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Crystal chemistry of Eu-bearing tuite synthesized at high-pressure and high-temperature conditions

机译:在高压和高温条件下合成欧盟元轴承的晶体化学

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摘要

Tuite, -Ca-3(PO4)(2), is a potential host for rare-earth elements in the deep mantle. Eu-bearing tuite single crystals with chemical formulas of Ca2.93Eu0.04(PO4)(2) and Ca2.88Eu0.07Na0.06(PO4)(2) were synthesized at 16 GPa and 1600 degrees C, and their structures were investigated at room temperature with single-crystal X-ray diffraction. The structure refinements of Eu-bearing tuite indicate the preference of Eu3+ for the smaller 6-coordinated Ca1 site with a coupled vacancy due to the substitution of 2Eu(3+)+3 Ca2+. In NaEu-bearing tuite, both Eu3+ and Na+ occupy the smaller 6-coordinated Ca1 site according to the coupled substitution of Eu3++Na(+)2 Ca2+. The presence of Na results in more Eu2O3 in NaEu-bearing tuite, because the coupled substitution is energetically more favorable. REE-bearing tuite could be found on the Moon and the deep Earth's mantle as a consequence of REE-bearing apatite or/and merrillite transformation under high-pressure and high-temperature conditions.
机译:Tuite,-CA-3(PO4)(2)是深层地幔中稀土元素的潜在主体。 含有Ca2.93EU0.04(PO4)(2)(2)和Ca2.88EU0.07NA0.06(PO4)(2)的化学式的欧盟元晶体在16GPA和1600摄氏度中合成,并研究了它们的结构 在室温下,用单晶X射线衍射。 Eu-轴承组的结构改进表明,由于2EU(3 +)+ 3Ca2 +的取代,较小的6配位Ca1位点的Eu3 +的偏好具有耦合空位。 在Naeu-uhibual Tuite中,根据Eu3 ++ Na(+)2 Ca2 +的偶联取代,Eu3 +和Na +占据较小的6个协调的CA1位点。 NA的存在导致Naeu承载元中的更多EU2O3,因为耦合替换是能量更有利的。 由于在高压和高温条件下,由于耐料磷灰石或/和美林转化,因此可以在月球和深地地幔上找到戒华。

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