首页> 外文会议>Interfacial Phenomena in Fine Particle Technology >THE ANISOTROPIC CHARACTER OF TALC SURFACES AS REVEALED BY STREAMING POTENTIAL MEASUREMENTS, ATOMIC FORCE MICROSCOPY, AND MOLECULAR DYNAMICS SIMULATIONS
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THE ANISOTROPIC CHARACTER OF TALC SURFACES AS REVEALED BY STREAMING POTENTIAL MEASUREMENTS, ATOMIC FORCE MICROSCOPY, AND MOLECULAR DYNAMICS SIMULATIONS

机译:滑行电位测量,原子力显微镜和分子动力学模拟显示滑石表面的各向异性

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A study of the interfacial properties of the basal plane and the edge surfaces of talc is described in this paper. The isoelectric point measured at the two different crystallographic planes by the streaming potential method was found to be similar and exists at about pH 3.0. In the case of the edge surface the zeta potential increases at higher pH values which can be attributed to the hydration of magnesium ions at the edge surface. The atomic force microscopy (AFM) colloidal probe technique was used to measure interaction forces. For such experiments a 20 μm talc particle was attached to the AFM cantilever and forces between the edge of the talc particle and two different crystallographic planes of talc were measured at various pH values. These measurements, while being qualitative due to the poorly characterized contact area, show differences between the properties of the base plane and edge of the talc and correspond to the results from streaming potential measurements. Finally, the differences in the hydration of the basal plane and the edge of talc are revealed from molecular dynamics (MD) simulations. The basal plane of the talc is much less hydrated than the edge, as can be seen from the water density distribution functions, which correlate quite well with the contact angle measurements at the basal plane surface and the edge surface of the talc sample.
机译:本文描述了对滑石基面和边缘表面的界面性质的研究。发现通过流动电势法在两个不同的晶体学平面上测得的等电点相似并且存在于约pH 3.0下。在边缘表面的情况下,ζ电势在较高的pH值下增加,这可以归因于镁离子在边缘表面的水合。原子力显微镜(AFM)胶体探针技术用于测量相互作用力。对于此类实验,将20μm滑石颗粒附着到AFM悬臂上,并在各种pH值下测量滑石颗粒边缘与两个不同滑石结晶平面之间的力。这些测量虽然由于接触区域的特征较差而定性,但显示出基面和滑石边缘的特性之间的差异,并且与流电势测量的结果相对应。最后,从分子动力学(MD)模拟揭示了基面和滑石边缘水合的差异。从水密度分布函数可以看出,滑石的基面比边缘的水合少得多,水密度分布函数与滑石样品的基面和边缘表面的接触角测量值非常相关。

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