The miscibility of isobutyric acid with water and the influence of the isotope substitution of oxygen (O-16/O-18) in water over a broad concentration range are reported. The system exhibits a phase diagram with, an upper critical solution temperature (UCST) and a visible isotope effect thereon. The oxygen isotope substitution decreases the UCST, leading to better miscibility of isobutyric acid with water. The isotope shift, Delta T-c = T-c(O-18) - T-c(O-16), extrapolated to the 100% enrichment in 180, is equal to-1.15 K; hence it is much smaller and opposite to that found for deuterium substitution. The origin of the observed miscibility isotope effect has been qualitatively discussed in terms of the condensed-phase isotope effect theory.
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Open Univ, Planetary & Space Sci Res Inst, Milton Keynes MK7 6AA, Bucks, EnglandOpen Univ, Planetary & Space Sci Res Inst, Milton Keynes MK7 6AA, Bucks, England
Baker, L
Franchi, IA
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Open Univ, Planetary & Space Sci Res Inst, Milton Keynes MK7 6AA, Bucks, EnglandOpen Univ, Planetary & Space Sci Res Inst, Milton Keynes MK7 6AA, Bucks, England
Franchi, IA
Maynard, J
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Open Univ, Planetary & Space Sci Res Inst, Milton Keynes MK7 6AA, Bucks, EnglandOpen Univ, Planetary & Space Sci Res Inst, Milton Keynes MK7 6AA, Bucks, England
Maynard, J
Wright, IP
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Open Univ, Planetary & Space Sci Res Inst, Milton Keynes MK7 6AA, Bucks, EnglandOpen Univ, Planetary & Space Sci Res Inst, Milton Keynes MK7 6AA, Bucks, England
Wright, IP
Pillinger, CT
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Open Univ, Planetary & Space Sci Res Inst, Milton Keynes MK7 6AA, Bucks, EnglandOpen Univ, Planetary & Space Sci Res Inst, Milton Keynes MK7 6AA, Bucks, England