Petrishcheva Elena, Tiede Lisa, Schweinar Kevin, Habler Gerlinde, Li Chen, Gault Baptiste, Abart Rainer
Department of Lithospheric Research, University of Vienna, Althanstrasse 14, 1090 Vienna, Austria.
Max-Planck-Institut für Eisenforschung GmbH, Max-Planck-Straße 1, 40237 Düsseldorf, Germany.
Phys Chem Miner. 2020;47(7):30. doi: 10.1007/s00269-020-01097-4. Epub 2020 Jun 7.
We used atom probe tomography to complement electron microscopy for the investigation of spinodal decomposition in alkali feldspar. To this end, gem-quality alkali feldspar of intermediate composition with a mole fraction of of the K end-member was prepared from Madagascar orthoclase by ion-exchange with (NaK)Cl molten salt. During subsequent annealing at and close to ambient pressure the ion-exchanged orthoclase unmixed producing a coherent lamellar intergrowth of Na-rich and K-rich lamellae. The chemical separation was completed, and equilibrium Na-K partitioning between the different lamellae was attained within four days, which was followed by microstructural coarsening. After annealing for 4 days, the wavelength of the lamellar microstructure was and it increased to after annealing for 16 days. The observed equilibrium compositions of the Na-rich and K-rich lamellae are in reasonable agreement with an earlier experimental determination of the coherent solvus. The excess energy associated with compositional gradients at the lamellar interfaces was quantified from the initial wavelength of the lamellar microstructure and the lamellar compositions as obtained from atom probe tomography using the Cahn-Hilliard theory. The capability of atom probe tomography to deliver quantitative chemical compositions at nm resolution opens new perspectives for studying the early stages of exsolution. In particular, it helps to shed light on the phase relations in nm scaled coherent intergrowth.
我们使用原子探针断层扫描技术来补充电子显微镜,以研究碱性长石中的旋节线分解。为此,通过与(NaK)Cl熔盐进行离子交换,从马达加斯加正长石制备了具有K端元摩尔分数为 的中间成分的宝石级碱性长石。在随后于 且接近常压下进行退火时,离子交换后的正长石发生分解,产生了富含Na和富含K的薄片的连贯层状共生体。化学分离完成,不同薄片之间的Na-K平衡分配在四天内达到,随后是微观结构粗化。退火4天后,层状微观结构的波长为 ,退火16天后增加到 。观察到的富含Na和富含K的薄片的平衡组成与早期对连贯溶线的实验测定结果合理吻合。利用Cahn-Hilliard理论,根据层状微观结构的初始波长和从原子探针断层扫描获得的层状组成,对层状界面处与成分梯度相关的过剩能量进行了量化。原子探针断层扫描能够以纳米分辨率提供定量化学成分,为研究出溶的早期阶段开辟了新的视角。特别是,它有助于阐明纳米尺度连贯共生体中的相关系。