研究了化学反应放热与流体混合运动间的耦合作用，分析了前者对可压混合层厚度、拟序结构及产物生成率等方面的影响。
The interaction of heat release and fluid dynamics is studied. The effects of the latter on the mixing growth, the coherent structure and the rate of product formed in the mixing layer are analyzed.
他们对放热的化学反应一无所知。
地壳中能够料想到的最重要的放热化学反应是硫化物的化学转变。
The most important exothermal reactions in the crust can be expected from the chemical transformations of sulfides.
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