黏土矿物对金盆水库软弱变质岩边坡失稳影响研究
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大连海事大学青年教师科研基金资助项目(DLMU-ZL-200809);辽宁省重点学科资助计划(363063)


Influence of Clay Minerals on Instability of Soft Metamorphic Rock Slope in Jinpen Reservoir
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    摘要:

    针对西安市金盆水库软弱变质岩边坡的地质条件, 在细致分析黏土矿物的主要特性及形成机制的基础上, 从微观到宏观的不同尺度, 系统研究了黏土矿物对软弱变质岩边坡失稳的影响。 结果表明, 软弱变质岩成因复杂, 矿物成分多样, 水稳定性差, 易于生成黏土矿物; 而次生黏土矿物的形成将引起源矿物、矿物集合体及岩块特性的显著变化, 诱发岩石向松散介质转化, 并触发黏土矿物在宏观结构面中的聚集和泥化夹层的形成, 导致结构面及岩体强度衰减, 进而促进边坡变形破坏, 对边坡演化及失稳的贡献显著。

    Abstract:

    In view of the geological condition of soft metamorphic rock slope in Jinpen Reservoir, the influence of clay minerals on soft metamorphic rock slope is systemat ically studied through a careful analysis of the main properties and formation mechanisms of clay minerals, from micro to macro levels. Results show that soft metamorphic rock can easily produce clay minerals because of such characteristics as complex origin, various mineral composition, and weak water stability. However, clay minerals in rock may bring about marked changes in some properties of parent minerals, mineral aggregation or rock and promote rock to evolve toward loose medium. Moreover, the illuviation of clay minerals in macro discontinuities and the formation of mudded intercalation will cause the strength of discont inuities and rock mass to decrease. To sum up, clay minerals may accelerate deformation of slopes and their contribution to slope evolution and failure is notable.

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于德海,彭建兵.黏土矿物对金盆水库软弱变质岩边坡失稳影响研究[J].水土保持通报,2009,(5):45-49

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  • 收稿日期:2008-12-24
  • 最后修改日期:2009-05-05
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  • 在线发布日期: 2014-11-26
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