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    干湿作用下紫色土埂坎裂隙开闭演化特征

    Evolution pattern of propagation and closure of cracks in the purple-soiled bunds following alternative drying and wetting treatments

    • 摘要: 为研究干湿作用下紫色土埂坎裂隙开闭演化特征,通过重塑埂坎进行干湿循环试验,提取裂隙图像并计算其特征参数指标,探究干湿作用下紫色土埂坎裂隙开闭演化过程和规律,为紫色土埂坎的建设与维护提供依据。结果表明:1)脱湿过程中,裂隙强度(面密度和面积-周长比)与复杂度(形状指数和分形维数)先迅速增加(1~9d)后缓慢增加并趋于稳定(>9~15d),裂隙强度和复杂度呈极显著正相关关系(P < 0.01)。2)增湿过程中,裂隙形态随含水率增长可分为次裂隙闭合(Ⅰ)、裂隙交叉点断开(Ⅱ)和主裂隙变窄(Ⅲ)3个阶段。总体上,裂隙强度和复杂度平均降幅分别为87%和61%,其中,裂隙强度平均降幅Ⅰ阶段(62%)>Ⅱ阶段(47%)>Ⅲ阶段(33%),复杂度平均降幅Ⅰ阶段(52%)>Ⅱ阶段(18%)>Ⅲ阶段(17%)。3)裂隙强度和复杂度均值与干湿循环次数呈正比关系,前2次干湿循环时裂隙开裂程度和网络复杂度变化比较剧烈,随后逐次减小,第4次干湿循环后达到最大,第5次增湿时埂坎土块出现剥落。

       

      Abstract:
      Background  Soil bund has been widely constructed as important soil conservation practice on sloping farmlands in the purple-soil area, while the stability of the soil bund affects its soil conservation benefits. The propagation and closure evolution of cracks reduces the stability of soil bund following drying and wetting alternations, thereby affecting the associated soil conservation benefit provided. This study aims to reveal the propagation and closure evolution pattern of cracks developed on purple-soiled bund following alternative drying and wetting condition using indoor simulation test, and to determine the relationship between crack evolution and stability of soil bund.
      Methods  Undisturbed soil samples were collected from in-situ sloping farmland soil bund in Xiema town, Beibei district, Chongqing. Alternative drying and wetting was simulated in the laboratory, then the cracks images were extracted dynamically, Photoshop and image software were used to calculate the characteristic parameters of cracks (area density, area-perimeter ratio, shape index and fractal dimension).
      Results  1) During the drying process, the cracks intensity (area density and area-perimeter ratio) and complexity (shape index and fractal dimension) firstly increased significantly (1-9d) and then slowly increased to a stable state (>9-15d), while cracks intensity and complexity indexes showed a significant positive correlation (P < 0.01). 2) During the wetting process, the evolutionary process of cracks morphology could be divided into 3 stages, i.e., (Ⅰ) secondary cracks closure stage, (Ⅱ) cracks intersection disconnection stage, and (Ⅲ) main cracks narrowing stage. The overall average declining rate of cracks intensity and complexity were 87% and 61%, respectively, following a sequence of stage Ⅰ (62%)>stage Ⅱ (47%)>stage Ⅲ (33%), and stage Ⅰ (52%)>stage Ⅱ (18%)>stage Ⅲ (17%) for cracks complexity. 3) The average values of cracks intensity and complexity was proportional to the number of wetting and drying alternations. During the initial two wetting and drying alternations, the cracking degree and network complexity changed sharply, and then gradually decreased, reached the maximum after the 4th of alternation, and the bunds peel appeared at the 5th wetting process.
      Conclusions  This study shows that propagation and closure evolution of cracks subjected to alternative drying and wetting is an important factor reducing the stability of the soil bunds. With the increase of the number of the alternations, the evolution intensity and network complexity of cracks gradually increase, leading to the instability of the soil bunds. This findings can provide implications for the construction and maintenance of purple soil bunds for soil conservation purpose.

       

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