As we all know, the interior of the Earth is composed of different layers, with the deeper layers having a higher temperature than the outer layers. This phenomenon has triggered enthusiastic research by scientists. The reasons for this are quite complex, with multiple factors intertwined affecting the formation of this temperature gradient.
Geothermal gradient is the rate of temperature change with depth. Generally speaking, the temperature of the earth's crust increases with depth.
Within the Earth's crust, temperatures rise at about 25 to 30 °C per kilometer, mostly because of the flow of heat from the hotter mantle. In addition to this, the increase in the temperature of the Earth's interior is also related to radioactive decay. Heat in the Earth's interior comes from a variety of sources, including radioactive decay, residual heat from the global formation process, and the latent heat of core crystallization.
In other words, the heat inside the Earth is the result of past geological changes and natural processes.
The Earth's internal heat is produced primarily by the decay of radioactive elements. These elements, such as potassium-40 and uranium-238, are abundant in some parts of the earth's crust, especially in granite and basalt. Therefore, the Earth's upper crust contains a higher concentration of radioactive elements than the mantle in the Earth's crust, and these elements provide most of the heat.
Today's geothermal production accounts for approximately 45 to 90% of the flow of heat within the Earth and is primarily derived from the radioactive decay of the Earth's mantle.
As depth increases, the temperature inside the Earth gradually increases, but the geothermal gradient varies in different regions. In the upper layers of the continental crust, the overall temperature rises faster, while in the oceanic crust, the geothermal flow is stronger. In addition, these geothermal flows are closely related to the movement of the earth's plates, because heat has to be transferred from the depths to the surface, and in this process the earth's crust plays the role of a thick insulating layer.
The heat flow inside the Earth is continuous and is lost from the interior to the surface. Studies around the world show that the Earth is losing approximately 44.2 terawatts of heat every second. The average heat flow is 65 milliwatts per square meter on continental crust, rising to 101 milliwatts per square meter on oceanic crust, reflecting global variations in geothermal energy.
Geothermal energy, as a renewable energy source, has great potential. As early as ancient Rome, people had begun to use this natural geothermal heat for heating and bathing. With the advancement of technology, we can now use geothermal energy to generate electricity. This method does not require fuel and extracts heat directly from geothermal storage.
Geothermal gradients vary from location to location. The researchers determined the geothermal gradient by measuring the temperature at the bottom of the borehole. In stable tectonic regions, temperature is related to hydrological performance, while in cold regions, geothermal dips can also have significant effects, such as in semi-permafrost regions, where changes in underground temperatures reflect climate changes over the past thousands of years.
Some areas may have a negative geothermal gradient, which means that the temperature decreases with greater depth. This is especially true in certain secondary water layers or subduction zones.
Overall, the temperature of the Earth's interior continues to change with depth. Such changes are driven by a variety of factors, from radioactive decay to crustal movement, all showing how complex the inner workings of the Earth are. and mystery. In the face of these natural phenomena, humans still have many unknown areas to explore. Have you ever thought about what undiscovered mysteries are hidden behind these heat forces?