Long-term changes in unconfined groundwater level in the southern Beppu volcanic fan

Heejun Yang, Tomo Shibata
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Abstract

Transition in effective precipitation, land use change and discharge of hot spring reveals the long-term changes in the unconfined groundwater level in the southern Beppu volcanic fan from 1971 to 2019 . The unconfined groundwater level was periodically fluctuated between 40 m and 50 m above sea level and indicated the maximum value in October or November and the minimum value in April or May. Annual effective precipitation was related to the maximum groundwater level in each year and it had decreased 0 . 7 mm every year. The urban area was slightly increased from the 1970 s to 2016 , but it was not a factor to decrease the unconfined groundwater level. The hot spring yield was inversely related to the maximum groundwater level in each year and it had increased 7 . 9 mm/y, which is approximately 11 times higher than the effective precipitation. Thus, it could conclude that the increase of the hot spring yield mainly affected the decline of the unconfined groundwater level from 1971 to 1999 .
别府火山扇南部无约束地下水位的长期变化
有效降水、土地利用变化和温泉流量的过渡揭示了1971 - 2019年别府火山扇南部无约束地下水位的长期变化。无承压地下水位在海拔40 ~ 50 m之间周期性波动,10月或11月最高,4月或5月最低。年有效降水量与各年最高地下水位有关,年最高地下水位下降了0。每年7毫米。从20世纪70年代到2016年,城市面积略有增加,但不是无限制地下水位下降的因素。温泉产量与历年最高地下水位呈负相关,均增加了7个百分点。9毫米/年,约为有效降水的11倍。因此,1971 ~ 1999年,温泉产量的增加是影响无承压地下水位下降的主要因素。
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