Articles | Volume 382
https://doi.org/10.5194/piahs-382-303-2020
https://doi.org/10.5194/piahs-382-303-2020
Pre-conference publication
 | 
22 Apr 2020
Pre-conference publication |  | 22 Apr 2020

Effect of brine injection into shallow formation on land subsidence in the Southern Kanto gas field, in Japan

Kenjiro Kawano, Hiroshi Iwamoto, Daisuke Murai, Takahiro Egami, Tatsuo Shimamoto, Yuji Hayashi, and Tsutomu Nakagawa

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Pilot test of study on brine injection into shallow formation for mitigating land subsidence in the Southern Kanto Gas Field in Japan
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Cited articles

Adachi, M., Matsuyama, R., Nakagawa, T., Kuroshima, S., Ogatsu, T., and Adachi, R.: Simulation study of the in-situ formation deformation behavior of a shallow formation in the Southern Kanto Natural gas field, Chiba Prefecture, Japan, Proc. IAHS, 372, 421–424, 2015. 
Geological Survey Of Japan (GSJ): AIST: Fuel Resource Map “Kanto Region”, 2015. 
Ikeda, H., Kunisue, S., Nohara, D., Ooba, K., and Kokubo, T.: In-situ formation compaction monitoring in deep reservoirs by use of fiber optics, Proc. IAHS, 372, 393–394, https://doi.org/10.5194/piahs-372-393-2015, 2015. 
Nakagawa, T., and Sekine K.: Study on Enhanced Gas Production with Controlling Land Subsidence in Water-Dissolved Natural Gas Field, JOGMEC Oil & Gas Technical Activity Report April 2017–March 2018, 128–131, 2018. 
Takeuchi, S., Morikawa, M., Yazawa, N., and Tazaki, Y.: Deformation behavior of the reservoir mudstone in the Minami-Kanto gas field, J. Jpn. Assoc. Petrol. Technol., 66, 643–651, 2001 (in Japanese). 
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Short summary
We plan to construct in situ formation deformation monitoring wells for shallow formation. In the pilot test, production and injection will be conducted to make the formation deform. Based on the result of the pilot test, we will investigate whether the compaction behavior was perfectly elastic or not. In the future, we would like to select the suitable constitutive equation for this gas field based on the obtained data and construct a prediction methodology to control subsidence.