Youngdo Park, Dal Yong Park, L. Evans, Jin-Han Lee
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The finite difference explicit method was used for the numerical calculation of lattice and boundary diffusion. For diffusion calculation, chemical concentrations of individual nodal points are used to calculate the amount of transported cations with diffusion coefficients determined from experiments. For lattice/boundary reaction, the lowest energy compositions of garnet and biotite were calculated using the distribution coefficient. Experimental runs were performed to test the consistency and reproducibility of the results. The results demonstrate the consistency and reproducibility, but show somewhat different zoning from that of Spear (1991), due to reduced dimension (3D in nature vs 2D in our model) and the arbitrarily chosen reaction constant. In spite of these limitations, we feel that the model presented here is at least a good starting point for diffusive mass transfer in a material with grain boundary structure. 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引用次数: 7
摘要
我们利用数值模拟系统Elle [Jessell et al. 2001]开发了石榴石扩散分区发展模型。Elle系统在薄片尺度上模拟纹理的发展,并假设长期的纹理变化可以通过增加增量过程来实现。目前已经建立了许多石榴石扩散分带模式的数值模型,但这些模型只考虑晶格扩散而不考虑晶界扩散。然而,我们的模型不仅考虑了晶格扩散,而且考虑了晶界/晶格反应和晶界扩散,模拟了石榴石中的扩散带。石榴石-黑云母体系的子过程包括(1)晶格扩散,(2)晶界扩散和(3)晶界/晶格反应。采用有限差分显式方法对晶格扩散和边界扩散进行了数值计算。对于扩散计算,通过实验确定的扩散系数,使用单个节点的化学浓度来计算阳离子的输运量。对于晶格/边界反应,利用分布系数计算了石榴石和黑云母的最低能组成。进行了实验运行,以测试结果的一致性和可重复性。结果显示出一致性和可重复性,但与Spear(1991)的结果显示出一些不同的分区,这是由于降低了维度(本质上是3D而我们的模型是2D)和任意选择的反应常数。尽管存在这些局限性,但我们认为这里提出的模型至少是具有晶界结构的材料中扩散传质的一个很好的起点。Journal of the Virtual Explorer, 2004卷15 Paper 6 http://virtualexplorer.com.au/基于elle的石榴石和黑云母之间阳离子交换反应的二维模型第2页虚拟浏览器杂志,2004卷15 Paper 6 http://virtualexplorer.com.au/基于elle的石榴石和黑云母之间阳离子交换反应的二维模型第3页
An Elle-based 2-D model for cation exchange reaction between garnet and biotite
We have developed a model for diffusion zoning development in garnet employing a numerical modeling system, Elle [Jessell et al. 2001]. The Elle system simulates textural development at thin section scale with an assumption that long term textural changes can be achieved by adding incremental processes. Many numerical models have been developed for the diffusion zoning pattern of garnet, but these models considered only lattice diffusion without allowing grain boundary diffusion. However, our model simulates the diffusion zoning in garnets by considering not only lattice diffusion but also grain boundary/lattice reaction and grain boundary diffusion. Sub-processes for our garnet-biotite system include (1) lattice diffusion, (2) grain-boundary diffusion, and (3) grain boundary/lattice reaction. The finite difference explicit method was used for the numerical calculation of lattice and boundary diffusion. For diffusion calculation, chemical concentrations of individual nodal points are used to calculate the amount of transported cations with diffusion coefficients determined from experiments. For lattice/boundary reaction, the lowest energy compositions of garnet and biotite were calculated using the distribution coefficient. Experimental runs were performed to test the consistency and reproducibility of the results. The results demonstrate the consistency and reproducibility, but show somewhat different zoning from that of Spear (1991), due to reduced dimension (3D in nature vs 2D in our model) and the arbitrarily chosen reaction constant. In spite of these limitations, we feel that the model presented here is at least a good starting point for diffusive mass transfer in a material with grain boundary structure. Journal of the Virtual Explorer, 2004 Volume 15 Paper 6 http://virtualexplorer.com.au/ An Elle-based 2-D model for cation exchange reaction between garnet and biotite Page 2 Journal of the Virtual Explorer, 2004 Volume 15 Paper 6 http://virtualexplorer.com.au/ An Elle-based 2-D model for cation exchange reaction between garnet and biotite Page 3