Medium-deep layer buried pipe fluid temperature field analysis method considering underground water seepage
A technology of groundwater seepage and fluid temperature, applied in special data processing applications, instruments, electrical digital data processing, etc., can solve the problems of small calculation amount, unable to analyze the influence of groundwater seepage or calculation amount, etc., and achieve small calculation amount and high precision , the effect of high calculation accuracy
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Embodiment 1
[0110] In this embodiment, for a virtual mid-deep buried pipe, the fluid temperature field analysis method of the mid-deep buried pipe of the present invention is used to calculate the fluid temperature field at different times, and the calculation results are compared with the simulation results of the Fluent software. The relevant parameters of the medium-deep buried pipe are shown in Table 1.
[0111] It is known that the length L=1000m of the middle-deep buried pipe, then the borehole and the rock and soil are divided into 201 sections axially, that is, M=201, then Δz=L / (M-1)=5m;
[0112] The total time simulated is 100 hours, namely t tol = 100 hours. Set the time step Δt=2 minutes, then the number of time segments N=t tol / Δt=3000.
[0113] initial time (i.e. t 0 The fluid temperature of the inner and outer pipes and the initial temperature of rock and soil at time) are functions of depth:
[0114]
[0115] based on t 0 The temperature field of the inner and out...
Embodiment 2
[0120] In this embodiment, for a virtual medium-deep buried pipe, the fluid temperature field analysis method of the medium-deep buried pipe of the present invention is used to calculate the fluid temperature field at different times, and the calculation results are compared with other model simulation results. The relevant parameters of the mid-deep buried pipe are shown in Table 2.
[0121] It is known that the length L=2000m of the middle-deep buried pipe, then the borehole and rock and soil are divided into 401 sections axially, that is, M=401, then Δz=L / (M-1)=5m;
[0122] The total time simulated is 80 hours, namely t tol = 80 hours. Set the time step Δt=2 minutes, then the number of time segments N=t tol / Δt=2400.
[0123] initial time (i.e. t 0 The fluid temperature of the inner and outer pipes and the initial temperature of rock and soil at time) are functions of depth:
[0124]
[0125] The calculation steps are the same as those in Embodiment 1, and will not ...
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