Indian Journal of Agricultural Research

  • Chief EditorV. Geethalakshmi

  • Print ISSN 0367-8245

  • Online ISSN 0976-058X

  • NAAS Rating 5.60

  • SJR 0.293

Frequency :
Monthly (January, February, March, April, May, June, July, August, September, October, November, December)
Indexing Services :
BIOSIS Preview, ISI Citation Index, Biological Abstracts, Elsevier (Scopus and Embase), AGRICOLA, Google Scholar, CrossRef, CAB Abstracting Journals, Chemical Abstracts, Indian Science Abstracts, EBSCO Indexing Services, Index Copernicus
Indian Journal of Agricultural Research, volume 59 issue 2 (february 2025) : 262-270

Agropastoralist Community-led Restoration of Degraded Drylands: Factors Influencing Adoption of Soil Conservation Practices in Semi-arid Regions of Kenya

James Mumo Mutio1,*, Ruth Njoroge1, Syphyline Kebeney1, Wilson Ng’etich1, Harrison Churu1, Boniface Alkamoi2, Denis Mugaa1, Fred Wamalwa3
1Department of Soil Science, University of Eldoret, Kenya.
2Department of Seed Crops and Horticultural Sciences, University of Eldoret, Kenya.
3Department of Agricultural Economics and Rural Development, University of Eldoret, Kenya.
Cite article:- Mutio Mumo James, Njoroge Ruth, Kebeney Syphyline, Ng’etich Wilson, Churu Harrison, Alkamoi Boniface, Mugaa Denis, Wamalwa Fred (2025). Agropastoralist Community-led Restoration of Degraded Drylands: Factors Influencing Adoption of Soil Conservation Practices in Semi-arid Regions of Kenya . Indian Journal of Agricultural Research. 59(2): 262-270. doi: 10.18805/IJARe.AF-860.

Background: The conventional approach of soil conservation practices in degraded drylands has shown little success. Lack of knowledge on factors influencing inhabitants of such regions to adopt appropriate conservation practices is the primary cause of low adoption. This is because the disseminators of conservation practices assume a one-fit-all design, resulting in a disconnect between them and farmers. Thus, this study aimed to understand factors influencing soil conservation practices in agropastoral dryland communities of semi-arid lowland West Pokot, with a particular interest in terraces.

Methods: A concurrent mixed-method approach embedded in a cross-sectional survey was used and data were collected through semi-structured questionnaires, focus group discussions and field measurements of existing terrace attributes. Data were subjected to descriptive analysis, Spearman’s rho correlation, Kruskal Wallis and Chi-Square Test of Independence.

Result: The community-driven approaches, gender, size of land and topography are key factors contributing to terrace adoption. Sixty percent of farmers living in degraded high-sloped lands have portions of their farms terraced with average terrace dyke volumes of 103.8±21.45 m³, 105.89±33.13 m³ and 129.6±15.97 m³ for highly sloped, relatively flat and moderately sloppy areas respectively. The study further established terrace dyke sedimentation and limited terrace embarkment reinforcement options as the major challenges facing terracing adoption in the region.

Soil degradation is one of the major challenges affecting  agroecosystems worldwide (Scherr, 2019; Zhu, 2020). The process deprives more than 35% of the arable landmass of its ecological functions (Pennock et al., 2015). In Sub-Saharan Africa, soil degradation is aggravated mainly by improper agricultural practices (Tindwa et al., 2019). This is spurred by extensive farming, which makes land size   the main factor determining crop yield. Thus, clearing natural vegetation for crops is rampant, contributing to soil erosion (Adonia and Kakurungu, 2014). This practice accounts for more than 70 billion tons of agricultural soil loss annually, with the statistics projected to exponentially increase with increasing population pressure (FAO, 2017).
       
In Kenya, land degradation is highly intensified in arid and semi-arid regions where soils are inherently weak with crop-growing inhibitors (Sidle et al., 2019).  The regions tend to be home to the most impoverished communities,   who depend on natural resources for livelihood (Gaur and Squires, 2018). Their low resource status further contributes to the low adoption of conservation management strategies (Shiferaw, 2002). As the rate of degradation continues rising, many counties in Kenya are on the verge of losing their productive farmland (Nguru and Rono, 2013). West Pokot County, is an example of a severely degraded arid and semi-arid (ASAL) region,  transformed to its current status through anthropogenic activities (LADA, 2016). In response to the soil loss problem farmers in the these drylands of Kenya adopt easy-to-apply, biological measures but recently have started venturing into mechanical soil conservation strategies, with terrace, emerging as one of the most important practices (Mudalagiriyappa et al., 2019; Oteng’i et al., 2000; Zougmore et al., 2014). The structures’ prominence and effectiveness are underscored by their ability to split the land’s slope into small hydrographic units, hence controlling surface runoff (Tenge et al., 2011), particurlarly on high sloped lands. Further  studies (Gachene et al., 2019) indicated that terraces could reduce surface runoff by more than 90% and curb soil loss by more than 85% on different slope levels, these findings corroborate with findings conducted in other parts of the world including Cyprus (Camera et al., 2018).
       
Although communities in drylands show efforts to combat soil erosion, the level of adopting soil conservation practices in agro-pastoralist communities of Kenya and across Africa has been low. Such a trend has not only resulted in continued soil erosion and increasing land degradation but also hindered the propagation of effective conservation practices. Therefore, this study aimed to  evaluate factors determining the adoption of indigenous soil and water conservation practices in drylands and challenges associated with terracing as a soil and water conservation practice.
The study was conducted in three villages (Parak, Kaporowo, Kapkitony) of Korellach Sub-location, Chepareria ward in West Pokot County from the year 2019 to 2021. The villages are positioned between 35°7' and 35°27' East and 01°15' and 01°55' North as shown in Fig 1. Parak village lies on altitudes ranging between 1906 to 1954 meters above sea level (asl) and with an average slope of>20%. Kaporowo is on the middle slopes (10-20% slope) and at an altitude ranging between 1776 and 1905m asl. The slightly gentle slopes of <10% are found in Kapkitony with an elevation of 1683-1755m above sea level (Maphill, 2011).

Fig 1: A map of the study location layered on elevation contours: Chepareria ward, West Pokot, Kenya.


       
The residents of the ward are mainly agro-pastoralists, cultivating their land during the long rainy season running from April to August, thereafter, opening up lands for animal grazing. This unregulated practice has severe erosion implications particularly on the poorly developed and young soils (Touber, 1991).
 
Study design
 
The study adopted a concurrent mixed-method approach embedded in a cross-sectional survey design. A three-tier methodology approach was used in data collection; (i) one-on-one interviews (ii) focus group discussion (FGD) and (iii) field measurement of terrace attributes.
 
One-on-one interviews
 
A sample size of sixty two households out of 120 households was cluster-sampled across three villages (Etikan et al., 2016). The interview provided primary qualitative and quantitative data that were complemented by FGDs. The questionnaire used for interviews comprised of a mixture of open and closed-ended questions for data collection. The survey was centred on farm-level soil conservation measures, their benefits and general perception towards soil degradation and contributing factors to terracing and household members involved in soil conservation.
 
Focus group discussion (FGD)
 
The discussions (1-2 focus group) were conducted in each village. According to the sparsely populated nature of the landscape number of the FGDs was estimated as adequate to achieve theme saturation for the content required to support the one-on-one interviews. Participants of each FGD comprised 10 farmers, with a follow-up discussion with 5 key informants to validate the information. For each FGD, at least 40% of the participants were women as per the two-third gender rule requirement (Kaimenyi et al., 2013; Opoku et al., 2018). The FGDs focused on the following thematic areas; community perception of soil conservation, drivers and barriers to adopting soil conservation practices in their community, socio-economic dynamics intensifying or alleviating soil erosion and potential solutions.
 
Measurements of constructed terrace attributes
 
Terrace characteristics were measured on 44 farms belonging to farmers who had adopted the technology and participated in one-on-one interviews. The measurements included horizontal interval (m) (Sheng, 2002), dyke cross-sectional area (m²) (Saiz et al., 2016), terrace length (m), terrace volume siltation level (m³) and farm slope (%). Fanya Juu and Fanya Chini terraces are shown in Fig 2. According to the designs used by farmers during construction, terrace volume was calculated as the product of cross-section, the width of cross-section and the length of the channel (width x breadth x height). The same method was used to calculate the amount of silt accumulation in the dyke.

Fig 2: Fanya Chini and Fanya Juu terrace design field layout.

The Focus Group Discussions (FGDs) elucidated information that was common across the three areas on some themes, however, some of the themes received contradicting points during the discussions. All participants across the FGDs agreed on the occurrence of soil erosion both on-farm and on the landscape, however, the severity of erosion was highly acknowledged in Kaporowo and Kapkitony citing weak fragile soils and poor soil structure for soil erosion occurrences. The thematic discussions were synthesized into four points.
 
Soil erosion awareness
 
Community awareness of soil erosion is evident and residents recognize the impact of erosion on various socio-economic aspects. Participants highlighted several indicators, such as declining soil fertility, erosion rills and threatening gullies that pose risks to crops andfodder production and livestock survival. To address the issue, the community ingeniously adopted and adapted various measures from different sources. Common practices include live fences, stone bands, cover-cropping and terraces with the latter (Fanya Juu and Fanya Chini) being hailed as the most effective and well-suited for their region. Implementing these terraces has visibly resulted in increased crop production and rapid vegetation recovery.
 
Drivers and barriers to adoption
 
Participants acknowledged that historically, the Pokot community solely depended on livestock for sustenance and income, with no tradition of crop cultivation. In the 1980s, the concept of soil erosion and its challenges dawned on them, posing a completely unfamiliar concept. This lack of awareness left the farmers oblivious to the dangers of soil erosion. The failure to adopt mitigation measures can also be attributed to low literacy levels and a rigid gender-based social structure. However, as literacy levels improved and with the intervention of extension services and non-governmental organizations, the community’s understanding of soil conservation has transformed. They have been enlightened about soil conservation practices and the advocacy for gender inclusivity has further reduced the gender barriers.
 
Benefits and challenges of Fanya Juu and Fanya Chini terraces
 
The participants highlighted numerous benefits spanning from on-farm like improved soil quality supporting crop growth during dry periods of growing season to landscape benefits like reduced soil deposition into rivers. Challenges included sediment build-up in the dykes hence compromising terrace efficiency, high labour demand and lack of information on where and how to appropriately place the terraces for optimal benefits.
 
Strategies for solving terrace adoption challenges
 
The community faces challenges in soil conservation due to the absence of suitable embankment reinforcement plants that can endure the harsh local climate. As a result, alternative erosion control methods need exploration. Educating farmers on soil conservation is key to improving awareness of the problem.
 
Indicators and impacts of soil degradations
 
Communities of drylands of Chepareria are aware of the soil degradations actively occurring at both landscape and farm levels. Loss of soil fertility, gully development, vegetation loss, silt build-up in water resources and on-farm soil loss are the most conspicuous indicators of soil degradation; with a significant rating of 61.0%, 78.0%, 67.8%, 33.9% and 64.4% respectively. Perceived impacts of degradation cut across the reduction of food production areas to the loss of animals, which accidentally fall into deep gullies. Fig 3, shows the impacts of degradation on the farmers.

Fig 3: Soil degradation impacts experienced by farmers.


 
Farm-level soil conservation practices adopted by farmers
 
The farmers use six main soil and water conservation practices at the farm level e.g. stone bands, enclosures, cover crops, terracing and ridges (Fig 4). The adoption of each technology varies with the villages and its suitability. Non-governmental soil conservation projects are the main propagators of the technologies; however, practices such as stone banding have been indigenously developed and inherited.

Fig 4: Farm-level soil conservation technologies adopted by farmers in Parak, Kapkitony and Kaporowo villages.


 
Main factors influencing agro-pastoral community soil conservation
 
Among the factors evaluated; land size owned, household size, source of income, gender and agents of soil conservation were found to be ranked as the leading contributors. The latter two were found to significantly influence how the community perceived and reacted toward soil degradation across the villages. Gender is a critical factor in adopting and maintaining soil conservation measures at the farm level. The women initiated live fencing in 30% of the households in the three villages (Table 1). They are also credited for the majority of stone bands constructed in many farms across the topo-sequence. Men initiated live fencing in 25% of the households but participated more in constructing the terrace, either in groups or individually. The study also revealed that men were more engaged in terrace reinforcement than women, participating in the reinforcement of terraces in 22.7% of the farms where terracing is practised. In comparison, women had only contributed to 9.1% of the reinforced farms at the time of the study. Agents of soil conservation, including non-governmental organizations and research projects, are the main propagators of soil conservation knowledge accounting for 73.3% of SWC practices adopted by the community, especially the newly adopted practices such as agroforestry and terracing. Other agents include; indigenous knowledge inheritance (15.56%) and lead farmers (8.9%). Community participatory approaches such as merry-go-round dubbed “Kemorokorenyo” (meaning let us reclaim our land) are some of the mushrooming agents of SWC facilitating the sharing of soil conservation knowledge.

Table 1: Gender influence on the installation of soil conservation strategies.


 
Terrace characteristics in chepareria ward
 
Fanya Juu and Fanya Chini are the only terrace designs practised in the area. The two designs are constructed in complementarity, with each playing a different role. Among the villages under study, Kaporowo village, located in the mid-slopes, was found to have the most substantial terrace volume per household with an average of 129.6±15.966 m3. Parak village recorded the second-largest volume of terraces per household and Kapikitony, with relatively flat land, had the least terrace volume; 105. 89 m3 (Table 2). Horizontal interval distances also varied as per the location; however, unexpectedly, terraces at high-sloped lands were constructed using long HI compared to other areas, (Table 2).

Table 2: Average length, slope and horizontal interval for terraces constructed at the farm level in the three Chepareria villages.


 
Influence of slope on terrace siltation
 
Slope significantly contribute to terrace filling with farms that had a slope ranging between 15 and 30%, contributing most to the highest filling of 60m3 to 122.7 m3 terrace volume in all the villages (Fig 5). Spearman’s rank-order correlation further affirmed a linear positive correlation between slope and terrace sediment filling [rs (37) = 0.628, p = 0.001].

Fig 5: Influence of slope on terrace sedimentation volume.


 
Terrace sediment build-up
 
Terrace dyke sediment volume differs significantly per village (Fig 6) as shown by Kruskal Wallis (KW) test conducted on sediment volume per village; H (2) =6.699, p=0.035. Parak, which sits on high sloped land experiences on average 79.69±32.04 m³ of sediment filling of their dykes during the long rainy season which is the highest among the three villages. Kaporowo and Kapikitony recorded 69.26±27.47 m³ and 47.26±13.72 m³ of dyke filling volume. Farmers who experience the complete filling of their terrace dykes, estimated filling time to range between 12 and 24 months, depending on the terrace’s spatial position relative to other terraces and slopes.
 
Terrace stabilization efforts
 
Reinforcement of terraces across the three villages is low. Only 31.8% of farmers with terraces had them reinforced. Terrace reinforcement does not significantly differ along with the topo-sequence, as indicated by the Chi-square Test of Independence, c2(2) = 1.564, p= 0.457. Parak and Kapkitony, had 13.6% reinforced terraces while Kaporowo recorded 4.6%. Locally available herbaceous plants, including; Aloe vera (Aloe spp) and Euphorbia spp were identified as the common terrace reinforcement materials used by farmers. Despite the low number of farmers who practised terrace reinforcement at the time of this study, they all identified it as an important terrace maintenance practice. However, farmers also suggested criteria on which reinforcement materials were to be underscored. They desired multiple benefits grass, trees, or crops that could withstand the local agroecological characteristics. The study found that farmers’ preferences were subjective as informed by climate, soil understanding and the need to optimize space. For instance, it was found that more than 60% of farmers in all the villages prefer sweet potatoes, while more than 50% of farmers would use fodder grasses as reinforcement materials (Table 3).

Table 3: Some of the terrace reinforcement materials suggested by farmers.


 
Benefits of terraces as a soil conservation measure
 
Terrace adoption has a wide spectrum of benefits, ranging from soil conservation at the farm level to restoration of degraded lands on landscape levels. Improvement of food and fodder productivity is ranked by 63.6% of farmers, 5% realized reduced soil erosion across different land slopes, 22.7% indicated increased vegetation regeneration and 31% cited reduced farm surface runoff. Improved water conservation at the farm level was also highlighted as a result of terracing by 27% of farmers. However, the realization of such benefits is subjective to individual farmers and past soil degradation challenges.
 
Community soil degradation awareness and conservation measures
 
For a community that is on a transition from pastoralism to crops-animal co-culture, it’s expected that their awareness of matters related to soil is shallow. However, in extreme scenarios, the awareness is intrinsically raised by the impacts such as poor crops and fodder production, formation and development of gullies and losses of animals attributed to a reduction in grazing area. The latter directly wreaks the basis of their livelihood and sources of income which elicit the crafting of indigenous solutions. For instance, stone banding and enclosures are indigenously developed practices for soil conservation. However, the nature of these solutions is appropriated by the community social-economic framework, accessibility and availability of the materials within the local context.
       
In addition, soil conservation agents, particularly research institutions and non-governmental organizations’ activities, have been at the forefront of creating awareness among dryland communities. Models like Farmer Research Networks (FRN) (Richardson et al., 2022) and merry-go-rounds are emerging as platforms for participatory community knowledge sharing. Direct participation of the community in co-creating soil conservation solutions has also been found critical in concerting efforts for conservation, as observed by Nigussie et al. (2018), they reported the beneficial impacts of centralizing conservation measures around the local communities making them the drivers of the process. Results of the participation approach have been reflected in the increasing numbers of farmers in Parak, Kapkitony and Kaporowo villages who have their farms terraced alongside other soil conservation practices.
       
The introduction of terraces has set forth numerous benefits in in the landscape, translating to improved food and fodder production which are at the heart of agro-pastoralist livelihood. These benefits support vegetative regrowth in the region, providing farmers with an opportunity to diversify their livestock. Such observations have been recorded worldwide, including Arnáez et al. (2015). The two indigenous terraces; (Fanya Juu and Fanya Chini) are therefore ideal for communities inhabiting drylands with landscape characteristics of West Pokot.
 
Gender influence on the community soil conservation
 
Gender disparity is a significant challenge in pastoral communities and significantly affects farm-level soil conservation, as shown by gender contributions toward the adoption of different conservation measures. Women tend to participate more in installing stone bands and live fences than men. The two are perceived as low labour intensive by men, although they require more time to construct indicating that women in the community spent more time on farm activities. Men on the other hand are involved in highly labor-intensive practices like terrace construction. These alone manifests disproportionality of gender participation towards conservation and might be the key reason for the low adoption of some practices. However, with increased awareness of soil degradation and efforts by conservation stakeholders, the gap is rapidly narrowing (Willy and Holm-Müller, 2013).
 
Influence of slope on terrace sediment Build-up
 
Terrace filling is severe and happens within 12-24 months after the construction of the terrace, particularly on high-sloped lands compared to moderately and relatively flat-lands, There are several explanatory aspects as the terrace design  might not be suitable for the slopes of more than 20%, as suggested by (Masereka, 1983; Mati, 2010). At the high hilly slopes, soils are shallow and fragile with high sand contents and this makes them easy to erode and the embarkment formed is very weak to withstand the high amounts of erosive surface run-off experienced at such slopes.
 
Reinforcement of terrace embarkments
 
Farmers practicing Fanya Juu terraces were found to have adopted locally available herbaceous plants such as Aloe spp species for terrace reinforcement. Terrace embankment reinforcement is key in reducing sedimentation of the dykes and contributes to the terrace’s general efficiency (Gebreyess and Amare, 2019). However, the material used for reinforcement depends on their availability and users’ agro-ecological zone e.g. drought-resistant grass has been recommended for upper Tana, Kenya (Muriuki and Macharia, 2011), while vetiver grass (Vertiveriazizanoides) has been recommended for the upper Blue Nile, Ethiopia (Sultan et al., 2018). Contrary to findings made in this study, reinforcement materials should possess other benefits besides stabilizing terrace embankments (Ahmed, 2018), such as fodder or crops. Adopting locally available herbaceous plants like Aloe spp for reinforcement reflects farmers’ desperation to access information and lack of appropriate materials for that purpose.
Soil erosion is the main land degradation process experienced in agro-pastoral drylands aggravated by land characteristics (high slope), soil characteristics (young and fragile) and anthropogenic activities. The advent of participatory community farm-level soil management practices raises awareness of land degradation and improves how conservation practices are adopted. More effective conservation practices, like  terraces, have been adopted through the approach. Despite terraces proving a potential solution to farm-level soil degradation, sediment build-up in the dykes has compromised their efficiency and increased maintenance costs. The two factors introduce trade-offs that might hinder the adoption of the structures by income-constrained agro-pastoral communities. Furthermore, inadequate information on the effectiveness of cover crops as reinforcement materials for terraces is a challenge that has extensively hindered their use and thus a study on it is warranted.
The authors are indebted to the McKnight Foundation, which provided financial support for implementing this study through the University of Eldoret.
All authors declare that they have no conflict of interest.

  1. Adonia, K. and Kakurungu, B. (2014). Assessment of the effects of changing land use from pastoralism to crop farming on Lake Nakivale wetland system in Isingiro District, Uganda. Journal of African Studies and Development. 6(4): 56-66. doi:10.5897/jasd2013.0249.

  2. Ahmed, J.M. (2018). Analysis gender role and factors affecting soil and water conservation adoption in Kersa Districts of Eastern Hararghe Zone, Ethiopia: The case of fanya juu, soil and stone bund measure. International Journal of Agricultural Science, Research Technology in Extension Education Systems. 8(1): 49-58. 

  3. Arnáez, J., Lana-Renault, N., Lasanta, T., Ruiz-Flaño, P. and Castroviejo, J. (2015). Effects of farming terraces on hydrological and geomorphological processes. A review. Catena. 128: 122-134. doi:10.1016/j.catena.2015.01.021.

  4. Camera, C., Djuma, H., Bruggeman, A., Zoumides, C., Eliades, M., Charalambous, K. and Faka, M. (2018). Quantifying the effectiveness of mountain terraces on soil erosion protection with sediment traps and dry-stone wall laser scans. CATENA. 171: 251-264. doi:10.1016/j.catena. 2018.07.017.

  5. Etikan, I., Musa, S.A. and Alkassim, R.S. (2016). Comparison of convenience sampling and purposive sampling. American Journal of Theoretical Applied Statistics. 5(1): 1-4. doi: 10.11648/j.ajtas.20160501.11.

  6. FAO. (2017). Voluntary guidelines for sustainable soil management. Retrieved from Rome: 

  7. Gachene, C.K.K., Nyawade, S.O. and Karanja, N.N. (2019). Soil and water conservation: An overview. Zero Hunger. doi:10.1007/978-3-319-69626-3_91-1.

  8. Gaur, M.K. and Squires, V.R. (2018). Drylands Under a Climate Change Regime: Implications for the Land and the Pastoral People they Support. In: Climate Variability Impacts on Land Use and Livelihoods in Drylands. [Gaur, M.K. and  Squires, V.R. (Eds.)], Springer, Cham. (pp. 319-334).

  9. Gebreyess, B.F. and Amare, A. (2019). Water Harvesting Technologies in Semi-Arid and Arid Areas. Journal of Degraded Mining Lands Management. 7(1): 1921. doi:10.15243/jdmlm.2019.071.1921.

  10. LADA. (2016). Land Degradation Assessment (LADA) in Kenya: Based on a Study of Land Degradation Assessment (LADA) with Remote Sensing and GIS, for Sustainable Land Management (SLM) in Kenya. Retrieved from Nairobi, Kenya.

  11. Maphill. (2011). Chepareria, West Pokot County, Kenya. Retrieved from http://www.maphill.com/kenya/rift-valley/west- pokot/chepareria/maps/gray-map/

  12. Masereka, E.M. (1983). A Study of Design, Construction and Bank Stabilization of Fanya Juu Terraces at Kabete, Kenya. (Post-Graduate Diploma), University of Nairobi, Nairobi, Kenya. 

  13. Mati, B.M. (2010). Agricultural Water Management Delivers Returns on Investment in Eastern and Southern Africa: A Regional synthesis. In Agricultural Water Management Interventions Delivers Returns on Investment in Africa - A Compendium of 18 Case Studies From Six Countries in Eastern and Southern Africa. [Mati, B. (Ed.)], Saarbrücken, Germany: VDM Verlag. (pp. 1-29). 

  14. Mudalagiriyappa, T., Vasanthi, B.G., Devaraja, K., Savitha, M.S., Puneetha, K.M., Jayashree, H.T. andRavindra Chary, G. (2019). Soil and Water Conservation Technologies in rainfed Agriculture for Alfisols of Southern Karnataka. Retrieved from Karnataka, India: http://krishi.icar.gov.in/ jspui/handle/123456789/32352.

  15. Muriuki, J.P. and Macharia, P.N. (2011). Inventory and Analysis of Existing Soil and Water Conservation Practices in the Upper Tana, Kenya. Retrieved from Wagenigen, Netherlands.

  16. Nguru, P.M. and Rono, D.K. (2013). Combating Desertification in Kenya. InCombating Desertification in Asia, Africa and the Middle East:  [Heshmati, G. and Squires, V. (Eds.)] Springer, Dordrecht. (pp.139-151).

  17. Nigussie, Z., Tsunekawa, A., Haregeweyn, N., Adgo, E., Cochrane, L., Floquet, A. and Abele, S. (2018). Applying Ostrom’s Institutional Analysis and Development Framework to Soil and Water Conservation Activities in North-Western Ethiopia. Land Use Policy. 71: 1-10. doi:10.1016/j.land usepol. 2017.11.039.

  18. Oteng’i, S.B.B., Stigter, C.J. and Mungai, D.N. (2000). Wind Protection in a Hedged Agroforestry System in Semiarid Kenya. Agroforestry Systems. 50(2): 137-156. doi:10.1023/ A:1006487007101

  19. Pennock, D., McKenzie, N. and Montanarella, L. (2015). Status of the World’s Soil Resources. Retrieved from Rome, Italy. 

  20. Richardson, M., Coe, R., Descheemaeker, K., Haussmann, B., Wellard, K., Moore, M. and Nelson, R. (2022). Farmer research networks in principle and practice. International Journal of Agricultural Sustainability. 20(3): 247-264. doi:10.1080/14735903.2021.1930954.

  21. Saiz, G., Wandera, F.M., Pelster, D.E., Ngetich, W., Okalebo, J.R., Rufino, M.C. and Butterbach-Bahl, K. (2016). Long-term assessment of soil and water conservation measures (Fanya-juu terraces) on soil organic matter in South Eastern Kenya. Geoderma. 274: 1-9. doi:10.1016/ j.geoderma.2016.03.022.

  22. Scherr, S.J. (2019). The Future Food Security and Economic Consequences of Soil Degradation in the Developing World. In Response to Land Degradation. CRC Press. (pp. 155-170).

  23. Sheng, T.C. (2002). Bench terrace design made simple. Retrieved from Fort Collins, CO 80523, USA.

  24. Shiferaw, B. (2002). Poverty and natural resource management in the semi-arid tropics: revisiting challenges and conceptual issues. Working Paper Series no. 14. International Crops Research Institute for the Semi-Arid Tropics. Patancheru, Andhra Pradesh, India. Retrieved from http://oar.icrisat.org/3780/

  25. Sidle, R.C., Jarihani, B., Kaka, S.I., Koci, J. and Al-Shaibani, A. (2019). Hydrogeomorphic Processes Affecting Dryland Gully Erosion: Implications for Modelling. Progress in Physical Geography: Earth Environment. 43(1): 46-64. doi: 10.1177/0309133318819403.

  26. Sultan, D., Tsunekawa, A., Haregeweyn, N., Adgo, E., Tsubo, M., Meshesha, D. T. and Ebabu, K. (2018). Efficiency of soil and water conservation practices in different agro- ecological environments in the upper blue nile basin of Ethiopia. Journal of Arid Land. 10(2): 249-263. doi:10.1 007/s40333-018-0097-8.

  27. Tenge, A.J., Sterk, G. and Okoba, B.O. (2011). Farmers’ preferences and physical effectiveness of soil and water conservation measures in the East African Highlands. Journal of Social Sciences. 2: 84-100. 

  28. Tindwa, H.J., Semu, E., Shelukindo, H.B. and Singh, B.R. (2019). Soil Degradation with Reference to Nutrient Mining and Soil Fertility Decline in Sub-Saharan Africa. In: Soil Degradation and Restoration in Africa. [Lal, R. and Stewart, B.A. (Eds.)], Boca Raton: CRC Press.  (pp. 24-38).

  29. Touber, L. (1991). Landforms and Soils of West Pokot District, Kenya: A Site Evaluation for Rangeland Use. Retrieved from Wageningen: https://edepot.wur.nl/360903.

  30. Willy, D.K. and Holm-Müller, K. (2013). Social influence and collective action effects on farm level soil conservation effort in Rural Kenya. Ecological Economics. 90: 94-103. doi:10.1016/j.ecolecon.2013.03.008.

  31. Zhu, Y.G. (2020). Exploring the complex belowground world: Soil Ecology-The Soil Food Webs and Their Ecological Functions. In: Springer.

  32. Zougmore, R., Jalloh, A. and Tioro, A. (2014). Climate-smart soil water and nutrient management options in semiarid west africa: A review of evidence and analysis of stone bunds and zaï techniques. Agriculture Food Security. 3(1): 16. doi: 10.1186/2048-7010-3-16.

Editorial Board

View all (0)