Method for evaluating terrestrial heat single-well stratum thermal property distribution
A technology of thermophysical properties and formation, applied in the field of geothermal single well formation thermophysical property distribution evaluation, can solve the problems of poor model applicability, complex analysis process, low data accuracy, etc., and achieve the effect of accurate specific heat capacity distribution
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Embodiment 1
[0023] Embodiment 1: This embodiment provides a geothermal single-well formation thermophysical property distribution evaluation method using dual wellbores, using Monte Carlo algorithm to invert formation thermal conductivity and specific heat capacity.
[0024] Such as figure 2 As shown, a single geothermal well includes an inner cylinder and an outer cylinder, and isothermal water is injected into the outer cylinder at a certain rate. The water flows from the wellhead to the bottom of the well in the outer cylinder, then enters the inner cylinder from the bottom of the well, and finally flows out at the wellhead. Place thermocouples at each depth in the outer cylinder and connect them to a data acquisition instrument to measure the temperature of water at each depth in the outer cylinder at different times.
[0025] Since there is no measured data, it can be assumed that a virtual geothermal single well is 5000m deep and the geothermal gradient is 0.03K m -1 , the formati...
Embodiment 2
[0028] Embodiment 2: This embodiment provides a geothermal single-well formation thermophysical property distribution evaluation method using dual wellbores, and uses the Monte Carlo algorithm based on Latin hypercube sampling to invert the formation thermal conductivity and specific heat capacity.
[0029] Such as figure 2 As shown, a single geothermal well includes an inner cylinder and an outer cylinder, and isothermal water is injected into the outer cylinder at a certain rate. The water flows from the wellhead to the bottom of the well in the outer cylinder, then enters the inner cylinder from the bottom of the well, and finally flows out at the wellhead. Place thermocouples at each depth in the outer cylinder and connect them to a data acquisition instrument to measure the temperature of water at each depth in the outer cylinder at different times.
[0030] Since there is no measured data, it can be assumed that a virtual geothermal single well is 5000m deep and the geo...
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