Read e-book online Handbook of Lithium and Natural Calcium Chloride. Their PDF

By Donald E. Garrett (Auth.)

This ebook is worried with significant business minerals: Lithium and Calcium Chloride. The geology in their deposits is first reviewed, in addition to discussions of many of the significant deposits and theories in their starting place. the industrial mining and processing crops are subsequent defined, via a evaluate of the fairly broad literature on different proposed processing equipment. The extra very important makes use of for lithium and calcium chloride are subsequent coated, in addition to their environmental concerns. this is often through a short evaluate of the construction data for every undefined, and a few in their compounds' section info and actual houses.

- Describes the chemistry, chemical engineering, geology and mineral processing facets of lithium and calcium chloride
- Collects in a single resource crucial details pertaining to those commercial minerals
- offers new innovations and extra accomplished theories on their foundation

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Extra info for Handbook of Lithium and Natural Calcium Chloride. Their Deposits, Processing, Uses and Properties

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The origin of the Salton Sea geothermal brine is believed to be meteoric water (based upon dD and d18O values) from the nearby Chocolate Mountains flowing through fault lines deep into the earth, where it is heated by hot rocks or magma. The brine composition might indicate that the descending water dissolved highmagnesium potash salts that had been formed in this former seawater estuary area (from the present Sea of Cortez [Gulf of Baja California]). Then this brine underwent the very common dolomitization reaction (see Chapter 2) by reacting with calcite and converting most of its calcium content to magnesium.

68 Na K Mg Ca Da Qaidam Intercryst. 16 Mahai Intercryst. 0021. 23 Several of the high-lithium Chinese Lakes, and their surface composition (Dapeng and Bingxiao, 1993; reprinted from the Seventh Symposium on Salt [ISBN 0444891439], Vol. 2, p. 179, Fig. 1, q 1993, with permission from Elsevier). 12% CO3, 948 HCO3 and 113 F. The age of the lakes is estimated to be 5600– 20,000 years. Several of these lakes are quite large, and the Qinghai playa was being prepared for commercial potash production in 2001, with its 8– 13 ppm Li brine to be sent to solar evaporation ponds.

12). , 1999). 11). There are other potential high-lithium brine sources that were initially mediumlithium brines extensively evaporated to recover other minerals (such as at the Great Salt Lake, Bonneville Salt Flats, the Dead Sea and the Qinghai playa noted above). The Sua Pan in Botswana (Fig. 9), and it is evaporated in solar ponds to produce soda ash. 2)k þ 16l d Li ¼ 1000 ([7Li/6Li]sample/[7Li/6Li]standard 2 1), while d6Li has the 6Li and 7Li reversed. 081315. 0, making the two values of opposite sign and somewhat different.

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