Add to ORKGIn semi-arid Kenya, the most dominatn soil types are of limited agricultural productivity due to crusting and compaction. The occurence of soil crusting and compaction is attributed to seasonal rainfall characteristics, physical soil properties and bad tillage practices. Soil crusting and compaction decrease rain water infiltration and increase surface runoff. Seasonal rainwater losses through increased runoff volumes reduce soil moistrue and hance result in agricultural drought. The objective of this sturdy was to examine the hydrological effects of two tillage practices with and without framyard manure on surface runoff and soil loss of crusting and compacting soils under field conditions at Katumani in semi-arid Kenya. Field investigtion...
Production of cereals in a dryland farming system forms an important part of agricultural production...
The West African Semi-Arid Tropics (WASAT) is characterized by a monomodal rainfall pattern, and bas...
Physical and chemical properties of soil surface crusts formed on overgrazed bare ground, in Mukogod...
In semi-arid Kenya, the most dominatn soil types are of limited agricultural productivity due to cru...
In semi-arid Kenya, the most dominant soil types are of limited agricultural productivity due to cru...
In semi-arid Kenya, the most dominant soil types are of limited agricultural productivity due to cru...
In semi-arid Kenya, episodes of agricultural droughts of varying severity and duration occur. The oc...
In semi-arid Kenya, episodes of agricultural droughts of varying severity and duration occur. The oc...
The aim of this work is to investigate the consequences of selected soil and water conservation tech...
In the highlands of Ethiopia, tillage methods and frequency affect drainage, soil erosion, moisture ...
International audienceThe study was aimed at evaluating the effect of rainfall and tillage-induced s...
There is limited documentation of soil and water management technologies that enhance ada...
AbstractAnnual rainfall is less than 500mm of rainfall in the dry farming regions in order to be sto...
The history of soil erosion is an integral part of the agriculture. All over the world, wherever hum...
Soil and water conservation practices need to be tailored to suit the diverse local conditions in s...
Production of cereals in a dryland farming system forms an important part of agricultural production...
The West African Semi-Arid Tropics (WASAT) is characterized by a monomodal rainfall pattern, and bas...
Physical and chemical properties of soil surface crusts formed on overgrazed bare ground, in Mukogod...
In semi-arid Kenya, the most dominatn soil types are of limited agricultural productivity due to cru...
In semi-arid Kenya, the most dominant soil types are of limited agricultural productivity due to cru...
In semi-arid Kenya, the most dominant soil types are of limited agricultural productivity due to cru...
In semi-arid Kenya, episodes of agricultural droughts of varying severity and duration occur. The oc...
In semi-arid Kenya, episodes of agricultural droughts of varying severity and duration occur. The oc...
The aim of this work is to investigate the consequences of selected soil and water conservation tech...
In the highlands of Ethiopia, tillage methods and frequency affect drainage, soil erosion, moisture ...
International audienceThe study was aimed at evaluating the effect of rainfall and tillage-induced s...
There is limited documentation of soil and water management technologies that enhance ada...
AbstractAnnual rainfall is less than 500mm of rainfall in the dry farming regions in order to be sto...
The history of soil erosion is an integral part of the agriculture. All over the world, wherever hum...
Soil and water conservation practices need to be tailored to suit the diverse local conditions in s...
Production of cereals in a dryland farming system forms an important part of agricultural production...
The West African Semi-Arid Tropics (WASAT) is characterized by a monomodal rainfall pattern, and bas...
Physical and chemical properties of soil surface crusts formed on overgrazed bare ground, in Mukogod...