Cation exchange with Mn
2+, Fe
+2, Co
+2 and Ni
2+ was carried out for synthetic swelling sodium-flourine micas having variable layer charges [Na
xMg
3-xLi
x(Si
4O
10)F
2, x =1.00, 0.76, 0.61, 0.42] and swelling-dehydration characteristics of M
2+-exchanged micas were investiga ted. The swelling characteristics of exchanged micas depend mainly on interlayer M
2+ cations and slightly on layer charge. According to the observed basal spacings (d
001) the stable phase of M
2+-exchanged micas in air (temp=20°C, R. H. =60%) was two-layer hydrated type (d
001≈14.6 Å), while that in water was three-layer hydrated type (d
001≈18.4 A). The b asal spacings of the two-layer hydrated type of M2
+-exchanged micas decreased in three steps with increasing temperature, and thee endothermic peaks appeared on DTA curves, indicating the dehydration of the micas. At the highest one of the endothermic peak temperatures (Th) dehydration of one-layer hydrated micas occurred. Then the temperature of Th was regarded as a parameter representing dehydration tendency of interlayer water molecules. In the case of the micas having the same layer charge, the temperature of Th increased in the order Mn2
+- <Fe
2+ -<CCo2
+- <Ni
2+- exchanged mica, and this order is the same as that of hydration energy of M2+. For M
2+- exchanged micas having the same species of interlayer cation, the Th increased with decreasing layer charge. These facts suggest that the dehydration characteristics of M
2+-exchanged micas can be explained in terms of the nature of M
2+cations and the effects of layer charge on the bond between M2+ and H
2O.
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