Abstract

Abstract. Over 40 million people live on and exploit the groundwater resources of the Kanto Plain. The Plain encompasses metropolitan Tokyo and much of Chiba Prefecture. Useable groundwater extends to the base of the Kanto Plain, some 2500 to 3000 m below sea level. Much of the Kanto Plain surface is at sea level. By the early 1970s, with increasing urbanization and industrial expansion, local overdraft of groundwater resources caused major ground subsidence and damage to commercial and residential structures as well as to local and regional infrastructure. Parts of the lowlands around Tokyo subsided to 4.0 m below sea level; particularly affected were the suburbs of Funabashi and Gyotoku in western Chiba. In the southern Kanto Plain, regulations, mainly by local government and later by regional agencies, led to installation of about 500 monitoring wells and almost 5000 bench marks by the 1990's. Many of them are still working with new monitoring system. Long-term monitoring is important. The monitoring systems are costly, but the resulting data provide continuous measurement of the "health" of the Kanto Groundwater Basin, and thus permit sustainable use of the groundwater resource.

Highlights

  • The Kanto plain is called “the Kanto fore-arc submarine basin” or “the paleo-Kanto-submarine basin”, based on surrounding geologic and physiographic features such as Nasu Volcanic Zone, Fuji Volcanic Zone, Japan trench and Izu-Ogasawara Trench (Nirei et al, 1990)

  • Over 40 million people live on the Kanto plain which includes the Tokyo metropolis

  • The used volume shows a little difference based on each autonomy on the Kanto groundwater basin and the scale of the volume used by the agriculture and the building is different at each prefectural government

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Summary

Introduction

The Kanto plain is called “the Kanto fore-arc submarine basin” or “the paleo-Kanto-submarine basin”, based on surrounding geologic and physiographic features such as Nasu Volcanic Zone, Fuji Volcanic Zone, Japan trench and Izu-Ogasawara Trench (Nirei et al, 1990). Uncontrolled use of groundwater has caused land subsidence. To ensure effective use of groundwater, a monitoring system for their management has been developed. Over-pumping of the groundwater (fresh water and brine groundwater) resulted in a serious land subsidence problem in various areas, especially alluvial plains and reclaimed area so that it was inevitable to control the groundwater use to solve the problem (Aihara et al, 1969). Systematic observations of pumping up volumes, groundwater level changes and land subsidence records for the effective groundwater use have been carried out for preventing the land subsidence from a geological point of view (Research Committee on Land subsidence Prevention in Southern Kanto District, 1974). K. Furuno et al.: Monitoring of land subsidence and groundwater levels, Kanto Plain

Kanto groundwater basin and underground fluid resources
Control of pumping volume and change of ground level and land subsidence
Control of groundwater over-pumping
Change of groundwater level
Change of land subsidence
Conclusion
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