We study power-law growth of step bunches produced by the drift of adatoms.
When evaporation of the adatoms is neglected (conserved system), the terra
ce width between the bunches increases as L proportional to t(beta) with be
ta approximate to 1/2 through a hierarchical bunching. The time dependence
of L is not affected by the form of step repulsion. When the adatoms evapor
ate to the atmosphere (non-conserved system), the motion of the steps chang
es drastically: isolated steps are always present in large terraces, and co
llision of the steps with the bunches is repeated. When the drift of adatom
s is fast, the terrace width grows by 'effective coalescence' of the bunche
s as L proportional to t(1/2), Similarly to the bunching in the conserved s
ystem. When the drift of adatoms is slow, the bunches grow by 'bunch size e
xchange' with beta smaller than and the terrace width saturates in a late s
tage. The exponent beta increases with increasing drift velocity and approa
ches beta approximate to 1/2. (C) 1999 Elsevier Science B.V. All rights res
erved.