No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6498","usgsCitation":"King, R.H., 1964, Report on three dolomite deposits near Helena, Montana: U.S. Geological Survey Open-File Report 64-98, 32 p., https://doi.org/10.3133/ofr6498.","productDescription":"32 p.","costCenters":[],"links":[{"id":490341,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1964/0098/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151546,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1964/0098/report-thumb.jpg"}],"country":"United States","state":"Montana","city":"Helena","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"id\":\"29\",\"properties\":{\"name\":\"Montana\",\"nation\":\"USA 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The concentration of radium-226 in potable water is of particular significance because this isotope is generally considered the most hazardous of all radionuclides with respect to ingestion. \r\n\r\nThe approximate concentration of radium-226 is determined after coprecipitating radium with barium sulfate. The short-lived daughters of radium are allowed to grow for 10-12 days, then the alpha activity of the precipitate is measured and compared with that of a precipitate containing a known amount of radium-226. Concentrations of the individual alpha-emitting isotopes of radium-223, radium-224, and radium-226, are determined by coprecipitating radium first with lead sulfate, then with barium chloride, and finally with barium sulfate. 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