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Soil degradative effects of slope length and tillage methods on alfisols in Western Nigeria. I. Runoff, erosion and crop response

✍ Scribed by R. Lal


Publisher
John Wiley and Sons
Year
1997
Tongue
English
Weight
213 KB
Volume
8
Category
Article
ISSN
1085-3278

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✦ Synopsis


Field runo plots were established in 1984 to evaluate the eects of slope length on runo, soil erosion and crop yields on newly cleared land for four consecutive years (1984±1987) on an Al®sol at Ibadan, Nigeria. The experimental treatments involved six slope lengths (60 m to 10 m at 10-m increments) and two tillage methods (plough-based conventional tillage and a herbicide-based no-till method) of seedbed preparation. A uniform crop rotation of maize (Zea mays)/cowpeas (Vigna unguiculata) was adopted for all four years. An uncropped and ploughed plot of 25 m length was used as a control. The water runo from the conventional tillage treatment was not signi®cantly aected by slope length, but runo from the no-till treatment signi®cantly increased with a decrease in slope length. The average runo from the no-till treatment was 1 . 85 per cent of rainfall for 60 m, 2 . 25 per cent for 40 m, 2 . 95 per cent for 30 m, 4 . 7 per cent for 20 m and 5 . 15 per cent for 10 m slope length. In contrast to runo, soil erosion in the conventional tillage treatment decreased signi®cantly with a decrease in slope length. For conventional tillage, the average soil erosion was 9 . 59 Mg ha À1 for 60 m, 9 . 88 Mg ha À1 for 50 m, 6 . 84 Mg ha À1 for 40 m, 5 . 69 Mg ha À1 for 30 m, 1 . 27 Mg ha À1 for 20 m and 2 . 19 Mg ha À1 for 10 m slope length. Because the no-till method was extremely eective in reducing soil erosion, there were no de®nite trends in erosion with regard to slope length. The average sediment load (erosion:runo ratio) also decreased with a decrease in slope length from 66 . 3 kg ha À1 mm À1 for 60 m to 36 . 3 kg ha À1 mm À1 for 10 m slope length. The mean C factor (ratio of soil erosion from cropped land to uncropped control) also decreased with a decrease in slope length. Similarly, the erosion:crop yield ratio decreased with a decrease in slope length, and the relative decrease was more drastic in conventional tillage than in the no-till treatment. The slope length (L) and erosion relationship ®ts a polynomial function (Y c aL bL 2 ). Formulae are proposed for computing the optimum terrace spacing in relation to slope gradient and tillage method. # 1997


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