Paper Title:
Formation Mechanism Study on Houchuangzi Slope Debris Flow
  Abstract

Taken the Houchuangzi slope debris flow along Kunming- -Songming highway as instance, analyzed the mineral composition of provenance on the slope debris flow adopted the polycrystal X ray diffractometer, which was rich in hydrophilic clay mineralssuch as kaolinite and montmorillnite; analyzed the fornation mechanism of the HouChuangzi slope debris flow by the laboratory model test, compartmentalized the fornation process of the HouChuangzi slope debris flow in to five stages from the aspects of slope debris flow morphology and crack extension mechanism.The results provide certain reference value for further research of the formation mechanical mechanism.

  Info
Periodical
Advanced Materials Research (Volumes 243-249)
Edited by
Chaohe Chen, Yong Huang and Guangfan Li
Pages
3082-3086
DOI
10.4028/www.scientific.net/AMR.243-249.3082
Citation
X. Y. He, H. K. Chen, H. M. Tang, G. J. Wen, "Formation Mechanism Study on Houchuangzi Slope Debris Flow", Advanced Materials Research, Vols. 243-249, pp. 3082-3086, 2011
Online since
May 2011
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Price
$32.00
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