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Shallow Landslide Spatial Early Warning Model Induced by Heavy Rainfall in South China Area

机译:南方地区大雨降雨诱导的浅层滑坡空间预警模型

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Controlled by the characteristics of regional geological environment, the mechanism of slope runoff and hydrological processes under severe rainfall conditions in South China is fundamentally different from other regions. Therefore, the formation mechanism of shallow landslides induced by heavy precipitation has unique regional characteristics. In this study, by analyzing the response mechanism of slopes in South China to heavy rainfall, the slope unit was selected as the basic unit for early warning, and the concept of slope physical mechanism model (SINMAP) was used for reference and expansion. Through the introduction of heavy rainfall impact coefficients and coupled hydrological models and landslide stability analysis models, Shallow landslide warning model suitable for the geological environment in South China was established. Taking Song gang River as a case, an early warning process calculation was carried out. The results show that the model calculation process is suitable for the small watershed area and the calculation results of the model are ideal. Construct a landslide space early warning model and explore the critical rainfall threshold for inducing landslides to provide a scientific basis for warning and prevention of landslide hazards.
机译:由区域地质环境的特点控制,南方严重降雨条件下的坡径流和水文过程的机制与其他地区根本不同。因此,重度沉淀诱导的浅层滑坡的形成机制具有独特的区域特征。在本研究中,通过分析南方山坡响应机制重大降雨,斜坡单位被选为预警基本单位,坡地物理机制模型(SINMAP)的概念用于参考和扩展。通过引入大雨冲击系数和耦合水文模型和滑坡稳定性分析模型,建立了适用于华南地质环境的浅层滑坡预警模型。采用宋刚河作为案例,进行了预警过程计算。结果表明,模型计算过程适用于小流域区域,模型的计算结果是理想的。构建滑坡空间预警模型,探讨诱导山体滑坡的临界阈值,为警告和预防滑坡危害提供科学依据。

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