饱和节理岩体中地震波散射分析
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摘要
通过建立饱和节理岩体的等效模型 ,利用饱和孔隙介质的 Biot理论 ,研究其在地震波作用下由于局部地形变化引起的散射特性。实例分析结果表明 ,按单相介质模型的计算结果较按饱和孔隙介质模型的计算结果小 ,特别对 P1波入射的地震波 ,且相对误差最多超过 80 %。因而 ,对常处于水饱和环境下工作的船闸及其它水工结构 ,在抗震设计中应充分考虑由于水饱和作用对船闸及其它水工结构安全性的影响
On the basis of the equivalence of the seepage and of the theory of Biot, this paper proposes the equivalent model of saturated jointed rock mass and the scattering of elastic seismic wave. Being as a special example, the scattering of elastic seismic wave in the ship-lock high slope of Three-gorges Project is studied numerically and abundant calculation results regarding the response to the incident wave directions, frequencies etc. are obtained. The results have shown that the dynamic response in the single-phase medium is different from that in the saturated jointed rock mass.
引文
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