2000
DOI: 10.5110/jjseg.41.87
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Evaluation of Recharge Mechanism of Confined Groundwater Using Long Term Tritium Concentration Records in the Metropolis of Tokyo.

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Cited by 6 publications
(8 citation statements)
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“…In confined aquifers, groundwater flows from southwest to northeast (Figure S2 in SI). The residence time of the confined groundwaters in Tokyo at depths of 40–124 m BGL was estimated, using tritium, to be 11–28 years . This relatively short residence time compared with the depth can be explained by the geology, as seen in Figure and Figure S1 (SI).…”
Section: Methodsmentioning
confidence: 99%
“…In confined aquifers, groundwater flows from southwest to northeast (Figure S2 in SI). The residence time of the confined groundwaters in Tokyo at depths of 40–124 m BGL was estimated, using tritium, to be 11–28 years . This relatively short residence time compared with the depth can be explained by the geology, as seen in Figure and Figure S1 (SI).…”
Section: Methodsmentioning
confidence: 99%
“…1). The study site is located about 3.5 km from Tama River and 35 km from Kanto Mountains in Kanagawa prefecture (Endo and Ishii 1984;Endo 1992;Imaizumi et al 2000). The groundwater is therefore expected to be influenced by relatively high-DO content water from those water sources.…”
Section: Environmental Factorsmentioning
confidence: 99%
“…The elevation of Fuchu is about 30-80 m above the mean sea level. Groundwater in shallow confined aquifers is originated from the Kanto Mountains in Kanagawa prefecture and Tama River (Endo and Ishii 1984;Endo 1992;Imaizumi et al 2000). Stratigraphy of the study area consists of two groups: the upper Tokyo group and the lower Kazusa group (Endo 1992).…”
Section: Experimental Site Descriptionmentioning
confidence: 99%
“…However, the elevated PPCP levels were not observed in the canals' vicinity and PPCPs were detected widely in the region (Kuroda et al, 2012). The residence time of the confined groundwater in Tokyo, at depths of 40-124 m BGL, was estimated to be 11-28 years, using tritium analysis (Imaizumi et al, 2000). This relatively short residence time, relative to the depth, can be explained by the geology (see Figure S1) Research, 1996) and Figure S1).…”
Section: Groundwater Rechargementioning
confidence: 98%
“…First, subsurface attenuation of PFAAs may be slower than that of PPCPs. The residence time of confined aquifers of 40-124 m depth were estimated to be 11-28 years (Imaizumi et al, 2000) and that of unconfined aquifers and springs would be shorter. The half-life of carbamazepine in groundwater is typically 5-10…”
Section: Comparison Of Pfaa and Ppcp Levelsmentioning
confidence: 98%