Consideration from Weathering Characteristics of Serpentine on Landslide in Serpetine Belt

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  • 蛇紋岩地すべりの素因としての蛇紋岩の風化特性に関する検討
  • ジャモンガン ヂスベリ ノ ソイン ト シテ ノ ジャモンガン ノ フウカ トクセイ ニ カンスル ケントウ

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Abstract

Many landslides have been occurred in the serpentine belt. It was seemed that the ease of the chemical weathering of serpentine were one of the reason. The chemical weathring characteristics were investigated. The perticles of serpentine were soaked in the carbonated water. The change of pH, clay minerals, cations in the eluate, elements, perticle size and shearing characteristics were obtained. It were clear that much Mg ion flowed out and the angle of shear resistance droped about 10° for three months.

Journal

  • Landslides

    Landslides 36 (2), 32-38_1, 1999

    The Japan Landslide Society

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