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Updated: May 5, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
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ソレット効果と,高温シリケート溶融における同位素分離

Gerardo Dominguez1, Gautam Wilkins, Mark H Thiemens

  • 1University of California, San Diego, Department of Chemistry and Biochemistry, California 92093, USA. gdominguez@ucsd.edu

Nature
|April 22, 2011
PubMed
まとめ

新しいモデルは,地質的な溶融における化学的および同位体拡散を説明し,高温でも量子力学が重要なことを明らかにしています. これは,質量輸送プロセスを統一し,惑星の進化と初期の太陽系の進化の洞察を提供します.

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Heating a crystalline solid increases the average energy of its atoms, molecules, or ions, and the solid gets hotter. At some point, the added energy becomes large enough to partially overcome the forces holding the molecules or ions of the solid in their fixed positions, and the solid begins the process of transitioning to the liquid state or melting. At this point, the temperature of the solid stops rising, despite the continual input of heat, and it remains constant until all of the solid is...
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