A kind of water age determination method of semi-enclosed water area
A measurement method, a semi-closed technology, applied in general water supply conservation, instruments, 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
Patent Information
- Authority / Receiving Office
- CN · China
- Patent Type
- Patents(China)
- Current Assignee / Owner
- Publication Date
- 2018-12-28
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Abstract
Description
technical field
[0001] The invention belongs to the technical field of hydrodynamic numerical simulation, in particular to a method for measuring water age in semi-enclosed waters. Background technique
[0002] There are more than 1,500 rivers with a drainage area of more than 1,000 square kilometers in my country, more than 2,800 natural lakes with an area of more than 1 square kilometer, and a coastline of more than 18,000 kilometers long and a sea area of more than 3 million square kilometers. With the rapid development of the coastal economy, a large amount of pollutants and nutrients are discharged into rivers, lakes and coastal waters, resulting in the deterioration of the water environment. Especially for semi-enclosed waters with poor flow, it is difficult for the water body to exchange and renew with the surrounding water body through physical processes such as convection and diffusion to improve water quality, resulting in more serious deterioration of the ...
Examples
Embodiment
[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...