1. 中国科学院 山地灾害与地表过程重点实验室,四川,成都,610041
2. 中国科学院 成都山地灾害与环境研究所,四川,成都,610041
3. 重庆川东南地质工程勘察设计院,重庆,400038
纸质出版:2017
移动端阅览
李秀珍, 张小红. 基于Mein-Larson入渗模型的降雨滑坡失稳破坏概率研究[J]. 水土保持通报, 2017,37(1):219-223.
LI Xiuzhen, ZHANG Xiaohong. A Study of Instability Probability of Rainfall-Induced Landslides Based on Mein-Larson Infiltration Model[J]. Bulletin of Soiland Water Conservation, 2017, 37(1): 219-223.
李秀珍, 张小红. 基于Mein-Larson入渗模型的降雨滑坡失稳破坏概率研究[J]. 水土保持通报, 2017,37(1):219-223. DOI: 10.13961/j.cnki.stbctb.2017.01.039.
LI Xiuzhen, ZHANG Xiaohong. A Study of Instability Probability of Rainfall-Induced Landslides Based on Mein-Larson Infiltration Model[J]. Bulletin of Soiland Water Conservation, 2017, 37(1): 219-223. DOI: 10.13961/j.cnki.stbctb.2017.01.039.
[目的] 评价降雨诱发浅层滑坡的失稳破坏概率,为相关研究提供理论依据。[方法] 在引入并扩展了Mein-Larson降雨入渗模型的基础上,将Mein-Larson入渗模型与无限边坡稳定性方法有机结合,建立2种降雨情形(高强度短历时和低强度长历时)下降雨滑坡稳定性的确定性评价模型,然后再将蒙特卡洛数值模拟方法与降雨滑坡的确定性评价模型结合,建立降雨滑坡稳定性的概率评价方法。[结果] 提出了1种降雨诱发浅层滑坡失稳的概率评价方法。[结论] 概率评价方法可以描述降雨滑坡发生及发展过程中存在的不确定性,可以计算不同降雨情形下,不同降雨时刻降雨诱发边坡的失稳破坏概率。该方法的评价结果更符合边坡实际情况。
[Objective] The objective of the study is to evaluate the instability probability of shallow landslide induced by rainfall
and to provide theoretical basis for related research. [Methods] We combine Mein-Larson model with infinite slope stability models of saturated soil by introducing and developing the Mein-Larson infiltration model
and establish deterministic models for rain-induced landslides under short duration rainfall with high intensity and long duration rainfall with low intensity. Then we establish a probability analysis method of the slope instability by combining the deterministic models with Monte Carlo method. [Results] One kind of evaluation method for the failure probability of shallow landslide induced by rainfall was proposed.[Conclusion] The probability method not only can describe the uncertainties in the process of occurrence and development of rain-induced landslides
but also can calculate the instability probability of rain-induced slope instability under the different rainfall time. The assessment results are in high agreement with the actual slope.
马崇武,刘忠玉.降雨入渗时无限边坡的水平位移与稳定性分析[J].岩土力学,2007,28(S1),563-568.
徐卫亚,张志腾.滑坡失稳破坏概率及可靠度研究[J].灾害学,1995,10(4):33-37.
Lee S, Pradhan B. Probabilistic landslide hazards and risk mapping on Penang Island, Malaysia[J]. Journal of Earth System Science, 2006,115(6):661-672.
Sivakumar B G L, Murthy D S. Reliability analysis of unsaturated soil slopes[J]. Journal of Geotechnical and Geoenvironmental Engineering, 2005,131(11):1423-1428.
Cassidy M J, Uzielli M, Lacasse S. Probability risk assessment of landslides: A case study at Finneidfjord[J]. Canadian Geotechnical Journal, 2008,45(9):1250-1267.
Zhang L L, Zhang L M, Tang W H.Rainfall-induced slope failure considering variability of soil properties[J]. Geotechnique, 2005,55(2):183-188.
Zhang J, Huang H W, Zhang L M, et al. Probabilistic prediction of rainfall-induced slope failure using a mechanics-based model[J]. Engineering geology, 2014, 168:129-140.
Melchiorre C, Frattini P. Modelling probability of rainfall-induced shallow landslides in a changing climate, Otta, Central Norway[J]. Climatic Change, 2012,113(2):413-436.
张光辉,邵明安.用土壤物理特性推求Green-Ampt入渗模型中吸力参数
S
f
*
.土壤学报,2000,37(4):553-557.
Xie M, Esaki t, Cai M. A time-space based approach for mapping rainfall-induced shallow landslide hazard[J]. Environmental Geology, 2004,46(6):840-850.
胡立雄,白会人.降雨入渗的边坡稳定评价方法[J].辽宁工程技术大学学报:自然科学版,2007,26(2):235-237.
Mein R G, Larson C L. Modeling infiltration during a steady rain[J]. Water Resources Research, 1973,9(2):384-394.
Chen Li, Young M H.Green-Ampt infiltration model for sloping surfaces[J]. Water Resources Research, 2006,42(7):1-9.
Shu Tungchu.Infiltration during an unsteady rain[J]. Water Resources Research, 1978,14(3):61-466.
李宁,许建聪,钦亚洲.降雨诱发浅层滑坡稳定性的计算模型研究[J].岩土力学,2012,23(5):1485-1490.
徐钟济.蒙特卡洛法[M].上海:上海科技出版社,1985:10-24.
0
浏览量
1095
下载量
4
CSCD
关联资源
相关文章
相关作者
相关机构
京公网安备11010802024621