Studies of mechanism for transition zone to control seepage field in concrete faced rockfill dam
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Studies of mechanism for transition zone to control seepage field in concrete faced rockfill dam
Vol. 32, Issue 12, (2011)
作者机构:
长江科学院 水利部岩土力学与工程重点实验室 国家大坝安全工程技术研究中心,武汉,430010
作者简介:
基金信息:
DOI:
CLC:TV641.4
Online First:13 December 2011,
Published:2011
稿件说明:
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ZHANG Jia-fa, DING Pei-zhong, ZHANG Wei, et al. Studies of mechanism for transition zone to control seepage field in concrete faced rockfill dam[J]. 2011, 32(12).
DOI:
ZHANG Jia-fa, DING Pei-zhong, ZHANG Wei, et al. Studies of mechanism for transition zone to control seepage field in concrete faced rockfill dam[J]. 2011, 32(12).DOI:
Studies of mechanism for transition zone to control seepage field in concrete faced rockfill dam
the seepage stability of the dam is satisfied; while the concrete face cracks locally or does not work properly
it is pivotal for the transition zone to control seepage field in the dam and to keep seepage stability. Taking the concrete faced rockfill dam of Shuibuya Hydropower Station for example
the coefficient between cushion layer and transition zone is analyzed; it is indicated that tests are necessary to study filtering and protection of transition zone for cushion layer. Tests are performed with cushion layer and transition zone material of whole size gradation; and the seepage deformation and filtering effect is studied. Synthesizing the test results and the results in author’s papers published already
the mechanism for the transition zone to control the seepage field in superhigh concrete faced rockfill dam is concluded. The transition zone
together with the main rockfill zone
could drain efficiently water from cushion layer. Ones the concrete face cracks or does not work properly
the interior structure of the cushion layer would change with the fine particles moving downward along water flow. Fortunately
with the protection of transition zone
the particles would stop around the interface between the two zones; and seepage stability of the cushion layer would be maintained. In the first abnormal experience
some fine particles would move out from the transition zone; but the framework of the material would remain stable. With the support of the main rockfill zone
the transition zone could continue to function at both aspects of filtering and drainage.