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Nano-solids in manganese nodules from northern part of Pacific Ocean floor-—— Nano-solids in minerals and prospects of its uses in industry

机译:太平洋海底北部锰结核中的纳米固体———矿物质中的纳米固体及其在工业中的应用前景

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摘要

The study of the crystal structure and particle size of manganese nodules from the northern part of the Central Pacific Ocean floor indicates that besides the phases of todorokite, birnessite and 5-MnO with the crystallite size at the micron scale, there are many other multi-phase solids having particle Size at the nanometer scale. The chemical analysis, TEM study, Mb'ssbauer spectroscopy and differential thermal analysis show that they are mainly ferri-hydroxides with the short-range ordered structure similar to that of goethite and lepidocrocite. The small-angle X-ray scattering measurements indicate that the peak position of the particle size distribution is at 5—10 nm, hence the existence of nano-solids in minerals is confirmed.
机译:对中太平洋海床北部锰结核的晶体结构和粒径的研究表明,除了钙钛矿,水钠锰矿和5-MnO的微晶尺寸均在微米级的相外,还有许多其他的具有纳米级粒度的固相固体。化学分析,TEM研究,Mb'ssbauer光谱和差示热分析表明,它们主要是氢氧化铁,其短程有序结构类似于针铁矿和纤铁矿。 X射线小角散射测量表明,粒径分布的峰值位置在5-10 nm,因此可以确认矿物中存在纳米固体。

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