摘要
通过对富铁的Ａｌ－Ｓｉ－Ｔｉ合金液进行自然沉降和添加锰元素再自然沉降后的组织观察和分析表明：自然沉降前后Ａｌ－Ｓｉ－Ｔｉ合金中铁相含量几乎无变化。
Through the microstructure observation and analysis of original and Mn added Fe rich Al Si Ti melt in natural deposition,it is shown that there is almost no change of iron phase in the original Fe rich Al Si Ti deposited melt while a large number of Fe phase has been removed in the Mn added Fe rich Al Si Ti deposited melt.
出处
《特种铸造及有色合金》
CAS
CSCD
北大核心
1999年第4期3-5,共3页
Special Casting & Nonferrous Alloys
基金
河南省杰出青年科学基金
