Capillary effects on natural remobilization of pools of dense non-aqueous phase liquid mixtures in porous media

被引:1
|
作者
Roy, J. W.
Smith, J. E.
Gillham, R. W.
机构
[1] Environm Canada, Canada Ctr Inland Waters, Burlington, ON L7R 4A6, Canada
[2] McMaster Univ, Sch Geog & Earth Sci, Hamilton, ON L8S 4L8, Canada
[3] Univ Waterloo, Dept Earth Sci, Waterloo, ON N2L 3G1, Canada
来源
SOIL & SEDIMENT CONTAMINATION | 2007年 / 16卷 / 03期
基金
加拿大创新基金会; 加拿大自然科学与工程研究理事会;
关键词
DNAPL; ground water; dissolution; immiscible displacement; wettability;
D O I
10.1080/15320380701285659
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The natural remobilization of an initially static mixed dense non-aqueous phase liquid (DNAPL) pool due to dissolution was demonstrated by Roy et al. (2002, 2004) using a compositional mathematical model and laboratory experiments with open pools over a porous medium. The purposes of this study were to: a) demonstrate natural remobilization for a pool within porous media (as opposed to an open pool); and b) analyze the capillary effects associated with residual formation, a changing saturation profile, hysteresis, and aging, as these processes may reduce the potential for natural remobilization of pools in porous media. DNAPL pools comprised of tetrachloroethene and benzene were created within a zone of larger glass beads overlying smaller glass beads, in a water-saturated 2-D flow cell. In one case, remobilization occurred in the form of a DNAPL finger, after 56 days of flushing. In another case, no remobilization had occurred after 64 days of flushing, though the density increased by 430 kg m(-3) and remobilization was predicted by the compositional model. Comparison of observations with model predictions suggest that contact angle hysteresis, related to an observed change in wettability, was the most significant contributing factor causing overprediction of the potential for natural remobilization.
引用
收藏
页码:253 / 268
页数:16
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