CHAPTER ONE
INTRODUCTION
1.1 Background of study
Nigerian Sudan savanna zone is situate etween latitude 9 3 and 12 31 N and longitude and 14 3 E whi h overs a out 22 8 million he tares representing a out one quarter of Nigeria‟s geographi al area (Odunze, 2006) The region is hara terized y high annual average temperature (28-32°C), short wet season and long dry season (6-9 months), abundant short grasses (<2 m) and a few scattered trees (Lal, 1997). Large expanse of arable land exists in the Sudan Savanna Zone of Nigeria with potential for the production of largely grain crops like maize, sorghum, millet, rice and wheat (FFD 2012). Most Nigerian Savanna soils are highly weathered and fragile with low activity clays, thus making their fertility decline under continuous arable cropping (Odunze 2006; FFD, 2012). Generally, soil productivity declines rapidly when vegetation cover is lost and inappropriate management practices are adopted (Lal 1997), thereby resulting in soil organic matter depletion and reduced agricultural productivity and food security.
Population increase and the need to achieve food security; especially in Nigeria, has given rise to clearing of forests for agricultural land use (Osakwe, 2014). Tropical soils are inherently fragile and therefore, sensitive to land use and management since removal of soil cover and subsequent tillage are activities that are likely to affect soil physical and chemical properties and micro aggregate stability (Osakwe, 2014).
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