Speciation and hydration forces in sodium carbonate/bicarbonate aqueous solutions nanoconfined between mica sheets.

IF 3.1 3区 化学 Q2 CHEMISTRY, PHYSICAL
Daria Turculet, Shurui Miao, Kieran J Agg, Susan Perkin
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Abstract

The equilibrium between hydrated and hydrolysed forms of CO2 in water is central to a multitude of processes in geology, oceanography and biology. Chemistry of the carbonate system is well understood in bulk solution, however processes such as mineral weathering and biomineralisation frequently occur in nano-confined spaces where carbonate chemistry is less explored. For confined systems, the speciation equilibria are expected to tilt due to surface reactivity, electric fields and reduced configurational entropy. In this discussion paper we provide measurements of interaction force between negatively charged aluminosilicate (mica) sheets across aqueous carbonate/bicarbonate solutions confined to nanoscale films in equilibrium with a reservoir of the solution. By fitting the measurements to a Poisson-Boltzmann equation modified to account for charge regulation at the bounding walls, we discuss features of the bicarbonate speciation in confinement. We find that (i) the presence of bicarbonate in the bulk reservoir causes a repulsive excess pressure in the slit compared to pH-neutral salt solutions at the same concentration, arising from a higher (negative) effective charge on the mica surfaces; (ii) the electrostatic screening length is lower for solutions of Na2CO3 compared to NaHCO3 at the same bulk concentration, due to a shift in the speciation equilibria with pH and in accordance with Debye-Hückel theory; (iii) hydration forces are observed at distances below 2 nm with features of size 0.1 nm and 0.3 nm; this was reproducible across the various bicarbonate electrolytes studied, and contrasts with hydration forces of uniform step size measured in pH-neutral electrolytes.

纳米云母片之间碳酸钠/碳酸氢钠水溶液的形态和水合力。
水中水合和水解形式的二氧化碳之间的平衡对地质学、海洋学和生物学的众多过程至关重要。碳酸盐体系的化学性质在散装溶液中得到了很好的理解,然而,矿物风化和生物矿化等过程经常发生在纳米密闭空间中,对碳酸盐化学的探索较少。对于受限系统,由于表面反应性、电场和减少的构型熵,物种形成平衡预计会倾斜。在这篇讨论论文中,我们提供了带负电荷的铝硅酸盐(云母)片之间的相互作用力的测量,这些相互作用力被限制在纳米级薄膜的碳酸盐岩/碳酸氢盐水溶液中,与溶液的储层处于平衡状态。通过将测量结果拟合到修正后的泊松-玻尔兹曼方程中,以考虑边界壁上的电荷调节,我们讨论了约束中碳酸氢盐形态形成的特征。我们发现(i)与相同浓度的ph中性盐溶液相比,块状储层中碳酸氢盐的存在导致狭缝中的排斥性超压,这是由云母表面上较高的(负)有效电荷引起的;(ii)与NaHCO3溶液相比,相同体积浓度下Na2CO3溶液的静电筛选长度较短,这是由于物质形态平衡随pH值的变化而改变,并且符合debye - hckel理论;(iii)水合力在距离小于2 nm处观察到,特征尺寸为0.1 nm和0.3 nm;这在研究的各种碳酸氢盐电解质中是可重复的,并与ph中性电解质中测量的均匀步长水合力形成对比。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Faraday Discussions
Faraday Discussions 化学-物理化学
自引率
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发文量
259
期刊介绍: Discussion summary and research papers from discussion meetings that focus on rapidly developing areas of physical chemistry and its interfaces
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