supercritical-fluid extraction
Quick Summary
Supercritical-fluid extraction (SFE) is a chemistry technique used for large-scale purification of complex liquid or solid materials. It utilizes a substance in a supercritical state, which exists at temperatures and pressures above its critical point. In this state, the substance is denser than a gas but less dense than a liquid, allowing it to dissolve substances effectively while maintaining low viscosity.1
A key advantage of SFE is the ease of removing the supercritical fluid after extraction. By reducing the temperature or pressure, the fluid returns to a gaseous state, leaving the extracted substances behind as a liquid or solid. This eliminates the problem of residual extracting liquid, as seen in the common example of removing caffeine from coffee.1
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- separation and purificationSupercritical-fluid methods
Supercritical-fluid extraction (SFE) is an important method for large-scale purification of complex liquid or solid matrices, such as polluted streams. The major advantage of this method over liquid-liquid extraction is that the supercritical fluid can easily be removed after extraction by lowering the temperature or…
Read MoreSupercritical-fluid extraction (SFE) is an important method for large-scale purification of complex liquid or solid matrices, such as polluted streams. The major advantage of this method over liquid-liquid extraction is that the supercritical fluid can easily be removed after extraction by lowering the temperature or…
Read More - chromatographySubsequent developments
…were the first to report separation of the porphyrins with dense gases in 1962. Carbon dioxide at 400 atmospheres is a typical supercritical-fluid mobile phase. (One atmosphere equals 760 millimetres, or 29.92 inches, of mercury; standard sea-level pressure is one atmosphere.) In an extreme case, Giddings and his group used…
Read More…were the first to report separation of the porphyrins with dense gases in 1962. Carbon dioxide at 400 atmospheres is a typical supercritical-fluid mobile phase. (One atmosphere equals 760 millimetres, or 29.92 inches, of mercury; standard sea-level pressure is one atmosphere.) In an extreme case, Giddings and his group used…
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