2) homogeneous conductivity
均匀电导率
3) Transverse inhomogeneous structure of conductivity
电导率横向不均匀结构
4) transversal heterogeneity of electro-conductivity
电导率的横向非均匀性
5) continuous variation of conductivity within each block
电导率分块连续
1.
The finite element method is used for modeling 2-D MT field on a geoelectrical model with continuous variation of conductivity within each block.
用有限元法进行电导率分块连续变化的二维大地电磁的模拟。
6) nonuniform conductive medium
不均匀导电媒质
1.
Gauss Theorem and the principles of charge conservation are used to derive the charge distribution of nonuniform conductive medium in electric field.
利用高斯定理和电荷守恒原理,求得电场中不均匀导电媒质的电荷分布规律,发现电荷分布与电场强度大小和方向及媒质的不均匀性有关,与初始条件无关,而且稳定电场和似稳电场中电荷分布是相同的。
补充资料：电导率(见电阻率)
电导率(见电阻率)
conductivity
d!日nd日O}已电导率(eonduetivity)见电阻率。
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