首页> 外文期刊>The Journal of Chemical Physics >A DETERMINATION OF THE PHASE DIAGRAM OF RELAXED LANGMUIR MONOLAYERS OF BEHENIC ACID
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A DETERMINATION OF THE PHASE DIAGRAM OF RELAXED LANGMUIR MONOLAYERS OF BEHENIC ACID

机译:酸的Langmuir单分子层的相图的测定

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Grazing incidence x-ray scattering (GIXS) and Brewster angle microscopy (BAM) are used to determine the pi-T phase diagram of Behenic acid monolayers supported on the surface of water (pH=2.0) over the temperature range of 3 degrees C to 20.6 degrees C. The phase diagram is constructed from measurements taken during isothermal compressions in which the surface pressure relaxed to a stable value at each surface density, and during temperature scans at fixed average surface density. The phase diagram is different than those previously reported for Behenic acid primarily because of the surface pressure relaxation. For temperatures less than 12 degrees C the phase diagram exhibits similar phases and topology as the published diagrams, although the location of the phases in the pi-T plane is different. Temperature scans combined with the isotherms, and the Clausius-Clapeyron relation are used to determine three coexistence lines that meet in a triple point. Changes in entropy across the phase boundaries are determined. Near room temperature (20.6 degrees C) only one phase is measured over the range of surface pressure from 0 dynes/cm to the collapse pressure in contrast to reported measurements on monolayers out of equilibrium (i.e., when the surface pressure is not allowed to relax) that exhibit several phases near room temperature at pressures higher than the collapse pressure. Discrepancies are observed between the average area per molecule (A(T)) and the area per molecule determined from measurements of the unit cell (A(X)) in the close parked regions of the phase diagram. It is conjectured that the pi A(X) plane is a better representation of the ordered equilibrium monolayer phases than the pi-A(T) plane. Isotherms plotted in the pi-A(X) plane are used to determine the compressibility of the ordered phases and the nature of the phase transitions. (C) 1996 American Institute of Physics. [References: 50]
机译:掠入射x射线散射(GIXS)和布鲁斯特角显微镜(BAM)用于确定在3摄氏度至200摄氏度的温度范围内负载在水表面(pH = 2.0)的山hen酸单层的pi-T相图。 20.6摄氏度。根据等温压缩过程中的测量结果构建相图,在等温压缩过程中,表面压力在每个表面密度下松弛到一个稳定值,而在温度扫描过程中以固定的平均表面密度进行。该相图与先前报道的山acid酸相图不同,主要是因为表面压力松弛。对于低于12摄氏度的温度,尽管pi-T平面中各相的位置不同,但该相图显示出与已发布的图相似的相和拓扑。温度扫描结合等温线,以及克劳修斯-克拉佩隆关系式用于确定在一个三点处相遇的三个共存线。确定跨相界的熵变化。接近室温(20.6摄氏度),在从0达因/厘米到崩溃压力的表面压力范围内,仅测量了一个相,这与报告的单层失衡测量结果相反(即,当表面压力不允许松弛时) )在高于室温的压力下比塌陷压力高时会显示出多个相。在相图的封闭停放区域中,观察到每个分子的平均面积(A(T))与根据单位晶胞的测量值(A(X))确定的每个分子的面积之间的差异。推测pi A(X)平面比pi-A(T)平面更好地表示了有序平衡单层相。在pi-A(X)平面上绘制的等温线用于确定有序相的可压缩性和相变的性质。 (C)1996年美国物理研究所。 [参考:50]

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