Brusseau M L, Narter M, Schnaar G, Marble J
Soil, Water and Environmental Science Department, University of Arizona, 429 Shantz Building, Tucson, Arizona 85721, USA.
Environ Sci Technol. 2009 May 15;43(10):3619-25. doi: 10.1021/es8020827.
The objective of this study was to quantitatively characterize the impact of porous-medium texture on interfacial area between immiscible organic liquid and water residing within natural porous media. Synchrotron X-ray microtomography was used to obtain high-resolution, three-dimensional images of solid and liquid phases in packed columns. The image data were processed to generate quantitative measurements of organic-liquid/water interfacial area and of organic-liquid blob sizes. Ten porous media, comprising a range of median grain sizes, grain-size distributions, and geochemical properties, were used to evaluate the impact of porous-medium texture on interfacial area. The results show that fluid-normalized specific interfacial area (A) and maximum specific interfacial area (Am) correlate very well to inverse median grain diameter. These functionalities were shown to result from a linear relationship between effective organic-liquid blob diameter and median grain diameter. These results provide the basis for a simple method for estimating specific organic-liquid/water interfacial area as a function of fluid saturation for a given porous medium. The availability of a method for which the only parameter needed is the simple-to-measure median grain diameter should be of great utility for a variety of applications.
本研究的目的是定量表征多孔介质结构对天然多孔介质中不混溶有机液体与水之间界面面积的影响。利用同步辐射X射线显微断层扫描技术获取填充柱中固相和液相的高分辨率三维图像。对图像数据进行处理,以生成有机液体/水界面面积和有机液体液滴尺寸的定量测量结果。使用了十种多孔介质,包括一系列中值粒径、粒度分布和地球化学性质,来评估多孔介质结构对界面面积的影响。结果表明,流体归一化比界面面积(A)和最大比界面面积(Am)与中值粒径的倒数具有很好的相关性。这些函数关系表明,有效有机液体液滴直径与中值粒径之间存在线性关系。这些结果为一种简单方法提供了基础,该方法可根据给定多孔介质中流体饱和度估算比有机液体/水界面面积。对于各种应用而言,一种仅需易于测量的中值粒径这一参数的方法应具有很大的实用性。