Reactivity of porous graphite in chlorinated acidic solution

Article abstract of DOI:10.1149/1.2095374

In this study, the rate of CO₂ and HCl formation are determined and compared to the postulated local-action mechanism. The experimental results strongly indicate that the rate of HC1 formation is four times the rate of CO₂ evolution, in agreement with the postulated mechanism. The amount of carbon loss over a 10-day period is roughly 0.5g. or about 3-4% of the original weight of the graphite sample. The significant losses can account for changes in surface area and pore size distribution.

Full text of DOI:10.1149/1.2095374

Downloaded on 2015-06-11 to IP 150.214.146.47 address. Redistribution subject to ECS terms of use (see ecsdl.org/site/terms_use) unless CC License in place (see abstract).

Downloaded on 2015-06-11 to IP 150.214.146.47 address. Redistribution subject to ECS terms of use (see ecsdl.org/site/terms_use) unless CC License in place (see abstract).

Downloaded on 2015-06-11 to IP 150.214.146.47 address. Redistribution subject to ECS terms of use (see ecsdl.org/site/terms_use) unless CC License in place (see abstract).