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A new 14 Å mineral of the birnessite group in deep-sea micronodules

Abstract

EXPERIMENTS by Feitknecht and Marti1 and more recently by Giovanoli et al. have shown that oxidation of Mn(OH)2 in NaOH solution gives rise to a Na-buserite. Drying Na-buserite converts it to Na-birnessite. If a solution of a calcium salt is shaken with Na-buserite the latter is transformed into pseudo-hexagonal Ca-buserite, characterised by a basal spacing of 10 Å. After drying this spacing is reduced up to 7 Å and buserite is converted into Ca-birnessite. We describe here a new natural Ca-bearing member of the birnessite group of unit cell parameters comparable with those of a synthetic compound described2 as Na–-Mn (p, m) manganate, belonging to the birnessite group. In ASTM (23–1046) this substance is called Na-birnessite.

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References

  1. Feitknecht, W. & Marti, W. Helv. chim. Acta 28, 129–156 (1945).

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  2. Giovanoli, R., Stähli, E. & Feitknecht, W. Helv. Chim. Acta, 53, 209–220 (1970); 53, 453–464 (1970).

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  3. Bardossy, G. & Brindley, G. Am. Miner. 63, 762–767 (1978).

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  4. Giovanoli, R., Bürki, P., Guiffredi, M. & Stumm, W. Chimia 29, 517–520 (1975).

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CHUKHROV, F., GORSHKOV, A., SIVTSOV, A. et al. A new 14 Å mineral of the birnessite group in deep-sea micronodules. Nature 280, 136–137 (1979). https://doi.org/10.1038/280136a0

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  • DOI: https://doi.org/10.1038/280136a0

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