A quartz crystal microbalance (QCM) is used to determine the phase equilibrium of paclitaxel-carbon dioxide system in the pressure range of 0-11 MPa and at temperatures of 35℃
40℃ and 45℃.The experimental results indicated that gaseous CO
2
could be absorbed poorly into paclitaxel.The swelling of paclitaxel film in CO
2
was observed before paclitaxel dissolved into supercritical carbon dioxide (ScCO
2
) with the increase of pressure.It was found that ScCO
2
was not a good solvent for paclitaxel.The mole fraction of paclitaxel in ScCO
2
was in the range of (4.5×10
-9
)-(7.8×10
-9
) under all our experimental conditions.Therefore
a much higher pressure than the CO
2
supercritical point and/or a cosolvent must be used in any processes wherever paclitaxel dissolution in ScCO
2
is required.
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Thermodynamic feasibility of nickel and cerium oxides as versatile oxygen carriers in chemical looping reforming of methane-rich feedstocks
Thermal decomposition behavior and kinetics of magnesite under carbon dioxide atmosphere
Insights on the effect of Si-Al interaction on Ni/Al2O3/SiC monolithic catalysts for CO2 methanation
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