GaSb:Te and GaInSb samples have been solidified! under microgravity conditi
ons during the D2 Spacelab mission. Experimental design and parameters are
described. Analysis of the thermal data taken during the flight, associated
to numerical simulations of heat transfer in the experiment, with the help
of FIDAP, gave the experimental conditions (thermal gradients and growth r
ate).
Quantitative chemical analyses of the samples show a chemical segregation c
haracteristic of strong mixing in the melt during crystal growth. Silica cr
ucibles with an internal screw thread groove on the inner wall were used in
order to get dewetting of samples from the crucible. It was therefore supp
osed that Marangoni convection on the free surface associated to the groove
might have been the source of convection. This hypothesis has been studied
by numerical simulation using FIDAP and the velocity field obtained is in
agreement with a strong perturbation of the solutal boundary layer ahead th
e solid-liquid interface. This can explain the observed chemical segregatio
n.