To carry out a soil stratification test effectively to assess the stability of cut slopes and the best location for high-density spur roads, estimates of soil particle size were made for silt- and clay-dominated colluvial soil layers over 50 cm thick that overlay weathered residual soil. Material exposed by road-cuts was classified as rock or soil, and the relationships between composition and local topography were analyzed. Using a 10-m digital elevation model (DEM), three topographic factors were assessed: (1) average slope; (2) horizontal openness (the degree of convergence/parallelism/divergence of contour lines); and (3) vertical openness (the degree of concavity/planarity/convexity of flow lines). The study area was divided into slope areas with roughly uniform characteristics with a limit angle between each grid. Soil samples from areas with slopes over 25 degrees and horizontal openness less than 140 degrees at a limit angle of less than 10 degrees, and slopes over 30 degrees and horizontal openness less than 145 degrees at a limit angle of less than 15 degrees contained significantly less silt and clay (p<0.05, by the t-test). The finding that points with comparatively high silt and clay content were generally located on gentle and divergent ground was verified by observations at other sites. Soil coverage was high on slopes of less than 25 degrees, but low on slopes steeper than 30 degrees. This study demonstrates that analysis of topographic characteristics using a 10-m gridded DEM is effective in assessing certain geological features and in estimating the silt and clay content of soil.
View full abstract