Hydrus 2d 3d Crack In 14 !!EXCLUSIVE!!

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Generally, the soil cracks are the main reason for hydrology and soil erosion. The nonuniform distribution of soil cracks on the hillside will influence the overland flow. The water bypassing the soil cracks will reduce the infiltration rate and increase the runoff volume. Besides, it is also an important source of environmental pollution. Soil cracks were widely used to represent the channels of preferential flow in many numerical models and studies [5-13]. In the computational models, the soil cracks were often considered as network structures, and the role of the crack network for overland flow and hydrologic transport were investigated [5-8]. They found that the influence of the crack network on the overland flow and infiltration rate was significant. The results have shown that the overland flow was significantly affected by the crack network. The water bypassing the cracks reduced the water infiltration rate and increased the runoff volume. However, the effects of the crack network on hydrologic transport were rarely examined. Some research has focused on the size distribution and the spatial variation of the crack network [9-13]. The results of the simulation show that the number of cracks increase with the increase of the width of the crack. The depth of the crack network also increase, but the variation of the maximum crack depth is small, and it increases with the increase of the width of the crack.

The objective of this study is to analyze the effects of the crack networks on the surface flow and the infiltration at the slope surface. The numerical simulations were conducted by the finite element method. The water flow and the soil moisture distribution were obtained by the successive approximation method. The simulation results show that the permeability and the internal flow are related to the crack numbers and the distribution of the soil cracks. The soil cracks reduce the soil permeability, and increase the runoff, which is mainly caused by the water bypassing the soil cracks. The number of cracks is positively correlated with the permeability and the internal flow, but it is not related to the slope. The permeability is negatively related to the number of cracks, but it is not related to the slope.

Generally, the morphology of the soil is determined by the mechanical properties of the soil and the conditions of the environment. The propagation and opening of the cracks and the behavior of the cracks are induced by the tensile stress of the soil. The tensile stress can be induced by the wetting and drying cycles and the change of the soil moisture content.

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