scholarly journals Temperature Gradient in the Earth's Crust

Nature ◽  
1924 ◽  
Vol 113 (2843) ◽  
pp. 623-623
Author(s):  
A. STRAHAN
2021 ◽  
Vol 07 (03) ◽  
pp. 16-21
Author(s):  
Rasim Nəcəfov Rasim Nəcəfov

It is known that in the center of the Earth the temperature is about 5000 0C and in the direction of the earth's crust it decreases. It is also known that the temperature gradient of the Earth is 3 0C every 100 meters in depth and it is constant throughout the planet. Consequently, the temperature of the Earth's crust is the most beneficial source of heat and energy. It accumulates the energy of the sun and is heated by the focal temperature. In Azerbaijan, at a depth of one meter to 50 meters, the temperature is stable and equal to 5-8 ° C. Keywords: geothermal energy, Earth's crust temperature, temperature gradient, thermal waters, steam turbines and heat pumps, 3D model of the field.


Professor Rutherford has given a calculation which suggests that there may be enough radium in the earth to account for the temperature gradient observed near the surface. The question is of great interest from a cosmical point of view. For if we find that the earth’s internal heat is due to radio-activity, and if we assume, as has been usual, that this heat is due to some vestiges of the cause operative in the sun and stars, it would follow that these latter are heated by radio-active changes also.


1915 ◽  
Vol 79 (2058supp) ◽  
pp. 382-383
Author(s):  
Alphonse Berget

2017 ◽  
Vol S36 ◽  
pp. 3-10
Author(s):  
P. G. Dyadkov ◽  
◽  
L. V. Tsibizov ◽  
M. P. Kozlova ◽  
A. V. Levicheva ◽  
...  

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