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The phase transitions of n-alkanes in mesoscopic pores of graphite

机译:正构烷烃在石墨介观孔隙中的相变

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The phase transitions of two n-alkanes of different parity, C16H34 and C17H36, confined in the mesoscopic pores of exfoliated graphite have been studied by differential scanning calorimetry. For samples from one statistical monolayer up to about four layers of paraffin, microcalorimetry shows a characteristic signature from the "surface phase" alone. At higher fillings the melting and phase transition temperatures and enthalpies of the additional "included" phase were depressed compared to those of the bulk paraffin. The depressions in the phase transition temperatures and the neperian logarithm of the enthalpies are to a good approximation inversely proportional to the number of included layers. Depending on the coverage, competing effects between the graphite surface and the degree of filling of the pores are observed for both the surface phase and the included phase. The results for the included phase are consistent with the Gibbs-Thompson equation down to pore sizes of the order of a few nanometres. (C) 2005 Elsevier Ltd. All rights reserved.
机译:采用差示扫描量热法研究了两种不同奇偶性正构烷烃C16H34和C17H36在剥落石墨介观孔隙中的相变.对于从一个统计单层到大约四层石蜡的样品,微量热法仅显示“表面相”的特征特征。在较高的填充物下,与块状石蜡相比,额外的“夹杂”相的熔融和相变温度以及焓被抑制。相变温度的凹陷和焓的neperian对数与包含层的数量成反比。根据覆盖范围的不同,在表面相和包含相中都观察到石墨表面和孔隙填充程度之间的竞争效应。所包含相的结果与Gibbs-Thompson方程一致,孔径为几纳米量级。(C) 2005 爱思唯尔有限公司保留所有权利。

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