American Journal of Agriculture and Forestry
Volume 3, Issue 3, May 2015, Pages: 65-72

Long-Term Impacts of Cultivation and Residue Burning Practices on Soil Carbon and Nitrogen Contents in Cambisols of Southwestern Ethiopia

Yacob Alemayehu Ademe*

Department of Plant Science, College Agriculture and Natural Resource, Dilla University, Dilla, Ethiopia

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To cite this article:

Yacob Alemayehu Ademe. Long-Term Impacts of Cultivation and Residue Burning Practices on Soil Carbon and Nitrogen Contents in Cambisols of Southwestern Ethiopia. American Journal of Agriculture and Forestry. Vol. 3, No. 3, 2015, pp. 65-72. doi: 10.11648/j.ajaf.20150303.11


Abstract: Soil organic carbon (OC) and total nitrogen (N) are important indices for evaluating land management system, so that assessing the management effects on soil OC and total N dynamics is essential for addressing sustainable land productivity and environmental quality issues. This study was carried out to determine the impact of long-term agricultural practices on the distribution and contents of OC and total N in Cambisols of Abobo, southwestern Ethiopia. Three adjacent fields: Cultivated field with continuous residue burning (CB), Grassland with annual burning (GB) and the Virgin land with native vegetation (VL) were used in this study. The soil in VL was used as a reference to assess extent of changes in soil OC and total N contents. Composite soil samples were collected from four soil depths (0-15, 15-30, 30-45 and 45-60 cm) of each land units, in the triplicate sites. A one-way ANOVA and correlation coefficient analysis were used to test the mean differences of the soil OC and total N contents in each soil depth, and to determine their degree of association with other soil variables. The result revealed that the existing management practices significantly affected soil OC and total N contents in all the studied soil depths. The depletion of soil OC and total N from CB and GB fields were up to 83 and 66%, respectively, as compared to those in the VL. Changes in soil OC and total N were more pronounced in the top 30 cm depth of soil, although significant reduction observed in the 30- to 60 cm depth. The contents of deeper soil layers (45-60 cm) in burned and burned/cultivated sites were comparable, implying that immediate fire/tillage impacts were restricted to the near surface soil depth. The overall results suggest that the existing land management is not sustainable; hence, proper residue management is imperative in order to sustain the soil quality and maintain long-term productivity of the farmland.

Keywords: Prolonged Cultivation, Residue Burning, Organic Carbon, Total Nitrogen, Soil Depth


1. Introduction

Soil organic carbon (OC) is one of the largest carbon pools on the earth's surface, accounting for 2344 Pg (56%) of overall global carbon [1]. Soil OC contents play a vital role in sustaining soil fertility for crop production and environmental quality due to its effects on soil physical and chemical properties, as well as biological activities [2]. This implies that soil quality is highly linked with soil OC content, whose status depends on biomass input and management, mineralization, leaching and erosion of soil organic matter. A type of agricultural landuse and/or management practices has a significant factor that controls soil OC levels, since it affects the amount and quality of litter input, decomposition rates and the processes of OM (~58% C) balance in soils [3,29]. For instance, removal or burning residues in the field causes considerable loss of organic C and N [8,9] and other nutrients by volatilization [10,11], which might adversely affect soil microorganisms [12].

Ethiopia has one of the oldest agrarian cultures in the sub-Saharan Africa with a large agriculture potential. Today, agriculture is not only the backbone of the economy, but also a major occupation for nearly 83% of Ethiopia’s inhabitants [9]. This sector is, however, beset by anthropogenic factors (land use/management systems) that adversely affect its productivity [4,5]. Improper land use and/or management practices mainly: continuous cultivation with low input, removal of crop residues (as animal feed or fuel wood) or burning plant residues as practiced under the traditional system of crop production are major contributors to the loss of soil OC and nutrients [6,27] that aggravates the decline of quality and productive capacity of soils in various parts of the country [5, 6, 7, 13, 33]. Different rates of decline in OC and total N after cultivation of forest soils have been reported, but most contain a great reduction. In the western Alfisols of Ethiopia, Wakene and Heluf [13] reported losses in OC and total N of 79 and 76%, respectively, from virgin soils after 40 year of cultivation. Tsehaye and Mohammed [14] found that surface OC and total N concentrations in Mollisols declined by 68% and 56%, respectively, after cultivation as compared to that of natural forest counterpart. Also reported by Nega and Heluf [15], significant decreases in OC and total N up to a depth of 50cm, in fifty year continuously cropped field when compared with forestland. Elsewhere, Reeder et al. [16] reported a decline of 18 and 26% in surface soil OC and total N, respectively, after sixty year of intensive cropping in the Great Plains.

The present study targets Abobo area, southwestern Ethiopia, where agricultural pressure became higher over the past three decades, and recurrent residue burning (both cultivated and open field) practice is common traditional agriculture. In this area, fire is widely used by farmers to clear vegetation and crop residues (in every dry season), because it provides an easy and economical means of access to fields. In this regard, very little is known about the soil variables with long-term different management practices. Previous studies [17,18] observed variations in soil properties (viz. OM content, soil depth) along landscapes of the area. However, the aforementioned researches merely compare variation soil properties as a function of landscape, and have tended to ignore the variation found due to differences in the existing land use and/or management practices. As land management effect varies depending on land use scenario (duration of land use, cropping systems, residue management) and climate of the area, it is impractical to take reported data from other areas to assess the situation in Abobo area. Hence, knowledge about the condition of soil quality indicators is vital for replenishing and maintaining soil fertility of the area.

In this work, it was hypothesized that soil OC and total N contents would vary due to the extended variation in land management practices in the site. Therefore, the objectives of this study were (i) to determine the quantity and the distribution of soil OC and total N at depths of fields affected by different land management practices (ii) to estimate the changes in OC and total N of soils under prolonged period of cultivation and burning practices that could contribute toward improved management of the agricultural land in the area.

2. Materials and Methods

2.1. Location and Site Characteristics

The study site is located in Gambella region, at the village of Abobo, southwest Ethiopia (Fig. 1). The agro-ecology of the area is typically hot to warm sub-humid lowlands [30] with mean annual rainfall of 1039.4 mm (uni-modal type), and mean annual temperature 26.4 0C [31]. Subsistent and mixed crop-livestock agriculture characterizes the farming system. The study site is flat terrain with elevation about 550 m a.s.l, and covering about 210 ha. The soils at the site were classified as Haplic Cambisols and Fluvi-Mollic Cambisols, according to WRB soil classification system [19], with moderately deep to deep soil profile and dark reddish brown color [18], and slightly acidic pH. For more understanding of the soil condition, selected physicochemical properties of soils of the site are presented in Table 1. The area is nearly level to gently sloping, and no salinity and drainage problems existed.

2.2. Land Use/Management

The study area is known to have a three distinguishable land use and/or management practices: namely long-term cultivated field, grassland and forest/shrub land. Based on the land use and/or management history, all the sites were similar before, and changes in land use have been introduced since the last three decades. Information on the land use and/or management history and characteristics of the site is briefly presented as follows:

Long-term cultivated field with annual residue burning (CB): The field has been cultivated continuously for about 30 years with annual mechanized plow, and cropped predominantly to maize (Zea mays L.), cotton (Gossypium hirsutum L.) and haricot bean (Phaseolus vulgaris L.). Small vegetation and crop residues burning in the dry season (January-March) of every year, has been common practice of land preparation for cultivation. It covers about 154 ha of land.

Grassland with annual burning practice (GB): the site occupied by annual grasses, mainly Sudan grass (Sorghum bicolor subsp. drummondii), which is used as forage for livestock. Similar to cultivated land, this field has been undergoing annual burning practice, for rejuvenation and establishment of the grass for better forage. This site has never been cultivated for several years, and covering nearly 36 ha.

Virgin forestland (VL): located adjacent to the Grassland field, which is occupied by various shrubs and tree species such as: Azadirachta indica, Acacia sp. and other local tree species. In addition, plantations have been established in early 1980s.

2.3. The Research Approach and Soil Sampling

A necessary assumption made in this research approach was that soil conditions or parameters for all the sites should be similar before changes in the land use/management have been introduced. Accordingly, three treatments based on agricultural management practices: long-term cultivated field with annual residue burning (CB), grassland which had been received annual burning (GB), and virgin forestland (VL) were set up; with four sampling depths (0-15, 15-30, 30-45 and 45-60 cm) for each. Three replicate sampling locations approximately 200m apart were bordered within the specific land unit.

The replicate fields were sampled randomly over the whole area. At the time of soil sampling (in March, 2012), both under cultivation and grassland had been received residue burning, as usual as it was done before. A total of 36 composite soil samples (each composite sample made from a pool of 9 subsamples) were collected from each sampling depth of soils of the three land management classes. The sites had comparable slope (gradient and aspect) and parent materials they developed [18], hence, similarity in slope and topographical conditions among sampling plots were maintained as much as possible in order to minimize extraneous errors.

Figure 1. Location map of the study area and the sampling points (Abobo area, southwestern Ethiopia).

Table 1. Mean values of the selected physicochemical properties of soils sampled from different lend use/management practices (data collected in 2012).

Land unit # Depth sand silt clay pH P Na K Ca Mg CEC PBS
(cm) --------------(%)---------------   (mg kg-1) ---------------------(cmolc kg-1)----------------------- (%)
CB 0-15 15.60 37.23 47.80 6.06 9.64 0.57 1.00 9.11 9.51 31.51 64
  15-30 16.00 34.83 47.13 5.88 8.37 1.55 1.57 8.81 10.12 31.88 69
  30-45 20.16 39.00 40.80 6.06 8.41 1.97 2.13 8.10 9.51 32.31 67
  45-60 19.23 37.05 45.61 6.02 8.66 1.97 2.21 6.13 9.21 30.30 64
GB 0-15 16.40 40.10 42.63 6.37 10.73 1.59 1.59 8.67 9.32 34.17 62
  15-30 21.06 33.80 45.13 6.19 11.67 2.17 1.20 10.42 10.51 35.71 68
  30-45 16.40 40.63 43.03 6.01 9.72 2.66 2.26 8.66 10.62 35.61 68
  45-60 -- -- -- -- -- -- -- -- -- -- --
VL 0-15 13.20 32.43 54.37 6.60 27.61 0.33 1.73 10.14 15.95 38.91 72
  15-30 19.07 34.7 47.13 6.23 25.18 1.02 1.72 11.45 15.23 36.97 80
  30-45 29.8 29.83 40.36 6.33 22.82 1.57 1.22 10.93 13.18 35.67 75
  45-60 -- -- -- -- -- -- -- -- -- -- --

# CB (long-term cultivated field with annual residue burning) and GB (grassland with annual burning) and VL (virgin forest soil).

-- = Not determined

2.4. Soil Sample Analysis

Composite samples collected from the respective depths of each land units were air-dried and crushed to pass a 2-mm sieve, and the selected soil physicochemical parameters were determined in the laboratory, using standard analytical methods. Soil OC was determined by the Walkley-Black wet digestion method [20]. Total N was determined using the micro-Kjeldahl digestion, distillation and titration procedure [21]. Soil texture was determined by hydrometer method as described by Van Reeuwijk [22] after dispersion of clays with sodium hexametaphosphate. Available P quantified by Olsen method [23], as the method recommended for all types of Ethiopian soils [24]. The pH of soil samples were measured in 1:2.5 soil-water ratio. Cation exchange capacity (CEC) was determined after extracting the soil samples by ammonium acetate at pH 7.0 [25]. Exchangeable Ca and Mg in the extracts were determined using atomic absorption spectrophotometer, whereas Na and K were quantified by flame photometer [22], and then percent base saturation (PBS) was computed as:

(1)

2.5. Statistical Analysis

A one-way analysis of variance (ANOVA) was used to test differences in soil OC and total N contents and C:N ratio among land units for each soil depth, using the General Linear Model (GLM) procedure of SAS program [26]. All tests of significance were made at p < 0.05, and the least significant difference (LSD) test to separate means between treatments. Similarly, individual land units were evaluated for soil OC and total N contents in the four depths down to 60 cm. Pearson’s correlation coefficient analyses were performed to determine the relationships between organic C and selected soil variables. In addition, the changes due to long-term cultivation and residue burning were determined by comparing the current values of C and N under CB and GB fields with those C and N content of undisturbed virgin soils (VL), assuming to have similar properties earlier to the present land uses.

3. Results and Discussion

3.1. Soil Organic Carbon Content

Analysis of variance (ANOVA) showed an overall significant effect (p<0.01) of land management practices on soil OC contents in all the considered soil depths (Table 2). Across the land units, the mean value of OC ranges between 12.2 g kg-1and 72.7 g kg-1 of soil. The largest apparent variation in OC concentration was found in surface soils (0-30 cm) of long-term cultivated field (Table 3). The reduction of OC from the topsoil (0-15 cm) under long-term cultivated field with annual burning (CB) and grassland with annual burning (GB) were 83 and 72%, respectively, as compared to the virgin forestland, VL (Fig. 2A). The amount of soil OC decline in CB, in this case, is about 32% greater than that of reported from the Great Plains soils subjected to intensive cultivation for 60 years [16]. The reduction occurred mostly in the top 30 cm of soil, although significant reductions were observed in the 30 to 60 cm depth. This is due to the fact that prolonged cultivation coupled with frequent burning of crop residues practices have been accelerated the rapid turnover rates of organic materials in both fields. Conversely, the virgin soil (VL) produced high mean value of OC (Table 3) which is mainly due to the continuous accumulation of decomposed plant and animal residues in the absence of disturbance of soil environment over a long time period.

Compared to GB field, long-term cultivated field with annual burning (CB) has produced significantly lower quantity of OC (p < 0.01) at the topsoil (0-15 cm depth) (Table 3), in which the difference in OC corresponds to about 38% lower than the long-term burned/grass field. However, the concentrations in the all the subsoil depths (15-60 cm) of both fields were remained statistically at par, that the contents of deeper soil layers (30-60 cm) in burned/cultivated and burned sites was similar, suggesting that immediate fire/tillage impacts were restricted to the surface soil (0-30 cm). Low quantity of OC under CB than GB field is due to the combined effect of prolonged cultivation and recurrent residue burning practices.

However, despite the absence of such soil disturbance by cultivation practices, periodic burning and removal of grasses in GB field has brought to a considerable decline in OC, compared with the neighboring virgin forest field.

Table 2. Mean square (MS) and results of one-way ANOVA for soil organic carbon (OC) and total nitrogen (TN) contents in different land management at different soil sampling depth.

Sampling depth OC     TN     C:N    
MS F-value p-value MS F-value p-value MS F-value p-value
0-15 3265.1 6.29 <0.0001 6.94 150.46 0.0002 69.42 114.54 0.0003
15-30 2631.3 424.1 0.001 4.48 28.14 0.004 93.54 33.57 0.032
30-45 324.9 41.64 0.002 0.69 18.21 0.009 32.80 578.88 <0.0001
45-60 29.04 16.56 0.012 0.074 26.80 0.0048 12.30 7.48 0.045

* Land units: long-term cultivated field with annual residue burning (CB), grassland with annual burning (GB) and virgin forestland (VL).

Table 3. Mean values soil organic carbon (OC), total N (TN) and C:N ratio under different land units are compared within each sampling depth.

land units 0-15 cm 15-30 cm 30-45 cm 45-60 cm
OC TN C:N OC TN C:N OC TN C/N OC TN C:N
---(g kg-1)---   ---(g kg-1)---   ----(g kg-1)----   ---(g kg-1)---  
CB 12.2c 1.7b 7.9c 10.9b 1.5b 6.8b 10.3b 1.1b 9.1c 9.4b 0.9b 10.1ab
GB 19.6b 1.9b 10.8b 14.9b 1.6b 9.9b 9.7b 1.3b 7.9b 9.3b 1.1a 7.9b
VL 72.7a 4.4a 16.7a 63.8a 3.6a 17.7a 28.1a 2.0a 13.8a 14.6a 1.2a 11.8a
LSD(0.05) 6.12 0.49 1.76 5.64 0.48 3.78 6.36 0.44 0.54 3.01 0.11 2.91
CV(%) 7.74 8.22 6.68 8.36 9.66 14.6 17.5 13.1 2.35 11.9 4.74 12.8

Comparison is based on one-way ANOVA and LSD test; Means within column followed by the same letter are not significantly different; triplicate samples for each land management type and depth were used.

Considering the soil depths of each field, the ANOVA also indicated the existence of highly significant difference (p<0.001) in OC among the depths of VL, and significant difference (p=0.05) GB and CB fields (Table 4). Similarly, mean comparison test showed a consistent and significant decrease (p=0.05) with increasing depth of VL field. Compared to their respective surface soils, the amount of soil OC at 45-60 cm depth was declined by 23%, 53% and 79%, respectively, for burned/cultivated field, burned/grassland and virgin soils. Statistically higher values at 15-30 cm depth of virgin land than its deeper depths (Table 4), suggest that the layer is still the most biologically active part of the soil profile. In contrast, the decrease of OC was gradual with depth of CB as compared to other fields, this might be due to disturbances by tillage implements, which could mix different soil layers. This observation is consistent with David et al. [2] who reported the decline in OC in paired fields after 50 year of cultivation in central Illinois.

Figure 2. Percentage decline in (A) soil organic carbon contents and (B) total nitrogen contents for each soil depth of CB (long-term cultivated field with annual residue burning) and GB (grassland with annual burning), as compared to virgin forest soils.

Following the ratings for tropical soils [28], the OC concentration of topsoil of both CB and GB fields qualify for ‘low’ level; hence such condition could render the soil quality which directly relates to reduced agricultural production. The result supports the suggestions that most cultivated soils of Ethiopia are poor in OC content due to the effect of reduced soil OM (~ 58% C) inputs apparently complete removal of crop residues from cultivated fields [7,15,27]. The values obtained under VL are comparable to those reported in forest soils of southern Ethiopia [6,32] and Alfisols of western highlands Ethiopia [13], however, the magnitude of decline in this case is higher than those reported by the authors mentioned. On the other hand, tremendously higher OC decline (up to 90%) from burned soils compared to unburned soils have also been reported [8,11] within a short-term (< 10 year) duration.

3.2. Total Nitrogen Content

The result presented in Table 2 indicated that soil total N content was significantly (p ≤ 0.01) affected by land management in all the measured soil depths. Considering the topsoil (0-15 cm) of land units, the highest soil total N content (4.4 g kg-1) was found in VL, followed by CB (1.9 g kg-1) and GB (1.7 g kg-1). Mean comparison of soil total N also showed that the forest soil (VL) significantly differ (p < 0.05) in all the soil depths from the soil of other land units, while the values under GB and CB remain statistically at par except 30-45 cm (Table 3). Variations in soil total N were more pronounced in the top 30 cm of soil, in which the contents were normally 58 - 61% less in CB compared with VL, whereas 57% decline in total N content of GB fields (Fig. 2B). The value observed in surface of CB was about 27% greater than that of reported [17] from the nearby site that was subjected to burning and removal of crop residue for several years.

The quantity of total N was strongly associated with OC (r = +0.59; p ≤ 0.01) (Table 5), and decreased consistently with increasing soil depth of all land units. Compared to the respective soil depth of the virgin forestland, about 46 and 35% (30-45 cm) as well as 25 and 8% (45-60 cm) of total N decline were observed in the subsoil of CB and GB fields, separately. It can be suggested that the low content of total N in CB and GB fields, possibly due to the effects of continuous cultivation and subsequent burning of crop residues, which aggravated the oxidation of organic C. Comparable studies from northwest Ethiopia [33] and boreal interior of Alaska [8] also noticed that frequent burning crop residues had significantly reduced soil total N contents under cultivated land as compared to the uncultivated counterpart of the same site. Earlier study [14] also reported that surface total N contents declined by 56%, after cultivation as compared to that of natural forest counterpart.

Soil total N contents significantly (p ≤ 0.01) decreased with the increasing soil depth of VL and GB fields, but the decrease was non-significant (p > 0.05) in CB field and almost similar for soil depths (Table 4). Moreover, in all the land units, the soil depth below 45 cm was similar decline in total N concentrations, indicating that the depletion in OM occurred at the upper layers. In general, the amount of total N at the surface soils of CB and GB fields can be rated as ‘very low’ level [28], whereas the VL field exceeds the ‘medium’ range. Such decline might have significant consequences on crop production in the area, because OM supplies most of the nitrogen taken up by unfertilized crops [8].

3.3. Soil Carbon-Nitrogen Ratio

Soil C:N ratio is often considered as an indication of soil N mineralization capacity [29]. The mean value of C:N ratio of soils varied from 6:1 in CB to 18:1 in VL. In all the soil depths, the undisturbed virgin soil (VL) had significantly (p ≤ 0.01) higher C:N ratio (17:1) than the other soils (Table 3). On the contrary, the C:N ratio of most of depths in CB field was found to be narrow, below the ‘optimum’ range (10 - 12:1) for arable soils [29]. In fact, natural lands usually have higher C:N ratio than prairies and cultivated areas, since cultivation/burning leads to losses of C and N, but the loss of C was much higher than the loss of N, the C:N ratio narrows. Hence, massive burning of crop residues are reasons for low C:N ratios in CB and GB fields, and this could accelerate the process of microbial decomposition of OM and N [10]. This observation is in consistent with earlier studies [14,28] which reported greater C:N ratios in forest soils than agricultural soils.

3.4. Association of OC with Other Soil Variables

The computed correlation coefficient indicated a strong and positive association of OC with some important soil variables: which was highly significant with CEC (r = +0.76; p ≤ 0.001), P (r = +0.72; p ≤ 0.01) and Mg (r = +0.61; p ≤ 0.01), C:N (r = +0.88; p ≤ 0.001), and positive but non-significant with pH (r = +0.46; p > 0.05), Ca (r = +0.37; p > 0.05), PBS (r = +0.22; p > 0.05)  (Table 5). This implies that deprivation of OC by the existing management practices had also left the soils of CB and GB fields with a discernible decrease in some vital soil variables. On the other hand, increased soil variables in VL with the soil depth (Table 1) indicates vegetation restoration has implication for improvement of soil nutrients. Equally, as CEC depends largely on clay and OM contents of the soil [29], continuous burning of organic residues had depleted soil OM that attributed to reduction in CEC of soils in CB and GB compared to the undisturbed VL counterpart. The findings are in harmony with the earlier studies [12,18], who reported higher reduction of CEC, PBS and P contents of soils under comparable management.

Table 4. Mean values for soil OC, total N and C:N ratio of each land units with the soil depth.

Sampling depth (cm) CB     GB     VL    
OC TN C:N OC TN C:N OC TN C/N
-----(g kg-1)----   -----(g kg-1)----   -----(g kg-1)----  
0-15 12.2a 1.7 7.2b 19.6a 1.9a 10.8a 72.7a 4.4a 16.7a
15-30 10.9ba 1.5 6.8b 14.9b 1.6b 9.9a 63.8b 3.6b 17.7a
30-45 10.3b 1.1 9.1a 9.7c 1.3c 7.9b 28.1c 2.0c 13.8b
45-60 9.4b 0.9 10.2a 9.1c 1.1c 7.9b 14.6d 1.2d 11.8b
Mean (60cm) 10.5 1.3 8.3 13.5 1.5 9.1 44.8 2.8 15.1
LSD 2.05 - 1.55 3.68 0.17 1.78 8.22 0.69 2.79
Significance * NS ** * ** ** *** *** **
CV 9.78 6.1 9.7 14.3 5.97 9.6 9.18 12.1 9.31

Soil OC, TN and C:N values of the sampling depths are compared within land unit; comparison is based on one-way ANOVA (LSD test; p<0.05); values followed by the same letter are not significantly different.

*, **, *** indicates that the ANOVA is significant at 0.05, 0.01 and 0.001 probability levels, respectively; NS = non-significant.

Table 5. Pearson’s Correlation Coefficients for the selected soil chemical parameters.

Parameters pH TN C/N P Na K Ca Mg CEC PBS
OC 0.46 0.59** 0.88*** 0.72** -0.64*** -0.14 0.37 0.62** 0.76*** 0.22
TN 0.51* 1.00 -0.18 -0.18 -0.51** -0.42 0.08 0.02 -0.05 -0.20
C/N 0.31 0.02 1.00 0.88*** -0.49** -0.02 0.36 0.56** 0.61** 0.25

*, **, *** indicates that the correlation is significant at 0.05, 0.01 and 0.001 significant levels, respectively.

4. Conclusions

Assessing long-term land management effects on soil OC and total N dynamics is essential for addressing sustainable land productivity issues. Results of the present study showed that the existing management practices significantly affected soil OC and total N contents and distribution in all the studied soil depths. Prolonged cultivation coupled with residue burning practices had severely depleted soil OC and total N contents of the cultivated field, as compared to the uncultivated grassland site. Similarly, great declines in soil OC and total N content was found in the grass field that has been undergoing annual burning practice, compared with the adjacent virgin forest field. Variations in soil OC was more pronounced at topsoil, and the contents of deeper soil depths in burned and unburned/cultivated sites was more or less similar, suggesting that immediate fire/tillage impacts were restricted to the surface soil depth. On the other hand, positive and strong association of OC with some soil variables as well as increased soil variables in forest field with its soil depth indicates vegetation restoration has implication for improvement of soil nutrients. Since soil organic matter is a key resource of soil nutrients for plant growth, soil structural stability and carbon stock, it must be well managed if agricultural activities were to be sustainable. Thus, precautions should be taken with residue burning to avoid loss of plant nutrients around the root zone, and improvement in soil management (such as fallowing, biomass transfer) should be implemented to ensure sustainability of the farming system. Because, the adverse impacts of residue burning and intensive cultivation are not only dropping input of biomass OC, but also reduction in nutrient cycling, which in turn brought to decline in soil quality.

Acknowledgements

Funding was provided by the Rural Capacity Building Project (RCBP) for training and research in Ethiopia. My sincere thanks goes to the anonymous field and laboratory assistants for their unreserved collaboration in collecting samples and analyzing the soil parameters. Also, Mr. Ararsa Boki and two anonymous reviewers, who provided helpful suggestions on the manuscript are highly acknowledged.


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