초록
화강암질풍화토(SP, SM)로 축조된 사면에 사면경사강우강도에 따른 사면 내 간극수압, 침투깊이, 강도정수를 산정하였다. 그리고 불포화토의 전단강도 식을 적용하여 강우에 따른 전단강도의 변화를 비교${\cdot}$분석하였다. 그 결과 강우에 따른 침투속도는 강우강도가 클수록, 사면의 완만할수록 침투가 빨리 진행되었다. Lumb의 이론치와 모형실험의 실측치를 비교분석한 결과 실측치가 더 빠른 것을 알 수 있었다. 그리고 SM은 SP에 비해 전단강도가 크게 나타나는데 세립분이 증가할수록 투수계수가 작아지고 침투율이 작아짐에 따라 침투속도에 영향을 주는 것을 알 수 있었다. 또한, 사면내 전단강도는 1:1.5의 경사에서 가장 작은 전단강도를 보이는데 간극수압의 상승으로 인하여 저하되는 것으로 나타났다.
This study calculated the pore water pressure, the depth of seepage, the constant of the strength in accordance with the slope inclination and the rainfall intensity over the slope built by the weathered granite soil (SP, SM). And, the change of the shear strength in accordance with the rainfall has been compared and analyzed by applying the shear strength formula of the unsaturated soil. As a result, the rainfall intensity is stronger and the slope inclination is gentler the seepage speed in accordance with the rainfall became faster proportionally. As a result of comparing and analyzing both the theoretical value of Lumb and the actual value of the model, it can be said that the actual value is faster. Since SM shows the bigger shear strength than SP, it can also be said that as the granules increase, the coefficient of permeability becomes smaller; and as the seepage rate became smaller, it affects the seepage speed. Likewise, the shear strength within the slope displays the smallest shear strength at the inclination of 1:1.5 the reason of its decrease turned out that it was due to the increase of the pore water pressure.