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Influence of smectite suspension structure on sheet orientation in dry sediments : XRD and AFM applications

机译:蒙脱石悬浮结构对干沉积物中片状取向的影响:XRD和AFM应用

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摘要

The structure-building phenomena within clay aggregates are governed by forces acting between clay particles. Measurements of such forces are important to understand in order to manipulate the aggregate structure for applications such as dewatering of mineral processing tailings. A parallel particle orientation is required when conducting XRD investigation on the oriented samples and conduct force measurements acting between basal planes of clay mineral platelets using at. force microscopy (AFM). To investigate how smectite clay platelets were oriented on silicon wafer substrate when dried from suspension range of methods like SEM, XRD and AFM were employed. From these investigations, we conclude that high clay concns. and larger particle diams. (up to 5 μm) in suspension result in random orientation of platelets in the substrate. The best possible laminar orientation in the clay dry film, represented in the XRD 0 0 1/0 2 0 intensity ratio of 47 was obtained by drying thin layers from 0.02 wt.% clay suspensions of the natural pH. Conducted AFM investigations show that smectite studied in water based electrolytes show very long-range repulsive forces lower in strength than electrostatic forces from double-layer repulsion. It was suggested that these forces may have structural nature. Smectite surface layers rehydrate in water environment forms surface gel with spongy and cellular texture which cushion approaching AFM probe. This structural effect can be measured in distances larger than 1000 nm from substrate surface and when probe penetrate this gel layer, structural linkages are forming between substrate and clay covered probe. These linkages prevent subsequently smooth detachments of AFM probe on way back when retrieval. This effect of tearing new formed structure apart involves larger adhesion-like forces measured in retrieval. It is also suggested that these effect may be enhanced by the nano-clay particles interaction.
机译:粘土骨料中的结构建立现象受粘土颗粒之间作用的力控制。为了操作诸如矿物质加工尾矿的脱水之类的应用而操纵骨料结构,了解这种力的测量很重要。当对定向样品进行XRD研究并使用at进行粘土矿物血小板基面之间的力测量时,需要平行的颗粒取向。力显微镜(AFM)。为了研究当从悬浮液范围干燥后,如SEM,XRD和AFM之类的方法,蒙脱石粘土薄片如何在硅晶片基底上取向。从这些调查,我们得出结论,高粘土含量。和更大的颗粒直径。 (最大5μm)的悬浮液会导致血小板在基质中随机取向。通过从0.02重量%的天然pH的粘土悬浮液中干燥薄层,获得了以47的XRD 0 0 1/0 2 0强度比表示的在粘土干膜中的最佳层流取向。进行的原子力显微镜研究表明,在水基电解质中研究的蒙脱石显示出很强的远距离排斥力,其强度低于双层排斥产生的静电力。有人认为这些力量可能具有结构性。在水环境中复水的蒙脱石表面层形成具有海绵状和蜂窝状结构的表面凝胶,从而缓冲了接近AFM探针的能力。可以在距基材表面大于1000 nm的距离中测量这种结构效果,当探针穿透该凝胶层时,基材和粘土覆盖的探针之间就会形成结构联系。这些联动装置可防止AFM探针随后在取回时顺畅脱离。撕开新形成的结构的这种效果涉及在回收中测得的较大的类似粘附力。还建议可以通过纳米粘土颗粒的相互作用来增强这些效果。

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  • 作者

    Frost Ray L.; Zbik Marek;

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  • 年度 2010
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  • 原文格式 PDF
  • 正文语种 {"code":"en","name":"English","id":9}
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