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首页> 外文期刊>Geochemical Transactions >Friction characteristics of Cd-rich carbonate films on calcite surfaces: implications for compositional differentiation at the nanometer scale
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Friction characteristics of Cd-rich carbonate films on calcite surfaces: implications for compositional differentiation at the nanometer scale

机译:方解石表面富镉碳酸盐薄膜的摩擦特性:对纳米尺度成分差异的影响

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Lateral Force Microscopy (LFM) studies were carried out on cleaved calcite sections in contact with solutions supersaturated with respect to otavite (CdCO3) or calcite-otavite solid solutions (SS) as a means to examine the potential for future application of LFM as a nanometer-scale mineral surface composition mapping technique. Layer-by-layer growth of surface films took place either by step advancement or by a surface nucleation and step advancement mechanisms. Friction vs. applied load data acquired on the films and the calcite substrate were successfully fitted to the Johnson Kendall Roberts (JKR) model for single asperity contacts. Following this model, friction differences between film and substrate at low loads were dictated by differences in adhesion, whereas at higher load they reflect differences in contact shear strength. In most experiments at fixed load, the film showed higher friction than the calcite surface, but the friction-load dependence for the different surfaces revealed that at low loads (0–40 nN), a calcian otavite film has lower friction than calcite; a result that is contrary to earlier LFM reports of the same system. Multilayer films of calcian-otavite displayed increasing friction with film thickness, consistent with the expectation that the film surface composition will become increasingly Cd-rich with increasing thickness. Both load- and thickness-dependence trends support the hypothesis that the contact shear strength correlates with the hydration enthalpy of the surface ions, thereby imparting friction sensitivity in the LFM to mineral-water interface composition.
机译:在与方解石(CdCO3)或方解石-方解石固溶体(SS)相比过饱和的溶液接触的解理方解石切片上进行了横向力显微镜(LFM)研究,以此作为检查将来将LFM作为纳米材料应用的潜力的一种方法尺度矿物表面成分测绘技术。表面膜的逐层生长是通过逐步推进或通过表面成核和逐步推进机理进行的。在薄膜和方解石基板上获得的摩擦力与外加载荷数据已成功拟合到Johnson Kendall Roberts(JKR)模型中,用于单次粗糙接触。根据该模型,在低负载下薄膜与基材之间的摩擦力差异取决于粘附力的差异,而在较高负载下它们反映的是接触剪切强度的差异。在大多数固定载荷实验中,薄膜的摩擦力均比方解石表面高,但不同表面的摩擦载荷相关性表明,在低载荷(0–40 nN)下,方解石卵石膜的摩擦力比方解石低。结果与同一系统的早期LFM报告相反。氧化钙钙石的多层膜显示出随着膜厚度的增加的摩擦,这与膜表面组成将随着厚度增​​加而变得越来越富含Cd的期望相一致。载荷和厚度依赖性趋势均支持以下假设:接触剪切强度与表面离子的水合焓相关,从而在LFM中赋予矿泉水界面成分以摩擦敏感性。

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