| 摘要 |
The water in a closed loop geothermal system is caused to flush the system by reverse flow of water in and through the system. This provides a "well-to-well" full reversal of the water flow, thus permitting the factor of a primary receiver well to not only receive the geothermally used water from the primary well, but for that receiver well to then serve as an aquifer subsequently for causing the flow to go back to the primary well.
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