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Thermal Response of Langmuir-Blodgett Films of Dipalmitoylphosphatidylcholine Studied by Atomic Force Microscopy and Force Spectroscopy

机译:原子力显微镜和力谱研究双棕榈酰磷脂酰胆碱Langmuir-Blodgett膜的热响应

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摘要

The topographic evolution of supported dipalmitoylphosphatidylcholine (DPPC) monolayers with temperature has been followed by atomic force microscopy in liquid environment, revealing the presence of only one phase transition event at ∼46°C. This finding is a direct experimental proof that the two phase transitions observed in the corresponding bilayers correspond to the individual phase transition of the two leaflets composing the bilayer. The transition temperature and its dependency on the measuring medium (liquid saline solution or air) is discussed in terms of changes in van der Waals, hydration, and hydrophobic/hydrophilic interactions, and it is directly compared with the transition temperatures observed in the related bilayers under the same experimental conditions. Force spectroscopy allows us to probe the nanomechanical properties of such monolayers as a function of temperature. These measurements show that the force needed to puncture the monolayers is highly dependent on the temperature and on the phospholipid phase, ranging from 120 ± 4 pN at room temperature (liquid condensed phase) to 49 ± 2 pN at 65°C (liquid expanded phase), which represents a two orders-of-magnitude decrease respective to the forces needed to puncture DPPC bilayers. The topographic study of the monolayers in air around the transition temperature revealed the presence of boundary domains in the monolayer surface forming 120° angles between them, thus suggesting that the cooling process from the liquid-expanded to the liquid-condensed phase follows a nucleation and growth mechanism.
机译:负载的二棕榈酰磷脂酰胆碱(DPPC)单层的形貌随温度变化,随后在液体环境中进行原子力显微镜观察,揭示了在约46°C下仅存在一个相变事件。该发现是直接的实验证明,即在相应双层中观察到的两个相变对应于组成双层的两个小叶的单个相变。讨论了转变温度及其对测量介质(液体盐溶液或空气)的依赖性,涉及范德华力,水合和疏水/亲水相互作用的变化,并将其与相关双层中观察到的转变温度直接进行了比较。在相同的实验条件下力谱法使我们能够探测这种单层的纳米力学性能随温度的变化。这些测量结果表明,穿刺单层所需的力在很大程度上取决于温度和磷脂相,范围从室温下的120±4 pN(液体冷凝相)到65°C下的49±2 pN(液体膨胀相) ),这表示穿刺DPPC双层所需的力分别减少了两个数量级。在转变温度附近的空气中对单层进行的地形研究表明,在单层表面中存在边界区域,它们之间形成了120°角,因此表明从液相膨胀到液相凝结的冷却过程遵循成核和增长机制。

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