温度介于 (260 和 350) K 之间、压力介于 (0.5 和 20) MPa 之间的两种二元($N_{2}$ + $H_{2}$)混合物的声速数据和声学病毒系数

José J. Segovia, Daniel Lozano-Martín, Dirk Tuma, Alejandro Moreau, M. Carmen Martín, David Vega-Maza
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摘要

这项工作旨在解决与氢气混合气体的热力学特性有关的技术问题,以便将氢气作为一种新的能源载体。为此,利用现有最精确的技术,即球形声共振,对氮和氢的两种二元混合物的气态和超临界相进行了新的声速实验测量,得出实验扩展($k$ = 2)的不确定性仅为 10^{6}$ 中的 220 份(0.022%)。测量的压力范围在 0.5 至 20 兆帕(MPa)之间,温度范围在 260 至 350 开氏度(K)之间,氢气的标称摩尔百分比在 5 至 10 摩尔(mol%)之间。根据声速数据集推导出了与混合物特性相关的热物理性质,即第二$\beta_{a}$ 和第三$\gamma_{a}$ 声学维里系数。这些结果与已建立的适用于氮氢混合物的参考混合物模型,如 AGA8-DC92 EoS、GERG-2008 EoS 和最近开发的 GERG-2008 EoS 的改编版(后称为 GERG-$H_{2}$_proved EoS)进行了全面的比较和讨论。我们特别关注了氢浓度对这些特性的影响,结果表明,在大多数测量条件下,只有 GERG-$H_{2}$_proved EoS 与实验不确定性范围内的数据集保持一致。
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Speed of sound data and acoustic virial coefficients of two binary ($N_{2}$ + $H_{2}$) mixtures at temperatures between (260 and 350) K and at pressures between (0.5 and 20) MPa
This work aims to address the technical concerns related to the thermodynamic characterization of gas mixtures blended with hydrogen for the implementation of hydrogen as a new energy vector. For this purpose, new experimental speed of sound measurements have been done in gaseous and supercritical phases of two binary mixtures of nitrogen and hydrogen using the most accurate technique available, i.e., the spherical acoustic resonator, yielding an experimental expanded ($k$ = 2) uncertainty of only 220 parts in $10^{6}$ (0.022%). The measurements cover the pressure range between (0.5 and 20) MPa, the temperature range between (260 and 350) K, and the composition range with a nominal mole percentage of hydrogen of (5 and 10) mol%, respectively. From the speed of sound data sets, thermophysical properties that are relevant for the characterization of the mixture, namely the second $\beta_{a}$ and third $\gamma_{a}$ acoustic virial coefficients, are derived. These results are thoroughly compared and discussed with the established reference mixture models valid for mixtures of nitrogen and hydrogen, such as the AGA8-DC92 EoS, the GERG-2008 EoS, and the recently developed adaptation of the GERG-2008 EoS, here denoted GERG-$H_{2}$_improved EoS. Special attention has been given to the effect of hydrogen concentration on those properties, showing that only the GERG-$H_{2}$_improved EoS is consistent with the data sets within the experimental uncertainty in most measuring conditions.
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