Temperature Changes associated with Adiabatic Decompression in Geological Processes

Autor: WALDBAUM, D. R.
Zdroj: Nature; August 1971, Vol. 232 Issue: 5312 p545-547, 3p
Abstrakt: Joule-Thomson coefficients of crystals indicate that temperatures may increase during irreversible adiabatic release of pressure. Isenthalpic decompression provides a mechanism for “self-heating” in igneous and metamorphic processes.
Databáze: Supplemental Index