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Groundwater Potential in the Central District of Tokyo

  • Tomochika Tokunaga
Part of the cSUR-UT Series: Library for Sustainable Urban Regeneration book series (LSUR, volume 2)

Abstract

Tokyo, the capital of Japan, is situated in the south-western part of the Kanto Plain, a large, flat plain with an area of approximately 16,000 km2 (Fig. 4.1). The underground environment beneath the central district of Tokyo has been changing dramatically in accordance with the continuous increase and heavy use of underground space. Because of the complex interaction between the change of the groundwater environment and human activities underground, society has been affected in various ways. This chapter describes the temporal change of the groundwater environment and associated problems in the central district of Tokyo. Then, new techniques that are considered to be usable for the strategic management of groundwater resources are briefly presented. We believe that transferring our experience regarding the central districts of Tokyo to presently developing and expanding urban areas in the similar geological/hydrogeological settings, i.e., Bangkok, Hanoi and so on, is crucial to achieve sustainable urban development.

Keywords

Groundwater Level Pore Water Pressure Land Subsidence Unconfined Aquifer Groundwater Potential 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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References

  1. Aichi M, Tokunaga T (2006) A nested modeling scheme for high-resolution simulation of the aquitard compaction in a regional groundwater extraction field H41B-0399, AGU Fall Meeting, San Francisco, CA, December 11–15Google Scholar
  2. Aichi M, Hayashi T, Tokunaga T (2007) A nested modeling scheme to integrate regional groundwater flow and local groundwater flow/land subsidence; an application to the Tokyo metropolitan area, Japan. H53E-03, AGU Joint Assembly, Acapulco, Mexico, May 21–25Google Scholar
  3. Colesanti C, Ferretti A, Novali E, Prati C, Rocca E (2003) SAR monitoring of progressive and seasonal ground deformation using the permanent scatterers technique. IEEE Trans. Geosci Remote Sens 40:1685–1701CrossRefGoogle Scholar
  4. Endo T, Ishii M (1984) Hydrogeology and subjects caused by recovering of groundwater level in Tokyo (in Japanese with English abstract). J Japan Soc Eng Geol 25:111–20Google Scholar
  5. Endo T, Kawashima S, Kawai M (2001) Historical review of development of land subsidence and its cease in Shitamachi Lowland, Tokyo. J Japan Soc Eng Geol 42:74–84Google Scholar
  6. Ferretti A, Novali F, Bürgmann R, Hilley G, Prati C (2004) InSAR permanent scatterer analysis reveals ups and downs in San Francisco Bay area. EOS 85:317–24CrossRefGoogle Scholar
  7. Ferretti A, Prati C, Rocca E (2000) Nonlinear subsidence rate estimation using permanent scatterers in differential SAR interferometry. IEEE Trans Geosci Remote Sens 38:2202–12CrossRefGoogle Scholar
  8. Ferretti A, Prati C, Rocca E (2001) Permanent scatterers in SAR interferometry. IEEE Trans Geosci Remote Sens 30:8–20CrossRefGoogle Scholar
  9. Fetter CW (1994) Applied hydrogeology, 3rd edn. Prentice Hall, p 691Google Scholar
  10. Freeze RA and Cherry JA (1979) Groundwater. Prentice Hall, p 604Google Scholar
  11. Hashimoto T (2004) Groundwater problems in Osaka plain (in Japanese). In: Proceedings of the 2004 Symposium, Japan Soc Eng Geol, pp 1–7Google Scholar
  12. Hayashi T, Tokunaga T, Aichi M, Shimada J, Taniguchi M, Effects of human activities and urbanization on groundwater environments: An example from the aquifer system of Tokyo and the surrounding area. Sci Total Env, submittedGoogle Scholar
  13. Heath RC (1987) Basic ground-water hydrology. Technical report. US Geological Survey (http://pubs.usgs.gov/wsp/wsp2220/pdf/wsp 2220.pdf)
  14. Hirose M, Kawagoe T, Kiya H (2004). A relation of a groundwater level change for construction and underground structures (in Japanese). In: Proceedings of Ann. Meet., Japan Soc Eng Geol. pp 419–422Google Scholar
  15. Hoffman J, Zebker HA, Galloway DL, Amelung F (2001) Seasonal subsidence and rebound in Las Vegas Valley, Nevada, observed by synthetic aperture radar interferometry. Water Resour Res 37:1551–1566CrossRefGoogle Scholar
  16. Imaizumi M, Komae T, Nishira S (2000) Evaluation of recharge mechanism of confined groundwater using long term tritium concentration records in the Metropolis of Tokyo (in Japanese with English abstract). J Japan Soc Eng Geol 41:81–102Google Scholar
  17. Institute of Civil Engineering of Tokyo Metropolitan Government (1977) Synthetic ground chart in Tokyo Metropolis (in Japanese). Gihodo PublGoogle Scholar
  18. Kajino N, Tokunaga T, Mogi G, Yasumochi S, Bando K (2004). Research on the pavement cooling system using groundwater (in Japanese). In: Proc Ann. Meet. Japan Soc Eng Geol, pp 109–112Google Scholar
  19. Kawashima S (2001) Temporal change of groundwater level in Tokyo. Found Eng Equip 29(11):77–79Google Scholar
  20. Kayane I (1994) Study on interaction between surface and groundwater in Tamagawa River system (in Japanese) (Report submitted to Tokyu Foundation for Better Environment)Google Scholar
  21. Kurasawa N (2001) Examples of countemeasure constructions to overcome groundwater pressure due to the recovery of groundwater level—Ueno underground station and Tokyo underground station (in Japanese). Found Eng Equip 29(11):72–76Google Scholar
  22. Mitamura M, Takahashi H (1993) Obstacles caused by groundwater development (in Japanese). In: Research Group on Water Budget (ed). Groundwater Resources and Environments Kyoritsu Publ, pp 28–38Google Scholar
  23. Peltzer G, Rosen P, Rogez F, Hudnut K (2004) Postseismic rebound in fault step-overs caused by pore fluid flow. Science 273:1202–1204CrossRefGoogle Scholar
  24. Shimada J (2002) The mechanism of unsaturated flow through a volcanic ash layer under humid climatic conditions. Hydrol Proc 2:43–59CrossRefGoogle Scholar
  25. Shimada J, Tang C, Tanaka T, Yang Y, Sakura Y, Song X, Liu C (2002) Irrigation caused groundwater drawdown beneath the North China Plain. In: Proceedings of Int. Groundwater Conf., Darwin, Australia, pp 1–7Google Scholar
  26. Shimizu M (2004) Groundwater problems related to construction of underground structures (in Japanese). In: Proceedings of 2004 Symp., Japan Soc Eng Geol, pp 26–33.Google Scholar
  27. Shindo S (1972) Groundwater in Southern part of the Kanto Plain (in Japanese). Soil Mech Found Eng 20(5):25–11Google Scholar
  28. Stancliffe RPW, van der Kooij MWA (2001) The use of satellite-based radar interferometry to monitor production activity at the Cold Lake heavy oil field, Alberta, Canada. Amer Assoc Petrol Geol Bull 85:781–93Google Scholar

Copyright information

© Springer 2008

Authors and Affiliations

  • Tomochika Tokunaga
    • 1
  1. 1.Department of Environment Systemsthe University of TokyoTokyoJapan

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