The anisotropies of magnetization curves and magnetic critical current are analysed in detail.
详细分析了磁化曲线和磁临界电流的各向异性。
2
The internal stress fields and the stress-magnetic anisotropies in different regions of the amorphous ribbon were calculated theoretically.
从理论上计算了非晶态薄带中不同区域的内应力场和应力磁各向导性。
3
Seismic velocity anisotropies are mainly caused by lattice preferred orientation( LPO) , shape preferred orientation( SPO) of the major minerals, and oriented microcracks.