Effects of conservation agriculture on runoff, soil loss and crop yield under rainfed conditions in Tigray, Northern Ethiopia

Abstract

The aim of conservation agriculture (CA) is to improve soil quality and crop yield whilst reducing runoff and topsoil erosion. An experiment was carried out in a rainfed field using a permanent raised bed planting system for 3 yr (2005-2007) in Adigudem, northern Ethiopia in order to evaluate the effect of CA on runoff, soil loss and crop yield. CA practices were introduced in fields with Vertisols in a randomized complete block design on permanent 5 x 19 m plots. Three treatments were evaluated: (1) conventional tillage (CT) with a minimum of three tillage operations and removal of crop residues, (2) terwah (TER) that was similar to CT except that contour furrows were included at 1.5 m intervals, and (3) derdero+ (DER+), which consists of permanent raised beds with a furrow and bed system, retention of 30% of standing crop residues and zero tillage on the top of the bed. All ploughing as well as the maintenance of the furrows of the permanent raised beds was done using a local ard plough called maresha. Results from monitoring over 3 yr showed that soil loss and runoff were significantly higher (P < 0.05) in CT followed by TER and DER+. Average soil losses of 5.2, 20.1 and 24.2 t/ha were recorded from DER+, TER and CT, respectively. Runoff was 46.3, 76.3 and 98.1 mm from DER+, TER and CT, respectively. Grain yield was significantly lower (P < 0.05) in DER+ under teff in 2006, probably due to the high sensitivity of teff to weeds. The yield of wheat in 2007 was significantly higher in DER+ followed by TER. The terwah system is recommended as a first measure for wider adoption to reduce runoff and soil loss and to increase crop yield. The long-term goal is to achieve a derdero+ system, i.e. a permanent raised bed planting system along with the application of crop residues

Land Degradation in the Ethiopian Highlands

“…Furthermore, on Vertisols, which are well represented in Ethiopia (Kanwar and Virmani 1986;Moeyersons et al 2006), the first rains are well absorbed, because of the deep shrinkage cracks. After some time, with the closing of the cracks, these soils become completely impervious and favour significant runoff production (Bauduin and Dubreuil 1973;Gebreegziabher et al 2009;Oicha et al 2010;Araya et al 2011). Moreda and Bauwens (1998) found the most significant correlation between monthly precipitation and summer flow in the Awash headwaters to occur in August, at the beginning of the second half of the rainy season, when 'there is greater opportunity for flow generation (even for smaller storms) since the catchment is already moist'.…”

Effects of land use, slope gradient, and soil and water conservation structures on runoff and soil loss in semi-arid Northern Ethiopia

“…However, despite a huge capital and labour investment to install this reservoir, it has never been used for irrigation apart from Araya et al (2011). The spacing of SWCT which depends on slope gradient (Table 1) is based on regional guidelines (BoNAR, 1997).…”

Sediment yield and alternatives soil conservation practices of teak catchments

“…Cracking at a dry season can reach 50 cm depth, at least 1 cm wide and washing materials on surface soil in the cracks (Aydinalp, 2010). A deeper chrack (100 cm depth and 1-2 cm wide) in Trigay, Northen Ethiopia has been found by Araya et al (2011). A unique characteristic of the teak plantations in the study area is that the teak stands release their leaves in dry season.…”