Japan Geoscience Union Meeting 2019

Presentation information

[J] Poster

O (Public ) » Public

[O-03] Poster presentations by senior high school students

Sun. May 26, 2019 1:45 PM - 3:15 PM Poster Hall (International Exhibition Hall8, Makuhari Messe)

convener:Tatsuhiko Hara(International Institute of Seismology and Earthquake Engineering, Building Research Institute), Katsuyoshi Michibayashi(Department of Earth and Planetary Sciences, Nagoya University), Miwa Kuri(International Research Institute of Disaster Science, Tohoku University), Kou Yamada(Waseda University)

1:45 PM - 3:15 PM

[O03-P40] Considering the recent landslide disasters in Japan -Movement of water in pedosphere-

*Rina Matsuki1, Nahoko Kubo1, Yo Sayama1, Arika Tsuji1, Yuna Miyachi1, Yuzuki Kobayashi1, Sae Takami1, Tatuki Morikawa1, Ryota Yamasaki1, Yuto Umeda1 (1.Kyoto Prefectural Sagano High School)

Keywords:Forestry, Landslide Disasters, Soil

The importance and function of retaining water in that forests has been clearly stated in studies before said, and landslides are still occuring have continued to report. In researches performed by our school, the decreasing in understory vegetation by deer (Cervidae) was reported, and the water holding property of the soil was be decreased because of the possibility decrease of evapotranspiration and soil erosion. It means that rainwater reaches the rock layer directory and this condition cause will cause landslides. In this research study, We performed a soil profile, a soil three-phase distribution and a soil permeability investigation to measure the state of soil especially the water retention capacity within on the soil of the Woods for Field Practice Owned by Sagano High School (WFS). As a result of this soil profile, the WFS was found to have (the Woods for Field Practice Owned by Sagano H.S.) has Japanese general soil and the pedosphere was up is to 60 cm in depth. And the WFS’s soil has a reasonable water retention capacity for plants. On the other hand, soil permeability was relatively good. It means that water will reach the rock layer when it have rains beyond the fixed quantity.