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1 Catenary Variation of Soil Properties Under Oil Palm Plantation Ethiopian Journal of Environmental Studies and Management Vol.3 No.1 2010 Catenary Variation of Soil Properties under Oil Palm Plantation in South Western Nigeria *Aweto A.O. and ** Enaruvbe G. O Abstract This study characterizes variations in soil properties in a catena under a 30-year oil palm (Elaeis guineesis) plantation established on sedimentary soil in south-western Nigeria. A 300 metre transect was delimited in an oil palm plantation adjoining a tributary of Ossiomo River at Okhuo, near Benin, Nigeria. The transect was divided into upper, middle and lower slope segments. Each segment was further subdivided into ten 10 by 10 metres quadrats, making a total of 30 quadrats. Five soil samples were randomly collected from 0-20cm layer of each quadrat and analysed for particle size composition, organic carbon, macronutrients and micronutrients. Exchangeable calcium and cation exchange capacity were significantly higher in the middle slope segment of the catena due to the combined influence of soil organic matter and clay which were also higher in the middle slope than in the upper and lower slopes. Soil pH was highest in the upper slope and declined down slope. There were no significant variations in the levels of extractable manganese, copper and zinc between the upper, middle and lower slopes but extractable iron was significantly higher in the lower slope due to the occurrence of more moist and acidic soils in the lower slope. Topographic position and ground slope are the main factors accounting for variations in soil properties along the catena. There is the need to manage parts of oil palm plantation on different topographic positions differently, taking cognizance of variations in soil properties along the catena, in order to ensure long term sustainability. Key words: Oil palm, catena, soil, macronutrients, micronutrients, Nigeria. Introduction s with other parts of the tropics, rubber and palm oil and kernel of the sub- Aplantation agriculture, featuring region comes from peasant holdings. the production of crops in monocultures in Most of tree crops such as teak, large commercial estates, has gained gmelina, pines, eucalyptus, cocoa and para widespread acceptance and has consequently, rubber grown in plantations in West Africa are become an important feature of the agricultural exotics. The oil palm (Elaeis guineensis), a economy of tropical Africa. The plantation native of tropical West Africa occurring in a system of agriculture is assuming increasing zone extending from Guinea to Congo basin popularity, particularly in tropical countries (Irvine1969, Onwueme & Sinha 1991) is a such as Malaysia, Indonesia, Cote d’Ivoire, noteworthy exception. Nigeria was the Nigeria and many other parts of the world. world’s largest exporter of palm oil and kernel Evans (1992) reported that the areal extent of in the 1960s accounting for 43% of the world’s plantation agriculture of all types doubled in production. Today, however, it only accounts tropical Africa and increased about six fold in for 7% of total output (World Rainforest other parts of the tropics between 1965 and Movement 2001). The country has ceased to 1980. export palm oil and is now a net importer of This increasing interest in plantations vegetable oil. Most of the oil palm plantations can be attributed to advantages of the and the small-scale peasant holdings in Nigeria plantation system of agriculture, such as were established without adequate environmental conservation and protection, consideration of the impact of environmental and economic and social benefits. Tree crops factors, especially, the soil and its spatial (and are commonly grown in plantations in the hence, catenary) variation on the productivity tropics. Some of these include coffee (Coffea and sustainability of oil palm plantations. The arabica), cocoa (Theobroma cacao), rubber soil varies along the landscape, even within (Hevea braziliensis) oil palm (Elaeis limited areas, giving rise to a succession of soil guineensis), eucalypts ( Eucalyptus spp), teak types, known as a catena, from the hill top to (Tectona grandis ), gmelina (Gmelina the valley bottom (Milne 1935). The catenary arborea) and pines (Pinus spp.). Small-scale differentiation of soils is of pivotal importance indigenous farmers in West Africa have to the management of soils in different embraced monoculture, a diagnostic feature of topographic positions in the landscape, plantation agriculture, and a significant especially in large plantation monocultures. proportion of exports such as cocoa, coffee, *Department of Geography University of Ibadan, Ibadan, Nigeria [email protected] **25 Saka Tinubu Street,Victoria Island, Lagos, Nigeria. 1 Catenary Variation of Soil .... Aweto and Enaruvbe EJESM Vol.3 No.1 2010 Several studies have examined the The natural vegetation is moist ecological requirements and environmental evergreen rain forest ( Hopkins 1974) that is impact of oil palm on soil ( Irvine 1969, rich in timber producing trees such as Onwueme & Sinha 1991, Aweto & Ekiugbo Piptadeniastrum africanum , Triplochiton 1994), while others considered catenary scleroxylon , Milicia excelsa , Antiaris toxicaria relationship between slope, soil and vegetation and Ceiba pentandra . Raffia palms, especially in the tropical environment (Furley & Newey Raphia hookeri and Raphia vinifera are locally 1979, Aweto & Iyamah 1993, Abrams et al abundant in riparian forests fringing rivers. As 1997). Apart from Vine (1941) who studied a a result of centuries of traditional agriculture catena under cacao in south western Nigeria, it featuring rotational bush fallowing and the appears that catenas under tree crop plantations production of cassava ( Manihot esculenta ) and have not been characterized and hence, soil maize ( Zea mays) coupled with unsustainable variation along topography in these plantations timber exploitation, the natural forest have not been adequately studied. This study vegetation has been destroyed. The soils are therefore attempts to evaluate catenary sandy and were derived from sedimentary variation of surface soil properties under oil rocks, especially unconsolidated sediments of palm (Elaeis guineensis) in South Western sandstone of Tertiary Age. They are mainly Nigeria. Studies on catenary differentiation of Ultisols, according to United States Soil soils in the forest zone of Nigeria concentrated Taxonomy ( Soil Survey Staff, 1996) and on soil profile characteristics and Acrisols according the Food and Agricultural macronutrients and ignored micronutrients Organization system of soil classification. The (Vine 1941, Smyth & Montgomery 1962, soils are deeply weathered, strongly leached Ogunwale et al 1986, Aweto & Iyamah 1993) and lack significant weatherable minerals which sometimes exert a more severe limiting within the soil solum. effect on the growth of crops, tree and field Methodology crops inclusive. It was therefore considered In this study, a sloping portion of a 30 important in the current study to evaluate the – year old oil palm plantation, adjoining a extractable micronutrients iron, copper, lead tributary of the Ossiomo River, was selected and zinc in different slope segments in a catena for the purpose of evaluating the impact of under oil palm, in addition to the topography on soil physical and chemical macronutrients routinely analysed in properties in a plantation of the same age. pedological studies. Differentiation of soils along a catena is most Study area marked along transects running from the crest The present study was conducted at of the interfluve to the valley bottom ( Gerrard Okhuo, about 25 kilometres to the north east of 1981). Accordingly, a transect was delimited Benin City, the capital of Edo State, Nigeria. on the valley slope of the tributary of the The area is a part of the coastal plain of Ossiomo River, traversing the plantation, from southern Nigeria and is generally below 120 the crest of the spur to the valley bottom. The metres above mean sea level (Udo 1970).The transect was 300 metres long and it was topography is gently undulating, except near divided into three slope segments – the upper, rivers where steep slopes occasionally occur middle and lower slopes. Each of the three near the floors of the river channels. The slope segments was further sub-divided into climate is tropical rainforest climate (Koppen’s ten quadrats measuring 10 metres by 20 Af climate) with a bi-modal rainfall regime. metres, making a total of 30 plots. At the The mean annual rainfall is about 1700 mm, centre of each quadrat, slope angle was with most of the rains concentrated in the wet measured using an abney level. Soil samples season lasting from March to October. Two were collected from five randomly selected periods of peak rainfall occur in June – July points within each plot at the depth of 0-20cm and September – October, the two peaks being using a soil auger. The five samples for each separated by a relatively dry period in August. quadrat were mixed thoroughly together to Temperatures are relatively uniform obtain a composite sample. Soil sampling was throughout out the year, with an average restricted to the top 20 cm of the profiles annual average of 27º C and no marked because it is the most productive soil layer that seasonal or monthly departure from the annual exerts the greatest effect on crop yield. average (Figure 1) 2 Ethiopian Journal of Environmental Studies and Management Vol.3 No.1 2010 Fig. 1: Map of Benin Plains, S.W. Nigeria, showing the study area The study of Lal et al has shown that removing micronutrients were leached from the soil the top 7.5cm of the soil in south-western using 0.1 M HCL and zinc, iron, copper and Nigeria resulted in 90% reduction in corn yield manganese in the leachate determined on the ( Lal et al 1975). Furthermore, it has been atomic absorption spectrophotometer. shown that the effect of tree vegetation on soil Soil physical and chemical properties organic matter and nutrients in the forest zone in the three slope positions were compared of south-western Nigeria is largely restricted to using Analysis of variance (ANOVA) to the top 10cm of the soil solum (Aweto 1981).
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