Formation Mechanism Study on Houchuangzi Slope Debris Flow
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.
Chaohe Chen, Yong Huang and Guangfan Li
X. Y. He et al., "Formation Mechanism Study on Houchuangzi Slope Debris Flow", Advanced Materials Research, Vols. 243-249, pp. 3082-3086, 2011