Zobrazeno 1 - 10
of 66
pro vyhledávání: '"Masahiko Ono"'
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
Autor:
SOICHI HASHIMOTO, MASATO ONOSE, HIROMI KOTANI, SHINKICHI SUGIMORI, MASAHIKO ONO, REIKO YOSHIKAWA, CHIE HATAGAKI
Publikováno v:
The Annual Report of Educational Psychology in Japan. 61:230-241
Autor:
Masahiko Ono, Makoto Kagabu
Publikováno v:
Journal of Groundwater Hydrology. 62:643-651
Autor:
Takuma Hasegawa, Kotaro Nakata, Yuichi Tomioka, Tomoko Ohta, Shunichi Okamoto, Atsunao Marui, Isao Machida, Reo Ikawa, Masahiko ONO, Shinji Matsumoto
Publikováno v:
Goldschmidt2022 abstracts.
Autor:
Yuichi Tomioka, Kotaro Nakata, Kazuya Miyakawa, A. Marui, Takuya Matsumoto, Teruki Iwatsuki, T. Hasegawa, Tomoko Ohta, D. K. Solomon, Katsuhiro Hama, Masahiko Ono
Publikováno v:
Applied Geochemistry. 104:60-70
Noble gases dissolved in groundwater have been used to evaluate characteristics such as origin, residence time and recharge temperature. Although obtaining samples without degassing is highly desired, in certain cases, degassing during sampling is un
Publikováno v:
GEOCHEMICAL JOURNAL. 53:235-247
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
Autor:
Kiyoshi Takikawa, Yaser Nikpeyman, Kimpei Ichiyanagi, Takahiro Hosono, Jun Shimada, Heejun Yang, Masahiko Ono
Publikováno v:
Environmental Earth Sciences. 78
Submarine groundwater discharge (SGD) is a process through which groundwater and solutes are transferred from coastal aquifers into the oceans. Generally, the SGD is composed of two basic components: (1) fresh groundwater, FSGD; and (2) recirculated
Publikováno v:
RADIOISOTOPES. 65:431-439
Autor:
Masahiko Ono
Publikováno v:
The Japanese Journal of Special Education. 54:307-315