蒙古天然沸石晶体结构研究

G. Batdemberel, S. Chadraabal, P. Jargalbat, D. Sangaa, B. Namjildorj
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引用次数: 0

摘要

利用电子显微镜(SEM)、x射线荧光(XRF)、x射线衍射(XRD)等方法对蒙古地区发现的沸石岩石进行了研究。SEM, XRF和XRD测量在德国斯图加特Max Plank研究所进行。我们的样品收集于蒙古的矿床:tagaan tsav, Tushig uul, Urgun矿床,Bayan Zurkh Black Mountain和Mandal ovoo。首先,我们用x射线荧光光谱法进行了化学元素分析,给出了所有沸石矿床样品的化学成分。对比上述5个矿床样品的钾含量,多诺戈壁土师山沸石中钾含量最高,可鉴定为钾斜发沸石- K (2.56 at %),其余为钾斜发沸石- Na。上述矿床样品的主要阳离子为K、Na、Ca、Mg、Fe、Ti。(Si Al)/O比值也表明蒙古沸石具有较好的品质。我们对Bruker-Axes D8型x射线粉末衍射仪进行了x射线相位分析研究,并利用≪Match!水晶冲击》节目。结果表明,这些沸石为Na型和K型斜沸石,具有单斜对称性(C2/m)。最后,斜发沸石的精确晶体化学式可写为:•(Na2.02, K1.81, Mg0.49, Ca0.46, Fe0.36)(Al6.28O30.45) (Si28.47O30.45)·z·H2O。•(K2.56, Na1.69, Mg0.64, Ca0.47, Fe0.78)(Al6.39O28.15) (Si31.17O28.15)·z·H2O•Urgun矿床样品(Na2.34, K1.48, Mg0.86, Ca0.57, Fe0.62)(Al7O29.03) (Si29.07O29.03)·z·H2O•(Na2.14, K1.64, Mg0.53, Fe0.64, Ti0.19)(Al6.38O28.95) (Si30.59O28.95)·z·H2O•(Na3.59, K1.17, Ca1.17, Mg0.68, Fe0.30)(Al6.58O28.90) (Si28.65O28.90)·z·H2O
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Crystal structural investigations of Mongolian natural zeolites
We have studied zeolitic rocks discovered in Mongolia using electron microscopy (SEM), X-ray fluorescence (XRF), X-ray diffraction (XRD) methods. SEM, XRF and XRD measurements were carried out in the Max Plank Institute of Stuttgart, Germany. Our samples are collected from Mongolian deposits: Tsagaan tsav, Tushig uul, Urgun deposit, Bayan Zurkh Black Mountain and Mandal ovoo. Firstly, we have made chemical element analysis by using X-ray fluorescence spectroscopy which gives chemical contents of samples from all zeolite deposits. Comparing contents of above 5 deposits samples shows us that zeolite of Tushig Mountain, Dornogobi, is has the highest content of potassium and can be identified in potassium clinoptilolite- K (2.56 at %), others belong to clinoptilolite- Na. The main cations are K,Na,Ca,Mg,Fe,Ti for all the samples from the above mentioned deposits. Also, the (Si Al)/O ratio shows that the Mongolian zeolites have comparatively good qualities. We made X-ray phase analysis study on X-ray powder diffractometer Bruker-Axes D8 and refined the X-ray diffraction spectra by using ≪Match! Crystal Impact≫ program. As a result, we established that these zeolites are Na and K type of clinoptilolite with monoclinic symmetry (C2/m). Finally, the exact crystallochemical formula of clinoptilolites can be written as the next: • (Na2.02, K1.81, Mg0.49, Ca0.46, Fe0.36)(Al6.28O30.45) (Si28.47O30.45)·z·H2O for Tsagaan tsav sample. • (K2.56, Na1.69, Mg0.64, Ca0.47, Fe0.78)(Al6.39O28.15) (Si31.17O28.15)·z·H2O for Tushig Mountain sample. • (Na2.34, K1.48, Mg0.86, Ca0.57, Fe0.62)(Al7O29.03) (Si29.07O29.03)·z·H2O for Urgun deposit sample. • (Na2.14, K1.64, Mg0.53, Fe0.64, Ti0.19)(Al6.38O28.95) (Si30.59O28.95)·z·H2O for Bayan Zurh Black Mountain sample. • (Na3.59, K1.17, Ca1.17, Mg0.68, Fe0.30)(Al6.58O28.90) (Si28.65O28.90)·z·H2O for Mandalovoo sample.
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