Japan Geoscience Union Meeting 2018

Presentation information

[JJ] Oral

H (Human Geosciences) » H-TT Technology & Techniques

[H-TT19] New Developments in Shallow Geophysics

Thu. May 24, 2018 1:45 PM - 3:15 PM 101 (1F International Conference Hall, Makuhari Messe)

convener:Kyosuke Onishi(Public Works Research Institute), Kunio Aoike(Oyo corporation), Keisuke Inoue(国立研究開発法人 農業・食品産業技術総合研究機構, 共同), Tishiyuki Yokota(National Institute of Advanced Industrial Science and Technology), Chairperson:Yokota Toshiyuki, Aoike Kunio

2:45 PM - 3:00 PM

[HTT19-11] Estimation of thermal resistance of soil around underground power transmission line using geophysical surveys

*Koichi Suzuki1 (1.Central Reseach Institute of Electric Power Industry)

Keywords:Underground power transmission line, Soil thermal resistance, Geophysical exploration, Electrical resistivity, S-wave velocity

The thermal resistance of soil around underground power transmission lines is an important parameter affecting transmission capacity. Thermal resistance of soil is conventionally measured by inserting a heating element and a thermocouple into a borehole. Because, this method is expensive, the thermal resistance is often assumed to be the standard value (80℃cm/W). However, this is a conservative estimate, which inadvertently leads to the condition of cables that have a large diameter than is required. Kubota et al. (2015) and Suzuki et al. (2015) suggested a method to estimate the thermal resistance from resistivity data using an empirical formula and artificial soil samples. However, it is important to use the measured resistivity and thermal resistance of actual soil samples surrounding the survey lines. In this study, we propose a new soil thermal resistance model composed of sand particles, clay particles, pore water, and air which was based on the unconsolidated sand model (Avseth, 2005). The theoretical thermal resistance derived by this model is comparable to the saturation–thermal resistance relationship measured by laboratory tests performed on artificial unconsolidated soil samples. Additionally, we propose a method to estimate the thermal resistance profile by combining the S-wave velocity–porosity (Avseth, 2005) and resistivity–porosity relationships (Katsube and Hume, 1983). This method was applied to geophysical survey data obtained using the surface wave and the electrical methods in the field where underground power transmission lines are planned. Thermal resistance profile obtained using integrated geophysical data matches the values measured directly in the borehole drilled along the survey line (Fig.1). In conclusion, this method is suitable for use in designing power transmission cables.

Avseth, P., Mukerji, T. and Mavko, G. (2005): Quantitative seismic interpretation, Cambrige University Press.
Katsube, T. J., and Hume, J. P. (1983): Electrical resistivities of rocks from Chalk River, Proc. Ws. Geophys. Geosci. Res. at Chalk River, 105-114.
K. Kubota, K.Suzuki, H. Kaieda, T. Yamamoto, S. Yamaguchi, and Y. Fujimitsu (2015): Evaluation of soil specific thermal resistance around underground power transmission lines using geophysical surveys –Relationship between thermal resistance and electrical resistivity -, Geophysical Exploration, 68, 131-148.
K. Suzuki, K.Kubota, H.Kaieda, T. Yamamoto, and S. Yamaguchi (2015): Estimation of thermal resistance of soil around underground power transmission line using geophysical explorations - Application to the sites of underground power transmission lines -, Geophysical Exploration, 68, 177-188.