TY - JOUR
T1 - Corrigendum to “Radiolytic evaluation of select sulfur chlorides (S2Cl2 and SOCl2) for advanced low temperature chlorination of zirconium-based used nuclear fuel cladding” [Radiat. Phys. Chem. 206 110732] (Radiation Physics and Chemistry (2023) 206, (S0969806X22007952), (10.1016/j.radphyschem.2022.110732))
AU - Conrad, Jacy K.
AU - Woods, Michael E.
AU - Horne, Gregory P.
N1 - Publisher Copyright:
© 2024 Elsevier Ltd
PY - 2024/7
Y1 - 2024/7
N2 - In our original article, the Raman-active S2Cl2 and SOCl2 radiolysis product at 516 cm−1 in Figures 1 and 3 was assigned to Cl2, as this closely matched gas-phase density functional theory (DFT) predictions, and no additional peaks at other Raman shifts were observed at that time to indicate other radiolysis products. However, the spectrum of Cl2 in S2Cl2 is typically seen as two peaks at slightly higher wavenumbers than predicted: 536 and 542 cm−1 vs. 516 cm−1, respectively (Steudel et al., 1987). The two vibrational peaks are from the Cl–Cl bond stretch in Cl2 for 35Cl–35Cl and 35Cl–37Cl. Therefore, we now believe that our initial assignment for the peak at 516 cm−1 was incorrect. The in-growth of Cl2 is observed during the irradiation of SOCl2, as indicated by the two Raman peaks at 538 and 545 cm−1 in Figure 3. The observed degradation product at 516 cm−1 in both S2Cl2 and SOCl2 is likely sulfur dichloride (SCl2), which has a known Raman spectrum with two strong vibrational modes at 208 and 517 cm−1 (Steudel et al., 1987). The mode at 208 cm−1 is beneath strong vibrational modes for S2Cl2 and SOCl2, and thus, was likely masked in our study by the parent compounds. The DFT calculated spectrum of SCl2 was given in the original Supplementary Information (SI) as Figure S19 and is reproduced below. The calculated mode at 485 cm−1 is very weak (Steudel et al., 1987).[Formula presented] It is known that SCl2 is formed in an equilibrium with the parent compound in the presence of dissolved Cl2 (Weil and Sandler, 2000): S2Cl2 + Cl2 ⇌ 2SCl2, K = 77 at 18 °C. Therefore, even though Cl2 does not appear in our S2Cl2 Raman spectra as we previously thought, it may have been initially formed by a mechanism consistent with our reported results and reacted with the parent compound to yield SCl2 according to Eq. (1). The small amount of Cl2 remaining in the solution could also have been masked by the S–S stretch of S2Cl2 at 539 cm−1, especially considering the weak Raman effect of elemental chlorine (Steudel et al., 1987). Jacy K. Conrad: Conceptualization, Formal analysis, Investigation, Methodology, Validation, Writing – original draft. Michael E. Woods: Investigation, Writing – review & editing. Gregory P. Horne: Conceptualization, Funding acquisition, Supervision, Writing – original draft.
AB - In our original article, the Raman-active S2Cl2 and SOCl2 radiolysis product at 516 cm−1 in Figures 1 and 3 was assigned to Cl2, as this closely matched gas-phase density functional theory (DFT) predictions, and no additional peaks at other Raman shifts were observed at that time to indicate other radiolysis products. However, the spectrum of Cl2 in S2Cl2 is typically seen as two peaks at slightly higher wavenumbers than predicted: 536 and 542 cm−1 vs. 516 cm−1, respectively (Steudel et al., 1987). The two vibrational peaks are from the Cl–Cl bond stretch in Cl2 for 35Cl–35Cl and 35Cl–37Cl. Therefore, we now believe that our initial assignment for the peak at 516 cm−1 was incorrect. The in-growth of Cl2 is observed during the irradiation of SOCl2, as indicated by the two Raman peaks at 538 and 545 cm−1 in Figure 3. The observed degradation product at 516 cm−1 in both S2Cl2 and SOCl2 is likely sulfur dichloride (SCl2), which has a known Raman spectrum with two strong vibrational modes at 208 and 517 cm−1 (Steudel et al., 1987). The mode at 208 cm−1 is beneath strong vibrational modes for S2Cl2 and SOCl2, and thus, was likely masked in our study by the parent compounds. The DFT calculated spectrum of SCl2 was given in the original Supplementary Information (SI) as Figure S19 and is reproduced below. The calculated mode at 485 cm−1 is very weak (Steudel et al., 1987).[Formula presented] It is known that SCl2 is formed in an equilibrium with the parent compound in the presence of dissolved Cl2 (Weil and Sandler, 2000): S2Cl2 + Cl2 ⇌ 2SCl2, K = 77 at 18 °C. Therefore, even though Cl2 does not appear in our S2Cl2 Raman spectra as we previously thought, it may have been initially formed by a mechanism consistent with our reported results and reacted with the parent compound to yield SCl2 according to Eq. (1). The small amount of Cl2 remaining in the solution could also have been masked by the S–S stretch of S2Cl2 at 539 cm−1, especially considering the weak Raman effect of elemental chlorine (Steudel et al., 1987). Jacy K. Conrad: Conceptualization, Formal analysis, Investigation, Methodology, Validation, Writing – original draft. Michael E. Woods: Investigation, Writing – review & editing. Gregory P. Horne: Conceptualization, Funding acquisition, Supervision, Writing – original draft.
UR - http://www.scopus.com/inward/record.url?scp=85189696594&partnerID=8YFLogxK
U2 - 10.1016/j.radphyschem.2024.111628
DO - 10.1016/j.radphyschem.2024.111628
M3 - Comment/debate
AN - SCOPUS:85189696594
SN - 0969-806X
VL - 220
JO - Radiation Physics and Chemistry
JF - Radiation Physics and Chemistry
M1 - 111628
ER -