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A study on the fractal characteristics of displacement time-series during the evolution of landslides

机译:滑坡演化过程中位移时间序列的分形特征研究

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Abstract Landslides are one of the major natural disasters that are frequently occurring in southwestern China. The main objective of this study is to investigate the relationship between failure of landslide and fractal dimension using displacement time-series. Taking two slopes in southwestern China as examples, we estimate the fractal parameters of displacement time-series and analyze the relationship between fractal dimension and the stability of the slope during the evolution of landslides. The result shows that the fractal dimension increases when a landslide undergoes a transition from stability to failure, but decreases during the evolution from active to stable. Fractal dimension has a critical value of 1.10 in the transition between active and stable, which indicates that fractal dimension is an important nonlinear parameter in the evaluation of the stability of landslides, although more studies and in situ data are required for validation.
机译:摘要滑坡是中国西南地区经常发生的重大自然灾害之一。本研究的主要目的是利用位移时间序列研究滑坡破坏与分形维数之间的关系。以西南地区的两个边坡为例,估算了位移时间序列的分形参数,并分析了滑坡演化过程中分形维数与边坡稳定性之间的关系。结果表明,当滑坡经历从稳定到破坏的过渡时,分形维数增加,但是从活动到稳定的演化过程中,分形维数减小。分形维数在活动和稳定之间的转换中的临界值为1.10,这表明分形维数是评估滑坡稳定性的重要非线性参数,尽管需要进行更多的研究和现场数据来验证。

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