Spectroscopic Measurement of Critical Points and Characteristics of Supercritical State of H2O and CO2
Noriyoshi Tsuchiya, Chizu Sekiguchi, Nobuo Hirano
Abstract
Open-access reader
Noriyoshi Tsuchiya, Chizu Sekiguchi, Nobuo Hirano
Abstract
Open-access reader
Spectroscopic measurements in the range from 350 nm to 1050 nm for pure H2O and CO2 fluids at high temperatures and pressures were carried out to observe critical phenomena using an optical cell autoclave. The intensity of transmitted light though the fluid became drastically lower around the critical point in both cases of H2O. The minimum intensity of transmitted light corresponded to the critical temperature and pressure of each fluid. The supercritical region beyond the critical point for water has been inferred to be a homogeneous state, which does not correspond to either a true liquid phase or a true vapor phase. Results of supercritical-state dissolution experiments using granite and quartz show that this fluid can be subdivided into two apparent phases comprising a ‘liquid-like’ region and a ‘vapor-like’ region. Spectroscopic measurements are powerful tool to identify bulk molecular behavior of fluids at sub-and supercritical states.
OpenAlex reports 2 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
Spectroscopic measurements in the range from 350 nm to 1050 nm for pure H2O and CO2 fluids at high temperatures and pressures were carried out to observe critical phenomena using an optical cell autoclave. The intensity of transmitted light though the fluid became drastically lower around the critical point in both cases of H2O. The minimum intensity of transmitted light corresponded to the critical temperature and pressure of each fluid. The supercritical region beyond the critical point for water has been inferred to be a homogeneous state, which does not correspond to either a true liquid phase or a true vapor phase. Results of supercritical-state dissolution experiments using granite and quartz show that this fluid can be subdivided into two apparent phases comprising a ‘liquid-like’ region and a ‘vapor-like’ region. Spectroscopic measurements are powerful tool to identify bulk molecular behavior of fluids at sub-and supercritical states.
Key concepts: Supercritical fluid, Critical point (mathematics), Autoclave, Dissolution, Materials science, Intensity (physics), Phase (matter), Quartz