JpGU-AGU Joint Meeting 2020

Presentation information

[J] Oral

H (Human Geosciences ) » H-GM Geomorphology

[H-GM03] Geomorphology

convener:Tsuyoshi Hattanji(Faculty of Life and Environmental Sciences, University of Tsukuba), Masayuki Seto(Fukushima Future Center for Regional Revitalization, Fukushima University)

[HGM03-05] Transition of soil sustainability in granite watersheds through artificial deforestation: quantifying acceleration of hillslope erosion in the Tanakami Mountains, central Japan

*Ryoga Ohta1,2, Yuki Matsushi3, Hiroyuki Matsuzaki4 (1.Graduate School of Science, Kyoto university, 2.JSPS Research Fellow DC1, 3. DPRI, Kyoto University, 4. MALT, The University of Tokyo)

Keywords:human impact, soil sustainability, tree roots, terrestrial cosmogenic nuclide, raised-bed river

Destabilization of soil layer on hillslopes by deforestation accelerate sediment discharge, resulting in an irreversible state transition of watersheds. This study established a model of soil development on steep hillslopes incorporating effects of surface protection by organic materials and tree-root reinforcement of soil to quantify human impact on soil coverage. We selected two typical watersheds under contrasting soil and vegetation conditions for model application, and then conducted filed survey, topographic analysis, cosmogenic nuclide analysis for model parameterization. Natural-state watershed is mantled by cohesive soil (c = 4.1 kPa, φ = 31.5°) and covered with mixed forest of broad-leaf trees and conifer stands, while transition-state watershed is mostly saprolite-exposed and thinly covered by cohesion-less sand (c = 1.9 kPa, φ = 34.6°). Each property of soil indicates that the changes of weathering process by state-transition appear as the difference in cohesive strength and grain-size. Tree roots produce an additional cohesive strength via fiber reinforcement, promoting stability of bulk soil in a natural-state watershed. Based on the in-situ measurement of reinforcement and distribution of tree roots, the calculated additional cohesive strength reaches 101 kPa at the surface and gradually decreases with soil depth. Stability analysis for the modeled soil mantle in these contrasting watersheds suggested that the changes of the properties of soils as well as disappearance of vegetation cover and the tree-roots regulate the sustainability of soil layer on a hillslope. In this presentation, we also demonstrate a strategy for validation of the transition process of hillslope denudation via 10Be depth-profiling for lowland deposits forming raised-bed rivers.