Colorado Nahcolite Deposits: Geology And Outlook For Development

- Organization:
- Society for Mining, Metallurgy & Exploration
- Pages:
- 12
- File Size:
- 1159 KB
- Publication Date:
- Jan 1, 1980
Abstract
Colorado nahcolite deposits, estimated at 29 billion metric tons, formed in an asp metric permanent-lake basin whose waters were rich in algae and sulfate-reducing bacteria. Nahcolite (NaHCOg) occurs in oil shale of the Green River Formation (Eocene) as aggregates (62 percent), disseminated crystals (24 percent), and impure beds (14 percent). Because much of the nahcolite is nonbedded, it will be mined with oil shale and can be concentrated to marketable grade by crushing and screening Impurities in nahcolite are kerogen, quartz, pyrite, and carbonate minerals. A promising new market for nahcolite is in the process of removal of sulfur dioxide from industrial stack gases. When heated, nahcolite reacts with sulfur dioxide to form sodium sulfate. Differences in thermally induced microporosity may explain why nahcolite is more reactive than trona, a possible competitor with nahcolite for SO2 removal. Limited production of nahcolite at one or possibly two localities is expected in the next several years, but large-scale production is probably at least 10 years away.
Citation
APA:
(1980) Colorado Nahcolite Deposits: Geology And Outlook For DevelopmentMLA: Colorado Nahcolite Deposits: Geology And Outlook For Development. Society for Mining, Metallurgy & Exploration, 1980.