Infiltration and redistribution of perchloroethylene in partially saturated, stratified porous media

被引:37
|
作者
Hofstee, C
Oostrom, M
Dane, JH
Walker, RC
机构
[1] Auburn Univ, Dept Agron & Soils, Auburn, AL 36849 USA
[2] Pacific NW Natl Lab, Environm Technol Div, Richland, WA USA
[3] Auburn Univ, Dept Civil Engn, Auburn, AL 36849 USA
关键词
DNAPL; nonspreading; gamma radiation; numerical simulator (STOMP); multifluid flow;
D O I
10.1016/S0169-7722(98)00101-6
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Contamination of the subsurface by nonaqueous phase liquids (NAPLs) is a widespread problem. To investigate the behavior of a nonspreading, dense NAPL (DNAPL) in the vadose zone, we conducted perchloroethylene (PCE) infiltration experiments in nominally 1- and 2-dimensional (D), stratified porous media. In addition, the usefulness and limitations of a multifluid flow simulator to describe PCE infiltration and redistribution under the experimental conditions were tested. The physical simulations were conducted in a column (1-D) and a flow container (2-D) which were packed with two distinct layers of coarse-grained sand and a fine-grained sand layer in between. Volumetric water and PCE contents were determined with a fully automated dual-energy gamma radiation system. While migrating through the drier parts of the coarse-grained sand layers, PCE appeared to wet the water-air interface rather than displacing any water. In the wetter parts of the porous medium, PCE displaced water and behaved as a true nonwetting fluid. PCE showed a limited response to gradients in capillary pressure and rather high values for the volumetric PCE content were measured in the fine-grained sand layers. This was attributed to the nonspreading nature of PCE. The multifluid flow simulator appeared to predict the initial PCE movement in the vadose zone reasonably well. However, the model was not capable of predicting the final amounts of PCE retained in either the unsaturated of saturated part of the flow domain, mainly because the simulator does not consider the nonspreading flow behavior of NAPLs. (C) 1998 Elsevier Science B.V. All rights reserved.
引用
下载
收藏
页码:293 / 313
页数:21
相关论文
共 50 条
  • [21] Contaminant transport in partially saturated fractured porous media
    Valliappan, S
    Wang, W
    Khalili, N
    COMPUTER METHODS AND ADVANCES IN GEOMECHANICS, VOL 1, 1997, : 267 - 275
  • [22] NMR Measurements of Tortuosity in Partially Saturated Porous Media
    Zecca, Marco
    Vogt, Sarah J.
    Connolly, Paul R. J.
    May, Eric F.
    Johns, Michael L.
    TRANSPORT IN POROUS MEDIA, 2018, 125 (02) : 271 - 288
  • [23] Diffusiophoresis of colloids in partially-saturated porous media
    Jotkar, Mamta
    Ben-Noah, Ilan
    Hidalgo, Juan J.
    Dentz, Marco
    Advances in Water Resources, 2024, 193
  • [24] Dynamic hydraulic fracturing in partially saturated porous media
    Sonntag, Alixa
    Wagner, Arndt
    Ehlers, Wolfgang
    COMPUTER METHODS IN APPLIED MECHANICS AND ENGINEERING, 2023, 414
  • [25] NMR Measurements of Tortuosity in Partially Saturated Porous Media
    Marco Zecca
    Sarah J. Vogt
    Paul R. J. Connolly
    Eric F. May
    Michael L. Johns
    Transport in Porous Media, 2018, 125 : 271 - 288
  • [26] Localisation modelling in fully and partially saturated porous media
    Schrefler, B
    Sanavia, L
    Gawin, D
    COMPUTATIONAL PLASTICITY: FUNDAMENTALS AND APPLICATIONS, PTS 1 AND 2, 1997, : 88 - 100
  • [27] FLUID CONFIGURATIONS IN PARTIALLY SATURATED POROUS-MEDIA
    MCCALL, KR
    GUYER, RA
    PHYSICAL REVIEW B, 1991, 43 (01): : 808 - 815
  • [28] Effective hydraulic conductivity for partially saturated porous media
    Jayawardena, AW
    Dissanayake, PBG
    JOURNAL OF IRRIGATION AND DRAINAGE ENGINEERING, 1999, 125 (02) : 82 - 89
  • [29] Isothermal moisture transport in partially saturated porous media
    vanderZanden, AJJ
    Coumans, WJ
    Kerkhof, PJAM
    Schoenmakers, AME
    DRYING TECHNOLOGY, 1996, 14 (7-8) : 1525 - 1542
  • [30] Dynamic permeability functions for partially saturated porous media
    Solazzi, Santiago G.
    German Rubino, J.
    Jougnot, Damien
    Holliger, Klaus
    GEOPHYSICAL JOURNAL INTERNATIONAL, 2020, 221 (02) : 1182 - 1189