The U.S. Geological Survey and the Wyoming Department of Environmental Quality are involved in a cooperative effort to assess the probable cumulative impacts of coal mining on the hydrology of a part of the Powder River Structural Basin in Wyoming. It was assumed that the principal impacts on the ground-water system due to mining will occur in the relatively shallow aquifers which can be grouped into three homogeneous aquifers, namely, the Wyodak coal, the overburden, and the under burden. Emphasis of this report is on the results of analysis of surface-water resources in the Caballo Creek drainage. A surface-water model of the Caballo Creek drainage was developed using the Hydrological Simulation Program-Fortran model to help assess the impacts of mining activities on streamflow. The Caballo Creek drainage was divided into 10 land segments and 6 stream reaches in the modeling process. Three simulation runs show little, if any, change in streamflow between pre- and post-mining conditions and very little change between pre-mining and during-mining conditions. The principal reason for the absence of change is the high infiltration rate used in the model for all three conditions.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834235","usgsCitation":"Jordan, P.R., Bloyd, R., and Daddow, P., 1984, An assessment of cumulative impacts of coal mining on the hydrology in part of the Powder River structural basin, Wyoming: A progress report: U.S. Geological Survey Water-Resources Investigations Report 83-4235, iv, 29 p., https://doi.org/10.3133/wri834235.","productDescription":"iv, 29 p.","costCenters":[],"links":[{"id":394363,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35874.htm"},{"id":56748,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4235/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123888,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4235/report-thumb.jpg"}],"country":"United States","state":"Wyoming","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -105.75,\n 44\n ],\n [\n -105.25,\n 44\n ],\n [\n -105.25,\n 44.217\n ],\n [\n -105.75,\n 44.217\n ],\n [\n -105.75,\n 44\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684e08","contributors":{"authors":[{"text":"Jordan, P. R.","contributorId":7282,"corporation":false,"usgs":true,"family":"Jordan","given":"P.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":198927,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bloyd, R. M.","contributorId":34549,"corporation":false,"usgs":true,"family":"Bloyd","given":"R. M.","affiliations":[],"preferred":false,"id":198929,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Daddow, P. B.","contributorId":26700,"corporation":false,"usgs":true,"family":"Daddow","given":"P. B.","affiliations":[],"preferred":false,"id":198928,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":48838,"text":"ofr83852 - 1984 - Description and evaluation of the information transfer workshop series \"Coal hydrology in Virginia\"","interactions":[],"lastModifiedDate":"2012-02-02T00:10:05","indexId":"ofr83852","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"83-852","title":"Description and evaluation of the information transfer workshop series \"Coal hydrology in Virginia\"","docAbstract":"A series of workshops was conducted in September, 1982, by staff of the Virginia Office, Mid-Atlantic District of the U.S.-Geological Survey for the benefit of coal operators, consultants, and resource managers in the coal-producing area of southwest Virginia. The purpose of the workshop series was to present hydrologic information and data by the U.S. Geological Survey collected during four years of study of the. coal hydrology of Virginia. The workshop series was held one day a week for three weeks at two locations within southwest Virginia in order to reduce travel time and overnight travel costs for participants. Results of an independently conducted questionnaire indicate the series was a success. The report summarizes the workshop preparation, organization, and presentation, and gives general conclusions and suggestions for those interested in conducting workshops.","language":"ENGLISH","doi":"10.3133/ofr83852","usgsCitation":"Hufschmidt, P.W., 1984, Description and evaluation of the information transfer workshop series \"Coal hydrology in Virginia\": U.S. Geological Survey Open-File Report 83-852, 23 p. ill., map ; 28 cm., https://doi.org/10.3133/ofr83852.","productDescription":"23 p. ill., map ; 28 cm.","costCenters":[],"links":[{"id":162746,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0852/report-thumb.jpg"},{"id":85671,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0852/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66db44","contributors":{"authors":[{"text":"Hufschmidt, Peter W.","contributorId":85185,"corporation":false,"usgs":true,"family":"Hufschmidt","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":238394,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26360,"text":"wri844012 - 1984 - A reconnaissance study of saltwater contamination in the El Dorado aquifer, Union County, Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:08:33","indexId":"wri844012","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4012","title":"A reconnaissance study of saltwater contamination in the El Dorado aquifer, Union County, Arkansas","docAbstract":"Since 1960 chloride concentrations in the El Dorado aquifer have increased near El Dorado, Arkansas. The aquifer is a major source for municipal and industrial water supply in Union County. Greatest withdrawal occurs near El Dorado. Because of this withdrawal, the potentiometric surface at El Dorado has been lowered more than 300 feet. Geologic, hydrologic, and chemical data indicate that water from a graben south and east of El Dorado is the source of contamination from salt within the El Dorado aquifer. The data indicates that surface brines and deeper aquifers are not the sources of chloride contamination. Lowering the potentiometric surface near El Dorado has caused water to move out of the graben toward El Dorado. Estimates based on interpretation of electric logs for two wells in the graben indicate chloride equivalents may be as high as 2,500 milligrams per liter in the aquifer. Concentrations outside the graben range from 130 to 650 milligrams per liter at the west end of the graben and from 25 to 150 milligrams per liter farther west and north. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri844012","usgsCitation":"Broom, M.E., Kraemer, T.F., and Bush, W.V., 1984, A reconnaissance study of saltwater contamination in the El Dorado aquifer, Union County, Arkansas: U.S. Geological Survey Water-Resources Investigations Report 84-4012, v, 47 p. :ill., maps (some folded) ;28 cm., https://doi.org/10.3133/wri844012.","productDescription":"v, 47 p. :ill., maps (some folded) ;28 cm.","costCenters":[],"links":[{"id":124131,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4012/report-thumb.jpg"},{"id":55157,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4012/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a85ef","contributors":{"authors":[{"text":"Broom, Matthew E.","contributorId":101668,"corporation":false,"usgs":true,"family":"Broom","given":"Matthew","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":196253,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kraemer, T. F.","contributorId":63400,"corporation":false,"usgs":true,"family":"Kraemer","given":"T.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":196251,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bush, William V.","contributorId":93536,"corporation":false,"usgs":true,"family":"Bush","given":"William","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":196252,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":28640,"text":"wri834260 - 1984 - Potential effects of surface coal mining on the hydrology of the Corral Creek area, Hanging Woman Creek coal field, southeastern Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:08:39","indexId":"wri834260","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4260","title":"Potential effects of surface coal mining on the hydrology of the Corral Creek area, Hanging Woman Creek coal field, southeastern Montana","docAbstract":"The Corral Creek area of the Hanging Woman Creek coal field, 9 miles east of the Decker coal mines near the Tongue River, contains large reserves of Federal coal that have been identified for potential lease sale. A hydrologic study was conducted in the area to describe existing hydrologic systems and to study assess potential impacts of surface coal mining on local water resources. Hydrogeologic data collected indicate that aquifers are coal and sandstone beds within the Tongue River Member of the Fort Union Formation (Paleocene age) and sand and gravel in valley alluvium (Pleistocene and Holocene age). Surface-water resources are limited to a few spring-fed stock ponds in the higher parts of the area and the intermittent flow of Corral Creek near the mouth. Most of the stock ponds in the area become dry by midsummer. Mining of the Anderson coal bed would remove three stock wells and would lower the potentiometric surface within the coal and sandstone aquifers. The alluvial aquifer beneath Corral Creek and South Fork would be removed. Although mining would alter the existing hydrologic systems and remove several shallow wells, alternative ground-water supplies are available that could be developed to replace those lost by mining. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834260","usgsCitation":"McClymonds, N.E., 1984, Potential effects of surface coal mining on the hydrology of the Corral Creek area, Hanging Woman Creek coal field, southeastern Montana: U.S. Geological Survey Water-Resources Investigations Report 83-4260, v, 53 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834260.","productDescription":"v, 53 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123241,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4260/report-thumb.jpg"},{"id":57475,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4260/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a628f","contributors":{"authors":[{"text":"McClymonds, N. E.","contributorId":94653,"corporation":false,"usgs":true,"family":"McClymonds","given":"N.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":200159,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25971,"text":"wri844194 - 1984 - Evaluation of the hydrologic system and potential effects of mining in the Dickinson lignite area, eastern slope and western Stark and Hettinger counties, North Dakota","interactions":[],"lastModifiedDate":"2018-02-14T15:41:55","indexId":"wri844194","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4194","title":"Evaluation of the hydrologic system and potential effects of mining in the Dickinson lignite area, eastern slope and western Stark and Hettinger counties, North Dakota","docAbstract":"The investigation of the water resources of the Dickinson lignite area, an area of about 500 square miles, was undertaken to define the hydrologic system of the area and to project probable effects of coal mining on the system.
Aquifers occur in sandstone beds in: the Fox Hills Sandstone and the lower Hell Creek Formation of Cretaceous age, the upper Hell Creek Formation of Cretaceous age and the lower Ludlow Member of the Fort Union Formation of Tertiary age, and the upper Ludlow and lower Tongue River Members of the Fort Union Formation of Tertiary age. Aquifers also occur in the sandstone and lignite lenses in the upper Tongue River Member and the Sentinel Butte Member of the Fort Union Formation.
Depths to the Fox Hills-lower Hell Creek aquifer system range from about 1,300 to 1,710 feet. Well yields range from 18 to 100 gallons per minute. The water is soft and is a sodium bicarbonate type. Dissolvedsolids concentrations in samples collected from the aquifer system ranged from 1,230 to 1,690 milligrams per liter.
Depths to the upper Hell Creek-lower Ludlow aquifer system range from about 720 to 1,040 feet. Well yields generally are less than 30 gallons per minute but may be as much as 150 gallons per minute. The water is soft and a sodium bicarbonate type. Dissolved-solids concentrations in samples collected from the aquifer system ranged from 1,010 to 1,450 milligrams per liter.
Depths to the upper Ludlow-lower Tongue River aquifer system range from about 440 to 713 feet. Well yields may range from about 1 to 100 gallons per minute. The water generally is soft and a sodium bicarbonate type but may be moderately hard and a sulfate type in the southwestern part of the area. Dissolved-solids concentrations in samples collected from the aquifer system ranged from 995 to 1,990 milligrams per liter.
Depths to the upper Tongue River-Sentinel Butte aquifer system range from near land surface to about 530 feet below land surface. Well yields generally range from about 1 to 185 gallons per minute. Yields from the lignite parts of the system range from about 2 to 60 gallons per minute. The water generally is a sodium bicarbonate type, but locally sulfate is the dominant anion. Dissolved-solids concentrations in samples collected from the aquifer system generally ranged from 574 to 2,720 milligrams per liter.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844194","usgsCitation":"Armstrong, C.A., 1984, Evaluation of the hydrologic system and potential effects of mining in the Dickinson lignite area, eastern slope and western Stark and Hettinger counties, North Dakota: U.S. Geological Survey Water-Resources Investigations Report 84-4194, Report: v, 35 p.; Plate: 22.55 x 19.31 inches, https://doi.org/10.3133/wri844194.","productDescription":"Report: v, 35 p.; Plate: 22.55 x 19.31 inches","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":123870,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4194/report-thumb.jpg"},{"id":54717,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4194/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54718,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4194/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Dakota","county":"Hettinger County, Stark County","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa3b1","contributors":{"authors":[{"text":"Armstrong, C. A.","contributorId":66231,"corporation":false,"usgs":true,"family":"Armstrong","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":195565,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26649,"text":"wri844136 - 1984 - Comment on the International Atomic Energy Agency Report on the Advisory Group Meeting on Stable Isotope Reference Samples for Geochemical and Hydrological Investigation, Vienna, Austria, September 19-21, 1983","interactions":[],"lastModifiedDate":"2012-02-02T00:08:33","indexId":"wri844136","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4136","title":"Comment on the International Atomic Energy Agency Report on the Advisory Group Meeting on Stable Isotope Reference Samples for Geochemical and Hydrological Investigation, Vienna, Austria, September 19-21, 1983","docAbstract":"According to U.S. Geological Survey records, a report prepared by R. Gonfiantini summarizing the findings and recommendations of the 1983 Advisory Group Meeting on Stable Isotope Reference Samples for Geochemical and Hydrologic Investigations held in Vienna does not accurately represent the consultants ' consensus on three important points. The consultants (1) recommended no value for the C02-H20 oxygen isotope fractionation factor, not the cited value of 1.04115, (2) adopted a value of 1.0309 rather than 1.03086 to relate the PDB and SMOW scales, and (3) adopted a firm 180 value of -2.20% for NBS-19 on the PDB scale rather than agreeing that this would be a tentative value subject to modification when more measurements in selected laboratories are available. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nOpen-file Services Section, Western Distribution Branch [distributor],","doi":"10.3133/wri844136","usgsCitation":"Coplen, T., Friedman, I., and O’Neil, J.R., 1984, Comment on the International Atomic Energy Agency Report on the Advisory Group Meeting on Stable Isotope Reference Samples for Geochemical and Hydrological Investigation, Vienna, Austria, September 19-21, 1983: U.S. Geological Survey Water-Resources Investigations Report 84-4136, iii, 7 p. ;28 cm., https://doi.org/10.3133/wri844136.","productDescription":"iii, 7 p. ;28 cm.","costCenters":[],"links":[{"id":122943,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4136/report-thumb.jpg"},{"id":55526,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4136/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae693","contributors":{"authors":[{"text":"Coplen, T.B.","contributorId":34147,"corporation":false,"usgs":true,"family":"Coplen","given":"T.B.","affiliations":[],"preferred":false,"id":196769,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friedman, Irving","contributorId":90664,"corporation":false,"usgs":true,"family":"Friedman","given":"Irving","email":"","affiliations":[],"preferred":false,"id":196771,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"O’Neil, J. R.","contributorId":69633,"corporation":false,"usgs":true,"family":"O’Neil","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":196770,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":30416,"text":"wri844193 - 1984 - Preliminary evaluation of hydrologic properties of cores of unsaturated tuff, test well USW H-1, Yucca Mountain, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:08:57","indexId":"wri844193","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4193","title":"Preliminary evaluation of hydrologic properties of cores of unsaturated tuff, test well USW H-1, Yucca Mountain, Nevada","docAbstract":"Analyses were made on 19 core samples of unsaturated tuff from test well USW H-1. Moisture-characteristic curves relating saturation and moisture tension were developed from results of mercury-injection tests. Ambient moisture tension estimated from these curves generally was 1 to 2 bars. Values of relative permeability ranging from about 0.002 to 0.1 were determined by fitting an analytical expression to eight of the moisture-characteristic curves, and then integrating to solve for relative permeability. These values of relative permeability were applied to values of saturated hydraulic conductivity of core from a nearby test well to obtain effective hydraulic conductivities of about 8 x 10 to the minus twelfth power to 7 x 10 to the minus tenth power centimeter per second. If a unit hydraulic-head gradient is assumed, these values convert to a vertial matrix flux of 0.003 to 0.2 millimeter per year. The validity of this assumption was not verified due to the sparseness of data and uncertainties in their reliability. Consequently, the results of this study are preliminary and need to be used principally as a guide for future studies. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844193","usgsCitation":"Weeks, E., and Wilson, W., 1984, Preliminary evaluation of hydrologic properties of cores of unsaturated tuff, test well USW H-1, Yucca Mountain, Nevada: U.S. Geological Survey Water-Resources Investigations Report 84-4193, iv, 30 p. :ill. ;28 cm., https://doi.org/10.3133/wri844193.","productDescription":"iv, 30 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":159691,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4193/report-thumb.jpg"},{"id":59185,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4193/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699d06","contributors":{"authors":[{"text":"Weeks, E.P.","contributorId":38514,"corporation":false,"usgs":true,"family":"Weeks","given":"E.P.","email":"","affiliations":[],"preferred":false,"id":203213,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, W.E.","contributorId":100831,"corporation":false,"usgs":true,"family":"Wilson","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":203214,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":30395,"text":"wri844025 - 1984 - Hydrologic conditions in the Chicod Creek basin, North Carolina, before and during channel modifications, 1975-81","interactions":[],"lastModifiedDate":"2017-01-24T09:37:21","indexId":"wri844025","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4025","title":"Hydrologic conditions in the Chicod Creek basin, North Carolina, before and during channel modifications, 1975-81","docAbstract":"Beginning in late 1978, stream channels throughout the 60-square mile Chicod Creek basin underwent extensive modification to increase drainage efficiency and reduce flooding potential. Drainage modifications in this Coastal Plain basin, consisting primarily of channel excavation and clearing of channel blockages, were completed in December 1981. The hydrologic condition of the basin before and during modification was determined from observed data.\r\n\r\nObserved data indicate hydrologic changes occurred in selected basin characteristics. For example, water levels in the surficial aquifer within 250 feet of Juniper Branch declined as much as 0.4 feet during modifications; at distances greater than 250 feet from the stream, ground-water levels did not change. Base flows increased, and suspended-sediment concentrations for high flows were several times greater than before channel modifications. Increases in selected chemical constituent concentrations in stream water during modifications were as follows: calcium, 12 percent; sodium, 18 percent; bicarbonate, 84 percent; and phosphorous, 80 percent. Significant changes were not found in either pesticide concentrations or coliform bacteria counts.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844025","usgsCitation":"Watkins, S., and Simmons, C., 1984, Hydrologic conditions in the Chicod Creek basin, North Carolina, before and during channel modifications, 1975-81: U.S. Geological Survey Water-Resources Investigations Report 84-4025, vii, 36 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844025.","productDescription":"vii, 36 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":59167,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4025/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123292,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4025/report-thumb.jpg"}],"country":"United States","state":"North Carolina","otherGeospatial":"Chicod Creek basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -77.3382568359375,\n 35.60818490437746\n ],\n [\n -77.32177734375,\n 35.60148556537354\n ],\n [\n -77.31216430664061,\n 35.594785665487244\n ],\n [\n -77.2998046875,\n 35.595902354416566\n ],\n [\n -77.28881835937499,\n 35.58808520476323\n ],\n [\n -77.27371215820312,\n 35.5936689609791\n ],\n [\n -77.25997924804688,\n 35.60036895434144\n ],\n [\n -77.24624633789062,\n 35.60930140634475\n ],\n [\n -77.21466064453125,\n 35.610417892730524\n ],\n [\n -77.2064208984375,\n 35.598135685537905\n ],\n [\n -77.19680786132812,\n 35.59255224089235\n ],\n [\n -77.18994140625,\n 35.586968406786475\n ],\n [\n -77.18170166015625,\n 35.576916524038616\n ],\n [\n -77.16659545898438,\n 35.570214567965984\n ],\n [\n -77.14324951171875,\n 35.56686337967425\n ],\n [\n -77.12127685546875,\n 35.563512051219696\n ],\n [\n -77.11166381835938,\n 35.561277754384555\n ],\n [\n -77.10479736328125,\n 35.555691739779654\n ],\n [\n -77.06634521484375,\n 35.543401137387335\n ],\n [\n -77.07321166992188,\n 35.48415637985317\n ],\n [\n -77.07870483398436,\n 35.43605776486772\n ],\n [\n -77.09312438964844,\n 35.38513141280172\n ],\n [\n -77.12265014648438,\n 35.383451974194934\n ],\n [\n -77.29774475097656,\n 35.38569121790089\n ],\n [\n -77.3382568359375,\n 35.60818490437746\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db61161b","contributors":{"authors":[{"text":"Watkins, S.A.","contributorId":83962,"corporation":false,"usgs":true,"family":"Watkins","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":203182,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simmons, C.E.","contributorId":32572,"corporation":false,"usgs":true,"family":"Simmons","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":203181,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70098432,"text":"70098432 - 1984 - Summary of water-resources activities of the U.S. Geological Survey in Colorado: fiscal year 1984","interactions":[],"lastModifiedDate":"2014-04-09T15:20:58","indexId":"70098432","displayToPublicDate":"1985-01-01T14:13:27","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Summary of water-resources activities of the U.S. Geological Survey in Colorado: fiscal year 1984","docAbstract":"Water-resources investigations of the U.S. Geological Survey in Colorado consist of collecting water-resources data and conducting interpretive hydrologic investigations. The water-resources data and the results of the investigations are published or released by either the U.S. Geological Survey or by cooperating agencies. This report describes the water- resources investigations in Colorado for the 1984 fiscal year (October 1, 1983, to September 30, 1984).","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lakewood, CO","doi":"10.3133/70098432","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Summary of water-resources activities of the U.S. Geological Survey in Colorado: fiscal year 1984, Report: iv, 82 p.; Plate: 26.78 x 21.51 inches, https://doi.org/10.3133/70098432.","productDescription":"Report: iv, 82 p.; Plate: 26.78 x 21.51 inches","numberOfPages":"87","additionalOnlineFiles":"Y","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":284177,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70098432.jpg"},{"id":286062,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70098432/report.pdf"},{"id":286063,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70098432/plate-1.pdf"}],"scale":"1000000","country":"United States","state":"Colorado","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0603,36.9924 ], [ -109.0603,41.0034 ], [ -102.0409,41.0034 ], [ -102.0409,36.9924 ], [ -109.0603,36.9924 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53559598e4b0120853e8c23a","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535640,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70199566,"text":"70199566 - 1984 - Transport and concentration controls for chloride, strontium, potassium and lead in Uvas Creek, a small cobble-bed stream in Santa Clara County, California, U.S.A.: 1. Conceptual model","interactions":[],"lastModifiedDate":"2018-09-20T17:13:40","indexId":"70199566","displayToPublicDate":"1984-12-05T17:13:09","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Transport and concentration controls for chloride, strontium, potassium and lead in Uvas Creek, a small cobble-bed stream in Santa Clara County, California, U.S.A.: 1. Conceptual model","docAbstract":"Stream sediments adsorb certain solutes from streams, thereby significantly changing the solute composition; but little is known about the details and rates of these adsorptive processes. To investigate such processes, a 24-hr. injection of a solution containing chloride, strontium, potassium, sodium and lead was made at the head of a 640-m reach of Uvas Creek in west-central Santa Clara County, California. Uvas Creek is a cobble-bed pool-and-riffle stream draining the eastern slopes of the Santa Cruz Mountains. By September 12, 1973, after a long dry season, Uvas Creek had a low (0.0215 m3s−1 average) flow which varied diurnally, from 0.018 to 0.025 m3s−1. Because stream discharge varied while the injection rate was constant, the concentration of tracers (injected solutes), after mixing in the stream, varied inversely with discharge.
Chloride, a nonreactive solute, served as a tracer of water movement. Analysis of extensive chloride concentration data at five sites below the injection point during and after the injection demonstrated that there was considerable underflow of water through the stream gravels; however, the extent of underflow varied greatly within the study reach. Pre-injection water, displaced by tracer-laden water percolating through the gravels, diluted tracers in the stream channel, giving the mistaken impression of groundwater inflow at some points. Accurate measurement of total discharge in such streams requires prolonged tracer injection unless a reach can be found where underflow is negligible.
Strontium and potassium were adsorbed by the bed sediments to a moderate extent and lead was strongly adsorbed. A high proportion of these metals could be removed by adsorption from percolating underflow because of extensive and intimate contact with bed sediments. After channel clearing following injection cutoff, 51% of the added strontium and 96% of the lead remained in the study reach, whereas only 19% of the chloride remained. Packets of sized sediment, placed in the stream before the experiment and withdrawn during and after the injection, indicated that the strontium absorbed on the 0.42–0.50-mm size sediment appeared to achieve near equilibrium with dissolved strontium within less than 2 hr. whereas 3.4–4.0-mm grains had not reached that stage after 24 hr.
The cation-exchange capacity (CEC) of the sediments shows a “bimodal” distribution with grain size. Largest values are in the finest sizes, lower values in the fine-to-medium sand-size range, intermediate values in the coarse- to very coarse-grained sand, and decreasing values with size above very coarse-grained sand. This considerable exchange capacity in coarse-sand to granule-size particles means that a streambed, that has not been infilled with fines to reduce permeability, can be highly reactive and accessible throughout a rather thick sediment layer and hence have a large and available reactive capacity.
As stream discharge increases from low flow, the ratio of underflow to channel flow should decrease rapidly with resultant diminution in percent of solutes sorbed within a particular stream reach.
","language":"English","doi":"10.1016/0022-1694(84)90046-5","usgsCitation":"Kennedy, V.C., Jackman, A.P., Zand, S., Zellweger, G.W., and Avanzino, R., 1984, Transport and concentration controls for chloride, strontium, potassium and lead in Uvas Creek, a small cobble-bed stream in Santa Clara County, California, U.S.A.: 1. Conceptual model: Journal of Hydrology, v. 75, no. 1-4, p. 67-110, https://doi.org/10.1016/0022-1694(84)90046-5.","productDescription":"44 p.","startPage":"67","endPage":"110","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":357589,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","county":"Santa Clara County","otherGeospatial":"Uvas Creek","volume":"75","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Kennedy, V. C.","contributorId":46080,"corporation":false,"usgs":true,"family":"Kennedy","given":"V.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":745872,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jackman, A. P.","contributorId":46957,"corporation":false,"usgs":true,"family":"Jackman","given":"A.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":745873,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zand, S.M.","contributorId":25699,"corporation":false,"usgs":true,"family":"Zand","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":745874,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zellweger, G. W.","contributorId":55445,"corporation":false,"usgs":true,"family":"Zellweger","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":745875,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Avanzino, R.J.","contributorId":37336,"corporation":false,"usgs":true,"family":"Avanzino","given":"R.J.","affiliations":[],"preferred":false,"id":745876,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70186165,"text":"70186165 - 1984 - On the expected width function for topologically random channel networks","interactions":[],"lastModifiedDate":"2020-01-19T11:25:50","indexId":"70186165","displayToPublicDate":"1984-12-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5356,"text":"Journal of Applied Probability","active":true,"publicationSubtype":{"id":10}},"title":"On the expected width function for topologically random channel networks","docAbstract":"No abstract available.
","language":"English","publisher":"Applied Probability Trust","doi":"10.2307/3213700","usgsCitation":"Troutman, B., and Karlinger, M.R., 1984, On the expected width function for topologically random channel networks: Journal of Applied Probability, v. 21, no. 4, p. 836-849, https://doi.org/10.2307/3213700.","productDescription":"14 p. ","startPage":"836","endPage":"849","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338828,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"4","noUsgsAuthors":false,"publicationDate":"2016-07-14","publicationStatus":"PW","scienceBaseUri":"58de1955e4b02ff32c699cdb","contributors":{"authors":[{"text":"Troutman, Brent M.","contributorId":41040,"corporation":false,"usgs":true,"family":"Troutman","given":"Brent M.","affiliations":[],"preferred":false,"id":687724,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Karlinger, Michael R.","contributorId":10777,"corporation":false,"usgs":true,"family":"Karlinger","given":"Michael","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":687725,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70175808,"text":"70175808 - 1984 - Areal lithologic changes in bedrock aquifers in southeastern Minnesota as determined from natural-gamma borehole logs methods","interactions":[],"lastModifiedDate":"2018-04-02T12:16:32","indexId":"70175808","displayToPublicDate":"1984-06-12T11:45:00","publicationYear":"1984","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Areal lithologic changes in bedrock aquifers in southeastern Minnesota as determined from natural-gamma borehole logs methods","docAbstract":"Sedimentary rocks of Paleozoic age in the Hollandale embayment in southeastern Minnesota are as much as 2,000 feet thick and, with the underlying Hinckley sandstone of Proterozoic age, comprise the following five layered aquifers (beginning with the oldest): the Mount Simon-Hinckley, Ironton-Galesville, Prairie du Chien-Jordan, St. Peter and Upper Carbonate. Many of the Paleozoic formations show transitional facies changes from a deep marine depositional environment in the middle of the embayment to a near shore environment along the periphery. Borehole natural-gamma logs were collected to investigate the effects of regional lithologic changes on the hydrology of the Ironton-Galesville, Prairie du Chien-Jordan and St. Peter aquifers.
\nInterpretation of natural-gamma logs shows that a fine-grained sandstone at the base of the Galesville sandstone (basal part of the Ironton-Galesville aquifer) thickens toward the central part of the embayment, which may account for the decrease in hydraulic conductivity of the Ironton-Galesville aquifer in that direction.
\nThe Jordan sandstone, which underlies the Prairie du Chien Group, consists of three members in southeastern Minnesota: the basal Norwalk member, a silty, fine-grained sandstone; the middle Van Oser member, a coarse- to medium-grained quartzose sandstone; and the upper Sunset Point member, a clayey dolomitic sandstone. The Norwalk and Van Oser members were identified by interpretation of natural-gamma logs. Hydraulic conductivity of the Prairie du Chien-Jordan aquifer generally is highest in the Twin City basin (50 feet per day) where the Van Oser is the predominant member; it is lowest to the east and southeast (25 feet per day) where the Norwalk member thickens.
\nInterpretation of natural-gamma logs indicates that the shaley and silty sandstones that comprise the basal St. Peter confining bed, which separates the St. Peter and Prairie du Chien aquifers, are as much as 80 feet thick in the Twin City basin, but are absent in the southern part of the embayment. Differences in potentiometric head across the basal St. Peter are about 30 feet in the Twin City basin where the confining bed is present but only 5 to 10 feet to the south where the confining bed is absent and where the St. Peter aquifer directly overlies the Prairie du Chien-Jordan aquifer.
","conferenceTitle":"Conference on Surface and Borehole Geophysical Investigations","conferenceDate":"February 7-9, 1984","conferenceLocation":"San Antonio, Texas","language":"English","publisher":"National Water Well Association/Environmental Protection Agency","usgsCitation":"Woodward, D.G., 1984, Areal lithologic changes in bedrock aquifers in southeastern Minnesota as determined from natural-gamma borehole logs methods, Conference on Surface and Borehole Geophysical Investigations, San Antonio, Texas, February 7-9, 1984, p. 788-800.","productDescription":"13 p.","startPage":"788","endPage":"800","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":326935,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"Twin Cities Metropolitan 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","language":"English","publisher":"Edwards Underground Water District","publisherLocation":"San Antonio, TX","collaboration":"Prepared in Cooperation with the U.S. Geological Survey and the Texas Department of Water Resources","usgsCitation":"Reeves, R., Maclay, R., and Ozuna, G., 1984, Compilation of hydrologic data for the Edwards Aquifer, San Antonio area, Texas, 1981, with 1934-81 summary: Edwards Underground Water District Bulletin 41, 135 p.","productDescription":"135 p.","numberOfPages":"145","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":282805,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70094969.JPG"},{"id":284822,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70094969/report.pdf"}],"country":"United States","state":"Texas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -100.7971,29.0834 ], [ -100.7971,30.233 ], [ -97.7105,30.233 ], [ -97.7105,29.0834 ], [ -100.7971,29.0834 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57c6aef1e4b0f2f0cebe4619","contributors":{"authors":[{"text":"Reeves, R.D.","contributorId":95043,"corporation":false,"usgs":true,"family":"Reeves","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":491011,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Maclay, R.W.","contributorId":72804,"corporation":false,"usgs":true,"family":"Maclay","given":"R.W.","affiliations":[],"preferred":false,"id":491010,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ozuna, G. B.","contributorId":25205,"corporation":false,"usgs":true,"family":"Ozuna","given":"G. B.","affiliations":[],"preferred":false,"id":491009,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70198691,"text":"70198691 - 1984 - Volatilization of chlorinated hydrocarbons from water","interactions":[],"lastModifiedDate":"2018-08-15T07:51:03","indexId":"70198691","displayToPublicDate":"1984-01-01T07:49:22","publicationYear":"1984","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Volatilization of chlorinated hydrocarbons from water","docAbstract":"Coefficients for the volatilization from water of 1,1,1-trichloroethane and 1,2-dichloroethane were measured in a stirred tank. Experiments at constant mixing conditions over a wide range of concentrations showed that the volatilization coefficient was independent of concentration, confirming the assumption that volatilization is a first order process. Simultaneous measurements of the volatilization coefficient and the oxygen absorption coefficient over a wide range of mixing conditions showed that the chlorinated hydrocarbon/oxygen coefficient ratios for both compounds were independent of mixing conditions. Ratios of 0.596 and 0.621 were obtained for 1,1,1-trichloroethane and 1,2-dichloroethane, respectively.
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","language":"English","publisher":"Elsevier","doi":"10.1016/0045-6535(84)90060-2","usgsCitation":"Rathbun, R.E., and Tai, D.Y., 1984, Volatilization of ketones: Chemosphere, v. 13, no. 9, p. 1009-1023, https://doi.org/10.1016/0045-6535(84)90060-2.","productDescription":"15 p. ","startPage":"1009","endPage":"1023","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338314,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d6303ee4b05ec799131111","contributors":{"authors":[{"text":"Rathbun, R. E.","contributorId":61796,"corporation":false,"usgs":true,"family":"Rathbun","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":686122,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tai, D. Y.","contributorId":59778,"corporation":false,"usgs":true,"family":"Tai","given":"D.","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":686123,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70185616,"text":"70185616 - 1984 - Pore volume determination in activated carbon and coal","interactions":[],"lastModifiedDate":"2020-01-20T19:30:05","indexId":"70185616","displayToPublicDate":"1984-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1182,"text":"Carbon","active":true,"publicationSubtype":{"id":10}},"title":"Pore volume determination in activated carbon and coal","docAbstract":"No abstract available.
","language":"English","publisher":"Elsevier","doi":"10.1016/0008-6223(84)90140-4","usgsCitation":"Reucroft, P., Patel, K., and Chiou, C.T., 1984, Pore volume determination in activated carbon and coal: Carbon, v. 22, no. 1, p. 100-102, https://doi.org/10.1016/0008-6223(84)90140-4.","productDescription":"3 p. ","startPage":"100","endPage":"102","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338315,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d6303ee4b05ec79913110f","contributors":{"authors":[{"text":"Reucroft, P.J.","contributorId":189816,"corporation":false,"usgs":false,"family":"Reucroft","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":686125,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Patel, K.B.","contributorId":189817,"corporation":false,"usgs":false,"family":"Patel","given":"K.B.","email":"","affiliations":[],"preferred":false,"id":686126,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chiou, C. T.","contributorId":97080,"corporation":false,"usgs":true,"family":"Chiou","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":686127,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}