Water resource simulation method based on SWMM and MODFLOW coupling
A simulation method and technology of water resources, applied in general water supply conservation, structured data retrieval, instruments, etc., can solve problems such as deterioration of water body ecological environment, local waterlogging, serious water pollution of rivers, etc., and achieve the effect of convenient layout and selection
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Embodiment 1
[0094] The runoff calculation method for permeable surface, subsidence impermeable surface and non-depression impermeable surface is:
[0095] For the impermeable surface without depression storage, except for surface evaporation, the rainfall is basically converted into runoff, and runoff begins to form when the rainfall intensity is greater than the evaporation. Therefore, the formula for calculating the flow rate of impermeable surface without depression storage is:
[0096] R 1 = P-E (1)
[0097] Where: R 1 -The flow rate of the impermeable area of non-sag storage, mm;
[0098] P-precipitation, mm;
[0099] E-evaporation, mm.
[0100] For the impermeable surface with depressions, the maximum depression volume of the surface should be deducted from the rainfall first, and then the runoff will start to form. Therefore, the formula for calculating the flow rate of impermeable surface with depressions is:
[0101] R 2 =P-D (2)
[0102] Where: R 2 - The production f...
Embodiment 2
[0112] The derivation method of the nonlinear reservoir model is:
[0113] The surface confluence process refers to the collection of net rain from each sub-catchment to the outlet control section or directly discharged into the reservoir or river. The simulation of surface confluence routing adopts a nonlinear reservoir model, which is solved by the continuity equation and Manning's formula simultaneously. To complete the surface flow routing, the following parameters need to be entered in the SWMM model: the surface slope of the sub-catchment, the area of the sub-catchment, the width of the sub-catchment, the ratio of the permeable area of the sub-catchment and various types of surface depressions Stock volume and Manning's roughness coefficient. The runoff calculation methods for the three types of underlying surfaces use the nonlinear reservoir calculation model for calculation and simulation. The schematic diagram of the calculation method for the nonlinear reservoir...
Embodiment 3
[0135] The construction method of the infiltration model is as follows:
[0136] There are three infiltration models in SWMM: the Horton model; the Green-Ampert model and the runoff curve number method. Combined with rainfall, soil type and ground conditions, etc., an infiltration model suitable for the local area is selected to simulate the local infiltration process.
[0137] The Horton model is empirically derived from observations and is only suitable for projects where rainfall intensity always exceeds infiltration capacity, and the purpose of using the modified form in SWMM is to overcome this deficiency. The Horton infiltration model can be represented by the following function:
[0138] f=(f 0 -f ∞ )e -kt + f ∞ (7)
[0139] In the formula: f is the infiltration capacity, mm / min; k is the infiltration attenuation index, s-1 or h-1; t is the rainfall time, min; f0 is the initial infiltration rate, mm / min; Rate, mm / min.
[0140] The Green-Ampter model equation is...
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