SONG Jiangping1, 2, LI Zhongwu1, et al. Effects of Typical Soil and Water Loss Control Patterns on Runoff and Sediment of Red Soil in Low Hilly Areas from the Northern Hunan Province[J]. 2018, 32(1): 32-38.
SONG Jiangping1, 2, LI Zhongwu1, et al. Effects of Typical Soil and Water Loss Control Patterns on Runoff and Sediment of Red Soil in Low Hilly Areas from the Northern Hunan Province[J]. 2018, 32(1): 32-38. DOI: 10.13870/j.cnki.stbcxb.2018.01.006.
Clarifying the runoff and sediment in runoff plot under different soil and water loss control patterns plays an important role for large-scale soil and water loss. In this study
the runoff and sediment of red soil under three typical soil and water loss control patterns (S1 pattern: slope change ladder + Fruit trees
S2 pattern: contour trench and ridge + Crops
S3 pattern: flat wasteland slope + Herbs) were investigated through the field standard runoff areas under natural rainfall experiment in low hilly areas. The results showed that the average runoff volume under three control patterns was S3 (1.84?m3) > S1 (1.03?m3) > S2 pattern (0.78?m3)
and the average sediment yield was S3 (1.191?t/hm2) > S1 (0.411?t/hm2) > S2 pattern (0.311?t/hm2). The cumulative runoff under the three control patterns was S3 (33.19
15.25
14.13?m3) > S1 (19.40
9.06
6.48?m3) > S2 pattern (16.60
5.89
4.15?m3) in the A
B
and C rainfall types (K-means clustering). The cumulative sediment also showed the similar trend that was S3 (14.474
10.863
15.153?t/hm2) > S1 (7.521
2.695
3.766?t/hm2) > S2 pattern (6.149
1.685
2.741?t/hm2). Different control patterns maintained a significant positive correlation between sediment yield had significant positive correlations with runoff volume under the tree control patterns (P<0.01
r > 0). The correlation coefficient (r) was 0.853
0.920
and 0.677
respectively. Furthermore
the linear regression slope (k) of sediment yield and runoff volume was 0.356
0.420 and 0.493
respectively under S1
S2
and S3 patterns
indicating the response degree of sediment to runoff in different control patterns was S3 > S2 > S1 pattern. Thus
three typical patterns have significantly different effects for controlling soil and water loss.