As shown in Fig.1, precipitates microstructure confirms that near solvus temperature precipitation can limit grain boundary precipitation.
由调整温度, 五谷雨雪由生核能量限制并且唯一
雨雪存在。
As shown in Fig.1, precipitates microstructure confirms that near solvus temperature precipitation can limit grain boundary precipitation.
由调整温度, 五谷雨雪由生核能量限制并且唯一
雨雪存在。
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