1998
DOI: 10.1080/00103629809369969
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Effect of cultivation on physical and chemical properties of a Vertisol in middle Awash Valley, Ethiopia

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Cited by 15 publications
(9 citation statements)
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“…As carbon to nitrogen ratio (C/N) is an index of nutrient mineralization and immobilization where by low C/N ratio indicates higher rate of mineralization (Brady and Weil, 2002), rate of soil organic matter mineralization is lower under closed area with SWC. In addition, the lower C inputs because of less biomass C return on free grazing lands caused the reduction of SOM and TN (Girma, 1998). The most evident impact of grazing is the removal of a major part of above ground biomass by livestock that decreases the input of aboveground litter to the soil.…”
Section: Soil Chemical Propertiesmentioning
confidence: 99%
“…As carbon to nitrogen ratio (C/N) is an index of nutrient mineralization and immobilization where by low C/N ratio indicates higher rate of mineralization (Brady and Weil, 2002), rate of soil organic matter mineralization is lower under closed area with SWC. In addition, the lower C inputs because of less biomass C return on free grazing lands caused the reduction of SOM and TN (Girma, 1998). The most evident impact of grazing is the removal of a major part of above ground biomass by livestock that decreases the input of aboveground litter to the soil.…”
Section: Soil Chemical Propertiesmentioning
confidence: 99%
“…Due to forest clearance lower total N content in soil was reported by several authors from different parts of the world (Girma 1998;Jing-cheng et al 2004). DeBano et al (1979) reported that losses of soil N can occur when heated to temperature as high as 100 o C, which may happen during burning associated with shifting cultivation.…”
Section: Discussionmentioning
confidence: 99%
“…Thus carbon fractions resulting from the decomposition of acacia are more resistant to degradation and therefore persist for longer times than those resulting from Gliricidia decomposition. The lower levels of soil organic carbon fractions in cultivated soils may have resulted from a combination of low carbon inputs because of less biomass C return on harvested land and greater C losses because of aggregate disruption, increased aeration by tillage, crop residue burning, accelerated water erosion and livestock grazing [26,27]. In contrast, higher soil organic carbon contents of soils under Acacia and Gliricidia land uses are probably due to higher litter production and N fixation by the leguminous Acacia [28] and Gliricidia biomass.…”
Section: Wwwijeabcommentioning
confidence: 99%