apparent chargeability，是指在多种岩石、矿石存在的情况下(即所谓介质不均匀时)测得的极化率。它是表示直流激发极化法观测结果的一个参数。
实践证明，利用视电阻率法和激发极化法相结合的方法找寻地下水是非常成功的。
Practice proved the combined apparent resistivity and induced polarization method to find underground water was very successful.
本文的重点是通过建立理论模型，进行正反演并寻找在这些模型条件下TE和TM模式极化视电阻率曲线的变化规律。
The paper put emphasis on carrying forward and inversion and finding changing laws of polarization apparent resistivity curve with TE and TM modes by constructing theoretic models.
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