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Lattice strain across Na–K interdiffusion fronts in alkali feldspar: an electron back-scatter diffraction study

机译:碱长石中Na–K互扩散前沿的晶格应变:电子背散射衍射研究

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摘要

Cation exchange experiments between gem quality sanidine (XOr = 0.85) and KCl melt produced chemical alteration of alkali feldspar starting at the grain surface and propagating inwards by highly anisotropic Na–K interdiffusion on the alkali sublattice. Diffusion fronts developing in b-direction are very sharp, while diffusion fronts within the a–c-plane are comparatively broad. Due to the composition dependence of the lattice parameters of alkali feldspar, the diffusion induced compositional heterogeneity induces coherency stress and elastic strain. Electron back-scatter diffraction combined with the cross-correlation technique was employed to determine the lattice strain distribution across the Na–K interdiffusion fronts in partially exchanged single crystals of alkali feldspar. The strain changes gradually across the broad fronts within the a–c-plane, with a successive extension primarily in a-direction conferring to the composition strain in unstressed alkali feldspar. In contrast, lattice strain characterised by pronounced extension in b-direction is localised at the sharp diffusion fronts parallel to b, followed by a slight expansion in a-direction in the orthoclase-rich rim. This strain pattern does not confer with the composition induced lattice strain in a stress-free alkali feldspar. It may rather be explained by the mechanical coupling of the exchanged surface layer and the mechanically strong substratum. The lattice distortion localised at the sharp diffusion front may have an influence on the diffusion process and appears to produce a self-sharpening feedback, leading to a local reduction of component mobilities.
机译:宝石品质的山梨定型(XOr = 0.85)和KCl熔体之间的阳离子交换实验产生了碱长石的化学变化,该碱长石从晶粒表面开始并通过碱金属亚晶格上高度各向异性的Na-K相互扩散而向内传播。沿b方向发展的扩散锋非常尖锐,而沿a-c平面的扩散锋则相对较宽。由于碱长石晶格参数的成分依赖性,扩散引起的成分异质性引起相干应力和弹性应变。电子背散射衍射与互相关技术相结合,用于确定碱长石部分交换的单晶中Na–K互扩散前沿的晶格应变分布。应变在a-c平面内的整个宽前线上逐渐变化,并且连续的延伸主要在a方向上,这导致无应力的碱长石中的成分应变。相反,以沿b方向显着扩展为特征的晶格应变位于平行于b的急剧扩散前沿,然后在富含正长石酶的边缘沿a方向略微扩展。该应变模式与无应力的碱性长石中的成分诱导晶格应变无关。而是可以通过交换的表面层和机械强度高的基质的机械耦合来解释。位于尖锐扩散前沿的晶格畸变可能会对扩散过程产生影响,并且似乎会产生自锐化反馈,从而导致部件迁移率局部降低。

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