高密度电法在输电线路塔基基础附近多年冻土探测中的应用
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游艳辉 1( ), 李党民 2, 单波 2, 田生祥 3, 王新斌 1, 俞祁浩 1( )
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Application of high density electrical resistivity tomography in investigating the permafrost around tower foundations of power transmission line
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Yanhui YOU 1( ), Dangmin LI 2, Bo SHAN 2, Shengxiang TIAN 3, Xinbin WANG 1, Qihao YU 1( )
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图5. 活动层冻结时不同装置的高密度电法反演结果(黑色虚线表示正演模型结构)
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Fig. 5. Inversion results of high density electrical resistivity tomography using different types of arrays when the active layer is frozen: Wenna alpha (a), Wenna beta (b), dipole-dipole (c) and Schlumberger (d) (The black dashed lines represent configurations in forward modeling)
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