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引言近年来用物理化学动力学作用作为模型来研究火山机制,使得对火山现象的理论解释取得了较大进展。在这方面,火山学与其它很多地球科学学科分享成果,这成果来自其它学科的方法和概念应用到某一问题中。在培养新的见识方面,热力学、流体力学、流变学等领域的基本概念具有特殊的重要性。近来在这方面的进展很多,我们有必要把这篇评论的视野局限集中于岩浆上升至地表和地表上以至大气中喷发产物分布的基本物理作用。行星火山作用的远景强调的事实是火山可以看作是对行星内部组成和构造的探查物,而这又是位置、深度和时间的函数。
Introduction In recent years, physical and chemical kinetics as a model to study volcanic mechanisms, making the theoretical interpretation of volcanic phenomena made great progress. In this regard, volcanology shares the fruits of many other earth science disciplines, and the results come from the methods and concepts of other disciplines applied to a particular issue. The basic concepts in the fields of thermodynamics, fluid mechanics and rheology are of particular importance in developing new insights. Recent progress has been made in this area. It is necessary for us to focus the limitations of this commentary on the fundamental physical role of magma in distributing the distribution of the eruptions of the magma up to the surface and the earth and to the atmosphere. The fact that the vision of planetary volcanism emphasizes the fact that volcanoes can be thought of as probes of the composition and formation of the planet’s interior is a function of location, depth, and time.