王志兵, 麦棠坤, 齐程. 2017: 泥石流孕育-启动过程的细粒作用. 工程地质学报, 25(s1): 357-364. DOI: 10.13544/j.cnki.jeg.2017.s1.056
    引用本文: 王志兵, 麦棠坤, 齐程. 2017: 泥石流孕育-启动过程的细粒作用. 工程地质学报, 25(s1): 357-364. DOI: 10.13544/j.cnki.jeg.2017.s1.056
    WANG Zhibing, MAI Tangkun, QI Cheng. 2017: EFFECTS OF FINES OF SOIL IN THE PROCESS OF DEBRIS FLOW PREPARATION AND INITIATION. JOURNAL OF ENGINEERING GEOLOGY, 25(s1): 357-364. DOI: 10.13544/j.cnki.jeg.2017.s1.056
    Citation: WANG Zhibing, MAI Tangkun, QI Cheng. 2017: EFFECTS OF FINES OF SOIL IN THE PROCESS OF DEBRIS FLOW PREPARATION AND INITIATION. JOURNAL OF ENGINEERING GEOLOGY, 25(s1): 357-364. DOI: 10.13544/j.cnki.jeg.2017.s1.056

    泥石流孕育-启动过程的细粒作用

    EFFECTS OF FINES OF SOIL IN THE PROCESS OF DEBRIS FLOW PREPARATION AND INITIATION

    • 摘要: 形成泥石流的固体物质颗粒具有宽级配,粒径大小悬殊的特点,其中细粒组分(d0.075mm)对泥石流体的结构状态、流变性、屈服应力、运动形态和冲淤性都有重要影响;虽然细粒组分在泥石流土体中的含量较低,但常常具有独特的物理化学力学性质(如分散性),在雨水入渗与渗流过程中表现为内在的不稳定性,对泥石流的孕育-启动有重要影响。在降雨入渗和渗流过程中,泥石流土体流失颗粒主要为细颗粒,携带了细粒的水流会堵塞土体孔隙并降低土体渗透性,对坡面产流的形成具有重要影响,坡面产流的形成会加剧斜坡的失稳破坏。深入研究细粒运移堵塞效应对泥石流孕育-启动过程的影响,不仅为泥石流灾害的形成机理提供新的研究思路,而且能为泥石流的防灾减灾提供理论基础。

       

      Abstract: Soil of debris flow has a broadly graded weight distribution, a great disparity in size, a high dispersion in fine components, which caused the effects of Particles Transport on Soil Pores Clogging(PTSPC)in the process of rainfall and seepage. Due to the interaction between soil and rainwater, small particles can be detached and transported, some of them may clog at pores, PTSPC decreased the permeability of soils in debris flow sources, PTSPC played an important role in the process of debris flow preparation and initiation. This research article summarized extensive literature of debris flow, and reviews relevant fine particles transport at home and abroad. Finally, several research directions were proposed based on the effects of PTSPC.The study provided new ideas for the mechanism of rainfall-induced debris flow, and a theoretical basis for disaster prevention and mitigation.

       

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