中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Deformation characteristics of loess landslide along the contact between loess and Neocene red mudstone

文献类型:期刊论文

作者Wen, BP; Wang, S; Wang, E; Zhang, JM; Wu, YG; Wang, X
刊名ACTA GEOLOGICA SINICA-ENGLISH EDITION
出版日期2005
卷号79期号:1页码:139-151
关键词Loess Landslide Contact Between Loess And Neogene Red Mudstone Deformation Mechanism Field Monitoring Physical Modeling
ISSN号1000-9515
文献子类Article
英文摘要The loess landslide along the contact between loess and Neogene red mudstone (NRM) is one of those that have occurred extensively and frequently in loess areas of China. To better understand the mechanism of this type of landslides, a distressed loess slope being subjected to deformation along the loess-NRM contact was comprehensively investigated through approaches of field monitoring and laboratory physical modeling. Field observation and physical modeling shows that the slope deformation will experience two distinct processes: 1) laterally retrogressive and vertically progressive propagation, which was initiated by falling of the slope head; and 2) retrogressively separate mass sliding along the weak basal zone of the loess-NRM contact with minor sliding along the paleosols within the loess. Shear failure of the loess-NRM contact may initiate in the middle section, followed by a progressive propagation towards the slope toe and inner slope. Analysis reveals that the deformation characteristics of the distressed slope are largely constrained by slope topography, the unique structure, physical and mechanical properties of loess and paleosols, and occurrence and nature of the loess-NRM contact. Rainfall has significantly influence on the deformation characteristics of the slope through its interaction with the loess and soil of the loess-NRM contact. Additionally, improper style and intensity of cutting on the slope greatly enhance and accelerate the deformation course of the slope.
WOS研究方向Geology
语种英语
WOS记录号WOS:000228762000016
出版者GEOLOGICAL SOC CHINA
源URL[http://ir.iggcas.ac.cn/handle/132A11/65866]  
专题中国科学院地质与地球物理研究所
通讯作者Wen, BP
作者单位1.Tsing Hua Univ, Dept Hydraul Engn, Beijing 100084, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
3.Gansu Bur Geol Explorat, Inst Hydrogeol & Engn Geol Explorat, Tianshui 741020, Gansu, Peoples R China
推荐引用方式
GB/T 7714
Wen, BP,Wang, S,Wang, E,et al. Deformation characteristics of loess landslide along the contact between loess and Neocene red mudstone[J]. ACTA GEOLOGICA SINICA-ENGLISH EDITION,2005,79(1):139-151.
APA Wen, BP,Wang, S,Wang, E,Zhang, JM,Wu, YG,&Wang, X.(2005).Deformation characteristics of loess landslide along the contact between loess and Neocene red mudstone.ACTA GEOLOGICA SINICA-ENGLISH EDITION,79(1),139-151.
MLA Wen, BP,et al."Deformation characteristics of loess landslide along the contact between loess and Neocene red mudstone".ACTA GEOLOGICA SINICA-ENGLISH EDITION 79.1(2005):139-151.

入库方式: OAI收割

来源:地质与地球物理研究所

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