首页> 外文期刊>Hallesches Jahrbuch fur Geowissenschaften, Reihe B. Geologie, Palaontologie, Mineralogie >Sodalite-like layer structures in the series 4CaO*3Al203*3H20 —4CaO~*3Ga_2O_3~*3H2_O,and their three-dimensional sodalite-typedehydration products: The first gallate–sodalite established.
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Sodalite-like layer structures in the series 4CaO*3Al203*3H20 —4CaO~*3Ga_2O_3~*3H2_O,and their three-dimensional sodalite-typedehydration products: The first gallate–sodalite established.

机译:4CaO * 3Al2O3 * 3H20_4CaO〜* 3Ga_2O_3〜* 3H2_O系列中的方钠石状层状结构及其三维方钠石型脱水产物:建立了第一个镓酸盐-苏打石。

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Aluminate sodalites have been known for quite a long time, and received some attention because oftheir wealth of structural phase transitions and modulated phases. The preparation of gallate sodalitesremained a challenge. We have now succeeded in the preparation, and characterization, of mixedaluminate-gallate and of pure gallate sodalites. In order to do so we had to employ a three-stepprocedure. First, oxide precursors were prepared in the right stoichiometry which were then transformed hydrothermally into members of the solid solution series 4CaO*3Al203*3H20 —4CaO*3Ga203*3H20. Finally, three-dimensional sodalites were obtained by careful dehydration. The intermediate products formed were studied by X-ray powder diffraction, electron microprobe analysisand FTIR spectroscopy, and it was found that they all have structures which can be described asinterrupted sodalite structures, or perhaps more appropriately as layered sodalites. No miscibility-gapswere observed in the series of eleven compounds, and the IR-spectra, lattice parameters and bondlengths in the solid solution series vary smoothly with composition. The volume increase from the Al-to the Ga-endmember is -5.4 %, the average T-0-bond length increases linearly from 1.75(1) A forthe aluminate to 1.84(1) A for the gallate.
机译:铝酸盐方钠石早已为人所知,并且由于其丰富的结构相变和调制相而受到关注。没食子酸钠方钠石的制备仍然是一个挑战。现在,我们已经成功制备和表征了混合铝酸镓盐和纯没食子钠方钠石。为此,我们必须采用三步过程。首先,以正确的化学计量制备氧化物前体,然后将其水热转化为固溶体系列4CaO * 3Al2O3 * 3H20-4CaO * 3Ga2O3 * 3H20的成员。最后,通过仔细脱水获得三维方钠石。通过X射线粉末衍射,电子探针分析和FTIR光谱对形成的中间产物进行了研究,发现它们都具有可以描述为间断的方钠石结构的结构,或者可能更适合作为层状方钠石。在这11种化合物的系列中未观察到混溶间隙,并且固溶体系列中的IR光谱,晶格参数和键长随组成的变化而变化。从Al端到Ga端的体积增加为-5.4%,平均T-0键长度从铝酸盐的1.75(1)A线性增加至没食子酸酯的1.84(1)A。

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