Farmers’ soil knowledge, fertility management logic and its linkage with scientifically analyzed soil properties in southern Ethiopia
© The Author(s) 2017
Received: 12 July 2017
Accepted: 8 September 2017
Published: 27 September 2017
Farmers’ locally have acquired knowledge from generations of experience and experimentation that fit local conditions. Yet, the scientific approach less used farmers’ soil knowledge (FSK) and site-specific soil information. The objectives of this study were to investigate FSK and rationality; to demonstrate how FSK relates to scientifically analyzed soil properties; and to explore the implemented soil management practices and crop performances in selected districts of Wolaita zone, southern Ethiopia. A total of 789 farmers were included, and their fields were evaluated. Data on farmer’s soil nomenclature, soil physicochemical property, soil fertility management practices and crop yield performance were recorded and analyzed.
Farmers describe and classify their soils using holistic approach. Soil nomenclature and classification indicators are relatively homogeneous over large area. Accordingly, seven soil types common over large area were identified. Mostly, soil types perceived fertile by farmers (e.g., Arrada bita) were found better in measured physicochemical properties than infertile soil types (e.g., Lada bita, Zo’o bita). Simple regression analysis revealed a declining trends of soil properties with a decrease in fertility of farmers soil types such as soil bulk density (r 2 = 0.78), pH (r 2 = 0.53), available phosphorous (r 2 = 0.83), total exchangeable bases (r 2 = 0.71), copper (r 2 = 0.64) and zinc (r 2 = 0.69). Farmers are rational to allocate the scarce fertilizers. They apply more chemical fertilizer when soil type was getting poor in soil fertility (r 2 = 0.61), whereas it was opposite for manure (r 2 = 0.85). Furthermore, crop response and farmers’ soil type also demonstrated an observable relationship where yield was declining with a decrease in fertility level of farmers’ soil types.
Farmers understand within farm soil variability and exploit soil fertility differences of their field. This is supported with noticeable relationship with scientifically analyzed soil properties, fertility management strategy and crop responses. It suggests that FSK is relevant for site-specific soil management. Yet, FSK is deficient to identify yield-limiting nutrients, implying it has to be complemented with scientific soil knowledge. Additionally, further investigation to systematically link both approaches is also suggested.
KeywordsFarmer’ soil nomenclature Physicochemical property Soil variability Yield
Soil fertility management is an agenda of farmers and scientists as soil properties are characterized by spatial and temporal variability to the extent of short distances [1–3]. This heterogeneity can be caused by inherent properties and external factors such as farmers’ differences in soil management [4–6] and land use . Without systematic consideration of different soil types, soil nutrient management interventions have proved to be risky interventions and have failed to constitute economically valid options . Soil interventions in most African countries, in general, have been dominated by the scientific thinking; soil management aspects are dominated by discussions of inorganic fertilizers  and blanket recommendations . Yet, the scientific approach less used farmers’ soil knowledge (FSK) and site-specific soil information [9, 10]; subsequently, this leads to the poor adoption of recommendations such as fertilizer use. On contrary, farmers have been accused of ignorance and resistance to adopting recommended productivity-enhancing measures that go beyond traditional subsistence farming logic (MINECOFIN, 2007 cited by ). The rationale of farmers is related to the compatibility of the recommended technology with the existing biophysical environment such as soil, topography, resource and climate.
Interventions that lack systematic consideration of soil fertility variability have been leading to differences in: opinions between actors  and problem formulation and solutions sought , and hence resulted in poor adoption . For instance, the absence of local participation and non-recognition of indigenous conservation‐oriented land use practices in Ethiopia has been reported among reasons for not achieving the desired objectives of soil conservation efforts (Yeraswork, 1998 cited by ). In addition, the poor adoption of fertilizer due to recommendation of the same rate of fertilizer on a blanket basis for entire ‘Agro-Ecological Zones’ (AEZs) but having different soil types was also reported . This highlights the importance of integrating FSK to support site-specific soil management decisions.
Farmers locally have acquired knowledge from generations of experience and experimentation that fit local conditions since they have been interacting with their soils for long time [12–15]. Their knowledge can offer many insights to formulate sustainable management of soils [13, 16, 17]. These days, the value of FSK has received considerable attention by many scientists [7, 12, 16, 17]. Its integration with scientific approach is socially acceptable, ecologically sustainable and economically viable [7, 17]; and also it is believed to overcome the shortcomings of scientific intervention while performing under wider ranges [3, 17]. The FSK is also referred as local, traditional, folk, native or indigenous soil knowledge . The acknowledgement of FSK worldwide has led to a new field of science which is called Ethnopedology [7, 17]. Ethnopedology as a field of study aims to document and understand local approaches to soil perception, classification, appraisal, use and management . Thus, in order to facilitate communication between researchers and farmers, and potentially improve the likelihood of success of soil fertility management interventions, incorporation of site-specific soil information and knowledge is needed for getting huge benefits.
Findings from different parts of the world such as Ethiopia [8, 12, 19, 20], Kenya , Burkina Faso , Rwanda , Mexico , Nepal  and Costa Rica  highlight that farmers locally have a broad knowledge to describe and classify soils that are relevant for development of soil-specific technologies. The farmers’ rationality while classification combines cognitive soil knowledge (e.g., color, texture, soil types, soil suitability) and soil-related practices including land use, crop suitability and soil fertility management [e.g., 7, 15]. In view of that, different scholars suggested the need to incorporate farmers’ soil knowledge in the development of holistic soil management approaches [7, 8, 12, 15, 22].
In the complex physiographic conditions like Wolaita , tailoring soil fertility management recommendations to specific soil types has been a crucial problem. Few studies in the area reported that farmers have a broader knowledge of their soils [8, 23]. However, their knowledge and site-specific soil information are much less studied so as to support the scientific information and objectively interpret the farmers’ logic in soil fertility management. Consequently, it affects communication between extension practitioners and farmers to assure soil-specific interventions. It is supposed that the introduction of any soil-related intervention in harmony with the FSK system is likely to increase its relevance and adoption. Thus, the objectives of this study were to identify farmers’ soil nomenclature and rationality; to demonstrate how FSK relates to scientifically analyzed soil properties; and to explore the implemented soil management practices and crop performances in selected districts of Wolaita zone, southern Ethiopia.
Description of the study area
The elevation of the study districts ranges between 1473 and 2873 meters above sea level (m.a.s.l). As per the traditional agro-ecological zone classification of Ethiopia, the area is predominantly characterized by mid-highland agro-ecology. Besides, small portion of highlands in Damot Gale and Sodo Zuria districts and very small pocket lowland areas in Damot Sore districts is identified. Spatially, out of the total study area, about 0.003, 96 and 3.7% are found under lowland, mid-highland and highland agro-ecologies, respectively.
Eutric Nitisols associated with Humic Nitisols are the most prevalent soils in Wolaita Zone . These are dark reddish brown soils with deep profiles. Agriculture in the study area is predominantly smallholder mixed subsistence farming and is dominantly rain-fed. Continuous cultivation without any fallow periods coupled with complete removal of crop residues is a common practice on cultivated fields. Farmers use diammonium phosphate (DAP), urea and farmyard manure (FYM) as sources of fertilizers.
The major crops grown in the study area include tef (Eragrostis tef (Zucc.) Trotter), maize (Zea mays L.), bread wheat (Triticum aestivum L.), haricot bean (Phaseolus vulgaris L.), field pea (Pisum sativum L.), potato (Solanum tuberosum), sweet potato (Ipomea batatas (L) Lam.), taro (Colocasia esculenta (L.) shoot.), enset (Ensete ventricosum (Welw.) chesman) and coffee (Coffea arabica).The vegetation is dominated by eucalyptus trees (Camaldulensis spp.). Remnants of indigenous tree species such as croton (Croton macrostachyus Hochst. ex Rich.), cordia (Cordiaa fricanaLam.), Erythrina spp, podocarpus (Podocarpus falcatus) and Juniperus (Juniperus procera) are also present.
Soil sampling procedure and laboratory analysis
Soil sampling procedure
At the beginning, a preliminary interpretation of the topographic map (scale 1:50,000) obtained from Ethiopian Mapping Authority (EMA) was utilized. Geographical information system (GIS) software (Arc Map version 10) was employed to randomly assign sample collection points. A total of 789 randomly selected agricultural fields (i.e., 243 on Damot Gale, 216 on Damot Sore and 330 on Sodo Zuria) covering all representative land use types were generated for sample and data collection. The samples were randomly distributed at an average distance of 512 meters. During survey work, the pre-defined sample locations were visited in the field and the location was recorded using the GPS (geographical positioning system) receiver (model Garmin GPSMAP 60Cx).
Apart from soil sample collection, soil color, local soil name, land use type, crop type grown, fertilizer use (types and rates) and farmers-estimated crop yield from each field were recorded. Farmers were asked the name of soil color, and it was also described using Munsell soil color chart . Farmers’ owning the fields were interviewed about local soil name and fertilizer usage (type and rate) for the existing crops sown at the time of sampling. This helped to explore farmers’ rationality to implement soil management practices.
Soil sampling, sample preparation and soil analysis
Disturbed and undisturbed soil samples were taken from the field using augur and core sampler, respectively. In order to form a composite sample, 10–15 subsamples from each field were collected. The sampling depth was 20 cm for annual crops such as tef, haricot bean, maize, etc., while it extends up to 50 cm for perennial crops such as enset and coffee growing fields. From the composited sample, one kilogram (kg) of soil was taken with a labeled soil sample bag.
Sample preparation (drying, grinding and sieving) was conducted at the National Soil Testing Center (NSTC), Addis Ababa, Ethiopia. Particle size distribution (PSD) was analyzed by laser diffraction method using laser scattering particle size distribution analyzer (Horiba-Partica LA-950V2) . Soil bulk density was determined using the core method . Soil pH (1:2 soil/water suspension) was measured with glass electrode (model CP-501) . Available phosphorous (P), available sulfur (S), exchangeable basic cations [calcium (Ca), magnesium (Mg) and potassium (K)] and extractable micronutrients [iron (Fe), manganese (Mn), boron (B), copper (Cu) and zinc (Zn)] were determined using Mehlich-III multi-nutrient extraction method . The concentration of elements in the supernatant was measured using inductively coupled plasma (ICP) spectrometer.
Mid-infrared diffused reflectance (MIR) spectral analysis was used to determine the amount of soil organic carbon (OC), total nitrogen (N) and cation exchange capacity (CEC). The available soil Mn content was determined using manganese activity index (MnAI) as described by Karltun et al. . Particle size distribution, pH, OC, TN and CEC were analyzed at the National Soil Testing Center (NSTC), Addis Ababa, Ethiopia, whereas Ca, Mg, K, B, Cu, Fe, Mn and Zn were analyzed in Altic B.V., Dronten, The Netherlands.
Descriptive statistics was employed for data analysis. In addition, F tests were also computed. Data analysis was carried out using Microsoft excel and statistical package for social sciences (SPSS) software version 20.
Results and discussion
Farmer’s soil type
Farmers’ soil types and perceived soil characteristics in studied districts of Wolaita Zone, southern Ethiopia.
Source: Survey result (2013)
Local soil typesa
Brown (42%) > reddish brown (20%) > dark reddish brown (17%) > gray (7%), other brownish
Easy to moderate
GL to HL
Brown = dark reddish brown (30% each), reddish brown (24%), yellowish brown (4%)
Highly permeable soil
Dark reddish brown (42%) > reddish brown (32%) > brown (20%)
Low > medium
GL to HL
Brown = dark reddish brown (34% each), reddish brown (11%), gray (8%)
Difficult to work (sticky when wet and strong when dry)
GL to HL
Dark reddish brown (45%) > reddish brown (36%) > brown (11%)
Low > medium
Gray (55%), grayish brown (17%), brown (15%), other gray to brownish
Difficult to work (when wet)
Low (water-retaining soil)
FL to GL
Brown (44%) > reddish brown (19%), grayish brown = gray (11%), dark gray = dark reddish brown (7.4%)
Difficult to work (when dry and wet)
Soil on stony and eroded land
Brown > pinkish brown = very dark gray
A field having both infertile and permeable soils
Soil on newly fallowed land
Infertile and permeable soil
GL to HL
Infertile soil on sloppy area
Among soil types, Arrada bita predominates in proportion followed by Lada bita > Gobo bita > Talla bita > Zo’o bita (Fig. 3). Similarly, the study made by Data  indicated that most adult male farmers in Wolaita can name up to eight different soil types, depending on whether they reside in a highland, midland or lowland area. In addition, the study by Pound and Jonfa  conducted in the neighboring district (Kindo Koyisha), Wolaita zone, indicated similar soil types such as Kereta, Gobo, Talla, and Chere bita. Generally, the occurrence of soil types varied across landscape positions. Chere bita was common on flat slope positions. Arrada, Gobo and Kereta bita were dominantly found in gentle slopes. Lada, Talla and Zo’o bita, which are prominently regarded as low fertile soils, were located from gentle to hilly slope lands. According to Data and Scoones , the greater diversity of soil types identified by farmers in Wolaita derives from a combination of several factors such as landscape positions, variation in soil property (e.g., texture and color most notably) and their effects on crop growth.
Soil color was commonly used indicator among farmers to classify soil. The dominant soil colors were brown, dark reddish brown and reddish brown colors. Farmers locally regarded reddish brown soil as poor in fertility, and darker soils as good fertile soils. They mostly perceived that soils rich in soil organic matter, i.e., fertile soils, have darker color. The uses of color as a descriptor of soils have been reported by different scholars [14, 17, 19, 21, 23], and the authors stated that farmers’ perceived and preferred black soils than red soils.
Farmer’s soil fertility knowledge is a function of many variables that are being considered simultaneously, and most of them are interrelated. They locally regarded soil fertility from low to high levels. Summarizing farmers’ beliefs, 58% of the sampled fields were found within dominantly low-fertility category. In terms of workability, the soils vary from easy to difficult to work categories (Table 1). The difference might be attributed to the amount of clay having sticky property and soil moisture content. Hence, soils thought to have high clay content (e.g., Chere, Talla and Kereta bita) become sticky upon wetting, and difficult to plow during dry season cultivation. The rate of water infiltration is critical in the study area as it affects crop growth, crop choice, cropping intensity and management. For this reason, farmers are permanently assessing the degree and distribution of moisture in the soil layers throughout the agricultural cycle . The capacity of soils to permit water movement (permeability) and retain within root zone depends on soil types. According to farmers ranking, soil permeability varies between low (water-retaining soil) and high (percolate and dry fast). For instance, the limitation in Gobo bita is the excessive permeability which makes it more sensitive to water shortage. On the other hand, Chere bita has low permeability, difficult to work (when wet and dry), and used to cultivate crops that adapt to the condition once in a year.
The knowledge of farmers in judging their soils using holistic views, such as soil color, permeability, water holding capacity, workability and soil fertility, has been reported in Ethiopia [19, 20], Burkina Faso , Northern Laos , western Kenya , Nepal , Mexico  and Rwanda .
Farmers’ soil types and their properties
Mean values of the physicochemical properties of locally classified soils in studied districts of Wolaita zone, southern Ethiopia
Farmers soil types
Silty clay loam
Bulk density (g cm−3)
P (mg kg−1)
Ca (Cmolc kg−1)
K (Cmolc kg−1)
Mg (Cmolc kg−1)
S (mg kg−1)
B (mg kg−1)
Cu (mg kg−1)
Fe (mg kg−1)
Mn (mg kg−1)
MnAI (mg kg−1)
Zn (mg kg−1)
TEB (Cmolc kg−1)
CEC (Cmolc kg−1)
The mean soil pH (H2O) varied from 5.6 (Zo’o bita) to 6.4 (Arrada bita). Variations in soil management practices among soil types might contribute to the observed pH values. Relatively, the higher organic fertilizer and home-left residue application on Arrada bita ought to contribute to the higher pH compared to Zo’o bita (Table 2) which is mostly subjected to complete crop residue removal and inorganic fertilizer use. Soil pH showed a declining trend from Arrada bita toward infertile soil types (Lada, Gobo, Zo’o bita). This trend was explained by polynomial regression (r 2 = 0.54). Similarly, Saito et al.  reported that soils farmers described as fertile had the higher pH than the other soils. However, the mean pH value of soil types was rated under moderately acidic category (5.6–6.5) .
The soil organic carbon (OC) content was between 1.6% (Talla bita) and 2.2% (Arrada, Gobo and Zo’o bita). Regardless of the values, the soil types were grouped under very low (<2%) and low (2–4%) . This could indicate how the soil types in the study area have been exposed to intensive cultivations. Total nitrogen (TN) varies from 0.1 to 0.2% (Table 2). Generally, soils perceived to be fertile (e.g., Arrada bita) and infertile (e.g., Lada bita) by farmers recorded the highest and least values, respectively. Likewise, soils types which are difficult to plow and high-water-retaining soil (e.g., Talla, Gobo and Chere bita) had the least TN value which could be ascribed to high uptake and susceptibility of N to different losses. Asongwe et al.  stated that farm-specific practices might have influenced mineralization where areas characterized by rapid mineralization would result in high nitrogen losses. The soil TN was under low (0.1–0.2%) status . Total soil N is normally considered a rather poor indicator of plant-available N. However, it is believed that TN becomes a good proxy for soil N mineralization capacity .
Available P concentration of soil types ranged between 3 and 21 mg kg−1 (Table 2). The soil type having higher soil pH and OC (i.e., Arrada bita) recorded the highest value compared to all other soils that had between 3 and 8 mg kg−1 (Table 2). This relationship was significant and best described by exponential regression (r 2 = 0.83). However, irrespective of numerical differences, all locally identified soils showed P concentration below the critical level (30 mg kg−1) suggested for Ethiopian soils . The lower P content might be ascribed to the combined effects of intensive cultivation, lower P and organic fertilizer application, and lower pH values. Lower P content on cultivated soils was also reported in the literature [4, 5, 37–39].
The result regarding exchangeable bases revealed differences among soil types (Table 2). The cation exchange site of soil types was mainly occupied by Ca > Mg > K. The concentration of bases in the exchange complex ranged from 9 to 15 Cmolc kg−1 (Table 2). The highest and least values were recorded from Arrada bita and Lada bita, respectively. Total exchangeable bases of soil types seem decreased from Arrada bita to Lada bita. This relationship between soil types and exchangeable bases was significant and best described by logarithmic regression (r 2 = 0.71). Mostly, Arrada bita is located close to homestead areas where it received ash, household refuse and manure. These practices could result in the higher base status in Arrada bita instead of Lada bita where continuous uptake without nutrient application and leaching is more [33, 37]. On the other hand, available S status of soil types was found under narrow ranges (10–13.5 mg kg−1) which is below the critical levels used for Ethiopian soils (20 mg kg−1) . The lower S in all soil types could be linked to lower soil OC, crop uptake and non-use of S fertilizers. In Ethiopia, different researchers also reported the lower available S content in cultivated soils [4, 5, 35, 40].
There existed variability of micronutrient contents of soil types (Table 2). Boron and Cu concentrations varied from 0.4 to 0.7 mg kg−1 in which the higher content was recorded from fertile soil (e.g., Arrada bita), while the least on infertile soil (e.g., Lada bita). In the meantime, the relationship between Cu and soil types was significantly predicted by a positive linear regression (r 2 = 0.64). The coefficient of regression for B with soil types was not significant but explained by logarithmic regression (r 2 = 0.33). Nonetheless, irrespective of the soil types, their status was found below critical levels suggested for Ethiopian soils, i.e., 0.8 mg kg−1 for B and 0.9 mg kg−1 for Cu . On the other hand, Fe, Mn and Zn in all soil types were found above the critical level of Fe (80 mg kg−1), Mn (25 mg kg−1) and Zn (1.5 mg kg−1) .
The CEC of the soil varied from 18 to 23 Cmolc kg−1. The higher value was obtained from Arrada bita, and the least was on water-retaining soil (Chere bita) and infertile soil (e.g., Lada bita). According to Landon , soil types fall under medium CEC category (15–25 Cmolc kg−1), implying that they have moderate potential to hold nutrients against leaching losses. The finding reported by Fanuel  in the study area indicated that source of charges in the CEC is pH dependent. It is thus imperative to manage and raise the soil pH in order to increase their potential . This is witnessed on Arrada bita which received relatively better soil management and higher pH (6.4) and in turn owes higher CEC than the other soil types. Correspondingly, higher CEC values on soils identified as fertile by farmers’ compared to soils perceived as non-fertile soil were also reported .
In general, the farmers’ logic demonstrated an association with scientific knowledge on most of measured soil physical and chemical properties when looking the trends. This suggests farmers’ ability to differentiate soil fertility variability. This is consistent with [7, 12, 17, 21] who observed that FSK has a good agreement with scientifically measured soil properties. Despite farmers’ knowledge to understand soil variability of their field and exploit any soil fertility differences of their field, ratings using chemical properties identified nutrient limitation. This is demonstrating that scientific disciplines such as soil chemistry and soil biology are important tools to upgrade the FSK system . Hence, complementing FSK with scientific approaches (chemical soil properties) in the study area is important to better recognize the biophysical environment, interpret farmers’ rationality, establish robust relationship between the approaches, communicate with farmers in a friendly way and potentially improve the likelihood of success of soil fertility management interventions.
Farmers’ soil fertility management strategies
Farmers use diammonium phosphate (DAP), urea and farmyard manure (FYM) as sources of fertilizers. The crops on which inputs are applied in the area include Tef, maize, wheat, haricot bean, potato, sweet potato, taro, enset and coffee. Farmers preferably apply FYM or home-left wastes to enset, coffee and root and tubers crops, while mineral fertilizers are used for tef, maize, wheat, haricot bean and potato. Fertilizer-allocation practices by farmers in Wolaita area specifically to the study area are also briefly indicated in .
Soil fertility management on locally classified soils in studied districts of Wolaita zone, southern Ethiopia
Farmers soil types
DAP (kg ha−1)
Urea (kg ha−1)
FYM (t ha−1)
Farmers in the study area mostly grow perennial and vegetable crops on fertile soils using FYM. When asked reasons for the higher organic fertilizer on Arrada bita, farmers indicate that the better crop response, proximity of garden fields to home, the limited availability of home-left refuses and FYM, and type of crops grown around home were factors making them allocate more organic residues to Arrada bita. For farmers, organic matter is clearly the main factor to sustain soil fertility, and soils with organic matter in the topsoil are potentially of good agricultural quality . Conversely, farmers use high rates of inorganic fertilizers for annual grain crops that are grown on distant fields and less fertile soils. This finding agrees with previous studies in Wolaita [33, 41, 42]. Furthermore, the experience of Rwandan farmers to apply FYM on best soils than on other soil types by realizing best crop responses was reported by Rushemuka et al. .
Farmers soil types and their productivity
Average crop productivity on locally classified soils in studied districts of Wolaita zone, southern Ethiopia
Farmers soil types
Maize (W/O) (t ha−1)
Maize (with) (t ha−1)
Haricot bean (W/O) (t ha−1)
Haricot bean (with) (t ha−1)
Tef (W/O) (t ha−1)
Tef (with) (t ha−1)
Sweet potato (W/O) (t ha−1)
Sweet potato (with) (t ha−1)
The presence of organic matter in the soil is considered critical for crop performance. A higher yield from fertile soil (e.g., Arrada bita) compared to infertile soil types (e.g., Lada bita, Zo’o bita) could be attributed to relatively higher FYM application and soil properties. In agreement, Rushemuka et al.  reported that the favorable response of good soils to FYM application was attributed to supply of soil nutrients. Additionally, the positive impacts of soil organic matter in storing and supplying of nutrients were also described [43–45]. Furthermore, a significantly higher mean yield of rice from black soils (i.e., perceived as fertile by farmers) compared to other soil types was stated . On the other hand, remarkably low yield in Chere bita could be related to high-water-retaining characteristics of the soil.
Yet, farmers in the study area are getting very low yield compared to yield reported from research station in Ethiopia  such as maize (12 t ha−1), teff (3.4 t ha−1), haricot bean (4 t ha−1) and potato (6.5 t ha−1). The yield gap is emanated from very poor crop residue maintenance, inadequate compensation of plant nutrients and continuous cropping [4, 5]. Consequently, it resulted in the presence of multi-nutrient deficiencies including N, P, S, B and Cu. Hence, proper practices leading to soil fertility enhancement are mandatory to generate better yields.
The objectives of this study were to identify farmers’ soil nomenclature and their rationality; to demonstrate how farmers’ soil knowledge relates to scientifically analyzed soil properties; and to explore the implemented soil-specific fertility management practices. Results from this study have shown that farmers’ soil nomenclature is broad and often based more on observation and crop responses. Most of the soil types identified by farmers’ are common over large area speaking the same language, implying that a venue for developing crop-–soil-specific technology. Moreover, farmers’ soil types have also shown an association with scientific knowledge, signifying that their knowledge is relevant for site-specific soil management.
Fertilizer use strategy of farmers’ differs with soil types and crops. They prefer to apply organic fertilizers on fertile soils (Arrada bita) because an important food security crops such as enset and root and tubers are growing; proximity of the soil type to the source (i.e., home) and better crop yield. On poor fertility but input-responsive soil types (e.g., Lada and Zo’o bita) where crops such as maize, beans and other annual crops are growing, farmers apply chemical fertilizers. Farmers’ rationality is also demonstrated on crop responses. They noted better crop yield from fertile soils than from the others. When asked for reasons, farmers indicate that soils managed with organic materials are conducive for crops than those managed with chemical fertilizers. It was concluded that farmers’ soil knowledge is rational and specifically addresses farm soil variability occurring over short distances. Nevertheless, they are not capable of identifying yield-limiting nutrients. Hence, supplementing their knowledge with scientific soil information is recognized. Furthermore, systematic investigation is suggested to develop rational communication about soil and improve the success of soil fertility management interventions.
FL collected, analyzed and interpreted the data. KK and TM helped to draft the manuscript. All authors read and approved the final manuscript.
We would like to thank Ministry of Education (MOE) for the scholarship and the Ethiopian Soil Information System (EthioSIS) at the Agricultural Transformation Agency (ATA) for financial support. We are very grateful to all assistances, knowledge and experiences we have received from the farmers in Damot Gale, Damot Sore and Sodo Zuria districts. Our acknowledgment also goes to anonymous reviewers for their critical evaluation and constructive comments. The appreciation further extended to anonymous reviewers for sharing us their time and valuable comments.
The authors declare that they have no competing interests.
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This research was conducted with the financial support of Ethiopian Soil Information System (EthioSIS) at the Agricultural Transformation Agency (ATA).
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