This study investigates patterns of Anger development and propagation in la
yered porous media. Fingers are created with interfacial perturbations, for
med by adding a thin zone of regularly varying hydraulic conductivity along
the layer. Simulation results agree qualitatively with those observed in t
wo-dimensional laboratory experiments. In all cases, the formation of insta
bilities requires seeding of perturbations, even if the system is unstably
stratified. A series of simulations show how the shapes of the instabilitie
s differ according to where along the unstable interface the instabilities
form and the layer in which they develop. Pathline analyses indicate how th
e patterns of flow in the domain can be exceedingly complex. Concentration
distributions are influenced by movements of water between layers and the f
ormation of a large convection cell in the lowermost layer. These numerical
investigations reinforce inferences from the experimental studies that cla
ssical stability theory is less useful in determining whether instabilities
will form and what their shape will be. Even with the relatively simple la
yering, patterns of flow and resulting concentrations are complex. (C) 2000
Elsevier Science B.V. All rights reserved.