金红石
分压
氧气
Crystal(编程语言)
氧气压力
部分熔融
材料科学
结晶学
分析化学(期刊)
离子
矿物学
晶体生长
单晶
化学
地质学
色谱法
古生物学
有机化学
程序设计语言
地幔(地质学)
计算机科学
作者
Jong Kwan Park,Kyoung Hun Kim,Isao Tanaka,Kwang Bo Shim
标识
DOI:10.1016/j.jcrysgro.2004.04.105
摘要
Rutile single crystals with subgrain-boundary free were grown by a floating zone method (FZ) under two different specific oxygen partial pressure, 0.5 MPa and 1×103 Pa, and their structural and chemical properties were compared with each other. It was found that rutile crystals grown under the higher oxygen partial pressure experienced a melting growth behavior which produced bright and transparent crystals due to the concentration of interstitial Ti3+ ions, but rutile crystals grown under the lower oxygen partial pressure exhibited a deep dark color of the whole crystal due to their solid state growth behaviors.
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