Sciences in Cold and Arid Regions ›› 2015, Vol. 7 ›› Issue (5): 541–546.doi: 10.3724/SP.J.1226.2015.00541

• ARTICLES • 上一篇    

Detection of ground ice using ground penetrating radar method

Gennady M. Stoyanovich, Viktor V. Pupatenko, Yury A. Sukhobok   

  1. Transport Construction Institute, Department of Railway Track and Railway Engineering, Far Eastern State Transport University, Khabarovsk 680000, Russia
  • 收稿日期:2015-03-04 修回日期:2015-05-05 发布日期:2018-11-23
  • 通讯作者: Yury A. Sukhobok, Senior Lecturer of Railway Track and Railway Engineering Department, Far Eastern State Transport University, Khabarovsk 680000, Russia. Tel: +7-962-5852067; E-mail: khvyus@gmail.com E-mail:khvyus@gmail.com

Detection of ground ice using ground penetrating radar method

Gennady M. Stoyanovich, Viktor V. Pupatenko, Yury A. Sukhobok   

  1. Transport Construction Institute, Department of Railway Track and Railway Engineering, Far Eastern State Transport University, Khabarovsk 680000, Russia
  • Received:2015-03-04 Revised:2015-05-05 Published:2018-11-23
  • Contact: Yury A. Sukhobok, Senior Lecturer of Railway Track and Railway Engineering Department, Far Eastern State Transport University, Khabarovsk 680000, Russia. Tel: +7-962-5852067; E-mail: khvyus@gmail.com E-mail:khvyus@gmail.com

摘要: The paper presents the results of a ground penetrating radar (GPR) application for the detection of ground ice. We combined a reflection traveltime curves analysis with a frequency spectrogram analysis. We found special anomalies at specific traces in the traveltime curves and ground boundaries analysis, and obtained a ground model for subsurface structure which allows the ground ice layer to be identified and delineated.

关键词: ground penetrating radar, ground ice, common-offset reflection survey, wide angle reflection and refraction method

Abstract: The paper presents the results of a ground penetrating radar (GPR) application for the detection of ground ice. We combined a reflection traveltime curves analysis with a frequency spectrogram analysis. We found special anomalies at specific traces in the traveltime curves and ground boundaries analysis, and obtained a ground model for subsurface structure which allows the ground ice layer to be identified and delineated.

Key words: ground penetrating radar, ground ice, common-offset reflection survey, wide angle reflection and refraction method

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[1] YuZhong Yang, QingBai Wu, HuiJun Jin, Peng Zhang. δ18O,δD and d-excess signatures of ground ice in permafrost in the Beiluhe Basin on the Qinghai-Tibet Plateau,China[J]. Sciences in Cold and Arid Regions, 2017, 9(1): 38-45.
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