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首页> 外文期刊>Acta Crystallographica, Section B. Structural Science >Crystal chemistry of mimetite, Pb-10(AsO4 )(6)Cl1.48O0.26, and finnemanite, Pb-10(AsO3)(6)Cl-2
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Crystal chemistry of mimetite, Pb-10(AsO4 )(6)Cl1.48O0.26, and finnemanite, Pb-10(AsO3)(6)Cl-2

机译:蒙脱石Pb-10(AsO4)(6)Cl1.48O0.26和芬锰矿Pb-10(AsO3)(6)Cl-2的晶体化学

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摘要

The crystal chemistries of synthetic mimetite, Pb-10(As5+O4)(6)(Cl2-xOx/2), a neutral apatite, and finnemanite, Pb-10(As3+O3)(6)Cl-2, a reduced apatite, were characterized using a combination of X-ray powder diffraction, neutron diffraction, transmission electron microscopy and X-ray photoelectron spectroscopy. Both phases conform to hexagonal P6(3)/m symmetry; however, the temperature-driven transformation of clinomimetite to mimetite described earlier was not confirmed. The average mimetite structure is best described through the introduction of partially occupied oxygen sites. A better understanding of the mixed arsenic speciation in apatites can guide the formulation of waste form ceramics and improve models of long-term durability after landfill disposal.
机译:合成蒙脱石Pb-10(As5 + O4)(6)(Cl2-xOx / 2),中性磷灰石和非锰铁矿Pb-10(As3 + O3)(6)Cl-2的晶体化学磷灰石通过X射线粉末衍射,中子衍射,透射电子显微镜和X射线光电子能谱进行了表征。这两个相位均符合六边形P6(3)/ m对称性;但是,尚未证实之前所述的温铁硅铁矿向钛铁矿的温度驱动转变。通过引入部分被占据的氧位点可以最好地描述平均陨石结构。更好地了解磷灰石中混合砷形态可以指导陶瓷废料的配制,并改善垃圾填埋场处理后的长期耐久性模型。

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