| 地球地质历史中非生物成因的自组织耗散结构(英文) |
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| 作者姓名： | S.L.Shvartsev |
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| 作者单位： | Tomsk Department, Trofimuk Institute of Petroleum Geology and Geophysics of Siberian Branch of the RAS, Tomsk 634055, Russia |
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| 基金项目： | supported by grant NSh-9542.2006.5 from the Ministry of Industry and Science |
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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。
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| 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 |
Self-organizing abiogenic dissipative structures in the geologic history of the Earth |
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| S.L.Shvartsev.Self-organizing abiogenic dissipative structures in the geologic history of the Earth[J].Earth Science Frontiers,2009,16(6):257. |
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| Authors: | SLShvartsev |
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| Institution: | Tomsk Department, Trofimuk Institute of Petroleum Geology and Geophysics of Siberian Branch of the RAS, Tomsk 634055, Russia |
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| 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 equil... |
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| Keywords: | dissipative structures progressive self-organization equilibrium water-rock system energy of mineral formation geochemical types of secondary mineral formation |
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