Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Yasuhide Muranaka"'
Publikováno v:
Hydrogeology Journal. 30:2027-2041
Methods to determine the recharge elevation of groundwater using the altitude effect of δD and δ18O have been extensively applied in hydrogeological investigations. The secondary parameter d-excess has also been used as a groundwater tracer. In thi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3ca1f89b8253140489a4539620c4aab8
https://doi.org/10.1007/s10040-022-02526-0
https://doi.org/10.1007/s10040-022-02526-0
Publikováno v:
Journal of Groundwater Hydrology. 62:473-487
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d4919be271ab6a3e848974bc1f69e142
https://doi.org/10.5917/jagh.62.473
https://doi.org/10.5917/jagh.62.473
Autor:
Isao Machida, Takafumi Kamitani, Yasuhide Muranaka, Masahiko Ono, Akira Ito, Atsunao Marui, Koichi Oyama, Reo Ikawa
Publikováno v:
Hydrogeology Journal. 27:717-730
Groundwater movement through the slope area of Mt. Fuji to the coastal area of Suruga Bay (central Japan) was investigated using spatially dense geochemical data, as a case study for elucidating the groundwater flow system in a stratovolcano adjacent
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c6ccd19ce24bd220ebfb2852ddb00ab2
https://doi.org/10.1007/s10040-018-1889-9
https://doi.org/10.1007/s10040-018-1889-9
Publikováno v:
Journal of Geography (Chigaku Zasshi). 126:43-71
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5b45ef65b1aa93139a92b2db07f2cb4f
https://doi.org/10.5026/jgeography.126.43
https://doi.org/10.5026/jgeography.126.43
Publikováno v:
2012 14th International Conference on Ground Penetrating Radar (GPR).
It has been identified that New Fuji lava over Old Fuji lava form current Mt. Fuji. Although the area is known for abundant groundwater resources, it is still not well understood where groundwater actually flows. In this study, surface GPR was used t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::27f0eca4fb11aba13608a7c0218772eb
https://doi.org/10.1109/icgpr.2012.6254956
https://doi.org/10.1109/icgpr.2012.6254956
Publikováno v:
Proceedings of the 10th SEGJ International Symposium, Kyoto, Japan, 20-22 November 2011.
Mishima Lava Flow is an about 35km long lava flow stretching to the south-east of Mt. Fuji. It was formed about 100,000 years ago after one of the biggest eruptions of Mt. Fuji. Because of higher porosity, most precipitation and snowmelt water in thi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2093b08ed6098f5cb2077abc4d6d77da
https://doi.org/10.1190/segj102011-001.79
https://doi.org/10.1190/segj102011-001.79