Water age measurement method for semi-closed water area
A measurement method, a semi-closed technology, applied in general water supply conservation, special data processing applications, complex mathematical operations, etc., can solve the problems of underestimating the actual exchange capacity of water bodies, consuming large calculation time and storage space, and difficult calculations
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[0094] This embodiment discloses a method for determining the age of water in semi-enclosed waters, such as figure 1 As shown, the steps are as follows:
[0095] Step S1. Determine the model range and grid size according to the range of the water area to be measured, construct a triangular grid or a quadrilateral grid or a mixed grid, interpolate terrain data into the grid, and establish a hydrodynamic mathematical model.
[0096] In this step S1, a hydrodynamic mathematical model is established, mainly including the flow continuity equation and momentum equation:
[0097] The flow continuity equation is:
[0098]
[0099] The momentum equation is:
[0100]
[0101]
[0102] Where x and y are the coordinate axes of the Cartesian coordinate system;
[0103] h=η+d, h is the total water depth, η is the water level, and d is the still water depth;
[0104] u and v represent the average flow velocity along the water depth in the x and y directions, respectively;
[01...
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