scholarly journals ANOMALOUS CHANGES IN GROUNDWATER LEVEL AT THE ATAMI OBSERVATION WELL, SHIZUOKA PREFECTURE, CAUSED BY THE SWARM EARTHQUAKE OFF THE EAST COAST OF THE IZU PENINSULA, JAPAN, 1980

1982 ◽  
Vol 55 (4) ◽  
pp. 239-257
Author(s):  
Yusaku TAGUTSCHI ◽  
Shigeru NAGAI

2004 ◽  
Vol 31 (10) ◽  
pp. n/a-n/a ◽  
Author(s):  
Naoji Koizumi ◽  
Yuichi Kitagawa ◽  
Norio Matsumoto ◽  
Makoto Takahashi ◽  
Tsutomu Sato ◽  
...  


1999 ◽  
Vol 26 (23) ◽  
pp. 3509-3512 ◽  
Author(s):  
Naoji Koizumi ◽  
Eikichi Tsukuda ◽  
Osamu Kamigaichi ◽  
Norio Matsumoto ◽  
Makoto Takahashi ◽  
...  


1999 ◽  
Vol 26 (16) ◽  
pp. 2501-2504 ◽  
Author(s):  
Masao Ohno ◽  
Tsutomu Sato ◽  
Kenji Notsu ◽  
Hiroshi Wakita ◽  
Kunio Ozawa


2020 ◽  
Vol 13 (4) ◽  
pp. 1445-1459
Author(s):  
Liang He ◽  
Suozhong Chen ◽  
Ying Liang ◽  
Manqin Hou ◽  
Junyi Chen


2010 ◽  
Vol 193 (1-2) ◽  
pp. 25-36 ◽  
Author(s):  
Masayuki Murase ◽  
Takeo Ito ◽  
Yoshinari Hayashi ◽  
Takeshi Sagiya ◽  
Fumiaki Kimata ◽  
...  




Geologos ◽  
2019 ◽  
Vol 25 (3) ◽  
pp. 193-204
Author(s):  
Izabela Jamorska ◽  
Katarzyna Kubiak-Wójcicka ◽  
Arkadiusz Krawiec

Abstract The aim of the present study is to monitor changes in the location of the groundwater table in the catchment area of the River Gwda within the Quaternary and Neogene water-bearing level over a 35-year period, between 1981 and 2015. In addition, on account of very diverse total annual precipitation levels in particular parts of the catchment, attempts were made to determine the influence of precipitation on the location of the groundwater table. By correlating groundwater level and meteorological parameters (precipitation), it was discovered that precipitation in the previous year made the largest impact on the groundwater table. Moreover, low precipitation totals in the southern part of the catchment are not discernible in groundwater table fluctuations, which is linked to the location of the observation well within the drainage zone as well as to water ascension from deeper aquifers.



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