首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Simulation of the nucleation and growth of simple clay minerals in weathering processes: The NANOKIN code
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Simulation of the nucleation and growth of simple clay minerals in weathering processes: The NANOKIN code

机译:模拟简单粘土矿物在风化过程中的成核和生长:NANOKIN代码

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摘要

We present a numerical approach which accounts for nucleation, growth and/or resorption of particles of fixed composition in aqueous solutions, and which involves functionalities suited to the formation of simple clay minerals in weathering processes, such as: formation of non-spherical particles, heterogeneous/homogeneous nucleation, several growth laws, precipitation resulting from the dissolution of primary minerals. The overall model is now embedded into a new numerical code called NANOKIN, in which several optimization procedures have been introduced in order to allow long dynamics to be followed. NANOKIN was applied to the precipitation of Al- bearing minerals from aqueous solutions: halloysite, kaolinite and Ca-montmorillonite. It allowed us to propose a stable scheme for the competitive precipitation of halloysite and kaolinite under two different types of initial conditions: (1) a given initial super-saturation state of the aqueous solution; (2) progressive super-saturation resulting from the kinetic dissolution of the minerals from a granitic rock under weathering conditions. Both yield particle sizes in the micron range, but with distinct crystal size distribution functions. The interplay between kinetic and thermodynamic effects is discussed.
机译:我们提供了一种数值方法,用于说明水溶液中固定成分的颗粒的形核,生长和/或吸收,并且涉及适合于在风化过程中形成简单粘土矿物的功能,例如:非球形颗粒的形成,异质/均质成核,几种生长规律,主要矿物溶解导致的沉淀。现在,整个模型被嵌入到称为NANOKIN的新数字代码中,其中引入了多个优化过程,以便遵循长动态。 NANOKIN用于从水溶液中沉淀含铝矿物:埃洛石,高岭石和钙蒙脱石。它使我们能够为两种不同的初始条件下的埃洛石和高岭石的竞争性沉淀提出一个稳定的方案:(1)给定的水溶液初始超饱和状态; (2)在风化条件下,花岗岩中矿物的动力学溶解导致渐进超饱和。两者均产生微米级的粒径,但具有独特的晶体粒径分布功能。讨论了动力学和热力学效应之间的相互作用。

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