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通过巨正则蒙特卡罗模拟研究303K下氢气在石墨狭缝孔中的存储。

Storage of hydrogen at 303 K in graphite slitlike pores from grand canonical Monte Carlo simulation.

作者信息

Kowalczyk Piotr, Tanaka Hideki, Hołyst Robert, Kaneko Katsumi, Ohmori Takumi, Miyamoto Junichi

机构信息

Department of Chemistry, Faculty of Science, Chiba University, 1-3 Yayoi, Chiba 263, Japan.

出版信息

J Phys Chem B. 2005 Sep 15;109(36):17174-83. doi: 10.1021/jp0529063.

Abstract

Grand canonical Monte Carlo (GCMC) simulations were used for the modeling of the hydrogen adsorption in idealized graphite slitlike pores. In all simulations, quantum effects were included through the Feynman and Hibbs second-order effective potential. The simulated surface excess isotherms of hydrogen were used for the determination of the total hydrogen storage, density of hydrogen in graphite slitlike pores, distribution of pore sizes and volumes, enthalpy of adsorption per mole, total surface area, total pore volume, and average pore size of pitch-based activated carbon fibers. Combining experimental results with simulations reveals that the density of hydrogen in graphite slitlike pores at 303 K does not exceed 0.014 g/cm(3), that is, 21% of the liquid-hydrogen density at the triple point. The optimal pore size for the storage of hydrogen at 303 K in the considered pore geometry depends on the pressure of storage. For lower storage pressures, p < 30MPa, the optimal pore width is equal to a 2.2 collision diameter of hydrogen (i.e., 0.65 nm), whereas, for p congruent with 50MPa, the pore width is equal to an approximately 7.2 collision diameter of hydrogen (i.e., 2.13 nm). For the wider pores, that is, the pore width exceeds a 7.2 collision diameter of hydrogen, the surface excess of hydrogen adsorption is constant. The importance of quantum effects is recognized in narrow graphite slitlike pores in the whole range of the hydrogen pressure as well as in wider ones at high pressures of bulk hydrogen. The enthalpies of adsorption per mole for the considered carbonaceous materials are practically constant with hydrogen loading and vary within the narrow range q(st) congruent with 7.28-7.85 kJ/mol. Our systematic study of hydrogen adsorption at 303 K in graphite slitlike pores gives deep insight into the timely problem of hydrogen storage as the most promising source of clean energy. The calculated maximum storage of hydrogen is equal to approximately 1.4 wt %, which is far from the United States Department of Energy (DOE) target (i.e., 6.5 wt %), thus concluding that the total storage amount of hydrogen obtained at 303 K in graphite slitlike pores of carbon fibers is not sufficient yet.

摘要

巨正则蒙特卡罗(GCMC)模拟被用于对理想化石墨狭缝形孔隙中氢气吸附的建模。在所有模拟中,通过费曼和希布斯二阶有效势纳入了量子效应。氢气的模拟表面过剩等温线用于确定总储氢量、石墨狭缝形孔隙中氢气的密度、孔径和孔体积分布、每摩尔吸附焓、总表面积、总孔体积以及沥青基活性炭纤维的平均孔径。将实验结果与模拟相结合表明,在303 K时石墨狭缝形孔隙中氢气的密度不超过0.014 g/cm³,即三相点处液氢密度的21%。在所考虑的孔隙几何结构中,303 K时储氢的最佳孔径取决于储存压力。对于较低的储存压力,p < 30MPa,最佳孔宽等于氢气的2.2个碰撞直径(即0.65 nm),而对于p ≈ 50MPa,孔宽等于氢气的约7.2个碰撞直径(即2.13 nm)。对于更宽的孔隙,即孔宽超过氢气的7.2个碰撞直径,氢气吸附的表面过剩是恒定的。在整个氢气压力范围内,量子效应在狭窄的石墨狭缝形孔隙中以及在大量氢气的高压下更宽的孔隙中都很重要。所考虑的含碳材料的每摩尔吸附焓实际上随氢气负载量而恒定,并且在q(st) ≈ 7.28 - 7.85 kJ/mol的狭窄范围内变化。我们对303 K时石墨狭缝形孔隙中氢气吸附的系统研究深入洞察了作为最有前途的清洁能源来源的储氢这一及时问题。计算得出的最大储氢量约为1.4 wt%,远未达到美国能源部(DOE)的目标(即6.5 wt%),因此得出结论,在303 K时碳纤维的石墨狭缝形孔隙中获得的氢气总储存量仍然不足。

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