Seabed hydrothermal fluid circulation three-dimensional simulation method
A technology of fluid circulation and three-dimensional simulation, which is applied in design optimization/simulation, special data processing applications, instruments, etc., and can solve the problems that the evolution law of the driving mechanism cannot be directly observed
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Embodiment 1
[0048] The present invention relates to a three-dimensional simulation method of hydrothermal circulation under high-temperature and high-pressure environment on the seabed. Currently, the three-dimensional simulation of hydrothermal circulation is still a big challenge. The method (the geothermal simulation software HYDROTHERMAL issued by USGS) is compared to verify the reliability of the present invention. The effect display is as follows:
[0049] figure 2 Shows the 2D model mesh used in Example 1, figure 2 A and 2B represent orthogonal grids and non-orthogonal triangulations, respectively. HYDROTHERMAL simulation is limited to orthogonal grids, but the present invention can be simulated under both grids. The parameters of the model are: oceanic crust permeability k=10 -15 m 2 , porosity ε=0.1, rock specific heat C pr =800J / (kg℃), rock thermal conductivity λ r =2W / (m℃), rock density ρ r =2700kg / m 3 ;The boundary conditions are: the top represents the seabed with ...
Embodiment 2
[0051] The characteristics and advantages of the present invention are that complex three-dimensional hydrothermal circulation simulation can be performed, and the effects are as follows:
[0052] In the ultra-slow spreading mid-ocean ridge, the detachment fault has an important control effect on the hydrothermal circulation, and the method of the present invention is used to illustrate the characteristics and operation mechanism of the detachment fault's dominant hydrothermal circulation. Its geological model and grid division results are as follows: Figure 5 As shown in A, a heat source (at a constant temperature of 750°C) located about 1 km below the seafloor, a detachment fault with a width of about 100 m, and a cylinder with a radius of 50 m represent the permeability channel of the shallow oceanic crust, all of which have a permeability of 10 -14 m 2 , the oceanic crust background permeability is 10 -16 m 2 . The 100°C and 400°C isothermal surfaces, hydrothermal flu...
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