Illite equilibria in solutions: 2. Phase relationships in the system K sub 2 O-MgO-Al sub 2 O sub 3 -SiO sub 2 -H sub 2 O
- Washington State Univ., Pullman (United States)
The stability of the Marblehead illite has been investigated in the five-component system K{sub 2}O-MgO-Al{sub 2}O{sub 3}-SiO{sub 2}-H{sub 2}O in the presence of kaolinite and microcline. The mica-like solubility-controlling phases (K{sub x}(Mg{sub y}Al{sub 2{minus}y})(Al{sub x{minus}y}Si{sub 4{minus}(x{minus}y)}) O{sub 10}(OH){sub 2}) identified include (1) smectite x = 0.29 {plus minus} 0.04, y = 0.26 {plus minus} 0.02; (2) illite x = 0.50 {plus minus} 0.05, y = 0.22 {plus minus} 0.14; (3) illite x = 0.69 {plus minus} 0.08, y = 0.16 {plus minus} 0.03; (4) illite x = 0.85 {plus minus} 0.05, y = 0.12 {plus minus} 0.04; and (5) muscovite. Possible stability regions have been defined for these solubility-controlling phases using isothermal isobaric log a{sub Mg{sup +2}}{sup {1/2}}/a{sub H{sup +}} vs. log a{sub K{sup +}}/a{sub H{sup +}} diagrams. When illite stability is referred to the quaternary system K{sub 2}O-Al{sub 2}O{sub 3}-SiO{sub 2}-H{sub 2}O, the effect of (R{sup +2}){sup VI} substitution is neglected. The error inherent in this simplification has been estimated. Inasmuch as a four-fold increase in a{sub Mg{sup 2+}} shifts the illite-smectite-kaolinite-solution invariant point by less than 0.3 log units, stability relationships in the quaternary system provide an adequate representation of illite solution equilibria, to a first approximation, However, the error caused by neglecting Mg{sup 2+} is close to or within experimental error. Thus, a more precise determination of the effect of Mg{sup +2} on illite solution equilibria may not be possible using the solution equilibration method.
- OSTI ID:
- 6140309
- Journal Information:
- Geochimica et Cosmochimica Acta; (United States), Vol. 55:5; ISSN 0016-7037
- Country of Publication:
- United States
- Language:
- English
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ILLITE
SOLUBILITY
STABILITY
THERMODYNAMIC PROPERTIES
AQUEOUS SOLUTIONS
EQUILIBRIUM
GEOCHEMISTRY
KAOLINITE
PHASE STUDIES
SMECTITE
STOICHIOMETRY
TEMPERATURE EFFECTS
WISCONSIN
ALUMINIUM COMPOUNDS
ALUMINIUM SILICATES
CHEMISTRY
CLAYS
DEVELOPED COUNTRIES
DISPERSIONS
FEDERAL REGION V
MINERALS
MIXTURES
NORTH AMERICA
OXYGEN COMPOUNDS
PHYSICAL PROPERTIES
SILICATE MINERALS
SILICATES
SILICON COMPOUNDS
SOLUTIONS
USA
580000* - Geosciences