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Subsurface thermal environment and groundwater flow around Tokyo Bay, Japan

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Abstract

Previous studies and borehole temperature measurements suggest that subsurface temperature distribution on the west side of Tokyo Bay (from Tokyo to Yokohama) is higher than that of the east side (Chiba side). To understand the groundwater flow and other factors which may contribute to the subsurface temperature discrepancy such as geological setting in the study area, groundwater temperature profiles were measured in 119 boreholes around the Tokyo Bay from 2002 to 2007. The data were analyzed and compared with previous studies. Horizontal distribution of subsurface temperature at the depths of −50 and −100 m was made to show the distribution of thermal regime. A cross-section across the bay of Tokyo was made to see the isothermal lines and distribution of hydraulic heads in a vertical perspective. These results show that the highest subsurface temperature zone is in the Tokyo area, along the river valley. Subsurface temperature at the depth of 50- and 100-m below sea level in the western part of the bay is comparatively higher than its eastern side at the same elevation and distance from the bay. This fact suggests that there is a regional groundwater flow system in the area and it is strongly affected by the geological structure, particularly buried valley systems of the bay during the Paleo-Tokyo River and the topographical driving force which is the result of the different elevation of recharge areas. Groundwater discharge is concentrated along the buried valley of Paleo-Tokyo River.

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References

  • Chiba Prefecture’s Official Website http://www.pref.chiba.lg.jp/english/outline/location.html

  • Chujo J (1962) On the Paleo-Tokyo River. Chikyu Kagaku (Earth Sci) 59:30–39 (in Japanese with English Abstract)

  • Domenico PA, Palciauskas VV (1973) Theoretical analysis of forced convection heat transfer in regional groundwater-flow. Geol Soc Am Bull 84:143–160

    Article  Google Scholar 

  • Huang SP, Pollack HN, Shen PY (2000) Temperature trends over the past five centuries constructed from borehole temperatures. Nature 403:756–758

    Article  Google Scholar 

  • Kaizuka S, Naruse Y, Matsuda I (1977) Recent formations and their basal topography in and around Tokyo Bay, Central Japan. Quatern Res 8:32–50

    Article  Google Scholar 

  • Kanagawa Prefecture’s Official Website http://www.pref.kanagawa.jp/info/syoukai/e-profile.html#population

  • Kondoh A (1985) Study on the groundwater flow system by environmental tritium in Ichihara region, Chiba prefecture. Environmental Research Center, the University of Tsukuba, Paper No 6. Sankyo Sha, Tokyo, 12 p

  • Lubis RF (2008) Groundwater recharge and discharge processes in the Jakarata groundwater basin, Indonesia. Hydrogeol J 16:927–938

    Google Scholar 

  • Miyakoshi A, Uchida Y, Sakura Y, Hayashi T (2003) Distribution of subsurface temperature in the Kanto Plain, Japan; estimation of regional groundwater flow system and surface warming. Phys Chem Earth 28:467–475

    Google Scholar 

  • Otuka Y (1934) Physiography of Tokyo during late Quaternary. Proc Imp Acad 10:274–277

    Google Scholar 

  • Reconstruction Bureau (1929) Report on geology of Tokyo and Yokohama. (in Japanese)

  • Sakura Y (1993) Groundwater flow estimated from temperatures in the Yanezawa basin, northeast Japan. Int Assoc Hydrol Publ 215:161–170

    Google Scholar 

  • Salem ZE, Taniguch M, Sakura Y (2004) Use of temperature profiles and stable isotopes to trace flow lines: Nagaoka area, Japan. Ground Water 42:83–91

    Article  Google Scholar 

  • Shepard FP, Niino H, Chamberlain TK (1964) Submarine canyons and Sagami Trough, east-central Honshu, Japan. Bull Geol Soc Am 75:1117–1130

    Article  Google Scholar 

  • Suzuki H (2002) Underground geological structure beneath the Kanto Plain, Japan. Jp Sci Technol Agency 63:1–19

    Google Scholar 

  • Suzuki Y et al (1995) Explanatory text of geological map of Tokyo Bay and adjacent areas, 2nd edn. Geological Survey of Japan

  • Takahashi M (1967) On the groundwater temperature in Japan. Report number 219, Geological Survey of Japan, pp 1–39

  • Taniguchi M (1993) Evaluation of vertical groundwater fluxes and thermal properties of aquifers based on transient temperature-depth profiles. Water Resour Res 29:2021–2026

    Article  Google Scholar 

  • Taniguchi M (1987) Mechanism of groundwater temperature formation in Nagaoka plain. Geol Rev Jpn 60–11:725–738

    Google Scholar 

  • Taniguchi M, Shimada J, Tanaka T, Kayane I, Sakura Y, Shimano Y, Dapaah-Siakwan S, Kawashima S (1999a) Disturbances of temperature-depth profiles due to subsurface climate-change and subsurface water flow: an effect of linear increase in surface temperature caused by global warming and urbanization in the Tokyo metropolitan area, Japan. Water Resour Res 35:1507–1517

    Article  Google Scholar 

  • Taniguchi M, Williamson DR, Peck AJ (1999b) Disturbances of temperature depth profiles due to surface climate-change and subsurface water flow: an effect of step increase in surface temperature caused by forest clearing in Southwest of Western Australia. Water Resour Res 35:1519–1529

    Article  Google Scholar 

  • Tokyo Metropolitan’s Official Website http://www.metro.tokyo.jp/ENGLISH/PROFILE/overview03.htm

  • Uchida Y, Sakura Y, Anderson MP (1999) Subsurface temperature field in the Nobi Plain, Central Japan. In: Sakura Y, Tang C (eds) Proceedings of the international symposium on groundwater in environmental problems, Chiba University, pp 43–46

Download references

Acknowledgments

The authors are very grateful to Dr. John Moore, USGS and Professor Dr. Jozsef Toth, University of Alberta, Edmonton, Alberta, Canada for spending their valuable time reviewing, giving comments, and suggestions for the manuscript. We would like to thank Mr. Hiroaki Abe, Graduate School of Science and Technology, Chiba University, Japan, for his kind technical assistance in using computer software.

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Correspondence to Vuthy Monyrath.

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Monyrath, V., Sakura, Y., Miyakoshi, A. et al. Subsurface thermal environment and groundwater flow around Tokyo Bay, Japan. Environ Earth Sci 60, 923–932 (2010). https://doi.org/10.1007/s12665-009-0228-9

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  • DOI: https://doi.org/10.1007/s12665-009-0228-9

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