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African Crop Science Journal
African Crop Science Society
ISSN: 1021-9730 EISSN: 2072-6589
Vol. 8, Num. 4, 2000, pp. 411-418
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African Crop Science Journal, Vol. 8. No. 4, pp. 411-418
African Crop Science Journal, Vol. 8. No. 4, pp. 411-418
EFFECT OF CROP RESIDUE MANAGEMENT AND CROPPING SYSTEM ON PEARL MILLET AND COWPEA YIELD
Adama Coulibaly, Minamba Bagayoko, Samba Traore and S.C. Mason1
Institut dEconomie Rurale, Bamako, Mali 1University of Nebraska, Lincoln, NE 68583-0915 U.S.A.
(Received 6 January, 1999; accepted 30 July, 2000)
Code Number: CS00043
INTRODUCTION
Pearl millet [Pennisetum glaucum (L.) Br.] is the most
common crop produced and consumed in the Sudano-Sahelian zones of Mali. Over
1.7 million hactares are produced annually in Mali with low grain yield levels
of 450 to 735 kg ha-1. Despite increasing population growth the area under millet
production is expanding with shorter traditional fallow periods, stagnant crop
yields, and the soil nutrient status is declining (Bagayoko et al., 1996;
van der Pol, 1992).
Leaving crop residues in the field and using a pearl millet-legume
rotational system have been suggested as ways to simultaneously increase yields
and replenish soil nutrient levels.
Crop residue application to fields in West Africa has resulted
in increased pearl millet grain yields (Muehlig-Versen et al., 1997;
Marschner et al., 1995; Bationo and Mokwunye, 1991, Verma et al.,
1992), reduced crusting, enhanced seedling growth and improved N, P, and K nutrition
of seedlings (Muehlig-Verson et al., 1997), reduced wind erosion losses
and improved crop stands (Michels et al., 1995a; 1995b), and enhanced
root growth (Bababe, 1997; Hafner et al., 1993; Kretzschmar et al, 1991;
Rebfaka et al., 1994). Crop residues trapped wind-blown dust with high
nutrient levels (Bationo et al., 1993; ), and higher soil pH and lower
Al and Mn levels (Bationo et al., 1993; Hafner et al., 1993; Kretzschmar
et al., 1991). In addition, crop residue application increased N fixation
and dry matter of groundnut (Arachis hypogaea L.)(Rebafka et al.,
1993), but legumes have generally been affected less than cereal crops (Buerkert
et al., 1997). Although retaining crop residues on the field reduces
the export of nutrients (Bationo et al., 1993), a net loss of nutrients
commonly occurs (Buerkert, 1995). Crop response to residue application is greater
in the lower rainfall Sahelian zone than in the Sudanian zone (Buerkert et
al., 1997), and is greater on unfertile degraded soils than on more fertile
soils (Buerkert, 1995). Crop residue application is commonly used by producers
to regenerate soils with wind and water-eroded surfaces (Taylor-Powell et
al., 1991).
Crop residues are used for many other purposes in West Africa,
reducing the amount of residues available for soil replenishment. Lamers and
Bruentrup (1996) studied the use of crop residue and found that the highest
gross marginal returns for land was mulching with crop residues, but the highest
gross marginal returns for total labour was using residues for livestock feeding
and for weeding labour was burning residues. Linear programing indicated that
the multiple uses of crop residues for soil improvement, livestock feeding and
weed control, as already practiced, was an economically sound approach for crop
residue utilisation.
Cropping systems research in West Africa indicates that crop
rotation of pearl millet with cowpea [Vigna unguiculata (L.) Walp] or
groundnut enhances pearl millet grain yields (Bagayoko et al., 1996;
Nicou, 1978; Bationo et al., 1996; Reddy et al., 1994). Buerkert
et al. (1997) indicated that yield increases from rotation cropping systems
with cowpea varied from 4 to 37% and was site specific. Bagayoko et al.
(1996) reported varied grain yield responses across years from 17 to 31% at
one site in Mali, and that the pearl millet-cowpea rotation and continuous pearl
millet both removed soil nutrients at rates greater than they were being naturally
replenished.
The objective of this study was to investigate the influence
of two cropping systems and three crop residue management practices on the grain
and stover yields of pearl millet and cowpea. In addition, the paper also discusses
changes in soil nutrient status resulting from the experimental treatments used
in the study.
MATERIALS AND METHODS
A long-term pearl millet crop residue management and cropping
system study was initiated in 1990 at the Cinzana Agricultural Research Station
near Segou, Mali and was conducted over a period of 7 years. The area is characterised
by an average annual rainfall of 650 mm and has low soil organic matter and
nutrient levels on an acidic, sandy, leached ferriginous (Paleustalf) soil.
The experimental site had been kept under fallow for approximately 10 years,
and we assumed that the soils possessed great microvariability for N, P, K,
Ca, Mg and cation exchange capacity as is commonly found in the region (Bagayoko
et al., 1996).
The experiment was conducted in a randomised complete block
design with four replicates. The treatments consisted of a factorial combination
of three crop residue management treatments and two cropping systems on fixed
plots over time. Crop residue management treatments included total removal of
residues by hand gathering, incorporation of pearl millet residues produced
the previous year using animal traction, and retention of pearl millet residues
produced the previous year on the soil surface. Cowpea residues were constantly
removed from the plots by hand gathering. The cropping system treatments were
continuous pearl millet, continuous cowpea, and pearl millet-cowpea rotation.
Only one phase of the rotation was included in the study; thus, in the crop
rotation treatment pearl millet was present in even-numbered years and cowpea
in odd-numbered years.
The local pearl millet variety Boboni and the indeterminate
cowpea variety Suvita 2 were used throughout the duration of the experiment.
Pearl millet was planted in hills spaced 0.8 x 0.8 m apart, and thinned to two
plants per hill two weeks after emergence giving a seedling population of 31,250
plants ha-1. Cowpea was planted in hills at a spacing of 0.8 x 0.5 m and thinned
to two plants per hill giving a plant population of 50,000 plants ha-1. Pearl
millet and cowpea were planted on the same day for each year planting was done
in July.
All plots received a basal broadcast application of 300 kg
ha-1 Tilemsi rock phosphate (equivalent to 36 kg ha-1 P) prior to planting in
1990, 1993 and 1996. Rock phosphate particle size distribution was 20% by weight
less than 0.5 mm diameter, and 85% less than 3 mm. Annual application of 21
kg ha-1 N as urea was done as a side-dress applied near the pearl millet hills
at the early tillering growth stage. Soil samples were taken at 0-20 cm depth
in 1990 prior to the establishment of the study, and again before planting in
1996 when three cycles of the crop rotation were completed. The soil samples
were analysed in 1990 and 1996 for pH, Bray-2 P, organic carbon, cation exchange
capacity (CEC), and exchangeable K, Ca and Mg at the Institut dEconomie Rurale
Soil Testing Laboratory in Sotuba, Mali. The same soil analysis methods were
used in both years.
Plots consisted of 6 rows, 8 m long (38.4 m2 ) and the center
5 m of the middle four rows (16 m2) was harvested for grain and stover. Yields
were reported on a dry matter basis. Grain and stover yields were analysed separately
for each year and across years using analysis of variance (ANOVA). Where the
F statistics indicate significance between treatments, mean separations were
done using the LSD test at the 5% level of significance.
RESULTS AND DISCUSSION
Rainfall. Annual rainfall at the experimental site in
1991, 1995, 1996 and 1997 was similar to the long-term average of 650 mm (Table
1). Seasonal rainfall was below average in 1993, and above average in 1992 and
1994. Rainfall distribution was variable across the growing season with June
rainfall ranging from 22 to 138 mm, July from 99 to 259 mm, August from 155
to 279 mm, and September from 22 to 195 mm. August rainfall was the most uniform,
and over 32% of the annual rainfall occurred in August, except in 1992 when
high rainfall amounts occurred in July and September, and in 1995 and 1997 with
the highest rainfall received in September.
TABLE 1. Monthly rainfall distribution during
the growing season at Cinzana, Mali in 1991-1997 |
Month |
1991 |
1992 |
1993 |
1994 |
1995 |
1996 |
1997 |
mm |
May |
29 |
14 |
15 |
60 |
73 |
44 |
0 |
June |
57 |
123 |
25 |
138 |
22 |
62 |
108 |
July |
174 |
259 |
99 |
184 |
158 |
160 |
139 |
August |
279 |
155 |
205 |
274 |
173 |
173 |
203 |
September |
79 |
164 |
25 |
120 |
192 |
195 |
141 |
October |
22 |
5 |
11 |
71 |
18 |
37 |
44 |
Total |
640 |
720 |
380 |
847 |
636 |
671 |
635 |
Residue management. Crop residue management treatments
had no influence on pearl millet grain or stover yields from 1991 to 1997 (Tables
2 and 3), except for grain yield in 1993 when plots with incorporated crop residues
yielded more than plots with residues retained on the soil surface. This year
had the lowest seasonal rainfall of the seven years of the study (Table 1).
However, crop residue incorporation consistently increased grain and stover
yields (Tables 2 and 3). The seven-year mean pearl millet grain yield for plots
with incorporated crop residues was 180 kg-1 ha-1 year-1
(12%) greater than plots with residues removed (P = 0.07). The mean pearl millet
stover yield in plots with crop residue incorporated was 211 to 247 kg-1
ha-1 year-1 (15 to 18%) greater than plots with residues
removed or retained on the surface (P=0.19). Although the short-term benefit
of retaining crop residues in the field for this non-degraded soil was small,
as reported by Buerkert et al. (1997), the long-term benefits of crop
residue incorporation appeared to be important. In this study, the beneficial
effect on pearl millet yield of retaining crop residues in the field were optimised
by residue incorporation treatments. This is in agreement with the report of
Bababe (1997).
TABLE 2. Effect of crop residue management on
continuous pearl millet grain yields |
Residue management |
1991 |
1992 |
1993 |
1994 |
1995 |
1996 |
1997 |
Mean |
kg ha-1 |
Removed |
1266 |
1472 |
1392 |
1322 |
1861 |
1820 |
1154 |
1469 |
Surface |
1403 |
1687 |
1095 |
1424 |
1800 |
1896 |
1297 |
1515 |
Incorporated |
1413 |
1750 |
1596 |
1429 |
1907 |
1981 |
1468 |
1649 |
LSD(0.05) |
NS |
NS |
375 |
NS |
NS |
NS |
NS |
NS |
C.V.(%) |
22 |
28 |
16 |
23 |
15 |
18 |
18 |
22 |
NS = Not significant
Significant at P = 0.07; LSD (0.05) = 184 |
TABLE 3. Effect of crop residue management on
continuous pearl millet stover yields |
Residue management |
1991 |
1992 |
1993 |
1994 |
1995 |
1996 |
1997 |
Mean |
kg ha-1 |
Removed |
3174 |
2604 |
3296 |
3825 |
4557 |
4150 |
1302 |
3273 |
Surface |
3703 |
3066 |
2116 |
3845 |
4598 |
4028 |
1303 |
3237 |
Incorporated |
2848 |
3662 |
3296 |
3805 |
4313 |
4359 |
2116 |
3484 |
LSD(0.05) |
NS |
NS |
NS |
NS |
NS |
NS |
NS |
NS |
C.V.(%) |
28 |
34 |
28 |
19 |
17 |
27 |
42 |
27 |
NS = Not significant |
Crop residue management treatments did not over the years,
influence cowpea grain and stover yields (Table 4). However, the mean yields
over 1991, 1993, 1995 and 1997 indicated that, relative to residue removal,
surface retention of residues increased cowpea grain yields by 240 kg-1
ha-1 year-1 (25%) and residue incorportion increased grain
yield by 186 kg-1 ha-1 year-1 (19%). Cowpea
stover yield over the years increased by an average of 316 kg-1 ha-1
year-1 (41%) due surface retention of crop residues, and by 350 kg-1
ha-1 year-1 with residue incorporation, as previously
found by Rebafka et al. (1993) for groundnut. In this study, the grain
and stover yields increases from retaining crop residues in the field were slightly
greater for cowpea than for pearl millet, contrasting with results of Buerkert
et al. (1997).
TABLE 4. Crop residue management effect on cowpea
grain and stover yields |
Residue management |
Grain |
Stover |
1991 |
1993 |
1995 |
1997 |
Mean |
1991 |
1993 |
1995 |
1997 |
Mean |
kg ha-1 |
Removed |
1689 |
669 |
1079 |
392 |
955 |
1016 |
734 |
898 |
461 |
777 |
Surface |
1814 |
823 |
1349 |
792 |
1195 |
1641 |
1180 |
1035 |
516 |
1093 |
Incorporated |
1823 |
701 |
1566 |
475 |
1141 |
1895 |
836 |
1074 |
781 |
1147 |
LSD(0.05) |
NS |
NS |
NS |
NS |
208 |
NS |
NS |
NS |
NS |
242 |
C.V.(%) |
13 |
30 |
31 |
44 |
26 |
30 |
25 |
38 |
29 |
33 |
NS = Not significant |
Cropping systems. Rotation of cowpea with pearl millet
increased pearl millet grain yields in 1996, as well as mean yields over 1992,
1994 and 1996 (Table 5). Over the years, pearl millet grain yields increased
by an average of 228 kg-1 ha-1 year-1 (15%)
and stover yields increased by 628 kg-1 ha-1 year-1
(19%) in response to rotation with cowpea. This is less than the 17 to 31% yield
increase reported by Bagayoko et al. (1996), but well within the range
of the 4 to 37% yield increase reported by Buerkert et al. (1997). Cowpea
grain and stover yields were not significantly (P=0.05) increased by rotation
with pearl millet (data not presented) similar to results found by Bagayoko
et al. (1996).
TABLE 5. Previous crop effect on pearl millet
grain and stover yields |
Previous crop |
Grain |
Stover |
1992 |
1994 |
1996 |
Mean |
1992 |
1994 |
1996 |
Mean |
kg ha-1 |
Pearl Millet |
1489 |
1371 |
1724 |
1528 |
2780 |
3920 |
3472 |
3390 |
Cowpea |
1784 |
1412 |
2074 |
1756 |
3441 |
3730 |
4883 |
4018 |
LSD(0.05) |
NS NS |
241 |
155 |
NS |
NS |
723 |
360 |
|
C.V.(%) |
27 |
22 |
15 |
21 |
33 |
19 |
20 |
24 |
NS = Not significant |
Soil nutrient levels. Regardless of crop residue treatment,
all cropping systems over the six-year period increased soil pH, carbon and
phosphorus concentration, and decreased potassium and cation exchange capacity
(Table 6). Phosphorus concentration increase was certainly due to basal rock
phosphate application in 1990 (after soil sampling) and in 1993 prior to planting.
The 1996 rock phosphate application was applied after the soil samples were
collected. Crop residue treatments had little influence on soil pH, carbon and
cation exchange capacity after six years. However, leaving crop residues on
the soil surface resulted in higher soil P concentrations than other residue
treatments, possibly due to entrapment of wind blown dust with higher phosphorus
concentrations previously observed by Bationo et al. (1993). Both treatments
of incorporating and retaining crop residues on the surface of plots resulted
in higher soil K concentrations than for crop residue removal treatment.
TABLE 6. Crop residue management effect on soil
properties |
Crop residue management |
pH |
P (Bray 2) |
Organic carbon |
K |
Ca |
Mg |
CEC |
1990 |
1996 |
1990 |
1996 |
1990 |
1996 |
1990 |
1996 |
1990 |
1996 |
1990 |
1996 |
1990 |
1996 |
ppm |
% |
c mol kg-1 |
Removed |
4.8 |
5.3 |
8.0 |
24 |
0.17 |
0.37 |
0.24 |
0.05 |
1.47 |
1.10 |
0.30 |
0.13 |
3.6 |
1.2 |
Surface |
4.7 |
5.5 |
11 |
35 |
0.19 |
0.40 |
0.33 |
0.16 |
0.93 |
0.94 |
0.31 |
0.19 |
2.8 |
1.1 |
Incorporated |
4.7 |
5.5 |
10 |
26 |
0.21 |
0.36 |
0.26 |
0.12 |
0.88 |
1.04 |
0.28 |
0.18 |
2.5 |
1.0 |
ANOVA summary |
Cropping System (CS) |
NS |
NS |
NS |
NS |
NS |
NS |
NS |
Crop Residue Management (CR) |
NS |
*** |
NS |
** |
NS |
NS |
* |
Year x CS |
NS |
* |
NS |
NS |
NS |
NS |
NS |
Year x CR |
NS |
* |
NS |
NS |
NS |
NS |
NS |
CS x CR |
NS |
NS |
NS |
NS |
NS |
NS |
NS |
Year x CS x CR |
NS |
NS |
NS |
NS |
NS |
NS |
NS |
C.V. (%) |
4 |
24 |
36 |
51 |
52 |
28 |
30 |
* ,**, and *** + Significance at P = 0.05, 0.01, and 0.001,
respectively; NS = Not significant |
CONCLUSIONS
Crop residue management had apparent short-term effects on
the productivity of pearl millet and cowpea. Incorporation of crop residues
increased pearl millet grain and stover yields over seven years of production.
Also both incorporation or surface retention of residues on the surface increased
cowpea yields over the same time period. Crop residues retained on the surface
helped maintain soil P and K concentrations, suggesting that this treatment
reduced the rate of soil degradation. These results suggest leaving crop residues
in the production fields is an important practice that would help reduce nutrient
mining and thus ensure sustainable production of these two important crops.
Producers need to weigh the long-term benefits to grain and stover production,
and soil maintenance against the short-term economic benefits associated with
burning crop residue, using crop residues for livestock feed or construction,
and other alternate uses.
ACKNOWLEDGEMENTS
Contribution of the IER (Institut dEconomie Rurale), B.P.
258, Bamako, Mali and Dept. of Agronomy, University of Nebraska, Lincoln, NE
68583-0915 U.S.A. Paper No. 12490 of the Journal Series of the Nebraska Agricultural
Research Division are highly appreciated. This research was supported by USAID
Grant No. DAN 1254-G-0021 through INTSORMIL, the International Sorghum and Millet
Collaborative Research Program.
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