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首页> 外文期刊>Journal of the American Chemical Society >Dehydration-Induced Water Disordering in a Synthetic Potassium Gallosilicate Natrolite
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Dehydration-Induced Water Disordering in a Synthetic Potassium Gallosilicate Natrolite

机译:人工合成的镓硅酸钾钠沸石中的失水引起的失水

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摘要

A new potassium gallosilicate zeolite with a natrolite topology (approximate formula K_(8.2)Ga_(8.2)-Si_(11.8)O_(40)·11.5H_2O) was synthesized under hydrothermal conditions and characterized as a function of temperature using monochromatic synchrotron X-ray powder diffraction and Rietveld analyses. Unlike the previously known tetragonal K_8Ga_8Si_(12)O_(40)·6H_2O phase, the as-synthesized material contains twice the amount of water molecules in an ordered arrangement throughout the channels in an orthorhombic (I2_12_12_1) symmetry. The ordered configuration of water molecules is stabilized below 300 K, whereas heating above 300 K results in a selective dehydration and subsequent disordering of water molecules in a tetragonal (/42d) symmetry. Above 400 K, the material transforms to a fully dehydrated tetragonal phase with a concomitant volume reduction of ca. 15%. The fully dehydrated material transforms back to its original state when rehydrated over a period of up to 2 weeks. The distribution of potassium cations within the channels remains largely unperturbed during the water rearrangements and their order-disorder transition within the channels.
机译:在水热条件下合成了一种新的具有钠沸石结构的镓硅酸钾沸石(分子式为K_(8.2)Ga_(8.2)-Si_(11.8)O_(40)·11.5H_2O),并使用单色同步加速器X-表征了温度的函数。射线粉末衍射和Rietveld分析。与先前已知的四方K_8Ga_8Si_(12)O_(40)·6H_2O相不同,初生材料在正交晶格(I2_12_12_1)的整个通道中以有序排列的方式包含两倍数量的水分子。水分子的有序构型在300 K以下稳定,而在300 K以上加热会导致选择性脱水,随后水分子呈四方(/ 42d)对称性紊乱。高于400 K,该材料转变为完全脱水的四方相,并伴随着体积的减少。 15%。完全脱水的材料在长达2周的时间内重新脱水后,会变回其原始状态。在水重排及其在通道内的有序-无序过渡过程中,通道内钾阳离子的分布在很大程度上不受干扰。

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