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Effect of secondary alcohol ethoxylates on behavior of triolein‐water‐surfactant systems
Author(s) -
Tungsubutra Teeradetch,
Miller Clarence A.
Publication year - 1994
Publication title -
journal of the american oil chemists' society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.512
H-Index - 117
eISSN - 1558-9331
pISSN - 0003-021X
DOI - 10.1007/bf02541474
Subject(s) - triolein , oleyl alcohol , pulmonary surfactant , chemistry , chromatography , ethylene oxide , alcohol , isopropyl alcohol , emulsion , phase (matter) , organic chemistry , polymer , biochemistry , lipase , copolymer , enzyme
Study of the equilibrium phase behavior of systems containing water, triolein and secondary alcohol ethoxylates showed that a D or microemulsion phase, which solubilized significant amounts of triolein, formed at temperatures as low as 25°C when the surfactant was a suitable mixture of TERGITOL 15‐S‐3 and 15‐S‐5 (Union Carbide, Charleston, WV) with average ethylene oxide numbers of 3 and 5, respectively. In previous work with pure C 12 linear ethoxylates and triolein, the D phase had formed only at temperatures above about 55°C. Based on the earlier studies, formation of the D phase would be expected to improve soil removal from synthetic fabrics by a solubilization‐emulsification mechanism. When sufficient oleyl alcohol was mixed with triolein, the D phase was observed at 25°C with Tergitol 15‐S‐5 alone. Observation of dynamic behavior in this system for triolein‐oleyl alcohol drops injected into surfactant‐water mixtures revealed that intermediate phases frequently formed near the drop surfaces and that considerable spontaneous emulsification of triolein occurred for appropriate drop compositions. Experiments with drops initially attached to individual polyester fibers confirmed that little oil remained on the fibers when emulsification was extensive. This mechanism involving spontaneous emulsification provides a means for soil removal different from that found previously in other systems, where the soil was solubilized into an intermediate phase, and this phase was emulsified by externally imposed agitation.