Cheremisina Olga V, Ponomareva Maria A, Bolotov Victor A, Osipov Artyom S, Sitko Alexandr V
Saint Petersburg Mining University, 2, 21st Line, St Petersburg 199106, Russia.
ACS Omega. 2022 Jan 11;7(3):3007-3015. doi: 10.1021/acsomega.1c06037. eCollection 2022 Jan 25.
The work analyzes hydrogen sulfide sorption from model gas mixtures containing HS from 1.25 × 10 to 1.28 × 10 mol/L under static conditions at temperatures 253 and 298 K on the raw manganese ore of the Ulu-Telyak deposit (Bashkortostan, Russia), manganese(IV) oxide, and manganese(IV) and iron(III) oxide mixtures. The thermodynamic models for calculating the equilibrium constants and Gibbs energy changes were analyzed. The sorption isotherms were described by the Langmuir, Freundlich, Temkin, and Dubinin-Radushkevich models. The value of enthalpy of hydrogen sorption on the ore was -68.98 ± 3.45 kJ/mol and those on model mixtures Mn + FeO and MnO were ±12.20 kJ/mol and -103.826 ± 5.19 kJ/mol, respectively, and the entropies of the hydrogen sulfide sorption process on three manganese materials at 253 K were calculated. The limiting capacity values of manganese materials at 253 and 298 K were obtained. The morphological analysis of the ore samples, Mn + FeO, and MnO, before and after hydrogen sulfide sorption, was carried out at 253 K. The obtained thermodynamic parameters determine the advantage of using the raw manganese ore over pure oxides, which characterizes its effective practical application in the desulfurization process.
该工作分析了在253 K和298 K温度下,于静态条件下,从含硫化氢浓度为1.25×10至1.28×10摩尔/升的模拟气体混合物中,对乌卢-捷利亚克矿床(俄罗斯巴什科尔托斯坦)的原生锰矿石、二氧化锰以及二氧化锰与三氧化二铁混合物进行硫化氢吸附的情况。分析了用于计算平衡常数和吉布斯自由能变化的热力学模型。用朗缪尔、弗伦德里希、坦金和杜比宁-拉杜舍维奇模型描述了吸附等温线。矿石上硫化氢吸附的焓值为-68.98±3.45千焦/摩尔,模型混合物Mn + FeO和MnO上的分别为±12.20千焦/摩尔和-103.826±5.19千焦/摩尔,并且计算了三种锰材料在253 K下硫化氢吸附过程的熵。得到了锰材料在253 K和298 K下的极限容量值。在253 K下对硫化氢吸附前后的矿石样品、Mn + FeO和MnO进行了形态分析。所获得的热力学参数确定了使用原生锰矿石优于纯氧化物的优势,这表征了其在脱硫过程中的有效实际应用。