TY - JOUR
T1 - Spectroscopic determination of the critical temperatures and pressures of H2O, CO2, and C2H5OH
AU - Sekiguchi, Chizu
AU - Hirano, Nobuo
AU - Okamoto, Atsushi
AU - Tsuchiya, Noriyoshi
PY - 2013/12/28
Y1 - 2013/12/28
N2 - The transmittance of 500-800 nm light was shown to change significantly at the critical points of three pure fluids. Spectroscopic measurements of H2O, CO2, and C2H5OH were made in a visible-type autoclave at high temperature and pressure. Each fluid showed significantly decreased transmittance as its critical point was approached; transmittance reached a local minimum at the critical temperature and pressure. The experimentally determined critical temperature and pressure of H2O are 374 °C and 22.07-22.09 MPa, respectively, similar to reference values of 374.15 °C and 22.12 MPa; C2H5OH showed values of 243 °C and 6.30-6.31 MPa (versus reference values of 241 ± 7 and 243.4 °C and 6.3 ± 0.4 and 6.14 MPa); and CO2 showed values of 32 °C and 7.36-7.43 MPa (versus reference values of 31.04 ± 0.2 °C and 7.37 ± 0.04 MPa). The good agreement between the experimental results and the reference values indicates that the spectroscopic method used here could be applied to other fluids, including mixed geofluids.
AB - The transmittance of 500-800 nm light was shown to change significantly at the critical points of three pure fluids. Spectroscopic measurements of H2O, CO2, and C2H5OH were made in a visible-type autoclave at high temperature and pressure. Each fluid showed significantly decreased transmittance as its critical point was approached; transmittance reached a local minimum at the critical temperature and pressure. The experimentally determined critical temperature and pressure of H2O are 374 °C and 22.07-22.09 MPa, respectively, similar to reference values of 374.15 °C and 22.12 MPa; C2H5OH showed values of 243 °C and 6.30-6.31 MPa (versus reference values of 241 ± 7 and 243.4 °C and 6.3 ± 0.4 and 6.14 MPa); and CO2 showed values of 32 °C and 7.36-7.43 MPa (versus reference values of 31.04 ± 0.2 °C and 7.37 ± 0.04 MPa). The good agreement between the experimental results and the reference values indicates that the spectroscopic method used here could be applied to other fluids, including mixed geofluids.
KW - Critical point
KW - Geofluids
KW - Hydrothermal experiment
KW - Spectroscopic measurement
KW - Supercritical fluid
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U2 - 10.2465/jmps.130620b
DO - 10.2465/jmps.130620b
M3 - Letter
AN - SCOPUS:84891510327
SN - 1345-6296
VL - 108
SP - 356
EP - 361
JO - Journal of Mineralogical and Petrological Sciences
JF - Journal of Mineralogical and Petrological Sciences
IS - 6
ER -