, the U.S. Geological Survey is assessing the physical, chemical, and biological characteristics of surface water within the coal-mining region of southwestern Indiana. This report discusses benthic-invertebrate and periphyticalgal communities in streams draining homogeneous-agricultural, forested, active/reclaimed-mine, reclaimed-mine, and unreclaimed-mine watersheds--and relates the biological communities to the physical and chemical characteristics of the streams. \r\n\r\nAlkalinity and pH were lower and the concentrations of dissolved solids, suspended solids, calcium, magnesium, sodium, potassium, sulfate, iron, manganese, aluminum, and zinc were higher in unreclaimed-mine watersheds than in the other land-use watersheds. \r\n\r\nNumbers and community diversity of benthic invertebrates were less at sites affected by mining than at agricultural or forested sites, owing to (1) synergistic effects of low pH, metals, and unsuitable habitat and (2) lack of colonizing drift organisms because of the small drainage area upstream from the mined area. Only a few organisms, such as the caddisflies Cheumatopsyche and Hydropsyche and the chironomids Chironomus and Cricotopus were found in streams draining mine areas.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82566","usgsCitation":"Wangsness, D., 1982, Reconnaissance of stream biota and physical and chemical water quality in areas of selected land use in the coal-mining region, southwestern Indiana, 1979-80: U.S. Geological Survey Open-File Report 82-566, vi, 48 p. ill. ;28 cm., https://doi.org/10.3133/ofr82566.","productDescription":"vi, 48 p. ill. ;28 cm.","costCenters":[],"links":[{"id":145827,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0566/report-thumb.jpg"},{"id":39434,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0566/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624adb","contributors":{"authors":[{"text":"Wangsness, D. J.","contributorId":54208,"corporation":false,"usgs":true,"family":"Wangsness","given":"D. J.","affiliations":[],"preferred":false,"id":163364,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11616,"text":"ofr82352 - 1982 - A model for the simulation of flow of variable-density ground water in three dimensions under steady-state conditions","interactions":[],"lastModifiedDate":"2012-02-02T00:06:44","indexId":"ofr82352","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-352","title":"A model for the simulation of flow of variable-density ground water in three dimensions under steady-state conditions","docAbstract":"A computer program has been developed as part of the U.S. Geological Survey's national program of Regional Aquifer System Analysis (RASA) that generates input to ground-water flow models to enable them to simulate variable-density ground-water flow. Information required for the program's operation is: aquifer elevation, thickness, and ground-water density. Included in the report is a computer program for calculating ground-water density from aquifer depth, temperature, and dissolved solids concentration. The 60-page report describes the theoretical development and documents two FORTRAN programs used to generate the necessary flow-model input. An example for a symmetrical basin is fully worked out.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82352","usgsCitation":"Weiss, E., 1982, A model for the simulation of flow of variable-density ground water in three dimensions under steady-state conditions: U.S. Geological Survey Open-File Report 82-352, vii, 66 p., ill. ;28 cm., https://doi.org/10.3133/ofr82352.","productDescription":"vii, 66 p., ill. ;28 cm.","costCenters":[],"links":[{"id":145283,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0352/report-thumb.jpg"},{"id":39476,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0352/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adf42","contributors":{"authors":[{"text":"Weiss, Emanuel","contributorId":74383,"corporation":false,"usgs":true,"family":"Weiss","given":"Emanuel","affiliations":[],"preferred":false,"id":163451,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11617,"text":"ofr82447 - 1982 - A computer program for calculating relative-transmissivity input arrays to aid model calibration","interactions":[],"lastModifiedDate":"2012-02-02T00:06:44","indexId":"ofr82447","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-447","title":"A computer program for calculating relative-transmissivity input arrays to aid model calibration","docAbstract":"A program is documented that calculates a transmissivity distribution for input to a digital ground-water flow model. Factors that are taken into account in the calculation are: aquifer thickness, ground-water viscosity and its dependence on temperature and dissolved solids, and permeability and its dependence on overburden pressure. Other factors affecting ground-water flow are indicated. With small changes in the program code, leakance also could be calculated. The purpose of these calculations is to provide a physical basis for efficient calibration, and to extend rational transmissivity trends into areas where model calibration is insensitive to transmissivity values.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82447","usgsCitation":"Weiss, E., 1982, A computer program for calculating relative-transmissivity input arrays to aid model calibration: U.S. Geological Survey Open-File Report 82-447, iv, 22 p., ill. ;28 cm., https://doi.org/10.3133/ofr82447.","productDescription":"iv, 22 p., ill. ;28 cm.","costCenters":[],"links":[{"id":145284,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0447/report-thumb.jpg"},{"id":39477,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0447/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b09cb","contributors":{"authors":[{"text":"Weiss, Emanuel","contributorId":74383,"corporation":false,"usgs":true,"family":"Weiss","given":"Emanuel","affiliations":[],"preferred":false,"id":163452,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11630,"text":"ofr82740 - 1982 - Diatremes of the Hopi Buttes, Arizona; chemical and statistical analyses","interactions":[],"lastModifiedDate":"2012-02-02T00:06:30","indexId":"ofr82740","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-740","title":"Diatremes of the Hopi Buttes, Arizona; chemical and statistical analyses","docAbstract":"Lacustrine sediments deposited in maar lakes of the Hopi Buttes diatremes are hosts for uranium mineralization of as much as 1500 ppm. The monchiquites and limburgite turfs erupted from the diatremes are distinguished from normal alkalic basalts of the Colorado Plateau by their extreme silica undersaturation and high water, TiO2, and P2O5 contents. Many trace elements are also unusually abundant, including Ag, As, Ba, Be, Ce, Dy, Eu, F, Gd, Hf, La, Nd, Pb, Rb, Se, Sm, Sn, Sr, Ta, Tb, Th, U, V, Zn, and Zr. \r\n\r\nThe lacustrine sediments, which consist predominantly of travertine and clastic rocks, are the hosts for syngenetic and epigenetic uranium mineralization of as much as 1500 ppm uranium. Fission track maps show the uranium to be disseminated within the travertine and clastic rocks, and although microprobe analyses have not, as yet, revealed discrete uranium-bearing phases, the clastic rocks show a correlation of high Fe, Ti, and P with areas of high U. Correlation coefficients show that for the travertines, clastics, and limburgite ruffs, Mo, As, Sr, Co, and V appear to have the most consistent and strongest correlations with uranium. Many elements, including many of the rare-earth elements, that are high in these three rocks are also high in the monchiquites, as compared to the average crustal abundance for the respective rock type. This similar suite of anomalous elements, which includes such immobile elements as the rare earths, suggests that Fluids which deposited the travertines were related to the monchiquitic magma. The similar age of about 5 m.y. for both the lake beds and the monchiquites also appears to support this source for the mineralizing fluids.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82740","usgsCitation":"Wenrich, K., and Mascarenas, J., 1982, Diatremes of the Hopi Buttes, Arizona; chemical and statistical analyses: U.S. Geological Survey Open-File Report 82-740, iv, 131 p., ill. ;28 cm., https://doi.org/10.3133/ofr82740.","productDescription":"iv, 131 p., ill. ;28 cm.","costCenters":[],"links":[{"id":143780,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0740/report-thumb.jpg"},{"id":39490,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0740/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65dac8","contributors":{"authors":[{"text":"Wenrich, K. J.","contributorId":40203,"corporation":false,"usgs":true,"family":"Wenrich","given":"K. J.","affiliations":[],"preferred":false,"id":163475,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mascarenas, J. F.","contributorId":71179,"corporation":false,"usgs":true,"family":"Mascarenas","given":"J. F.","affiliations":[],"preferred":false,"id":163476,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11642,"text":"ofr82337 - 1982 - Estimating the magnitude of peak discharges for selected flood frequencies on small streams in South Carolina (1975)","interactions":[],"lastModifiedDate":"2016-12-14T12:26:13","indexId":"ofr82337","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-337","title":"Estimating the magnitude of peak discharges for selected flood frequencies on small streams in South Carolina (1975)","docAbstract":"A program to collect and analyze flood data from small streams in South Carolina was conducted from 1967-75, as a cooperative research project with the South Carolina Department of Highways and Public Transportation and the Federal Highway Administration. As a result of that program, a technique is presented for estimating the magnitude and frequency of floods on small streams in South Carolina with drainage areas ranging in size from 1 to 500 square miles. Peak-discharge data from 74 stream-gaging stations (25 small streams were synthesized, whereas 49 stations had long-term records) were used in multiple regression procedures to obtain equations for estimating magnitude of floods having recurrence intervals of 10, 25, 50, and 100 years on small natural streams. The significant independent variable was drainage area. Equations were developed for the three physiographic provinces of South Carolina (Coastal Plain, Piedmont, and Blue Ridge) and can be used for estimating floods on small streams. 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Carolina\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fc208","contributors":{"authors":[{"text":"Whetstone, B.H.","contributorId":104496,"corporation":false,"usgs":true,"family":"Whetstone","given":"B.H.","email":"","affiliations":[],"preferred":false,"id":163492,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11656,"text":"ofr821046 - 1982 - Preliminary geological investigation of the Bir Hayzan diatomite deposit, Kingdom of Saudi Arabia, with a section on selected physical properties and implications for future geophysical exploration","interactions":[],"lastModifiedDate":"2012-02-02T00:06:33","indexId":"ofr821046","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-1046","title":"Preliminary geological investigation of the Bir Hayzan diatomite deposit, Kingdom of Saudi Arabia, with a section on selected physical properties and implications for future geophysical exploration","docAbstract":"A 2.2-m-thick lake bed composed entirely of diatomite was found in the southwestern arm of the Nafud sand sea, about 67 km east of Tayma in northwestern Saudi Arabia. Its stratigraphic position above eolian sand and below a large barchanoid dune indicates deposition during an exceptional period of pluvial climate in an otherwise arid sand desert. Radiocarbon-dated carbonate lake beds found in similar stratigraphic settings in other parts of the Nafud suggest that the diatomite was deposited in the late Pleistocene epoch sometime between 32,000 and 20,000 years ago. Diatomite of the same pluvial episode has also been found in the Afar region of Ethiopia. \r\n\r\nFour samples of the diatomite were analyzed for major chemical components and 32 minor and trace elements. Two of the samples appeared to be representative of the lake bed. These samples contained about 85 percent SiO2, 2.34 percent Fe2O3, 1 4 percent Al2O3, and 8.27 percent ignition loss, with only traces of CaO, P2O5, MgO, Na2O, and TiO2. The high content of silica and low contents of alumina, iron oxide, lime, and other constituents indicate low contamination. Analyses of samples from the two atypical units indicate a small amount of contamination, probably clay or mica, in the basal unit and addition of iron oxide and carbonate by ground water in an isolated green-colored unit. Chemically the Bi'r Hayzan diatomite compares favorably with commercial deposits from other parts of the world. Low bulk densities of 0.64 g/cm3 (30-40 lbs/ft3) and an average porosity of 63 percent for five samples also suggest the deposit is of industrial grade. \r\n\r\nFurther studies are recommended to determine: (1) the size and extent of the deposit and (2) the suitability of the diatomite for commercial applications. As means to these ends, electrical-resistivity surveys following winter rains are suggested to determine both the extent and thickness of the lake bed beneath the overlying sand dunes. A complete species identification of the diatom association and further laboratory testing of physical properties of the diatomite also should be made. Further exploration in the Nafud is recommended to locate other possible diatomite deposits.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821046","usgsCitation":"Whitney, J., and Gettings, M.E., 1982, Preliminary geological investigation of the Bir Hayzan diatomite deposit, Kingdom of Saudi Arabia, with a section on selected physical properties and implications for future geophysical exploration: U.S. Geological Survey Open-File Report 82-1046, 27 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr821046.","productDescription":"27 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":144764,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1046/report-thumb.jpg"},{"id":39512,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1046/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db673b91","contributors":{"authors":[{"text":"Whitney, J.W.","contributorId":27437,"corporation":false,"usgs":true,"family":"Whitney","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":163520,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gettings, M. E.","contributorId":25148,"corporation":false,"usgs":true,"family":"Gettings","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":163519,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11669,"text":"ofr82371 - 1982 - Simulated changes in water levels in the Minjur Aquifer, Riyadh area, Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:33","indexId":"ofr82371","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-371","title":"Simulated changes in water levels in the Minjur Aquifer, Riyadh area, Saudi Arabia","docAbstract":"A two-dimensional finite-difference computer model of the Minjur aquifer in the Riyadh area of Saudi Arabia was developed to simulate and predict drawdown in an aquifer which, in 1979, supplied more than 80 percent of all water used in this capital area. The Minjur was modeled as a confined aquifer recharged by leakage through underlying confining beds. Pumpage was simulated for a 23-year period during which it increased from 2,160 to 220 ,000 cubic meters per day. At Riyadh, the top of the Minjur aquifer is about 1200 meters below land surface. Aquifer thickness within the 40,000-square-kilometer study area ranges from 74 to 138 meters inclusively. Values for aquifer characteristics used in the model are: transmissivity, from 0.001 to 0.0062 square meters per second; storage coefficients, 0.07 for the unconfined, and 0.0004 for the confined sectors of the model area. A value of 0.02 meters per second was used to represent the vertical conductivity of the confining bed. Predictive simulations indicate that if the Minjur aquifer in the Riyadh area is stressed by estimated future pumpages, static water-level declines ranging from 10 up to and including 90 meters, depending on location, will occur from 1980 through 1999. Simulations also demonstrated that pumping levels in the new Buwayb well field will decline substantially from 1980 through 1981. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82371","usgsCitation":"Williams, J., and Sagaby, I., 1982, Simulated changes in water levels in the Minjur Aquifer, Riyadh area, Saudi Arabia: U.S. Geological Survey Open-File Report 82-371, v, 40 p., 4 over-size sheets, ill., maps ;28 cm., https://doi.org/10.3133/ofr82371.","productDescription":"v, 40 p., 4 over-size sheets, ill., maps ;28 cm.","costCenters":[],"links":[{"id":144766,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0371/report-thumb.jpg"},{"id":39525,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0371/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39526,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0371/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39527,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0371/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39528,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0371/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39529,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0371/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f3971","contributors":{"authors":[{"text":"Williams, J. F.","contributorId":20754,"corporation":false,"usgs":true,"family":"Williams","given":"J. F.","affiliations":[],"preferred":false,"id":163546,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sagaby, I.A.","contributorId":94313,"corporation":false,"usgs":true,"family":"Sagaby","given":"I.A.","email":"","affiliations":[],"preferred":false,"id":163547,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11677,"text":"ofr82755 - 1982 - Water resources of Rockland Basin, southeastern Idaho","interactions":[],"lastModifiedDate":"2023-02-07T20:36:58.317284","indexId":"ofr82755","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-755","title":"Water resources of Rockland Basin, southeastern Idaho","docAbstract":"Rockland basin comprises about 320 sq mi of the Snake River drainage in southeastern Idaho. Mountain ranges bordering the basin are composed predominantly of limestone and are complexly faulted. Major aquifers include Holocene alluvium, Quaternary-Tertiary volcanic rocks, and Tertiary sedimentary rocks. Groundwater occurs under water table conditions except where it is locally confined. Groundwater discharges to springs in the Deep Creek Mountains and maintains perennial streamflow. Near the mouth of Rock Creek, groundwater movement is northward toward the Snake River. Underflow is estimated to be 51,000 acre-ft/yr.
Total water yield available to Rockland basin is estimated to be 5.0 in. (85,000 acre-ft) of the estimated 17.3 in. of annual precipitation. Evapotranspiration ranges from 9.9 to 17 in./yr, depending, in part, on altitude of the land surface.
An estimated 12,000 acre-ft of surface water and 3,500 acre-ft of groundwater are used annually for irrigation. Less than 100 acre-ft of water is used for public supply, domestic, and stock supplies. East Fork Rock Creek supplies the most surface water for irrigation of agricultural lands.
At the present (1980) state of groundwater development in Rockland basin, streams and aquifers are hydraulically connected. Pumping of groundwater in increased quantities from wells near streams will affect groundwater movement and may diminish streamflow. There are no long-term regional water table declines at present. Continued water level monitoring of selected wells may aid in documenting effects of future management practices on the groundwater system.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82755","usgsCitation":"Williams, R.P., and Young, H., 1982, Water resources of Rockland Basin, southeastern Idaho: U.S. Geological Survey Open-File Report 82-755, v, 68 p., https://doi.org/10.3133/ofr82755.","productDescription":"v, 68 p.","costCenters":[],"links":[{"id":39550,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0755/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145557,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0755/report-thumb.jpg"},{"id":412824,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75649.htm"}],"country":"United States","state":"idaho","otherGeospatial":"Rockland Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -113.00005230365849,\n 42.727096308338844\n ],\n [\n -113.00005230365849,\n 42.31807748978014\n ],\n [\n -112.73189310111351,\n 42.31807748978014\n ],\n [\n -112.73189310111351,\n 42.727096308338844\n ],\n [\n -113.00005230365849,\n 42.727096308338844\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65da57","contributors":{"authors":[{"text":"Williams, Rhea P.","contributorId":87114,"corporation":false,"usgs":true,"family":"Williams","given":"Rhea","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":163557,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Young, H.W.","contributorId":68278,"corporation":false,"usgs":true,"family":"Young","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":163556,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11678,"text":"ofr82874 - 1982 - Plan for hydrologic study of an area to be surface mined for coal in northwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:39","indexId":"ofr82874","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-874","title":"Plan for hydrologic study of an area to be surface mined for coal in northwestern Colorado","docAbstract":"A data-collection network was established in 1980 in northwestern Colorado in a drainage basin which may be surface mined for coal. This report describes the work plan set up to study the premining hydrology of this area near Steamboat Springs, Routt County, Colorado. The bedrock, alluvial, and surface-water systems as well as the climatic inputs to these systems, are monitored for this study.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82874","usgsCitation":"Williams, R., and Driver, N.E., 1982, Plan for hydrologic study of an area to be surface mined for coal in northwestern Colorado: U.S. Geological Survey Open-File Report 82-874, iv, 23 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82874.","productDescription":"iv, 23 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":145570,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0874/report-thumb.jpg"},{"id":39551,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0874/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db68432a","contributors":{"authors":[{"text":"Williams, Robert S.","contributorId":55444,"corporation":false,"usgs":true,"family":"Williams","given":"Robert S.","affiliations":[],"preferred":false,"id":163558,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Driver, Nancy E.","contributorId":67858,"corporation":false,"usgs":true,"family":"Driver","given":"Nancy","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":163559,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11702,"text":"ofr82869 - 1982 - Annotated report and data inventory for the Mississippi and Minnesota rivers, Minneapolis-St. Paul metropolitan area","interactions":[],"lastModifiedDate":"2018-04-02T12:10:14","indexId":"ofr82869","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-869","title":"Annotated report and data inventory for the Mississippi and Minnesota rivers, Minneapolis-St. Paul metropolitan area","docAbstract":"This inventory of reports and data concerning the Mississippi and Minnesota Rivers in the Twin Cities metropolitan area was compiled from November 1981 through January 1982 for a planned river-quality assessment to be conducted cooperatively by the U.S. Geological Survey and the Metropolitan Waste Control Commission. There are 260 annotated citations: 176 citations of reports; 8 citations of computer models that have been used to model either or both rivers; and 76 citations of data in reports , in field notes, lab sheets, or handwritten tabulations, and in computer data bases. Citations of all the reports and data located that might conceivably be useful in understanding and interpreting the biological and chemical quality of the Mississippi and Minnesota Rivers in the past, present, or future were included. The accuracy of the citations was not verified and secondary sources, such as other annotated bibliographies, were used in the compilation of this inventory.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Mounds View, MN","doi":"10.3133/ofr82869","collaboration":"Prepared in cooperation with the Metropolitan Waste Control Commission","usgsCitation":"Winterstein, T.A., 1982, Annotated report and data inventory for the Mississippi and Minnesota rivers, Minneapolis-St. Paul metropolitan area: U.S. Geological Survey Open-File Report 82-869, iii, 99 p., https://doi.org/10.3133/ofr82869.","productDescription":"iii, 99 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":39584,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0869/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144911,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0869/report-thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"Twin Cities 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T. A.","contributorId":25156,"corporation":false,"usgs":true,"family":"Winterstein","given":"T.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":163592,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11720,"text":"ofr811180 - 1982 - Comparison of automated satellite systems with conventional systems for hydrologic data collection in west-central Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:06:30","indexId":"ofr811180","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-1180","title":"Comparison of automated satellite systems with conventional systems for hydrologic data collection in west-central Florida","docAbstract":"This report provides results of reliability and cost-effective studies of the goes satellite data-collection system used to operate a small hydrologic data network in west-central Florida. The GOES system, in its present state of development, was found to be about as reliable as conventional methods of data collection. Benefits of using the GOES system include some cost and manpower reduction, improved data accuracy, near real-time data availability, and direct computer storage and analysis of data. The GOES system could allow annual manpower reductions of 19 to 23 percent with reduction in cost for some and increase in cost for other single-parameter sites, such as streamflow, rainfall, and ground-water monitoring stations. Manpower reductions of 46 percent or more appear possible for multiple-parameter sites. Implementation of expected improvements in instrumentation and data handling procedures should further reduce costs. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811180","usgsCitation":"Woodham, W.M., 1982, Comparison of automated satellite systems with conventional systems for hydrologic data collection in west-central Florida: U.S. Geological Survey Open-File Report 81-1180, iv, 27 p., map ;28 cm., https://doi.org/10.3133/ofr811180.","productDescription":"iv, 27 p., map ;28 cm.","costCenters":[],"links":[{"id":143920,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1180/report-thumb.jpg"},{"id":39606,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1180/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae3a6","contributors":{"authors":[{"text":"Woodham, W. M.","contributorId":72356,"corporation":false,"usgs":true,"family":"Woodham","given":"W.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":163617,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11790,"text":"ofr82104 - 1982 - Thermal springs in the Salmon River basin, central Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:06:34","indexId":"ofr82104","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-104","title":"Thermal springs in the Salmon River basin, central Idaho","docAbstract":"The Salmon River basin drains approximately 13,000 square miles in central Idaho underlain by the Idaho batholith. Geologic units in the basin include igneous, sedimentary, and metamorphic rocks and granitic rocks predominate. Water from thermal springs ranges in temperature from 20.5 degrees to 94.0 degrees Celsius. The waters are slightly alkaline and are generally a sodium carbonate or bicarbonate type. Dissolved-solids concentrations are variable and range from 103 to 839 milligrams per liter. Estimated reservoir temperatures determined from the silicic acid-corrected silica, sodium-potassium-calcium, and sulfate-water isotope geothermometers range from 30 degrees to 184 degrees Celsius. Tritium concentrations in sampled thermal waters are near zero and indicate the waters are at least 100 years old and may be considerably older. Stable-isotope data indicate it is unlikely that a single area of recharge or a single hot-water reservoir supplies all hot springs in the basin. Thermal springs discharged at least 15,800 acre-feet of water in 1980. Associated convective heat flux is 27 million calories per second. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82104","usgsCitation":"Young, H., and Lewis, R., 1982, Thermal springs in the Salmon River basin, central Idaho: U.S. Geological Survey Open-File Report 82-104, iv, 30 p., 2 over-size sheets, ill., maps ;28 cm., https://doi.org/10.3133/ofr82104.","productDescription":"iv, 30 p., 2 over-size sheets, ill., maps ;28 cm.","costCenters":[],"links":[{"id":144777,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0104/report-thumb.jpg"},{"id":39681,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0104/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39682,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0104/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39683,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0104/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a57e4b07f02db62e64e","contributors":{"authors":[{"text":"Young, H.W.","contributorId":68278,"corporation":false,"usgs":true,"family":"Young","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":163735,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lewis, R.E.","contributorId":31735,"corporation":false,"usgs":true,"family":"Lewis","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":163734,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":12162,"text":"ofr821004 - 1982 - Methods for the determination of organic substances in water and fluvial sediments, USGS TWRI, Book 5, Laboratory analysis, Chapter A3","interactions":[{"subject":{"id":12162,"text":"ofr821004 - 1982 - Methods for the determination of organic substances in water and fluvial sediments, USGS TWRI, Book 5, Laboratory analysis, Chapter A3","indexId":"ofr821004","publicationYear":"1982","noYear":false,"title":"Methods for the determination of organic substances in water and fluvial sediments, USGS TWRI, Book 5, Laboratory analysis, Chapter A3"},"predicate":"SUPERSEDED_BY","object":{"id":4663,"text":"twri05A3 - 1987 - Methods for the determination of organic substances in water and fluvial sediments","indexId":"twri05A3","publicationYear":"1987","noYear":false,"title":"Methods for the determination of organic substances in water and fluvial sediments"},"id":1}],"supersededBy":{"id":4663,"text":"twri05A3 - 1987 - Methods for the determination of organic substances in water and fluvial sediments","indexId":"twri05A3","publicationYear":"1987","noYear":false,"title":"Methods for the determination of organic substances in water and fluvial sediments"},"lastModifiedDate":"2021-05-27T18:31:10.557334","indexId":"ofr821004","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-1004","title":"Methods for the determination of organic substances in water and fluvial sediments, USGS TWRI, Book 5, Laboratory analysis, Chapter A3","docAbstract":"This manual contains analytical methods used by the U.S. Geological Survey for the determination of organic substances in water, water-suspended sediment mixtures, and bottom material. Some of the analytical procedures yield determinations for specific compounds, whereas others provide a measure of the quantity of groups of compounds present in the sample. Examples of the first category are procedures for the organochlorine and organophosphate insecticides, chlorophenoxy acid and triazine herbicides and specific substituted phenols. Examples of the second category are the various organic carbon analyses and the polychlorinated biphenyl methods. Each analytical method is presented in a standardized format which includes conditions for application of the method, a summary of the method, interferences, required apparatus and reagents, analytical procedures, calculations, reporting of results, and estimation of precision.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr821004","usgsCitation":"1982, Methods for the determination of organic substances in water and fluvial sediments, USGS TWRI, Book 5, Laboratory analysis, Chapter A3: U.S. Geological Survey Open-File Report 82-1004, vii, 173 p., https://doi.org/10.3133/ofr821004.","productDescription":"vii, 173 p.","numberOfPages":"185","costCenters":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true}],"links":[{"id":146426,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1004/report-thumb.jpg"},{"id":359249,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1004/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62bad6","contributors":{"editors":[{"text":"Wershaw, Robert L. rwershaw@usgs.gov","contributorId":4856,"corporation":false,"usgs":true,"family":"Wershaw","given":"Robert","email":"rwershaw@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":725467,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Fishman, Marvin J.","contributorId":87110,"corporation":false,"usgs":true,"family":"Fishman","given":"Marvin J.","affiliations":[],"preferred":false,"id":725468,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Grabbe, R. R.","contributorId":119654,"corporation":false,"usgs":true,"family":"Grabbe","given":"R. R.","affiliations":[],"preferred":false,"id":725469,"contributorType":{"id":2,"text":"Editors"},"rank":3},{"text":"Lowe, L. E.","contributorId":97482,"corporation":false,"usgs":true,"family":"Lowe","given":"L.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":725470,"contributorType":{"id":2,"text":"Editors"},"rank":4}]}} ,{"id":13011,"text":"ofr821024 - 1982 - Guidelines and techniques for obtaining water samples that accurately represent the water chemistry of an aquifer","interactions":[],"lastModifiedDate":"2015-09-22T15:40:55","indexId":"ofr821024","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-1024","title":"Guidelines and techniques for obtaining water samples that accurately represent the water chemistry of an aquifer","docAbstract":"Obtaining ground-water samples that accurately represent the water chemistry of an aquifer is a complex task. Before a ground-water sampling program can be started, an understanding of the kind of chemical data needed and the potential changes in water chemistry resulting from various drilling, well-completion, and sampling techniques is needed. This report provides a basis for such an evaluation and permits a choice of techniques that will result in obtaining the best possible data for the time and money allocated.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lakewood, CO","doi":"10.3133/ofr821024","usgsCitation":"Claassen, H.C., 1982, Guidelines and techniques for obtaining water samples that accurately represent the water chemistry of an aquifer: U.S. Geological Survey Open-File Report 82-1024, v, 49 p., https://doi.org/10.3133/ofr821024.","productDescription":"v, 49 p.","numberOfPages":"58","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":147145,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1024/report-thumb.jpg"},{"id":41478,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1024/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ae76","contributors":{"authors":[{"text":"Claassen, Hans C.","contributorId":25165,"corporation":false,"usgs":true,"family":"Claassen","given":"Hans","email":"","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":167132,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":20008,"text":"ofr821017 - 1982 - Water-quality data for streams in the southern Yampa River basin, northwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:07:34","indexId":"ofr821017","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-1017","title":"Water-quality data for streams in the southern Yampa River basin, northwestern Colorado","docAbstract":"Increases in coal mining in Colorado have raised questions regarding the impact of mining on the quality of surface water. An area where increases have caused particular concern is in northwestern Colorado, in the southern part of the Yampa River basin. In order to identify the changes produced by mining in the area it is necessary first to identify the water chemistry resulting from the geology, climate, and land use. To answer the above questions, a program for the synoptic collection of water-quality data was developed in which a network of sampling sites was established to determine the surface-water chemistry. \r\n\r\nThis study was begun in April 1981. Water-quality samples were collected from sites on all continuously flowing streams in the southern part of the Yampa River basin from the Oak Creek drainage near Steamboat Springs on the east to the surface-water gaging station on the Yampa River near Maybell on the west. Each water-quality site was sampled repetitively as changes occurred in discharge and specific conductance. Water-quality data from surface-water gaging stations in the area for water years 1976 to 1981 are included in the report.","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nOpen-File Services Section, Western Distribution Branch [distributor],","doi":"10.3133/ofr821017","usgsCitation":"Maura, W.S., 1982, Water-quality data for streams in the southern Yampa River basin, northwestern Colorado: U.S. Geological Survey Open-File Report 82-1017, iv, 116 p. :map ;28 cm., https://doi.org/10.3133/ofr821017.","productDescription":"iv, 116 p. :map ;28 cm.","costCenters":[],"links":[{"id":110123,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_33660.htm","linkFileType":{"id":5,"text":"html"},"description":"33660"},{"id":152502,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1017/report-thumb.jpg"},{"id":49537,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1017/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49538,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1017/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4888e4b07f02db51ad70","contributors":{"authors":[{"text":"Maura, Wendy S.","contributorId":9673,"corporation":false,"usgs":true,"family":"Maura","given":"Wendy","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":181892,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18183,"text":"ofr82575 - 1982 - Water quality of the tidal Potomac River and Estuary; hydrologic data report, 1981 water year, with a section on collection and analysis of chlorophyll-a","interactions":[],"lastModifiedDate":"2012-02-02T00:07:19","indexId":"ofr82575","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-575","title":"Water quality of the tidal Potomac River and Estuary; hydrologic data report, 1981 water year, with a section on collection and analysis of chlorophyll-a","docAbstract":"This report contains data on the physical and chemical properties measured in the Tidal Potomac River and Estuary during the 1981 water year. Data were collected at least weekly at five stations, and periodically at 15 stations and at two other stations near the mouth of the Potomac River in Chesapeake Bay. Each of the five stations represent a cross section at which the transport of selected dissolved and suspended materials can be computed. The remaining 17 stations are locations at which data were collected for special studies of selected phenomena, such as salt water migration and dissolved oxygen dynamics. Samples were routinely analyzed for chlorophyll-a, nitrogen, pheophytin, phosphorus, silica and suspended sediment. Additional samples were analyzed for adenosine triphosphate, algal growth potential, alkalinity, calcium, chloride, dissolved-solids residue, fluoride, iron, manganese, magnesium, nitrifying bacteria, organic carbon, potassium, seston, sodium, and sulfate. In addition, in-situ measurements of dissolved oxygen, specific conductance, pH, temperature, solar radiation, and secchi disk transparency were made. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82575","usgsCitation":"Blanchard, S.F., Coupe, R.H., and Woodward, J.C., 1982, Water quality of the tidal Potomac River and Estuary; hydrologic data report, 1981 water year, with a section on collection and analysis of chlorophyll-a: U.S. Geological Survey Open-File Report 82-575, ii, 304 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82575.","productDescription":"ii, 304 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":150310,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0575/report-thumb.jpg"},{"id":47547,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0575/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65db31","contributors":{"authors":[{"text":"Blanchard, Stephen F.","contributorId":54966,"corporation":false,"usgs":true,"family":"Blanchard","given":"Stephen","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":178669,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coupe, Richard H. 0000-0001-8679-1015 rhcoupe@usgs.gov","orcid":"https://orcid.org/0000-0001-8679-1015","contributorId":551,"corporation":false,"usgs":true,"family":"Coupe","given":"Richard","email":"rhcoupe@usgs.gov","middleInitial":"H.","affiliations":[{"id":394,"text":"Mississippi Water Science Center","active":true,"usgs":true}],"preferred":true,"id":178668,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Woodward, Joan C.","contributorId":91127,"corporation":false,"usgs":true,"family":"Woodward","given":"Joan","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":178670,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":18828,"text":"ofr82359 - 1982 - Field data describing the movement and storage of sediment in the East Fork River, Wyoming; Part III, river hydraulics and sediment transport, 1980","interactions":[],"lastModifiedDate":"2012-02-02T00:07:26","indexId":"ofr82359","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-359","title":"Field data describing the movement and storage of sediment in the East Fork River, Wyoming; Part III, river hydraulics and sediment transport, 1980","docAbstract":"Frequent measurements of river stage, water discharge, sediment-transport rate and particle-size gradation, and river slope were made at 44 cross sections along a 1.83-kilometer reach of East Fork River, Wyoming, during the spring 1980 snowmelt runoff. Data are tabulated and explanatory text facilitates its use for description of river hydraulics and sediment transport. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82359","usgsCitation":"Emmett, W.W., Myrick, R.M., and Meade, R., 1982, Field data describing the movement and storage of sediment in the East Fork River, Wyoming; Part III, river hydraulics and sediment transport, 1980: U.S. Geological Survey Open-File Report 82-359, ix, 298 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82359.","productDescription":"ix, 298 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":150701,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0359/report-thumb.jpg"},{"id":48215,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0359/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4d1c","contributors":{"authors":[{"text":"Emmett, W. W.","contributorId":107695,"corporation":false,"usgs":true,"family":"Emmett","given":"W.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":179815,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Myrick, R. M.","contributorId":29418,"corporation":false,"usgs":true,"family":"Myrick","given":"R.","middleInitial":"M.","affiliations":[],"preferred":false,"id":179814,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meade, R.H.","contributorId":27449,"corporation":false,"usgs":true,"family":"Meade","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":179813,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":20718,"text":"ofr82107 - 1982 - Regional hydrology of the Green River-Moab area, northwestern Paradox basin, Utah","interactions":[],"lastModifiedDate":"2021-11-22T21:41:59.4496","indexId":"ofr82107","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-107","title":"Regional hydrology of the Green River-Moab area, northwestern Paradox basin, Utah","docAbstract":"The Green River-Moab area encompasses about 7,800 square kilometers or about 25 percent of the Paradox basin. The entire Paradox basin is a part of the Colorado Plateaus that is underlain by a thick sequence of evaporite (salt) beds of Pennsylvanian age. The rock units that underlie the area have been grouped into hydrogeologic units based on their water-transmitting ability. Confining beds consist of evaporite beds of mostly salt, and over- lying and underlying thick sequences of rocks with minimal permeability; above and below these confining beds are aquifers. The upper Mesozoic sand- stone aquifer, probably is the most permeable hydrogeologic unit of the area and is the subject of this investigation. The principal component of ground- water outflow from this aquifer probably is subsurface flow to regional streams (the Green and Colorado Rivers) and is about 100 million cubic meters per year. All other components of outflow are relatively small. The average annual recharge to the aquifer is about 130 million cubic meters, of which about 20 million cubic meters is from local precipitation. For the lower aquifer, all recharge and discharge probably is by subsurface flow and was not estimated.
The aquifers are generally isolated from the evaporite beds by the bounding confining beds; as a result, most ground water has little if any contact with the evaporites. Brines are present in the confining beds, but solution of beds o£ salt probably is very slow in most parts of the area. No brine discharges' have been identified.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/ofr82107","collaboration":"Prepared in cooperaiton with the U.S. Department of Energy","usgsCitation":"Rush, F., Whitfield, M., and Hart, I.M., 1982, Regional hydrology of the Green River-Moab area, northwestern Paradox basin, Utah: U.S. Geological Survey Open-File Report 82-107, Report: vii, 86 p.; Table: 2 Plates: 26.00 in. x 28.00 inches, https://doi.org/10.3133/ofr82107.","productDescription":"Report: vii, 86 p.; Table: 2 Plates: 26.00 in. x 28.00 inches","numberOfPages":"92","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":392017,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13639.htm"},{"id":20448,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0107/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing generalized hydrology of the Green River-Moab area, Northwestern Paradox Basin, Utah"},{"id":20447,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0107/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing generalized hydrogeology of the Green River-Moab area, Northwestern Paradox Basin, Utah"},{"id":20449,"rank":402,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1982/0107/plate-3.pdf","text":"Table 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Rock and hydrogeologic units in the Green River-Moab area and vicinity"},{"id":153242,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0107/report-thumb.jpg"},{"id":50276,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0107/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Green River - Moab area, Paradox Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.25,\n 38\n ],\n [\n -110.5,\n 38\n ],\n [\n -110.5,\n 39.283\n ],\n [\n -109.25,\n 39.283\n ],\n [\n -109.25,\n 38\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db634869","contributors":{"authors":[{"text":"Rush, F. E.","contributorId":56234,"corporation":false,"usgs":true,"family":"Rush","given":"F. E.","affiliations":[],"preferred":false,"id":183122,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Whitfield, M.S.","contributorId":69547,"corporation":false,"usgs":true,"family":"Whitfield","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":183123,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hart, I. M.","contributorId":24806,"corporation":false,"usgs":true,"family":"Hart","given":"I.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":183121,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}