The penetration of light nonaqueous phase liquids (LNAPLs) in quantiti
es that lead to an accumulation in the form of a lens above the water
table is considered. First, the three-phase vertical gravity-capillary
equilibrium of water, NAPL, and air above the water table is specifie
d. The hypothesis of 'vertical equilibrium phase distribution' is used
to derive averaged asymptotic equations describing NAPL flow as a thi
n lens floating above the water table. Some problems of unsteady NAPL
lens movement and the development of a NAPL mound, spreading along an
inclined or horizontal phreatic surface are discussed and the analytic
al solutions are obtained.