Research Article

Soil and Water Conservation Effects of Contour Reverse Slope Terraces on Red Clay Sloping Farmland against Short and Heavy Rainfall

Table 5

Surface and underground cumulative runoff modulus and the percentages on the bare slope and contour reverse slope.

Rainfall intensity (mm/h)Bedrock porosity (%)Contour reverse slope terraceBare slope
(ml/m2) (ml/m2) (%) (%) (ml/m2) (ml/m2) (%) (%)

1511601.331743.7347.952.14429.531268.7377.722.3
3131.893088.624.195.9344.312247.8913.386.7
545.803146.641.498.6350.492490.4912.387.7

3015853.672915.9866.733.312616.271479.7389.510.5
34905.514071.6454.645.48686.821608.9884.415.6
51585.964936.8724.375.73967.473775.1851.248.8

5018907.804111.1168.431.619207.222164.3689.910.1
37278.823574.5067.132.913699.382577.5684.215.8
56357.714404.0059.140.910752.334103.7872.427.6

Note: = surface cumulative runoff modulus; = underground cumulative runoff modulus; = surface runoff proportion; = underground runoff proportion.