Zobrazeno 1 - 10
of 15
pro vyhledávání: '"Hanae Saishu"'
Autor:
Noriyoshi Tsuchiya, Masaoki Uno, Putri Setiani, Hanae Saishu, Noriaki Watanabe, Vani Novita Alviani, Masahiro Oba, Nobuo Hirano
Publikováno v:
International Journal of Hydrogen Energy. 44:29903-29921
The reaction of Al and H2O is a promising method for the renewable production of H2 (an environmentally friendly fuel whose combustion produces only water), because it does not directly include fossil fuels conversion. This reaction was studied at ex
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::217829d3d2c6f6aadc703d30cda27449
https://doi.org/10.1016/j.ijhydene.2019.09.152
https://doi.org/10.1016/j.ijhydene.2019.09.152
Autor:
Seiki Horimoto, Kyosuke Okamoto, Keigo Kitamura, Takuya Ishibashi, Toru Mogi, Hiroshi Asanuma, Noriyoshi Tsuchiya, Tatsuya Kajiwara, Kuniaki Shimada, Yasuo Ogawa, Yasuhiro Fujimitsu, Shigemi Naganawa, Hanae Saishu, Kazuya Ishitsuka, Norio Yanagisawa, Yusuke Yamaya, Atsushi Okamoto
Publikováno v:
Geothermics. 82:267-281
It has been suggested that a large amount of crustal fluid is trapped at a supercritical state within intrusive rocks beneath volcanoes or calderas near the mountain ranges of northeastern Japan. If we could extract and use these crustal fluids, we c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::476b2cadf2ff50d01a9923fed9022621
https://doi.org/10.1016/j.geothermics.2019.07.002
https://doi.org/10.1016/j.geothermics.2019.07.002
Pore fluid pressure (Pf) is of great importance to understand slow earthquake mechanics. In this study, we estimated the pore fluid pressure during the formation of foliation-parallel quartz veins filling mode I cracks in the Makimine mélange easter
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bd5ac26e6e7b48a6f2dd416b83030293
https://doi.org/10.5194/egusphere-egu21-7760
https://doi.org/10.5194/egusphere-egu21-7760
Autor:
Haruna Masuyama, Hiroyuki Kagi, Hanae Saishu, Kohtaro Ujiie, Naoki Nishiyama, Makoto Otsubo, Ake Fagereng
Publikováno v:
JAIRO
Geophysical Research Letters
Geophysical Research Letters 45 5371–5379
CORE (RIOXX-UK Aggregator)
ZENODO
Geophysical Research Letters
Geophysical Research Letters 45 5371–5379
CORE (RIOXX-UK Aggregator)
ZENODO
Episodic tremor and slow slip (ETS) occurs in the transition zone between the locked seismogenic zone and the deeper, stably sliding zone. Actual mechanisms of ETS are enigmatic, caused by lack of geological observations and limited spatial resolutio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::40f0d0fbd1e46b5c954abab528e4f62b
https://tsukuba.repo.nii.ac.jp/records/47865
https://tsukuba.repo.nii.ac.jp/records/47865
Publikováno v:
Geophysical Research Letters. 44:10-10,315
Fractures are the location of various water–rock interactions within the Earth's crust; however, the impact of the chemical heterogeneity of fractures on hydraulic properties is poorly understood. We conducted flow-through experiments on the dissol
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::71ab81ca910df75620a369b657258b0e
https://doi.org/10.1002/2017gl075476
https://doi.org/10.1002/2017gl075476
Autor:
Noriaki Watanabe, Hanae Saishu, Kiyotoshi Sakaguchi, Tatsuya Numakura, Noriyoshi Tsuchiya, Steven E. Ingebritsen, Atsushi Okamoto
Publikováno v:
Nature Geoscience. 10:140-144
The hypothesis that the brittle–ductile transition (BDT) drastically reduces permeability implies that potentially exploitable geothermal resources (permeability >10−16 m2) consisting of supercritical water could occur only in rocks with unusuall
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7af1edc1099510dccee2b0a7d49e6253
https://doi.org/10.1038/ngeo2879
https://doi.org/10.1038/ngeo2879
Porosity and Permeability Evolution Induced by Precipitation of Silica under Hydrothermal Conditions
Publikováno v:
Procedia Earth and Planetary Science. 17:249-252
Water-rock interaction provides significant influences on evolution of hydrological properties within the crusts. Especially, dissolution and precipitation of silica in fractures play essential roles on permeability evolution. In this study, we condu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a05c46a440271e82a4c83613b5c19076
https://doi.org/10.1016/j.proeps.2016.12.046
https://doi.org/10.1016/j.proeps.2016.12.046
Autor:
Takeshi Komai, Takuya Ishibashi, Noriyoshi Tsuchiya, Kohei Saito, Hanae Saishu, Kengo Nakamura, Noriaki Watanabe, Atsushi Okamoto
Publikováno v:
Applied Energy. 260:114306
Superhot geothermal environments in granitic crusts of ca. 400–500 °C and depths of 2–4 km are recognized as a frontier of geothermal energy. In developing such environments, hydraulic fracturing is a promising way to create or recreate permeabl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b77308009bd0dbfca393ab8854f2469a
https://doi.org/10.1016/j.apenergy.2019.114306
https://doi.org/10.1016/j.apenergy.2019.114306
Publikováno v:
Scientific Reports
Scientific Reports, Vol 7, Iss 1, Pp 1-10 (2017)
Scientific Reports, Vol 7, Iss 1, Pp 1-10 (2017)
Silica precipitation is assumed to play a significant role in post-earthquake recovery of the mechanical and hydrological properties of seismogenic zones. However, the relationship between the widespread quartz veins around seismogenic zones and eart
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c3ad6f9cc06c5f0b3136b6930f06e39b
https://pubmed.ncbi.nlm.nih.gov/29042653
https://pubmed.ncbi.nlm.nih.gov/29042653
Publikováno v:
Terra Nova. 26:253-259
The hydrological system within Earth's crust is divided into the permeable zone and the underlying, much less permeable zone. In this study, we investigated the solubility and precipitation kinetics of silica in water under the conditions of the Kakk
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::74b0c97a5e6abe2739e28f7a4be32d52
https://doi.org/10.1111/ter.12093
https://doi.org/10.1111/ter.12093