Hg0.84Zn0.16Te crystals were grown vertically by directional solidific
ation in a 5 T axial magnetic field. Growth in an identical thermal en
vironment but without the presence of magnetic field was also performe
d. The ingots were partially grown and quenched to preserve the growth
interface shapes. The effects of magnetic damping on the buoyancy-dri
ven convective flows in the melt were investigated by examining the qu
enched-in interface shapes and by measuring the composition variations
along the axial and radial directions of the grown ingots and compari
ng them with those of ingots grown without a field.