Effects of pressure on decomposition of formic acid in sub- and super-critical water

[Display omitted] ► Pressure affects negatively formic acid decomposition near the critical pressure. ► Apparent activation volume is higher at higher isothermal compressibility of water. ► Solvation effect is important for pressure dependence near the critical pressure. ► Pressure affects positivel...

Full description

Saved in:
Bibliographic Details
Published in:The Journal of supercritical fluids 2012-11, Vol.71, p.114-119
Main Authors: Fujii, Tatsuya, Hayashi, Rumiko, Kawasaki, Shin-ichiro, Suzuki, Akira, Oshima, Yoshito
Format: Article
Language:English
Subjects:
Compressibility
Constants
Critical pressure
Decarboxylation
Decomposition
Dehydration
Formic acid
Ionic reaction
Ionic reactions
Isothermal compressibility
Pressure
Solvation effect
Supercritical water
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:[Display omitted] ► Pressure affects negatively formic acid decomposition near the critical pressure. ► Apparent activation volume is higher at higher isothermal compressibility of water. ► Solvation effect is important for pressure dependence near the critical pressure. ► Pressure affects positively dehydration reaction at high pressure (>30MPa). ► Reaction order of H+ concentration for dehydration at high pressure was unity. The effects of pressure on formic acid decomposition in sub- and super-critical water from near the critical pressure to extremely high pressures (20–100MPa) at temperatures of 380 and 400°C were investigated. Near the critical pressure, the dehydration and decarboxylation rates decreased with increasing pressure. The apparent activation volumes near the critical pressure were high where the isothermal compressibility of water was large, implying that formic acid attracts water molecules better than the transition state does, and that the partial molar volume of the transition state is larger than those of the reactants. At higher pressures, dehydration rate increased with increasing pressure. Comparisons with experimental results for HCl addition at constant pressure suggest that dehydration proceeds via an ionic reaction at high pressures. The pressure may affect formic acid decomposition in supercritical water negatively through solvation effects near the critical pressure, and positively through ionic reactions above 30MPa.
ISSN:0896-8446
1872-8162
DOI:10.1016/j.supflu.2012.07.020