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粘土鉱物学の基礎 (2 ... - sci.kagoshima-u.ac.jp

(2) . 1 .. 2 X . X .. 2 3 .. (Pauling's Rules ). 1st Rule The cation-anion distance = radii Can use RC/RA to determine the coordination number of the cation This is an important rule to constract crystal structure of clay minerals .. Si-O (SiO4) Al-O (AlO6) or Mg-O (MgO6). - (Si4O10 / ) - (Al4O12 or Mg6O12/ ).. A) B) . d (001). d (001). d (001) = . d (001) = .. Pyrophyllite Al2Si4O10(OH) 2. Mica KAl2( Si3Al)O10(OH) 2. Smectite (Al2)( )O10(OH) 2. Vermiculite (Mg3)( )O10(OH) 2. Chlorite (Mg,Al)6(Si,Al)4O10(OH) 8. Kaolinite Al2Si2O5(OH) 4.

粘土鉱物学の基礎 (2):粘土鉱物の構造 1)粘土鉱物の構造と分類 ポーリングの原理と配位数 構造単位と基本構造 層電荷と分類基準 混合層鉱物 非晶質鉱物 2)粘土鉱物のx線回折

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