What is geothermal heat flow density?
Geothermal heat flow density measures the amount of thermal energy moving upward through a unit area of the Earth’s crust.
How do you calculate heat flow density?
Heat flow density (q) is calculated as the product of the rock’s thermal conductivity (k) and the vertical temperature gradient (ΞT/Ξz).
Why is geothermal heat flow density important?
It helps assess geothermal resource potential and understand the thermal regime of the lithosphere.
What factors affect heat flow density?
Higher rock thermal conductivity or steeper temperature gradients increase the upward heat flux.
How is thermal conductivity measured?
Thermal conductivity (k) can be measured using various laboratory techniques that assess a material’s ability to conduct heat.
What units are used for heat flow density?
Heat flow density is typically measured in milliwatts per square meter (mW/mΒ²).
Can this calculator be used globally?
Yes, the principles apply globally, but local data on thermal conductivity and temperature gradients are needed for accurate calculations.