兰州大学学报(自然科学版)
蘭州大學學報(自然科學版)
란주대학학보(자연과학판)
JOURNAL OF LANZHOU UNIVERSITY(NATURAL SCIENCES)
2014年
5期
733-738
,共6页
刘东飞%马金珠%田黎明%舒和平
劉東飛%馬金珠%田黎明%舒和平
류동비%마금주%전려명%서화평
数值模拟%铲刮深度%堆积厚度%泄流坡滑坡
數值模擬%鏟颳深度%堆積厚度%洩流坡滑坡
수치모의%산괄심도%퇴적후도%설류파활파
numerical simulation%erosion depth%stacking thickness%Xieliupo landslide
以舟曲泄流坡滑坡野外考察地质资料为基础,结合滑坡动力分析软件DAN-W对泄流坡滑坡全程运动进行模拟,着重探讨了铲刮效应以及不同流变模型对滑坡数值模拟的影响.结果表明:不同铲刮深度下,滑坡堆积体形态相似,堆积厚度随铲刮深度的加深而加大,运行时间随铲刮深度的加深而减少. F-V模型对泄流坡模拟的滑程最大可达255.75 m, Frictional模型模拟得到的最大堆积厚度为201.73 m,最大前缘速度为17.75 m/s,最长运行时间为64 s,并给出了泄流坡滑坡模拟最佳的流变参数,摩擦角为18?,摩擦系数为0.1,湍流系数为1000 m/s2.
以舟麯洩流坡滑坡野外攷察地質資料為基礎,結閤滑坡動力分析軟件DAN-W對洩流坡滑坡全程運動進行模擬,著重探討瞭鏟颳效應以及不同流變模型對滑坡數值模擬的影響.結果錶明:不同鏟颳深度下,滑坡堆積體形態相似,堆積厚度隨鏟颳深度的加深而加大,運行時間隨鏟颳深度的加深而減少. F-V模型對洩流坡模擬的滑程最大可達255.75 m, Frictional模型模擬得到的最大堆積厚度為201.73 m,最大前緣速度為17.75 m/s,最長運行時間為64 s,併給齣瞭洩流坡滑坡模擬最佳的流變參數,摩抆角為18?,摩抆繫數為0.1,湍流繫數為1000 m/s2.
이주곡설류파활파야외고찰지질자료위기출,결합활파동력분석연건DAN-W대설류파활파전정운동진행모의,착중탐토료산괄효응이급불동류변모형대활파수치모의적영향.결과표명:불동산괄심도하,활파퇴적체형태상사,퇴적후도수산괄심도적가심이가대,운행시간수산괄심도적가심이감소. F-V모형대설류파모의적활정최대가체255.75 m, Frictional모형모의득도적최대퇴적후도위201.73 m,최대전연속도위17.75 m/s,최장운행시간위64 s,병급출료설류파활파모의최가적류변삼수,마찰각위18?,마찰계수위0.1,단류계수위1000 m/s2.
Based on field survey geological data of the Xieliupo landslide in Zhouqu and combined with landslide dynamic analysis, the software DAN-W was used to simulate the motion of the Xieliupo landslide, and to explore the impact on landslide numerical simulations about the erosion effect and different rheologies. The results showed that the landslide deposit forms were similar to different erosion depths and stacking thickness along with the increase in erosion depth but decrease in running time. The maximum movement distance was 255.75 m simulated by F-V model. The maximum thickness was 201.73 m, the maximum front velocity was 17.75 m/s and the longest movement time is 64 s simulated by Frictional model. The best suitable rheological parameters have been found to simulate this landslide, with the friction angle being 18?, friction coe?cient being 0.1 and turbulence coe?cient being 1 000 m/s2.