Skip to main content
  • Article
  • Published:

Relationship in chemical composition between mother solution and allophane-like aluminosilicate precipitate through neutralization of acid hydrothermal water by seawater

Abstract

A series of experiments on the formation of allophane-like aluminosilicate precipitates were carried out through neutralization of acid solutions in variety of relative proportions of Si, Fe and Al by seawater. The retrieval and decomposition procedures were available for precise determination of those components in the precipitates. Iron in the mother solutions was completely precipitated and Al was mostly precipitated, however, Si was partly co-precipitated with iron and aluminum. Iron and/or Al coexisting with Si caused a remarkable rise of the precipitated proportion of Si. This was ascribed to co-precipitation of these components on the formation of the precipitates. Difference in effect on the precipitated proportion of Si between Fe and Al was not noticeable. This result indicated equivalence of Fe to Al on the formation of the precipitates through neutralization. The correlations in the (Fe + Al)/Si and the Fe/Al molar ratios between the mother solution and the precipitates strongly designated that the relative proportions of Si, Fe and Al in hydrothermal water discharged from submarine volcanoes were able to be determined uniquely through chemical analysis of the precipitates causing discolored seawater.

References

  • Ichikuni, M., Incorporation of aluminum and iron into siliceous sinters, Chemical Geology, 6, 273–279, 1970.

    Article  Google Scholar 

  • Kamada, M., J. Ossaka, and T. Ozawa, Hydro-alumina-silicate generating from acidic hot spring water along the seashore of Iwojima volcano, Abstract of the Geochemical Sco. Japan, 158–161, 1964 (in Japanese).

    Google Scholar 

  • Nogami, K., M. Yoshida, and J. Ossaka, Chemical composition of discolored seawater around Satsuma-Iwojima, Kagoshima, Japan, Bull. Vol-canol. Soc. Japan, 38, 71–77, 1993.

    Google Scholar 

  • Ossaka, J., The eruption of Nishinosima submarine volcano and geochemi-cal study on the composition of the ejecta and the volcanic activity, Chemistry Today (Gendai Kagaku), 55, 12–20, 1975 (in Japanese).

    Google Scholar 

  • Ossaka, J., Y. Ohira, J. Hirabayashi, and A. Mori, Comparison of amorphous hydro-alumina-silicate, formed in sea water with precipitated allophane, Jour. Min. Soc. Japan, 13, 178–186, 1977 (in Japanese).

    Google Scholar 

  • Ossaka, J., J. Hirabayashi, K. Nogami, M. Tsuchide, and N. Adachi, Chemical composition of discolored seawater corresponding to activity of Fukutoku-Oka-no-Ba submarine volcano—as an index of submarine volcanism—, Bull. Volcanol. Soc. Japan, 41, 107–113, 1996 (in Japanese).

    Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Kenji Nogami.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Nogami, K. Relationship in chemical composition between mother solution and allophane-like aluminosilicate precipitate through neutralization of acid hydrothermal water by seawater. Earth Planet Sp 56, 457–462 (2004). https://doi.org/10.1186/BF03352498

Download citation

  • Received:

  • Revised:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1186/BF03352498

Key words