Abstract:
The temperature gradient was calculated by measuring the temperature background values at different depths of 12 boreholes for seismic research in Jiangsu Province. Combined with the temperature change and the geological structure of the borehole, the characteristics of borehole water temperature in the study area are compared and analyzed. The result shows that the temperature gradient of the borehole is the result of the combined effect of the combined mechanism of hydrothermal dynamics and geothermal dynamics. The borehole geological structure and the distribution of aquifer have an important influence on the temperature gradient value. The research results can provide data support for quantitative analysis of wellbore water temperature.