ISSN 1000-3665 CN 11-2202/P

    金沙江上江坝址河床粘土层特性及工程意义

    Properties and engineering significance of the river bed clay layer in Shangjiang dam of the Jinsha River

    • 摘要: 金沙江中游上江坝址河床覆盖层中分布因下游堰塞坝堵江而形成的湖相低液限粘土层,埋深49.7~79.6m,厚度9.3~24.0m,左岸厚右岸薄,分布连续稳定,该层多呈可塑状,具强度较低、透水性微弱等特点,为坝基的一条相对软弱带。坝址河床覆盖层深厚,最大厚度206.2m,除分布低液限粘土层外,还分布有漂卵石、砾卵石、碎块石、砂砾石等强度相对较高的物质成份。坝址初拟布置心墙堆石坝,以覆盖层为基础持力层,大坝建基面的选择与粘土层关系密切,本文通过对河床低液限粘土的空间分布、成因、工程特性进行阐述分析,研究了坝基低液限粘土利用与否的筑坝技术难点,经过初步论证大坝利用粘土层浅层清基的筑坝方案要相对经济、合理。

       

      Abstract: Lacustrine low liquid limit clay layer,formed by downstream dammed lake,distributes in overburden layer of Shangjiang dam on the middle reaches of the Jinsha River,which is a relatively weak area of the dam foundation with the characters of the depth of 49.7~79.6m,the thickness of 9.3~24.0m,thick on the left bank and thin on the right bank,continuous distribution,high plasticity,low strength and water permeability.The river bed overburden layer is deep in the dam site,with the depth of 206.2m,where distribute low liquid limit clay layer but also drift gravel,boulders and gravel,stone fragments,gravel and so on,which have relatively high strength.It is planed to set core rockfill dam at the beginning in order to take the overburden layer as the bearing layer.For the choice of dam site is in close relations to the clay layer,the paper analyses on the spatial distribution,cause of formation and engineering properties of the bed low liquid limit clay,and studies on the dam technical problems of using the clay layer or not,finally proposes the economic and reasonable program of using the shallow layer of clay as the dam foundation.

       

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