We present a numerical study of transient natural convection in a rect
angular open thermosyphon having asymmetric thermal boundary condition
s. One vertical wall of the thermosyphon is either heated by constant
heat flux ( ''warmup '') or cooled by convection to the surroundings (
''cooldown ''). The top of the thermosyphon is open to a large reserv
oir of fluid at constant temperature. The vorticity, energy, and strea
m-function equations are solved by finite differences on graded mesh.
The ADI method and iteration with overrelaxation are used. We find tha
t the thermosyphon performs quite differently during cooldown compared
with warmup. In cooldown, flows are mainly confined to the thermosyph
on with little momentum and heat exchange with the reservoir. For warm
up, the circulation resembles that for a symmetrically heated thermosy
phon where there is a large exchange with the reservoir. The differenc
e is explained by the temperature distributions. For cooldown, the flu
id becomes stratified and the resulting stability reduces motion. In c
ontrast, the transient temperature for warmup does not become stratifi
ed but generally exhibits the behavior of a uniformly heated vertical
plate. For cooldown and Ra > 10(4), time-dependent heat transfer is pr
edicted by a closed-form expression for one-dimensional conduction, wh
ich shows that Nu --> Bi1/2/A in the steady-state limit. For warmup, t
ransient heat transfer behaves as one-dimensional conduction for early
times and at steady state and for Ra greater-than-or-equal-to 10(5),
can be approximated as that for a uniformly heated vertical plate.