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Soil Conservation

Effects on soil physical properties and soil conservation
Throughout the humid and subhumid tropics soil erosion is a major problem resulting in loss of soluble nutrients and organic matter. Decline of SOM in continuously cultivated soils leads to increased bulk density, decreased infiltration and soil capping. Exposed surface soils, especially in tilled lands, are especially susceptible to the erosive impact of rainfall.

Soil structure and water retention
Alley cropping can improve soil structure through the addition of SOM and activity of the tree root systems. One important parameter of soil structure is the size distribution and stability of aggregates. When large and stable aggregates are present, it creates macro-pores which increases the infiltration rate and water retention, reduces run-off and associated soil erosion, and maintain favorable soil aeration for soil biota (Pellek 1992). Both SOM and root activity contribute to aggregation of soil particles. In a study on an Alfisol in Sri Lanka, Mapa and Gunasena (1995) showed that the mean soil aggregate diameter increased from 1.3 mm of the control to 2.68 and 3.11 mm after three years of alley cropping with Cajanus cajan and Gliricidia sepium, respectively. Increased soil fauna activity, in particular earthworms, can further aid infiltration of water.

Studies conducted on Alfisols have shown that combining no-tillage and alley cropping with Leucaena leucocephala hedgerows results in significantly greater levels of transmission pores, soil moisture retention and available plant water capacity, and lower soil bulk density, penetrometer resistance, water runoff and soil erosion (Kang and Hulugalle 1992, Lal 1989c). On a newly-cleared Ultisol of high-rainfall area in southern Cameroon, Hulugalle and Ndi (1994) found that exchangeable calcium, effective CEC and water infiltration were greatly increased in the alleys of plots where either Flemingia congesta or Senna spectabilis had been planted within 3 years of hedgerow establishment. Increased soil cover by mulching not only protects surface soil from the impact of water splash but also improves microclimatic conditions by lowering soil temperature, minimizing temperature fluctuations, and increasing soil moisture. Budelman (1989) compared the effect of mulches from Leucaena leucocephala, Gliricidia sepium and Flemingia macrophylla applied at a rate of 5,000 kg dry matter ha-1 over a 60-day period in Côte d'Ivoire and found that all three, especially F. macrophylla, influenced soil temperature and moisture content favorably. Four years of mulch application in a study on taro alley-cropped with Calliandra calothyrsus and Gliricidia sepium hedgerows in Western Samoa measurably improved the soil's water holding capacity and soil structure (Rosecrance et al. 1992). Soil moisture levels were consistently higher and soil temperature significantly lower (as much as 10 C cooler in mid-afternoon) in the alley plots compared to the controls throughout the growth of the crop. Noticeably more macrofauna, especially worms, were found in the alley plots than in the controls.

Soil erosion control on sloping lands
The primary function of alley cropping on sloping lands is erosion control and soil conservation. A large number of experimental results and field projects have confirmed the efficacy of dense planting of hedgerows along contours on steeply-sloping lands in controlling soil erosion. Soil erosion is reduced by two approaches: the "barrier approach" and the "cover approach" (Nair 1993). Contour-planted hedgerows act as permeable barriers slowing the rate of water flow so that soil particles are deposited and infiltration of water into the soil is increased (Giller and Wilson 1991, Pellek 1992). The build-up of soil behind hedgerows can gradually lead to the formation of terraces. Soil cover by tree litter and prunings can effectively check raindrop impact and runoff for some time until they are decomposed. This cover effect is generally considered to account for most of the beneficial effects of alley cropping in controlling soil erosion (Kang 1993, Nair 1993).

Paningbatan (1990) provided convincing evidence for the efficacy of alley cropping in checking soil erosion. In a study on an Alfisol with 14% slope and a total rainfall of 1,412 mm during the 3-month study period, maize alley-cropped with contour hedgerows of Desmanthus virgatus, established at a 6-m interhedgerow spacing, effectively contained erosion. The presence of hedegrows combined with zero tillage and the prunings applied as mulch limited soil loss to 0.2 ton ha-1, a significant reduction from 127 tons ha-1 in the control and 41 tons ha-1 with hedgerow and contour cultivation but no mulch. Lal (1989a) showed in a study on an Alfisol in Nigeria that in plots tilled and alley-cropped with L. leucocephala and G. sepium with prunings used as mulch, erosion was reduced by 85% and 73%, respectively, comparing to the plow-tilled control plots.

Introduction | Definition | Hedgerow Species I Species Selection Criteria | Soil Organic Matter & Nutrients | System Management | Crop Yields | Soil Conservation | Weed Dynamics | Tree-Crop Competition | References

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