Abstract:The rise of geothermal water level can be observed in the discharge section in a convective hydrothermal system. It is hard to explain in terms of gravity-driven groundwater systems, suggesting the existence of an additional driving force. This geothermal driving force is closely related to the changes in density, salinity, and viscosity caused by the increase in groundwater temperature. It is significant to quantitatively characterize the geothermal driving force for the interpretation of geothermal water lev… Show more
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