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无序地的连贯溶液:实验,原子探头断层扫描和热力学模型
D Heuser1, R Dubosq2, E Petrishcheva1
1Department of Lithospheric Research, University of Vienna, Vienna, Austria.
概括
地的溶解会产生纳米级的片. 研究人员通过实验确定并理论建模了这些相互生长的连贯solvus,发现了很好的协议. 这项工作澄清了溶解的性地中相位平衡.
科学领域:
- 矿物学是一门学科.
- 地质化学 地质化学
- 材料科学 材料科学 材料科学
背景情况:
- 性地在高温 (>600°C) 时呈现连续固体溶液.
- 在较低的温度下,混合性差距会导致溶解成富含Na和富含K的片.
- 这些叶片的连贯相互生长涉及由于格子参数差异的弹性应变.
研究的目的:
- 为了实验性地确定性地中的连贯溶液.
- 从理论上建模连贯的溶液,并结合弹性应变能量.
- 对实验数据进行热力学模型的验证,以获得连贯的解决方案.
主要方法:
- 将中介成分的均地烧成两相区域.
- 产生连贯的相互生长与10-20纳米宽的叶片.
- 使用原子探头断层扫描分析状组成.
- 使用热力学混合模型计算连贯溶液,同时考虑弹性应变.
主要成果:
- 实验性地产生了性地酸盐片的连贯交织.
- 通过原子探头断层扫描分析确定了连贯溶液上的特定点.
- 在实验确定和计算一致的解决方案之间取得了很好的一致性.
- 证明了热力学模型对于描述相位平衡在连贯的相互生长中的充分性.
结论:
- 地中的连贯溶液已经通过实验和计算准确地确定.
- 热力学模型有效地描述了连贯溶解的地中的相位平衡.
- 这为解释地质样本中的相位关系提供了一个强大的框架,具有连贯的出溶结构.
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