CAJ | 학술논문

以宁夏石碑塬滑坡为研究对象，在工程地质测绘和试验测试的基础上建立了有限差分数值模型，对该黄土坡液化过程进行了模拟。分析结果表明：该黄土边坡在天然工况下处于稳定状态；在地震作用下，非饱和黄土几乎没有液化现象，而在地下水位附近的饱和黄土易发生液化，导致其物理力学参数降低，即使在很缓的角度下也易产生边坡失稳；地震结束之后，由于液化导致孔压比减小，黄土渗透性较之前更低，边坡的孔隙水压力消散缓慢，滑带强度恢复也缓慢，易产生长距离滑动。
이저하석비원활파위연구대상，재공정지질측회화시험측시적기출상건립료유한차분수치모형，대해황토파액화과정진행료모의。분석결과표명：해황토변파재천연공황하처우은정상태；재지진작용하，비포화황토궤호몰유액화현상，이재지하수위부근적포화황토역발생액화，도치기물리역학삼수강저，즉사재흔완적각도하야역산생변파실은；지진결속지후，유우액화도치공압비감소，황토삼투성교지전경저，변파적공극수압력소산완만，활대강도회복야완만，역산생장거리활동。
Taking Shibeiyuan landslide in Ningxia Autonomous Region as a research object, based on engineering geological mapping and laboratory tests, a loess landslide model of finite difference is established to simulate the liquefaction process. The results showed that the loess slope was in stable state under natural condition. In the earthquake process, no liquefaction phenom-enon occurred in unsaturated loess, but the saturated loess near the groundwater line is prone to liquefaction, decreasing the physical and mechanical parameters of loess, so landslide could occur for gentle slope. After the earthquake, the liquefaction re-sulted in the decrease of pore pressure ratio, so the loess permeability dropped down, and the pore water pressure dissipated slow-ly. As a result, the soil strength of sliding layer recovered slowly, causing long-range sliding.