Method for simulating hydrologic process of mountain slope scale in gneiss soil rocky mountain region
A technology for soil and rocky mountainous areas and process simulation, which is applied in special data processing applications, instruments, electrical and digital data processing, etc., and can solve problems such as low accuracy and model simulation distortion.
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[0114] This embodiment is a method for simulating hydrological processes at the hillside scale in gneiss rocky mountainous areas. The process is as follows figure 1 shown. The calculation process of the method described in this embodiment is as follows:
[0115] Hillside calculation unit division: The hillside is divided into several basic calculation units by using the isocurrent timeline method.
[0116] Vertical section division in the calculation unit: According to the characteristics of hillside vegetation, soil and rock, it is divided into 4 layers in the basic calculation unit (contour zone): vegetation canopy interception layer, surface storage layer (litter storage layer and depression Reservoir), soil layer, bedrock layer. The soil layer is further divided into homogeneous soil layer, soil-rock binary mixed medium layer, weathered gravel layer and bedrock layer. The state variables in the calculation unit include: vegetation canopy interception, depression storag...
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