铬
无水的
热重分析
化学
分析化学(期刊)
背景(考古学)
蒸发
质谱法
无机化学
热力学
有机化学
色谱法
生物
物理
古生物学
作者
Emna Mannei,Esther Asedegbega–Nieto,Faouzi Ayari
标识
DOI:10.1016/j.tca.2021.179102
摘要
Anhydrous CrCl3∙εH2O exhibited, under helium stream (6 L h–1, 5 K min–1), several transformations between room temperature and (1175 ± 2) K. The compound loses the physisorbed water molecules between (300 ± 2) K and (400 ± 2) K and the hydration degree (ε) was determined by thermogravimetry to be 0.14. However, using mass spectrometry, we were able to detect the transformation of CrCl3(cr) into CrCl3(g) at T = (776.00 ± 0.01) K. In this context, ΔsubH (776 K) value was estimated using some literature data and the Clausius-Clapeyron relation to be (245.20 ± 0.01) kJ mol–1. This value was corrected at (298.15 ± 0.01) K and (0.105 ± 0.01) MPa, resulting in (254.93 ± 0.01) kJ mol–1. Our thermodynamic calculations revealed that CrCl3(g) is decomposed into CrCl2(cr) and Cl2(g) within two distinct temperature ranges: (776 ± 2) to (860 ± 2) K and (950 ± 2) K to (1050 ± 2) K. Between (860 ± 2) and (950 ± 2) K, the evaporation of CrCl2(cr) in the form of CrCl4(g) takes place due to the presence of Cl2(g). However, at higher temperatures (T > 1050 K), residual CrCl2(cr) is evaporated and a final mass loss of 94 % is obtained.
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