再结晶(地质)
材料科学
铜
成核
退火(玻璃)
合金
冶金
大气温度范围
降水
粒度
晶界
微观结构
热力学
地质学
气象学
古生物学
物理
作者
B.J. Duggan,W. T. Roberts
出处
期刊:Metal science
[Informa]
日期:1975-01-01
卷期号:9 (1): 449-454
被引量:12
标识
DOI:10.1179/030634575790444711
摘要
Textures have been determined in an iron–1·2 % copper alloy and in a reference material with copper at a low level after heavy cold-rolling reduction and annealing. The main process variable examined was the rate of heating to the annealing temperature. Interactions between precipitates, nuclei, and migrating grain boundaries resulted in a range of recrystallization textures in the Fe–Cu alloy from almost random after rapid heating to well-defined textures after slower heating rates. The most noticeable variation was in the amount of near-{100} orientation, which was very low in a simulated box anneal, but which was strong when the heating programme involved holding at a temperature high in the recovery range. The observed differences in recrystallization textures are ascribed to the heterogeneous precipitation of Cu and to different nucleation processes for near-{111} and near-{100}grains.
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