Topological groundwater hydrodynamics is an emerging subdiscipline in the m
echanics of fluids in porous media whose objective is to investigate the in
variant geometric properties of subsurface flow and transport processes. In
this paper, the topological characteristics of groundwater flows governed
by the Darcy law are studied. It is demonstrated that: (i) the topological
constraint of zero helicity density during flow is equivalent to the Darcy
law; (ii) both steady and unsteady groundwater Rows through aquifers whose
hydraulic conductivity is an arbitrary scalar function of position and time
are confined to surfaces on which the streamlines of the flow are geodesic
curves; (iii) the surfaces to which the flows are confined either are flat
or are tori; and (iv) chaotic streamlines are not possible for these flows
, implying that they are inherently poorly mixing in advective solute trans
port. (C) 2001 Elsevier Science Ltd. All rights reserved.