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在潮湿环境中用原子力显微镜和 X 射线光电子能谱研究 NO2 在 CaCO3(1014)表面的反应。

Atomic force microscopy and X-ray photoelectron spectroscopy study of NO2 reactions on CaCO3 (1014) surfaces in humid environments.

机构信息

Departments of Chemistry and Chemical and Biochemical Engineering, University of Iowa , Iowa City Iowa 52242, United States.

出版信息

J Phys Chem A. 2012 Sep 13;116(36):9001-9. doi: 10.1021/jp305122d. Epub 2012 Sep 4.

Abstract

In this study, alternating current (AC) mode atomic force microscopy (AFM) combined with phase imaging and X-ray photoelectron spectroscopy (XPS) were used to investigate the effect of nitrogen dioxide (NO2) adsorption on calcium carbonate (CaCO3) (101̅4) surfaces at 296 K in the presence of relative humidity (RH). At 70% RH, CaCO3 (101̅4) surfaces undergo rapid formation of a metastable amorphous calcium carbonate layer, which in turn serves as a substrate for recrystallization of a nonhydrated calcite phase, presumably vaterite. The adsorption of nitrogen dioxide changes the surface properties of CaCO3 (101̅4) and the mechanism for formation of new phases. In particular, the first calcite nucleation layer serves as a source of material for further island growth; when it is depleted, there is no change in total volume of nitrocalcite, Ca(NO3)2, particles formed whereas the total number of particles decreases. This indicates that these particles are mobile and coalesce. Phase imaging combined with force curve measurements reveals areas of inhomogeneous energy dissipation during the process of water adsorption in relative humidity experiments, as well as during nitrocalcite particle formation. Potential origins of the different energy dissipation modes within the sample are discussed. Finally, XPS analysis confirms that NO2 adsorbs on CaCO3 (101̅4) in the form of nitrate (NO3(-)) regardless of environmental conditions or the pretreatment of the calcite surface at different relative humidity.

摘要

在这项研究中,交流(AC)模式原子力显微镜(AFM)结合相衬成像和 X 射线光电子能谱(XPS)被用来研究在相对湿度(RH)存在的情况下,二氧化氮(NO2)吸附对碳酸钙(CaCO3)(101̅4)表面的影响。在 70% RH 下,CaCO3(101̅4)表面会迅速形成一种亚稳态无定形碳酸钙层,这反过来又成为非水合方解石相(可能是文石)再结晶的基底。二氧化氮的吸附改变了 CaCO3(101̅4)的表面性质和新相形成的机制。特别是,第一方解石成核层作为进一步岛状生长的物质来源;当它耗尽时,形成的硝钙石,Ca(NO3)2,颗粒的总体积没有变化,而颗粒的总数减少。这表明这些颗粒是可移动的并且会合并。相衬成像结合力曲线测量揭示了在相对湿度实验中水分吸附过程中以及在硝钙石颗粒形成过程中存在的不均匀能量耗散区域。还讨论了样品内不同能量耗散模式的潜在起源。最后,XPS 分析证实,NO2 以硝酸盐(NO3(-))的形式吸附在 CaCO3(101̅4)上,无论环境条件如何,或者在不同相对湿度下对方解石表面的预处理如何。

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