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Porosity and distribution of water in perlite from the island of Milos Greece

机译:希腊米洛斯岛珍珠岩中孔隙度和水的分布

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摘要

A perlite sample representative of an operating mine in Milos was investigated with respect to the type and spatial distribution of water. A set of different methods was used which finally provided a consistent view on the water at least in this perlite. Infrared spectroscopy showed the presence of different water species (molecular water and hydroxyl groups / strongly bound water). The presence of more than 0.5 mass% smectite, however, could be excluded considering the cation exchange capacity results. The dehydration measured by thermal analysis occurred over a wide range of temperatures hence confirming the infrared spectroscopical results. Both methods point to the existence of a continuous spectrum of water binding energies. The spatial distribution of water and/or pores was investigated using different methods (CT: computer tomography, FIB: scanning electron microscopy including focused ion beam technology, IRM: infrared microscopy). Computer tomography (CT) showed large macropores (20 – 100 μm) and additionally revealed a mottled microstructure of the silicate matrix with low density areas up to a few μm in diameter. Scanning electron microscopy (FIB) confirmed the presence of μm sized pores and IRM showed the filling of these pores with water. In summary, two types of pores were found. Airfilled 20 – 100 μm pores and μm-sized pores disseminated in the glass matrix containing at least some water. Porosity measurements indicate a total porosity of 26 Vol%, 11 Vol% corresponding to the μm-sized pores. It remains unsolved wether the water in the μm-sized pores entered after or throughout perlite formation. However, the pores are sealed and no indications of cracks were found which indicated a primary source of the water, i.e. water was probably entrapped by quenching of the lava. The water in these pores may be the main reason for the thermal expandability which results in the extraordinarily porous expanded perlite building materials.
机译:就水的类型和空间分布研究了代表米洛斯岛一个矿山的珍珠岩样品。使用了一组不同的方法,最终至少在此珍珠岩中对水有了一致的认识。红外光谱显示存在不同的水物种(分子水和羟基/强结合水)。但是,考虑到阳离子交换容量的结果,可以排除存在0.5质量%以上的蒙脱石。通过热分析测得的脱水发生在很宽的温度范围内,因此证实了红外光谱结果。两种方法都指出了水结合能的连续光谱。使用不同的方法(CT:计算机断层扫描,FIB:包括聚焦离子束技术的扫描电子显微镜,IRM:红外显微镜)研究了水和/或孔的空间分布。计算机断层扫描(CT)显示大孔(20 –100μm),并且还揭示了硅酸盐基质的斑驳的微观结构,其低密度区域的直径可达几微米。扫描电子显微镜(FIB)证实存在μm大小的孔,IRM显示这些孔被水填充。总之,发现了两种类型的孔。空气中弥散的20-100 µm孔和μm大小的孔散布在至少含有一些水的玻璃基质中。孔隙率测量表明总孔隙率为26 Vol%,对应于μm尺寸的孔隙为11 Vol%。在珍珠岩形成之后或整个珍珠岩形成过程中,进入微米级孔隙的水都无法溶解。但是,这些孔是密封的,没有发现裂纹的迹象表明是水的主要来源,也就是说,水可能是由于熔岩的淬灭而被夹带的。这些孔中的水可能是热膨胀性的主要原因,该热膨胀性导致产生异常多孔的膨胀珍珠岩建筑材料。

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