地学前缘 ›› 2009, Vol. 16 ›› Issue (6): 257-275.

• 论文 • 上一篇    下一篇

SELFORGANIZING ABIOGENIC DISSIPATIVE STRUCTURES IN THE GEOLOGIC HISTORY OF THE EARTH地球地质历史中非生物成因的自组织耗散结构

 S.L.Shvartsev   

  1. Tomsk Department, Trofimuk Institute of Petroleum Geology and Geophysics of Siberian Branch of the RAS,  Tomsk 634055, Russia
  • 收稿日期:2009-08-20 修回日期:2009-11-01 出版日期:2009-12-16 发布日期:2009-12-10
  • 作者简介:SLShvartsev(1936—),男,教授,水文地质学专业，长期从事水文地球化学研究。Email: tomsk@igng.tsc.ru

Selforganizing abiogenic dissipative structures in the geologic history of the Earth.

SLShvartsev   

  1. Tomsk Department, Trofimuk Institute of Petroleum Geology and Geophysics of Siberian Branch of the RAS,  Tomsk 634055, Russia
  • Received:2009-08-20 Revised:2009-11-01 Online:2009-12-16 Published:2009-12-10

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摘要：

自从地球上有水出现，就持续存在水岩体系的平衡不平衡。这一体系内部是不协调的，这就决定了它在地质历史的长河中自发地连续发展的可能性，并导致完全新的矿物相和水的不同地球化学类型的生成。在地壳中这一体系持续在一个热力学分支的线性域中，远离平衡而发育。它积聚太阳能，形成非生物成因耗散结构。它在连续发育惯性中起特殊作用,然后发育为一种生命物质。前进自组织将向该体系倾斜的趋向，定义为无机物质发育的基础之一。还有其他的一组体系都从这个体系中继承了它大多数的性质。水岩体系的演化导致了次生矿物相和水的地球化学新类型的形成。随着演化程度加深，体系在成分上、结构上逐渐变得复杂，形成新的地球化学介质,它们又反过来控制新矿物相的生成从而对自身的性质产生影响。这一过程在地质历史上是永恒的。这便是矿物界自组织的要点，即包括发生、生长及新结构形体的时空弥散以及矿物、地球化学介质的形成，最后是新的有机物质和生命的起源。

关键词: 耗散结构;前进自组织;平衡;水岩体系;矿物生成的能量;次生矿物生成的地球化学类型

Abstract:

It is shown that since the appearance of water on the Earth, a stationary disequilibriumequilibrium waterrock system came into existence.  This system is internally inconsistent, which determines its ability to develop continuously in a spontaneous manner for a long geologic time, leading to the formation of principally new mineral phases and geochemical types of water. Within the Earths crust, this system persistently develops in a nonlinear field of the thermodynamic branch under the conditions far from equilibrium; it is capable of accumulating the solar energy and forms abiogenic dissipative structures playing a special role in the progressive development of inert matter and then of living matter. The inclination of this system to the progressive selforganization defines it as one of the fundamental and basic system in the development of inorganic matter. From this system there was a set of others having inherited most of its properties. The evolution of the waterrock system led to the formation of  secondary mineral phases and new geochemical types of water, and as these increased, the system gradually became more complex in composition and structure and formed new geochemical media which, in turn, control the formation of new mineral phases having effect on the characteristics of the media. This process is geologically perpetual. This is the essence of selforganization in mineral kingdom, including initiation, growth and spatialtemporal dispersal of new structural forms, mineral and geochemical media formations, and finally, the origination of new organic substances and life.

Key words:  dissipative structures; progressive selforganization; equilibrium; waterrock system; energy of mineral formation; geochemical types of secondary mineral formation