Stability analysis of gravity-driven infiltrating flow

被引:70
|
作者
Egorov, AG
Dautov, RZ
Nieber, JL
Sheshukov, AY
机构
[1] Kazan VI Lenin State Univ, Chebotarev Res Inst Math & Mech, Kazan 420008, Russia
[2] Kazan VI Lenin State Univ, Fac Computat Math & Cybernet, Kazan 420008, Russia
[3] Univ Minnesota, Dept Agr & Biosyst Engn, St Paul, MN 55108 USA
关键词
Richards' equation; gravity-driven flow; dynamic capillary pressure; traveling wave solution; stability analysis; POROUS-MEDIA; PREFERENTIAL FLOW; CAPILLARY-PRESSURE; WATER-MOVEMENT; LAYERED SOILS; STATE; MECHANISM; PERSISTENCE; SIMULATION; EQUATIONS;
D O I
10.1029/2002WR001886
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
[1] Stability analysis of gravity-driven unsaturated flow is examined for the general case of Darcian flow with a generalized nonequilibrium capillary pressure-saturation relation. With this nonequilibrium relation the governing equation is referred to as the nonequilibrium Richards equation (NERE). For the special case where the nonequilibrium vanishes, the NERE reduces to the Richards equation (RE), the conventional governing equation for describing unsaturated flow. A generalized linear stability analysis of the RE shows that this equation is unconditionally stable and therefore not able to produce gravity-driven unstable flows for infinitesimal perturbations to the flow field. A much stronger result of unconditional stability for the RE is derived using a nonlinear stability analysis applicable to the general case of heterogeneous porous media. For the general case of the NERE model, results of a linear stability analysis show that the NERE model is conditionally stable, with lower-frequency perturbations being unstable. A result of this analysis is that the nonmonotonicity of the pressure and saturation profile is a requisite condition for flow instability.
引用
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页数:14
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