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Effects of divalent cations (Ca 2+, Mg 2+, Ni 2+, and Zn 2+ ) on a zwitterionic phospholipid monolayer at the air−water interface are investigated by surface pressure−area isotherms and in situ X-ray scattering. Divalent cations lower the surface pressure for the fluid (LE) to condensed (L 2 ) phase transition in a strongly ion-specific manner. Surprisingly, the two-dimensional lattice dimensions and the tilt of the lipids’ alkyl tails in the L 2 phase show a nearly ion-nonspecific dependence on the excess surface pressure above the transition pressure. An empirical “universal” relationship was found between the tail tilt and the excess pressure, with the tails in the L 2 phase always displaying a tilt of 29° at the transition. A practical implication of these results is that, regardless of the divalent cation present, the microscopic details of the lipid tail packing in the L 2 phase can be deduced at any surface pressure once the transition pressure is obtained from isotherms.
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Kewalramani et al. (2009) studied this question.
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