2009 年 15 巻 p. 423-428
Power of sediment discharge potential in river basins P [Nm/year] defined by the work of annual precipitation in river basins has proved to be effective to estimate sediment discharge in 102 to 104 km2 scale basin. So, its effectiveness is examined when it is applied for the estimation of those less than 102 km2 scale subject to debris control projects, reflecting confluence network of river system and geological feature. Consequently, its usefulness is confirmed and sediment yield is largest in accretionary complex for same values of the power of sediment discharge potential.