磁化强度

To cause AN orgANism to respond in a specific mANner to a conditioned stimulus in the absence of AN unconditioned stimulus.

现在，在研究一下在没有背景场的情况下，单个磁芯的磁化强度。

In [4] it was shown that in the process of magnetization of the plate and rollers, the combination of constant and variable magnetic fields for creating a special wave pattern on a plate surface and rollers surface was used.

在[ 4 ]它表明，在这一进程中的磁化强度的钢板和压路机，结合常数和可变的磁场创造一个特殊的波的模式板轧辊表面和表面使用。

The X-ray diffraction patterns were calculated analogically by using Rietveld method and the phase content in rare-earth two phase Nd2Fe14B/α-Fe magnet was determined based on standardless quantitative phase analysis.

稀土双相永磁合金是基于软磁相的高饱和磁化强度和硬磁相的高各向异性的特点，通过两相晶粒在纳米尺度上交换耦合而成的一种纳米晶复合永磁材料，它具有显著的剩磁增强效应，可望获得较高的综合磁性能[1~3]。

In the inversion process, an improved GaussSadel interative method with a weight coefficient determined according prism's berried depth is introduced.

本文采用改进的高斯-赛德尔迭代求解磁化强度矢量层析成像方程，在求解方程中引进了与深度有关的权系数。

In CeMnCuSi/sub 2/, M rapidly increases at 150 K, which suggests a 3d canted ferromagnetic mechnatism.

在CeMnCuSi/sub 2/中，在150K时磁化强度快速地增加，这建议了一个3d倾斜顺磁性的磁结构。

On the contrary, the reversal modes are only determined by the dipolar interaction strength.

发现偶极作用能对系统的磁化强度翻转模式有决定性的作用。

The results show that the global degree, the homocentric degree and the mural uniformity of the plated ICF glass targets were nearly the same as those of the ICF glass targets before plating.

结果表明：对ICF玻璃靶丸进行化学镀处理，其球形度、同心度和壁厚均匀性都与化学镀前未发生明显改变，其饱和磁化强度和矫顽力分别为3.883×10^(-3)A/g和1.046×10^(-3)T。

With increasing χ, the lattice constantincreases and the magnetization monotonically decreases.

随着x的增加，晶格常数增大，而磁化强度I_s单调地减小。

The least loss of the magnetization due to As diffusion has been found forFe overlayer grown on the surface covered with stable GaxS layer with well-ordered sites andlittle excess As.

结果显示，表面退火后富Ga的GaxS钝化层的状态以及表面富余As的存在，决定了生长在这一衬底上Fe薄膜的磁化强度。

In addition, the remanent magnetization vector field can not be transformed into potential field in general.

对地磁场的观测是在地表或卫星高度这样的球面上完成的，且岩石层的剩余磁化强度矢量场一般不能转换为位势场，因此需要研究球面各向同性随机矢量场。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。