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- W2091943145 abstract "Vertical profiles of manganese concentration in interstitial waters and of manganese and iron contents in five chemically-separated fractions of sediments have been studied in a sediment core (73 cm long) from a meromictic lake, Lake Suigetsu, which changed from freshwater to brackish conditions in 1664 A.D. The interstitial waters show a minimum manganese concentration of 0.13 ppm near a depth of 10 cm and a maximum of 26 ppm near 65 cm in the core. A predominant amount of manganese, up to 0.17%, is found in the hydrogen peroxide-soluble fraction of sediments in layers above a depth of 52 cm. It is suggested that the manganese is included in stable iron sulfides such as pyrite. Manganese, which diffuses upward from the lower layer, is thought to be deposited along with stable iron sulfide during diagenetic formation of the latter near a depth of 10 cm in the core." @default.
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- W2091943145 date "1982-05-01" @default.
- W2091943145 modified "2023-10-17" @default.
- W2091943145 title "Diagenetic deposition of manganese in sediment of a historically meromictic lake, Lake Suigetsu, Japan" @default.
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- W2091943145 doi "https://doi.org/10.1007/bf02110293" @default.
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