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在地质学背景后面隐藏着众多凝聚态问题。对它们需要运用凝聚态科学工具进行探索 ,才能发现蕴含其中的对称、相变、周期和突变等现象 ,以抓住其共有的科学本质。文中对结晶过程中的固熔体相变 ,上地幔部分熔融和地核差异旋转等典型地学问题 ,从凝聚态角度重新作了分析 ,指出尽管它们具有不同的时空范畴和地学内涵 ,曾分别被划归于不同的地学分支学科 ,但却共同体现出了大自然中模式形成的一个基本范式 ,即 :无序定态的空间对称破缺可以导致诸多宏观有序结构的形成。这也是其它一些类似的地学现象得以产生的共同原因。由此可认为 ,从各种地质分支学科的单一性探索 ,过渡到凝聚态地质学的统一研究 ,是地质科学发展过程中的一个必由阶段。而凝聚态物理学的成熟与深化 ,恰好为之提供了发展的契机。因此 ,就有可能从凝聚态地质学这一新的观点出发 ,将传统的地质研究领域进一步拓深 ,并且将其拓宽、推广到水利 ,环境 ,材料和生命科学中去。
Behind the background of geology hidden in many condensed matter problems. They need to use condensed matter science tools to explore, in order to find out the implications of the symmetry, phase transitions, cycles and mutations in order to seize the common scientific nature. In this paper, the typical geology problems of solid melt phase transformation, partial melting of the upper mantle and differential rotation of nucleus in the crystallization process are re-analyzed from the perspective of condensed matter. It is pointed out that although they have different spatial and temporal connotations, Is divided into different branches of science and geography, but they all embody a basic paradigm of the formation of patterns in nature. That is, the symmetrical breaking of disordered states can lead to the formation of many macroscopically ordered structures. This is also the common reason for the emergence of other similar phenomena of geosciences. From this, we can think that it is an essential stage in the development of geoscience from the single exploration and transition of various geological branches to the unification of condensed matter geology. The maturity and deepening of condensed matter physics provide an opportunity for development. Therefore, it is possible to proceed from the new point of view of condensed matter geology to further expand the field of traditional geological research and to extend it to water conservancy, environment, materials and life sciences.