Research Article
Volume 2 Issue 2 - 2017
On Farm Participatory Evaluation of Integration of both Mechanical and Biological Soil and Water Conservation Practices in West Arsi and East Shoa Zone, Oromia, Ethiopia
Kasahun Kitila*, Mekonnen Workina and Abay Chala
Oromia Agricultural Research Institute, Adami Tulu Agricultural Research center, Ziway, Ethiopia
*Corresponding Author: Kasahun Kitila, Oromia Agricultural Research Institute, Adami Tulu Agricultural Research center, Ziway, Ethiopia.
Received: November 14, 2017; Published: November 22, 2017
Abstract
Soil erosion is one of the major challenges of Ethiopia deteriorating the productivity of the land. Soil and water conservation (SWC) is the alternative to reverse the threat and protect the land. Over the last three decades, different soil and water conservation activities have been undertaken. However, soil erosion still persists and become major threats of Ethiopian farmers. Despite the massive mobilization of resources for SWC, only very few studies have been done to analyze the impacts of integrated soil and water conservation measures with respect to restoration of degraded agricultural lands. In addition, most plot-based studies are focused on assessing the severity of soil erosion in physical terms and lack information on the impact of SWC on soil fertility improvement and soil nutrient content dynamics. This study was conducted at purposively selected districts namely Adama and Shashemene in East Shoa and West Arsi Zones of Oromia regional state respectively. The study was aimed to evaluate the effect of integrated Soil and water conservation measures in restoring degraded agricultural land. Dasho grass (Pennisetum pedicellatum) and Elephant grasses (and Pennisetum purpureum) were planted on graded soil bund in both districts as an integration measures. It was identified that soil nutrient contents in terms of total nitrogen, available phosphorous, available potassium and soil organic carbon content showed an increasing trend since establishment (2013). On the other hand, this kind of soil and water conservation practices on agricultural land showed promising way of carbon sequestration as the climate change mitigation strategy. The findings recommended that use of integrated soil and water conservation measures as strategy of rehabilitating degraded agricultural land should be considered in implementing integrated water shed management. In conclusion, to reduce soil erosion sustainably, integrated soil and water conservation should be introduced considering agro ecology and climatic condition of the intervention area.
Keywords: Soil and water conservation; Soil erosion; Soil nutrient
Introduction
Agriculture is the major source of livelihood in Ethiopia. However, land degradation in the form of soil erosion has hampered agricultural productivity and economic growth of the nation (Haileslassie., et al. 2005; Balana., et al. 2010). Land degradation, low agricultural productivity and poverty are critical and closely related problems in the Ethiopian highlands (Gebremedhin, 2007; Yitbarek., et al. 2012). Investments in soil and water conservation (SWC) practices enhance crop production, food security and household income (Adgo., et al. 2013). Recognizing these connections, the government of Ethiopia is promoting SWC technologies for improving agricultural productivity, household food security and rural livelihoods. Particularly, in the Ethiopian highlands, different SWC technologies have been promoted among farmers to control soil erosion problem. The traditional physical SWC measures, such as soil bund and terraces, have been practiced in a few areas for several hundred years (e.g., Konso area by Tadesse, 2010), for which awareness and experience have been confined in that particular area. The structures having certain technical designs and specifications have been introduced to many new areas, assuming that land users can adopt it sooner or later. Recently, pilot projects, campaign work, food for work programs (grain and edible oil support), etc. were initiated and are ongoing by both government and non-governmental organizations. However, most of these SWC technologies, especially construction of SWC practices on agricultural land, has got less acceptance (Tesfaye., et al. 2013; Teshome., et al. 2014), largely because investments by farmers in SWC are influenced by the ecological, economic and social impacts of the SWC technologies. The actual and long term financial profitability to farm households critically influences the process of accepting and replicating such structures (De Graaff., et al. 2008). Poverty and a long time span to get return from soil conservation activities reduced adoption of SWC technologies in East Shewa (Ethiopia) (Shiferaw and Holden, 2009). In the northwestern Ethiopian highlands, labour shortage, problems with fitness of the SWC technologies to the requirements of farmers and land tenure insecurity discouraged farmers from adopting SWC measures such as soil and stone bunds, fanya juu, etc. (Bewket, 2007).
Therefore, it is important to improve farmers’ level of understanding on the effect of soil and water conservation technologies in controlling soil erosion and maintaining soil nutrient content on agricultural land. On the other hand, participatory evaluations of these technologies are also equally crucial to improve farmers’ level of adoption of SWC technologies. Despite the massive mobilization of resources for SWC, only very few studies have been done to analyze the impacts of integrated soil and water conservation measures with respect to restoration of degraded agricultural lands. In addition, most plot-based studies are focused on assessing the severity of soil erosion in physical terms and lack information on the impact of SWC on soil fertility improvement and soil nutrient content dynamics. Consequently in this study we highlighted some important aspects of importance of SWC with following objectives;
  1. To evaluate the impact of the integration of both physiscal and biological SWC on controlling soil erosion and improving soil fertility.
  2. To improve farmers’ practical level of awareness/understanding on SWC technologies.
Expected output
  1. The impact of the integration of both physiscal and biological SWC on controlling soil erosion and improving soil fertility will be identified.
  2. The contribution of the integrated SWC in storing SOC on agricultural land will be known.
  3. Production and productivity of the land will be improved.
Materials and Methods
This conservation measure was established at six different Sites (three in Shashemene, three in Adama districts). Animal forages such as Elephant grass (Pennisetum purpureum),Dansho grass (Pennisetum pedicellatum) and Rhodes grass (Chloris gayana)were used as an integration measure with soil bund.
Farmers’ field visit was done to improve farmers’ level of understanding on SWC technologies. Composite Soil samples were collected from each site every year since establishment and analyzed to evaluate soil nutrient dynamics.
Result and Discussions
Change in total Nitrogen, available phosphorous, potassium and SOC from 2013-2016 were analyzed every year. Accordingly, Total N, available phosphorous, potassium and soil organic carbon showed an increasing trend at all sites since 2013 (Figure 1)
Figure 1: Change in total Nitrogen, available phosphorous, potassium and SOC from 2013-2016.
Soil nutrient content is highly significantly different at p < 0.05 between and within experimental sites across the years (Table 1). Major soil nutrient contents also showed an increasing trend since 2013 (baseline) indicating that integrated SWC measures interventions have appositive effect in improving soil nutrient content. On the other hand, SOC content of the soil showed an increasing trend since establishment of integrated SWC indicating that it is a promising way of carbon sequestration on agricultural land. Major soil nutrients such as Total N, available phosphorous, potassium and soil organic carbon are highly significantly different p < 0.05 across the year in both districts (Table 2). In addition, Soil nutrient status in 2013 (baseline) is also smaller and highly significantly different from the soil nutrient status after intervention. EC (electrical conductivity) and soil pH are not significantly different across the year with in the district but are significantly different p < 0.05 between the districts.
District Sites Years Total N (%) Avail. P in ppm Avail. K in mg/kg soil EC in mmhos/cm Soil pH SOC (%) C/N
Adama Didibissa  2013 0.17fgh 30.00hi 120.40j 0.22f 6.23f 3.53d 21.01abcd
Didibissa  2014 0.19efg 43.00e 185.00g 0.37b 7.05d 3.49d 18.44bcd
Didibissa  2015 0.25bc 77.33b 274.00c 0.36b 6.63e 5.74b 22.66abc
Didibissa  2016 0.32a 89.44d 319.52e 0.32abc 7.51a 7.05a 21.82ab
Qobo  2013 0.15gh 32.00gh 125.00ij 0.31c 6.57e 2.90def 19.98abcd
Qobo  2014 0.20def 55.00c 145.00h 0.32c 7.55c 4.66c 23.81abc
Qobo  2015 0.25bc 72.00b 215.00f 0.21f 8.03b 5.62b 22.16abcd
Qobo  2016 0.33a 85.44d 322.52e 0.32abc 7.61a 8.05a 24.24ab
Futala  2013 0.15gh 57.00cd 130.10i 0.37b 6.10g 2.65ef 17.71cd
Futala  2014 0.22cde 74.00b 190.00g 0.29cd 8.00b 4.22c 19.20bcd
Futala  2015 0.30a 89.00a 262.27d 0.36b 8.17a 5.90ab 19.75abcd
Futala 2016 0.34a 85.00d 320.52e 0.33abc 7.61a 8.05a 24.14ab
Shashemene Ebicha  2013 0.14h 20.00j 122.41j 0.27de 5.62h 2.54f 18.38bcd
Ebicha  2014 0.19efg 37.00fg 250.00e 0.46a 5.55i 4.53c 24.00ab
Ebicha  2015 0.24bcd 59.00c 295.00a 0.26de 5.56hi 5.56b 23.18abc
Ebicha 2016 0.32a 91.50d 315.42e 0.31abc 7.25a 7.05a 21.82ab
Halache  2013 0.15gh 23.00j 110.00k 0.12h 5.27k 2.40f 16.18d
Halache  2014 0.18efg 35.00gh 215.00f 0.31c 5.45j 3.27de 18.32bcd
Halache  2015 0.25bc 57.00cd 283.33b 0.27de 5.58hi 6.19ab 25.49a
Halache 2016 0.36a 92.50d 325.42e 0.31abc 7.25a 7.05a 21.12ab
Abaro  2013 0.14h 25.00ij 142.07h 0.17g 5.15l 2.44f 18.45bcd
Abaro  2014 0.20def 42.00ef 270.00c 0.32c 5.55i 4.18c 22.26abcd
Abaro  2015 0.27ab 53.00d 296.17a 0.24ef 5.59hi 6.54a 24.29ab
Abaro 2016 0.35a 93.50d 324.42e 0.33abc 7.05a 7.25a 20.72ab
CV (%) 12.68 7.2 1.79 6.7 0.57 9.15 17.99
LSD0.05 0.04 5.89 6.00 0.03 0.06 0.64 6.21
Table 1: Mean comparison of soil nutrient content at different site across the years (significant at p < 0.05).
Districts Years Total N (%) Avail. P in ppm Avail. K in mg/kg soil EC in mmhos/cm Soil pH SOC (%) C/N
 Adama 2013 0.16c 39.67c 125.17d 0.30bc 7.30a 3.03c 19.57bc
2014 0.20b 57.33b 173.33c 0.33ab 7.53a 4.12b 20.48bc
2015 0.27a 79.44a 250.42b 0.31abc 7.61a 5.75a 21.52ab
2016 0.32a 89.44d 312.52e 0.32abc 7.51a 7.05a 21.82ab
Shashemene 2013 0.14c 22.67d 124.83d 0.29bc 5.35b 2.46d 17.67c
2014 0.19b 38.00c 245.00b 0.34ab 5.52b 4.00b 21.53ab
2015 0.25a 56.33b 291.50a 0.29bc 5.58b 6.10a 24.32a
2016 0.33a 76.33a 320.50e 0.30bc 5.50b 6.21a 24.52a
CV (%) 12.86 18.44 9.23 21.26 5.82 12.24 17.75
LSD0.05 0.02 8.55 17.64 0.05 0.34 0.49 3.50
p-value 0.001 0.001 0.001 0.065 0.001 0.001 0.012
Table 2: Mean comparison of major soil nutrient content across experimental period significant at p < 0.05.
Similarly, Eshatu (2004) reported that SWC practices significantly increased organic carbon, total nitrogen and soil-organic matter in the soil. Other studies also indicated that there is a positive contribution of SWC measures to the reduction of soil erosion, conservation of soil moisture, and soil nutrient content (Asefa., et al. 2003; Vancampenhout., et al. 2006; Gebreegziabher., et al. 2009; Mekuria., et al. 2011). Many other cases studies also indicated that integration of biological with physical measures improved effectiveness of the structure and soil fertility Zougmore., et al. (2002) and Adimassu., et al. (2012).
Conclusion and Recommendations
Major soil nutrients such as total nitrogen, phosphorous, potassium and SOC contents showed an increasing trend since establishments of integrated soil and water conservation measures at all sites. In addition to providing forage to the livestock and controlling soil erosion, integrated soil and water conservation can improve soil fertility and increase soil organic carbon pool. Based on this study, the following recommendations were given:
  1. Integrated SWC activities should be scaled up particularly on agricultural land as means to control soil erosion problem, improving soil fertility and as a source of feed for livestock.
  2. Integrated soil and water conservation is a promising way of carbon sequestration on agricultural land. Therefore, this should be considered in the implementation of climate smart agriculture as strategy to mitigate climate change.
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Citation: Kasahun Kitila., et al. “On Farm Participatory Evaluation of Integration of both Mechanical and Biological Soil and Water Conservation Practices in West Arsi and East Shoa Zone, Oromia, Ethiopia”. Innovative Techniques in Agriculture 2.2 (2017): 352-357.
Copyright: © 2017 Kasahun Kitila., et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.