Replacement of annular domain with trapezoidal domain in computational modeling of nonaqueous-phase-liquid dissolution-front propagation problems

被引:0
作者
Chong-bin Zhao
Thomas Poulet
Klaus Regenauer-Lieb
机构
[1] Central South University,Computational Geosciences Research Centre
[2] CSIRO Division of Earth Science and Resource Engineering,School of Earth and Environment
[3] The University of Western Australia,undefined
来源
Journal of Central South University | 2015年 / 22卷
关键词
nonaqueous phase liquid (NAPL); trapezoidal domain; computational simulation; dissolution front instability;
D O I
暂无
中图分类号
学科分类号
摘要
In order to simulate the instability phenomenon of a nonaqueous phase liquid (NAPL) dissolution front in a computational model, the intrinsic characteristic length is commonly used to determine the length scale at which the instability of the NAPL dissolution front can be initiated. This will require a huge number of finite elements if a whole NAPL dissolution system is simulated in the computational model. Even though modern supercomputers might be used to tackle this kind of NAPL dissolution problem, it can become prohibitive for commonly-used personal computers to do so. The main purpose of this work is to investigate whether or not the whole NAPL dissolution system of an annular domain can be replaced by a trapezoidal domain, so as to greatly reduce the requirements for computer efforts. The related simulation results have demonstrated that when the NAPL dissolution system under consideration is in a subcritical state, if the dissolution pattern around the entrance of an annulus domain is of interest, then a trapezoidal domain cannot be used to replace an annular domain in the computational simulation of the NAPL dissolution system. However, if the dissolution pattern away from the vicinity of the entrance of an annulus domain is of interest, then a trapezoidal domain can be used to replace an annular domain in the computational simulation of the NAPL dissolution system. When the NAPL dissolution system under consideration is in a supercritical state, a trapezoidal domain cannot be used to replace an annular domain in the computational simulation of the NAPL dissolution system.
引用
收藏
页码:1841 / 1846
页数:5
相关论文
共 47 条
  • [1] Miller C T(1990)Dissolution of trapped nonaqueous phase liquids: Mass transfer characteristics [J] Water Resources Research 26 2783-2796
  • [2] Poirier-Mcneil M M(1993)Mass transfer from nonaqueous phase organic liquids in water-saturated porous media [J] Water Resources Research 29 833-845
  • [3] Mayer A S(1994)An experimental investigation of nonaqueous phase liquid dissolution in saturated subsurface systems: Transient mass transfer rates [J] Water Resources Research 30 321-332
  • [4] Geller J T(1994)An experimental study of complete dissolution of a nonaqueous phase liquid in saturated porous media [J] Water Resources Research 30 307-320
  • [5] Hunt J R(1996)Dissolution fingering during the solubilization of nonaqueous phase liquids in saturated porous media: 2. Experimental observations [J] Water Resources Research 32 1929-1942
  • [6] Powers S E(2002)Evolving interface between clean and nonaqueous phase liquid (NAPL)-contaminated regions in two-dimensional porous media [J] Water Resources Research 38 1093-1106
  • [7] Abriola L M(1998)Effects of flow bypassing and nonuniform NAPL distribution on the mass transfer characteristics of NAPL dissolution [J] Water Resources Research 34 1657-1673
  • [8] Weber W J(1999)Factors affecting bank formation during surfactant-enhanced mobilization of residual NAPL [J] Environmental Science and Technology 33 2440-2446
  • [9] Imhoff P T(2008)The influence of wettability on NAPL dissolution fingering [J] Advances in Water Resources 31 1687-1696
  • [10] Jaffe P R(1996)iDissolution fingering during the solubilization of nonaqueous phase liquids in saturated porous media: 1. Model predictions [J] Water Resources Research 32 1919-1928