The geothermal gradient describes how temperature increases with depth beneath the Earth’s surface. It is a fundamental parameter for assessing subsurface heat flow, influencing geothermal energy potential, drilling safety, and hydrocarbon maturation.
In borehole measurements, the gradient is derived from the temperature recorded at a known depth and the surface temperature. By assuming a linear temperature increase, the simple ratio of temperature difference to depth provides a firstβorder estimate.
The calculation is expressed mathematically as shown below, where G denotes the geothermal gradient, T_b the temperature at the measured depth, T_0 the surface temperature, and z the depth in meters.
What is the geothermal gradient?
How is the geothermal gradient calculated?
Why is the geothermal gradient important?
What assumptions are made in calculating the geothermal gradient?
Can the geothermal gradient vary by location?
What units are typically used for the geothermal gradient?
How does the geothermal gradient affect drilling operations?
Results are for informational purposes only and do not constitute professional advice.
