The long-wavelength instability for thermocapillary-driven convection in tw
o dimensions is studied numerically. The system under consideration consist
s of a horizontal periodical liquid layer bounded from below by a rigid wal
l and from above by a deformable free surface. The liquid is heated from th
e bottom wall and cooled from above. The problem can be approximated by the
Stokes equation and has two dimensionless parameters, One parameter is the
dynamic Bond number which is the ratio between gravity and thermocapillary
force. The other is the static Bond number, which describes the ratio betw
een gravity and the surface tension. Using the boundary integral method we
present full-scale direct numerical simulations of the long-wavelength Mara
ngoni instability in two dimensions. The time evolution of the free surface
leads to the formation of drained regions (so-called "dry spots"). The sim
ulations demonstrate a remarkable complexity of the touchdown process, invo
lving a deep cascade from large to increasingly small structures. In the be
havior of the minimum height of the interface h(min), at large time simple
scaling dependence on time was not observed. Extrapolation of h(min) exhibi
ts infinite-time singularity. The dependence of the size of drained region
on the parameters is discussed, (C) 1999 American Institute of Physics. [S1
070-6631(99)01806-1].