KINETICS AND MECHANISM OF THE BAROTROPIC LAMELLAR GEL LAMELLAR LIQUID-CRYSTAL PHASE-TRANSITION IN FULLY HYDRATED DIHEXADECYLPHOSPHATIDYLETHANOLAMINE - A TIME-RESOLVED X-RAY-DIFFRACTION STUDY USING PRESSURE JUMP
Ac. Cheng et al., KINETICS AND MECHANISM OF THE BAROTROPIC LAMELLAR GEL LAMELLAR LIQUID-CRYSTAL PHASE-TRANSITION IN FULLY HYDRATED DIHEXADECYLPHOSPHATIDYLETHANOLAMINE - A TIME-RESOLVED X-RAY-DIFFRACTION STUDY USING PRESSURE JUMP, Biophysical journal, 67(1), 1994, pp. 293-303
The kinetics and mechanism of the barotropic lamellar gel (L(beta),)/l
amellar liquid crystal (L(alpha)) phase transition in fully hydrated 1
,2-dihexadecyl-sn-glycero-3-phosphoethanolamine (DH PE) has been studi
ed using time-resolved x-ray diffraction (TRXRD). The phase transition
was induced by pressure jumps of varying amplitudes in both the press
urization and depressurization directions at controlled temperature (7
8 degrees C). Both low- and wide-angle diffracted x rays were recorded
simultaneously in live time using an x-ray-sensitive image intensifie
r coupled to a CCD camera and Super-VHS videotape recorder. Such an ar
rangement allowed for the direct and quantitative characterization of
the long- (lamellar repeat spacing) and short-range order (chain packi
ng) during a kinetic experiment. The image-processed live-time x-ray d
iffraction data were fitted using a nonlinear least-squares model, and
the parameters of the fits were monitored continuously throughout the
transition. The pressure-induced transitions from the L(alpha) to the
L(beta), phase and from the L(beta), to the L(alpha) phase was two-st
ate (no formation of intermediates apparent during the transition) to
within the sensitivity limits of the method. The corresponding transit
time (the time during which both phases coexist) associated with the
long- and short-range order of the pressurization-induced L(alpha) and
L(beta), phase transition decreased to a limiting value of approximat
ely 50 ms with increasing pressure jump amplitude. This limiting value
was close to the response time of the detector/recording system. Thus
, the intrinsic transit time of this transition in fully hydrated DHPE
at 78 degrees C was less than or equal to 50 ms. In contrast, the dep
ressurization-induced L(beta),-to-L(alpha) phase transition was slower
, taking approximately 1 s to complete, and occurred with no obvious d
ependence of the transit time on pressure jump amplitude. In the depre
ssurization jump experiment, the liquid responded rapidly to the press
ure jump in the L(beta), phase up to the rate-determining L(beta),-to-
L(alpha) transition. Such behavior was examined carefully, as it could
complicate the interpretation of phase transition kinetic measurement
s.