崩岗是我国南方花岗岩地区特殊的土壤侵蚀现象,给山区经济造成了严重的影响。为了探索南方花岗岩地区崩岗侵蚀剖面的水分特性,明确水分与崩岗发育的关系,本研究采用野外调查采样与室内分析的方法,运用土壤粒径分形理论,并结合Brooks and Corey 模型,模拟花岗岩崩岗剖面土壤水分特征曲线。选择通城县花岗岩崩岗剖面5 个层次(表土层、红土层、过渡层、砂土层和碎屑层)采集土样,通过对土壤粒径分布和土壤含水量的测定,分析分形维数与土壤粒径之间的关系。同时,应用土壤粒径分形理论,模拟土壤水分特征曲线,基于估算结果与实测结果的比较,探讨分形方法估算土壤水分特征曲线的可行性。结果表明:崩岗剖面土壤黏粒质量分数越大,土壤粒径分维值越大;土壤粒径分维值越大,土壤水分特征曲线的分维值则越大,两者之间线性关系较好;运用分形理论,模拟土壤水分特征曲线的预测值与实测值具有良好的一致性,模拟结果的精度随土层的深度增加而增加,模拟效果以土壤黏粒和粉粒质量分数较少、砂粒质量分数较多的土壤效果较好。研究结果为花岗岩崩岗机理的探索奠定了基础,对崩岗水分的研究具有指导意义。
[Background] Collapsing gully, a serious soil erosion phenomenon in granite areas of South China, occurs mainly on mound or hill slopes under the interaction of water and gravity, causing severe destructions and threats in a wide range, including Hubei, Hunan, Jiangxi, Anhui, Fujian, Guangdong, and Guangxi, mainly south to the Yangtze River, and hence a grave impact on the economy in these hilly regions. [Methods] In order to explore the relationship between the soil moisture and the development of the collapsing gully, a field survey and indoor analysis were used to investigate the relationship between the soil moisture and the collapsing gully. The soil water characteristic curve of granite was simulated by fractal theory with Brooks and Corey model. The samples of profile ( surface soil, red soil, transition layer, sand layer, and debris layer ) in granite collapsing gully of Tongcheng County were collected, and the relationship between fractal dimension and soil particle size were analyzed by measuring the soil particle size distribution and soil moisture content. At the same time, the fractal theory of soil particle size was applied to simulate the soil water characteristic curve. Further, based on a comparison of estimated and measured results, the feasibility of estimating the soil water characteristic curve by fractal theory was explored. [Results] The higher the soil clay content in the profile of collapsing gully was, the larger the fractal dimension of soil particle size was; the larger the fractal dimension of soil particle size was, the larger the fractal dimension value of soil water characteristic curve was, indicating that there was a solid linear relationship between the two; the predicted values from the simulation of soil water characteristic curve by the fractal theory and measured values were in fine consistence, the accuracy of simulation results increased with the depth of soil increasing. The simulation effect was better for the soil containing less soil clay and silt content and more sand content. [Conclusions] The research results lay a foundation for the exploration of the mechanism of granite collapsing gully, which provides the guiding significance for the study of the water in collapse gully.
邓羽松,夏栋,蔡崇法,王秋霞,吕国安,丁树文. 基于分形理论模拟花岗岩崩岗剖面土壤水分特征曲线[J]. 中国水土保持科学, 2016, 14(2): 1-8.
Deng Yusong, Xia Dong, Cai Chongfa, Wang Qiuxia, Lyu Guoan, Ding Shuwen. Simulation of water characteristic curve in the soil profile of the collapsing gully on granite area of South China based on the fractal theory. SSWC, 2016, 14(2): 1-8.