3H/ 3He-based groundwater ages for springs located at the foot of Mt. Fuji

K. Asai, S. Koshimizu
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引用次数: 3

Abstract

Information of groundwater age is important for understanding circulation rate and resource of groundwater flow system. In this study, dating method using 3 H/ 3 He was applied to 5 springs located at the foot of Mt. Fuji. 3 H/ 3 He-based groundwater ages were determined successfully for 4 springs, ranging from 18 to 39 years. This 3 H/ 3 He ages is consistent with hydrogeological setting of Mt. Fuji and with reported ages estimated by 36 Cl, CFCs and SF 6 , suggested that 3 H/ 3 He method becomes a powerful tool in dating groundwater around Mt. Fuji area.
富士山脚下泉水的3H/ 3he基地下水年龄
地下水年龄信息对了解地下水循环速率和地下水流动系统资源具有重要意义。本文采用3 H/ 3 He法对富士山脚5个泉水进行了测年,成功测定了4个泉水的3 H/ 3 He法地下水年龄,年龄在18 ~ 39年之间。3h / 3he年龄与富士山的水文地质背景一致,也与36 Cl、CFCs和SF - 6估算的年龄一致,表明3h / 3he方法是富士山地区地下水测年的有力工具。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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