Carbon deposition boundaries and other constant parameter curves, in the triangular representation of CHO equilibria, with applications to fuel cells

G.H.J. Broers, B.W. Treijtel
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引用次数: 29

Abstract

In the CHO system, at pressures of the order of 1 atm and temperatures between 400°K and 1500°K, the only important species present at true thermodynamic equilibrium are the simple molecules: C, CH4, CO, CO2, H2 and H2O (apart from excess O2).

This has recently been shown by Cairns, Tevebaugh and Holm [2], [3], who also introduced the very useful triangular representation of carbon deposition data in CHO diagrams.

It will be shown in this communication that carbon deposition boundaries and other curves of constant parameter values can be computed directly from three independent equations involving three equilibrium constants, and the balance equation: σ partial pressures = total pressure. No material balance equations and no trial and error procedures are needed, while the mathematical “problems” are confined to the solution of a quadratic equation as the most involved step.

Apart from carbon deposition boundaries, CH4 and H2O “isobars” and curves of constant reversible oxidation potential in fuel cells with O= transport and CO3= transport have been computed for temperatures of usual interest. The method has been outlined for each of these cases.

Some theoretical consequences of the trend for p(H2O) to remain constant in low or intermediate temperature fuel cells with aqueous electrolyte, have been pointed out in connection with the possibility of C deposition on highly active fuel electrodes.

An example pertinent to the use of the diagrams shown, is given in Appendix 2, where also the calculation of the complete equilibrium composition from CH4 isobars is discussed.

碳沉积边界和其他常数参数曲线,以三角形表示CHO平衡,应用于燃料电池
在CHO体系中,当压力为1atm,温度在400°K和1500°K之间时,处于真正热力学平衡的唯一重要物质是简单分子:C、CH4、CO、CO2、H2和H2O(除了过量的O2)。最近Cairns, Tevebaugh和Holm[2],[3]已经证明了这一点,他们还在CHO图中引入了非常有用的碳沉积数据的三角形表示。在这次通信中,我们将会看到,碳沉积边界和其他恒定参数值的曲线可以由三个独立的方程直接计算出来,这些方程包含三个平衡常数,平衡方程是:σ分压=总压。不需要物质平衡方程和试错过程,而数学“问题”仅限于二次方程的解,这是最复杂的步骤。除了碳沉积边界外,还计算了O=输运和CO3=输运燃料电池中CH4和H2O的“等压线”和恒定可逆氧化电位曲线。该方法已针对每种情况进行了概述。在含有水电解质的低温或中温燃料电池中p(H2O)保持恒定的趋势的一些理论后果,已经指出了C沉积在高活性燃料电极上的可能性。在附录2中给出了与所示图的使用有关的一个例子,其中还讨论了从CH4等压线计算完全平衡组成。
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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