⟨110⟩ dendrite growth in aluminum feathery grains

被引:87
作者
Henry, S [1 ]
Jarry, P
Rappaz, M
机构
[1] Ecole Polytech Fed Lausanne, Met Phys Lab, CH-1015 Lausanne, Switzerland
[2] Pechiney Ctr Rech Voreppe, F-38340 Voreppe, France
来源
METALLURGICAL AND MATERIALS TRANSACTIONS A-PHYSICAL METALLURGY AND MATERIALS SCIENCE | 1998年 / 29卷 / 11期
关键词
D O I
10.1007/s11661-998-0321-9
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Automatic indexing of electron backscatterrd diffraction patterns, scanning electron microscopy, and optical microscopy observations have been carried out on aluminum-magnesium-silicon, aluminum-copper, and aluminum-silicon alloys directionally solidified or semicontinuously cast using the direct chill casting process. From these combined observations, it is shown that the feathery grains are made of [110] primary dendrite trunks (e.g., [01 (1) over bar]) split in their centers by a coherent (111) twin plane. The average spacing of the dendrite trunks in the twin plane (about 10 to 20 mu m) is typically one order of magnitude smaller than that separating successive rows of trunks (or twin planes). The [01 (1) over bar] orientation of these trunks is close to the thermal gradient direction (typically within 15 deg)-a feature probably resulting from a growth competition mechanism similar to that occurring during normal [100] columnar dendrite growth. On both sides of these trunks, secondary dendrite arms also grow along [110] directions. Their impingement creates wavy noncoherent twin boundaries between the coherent twin planes. In the twin plane, evidence is shown that [110] branching mechanisms lead to the propagation of the twinned regions, to the regular arrangement of the primary dendrite trunks along a [(2) over bar 11] direction, and to coherent planar twin boundaries. From these observations, it is concluded that the feathery grains are probably the result of a change from a normal [100] to a [110] surface tension/attachment kinetics anisotropy growth mode. This change might be induced by the added solute elements, by the local solidification conditions (thermal gradient, growth rate, and melt convection), and possibly by the help of the twin plane itself. Convection in the melt could also play a role in the symmetrization of the [110] growth directions of the side arms. Finally, the proposed mechanisms of feathery grain growth are further supported by the observation of [110] dendrite growth morphologies in thin aluminum-zinc coatings.
引用
收藏
页码:2807 / 2817
页数:11
相关论文
共 29 条
[1]  
ALTENPOHL D, 1968, MEM ETUD SCI REV MET, V65, P579
[2]  
ANADA H, 1975, J JPN I LIGHT MET, V36, P562
[3]  
[Anonymous], 1965, INTRO DISLOCATIONS
[4]  
AUST KT, 1952, JOM-J MIN MET MAT S, V4, P865, DOI 10.1007/BF03398154
[5]  
BACKERUD L, 1990, SOLIDIFICATION CHARA, P39
[6]   THE FORMATION OF PATTERNS IN NONEQUILIBRIUM GROWTH [J].
BENJACOB, E ;
GARIK, P .
NATURE, 1990, 343 (6258) :523-530
[7]  
Bunge H.J., 1985, PREFERRED ORIENTATIO, P73, DOI [10.1016/B978-0-12-744020-0.50009-2, DOI 10.1016/B978-0-12-744020-0.50009-2]
[8]   THEORY OF CRYSTAL GROWTH AND INTERFACE MOTION IN CRYSTALLINE MATERIALS [J].
CAHN, JW .
ACTA METALLURGICA, 1960, 8 (08) :554-562
[9]   STATIONARY GROWTH SHAPES OF NH-4CL DENDRITES [J].
CHAN, SK ;
REIMER, HH ;
KAHLWEIT, M .
JOURNAL OF CRYSTAL GROWTH, 1976, 32 (03) :303-315
[10]   SOME CRYSTALLOGRAPHIC OBSERVATIONS OF GROWTH-TWINNED DENDRITES IN ALUMINUM [J].
EADY, JA ;
HOGAN, LM .
JOURNAL OF CRYSTAL GROWTH, 1974, 23 (02) :129-136