Japan Geoscience Union Meeting 2023

Presentation information

[E] Online Poster

S (Solid Earth Sciences ) » S-EM Earth's Electromagnetism

[S-EM14] Electric, magnetic and electromagnetic survey technologies and scientific achievements

Wed. May 24, 2023 1:45 PM - 3:15 PM Online Poster Zoom Room (4) (Online Poster)

convener:Kiyoshi Baba(Earthquake Research Institute, The University of Tokyo), Tada-nori Goto(Graduate School of Science, University of Hyogo), Yuguo Li(Ocean University of China), Wiebke Heise(GNS Science, PO Box 30368, Lower Hutt, New Zealand)

On-site poster schedule(2023/5/23 17:15-18:45)

1:45 PM - 3:15 PM

[SEM14-P22] Estimation of subsurface temperature distribution from resistivity and seismic wave velocity using a neural network

*Souma Yamamoto1, Tada-nori Goto1 (1.University of Hyogo)

Keywords:Neural networks, Resistivity, Temperature estimation

Subsurface temperature distributions are necessary in geothermal development. It is fundamental information not only to confirm geothermal reservoirs, but also to discuss hydrothermal circulation patterns before and after geothermal development. Temperature measurement requires the drilling. In some cases, they are more than 3,000 m deep. However, the number of wells is limited due to the high cost and environmental impact by the drilling. In recent years, neural networks have been used to estimate temperature. In this study, we try to estimate the subsurface temperature distribution by applying neural networks to the known temperature. The temperature obtained by a numerical simulation is used. The resistivity and seismic velocity distribution based from this temperature distribution are also used additionally, which are based on the results of rock physical property measurements. First, a learning model was created to estimate temperature using only location data, and then a learning model was created to estimate temperature using location data and resistivity data. At the same time, a learning model was also created for location data and seismic wave velocity. Here, for the neural network, the number of neurons layers in the middle layer and the number of neurons per layer were varied, and the cost function and test data were verified to see how the accuracy of learning changes. The results showed that temperature estimation using resistivity data in addition to location data was more accurate in estimating temperature distribution. In the future, we plan to apply the actual data to the neural network.