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Lithium natural, deposit

L. B. Sand As mentioned in the text, these lithium-containing synthetic zeolites do not occur in nature, so experimental data do not apply to the problem of genesis. The synthesis of Na-mordenite at low temperature (75°C) could be of some significance, but a great deal of experimental data are required to apply to the interpretation the conditions for formation in a natural deposit. [Pg.140]

Lithium-ion batteries high energy density purified natural graphite carbon coated silicon graphite/metal composites chemical vapor deposition. [Pg.330]

The cycling improvement for the Cu-metallized graphite over the pristine graphite was also observed by K. Guo et al. [15] in their study of electroless Cu deposited on graphite cycled in a lithium cell with a 20% PC blend electrolyte. Also, they recorded a rate capability improvement in their Cu graphite material as well. At a current density of 1.4 mA/cm2, the cell achieved about 60% ( 200 mAh/g) of the charge capacity measured at 0.14 mA/cm2, compared to about 30% ( 100 mAh/g) for the non-treated pristine natural graphite cell [15]. [Pg.381]

This allows metal dissolution-deposition processes to occur at a relatively low overpotential. A typical example for such behavior is lithium in many polar aprotic systems. The nature of the surface films in these cases determines the following possibilities ... [Pg.301]

Like the other alkali metals, cesium is a soft, silvery metal, but it appears golden if it has been exposed to small amounts of oxygen. It is not found in its metallic state in nature it is obtained as a byproduct of lithium processing of the mineral lepidolite. Its most significant ore is pollucite, and the world s largest pollucite deposit is found in Bernic Lake, Manitoba, Canada. Cesium s average crustal abundance is about 3 parts per million. Cesium is the most electropositive stable element and will ignite if exposed to air. Cesium burns blue in the flame test. [Pg.216]


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Lithium natural

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