Ab initio study of ammonium perchlorate combustion initiation processes: unimolecular decomposition of perchloric acid and the related OH + ClO3 reaction
{"title":"Ab initio study of ammonium perchlorate combustion initiation processes: unimolecular decomposition of perchloric acid and the related OH + ClO3 reaction","authors":"R. Zhu, M. Lin","doi":"10.1039/B109523B","DOIUrl":null,"url":null,"abstract":"The unimolecular decomposition of HClO 4 has been investigated at the G2M//B3LYP/6-311+G(3df, 2p) level of theory. Above 500 K, the decomposition process was found to depend strongly on pressure below 200 atm. The rate constants at the high- and low-pressure limits were predicted to be k 1 ∞ = 1.5 × 10 17 exp(–26500/T) s –1 and k 1 0 = 3.39 × 10 30 T –10.9 exp(–29430/T) cm 3 molecule –1 s –1 , respectively. Under the atmospheric-pressure condition, the predicted first-order rate coefficient for the temperature range 300–3000 K, k 1 = 5.0 × 10 51 T –11.64 exp(–30700/T) s –1 , agrees reasonably with experimental data obtained at 550–750 K by different experimental groups. We have also calculated the rate constants for the bimolecular reaction of OH with ClO 3 producing HClO 4 by association/stabilization and HO 2 + ClO 2 by association/fragmentation. At the high-pressure limit, the rate constants can be given as:k –1 = 3.2 × 10 –10 T 0.07 exp(–25/T) cm 3 molecule –1 s –1 and k 2 = 2.1 × 10 –10 T 0.09 exp(–18/T) cm 3 molecule – 1 s –1 , respectively, for the temperature range 300–3000 K. Under the atmospheric pressure condition, the OH + ClO 3 reaction produces predominately the HO 2 + ClO 2 products.","PeriodicalId":20106,"journal":{"name":"PhysChemComm","volume":"4 1","pages":"127-132"},"PeriodicalIF":0.0000,"publicationDate":"2001-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"10","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"PhysChemComm","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1039/B109523B","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 10
Abstract
The unimolecular decomposition of HClO 4 has been investigated at the G2M//B3LYP/6-311+G(3df, 2p) level of theory. Above 500 K, the decomposition process was found to depend strongly on pressure below 200 atm. The rate constants at the high- and low-pressure limits were predicted to be k 1 ∞ = 1.5 × 10 17 exp(–26500/T) s –1 and k 1 0 = 3.39 × 10 30 T –10.9 exp(–29430/T) cm 3 molecule –1 s –1 , respectively. Under the atmospheric-pressure condition, the predicted first-order rate coefficient for the temperature range 300–3000 K, k 1 = 5.0 × 10 51 T –11.64 exp(–30700/T) s –1 , agrees reasonably with experimental data obtained at 550–750 K by different experimental groups. We have also calculated the rate constants for the bimolecular reaction of OH with ClO 3 producing HClO 4 by association/stabilization and HO 2 + ClO 2 by association/fragmentation. At the high-pressure limit, the rate constants can be given as:k –1 = 3.2 × 10 –10 T 0.07 exp(–25/T) cm 3 molecule –1 s –1 and k 2 = 2.1 × 10 –10 T 0.09 exp(–18/T) cm 3 molecule – 1 s –1 , respectively, for the temperature range 300–3000 K. Under the atmospheric pressure condition, the OH + ClO 3 reaction produces predominately the HO 2 + ClO 2 products.