Initialising ...
Initialising ...
Initialising ...
Initialising ...
Initialising ...
Initialising ...
Initialising ...
Ishii, Eiichi; Funaki, Hironori; Sanada, Hiroyuki
no journal, ,
no abstracts in English
Kawamura, Makoto; Niizato, Tadafumi; Yasue, Kenichi; Tokiwa, Tetsuya; Oi, Takao; Kawachi, Susumu; Ishimaru, Tsuneari; Umeda, Koji; Makino, Hitoshi
no journal, ,
no abstracts in English
Funaki, Hironori; Orukawa, Go; Nago, Makito*; Yasue, Kenichi; Niizato, Tadafumi; Tominaga, Eiji*
no journal, ,
no abstracts in English
Niwa, Masakazu; Mizuochi, Yukiiro*; Tanase, Atsushi*
no journal, ,
no abstracts in English
Umeda, Koji
no journal, ,
no abstracts in English
Shimada, Koji; Niwa, Masakazu; Kurosawa, Hideki; Nohara, Tsuyoshi
no journal, ,
no abstracts in English
Yasue, Kenichi; Sanga, Tomoji*; Nogami, Michio*; Tajikara, Masayoshi; Niizato, Tadafumi
no journal, ,
This paper presents the results of simulation of longitudinal river profile. Fast, we show that the longitudinal river profile is simulated in simplified model. Next, we simulated actual rivers by the same algorithm as the simplified model. This simulation shows that erosion rate and position of erosional front are different in each river. We think that Lithology influence the difference of erosional process in the river profile.
Niizato, Tadafumi
no journal, ,
On the description of the long-term transition of the geological environments it is important to integrate the all of results related to natural phenomena into geological history and to evaluate the total-systems performance.