Zobrazeno 1 - 10
of 34
pro vyhledávání: '"Tsuyoshi Hattanji"'
Autor:
Masato Sato, Tsuyoshi Hattanji
Publikováno v:
Progress in Earth and Planetary Science, Vol 5, Iss 1, Pp 1-10 (2018)
Abstract A laboratory experiment on salt weathering was carried out under changing humidity conditions. Three types of rock (tuff and dense and porous sandstone) with sodium chloride, sodium sulfate, or magnesium sulfate were subjected to humidity os
Externí odkaz:
https://doaj.org/article/702a7e568d0347fabd3c437312b860c9
Publikováno v:
Geomorphology. 329:129-137
Total and continuing denudation rates were estimated using cosmogenic nuclides and intensive field observations of sediment transport in two small basins (C3 and S3) from the Ashio Mountains, Japan. The C3 basin underlain by Triassic bedded chert, wh
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b2f45b6f9a9a4c88c3e40239af2d20c9
https://doi.org/10.1016/j.geomorph.2018.12.022
https://doi.org/10.1016/j.geomorph.2018.12.022
Autor:
Tsuyoshi Hattanji, Naoyuki Yoshihara
Publikováno v:
Journal of Applied Geophysics. 203:104704
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4473d741ea2409e6662879e927df83b9
https://doi.org/10.1016/j.jappgeo.2022.104704
https://doi.org/10.1016/j.jappgeo.2022.104704
Autor:
Ryuya Kodama, Tsuyoshi Hattanji, Daichi Takahashi, Shoji Doshida, Yasushi Tanaka, Takahisa Furuichi
Publikováno v:
Geomorphology. 393:107943
Channel initiation is a major mechanism of landform evolution, and channel heads are the points where channelization occurs. In mountainous or hilly landscapes, the channel initiation often occurs by shallow landslides. Although topographic observati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b2e732025ea74e6b1263a6bb3e991b6c
https://doi.org/10.1016/j.geomorph.2021.107943
https://doi.org/10.1016/j.geomorph.2021.107943
Autor:
Tsuyoshi Hattanji, Yukinori Matsukura
Publikováno v:
Journal of Geography (Chigaku Zasshi). 126:355-367
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b06b5f863baff653b11a50ecbc201d86
https://doi.org/10.5026/jgeography.126.355
https://doi.org/10.5026/jgeography.126.355
Autor:
Tsuyoshi Hattanji, Masato Sato
Publikováno v:
Progress in Earth and Planetary Science, Vol 5, Iss 1, Pp 1-10 (2018)
A laboratory experiment on salt weathering was carried out under changing humidity conditions. Three types of rock (tuff and dense and porous sandstone) with sodium chloride, sodium sulfate, or magnesium sulfate were subjected to humidity oscillation
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1c683808b5d31c6c944562c2bce62524
https://doi.org/10.1186/s40645-018-0241-2
https://doi.org/10.1186/s40645-018-0241-2
Publikováno v:
Journal of Geography (Chigaku Zasshi). 125:133-153
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0dfd4f77bc637ec9d7cf67cf7039c5f1
https://doi.org/10.5026/jgeography.125.133
https://doi.org/10.5026/jgeography.125.133
Publikováno v:
Geomorphology. 247:2-9
This study aims at estimating the controlling factors for the denudation rates of limestone, which often forms solution dolines on karst tablelands. Our approaches include (1) electrical resistivity tomography (ERT) to reveal shallow subsurface struc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4826c286fc7a48c6afbd9b9eff32b2ad
https://doi.org/10.1016/j.geomorph.2015.05.028
https://doi.org/10.1016/j.geomorph.2015.05.028
Autor:
Wonsuh Song, Nobuyuki Ishii, Yukinori Matsukura, Yasuhiko Takaya, Yuichi S. Hayakawa, Mariko Ueda, Tsuyoshi Hattanji
Publikováno v:
Geomorphology. 204:485-492
Field and laboratory experiments were performed to examine dissolution rates of limestone in stream flow. Field experiments were conducted in three stream sites (A–C) with different lithological or hydrological settings around a limestone plateau i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::13302c3c69c7342aa10f3969839d8b12
https://doi.org/10.1016/j.geomorph.2013.08.027
https://doi.org/10.1016/j.geomorph.2013.08.027
Publikováno v:
Physical Geography. 33:536-560
This study focuses on lithological contrasts of headmost channel morphology of two mountainous areas underlain by chert or sandstone. The areas have contrasting runoff processes: subsurface storm flow predominates in the chert area, whereas groundwat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::411ca40ebe78ad361890bef6b94dee49
https://doi.org/10.2747/0272-3646.33.6.536
https://doi.org/10.2747/0272-3646.33.6.536