亚稳态
马氏体
材料科学
转化(遗传学)
阶段(地层学)
无扩散变换
冶金
结晶学
化学
微观结构
地质学
生物化学
基因
古生物学
有机化学
标识
DOI:10.1134/s1063774522020249
摘要
The structure of the Fe–Ni alloy formed in the initial stage of transformation of the internal structure of α crystal during heating has been analyzed. A complex multistep character of the formation of intermediate multilayer martensite phase (3R + 18R + ε) is established. Its formation mechanism is compared with the known behavior of the calorimetric slow heating curve of metastable Fe–32%Ni alloy, existing initially in the α + γ state.
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