Thermonuclear processes in the core is the main source of energy of geodynamic evolution and degassing of the earth

Mathematics – Logic

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

The Earth, Earth'S Internal Structure, Thermonuclear Processes

Scientific paper

Based on some additional clarifications of the cosmological model of the formation of the Solar System it was shown that the main source of the Earth's energy are thermonuclear processes in the inner Earth's core consisting of metallic hydrides. This energy is quite significant, but it is substantially smaller (by about three orders of magnitude) than the energy received from the Sun. The proposed hypothesis suggests a presence of hydrogen fluxes or deep fluids propagating from the Earth's core and transporting thermal energy from the thermonuclear reactions to the Earth's surface. This energy has been a primary reason for the endogenic, geodynamic and tectonic processes over the course of the Earth's whole history.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Thermonuclear processes in the core is the main source of energy of geodynamic evolution and degassing of the earth does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Thermonuclear processes in the core is the main source of energy of geodynamic evolution and degassing of the earth, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Thermonuclear processes in the core is the main source of energy of geodynamic evolution and degassing of the earth will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-914118

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.