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读了陈伯舫先生《对“磁暴短周期感应场和佘山地区地幔电导率”一文的讨论》的文章,颇有收益,表示感谢。为了有利讨论和多求帮助,有关问题答覆如下。 一维水平成层电导率模型,尽管电导率结构层次有间断,但地表电磁阻抗随单一源场激励周期而变化的理论曲线却是连续的,反映了模型对场源的综合响应。研究理论曲线
After reading Mr. Chen Bo-Fang’s article “Discussion on” Short-period Induction Field of Magnetosphere and Mantle Conductivity in Sheshan Area, "the article is quite profitable. In order to facilitate discussion and seek more help, the answers to the relevant questions are as follows. The one-dimensional horizontal stratified conductivity model shows that although the conductivity structure is discontinuous, the theoretical curve of surface electromagnetic impedance changes with the excitation period of a single source field is continuous, which reflects the comprehensive response of the model to the field source. Research theoretical curve