Carbon-14 age and chemical evolution of Ca(HCO3)2-type groundwater of age less than 8,000 years in a confined sandy and muddy Pleistocene aquifer, Japan

Author:

Machida Isao,Suzuki Yohey,Takeuchi Mio

Publisher

Springer Science and Business Media LLC

Subject

Earth and Planetary Sciences (miscellaneous),Water Science and Technology

Reference47 articles.

1. Appelo CAJ, Postma D (2007) Geochemistry, groundwater and pollution, 2nd edn. Balkema, Amsterdam

2. Bath AH, Edmunds WM, Andrews JN (1979) Palaeoclimatic trends deduced from the hydrochemistry of a Triassic sandstone aquifer, United Kindgom. In: IAEA (ed) Isotope hydrology, vol II. IAEA, Vienna, pp 545–568

3. Chapelle FH, McMahon PB (1991) Geochemistry of dissolved inorganic carbon in a coastal plain aquifer. 1. Sulfate from confining beds as an oxidant in microbial CO2 production. J Hydrol 127:85–108

4. Chapelle FH, Knobel LL (1983) Aqueous geochemistry and the exchangeable cation composition of glauconite in the Aquia Aquifer, Maryland. Ground Water 21:343–352

5. Chiba Prefecture (1983) Chikasui tekisei riyouryou chousa houkokusyo -Kimitsu to Kisarazu [Survey report for suitable groundwater use: Kimitsu and Kisarazu]. Chiba Prefecture, Chiba, Japan

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