Roy J W, Smith J E, Gillham R W
Department of Earth Sciences, University of Waterloo, Waterloo, ON, N2L 3G1, Canada.
J Contam Hydrol. 2004 Oct;74(1-4):145-61. doi: 10.1016/j.jconhyd.2004.02.009.
Mixtures of dense non-aqueous phase liquids (DNAPLs) trapped in the subsurface can act as long-term sources of contamination by dissolving into flowing groundwater. In general, the components of higher solubility are removed more quickly, thus altering the composition of the remaining DNAPL, and possibly leading to changes in its physical properties. Through the development of a simple compositional model, Roy et al. [J. Contam. Hydrol. 2002 (59) 163] showed that preferential dissolution of a mixed DNAPL could potentially result in changes in density and interfacial tension that could subsequently lead to remobilization of an initially static DNAPL pool. The laboratory experiments presented in this next paper provide a proof-of-concept for the previously presented theory, demonstrating and quantifying this process of remobilization. In addition, the experiments provide a data set for evaluation of the model presented by Roy et al. [J. Contam. Hydrol. 2002 (59) 163]. In the four experiments, a DNAPL pool comprised of tetrachloroethene and benzene was created as an open pool overlying glass beads within a water-saturated 2-D flow box. Experiments included rectangular and triangular pools. In each of the experiments, remobilization (as breakthrough) was observed more than 2 weeks after formation of the initial pool. During each experiment, the pool height declined as mass was lost by dissolution, while sampling indicated a decrease in the mole fraction of benzene, the more soluble component. Small protuberances formed along the bottom of the pool as its composition changed with time and the displacement pressure was achieved for various pore throats. Eventually one of the protuberances extended further, forming a finger (breakthrough). In general, the pool emptied as the finger proceeded further into the beads. It was also shown theoretically and experimentally that remobilization will occur sooner for pools with a triangular (pointing down), rather than rectangular, shape. The experimental results were simulated using the model developed by Roy et al. [J. Contam. Hydrol. 2002 (59) 163]. The model matched the observations well, suggesting that it accurately represents the primary mechanisms involved with natural remobilization under the conditions of the study.
被困在地下的致密非水相液体(DNAPL)混合物可通过溶解进入流动的地下水中,成为长期的污染源。一般来说,溶解度较高的成分被去除得更快,从而改变了剩余DNAPL的组成,并可能导致其物理性质发生变化。通过开发一个简单的成分模型,罗伊等人[《污染水文杂志》2002年(59)163]表明,混合DNAPL的优先溶解可能会导致密度和界面张力的变化,进而可能导致最初静止的DNAPL池重新移动。下一篇论文中介绍的实验室实验为之前提出的理论提供了概念验证,证明并量化了这种重新移动的过程。此外,这些实验还提供了一个数据集,用于评估罗伊等人[《污染水文杂志》2002年(59)163]提出的模型。在这四个实验中,在一个水饱和的二维流动箱内,由四氯乙烯和苯组成的DNAPL池作为一个开放池覆盖在玻璃珠上。实验包括矩形池和三角形池。在每个实验中,在初始池形成后两周多观察到了重新移动(作为突破)。在每个实验过程中,随着质量因溶解而损失,池的高度下降,而采样表明更易溶的成分苯的摩尔分数降低。随着池的组成随时间变化,池底部形成了小突起,并且对于各种孔隙喉道达到了驱替压力。最终,其中一个突起进一步延伸,形成了一个指状物(突破)。一般来说,随着指状物进一步深入珠子,池排空。理论和实验还表明,对于三角形(朝下)形状的池,而不是矩形形状的池,重新移动会更快发生。使用罗伊等人[《污染水文杂志》2002年(59)163]开发的模型对实验结果进行了模拟。该模型与观测结果匹配良好,表明它准确地代表了研究条件下自然重新移动所涉及的主要机制。