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WATER IN POROUS CARBONS: A SIMULATION STUDY

机译:多孔碳中的水:模拟研究

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摘要

We present a simulation study of the adsorption mechanism of water in a realistic carbon structure at 300 K. Water molecules are modeled using a recently developed fixed-point charge water model optimized to the vapor-liquid coexistence properties (Errington and Panagiotopoulos, 1998). Reverse Monte Carlo techniques (Thomson and Gubbins, 2000) are used to generate a realistic model of carbon pore morphologies composed of rigid, carbon basal plates. Arrangements of the carbon plates are driven by a systematic refinement of simulated C-C radial distribution functions to match experiment. The resulting pore morphology is generally non-slitlike and highly connected. The adsorption of water on activated (surface oxygen sites, =O) and non-activated (graphitic) carbon is investigated using the grand canonical Monte Carlo simulation method. The adsorption behavior is found to be strongly dependent on the presence of active sites with no appreciable adsorption in the graphitic carbon until the pressure is above the bulk saturation point. Additionally, water adsorption is found to increase as the active site density increases.
机译:我们提出了在300 K下真实碳结构中水的吸附机理的模拟研究。使用最新开发的定点电荷水模型对水分子进行建模,该模型针对气液共存特性进行了优化(Errington和Panagiotopoulos,1998)。反向蒙特卡洛技术(Thomson和Gubbins,2000年)用于生成由刚性碳基底板组成的真实碳孔隙形态模型。碳板的排列由模拟的C-C径向分布函数的系统优化驱动以匹配实验。所得的孔形态通常是非狭缝状且高度连通的。使用经典的蒙特卡洛模拟方法研究了水在活性碳(表面氧位= O)和非活性碳(石墨)上的吸附。发现吸附行为强烈地取决于活性位点的存在,直到压力高于本体饱和点之前,石墨碳中才没有明显的吸附。另外,发现随着活性位点密度的增加,水的吸附也增加。

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