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引用次数: 0
摘要
相干片状微结构的时间演化受其弹性特性的显著影响,特别是当外相是相干的时候。本研究利用 Cahn-Hilliard 模型研究二元碱长石的形态和能量演化,将各向异性弹性能量纳入吉布斯能量方程。卡恩-希利亚德模型成功地模拟了在天然样品中观察到的薄片取向,弹性应变与之前的研究结果一致。我们还计算了不同前驱体成分和温度下退火模拟的相干溶解度。无应变溶解度与相干溶解度之间的温度差(\(\Delta T\))为\(\Delta T = 85\,{}^\circ \text {C}\),略低于之前报道的类似参数值。这种差异可能是由于在相分离开始时存在非平面薄片,它们比平面薄片更稳定。我们还模拟了不同前驱相组成的相干溶解度的二项曲线。计算出的溶解度并不是唯一的,而是根据前驱体成分的不同而变化。我们的模型非常灵活,因为它不假定片状界面有任何特定形状,而且适用于各种相干二元体系。
The Cahn–Hilliard model of coherent lamellar microstructure: application to alkali feldspar
The temporal evolution of coherent lamellar microstructures is significantly influenced by their elastic properties, particularly when the exsolved phases are coherent. This research utilizes the Cahn–Hilliard model to examine the morphological and energetic evolution of binary alkali feldspar, integrating anisotropic elastic energy into the Gibbs energy equation. The Cahn–Hilliard model successfully simulated the orientation of lamellae observed in natural samples and the elastic strain was consistent with previous research. We also computed the coherent solvus from the annealing simulation of various precursor compositions and temperatures. The temperature difference (\(\Delta T\)) between the strain-free solvus and the coherent solvus was \(\Delta T = 85\,{}^\circ \text {C}\), which is slightly lower than previously reported values obtained from similar parameters. This discrepancy is likely due to the presence of non-planar lamellae at the onset of phase separation, which are more stable than planar ones. We also simulated the binodal curves of the coherent solvi for different precursor phase compositions. The computed solvi were not unique but varied depending on the precursor composition. Our model is flexible because it does not assume any specific shapes for the lamellar interfaces and is applicable to various coherent binary systems.
期刊介绍:
Contributions to Mineralogy and Petrology is an international journal that accepts high quality research papers in the fields of igneous and metamorphic petrology, geochemistry and mineralogy.
Topics of interest include: major element, trace element and isotope geochemistry, geochronology, experimental petrology, igneous and metamorphic petrology, mineralogy, major and trace element mineral chemistry and thermodynamic modeling of petrologic and geochemical processes.