Innovations as Key to the Green Revolution in Africa 2011
DOI: 10.1007/978-90-481-2543-2_30
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Using Forage Legumes to Improve Soil Fertility for Enhanced Grassland Productivity of Semi-arid Rangelands of Kajiado District, Kenya

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Cited by 6 publications
(7 citation statements)
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“…Crop production depends greatly on soil fertility and the continuous decline in soil fertility is a major constraint to agriculture (Mucheru-Muna et al 2007). This decline in soil fertility is the result of natural and managerial activities such as leaching, erosion and crop harvest, continuous cultivation and overgrazing (Macharia et al 2011) and this decline of soil nutrients will continue unless there are means of replenishing the lost nutrients (Mucheru-Muna et al 2007).…”
Section: Introductionmentioning
confidence: 99%
“…Crop production depends greatly on soil fertility and the continuous decline in soil fertility is a major constraint to agriculture (Mucheru-Muna et al 2007). This decline in soil fertility is the result of natural and managerial activities such as leaching, erosion and crop harvest, continuous cultivation and overgrazing (Macharia et al 2011) and this decline of soil nutrients will continue unless there are means of replenishing the lost nutrients (Mucheru-Muna et al 2007).…”
Section: Introductionmentioning
confidence: 99%
“…Soil analysis at beginning and end of introduced forage legume experiment revealed that soil ph, carbon, nitrogen and potassium increased while calcium decreased significantly from the soil by end of the experiment. In this experiment the higher soil pH was probably due to addition of leaf litters and decay of roots and nodules by legumes (Macharia et al 2011). Decomposition and mineralization process released the nutrients from the organic residues and it enhanced due to increased microbial activities which accelerated by favourable soil condition and carbon availability (Landon 1984, Muriuki andQureshi 2001).…”
Section: Soil Chemical Propertiesmentioning
confidence: 84%
“…Forage legumes have potential to bind the soil aggregates with organic matter after decomposition of their residues hence these recognized as the soil building crops. Incorporation of legume residues in the soil enhanced the soil ph it might be due to decomposition and mineralization of organic residues by micro-organisms which resulted into increased soil ph (Macharia et al 2011). As a result of higher soil ph or less acidic condition nutrients such as carbon, nitrogen, phosphorus, potassium, calcium, magnesium, sulphur etc.…”
Section: Forage Legumes and Soil Healthmentioning
confidence: 99%
“…Los contenidos oscilaron de 0.78 cmol kg -1 a 1.97 cmol kg -1 , lo cual es alto para todos los sistemas de uso de suelo. Estos resultados concuerdan con lo reportado por Aghasi et al (2011), quienes no encontraron variaciones en K y P en suelo de pastizales convertidos a agrícola, así como Macharia et al (2011) donde los valores de P no fueron signif icativamente diferentes. Por otra parte, los resultados de P y K fueron menores para la profundidad 5-30 cm a diferencia de la profundidad 0-5 cm, en este sentido, Rosolem y Calonego (2013) reportan en su estudio bajo diferentes sistemas de gestión de suelo y rotación de cultivos, una tendencia a la pérdida de P en el sistema suelo-planta y una lixiviación del K en la capa superf icial del suelo.…”
Section: Propiedades Del Suelounclassified