{"pageNumber":"12","pageRowStart":"275","pageSize":"25","recordCount":409,"records":[{"id":25740,"text":"wri944057 - 1995 - Reconnaissance of ground-water quality in the North Platte Natural Resources District, western Nebraska, June-July 1991","interactions":[],"lastModifiedDate":"2012-02-02T00:08:14","indexId":"wri944057","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1995","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":"94-4057","title":"Reconnaissance of ground-water quality in the North Platte Natural Resources District, western Nebraska, June-July 1991","docAbstract":"One-hundred twenty wells completed in unconfined Quaternary alluvial, Ogallala, Arikaree, Brule fractured, sand and confined Chadron and undifferentiated Cretaceous water-bearing units were sampled in June and July 1991 to characterize the quality of ground water in the study area. More than 75 percent of the water samples had nitrate and nitrite as nitrogen concentrations equal to or less than 6.0 milligrams per liter. Samples from six wells completed in Quaternary alluvial and Brule fractured water-bearing units exceeded the U.S. Environmental Protection Agency Maximum Contaminant Level of 10 milligrams per liter nitrate and nitrite as nitrogen. Water from several wells completed in Quaternary alluvial and the Brule water-bearing units had detectable concentrations of alachlor, atrazine, deethylatrazine, or prometon. Major element concentrations in water from 44 wells indicated that the water-bearing units had distinct chemistry. Water from unconfined water- bearing units generally was a calcium bicarbonate type and water from the confined water-bearing units generally was a sodium bicarbonate type. Measurements of pH and concentrations of dissolved solids, sulfate, chloride, fluoride, arsenic, beryllium, manganese, adjusted gross alpha activities, radon, and uranium in ground water exceeded final or proposed U.S. Environmental Protection Agency Maximum Contaminant Levels or Secondary Maximum Contaminant Levels.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri944057","usgsCitation":"Verstraeten, I., Sibray, S., Cannia, J.C., and Tanner, D.Q., 1995, Reconnaissance of ground-water quality in the North Platte Natural Resources District, western Nebraska, June-July 1991: U.S. Geological Survey Water-Resources Investigations Report 94-4057, vi, 114 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944057.","productDescription":"vi, 114 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":156924,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4057/report-thumb.jpg"},{"id":54502,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4057/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db625003","contributors":{"authors":[{"text":"Verstraeten, Ingrid M.","contributorId":61033,"corporation":false,"usgs":true,"family":"Verstraeten","given":"Ingrid M.","affiliations":[],"preferred":false,"id":194875,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sibray, S. S.","contributorId":63048,"corporation":false,"usgs":true,"family":"Sibray","given":"S. S.","affiliations":[],"preferred":false,"id":194876,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cannia, J. C.","contributorId":105258,"corporation":false,"usgs":true,"family":"Cannia","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":194878,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tanner, D. Q.","contributorId":73224,"corporation":false,"usgs":true,"family":"Tanner","given":"D.","email":"","middleInitial":"Q.","affiliations":[],"preferred":false,"id":194877,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":44882,"text":"wri954034 - 1995 - Geohydrologic conditions and land use in the Gallatin Valley, southwestern Montana, 1992-93","interactions":[],"lastModifiedDate":"2023-01-04T20:56:01.737073","indexId":"wri954034","displayToPublicDate":"1995-08-01T00:00:00","publicationYear":"1995","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":"95-4034","title":"Geohydrologic conditions and land use in the Gallatin Valley, southwestern Montana, 1992-93","docAbstract":"The Gallatin Valley is part of an intermontane basin in southwestern Montana with an area of about 540 mi2. The valley is drained by the Gallatin River and its tributaries. After formation of the Three Forks structural basin, the Gallatin Valley was filled with as much as 6,000 feet of Tertiary and Quaternary sediments. Depth to water in the study area generally ranges from about 3 feet to about 460 feet below land surface. The median specific capacity of 26 wells completed in alluvium was 4.6 gallons per minute per foot. The median specific capacity of 21 wells completed in Quaternary and Tertiary alluvial-fan deposits in the southern and eastern part of the area was 1.6 gallons per minute per foot. The median specific capacity of 16 wells completed in Tertiary sediments was 0.78 gallon per minute per foot. Water from 38 wells sampled for water-quality analyses generally was a calcium bicarbonate type containing dissolved-solids concentrations ranging from 113 to 551 milligrams per liter. Radon-222 concentrations in water from 16 samples wells ranged from 170 to 1,565 picocuries per liter. Water samples collected from 6 wells were analyzed for a total of 54 pesticides and pesticide- degradation products. No pesticides or related analytes were detected in any of the samples. Agriculture is the primary land use in the Gallatin Valley; however, population growth has resulted in the establishment of numerous rural subdivisions. Water-level measurements made during this study coupled with long-term water-level trends do not indicate any significant water-level changes resulting from increased ground-water withdrawals. The occurrence of larger nitrate concentrations (maximum of 4.5 milligrams per liter) in ground water in more densely developed areas indicates a possible influence of subdivision development on ground-water quality.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri954034","usgsCitation":"Slagle, S.E., 1995, Geohydrologic conditions and land use in the Gallatin Valley, southwestern Montana, 1992-93: U.S. Geological Survey Water-Resources Investigations Report 95-4034, 2 Plates: 43.31 x 38.00 inches and 33.00 x 35.73 inches, https://doi.org/10.3133/wri954034.","productDescription":"2 Plates: 43.31 x 38.00 inches and 33.00 x 35.73 inches","costCenters":[],"links":[{"id":134547,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":82237,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4034/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82236,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4034/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":411382,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48148.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Montana","otherGeospatial":"Gallatin Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -110.9292,\n              45.5167\n            ],\n            [\n              -110.9292,\n              46\n            ],\n            [\n              -111.4767,\n              46\n            ],\n            [\n              -111.4767,\n              45.5167\n            ],\n            [\n              -110.9292,\n              45.5167\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8e2c","contributors":{"authors":[{"text":"Slagle, Steven E.","contributorId":35284,"corporation":false,"usgs":true,"family":"Slagle","given":"Steven","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":230611,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70018934,"text":"70018934 - 1995 - US Geological Survey research on the environmental fate of uranium mining and milling wastes","interactions":[],"lastModifiedDate":"2014-10-03T14:35:20","indexId":"70018934","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1539,"text":"Environmental Geology","active":true,"publicationSubtype":{"id":10}},"title":"US Geological Survey research on the environmental fate of uranium mining and milling wastes","docAbstract":"Studies by the US Geological Survey (USGS) of uranium mill tailings (UMT) have focused on characterizing the forms in which radionuclides are retained and identifying factors influencing the release of radionuclides to air and water. Selective extraction studies and studies of radionuclide sorption by and leaching from components of UMT showed alkaline earth sulfate and hydrous ferric oxides to be important hosts of radium-226 (<sup>226</sup>Ra) in UMT. Extrapolating from studies of barite dissolution in anerobic lake sediments, the leaching of <sup>226</sup>Ra from UMT by sulfate-reducing bacteria was investigated; a marked increase in <sup>226</sup>Ra release to aqueous solution as compared to sterile controls was demonstrated. A similar action of iron(III)-reducing bacteria was later shown. Ion exchangers such as clay minerals can also promote the dissolution of host-phase minerals and thereby influence the fate of radionuclides such as <sup>226</sup>Ra. Radon release studies examined particle size and ore composition as variables. Aggregation of UMT particles was shown to mask the higher emanating fraction of finer particles. Studies of various ores and ore components showed that UMT cannot be assumed to have the same radon-release characteristics as their precursor ores, nor can <sup>226</sup>Ra retained by various substrates be assumed to emanate the same fraction of radon. Over the last decade, USGS research directed at offsite mobility of radionuclides from uranium mining and milling processes has focused on six areas: the Midnite Mine in Washington; Ralston Creek and Reservoir, Colorado; sites near Canon City, Colorado; the Monument Valley District of Arizona and Utah; the Cameron District of Arizona; and the Puerco River basin of Arizona and New Mexico.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF00776028","issn":"09430105","usgsCitation":"Landa, E.R., and Gray, J.R., 1995, US Geological Survey research on the environmental fate of uranium mining and milling wastes: Environmental Geology, v. 26, no. 1, p. 19-31, https://doi.org/10.1007/BF00776028.","productDescription":"13 p.","startPage":"19","endPage":"31","numberOfPages":"13","costCenters":[],"links":[{"id":205768,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00776028"},{"id":226666,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbb50e4b08c986b32861f","contributors":{"authors":[{"text":"Landa, E. R.","contributorId":100002,"corporation":false,"usgs":true,"family":"Landa","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":381136,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gray, J. R.","contributorId":63372,"corporation":false,"usgs":true,"family":"Gray","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":381135,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70019651,"text":"70019651 - 1995 - 222Rn variations in Mystery Cave, Minnesota","interactions":[],"lastModifiedDate":"2012-03-12T17:19:21","indexId":"70019651","displayToPublicDate":"1995-01-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1884,"text":"Health Physics","active":true,"publicationSubtype":{"id":10}},"title":"222Rn variations in Mystery Cave, Minnesota","docAbstract":"222Rn concentrations and meteorological parameters were measured at 4- h intervals over a 2-y period in Mystery Cave, southeastern Minnesota. Continuous radon monitors and meteorological sensors connected to data loggers were installed at several locations along commercial tour routes. 222Rn concentrations ranged as high as 25 kBq m-3 in summer and 20 kBq m-3 in winter. Average winter concentrations were lower than summer by at least a factor of two. Seasonal radon variations were correlative with outside air temperatures. During the winter, radon concentrations were observed to fluctuate periodically by factors of 20 or more in under 24 h. Both the long- and short-term variations are correlative with temperature- induced mixing of cave air with surface air.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Health Physics","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00179078","usgsCitation":"Lively, R., and Krafthefer, B., 1995, 222Rn variations in Mystery Cave, Minnesota: Health Physics, v. 68, no. 4, p. 590-594.","startPage":"590","endPage":"594","numberOfPages":"5","costCenters":[],"links":[{"id":227880,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"68","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e252e4b0c8380cd45ab4","contributors":{"authors":[{"text":"Lively, R.S.","contributorId":70927,"corporation":false,"usgs":true,"family":"Lively","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":383446,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krafthefer, B.C.","contributorId":85735,"corporation":false,"usgs":true,"family":"Krafthefer","given":"B.C.","email":"","affiliations":[],"preferred":false,"id":383447,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70000602,"text":"70000602 - 1994 - Measurement of radon gas on major faults in California, USA","interactions":[],"lastModifiedDate":"2012-03-08T17:16:37","indexId":"70000602","displayToPublicDate":"2010-09-28T23:09:30","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":646,"text":"Acta Seismologica Sinica","active":true,"publicationSubtype":{"id":10}},"title":"Measurement of radon gas on major faults in California, USA","docAbstract":"Abundant data have been gathered through measurements of radon gas emission in the soil on several major active faults, such as San Andreas and Calaveras, in California, U.S.A.. They show radon emissions and their spatial variations at the unlocked, locked, and creeping sections of faults with different tectonic movements. The characteristics of these variations and the role of fault gases in the research on earthquake prediction are discussed in this paper. ?? 1994 Acta Seismologica Sinica.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Acta Seismologica Sinica","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Seismological Society of China","doi":"10.1007/BF02651919","issn":"10009116","usgsCitation":"Zhang, W., and King, C., 1994, Measurement of radon gas on major faults in California, USA: Acta Seismologica Sinica, v. 7, no. 1, p. 159-165, https://doi.org/10.1007/BF02651919.","startPage":"159","endPage":"165","costCenters":[],"links":[{"id":18973,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02651919"},{"id":203368,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db61118e","contributors":{"authors":[{"text":"Zhang, W.","contributorId":92399,"corporation":false,"usgs":true,"family":"Zhang","given":"W.","email":"","affiliations":[],"preferred":false,"id":346401,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, C.-Y.","contributorId":81225,"corporation":false,"usgs":true,"family":"King","given":"C.-Y.","affiliations":[],"preferred":false,"id":346400,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29780,"text":"wri944109 - 1994 - Hydrogeology and ground-water quality of northern Bucks County, Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-12T09:42:29","indexId":"wri944109","displayToPublicDate":"1995-07-01T00:00:00","publicationYear":"1994","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":"94-4109","title":"Hydrogeology and ground-water quality of northern Bucks County, Pennsylvania","docAbstract":"<p>The 187-square mile study area is in the Triassic-Jurassic Newark Basin. Most of the area is underlain by sedimentary rocks of Upper Triassic age (74 percent) and intrusive diabase of Jurassic age (12 percent) and includes two southwest-northeast trending valleys underlain by carbonate and crystalline rock.</p>\n<p>Ground water in the sedimentary rocks of Triassic age moves through a network of interconnecting secondary openings fractures, bedding planes, and joints. The ground-water system consists of beds with a relatively high transmissivity separated by beds with a relatively low transmissivity that form a leaky, multiaquifer system. Ground water is unconfined in the shallower part of the aquifer and confined or semiconfined in the deeper part of the aquifer. Most deep wells are open to several water-bearing zones and are multiaquifer wells.</p>\n<p>The frequency of occurrence of water-bearing zones decreases with depth. Sixty-five percent of water-bearing zones for all hydrogeologic units are within 200 feet of land surface, and 85 percent are within 300 feet of land surface. On the basis of the median specific capacity of nondomestic wells, carbonate rocks, the Brunswick Group, and the Stockton Formation are the most productive hydrogeologic units. Carbonate rocks and the Stockton Formation have the highest median nondomestic well yields (156 and 120 gallons per minute, respectively) among the hydrogeologic units. Thirty-four percent of domestic wells drilled in diabase, 30 percent in the Lockatong Formation, and 21 percent in carbonate rock yield less than 5 gallons per minute.</p>\n<p>Average water budgets for the Cooks, Tinicum, Paunnacussing, and Mill Creek Basins weighted by drainage area were calculated for 1991-92. Average annual precipitation was 41.7 in. (inches); average annual evapotranspiration (ET) and other losses were 26.2 in. or 63 percent of precipitation; average annual streamflow was 15.9 in., or 38 percent of the average precipitation; and the average annual change in ground-water storage was a decrease of 0.3 in., or less than 1 percent of the average annual precipitation. Average estimated recharge for 1991-92 weighted by drainage area was 10.1 in. [0.485 (Mgal/d)/mi<sup>2</sup> (million gallons per day per square mile)]; this is equal to a recharge rate of 758 gallons per day per acre.</p>\n<p>Water budgets for the Tohickon Creek Basin were calculated for 1968-91 (prior to regulation of the stream by Lake Nockamixon). The average annual precipitation was 47.2 in.; average annual ET and other losses were 24.3 in., or 51 percent of the average annual precipitation; and annual streamflow was 22.6 in., or 48 percent of the average annual precipitation.</p>\n<p>Streamflow hydrographs for 1991-92 for Cooks, Tinicum, Paunnacussing, and Mill Creeks were separated into baseflow and surface-runoff components. Average annual ground-water discharge to streams weighted by drainage area was 8.4 in. [0.403 (Mgal/d)/mi<sup>2</sup>], which was 20 percent of the average annual precipitation and 53 percent of the average annual streamflow. Average annual surface runoff weighted by drainage area was 7.4 in., which was 18 percent of the average annual precipitation and 47 percent of the average annual streamflow. Annual base flow for 1936-71 for Tohickon Creek ranged from 2.5 in. [0.12 (Mgal/d)/mi<sup>2</sup>] in 1965 to 8.4 in. [0.40 (Mgal/d)/mi<sup>2</sup>] in 1945. The median base flow was 5.3 in. [0.25 (Mgal/d)/mi<sup>2</sup>].</p>\n<p>Water from wells in the crystalline rocks has the lowest median pH (5.8), the lowest median specific conductance (139 microsiemens per centimeter), the lowest median alkalinity [16 mg/L (milligrams per liter) as CaCOg], and the highest dissolved oxygen concentration (9.0 mg/L) of the hydrogeologic units. Water from wells in carbonate rocks has the highest median pH (7.8) and the highest median alkalinity (195 mg/L as CaCO3) of the hydrogeologic units. Water from wells in the Lockatong Formation has the highest median specific conductance (428 microsiemens per centimeter) and the lowest dissolved oxygen concentration (0.8 mg/L) of the hydrogeologic units. Water from wells in crystalline rocks contains the lowest concentrations of total dissolved solids (TDS) of the hydrogeologic units. Water from the Lockatong Formation contains the highest concentration of TDS of the hydrogeologic units. Water from only 1 of 83 wells sampled exceeded the U.S. Environmental Protection Agency (USEPA) secondary maximum contaminant level (SMCL) for TDS; the well is in the Lockatong Formation. Five of 86 samples (6 percent) and 6 of 75 samples (8 percent) exceed the USEPA SMCL for iron and manganese, respectively. Nitrate is the most prevalent nitrogen species in ground water. The median nitrate concentration for all hydrogeologic units is 2.3 mg/L. Of 71 water samples from wells, no concentrations of nitrate exceed the USEPA maximum contaminant level. The median dissolved radon-222 activity was highest for water samples from wells in crystalline rock [3,600 pCi/L (picocuries per liter)] and lowest for water samples from wells in the Lockatong Formation (340 pCi/L) and diabase (350 pCi/L). Water samples for analysis for volatile organic compounds (VOC's) were collected from 34 wells in areas where the potential existed for the presence of VOC's in ground water. VOC's were detected in 23 percent of the 34 wells sampled. The most commonly detected compound was trichloroethylene (13 percent of sampled wells).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944109","collaboration":"Prepared in cooperation with New Hope Borough and Bridgeton, Buckingham, Nockamixon, Plumstead, Solebury, Springfield, Tinicum, and Wrightstown townships","usgsCitation":"Sloto, R.A., and Schreffler, C.L., 1994, Hydrogeology and ground-water quality of northern Bucks County, Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 94-4109, Report: viii, 85 p.; 1 Plate: 36.71 x 38.57 inches, https://doi.org/10.3133/wri944109.","productDescription":"Report: viii, 85 p.; 1 Plate: 36.71 x 38.57 inches","numberOfPages":"93","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":313236,"rank":301,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4109/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"},{"id":58583,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4109/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":119628,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4109/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania","county":"Bucks 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Ronald A. rasloto@usgs.gov","contributorId":424,"corporation":false,"usgs":true,"family":"Sloto","given":"Ronald","email":"rasloto@usgs.gov","middleInitial":"A.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":202112,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schreffler, Curtis L. clschref@usgs.gov","contributorId":333,"corporation":false,"usgs":true,"family":"Schreffler","given":"Curtis","email":"clschref@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":202113,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":17243,"text":"ofr94381 - 1994 - Hydrologic data for northern Bucks County, Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-13T10:26:56","indexId":"ofr94381","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1994","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":"94-381","title":"Hydrologic data for northern Bucks County, Pennsylvania","docAbstract":"Hydrologic and water-quality data were collected in northern Bucks County, Pa., as part of a study conducted by the U.S. Geological Survey, in cooperation with Bridgeton, Buckingham, Nockamixon, Plumstead, Solebury, Springfield, Tinicum, and Wrightstown Townships and New Hope Borough. Hydrologic data on ground water and surface water were collected to provide basic information on the quality and quantity of water resources in northern Bucks County. \r\n\r\n      Ground-water data include descriptions of 1,357 wells and water levels for 28 observation wells measured during 1990-93. Ground-water-quality analyses for 117 wells include physical properties and concentrations of major ions, nutrients, selected metals and other trace constituents, radon, and volatile organic compounds. Surface-water data include chemical analyses of water samples collected at sites on Beaver Creek, Crooks Creek, Geddes Run, Little Tinicum Creek, Paunnacussing Creek, Pidcock Creek, Rapp Creek, Smithtown Creek, and Tinicum Creek.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94381","usgsCitation":"Schreffler, C.L., McManus, B., Rowland-Lesitsky, C.J., and Sloto, R., 1994, Hydrologic data for northern Bucks County, Pennsylvania: U.S. Geological Survey Open-File Report 94-381, iv, 90 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr94381.","productDescription":"iv, 90 p. :ill., maps ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":149360,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0381/report-thumb.jpg"},{"id":21610,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0381/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":46392,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0381/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c80e","contributors":{"authors":[{"text":"Schreffler, Curtis L. clschref@usgs.gov","contributorId":333,"corporation":false,"usgs":true,"family":"Schreffler","given":"Curtis","email":"clschref@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":175571,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McManus, B. C.","contributorId":45731,"corporation":false,"usgs":true,"family":"McManus","given":"B. C.","affiliations":[],"preferred":false,"id":175573,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rowland-Lesitsky, C. J.","contributorId":52982,"corporation":false,"usgs":true,"family":"Rowland-Lesitsky","given":"C.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":175574,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sloto, R. A.","contributorId":36155,"corporation":false,"usgs":true,"family":"Sloto","given":"R. A.","affiliations":[],"preferred":false,"id":175572,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":19835,"text":"ofr9431 - 1994 - Ground-water quality and geochemistry, Carson Desert, western Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:07:41","indexId":"ofr9431","displayToPublicDate":"1995-05-01T00:00:00","publicationYear":"1994","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":"94-31","title":"Ground-water quality and geochemistry, Carson Desert, western Nevada","docAbstract":"Aquifers in the Carson Desert are the primary source of drinking water, which is highly variable in chemical composition. In the shallow basin-fill aquifers, water chemistyr varies from a dilute calcium bicarbonate-dominated water beneath the irrigated areas to a saline sodium chloride- dominated water beneath unirrigated areas. Water samples from the shallow aquifers commonly have dissolved solids, chloride, magnesium, sulfate, arsenic, and manganese concentrations that exceed State of Nevada drinking-water standards. Water in the intermediante basin-fill aquifers is a dilute sodium bicarbonate type in the Fallon area and a distinctly more saline sodium chloride type in the Soda Lake-Upsal Hogback area. Dissolved solids, chloride, arsenic, fluoride, and manganese concen- trations commonly exceed drinking-water standards. The basalt aquifer contains a dilute sodium bicarbonate chloride water. Arsenic concentrations exceed standards in all sampled wells. The concen- trations of major constituents in ground water beneath the southern Carson Desert are the result of evapotranspiration and natural geochemical reactions with minerals derived mostly from igneous rocks. Water with higher concentrations of iron and manganese is near thermodynamic equilibrium with siderite and rhodochrosite and indicates that these elements may be limited by the solubility of their respective carbonate minerals. Naturally occurring radionuclides (uranium and radon-222) are present in ground water from the Carson Desert in concen- tratons higher than proposed drinking-water standards. High uranium concentrations in the shallow aquifers may be caused by evaporative concentration and the release of uranium during dissolution of iron and manganese oxides or the oxidation of sedimentary organic matter that typically has elevated uranium concentrations. Ground water in the Carson Desert does not appear to have be contaminated by synthetic organic chemicals.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr9431","usgsCitation":"Lico, M.S., and Seiler, R.L., 1994, Ground-water quality and geochemistry, Carson Desert, western Nevada: U.S. Geological Survey Open-File Report 94-31, v, 91 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr9431.","productDescription":"v, 91 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":153446,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0031/report-thumb.jpg"},{"id":49319,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0031/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4822e4b07f02db4e20d8","contributors":{"authors":[{"text":"Lico, Michael S.","contributorId":75897,"corporation":false,"usgs":true,"family":"Lico","given":"Michael","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":181599,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Seiler, R. L.","contributorId":87546,"corporation":false,"usgs":true,"family":"Seiler","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":181600,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21345,"text":"ofr9333 - 1994 - Ground-water quality and geochemistry in Carson and Eagle Valleys, western Nevada and eastern California","interactions":[],"lastModifiedDate":"2022-10-18T11:22:58.709129","indexId":"ofr9333","displayToPublicDate":"1995-04-01T00:00:00","publicationYear":"1994","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":"93-33","title":"Ground-water quality and geochemistry in Carson and Eagle Valleys, western Nevada and eastern California","docAbstract":"Aquifers in Carson and Eagle Valleys are an important source of water for human consumption and agriculture. Concentrations of major constituents in water from the principal aquifers on the west sides of Carson and Eagle Valleys appear to be a result of natural geochemical reactions with minerals derived primarily from plutonic rocks. In general, water from principal aquifers is acceptable for drinking when compared with current (1993) Nevada State drinking-water maximum contaminant level standards. Water was collected and analyzed for all inorganic constituents for which primary or secondary drinking-water standards have been established. About 3 percent of these sites had con- stituents that exceeded one or more primary or secondary drinking-water standards have been established. About 3 percent of these sites had con- stituents that exceeded one or more primary standards and water at about 10 percent of the sites had at least one constituent that surpassed a secondary standard. Arsenic exceeded the standard in water at less than 1 percent of the principal aquifer sites; nitrate surpassed its standard in water at 3 percent of 93 sites. Water from wells in the principal aquifer with high concentrations of nitrate was in areas where septic systems are used; these concentrations indicate that contamination may be entering the wells. Concentrations of naturally occurring radionuclides in water from the principal aquifers, exceed the proposed Federal standards for some constituents, but were not found t be above current (1993) State standards. The uranium concen- trations exceeded the proposed 20 micrograms per liter Federal standard at 10 percent of the sites. Of the sites analyzed for all of the inorganic constituents with primary standards plus uranium, 15 percent exceed one or more established standards. If the proposed 20 micrograms per liter standard for uranium is applied to the sampled sites, then 23 percent would exceed the standard for uranium or some other constituent with a primary drinking water standard. This represents a 50-percent increase in the frequency of exceedance. Almost all water sampled from the principal aquifers exceeds the 300 picocuries per liter proposed standard for radon. Ground-water sampling sites with the highest radon activities in water are most commonly located in the upland aquifers in the Sierra Nevada and in the principal aquifers beneath the west sides of Carson and Eagle Valleys.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr9333","usgsCitation":"Welch, A., 1994, Ground-water quality and geochemistry in Carson and Eagle Valleys, western Nevada and eastern California: U.S. Geological Survey Open-File Report 93-33, vi, 99 p., https://doi.org/10.3133/ofr9333.","productDescription":"vi, 99 p.","costCenters":[],"links":[{"id":50907,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0033/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":155148,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0033/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a214","contributors":{"authors":[{"text":"Welch, Alan H.","contributorId":45286,"corporation":false,"usgs":true,"family":"Welch","given":"Alan H.","affiliations":[],"preferred":false,"id":184258,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70209724,"text":"70209724 - 1994 - Geology and occurrence of radon","interactions":[],"lastModifiedDate":"2020-04-30T18:55:51.538414","indexId":"70209724","displayToPublicDate":"1994-12-31T12:51:33","publicationYear":"1994","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"6","title":"Geology and occurrence of radon","docAbstract":"<p><span>The accumulation of radon indoors is commonly due to movement of radon from adjacent soil and rock into a building foundation through joints, utility openings, cracks, or porous block walls. When air pressure inside the building is lower than that in the soil, pressure-driven flow of radonbearing soil gas can occur (see Chapter 2). Whether or not an indoor radon problem results depends on: (1) the radium concentration in the soil and underlying rock, (2) the ability of radon to escape from the solid material holding the parent radium, and (3) the ability of radon to move through the rock and soil fractures and pores.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Radon: Prevalence, measurements, health risks and control","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"American Society for Testing and Materials","usgsCitation":"Schumann, R.R., Gundersen, L.C., and Tanner, A.B., 1994, Geology and occurrence of radon, chap. 6 <i>of</i> Radon: Prevalence, measurements, health risks and control, p. 83-96.","productDescription":"14 p.","startPage":"83","endPage":"96","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":374204,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Schumann, R. Randall 0000-0001-8158-6960 rschumann@usgs.gov","orcid":"https://orcid.org/0000-0001-8158-6960","contributorId":1569,"corporation":false,"usgs":true,"family":"Schumann","given":"R.","email":"rschumann@usgs.gov","middleInitial":"Randall","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":787684,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gundersen, Linda C. lgundersen@usgs.gov","contributorId":238,"corporation":false,"usgs":true,"family":"Gundersen","given":"Linda","email":"lgundersen@usgs.gov","middleInitial":"C.","affiliations":[{"id":501,"text":"Office of Science Quality and Integrity","active":true,"usgs":true}],"preferred":true,"id":787685,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tanner, A. B.","contributorId":117522,"corporation":false,"usgs":true,"family":"Tanner","given":"A.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":787686,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":20319,"text":"ofr9493 - 1994 - Activities and summary statistics of radon-222 in stream- and ground-water samples, Owl Creek basin, north-central Wyoming, September 1991 through March 1992","interactions":[],"lastModifiedDate":"2012-02-02T00:07:38","indexId":"ofr9493","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-93","title":"Activities and summary statistics of radon-222 in stream- and ground-water samples, Owl Creek basin, north-central Wyoming, September 1991 through March 1992","docAbstract":"Radon-222 activity was measured for 27 water samples from streams, an alluvial aquifer, bedrock aquifers, and a geothermal system, in and near the 510-square mile area of Owl Creek Basin, north- central Wyoming.  Summary statistics of the radon- 222 activities are compiled.  For 16 stream-water samples, the arithmetic mean radon-222 activity was 20 pCi/L (picocuries per liter), geometric mean activity was 7 pCi/L, harmonic mean activity was 2 pCi/L and median activity was 8 pCi/L.  The standard deviation of the arithmetic mean is 29 pCi/L.  The activities in the stream-water samples ranged from 0.4 to 97 pCi/L.  The histogram of stream-water samples is left-skewed when compared to a normal distribution.  For 11 ground-water samples, the arithmetic mean radon- 222 activity was 486 pCi/L, geometric mean activity was 280 pCi/L, harmonic mean activity was 130 pCi/L and median activity was 373 pCi/L. The standard deviation of the arithmetic mean is 500 pCi/L.  The activity in the ground-water samples ranged from 25 to 1,704 pCi/L.  The histogram of ground-water samples is left-skewed when compared to a normal distribution.  (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr9493","usgsCitation":"Ogle, K., and Lee, R.W., 1994, Activities and summary statistics of radon-222 in stream- and ground-water samples, Owl Creek basin, north-central Wyoming, September 1991 through March 1992: U.S. Geological Survey Open-File Report 94-93, iv, 15 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr9493.","productDescription":"iv, 15 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":152105,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0093/report-thumb.jpg"},{"id":49850,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0093/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699da6","contributors":{"authors":[{"text":"Ogle, K.M.","contributorId":38178,"corporation":false,"usgs":true,"family":"Ogle","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":182442,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, R. W.","contributorId":86757,"corporation":false,"usgs":true,"family":"Lee","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":182443,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70017596,"text":"70017596 - 1994 - Seasonal variability of soil-gas radon concentration in central California","interactions":[],"lastModifiedDate":"2025-07-17T13:14:58.62786","indexId":"70017596","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3222,"text":"Radiation Measurements","active":true,"publicationSubtype":{"id":10}},"title":"Seasonal variability of soil-gas radon concentration in central California","docAbstract":"<p><span>Radon concentrations in soil gas were measured by the track-etch method in 60 shallow holes, each 70 cm deep and supported by a capped plastic tube, along several major faults in central California during 1975–1985. This set of data was analyzed to investigate the seasonal variability of soil-gas radon concentration in an area which has various geological conditions but similar climate. The results show several different patterns of seasonal variations, but all of which can be largely attributed to the water-saturation and moisture-retention characteristics of the shallow part of the soil. During the rainy winter and spring seasons, radon tended to be confined underground by the water-saturated surface soil which had much reduced gas permeability, while during the sunny summer and autumn seasons, it exhaled more readily as the soil became drier and more permeable. At several sites located on creeping faults, the radon-variation patterns changed with time, possibly because of disturbance of site condition by fault movement.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/1350-4487(94)90004-3","issn":"13504487","usgsCitation":"King, C., and Minissale, A., 1994, Seasonal variability of soil-gas radon concentration in central California: Radiation Measurements, v. 23, no. 4, p. 683-692, https://doi.org/10.1016/1350-4487(94)90004-3.","productDescription":"10 p.","startPage":"683","endPage":"692","numberOfPages":"10","costCenters":[],"links":[{"id":228473,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b88e5e4b08c986b316c13","contributors":{"authors":[{"text":"King, C.-Y.","contributorId":81225,"corporation":false,"usgs":true,"family":"King","given":"C.-Y.","affiliations":[],"preferred":false,"id":376955,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Minissale, A.","contributorId":94441,"corporation":false,"usgs":true,"family":"Minissale","given":"A.","email":"","affiliations":[],"preferred":false,"id":376956,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70017670,"text":"70017670 - 1994 - Fractionation of families of major, minor, and trace metals across the melt-vapor interface in volcanic exhalations","interactions":[],"lastModifiedDate":"2019-06-06T13:19:00","indexId":"70017670","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Fractionation of families of major, minor, and trace metals across the melt-vapor interface in volcanic exhalations","docAbstract":"Chemical families of metals fractionate systematically as they pass from a silicate melt across the interface with the vapor phase and on into a cooled volcanic plume. We measured three groups of metals in a small suite of samples collected on filters from the plumes of Kilauea (Hawaii, USA), Etna (Sicily), and Merapi (Java) volcanoes. These were the major, minor, and trace metals of the alkali and alkaline earth families (K, Rb, Cs, Ca, Sr, Ba), a group of ordinarily rare metals (Cd, Cu, In, Pb, Tl) that are related by their chalcophile affinities, and the radon daughter nuclides 210Po, 210Bi, and 210Pb. The measurements show the range and some details of systematic melt-vapor fractionation within and between these groups of metals. In the plumes of all three volcanoes, the alkali metals are much more abundant than the alkaline earth metals. In the Kilauea plume, the alkali metals are at least six times more abundant than the alkaline earth metals, relative to abundances in the melt; at Etna, the factor is at least 300. Fractionations within each family are, commonly, also distinctive; in the Kilauea plume, in addition to the whole alkaline earth family being depleted, the heaviest metals of the family (Sr, Ba) are progressively more depleted than the light metal Ca. In plumes of fumaroles at Merapi, K/Cs ratios were approximately three orders of magnitude smaller than found in other earth materials. This may represent the largest observed enrichment of the \"light ion lithophile\" (LIL) metals. Changes in metal ratios were seen through the time of eruption in the plumes of Kilauea and Etna. This may reflect degree of degassing of volatiles, with which metals complex, from the magma bodies. At Kilauea, the changes in fractionation were seen over about three years; fractionation within the alkaline earth family increased, and that between the two families decreased, over that time. All of the ordinarily rare chalcophile metals measured are extremely abundant in volcanic plumes, and Cd and Tl are enriched relative to the others. Indium is much more abundant in the plume of the hotspot volcano Kilauea than in the Etna plume (probably non-hotspot in character). It may be a useful indicator of the tapping of deep mantle zones, or could aid in the interpretation of reports of Pt group metals in exhalations from hot spot volcanoes. Indium in old glacial ice strata could help assess magnitude and variability of exhalations from hotspot volcanoes in past time. Strong melt-vapor fractionation of the alkali and alkaline earth metals may only be observed in plumes during quiescent degassing of volcanoes; when large amounts of ash or spatter (undifferentiated lava) enter the plume, its alkali and alkaline earth metal composition may approach that of the melt. Ratios among the chalcophile metals may not be much changed by addition of ash, because their concentrations in melt are so small, and masses of them in any plume may remain dominated by transfer across the melt-vapor interface. Radon daughter nuclides give information about state of volcanic activity at time of sampling. The precisely known origins, ultratrace detectability, decay systematics, and wide variations in volatility of these species provide information about residence times, degassing and travel histories, and identities of melt bodies in volcanic systems. ?? 1994.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geochimica et Cosmochimica Acta","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/0016-7037(94)90053-1","issn":"00167037","usgsCitation":"Hinkley, T.K., Le Cloarec, M., and Lambert, G., 1994, Fractionation of families of major, minor, and trace metals across the melt-vapor interface in volcanic exhalations: Geochimica et Cosmochimica Acta, v. 58, no. 15, p. 3255-3263, https://doi.org/10.1016/0016-7037(94)90053-1.","productDescription":"9 p.","startPage":"3255","endPage":"3263","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":228524,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"58","issue":"15","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a13a9e4b0c8380cd5471e","contributors":{"authors":[{"text":"Hinkley, T. K. 0000-0001-8507-6271","orcid":"https://orcid.org/0000-0001-8507-6271","contributorId":78731,"corporation":false,"usgs":true,"family":"Hinkley","given":"T.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":377199,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Le Cloarec, M.-F.","contributorId":52348,"corporation":false,"usgs":true,"family":"Le Cloarec","given":"M.-F.","email":"","affiliations":[],"preferred":false,"id":377198,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lambert, G.","contributorId":12994,"corporation":false,"usgs":true,"family":"Lambert","given":"G.","email":"","affiliations":[],"preferred":false,"id":377197,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":17008,"text":"ofr9466 - 1994 - Concentrations of dissolved radon-222 in water from selected wells and springs in Idaho, 1989-91","interactions":[],"lastModifiedDate":"2012-02-02T00:07:00","indexId":"ofr9466","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-66","title":"Concentrations of dissolved radon-222 in water from selected wells and springs in Idaho, 1989-91","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr9466","usgsCitation":"Cecil, L., Parliman, D., Edwards, D., and Young, H., 1994, Concentrations of dissolved radon-222 in water from selected wells and springs in Idaho, 1989-91: U.S. Geological Survey Open-File Report 94-66, iii, 40 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr9466.","productDescription":"iii, 40 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":148146,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0066/report-thumb.jpg"},{"id":46141,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0066/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a5482","contributors":{"authors":[{"text":"Cecil, L.D.","contributorId":62616,"corporation":false,"usgs":true,"family":"Cecil","given":"L.D.","email":"","affiliations":[],"preferred":false,"id":174537,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parliman, D. J.","contributorId":64220,"corporation":false,"usgs":true,"family":"Parliman","given":"D. J.","affiliations":[],"preferred":false,"id":174538,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Edwards, D.D.","contributorId":52980,"corporation":false,"usgs":true,"family":"Edwards","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":174536,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Young, H.W.","contributorId":68278,"corporation":false,"usgs":true,"family":"Young","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":174539,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":18075,"text":"ofr9476 - 1994 - Radionuclides, inorganic constituents, organic compounds, and bacteria in water from selected wells and springs from the southern boundary of the Idaho National Engineering Laboratory to the Hagerman area, Idaho, 1992","interactions":[],"lastModifiedDate":"2012-02-02T00:07:27","indexId":"ofr9476","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-76","title":"Radionuclides, inorganic constituents, organic compounds, and bacteria in water from selected wells and springs from the southern boundary of the Idaho National Engineering Laboratory to the Hagerman area, Idaho, 1992","docAbstract":"Dissolved concentrations of radon-222, a naturally occurring radioactive gas, are found in water in Idaho.  The U.S. Geological Survey collected water samples for radon-222 analyses from 339 Idaho wells and springs during 1989-91.  These water samples were collected as part of ongoing monitoring programs with the Idaho Department of Water Resources and the U.S. Department of Energy. Concentrations of dissolved radon-222 ranged from -58+30 to 5,715+66 picocuries per liter; the mean and median concentrations were 446+35 and 242+25 picocuries per liter, respectively.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr9476","usgsCitation":"Bartholomay, R.C., Edwards, D., and Campbell, L., 1994, Radionuclides, inorganic constituents, organic compounds, and bacteria in water from selected wells and springs from the southern boundary of the Idaho National Engineering Laboratory to the Hagerman area, Idaho, 1992: U.S. Geological Survey Open-File Report 94-76, v, 41 p. :maps ;28 cm., https://doi.org/10.3133/ofr9476.","productDescription":"v, 41 p. :maps ;28 cm.","costCenters":[],"links":[{"id":150600,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0076/report-thumb.jpg"},{"id":47428,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0076/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649aec","contributors":{"authors":[{"text":"Bartholomay, R. C.","contributorId":66271,"corporation":false,"usgs":true,"family":"Bartholomay","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":178498,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Edwards, D.D.","contributorId":52980,"corporation":false,"usgs":true,"family":"Edwards","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":178496,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Campbell, L.J.","contributorId":59820,"corporation":false,"usgs":true,"family":"Campbell","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":178497,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":17163,"text":"ofr93292F - 1993 - Geologic radon potential of EPA Region 6; Arkansas, Louisiana, New Mexico, Oklahoma, and Texas","interactions":[{"subject":{"id":17163,"text":"ofr93292F - 1993 - Geologic radon potential of EPA Region 6; Arkansas, Louisiana, New Mexico, Oklahoma, and Texas","indexId":"ofr93292F","publicationYear":"1993","noYear":false,"chapter":"F","title":"Geologic radon potential of EPA Region 6; Arkansas, Louisiana, New Mexico, Oklahoma, and Texas"},"predicate":"IS_PART_OF","object":{"id":70262885,"text":"ofr93292 - 1993 - Geologic radon potential of the United States","indexId":"ofr93292","publicationYear":"1993","noYear":false,"title":"Geologic radon potential of the United States"},"id":1}],"isPartOf":{"id":70262885,"text":"ofr93292 - 1993 - Geologic radon potential of the United States","indexId":"ofr93292","publicationYear":"1993","noYear":false,"title":"Geologic radon potential of the United 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,{"id":27683,"text":"wri924092 - 1993 - Geochemistry of and radioactivity in ground water of the Highland Rim and Central Basin aquifer systems, Hickman and Maury counties, Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:08:43","indexId":"wri924092","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"92-4092","title":"Geochemistry of and radioactivity in ground water of the Highland Rim and Central Basin aquifer systems, Hickman and Maury counties, Tennessee","docAbstract":"A reconnaissance of the geochemistry of and radioactivity in ground water from the Highland Rim and Central Basin aquifer systems in Hickman and Maury Counties, Tennessee, was conducted in 1989. Water in both aquifer systems typically is of the calcium or calcium magnesium bicarbonate type, but concentrations of calcium, magnesium, sodium, potassium, chloride, and sulfate are greater in water of the Central Basin system; differences in the concentrations are statistically significant. Dissolution of calcite, magnesium-calcite, dolomite, and gypsum are the primary geochemical processes controlling ground-water chemistry in both aquifer systems. Saturation-state calculations using the computer code WATEQF indicated that ground water from the Central Basin system is more saturated with respect to calcite, dolomite, and gypsum than water from the Highland Rim system. Geochemical environments within each aquifer system are somewhat different with respect to dissolution of magnesium-bearing minerals. Water samples from the Highland Rim system had a fairly constant calcium to magnesium molar ratio, implying congruent dissolution of magnesium-bearing minerals, whereas water samples from the Central Basin system had highly variable ratios, implying either incongruent dissolution or heterogeneity in soluble constituents of the aquifer matrix.\r\n\r\nConcentrations of radionuclides in water were low and not greatly different between aquifer systems. Median gross alpha activities were 0.54 picocuries per liter in water from each system; median gross beta activities were 1.1 and 2.3 picocuries per liter in water from the Highland Rim and Central Basin systems, respectively. Radon-222 concentrations were 559 and 422 picocuries per liter, respectively. Concentrations of gross alpha and radium in all samples were substantially less than Tennessee?s maximum permissible levels for community water-supply systems. The data indicated no relations between concentrations of dissolved radionuclides (uranium, radium-226, radium-228, radon-222, gross alpha, and gross beta) and any key indicators of water chemistry, except in water from the Highland Rim system, in which radon-222 was moderately related to pH and weakly related to dissolved magnesium. The only relation among radiochemical constituents indicated by the data was between radium-226 and gross alpha activity; this relation was indicated for water from both aquifer systems.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri924092","usgsCitation":"Hileman, G.E., and Lee, R.W., 1993, Geochemistry of and radioactivity in ground water of the Highland Rim and Central Basin aquifer systems, Hickman and Maury counties, Tennessee: U.S. Geological Survey Water-Resources Investigations Report 92-4092, v, 26 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri924092.","productDescription":"v, 26 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":2210,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri924092/","linkFileType":{"id":5,"text":"html"}},{"id":124659,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_92_4092.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ee4b07f02db6aa6de","contributors":{"authors":[{"text":"Hileman, G. E.","contributorId":11639,"corporation":false,"usgs":true,"family":"Hileman","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":198531,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, R. W.","contributorId":86757,"corporation":false,"usgs":true,"family":"Lee","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":198532,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38146,"text":"ofr93292G - 1993 - Geologic radon potential of EPA Region 7: Iowa, Kansas, Missouri, and Nebraska","interactions":[{"subject":{"id":38146,"text":"ofr93292G - 1993 - Geologic radon potential of EPA Region 7: Iowa, Kansas, Missouri, and Nebraska","indexId":"ofr93292G","publicationYear":"1993","noYear":false,"chapter":"G","title":"Geologic radon potential of EPA Region 7: Iowa, Kansas, Missouri, and Nebraska"},"predicate":"IS_PART_OF","object":{"id":70262885,"text":"ofr93292 - 1993 - Geologic radon potential of the United States","indexId":"ofr93292","publicationYear":"1993","noYear":false,"title":"Geologic radon potential of the United States"},"id":1}],"isPartOf":{"id":70262885,"text":"ofr93292 - 1993 - Geologic radon potential of the United States","indexId":"ofr93292","publicationYear":"1993","noYear":false,"title":"Geologic radon potential of the United States"},"lastModifiedDate":"2025-06-25T20:17:04.665154","indexId":"ofr93292G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"93-292","chapter":"G","title":"Geologic radon potential of EPA Region 7: Iowa, Kansas, Missouri, and Nebraska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr93292G","usgsCitation":"1993, Geologic radon potential of EPA Region 7: Iowa, Kansas, Missouri, and Nebraska: U.S. Geological Survey Open-File Report 93-292, ii, 147 p., https://doi.org/10.3133/ofr93292G.","productDescription":"ii, 147 p.","costCenters":[],"links":[{"id":491342,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12705.htm","text":"Nebraska","linkFileType":{"id":5,"text":"html"}},{"id":491341,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12704.htm","text":"Missouri","linkFileType":{"id":5,"text":"html"}},{"id":491340,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12703.htm","text":"Kansas","linkFileType":{"id":5,"text":"html"}},{"id":64407,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0292g/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":403007,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12702.htm","text":"Iowa","linkFileType":{"id":5,"text":"html"}},{"id":162555,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0292g/report-thumb.jpg"}],"country":"United States","state":"Iowa, Kansas, Missouri, 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,{"id":20269,"text":"ofr93443 - 1993 - Well-construction, water-level, and ground-water-quality data for Prince William County, Virginia, 1992","interactions":[],"lastModifiedDate":"2012-02-02T00:07:40","indexId":"ofr93443","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"93-443","title":"Well-construction, water-level, and ground-water-quality data for Prince William County, Virginia, 1992","docAbstract":"Well-construction, water-level, and ground-water- quality data were collected by the U.S. Geological Survey during 1989-92 in Prince William County, Virginia. The data are presented on a map, in tables, and in hydrographs to record ambient ground-water quality. Well construction data include descriptions of 182 well sites. Water-level data include measurements from 159 wells that were collected in the spring and fall of 1991 and hydrographs from six of the wells. Ground-water- quality data collected at 87 wells include analyses for major dissolved constituents, trace metals, nutrients, dissolved organic carbon, radon-222, and alkalinity. Environmental or stable isotope analyses were collected at 57 wells and dissolved gas analyses were collected at 18 wells. Field proper- ties were also recorded during sampling.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center [distributor],","doi":"10.3133/ofr93443","usgsCitation":"Nelms, D., and Brockman, A.R., 1993, Well-construction, water-level, and ground-water-quality data for Prince William County, Virginia, 1992: U.S. Geological Survey Open-File Report 93-443, iii, 66 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr93443.","productDescription":"iii, 66 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":152285,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0443/report-thumb.jpg"},{"id":49804,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1993/0443/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49805,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0443/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4acb","contributors":{"authors":[{"text":"Nelms, D.L.","contributorId":32189,"corporation":false,"usgs":true,"family":"Nelms","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":182358,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brockman, A. R.","contributorId":49388,"corporation":false,"usgs":true,"family":"Brockman","given":"A.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":182359,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":18487,"text":"ofr9364 - 1993 - Radon in ground water of western Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:07:32","indexId":"ofr9364","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1993","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":"93-64","title":"Radon in ground water of western Montana","language":"ENGLISH","publisher":"U.S. Geological Survey, Dept. of the Interior,","doi":"10.3133/ofr9364","usgsCitation":"Clark, D.W., and Briar, D., 1993, Radon in ground water of western Montana: U.S. Geological Survey Open-File Report 93-64, 2 p. :ill. ;28 cm., https://doi.org/10.3133/ofr9364.","productDescription":"2 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":151433,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0064/report-thumb.jpg"},{"id":47841,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0064/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649a6f","contributors":{"authors":[{"text":"Clark, David W.","contributorId":77146,"corporation":false,"usgs":true,"family":"Clark","given":"David","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":179219,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Briar, D.W.","contributorId":58287,"corporation":false,"usgs":true,"family":"Briar","given":"D.W.","affiliations":[],"preferred":false,"id":179218,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":17164,"text":"ofr93292H - 1993 - Geologic radon potential of EPA Region 8: Colorado, Montana, North Dakota, South Dakota, Utah, and Wyoming","interactions":[{"subject":{"id":17164,"text":"ofr93292H - 1993 - Geologic radon potential of EPA Region 8: Colorado, Montana, North Dakota, South Dakota, Utah, and Wyoming","indexId":"ofr93292H","publicationYear":"1993","noYear":false,"chapter":"H","title":"Geologic radon potential of EPA Region 8: Colorado, Montana, North Dakota, South Dakota, Utah, and Wyoming"},"predicate":"IS_PART_OF","object":{"id":70262885,"text":"ofr93292 - 1993 - Geologic radon potential of the United States","indexId":"ofr93292","publicationYear":"1993","noYear":false,"title":"Geologic radon potential of the United States"},"id":1}],"isPartOf":{"id":70262885,"text":"ofr93292 - 1993 - Geologic radon potential of the United States","indexId":"ofr93292","publicationYear":"1993","noYear":false,"title":"Geologic radon potential of the United 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