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- W2244128051 abstract "Regularly interstratified chlorite-vermiculite (1:1) is found as a weathering product of chlorite in a Highfield channery silt loam soil profile in Adams County, Pennsylvania. The parent rock is greenstone, a metamorphosed basalt, composed of chlorite, epidote, alibite and ilmenite. Greenstone fragments in the soil are found with different degrees of chlorite alteration to chlorite-vermiculite. Most prominant development is in the fine silt separate of the soil. X-ray examination revealed that d(001)=28.5 A for magnesium saturated, air dry material; d(001)=28.5 A for magnesium saturated, ethylene glycol solvated material; and d(001)=24.3 A for potassium saturated, air dry material. Cation exchange capacity is estimated to be 85 me/100 grams. It is suggested that the parent chlorite is a 2-layer polytype with different degrees of bonding of alternate brucite interlayers. When subjected to a leaching environment, the more weakly bonded interlayers are preferentially removed." @default.
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- W2244128051 date "1964-06-01" @default.
- W2244128051 modified "2023-09-23" @default.
- W2244128051 title "Occurrence of regularly interstratified chlorite-vermiculite as a weathering product of chlorite in a soil" @default.
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