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- W2018802948 abstract "Massive, but very localized, iron formations have been noted in some Humic Gleysols in southern Ontario. Some of these formations weigh up to 9 kg, and invariably occur at the contact zone between sandy loam to loam surface horizons and underlying clay-rich subsoils. The contents of Fe 2 O 3 and MnO 2 of 16 samples varied from 19.6 to 49.9% and 0.8 to 11.1%, respectively, although no crystalline oxides or hydroxides of Fe or Mn could be detected by X-ray diffraction. The localized occurence of these formations suggests that Fe 2+ and Mn 2+ are moving laterally through the subsoil and oxidizing at some seepage point downslope in the more aerated surface horizons." @default.
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- W2018802948 date "1978-08-01" @default.
- W2018802948 modified "2023-09-25" @default.
- W2018802948 title "MASSIVE IRON FORMATIONS IN SOME GLEYSOLIC SOILS OF SOUTHWESTERN ONTARIO" @default.
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- W2018802948 doi "https://doi.org/10.4141/cjss78-046" @default.
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