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首页> 外文期刊>Journal of Chemical and Engineering Data: the ACS Journal for Data >Interfacial Tension Measurements of the (H2O + n-Decane + CO2) Ternary System at Elevated Pressures and Temperatures
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Interfacial Tension Measurements of the (H2O + n-Decane + CO2) Ternary System at Elevated Pressures and Temperatures

机译:(H2O +正癸烷+ CO2)三元体系在升高的压力和温度下的界面张力测量

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摘要

The interfacial tension between H2O and [(1 - x)n-decane + αCO2] was investigated for three different compositions of CO2 in the alkane-rich phase, of mole fractions x = (0.0, 0.2, and 0.5), along several isotherms at temperatures up to 443 K and pressures ranging from the miscibility state points for (n-decane + CO2) up to 50 MPa. The pendant drop method was implemented using a high pressure apparatus consisting of a view cell, fitted with a high pressure capillary tube for creating pendant H2O drops in the [w-decane + CO2] bulk phase. The conditions investigated cover a wide range relevant to carbon storage, providing information as to how the variation of the CO2 content in hydrocarbon fluids affects their interfacial tension with aqueous phases, which influences the trapping potential of underground formations. The results were compared to literature values where possible. A thermodynamic analysis of the dependence of the interfacial tension on CO2 composition, as well as on temperature, was discussed with respect to the Gibbs surface excess concentration and the enthalpy of interface formation, respectively. The present work provides novel interfacial tension data for the ternary system and addresses possible reasons for the observed discrepancies in literature values for the binary (H2O + n-decane) system observed over the range of conditions investigated. The reported results have a relative average standard deviation of 1.7 %.
机译:研究了H2O与[(1-x)n-癸烷+αCO2]之间的界面张力,研究了在富烷烃相中摩尔分数x =(0.0、0.2和0.5)的三种不同CO2组成以及沿多个等温线的情况。在高达443 K的温度和压力(正癸烷+ CO2的混溶性状态点)至50 MPa的范围内变化。使用由视单元组成的高压设备实施悬滴法,该视单元安装有高压毛细管,用于在[w-癸烷+ CO2]本体相中生成悬滴H2O。研究的条件涵盖了与碳储存有关的广泛范围,提供了有关烃类流体中CO2含量变化如何影响其与水相的界面张力的信息,从而影响了地下地层的捕集潜力。将结果与可能的文献值进行比较。分别针对吉布斯表面过量浓度和界面形成焓讨论了界面张力对CO2组成以及温度的依赖性的热力学分析。本工作为三元系统提供了新颖的界面张力数据,并解决了在所研究的条件范围内观察到的二元(H2O +正癸烷)系统文献值中观察到的差异的可能原因。报告的结果的相对平均标准偏差为1.7%。

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