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在高表面压力下二饱和磷脂酰胆碱单分子层中相共存的持久性。

Persistence of phase coexistence in disaturated phosphatidylcholine monolayers at high surface pressures.

作者信息

Crane J M, Putz G, Hall S B

机构信息

Departments of Biochemistry and Molecular Biology, Medicine, and Physiology and Pharmacology, Oregon Health Sciences University, Portland, Oregon 97201-3098 USA.

出版信息

Biophys J. 1999 Dec;77(6):3134-43. doi: 10.1016/S0006-3495(99)77143-2.

Abstract

Prior reports that the coexistence of the liquid-expanded (LE) and liquid-condensed (LC) phases in phospholipid monolayers terminates in a critical point have been compromised by experimental difficulties with Langmuir troughs at high surface pressures and temperatures. The studies reported here used the continuous interface of a captive bubble to minimize these problems during measurements of the phase behavior for monolayers containing the phosphatidylcholines with the four different possible combinations of palmitoyl and/or myristoyl acyl residues. Isothermal compression produced surface pressure-area curves for dipalmitoyl phosphatidylcholine (DPPC) that were indistinguishable from previously published data obtained with Langmuir troughs. During isobaric heating, a steep increase in molecular area corresponding to the main LC-LE phase transition persisted for all four compounds to 45 mN/m, at which collapse of the LE phase first occurred. No other discontinuities to suggest other phase transitions were apparent. Isobars for DPPC at higher pressures were complicated by collapse of the monolayer, but continued to show evidence up to 65 mN/m for at least the onset of the LC-LE transition. The persistence of the main phase transition to high surface pressures suggests that a critical point for these monolayers of disaturated phospholipids is either nonexistent or inaccessible at an air-water interface.

摘要

先前有报道称,磷脂单分子层中液体膨胀(LE)相和液体凝聚(LC)相的共存会在临界点终止,但由于在高表面压力和温度下使用朗缪尔槽存在实验困难,这些报道受到了影响。本文报道的研究使用了俘获气泡的连续界面,以在测量含有棕榈酰和/或肉豆蔻酰酰基残基四种不同可能组合的磷脂酰胆碱的单分子层相行为时将这些问题降至最低。等温压缩产生的二棕榈酰磷脂酰胆碱(DPPC)表面压力-面积曲线与先前用朗缪尔槽获得的已发表数据无法区分。在等压加热过程中,对应于主要LC-LE相变的分子面积急剧增加,这四种化合物在45 mN/m时均持续存在,此时LE相首先发生塌陷。没有其他明显的不连续性表明存在其他相变。在较高压力下,DPPC的等压线因单分子层塌陷而变得复杂,但至少在65 mN/m时仍显示出LC-LE转变开始的证据。主要相变持续到高表面压力表明,这些二饱和磷脂单分子层的临界点在气-水界面不存在或无法达到。

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