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- W2317682017 abstract "Chemical and mineralogical data on Holocene coastal plain soils from Thailand suggest that during formation of pyrite in tidal swamps Fe(III) is extracted from smectite and replaced by Mg. During drainage of these sediments pyrite oxidizes and the reaction is reversed. Replacing Fe(III) by Mg in clay minerals stores alkalinity that can neutralize three-quarters of the acidity released during oxidation of pyrite, and thus lowers the potential acidity of pyritic sediments. Possible causes for variation in the amounts of Mg taken up during pyrite formation are discussed." @default.
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- W2317682017 date "1980-01-01" @default.
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- W2317682017 title "IRON REPLACEMENT IN SMECTITE DURING A ERATION OF PYRITIC SEDIMENTS" @default.
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