1) Homogeneous half-space
均匀半空间
1.
In this paper, the tensor Green s function of homogeneous half-space is studied for three-dimensional electromagnetic field.
针对三维电磁场,研究了均匀半空间的张量格林函数,导出了该函数不含索末菲积分的张量格林函数解析表达式,由张量格林函数求解Fredholm积分方程,将异常体划分为一系列立方单元,并将该积分方程转化为矩阵方程,从而计算出空间任一点的电场。
2) homogeneous conductive half space
均匀导电半空间
1.
According to physical sense of the tensor Green's function, the three dimensional tensor Green's functions in a homogeneous conductive half space both for time domain and for frequency domain are studied respectively.
从电张量格林函数的物理意义出发 ,在频率域和时间域研究了均匀导电半空间中的电张量格林函数 ,并基于 Fredholm方程分析了三维电磁散射的数值模拟方法。
3) half-space homogeneous model
半空间均匀模型
1.
Considering the inhomogeneousness, stratified and spherical characteristic of earth structure, the co-seismic deformation difference among spherical earth layering model, spherical homogeneous model and half-space homogeneous model has been studied in this paper.
顾及地球结构的非均匀性、分层和球体特性,定量研究了球体分层模型、球体均匀模型、半空间均匀模型分别作用于地震断层(走滑断层,逆冲断层)产生的地表同震变形的差异。
4) Homogeneous half-space condtalr
均匀半空间导体
补充资料：半空
1.半数已空。 2.谓空中。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条