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- W83045504 abstract "Abstract Palygorskite was the dominant clay mineral in some Ground-water rendzinas developed on Pleistocene interdunal flats in the south-east of South Australia. The clay fraction from one soil contained 9.2% MgO and palygorskite was identified by a prominent 10.5 A X-ray diffraction spacing for the c-axis and by fine rod-like morphology. The clay had a high charge and surface area and was strongly associated with organic matter. It is concluded that the palygorskite developed in situ along with smectite in an environment subject to prolonged seasonal inundation by surface waters and groundwaters containing substantial quantities of salts including Ca and Mg." @default.
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- W83045504 date "1984-01-01" @default.
- W83045504 modified "2023-09-25" @default.
- W83045504 title "Occurrence of Palygorskite in Ground-Water Rendzinas (Petrocalcic Calciaquolls) in South-East South Australia" @default.
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- W83045504 doi "https://doi.org/10.1016/s0070-4571(08)70039-6" @default.
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