In the present study, about 94% of the arable land had a phosphorus deficiency (available P < 10 mg ·kg - 1). To compensate for this deficiency, high amounts of phosphorous fertilization were applied to soils to get better crop yield. In the past two decades, soil organic matter has sharply declined from 34.8 g/kg in late 1980s’ to 12.0 g/kg in 2010. The soil has moderate to high cation exchanging capacity (CEC) in the range of 45 - 58 Meq/100 gm. The low soil organic carbon, high CEC and high phosphorus fertilization could lead to poor heavy metal availability to plants. Nevertheless, DTPA extractable concentrations were 40.5 mg/kg for copper, 35.5 mg/kg for iron, 134 mg/kg for manganese, 2.1 mg/kg for nickel, 2.6 mg/kg for lead and 53.5 mg/kg for zinc. All the available micronutrients seem to be adequate for plant growth. In terms of toxicity, the values of Cu, Fe, Mn, Zn, Ni and Pb found in the present investigation were lower than those of above critical value set by the international guidelines and other researchers. Variations in heavy metal content in the soil were attributed due to differences in land use types and disparity in organic sources amongst the plant and animal composites. For better crop productivity, more organic matter should be added to the soils. The traditional nutrient cycling practices, such as manure application, allow crop residue to decay on fields, fallowing and rotational cropping has to be followed to rehabilitate the soil and buildup both macro-and micro-nutrients to their natural level.
The central Ethiopian highland is coming under increased pressure for the expansion of factories, export abattoirs, flower farms and other processing plants. These factories produce packed and semi-processed foods, tanneries and finished products like textiles, cosmetics, detergents, cement, metal and beverage products and largely congregate in 100 km radius of Addis Ababa, the capital of Ethiopia. This has resulted in shrinkage of the adjoining smallholders’ farms that used for the production of food in the land they have used for crop cultivation and cattle grazing. The result is that at the present rate of expansion due to both urbanization and industrialization, the survival of these farmers and their farm land is at stake. Most of the cultivated area is put to food crops like teff (Eragrostis abyssinica) and wheat (Triticum aestivum) and marsh and hillsides for sheep, goats and cattle grazing. The central Ethiopian highland is also a potential cereal producing zone and it is the highest supplier of high quality crop like teff to Addis Ababa and other towns in the country. Ethiopia also needs to boost food production and this is believed to be achieved by increased crop production per unit area to meet the needs of the increasing population. In the future, increased and sustained food production will need more fertilizer amendments. Under heavy or continuous fertilization, micronutrients and other heavy metals could also be introduced into the soil [
In Ethiopia context, researches on heavy metal toxicity and availability to crops have been limited around few towns’ along the river banks that are contaminated by factory effluents and have been used for vegetable production [
Given the important role of micronutrients in plant growth and animal nutrition and the deleterious effects of heavy metal contamination in the environment, the determination of background levels of these elements is therefore an important guide to prevent physiological disorders in grazing animals as well as serving as initial threshold levels for studying micronutrient concentrations and heavy metal pollution in future [
The naturally occurring background levels of heavy metals in uncontaminated soils usually occur in trace amounts related to the biogeochemistry of the parent materials [
In the current study six heavy metals (Cu, Fe, Mn, Ni, Pb and Zn) were analyzed for their level of heavy metal concentration in smallholders’ farms in Central Ethiopia. Fe and Cu are very important and mobile elements which have been widely studied globally, Ni and Zn are mobile in the soil are essential for plant growth, while Pb (although a relatively immobile metal) is considered a very serious environmental contaminant [
The specific purpose of this study was to:
Determine the heavy metal concentration in agricultural soils of the study area.
Compute the variation of heavy metal in different land use at the soil depths of 0 to 15 cm and 15 to 30 cm.
Compare heavy metal variation under the influence of different organic sources at the soil depths of 0 to 15 cm and 15 to 30 cm.
Ada district lies between longitudes 38˚51' to 39˚04'E and latitudes 8˚46' to 8˚59'N covering an area of 1750 km2 east of Addis Ababa. Most of the land (90%) was plain highlands ranging between 1600 to 2000 meters above sea level. The district is characterized by sub-tropical climate and receives 860 mm rain per annum [
In the study area 15 soil samples sites were taken at the depth of 0 to 15 cm and 15 to 30 cm. Four subsamples were taken from each sample site. Subsamples of each site were mixed and pooled in one bag. The sample sites were grouped in two categories by [
The sites were also categorized according to their land use as follows (a) Sites with chemical disposal effluents reach farms through water flow and folds from factory outlets such as detergents, steel, plastic bags, and food processing plants, Number of sites or N = 4; (b) Grazing land these are communal grazing land allocated for livestock grazing only, N = 2; (c) Croplands that were solely used for crop cultivation for more than 3 decades, N = 7; (d) Undisturbed land that was free of human and animal interference for more than 3 decades, such as church and research compounds and areas enclosed for conservation and biodiversity, N = 2.
The other grouping of the sample sites was the three classes of organic sources such as: (a) Animal debris from slaughter house waste disposal places sites, N = 5; (b) Plant debris which included decayed crop residues and
Case number | Sample site | Land use | Source of organic manure |
---|---|---|---|
1 | DZ research center | Uncultivated | None |
2 | Private commercial Farm | Cropland | Animal |
3 | Crop rotation plot | Cropland | Plant |
4 | Minimum tillage | Cropland | Plant |
5 | Farmyard manure plot | Cropland | Animal |
6 | Compost plot | Cropland | Plant |
7 | Recycling residue | Cropland | Plant |
8 | Communal grazing | Grazing | Animal |
9 | Fenced | Uncultivated | None |
10 | Mechanized farming | Cropland | None |
11 | Effluent contaminated | Chemical disposal | None |
12 | Effluent contaminated | Chemical disposal | None |
13 | Effluent contaminated | Chemical disposal | None |
14 | Abattoir waste disposal | Chemical disposal | Animal |
15 | Swampy disposal site | Grazing | Animal |
compost from crop rotation and non-organic sources, N = 4; (c) no external plant and animal organic additions, N = 6. The last category was helpful in the analysis of heavy metal loads in soils and their mobility due to natural sediments and soil contents.
Soil samples were collected purposely to describe the different land management practices and different organic sources such as degradation, area enclosure, crop history, tillage type, and levels of fertilization, residues left in the field and presence or absences of compost or manure applications. Samples were taken at the depths of 0 to 15 cm and at 15 to 30 cm with four subsamples at each composite site. Thus, a composite sample was made from four pooled subsamples. The four subsamples at each site were pooled for homogeneity and stored in a plastic bag and transported to Debrezeit Research Centre for soil chemical analysis in the Soil Laboratory within two hours of collection.
The pooled samples were air dried at ambient temperature and crushed to pass through a 2 mm stainless sieve. Then portions of pooled samples (about 50 cm) were ground to pass through a 0.149 mm sieve and stored in plastic bags prior to the chemical analysis. The pooled samples were analyzed for the following properties: pH, CEC, soil organic matter (SOM), available P, Fe, Mn, Ni, Cu, Zn and Pb. All the micro-nutrients were determined by DTPA extract through Atomic Absorption Spectrometer [
Statistical analysis and graphs were performed using [
Cluster analysis was used in the grouping of different sample sites with various levels of heavy metal content in the soil. Cluster analysis or clustering is the task of assigning a set of objects into groups (clusters) so that the objects in the same cluster are more similar to each other than to those in other clusters [
In a dendrogram, the X-axis marks the distance at which the clusters merge, while the objects are placed along the Y-axis so that the clusters don’t mix. Popular choices are known as single-linkage clustering that use minimum distance between objects [
The concentrations of heavy metals in the soil and their impacts on ecosystems can be influenced by many factors such as parent material, climate and anthropogenic activities ( [
The important consideration in the heavy metal identification in soils was to determine the original sources such as natural weathering, industrial processing, use of metal components in commercial processes, aerial deposition of smelting materials, leaching from garbage and solid waste dumps, the application of animal products, or some other sources [
Heavy metals in smallholder agriculture were mostly related to the addition of organic and inorganic nutrients to the soil. Most of the materials were added to soil for agricultural purposes such as manure, lime and other inorganic fertilizers have low trace element levels and when they were applied at normal rates and they did not affect overall concentrations of trace elements in soil. However, when they were applied at a higher rate they raised the concentration of trace elements in the soil. Other sources of inputs that increased the concentration of heavy metals in soil, included herbicides, fungicides, irrigation water, biosolid application, dredged materials, fly ash and municipal composts [
In the current study, the cluster analysis sample sites were classified into seven groups, after assigning average weight based on Eculdian distance measurement for all variables [
The physical and chemical characteristics of heavy metal concentrations in topsoil of the study area are shown in
Variables with soil depth | Mean | SD | Minimum | Maximum | |
---|---|---|---|---|---|
Soil carbon % | 0 - 15 cm | 1.40 | 1.03 | 0.07 | 3.90 |
15 - 30 cm | 0.99 | 0.73 | 0.07 | 2.48 | |
Cation exchange | 0 - 15 cm | 44.95 | 14.22 | 14.80 | 58.80 |
Meq/100gm | 15 - 30 cm | 46.88 | 10.58 | 27.80 | 58.80 |
Electrical cond. | 0 - 15 cm | 93.62 | 100.12 | 19.23 | 435.00 |
Mic. Siem | 15 - 30 cm | 132.06 | 135.83 | 19.24 | 496.00 |
PH | 0 - 15 cm | 7.00 | 0.36 | 6.47 | 8.08 |
15 - 30 cm | 7.00 | 0.37 | 6.38 | 7.97 | |
Available P (ppm) | 0 - 15 cm | 31.94 | 33.54 | 7.92 | 137.19 |
15 - 30 cm | 37.17 | 66.87 | 3.75 | 271.88 | |
Ca | 0 - 15 cm | 21.54 | 8.37 | 7.05 | 36.33 |
Meq/100gm | 15 - 30 cm | 21.87 | 8.31 | 9.48 | 37.29 |
mmol∙kg−1. The range was between 45.00 and 58.80 mmol∙kg−1, implying that the soils had higher CEC [
The decline in soil carbon over the past two decades was attributed due to decrease in soil nutrient cycling under mixed crop-livestock production systems. This has happened for the reason that straw and crop stalks are used as animal feed, for construction material and off-farm sales. In addition, dung was used as fuel for household energy consumption and sold for income generation instead of being used as organic fertilizer [
In the present study about 94% of the arable land had a phosphorus deficiency (available P < 10 mg∙kg−1), and 67% of that had a severe phosphorus deficiency (available P < 5 mg∙kg−1) [
DTPA extractable critical concentrations for plant growth were 0.12 to 0.25 mg/kg for copper, 2.5 to 5.0 mg/kg for iron, 1.0 to 5.0 mg/kg for manganese and 0.5 to 1.0 mg/kg zinc [
In physical terms organic matter improves the stability of soil aggregates resulting in better aeration of the soil and better water retention. It also improves the hydraulic conductivity as a result of the increasing percentage of soil macro-pores [
Fulvic acids are organic substances found in organic compounds in soils, which predominantly have lower molecular weights than humic acids, usually not more than 5,000 gm mol−1, and are often called dissolved organic carbon (DOC) [
In the current study the relationship between organic sources and trace minerals was identified as substantial. It was found that Cu, Zn and Ni have significant differences (P < 0.05) between different organic sources at 0 to 15 cm soil depth. In case of Zn there was a significant difference observed between animal sources (0.86 ppm ± 0.58) and the other two organic sources (no fertilizer addition 0.44 ppm ± 0.15 and plant sources 0.42 ppm ± 0.17). It showed that animal source was the major contributor to Zn load at 0 to 15 cm soil depth. Ni was higher for non-organic sources as shown in
Element | Bulbula (Addis Ababa) | Kera (Addis Ababa) | Current study area | Guidelines for metal above standard level |
---|---|---|---|---|
Soil (total) | Soil (total) | Soil (total) | Soil (total) | |
(mg∙kg−1) | (mg∙kg−1) | (mg∙kg−1) | (mg∙kg−1) | |
Cu | 38.96 | 55 | 40.5 | 100 |
Fe | 163.86 | 79.7 | 35.5 | 50000 |
Mn | 6587 | 3598 | 134.0 | 2000 |
Ni | 74.13 | 115 | 2.1 | 50 |
Pb | 46.47 | 110 | 2.6 | 100 |
Zn | 2985.5 | 263 | 53.5 | 300 |
Source: For Bulbula and Kera [
the concentration of all heavy metals was higher for those organic sources from animal origin than for those from plant origin (see
The heavy metal concentration was significantly influenced by the addition of fertilizers from different organic sources, especially for Fe and Zn at 15 to 30 cm soil depth. The F test at P < 0.05 based on the linearity of independent variables for paired comparisons among the estimated marginal means of Fe and Zn showed a
Organic source | ||||
---|---|---|---|---|
Element | Soil depth | Animal source (N = 5) | No organic fertilizer (N = 6) | Plant source (N = 4) |
Cu | 0 - 15 cm | 0.50 ± 0.43 | 0.51 ± 0.22 | 0.18 ± 0.09 |
15 - 30 cm | 0.50 ± 0.51 | 0.46 ± 0.28 | 0.15 ± 0.09 | |
Fe | 0 - 15 cm | 4.36 ± 4.32 | 2.13 ± 1.37 | 1.76 ± 2.16 |
15 - 30 cm | 8.88 ± 8.95 | 2.41 ± 1.76 | 1.54 ± 2.32 | |
Mn | 0 - 15 cm | 1.78 ± 2.71 | 1.76 ± 0.43 | 0.53 ± 0.35 |
15 - 30 cm | 1.60 ± 2.01 | 1.46 ± 0.42 | 0.48 ± 0.36 | |
Zn | 0.15 cm | 0.86 ± 0.58 | 0.44 ± 0.15 | 0.42 ± 0.17 |
15 - 30 cm | 0.75 ± 0.51 | 0.04 ± 0.01 | 0.38 ± 0.19 | |
Ni | 0 - 15 cm | 0.01 ± 0.01 | 0.04 ±0.01 | 0.01 ± 0.01 |
15 - 30 cm | 0.02 ± 0.01 | 0.03 ± 0.01 | 0.01 ± 0.00 | |
Pb | 0.15 cm | 0.03 ± 0.01 | 0.02 ± 0.01 | 0.01 ± 0.01 |
15 - 30 cm | 0.02 ± 0.01 | 0.03 ± 0.01 | 0.02 ± 0.01 |
significant difference in the addition of fertilizer from organic sources into the soil. The mean Fe concentration at 15 to 30 cm depth was 8.88 ppm ± 8.95 for animal sources as compared from plant sources of 1.54 p.m. ± 2.32 and no-fertilizer was 2.41 ppm ± 1.76.
At the depth of 15 to 30 cm, the concentration of Zn was higher for Animal sources (0.86 ppm ± 0.58) medium for no fertilizer (0.44 ppm ± 0.15) and lower for plant sources (0.42 ppm ± 0.17). The result showed at 15 - 30 cm soil depth implied that animal waste products had a significant impact on the concentration of Fe and Zn in the subsoil. Other trace minerals Cu, Mn, Ni and Pb did not show any significant difference for different organic sources at 15 to 30 cm depth, particularly the insignificance of Pb could be associated with poor mobility potential of Pb in the soil [
In general animal source contribution to heavy metal concentration was higher for Zn and Fe at both 0 to 15 cm and 15 to 30 cm soil depth as shown in
In the present study animal sources enhanced heavy metal mobility down the soil profile (except for Pb) when compared with two other sources, mainly due to relatively high organic carbon content from animal sources (1.96% organic carbon (OC) ± 1.32 at 0 to 15 cm depth and 1.57% OC ± 0.73 at 15 to 30 cm depth). Carbon content of plant sources was 1.20% OC ± 0.92 at 0 to 15cm depth and 0.88% OC ± 0.42 at 15 to 30 cm, and that of no-fertilizer was 1.06% OC ± 0.76 at 0 to 15 cm depth and 0.57% OC ± 0.64 at 15 to 30 cm. These findings were in agreement with the findings of [
Available heavy metals were the fractions of the total concentration of these metals in the soil, which was soluble in the soil solution or easily exchangeable from the soil surfaces. The availability of metals in soils depended on their forms and concentrations in the parent material and their input through commercial fertilizer, manure and municipal wastes, factory effluents and aerial deposition. In the absence of pollutants, natural levels of metals in soils were dictated by the types of elements in rocks, weathering rates, organic matter content, soil texture and soil depth [
In the current study relationship of heavy metal concentration and land use type gave a different picture for various land use categories as shown in
At the depth of 0 to 15 cm grazing land had a significant level of Fe (7.70 ppm ± 3.95) compared with other ecological groups (Cropland 0.82 ppm ± 0.81, chemical discharged sites 3.80 ppm ± 2.26 and undisturbed sites 2.60 ppm ± 1.86). The difference in Fe concentration could be due to livestock manure and urine on grazing land. Cropland had the lowest iron concentration of 0 to 15 cm depth, indicated that crops with high iron content like Teff [
There was a significant difference in Ni concentration (0.03 ppm ± 0.02) at 0 to 15 cm between chemical discharged sites and others land use groups which illustrated that effluents from factories with high Ni concentration could be a threat to farms situated near factories. In general chemical load by Ni and Cu at 0 to 15 cm depth was a threat, but still the hazard level is far below the environmental standard limit. In general farm sites near to chemical discharged areas have higher heavy chemical loads as compared to other site categories (see
An ecological history | |||||
---|---|---|---|---|---|
Element | Soil depth | Chemical discharged sites (N = 4) | Crop land (N = 7) | Grazing land (N = 2) | Undisturbed sites (N = 2) |
Cu | 0 - 15 cm | 0.83 ± 0.27 | 0.28 ± 0.14 | 0.18 ± 0.14 | 0.34 ± 0.12 |
15 - 30 cm | 0.79 ± 0.36 | 0.17 ± 0.11 | 0.18 ± 0.04 | 0.58 ± 0.42 | |
Fe | 0 - 15 cm | 3.8 ± 2.26 | 0.82 ± 0.81 | 7.70 ± 3.95 | 2.60 ± 1.86 |
15 - 30 cm | 6.63 ± 6.76 | 0.77 ± 0.92 | 6.30 ± 1.85 | 10.3 ± 13.22 | |
Mn | 0 - 15 cm | 1.70 ± 0.55 | 0.97 ± 0.72 | 0.26 ± 0.26 | 3.73 ± 3.99 |
15 - 30 cm | 1.54 ± 0.41 | 0.73 ± 0.52 | 0.08 ± 0.63 | 2.92 ± 3.01 | |
Zn | 0.15 cm | 0.49 ± 0.16 | 0.43 ± 0.18 | 0.59 ± 0.15 | 1.26 ± 0.90 |
15 - 30 cm | 0.49 ± 0.20 | 0.35 ± 0.13 | 0.57 ± 0.13 | 0.98 ± 0.94 | |
Ni | 0 - 15 cm | 0.03 ± 0.02 | 0.02 ± 0.01 | 0.01 ± 0.00 | 0.01 ± 0.00 |
15 - 30 cm | 0.03 ± 0.01 | 0.02 ± 0.01 | 0.00 ± 0.00 | 0.03 ± 0.02 | |
Pb | 0.15 cm | 0.02 ± 0.01 | 0.02 ± 0.01 | 0.03 ± 0.01 | 0.03 ± 0.02 |
15 - 30 cm | 0.02 ± 0.01 | 0.02 ± 0.01 | 0.03 ± 0.01 | 0.03 ± 0.01 |
There was a significant difference (P < 0.05) for Cu, Fe, Mn and Zn at 15 to 30 cm depth due to differences in ecological history. However, there was no significant difference for Ni and Pb at this soil depth. The concentration of Cu was significantly different between sites; chemical discharge (0.79 ppm ± 0.36), crop land (0.17 ppm ± 0.11) and grazing land (0.18 ppm ± 0.04), but there was no significant difference with undisturbed sites (0.58 ppm ± 042). At 15 to 30 cm depth the concentration of Fe was significantly different from crop land (0.77 p.m. ± 0.92) and the other three ecological groups (grazing land 6.30 ppm ± 1.85, undisturbed sites 10.30 p.m. ± 13.22 and sites with chemical discharges 6.63 ppm ± 6.76). It showed that crops absorbed a significant amount of Fe from the soil, particularly Teff for its highest iron content [
Mn concentration at the depth of 15 to 30 cm was significantly different between grazing land and the other three groups of ecological history. The highest Mn concentration was from undisturbed sites (2.92 ppm ± 3.01) and the lowest was from grazing land (0.08 ppm ± 0.63). Zn concentration was significantly different between the undisturbed sites and the other three ecologically different groups. There was a higher concentration of Zn at 15 to 30 cm depth for undisturbed sites (0.98 ppm ± 0.94) compared with the other three ecologically different groups as shown in
Crop lands suffer from low amounts of trace elements, which calls for further investigation to see how micro- nutrients could be supplemented to crop lands based on crop nutrient requirements. Some crops such as Teff remove more nutrients from the soil than others. This was in agreement with the findings by other workers who reported that Teff has high micro nutrient content demands such as Ca, Co, Zc, Al, Se and others [
This argument was further consolidated by findings obtained by [
In terms of toxicity, the values of Cu, Fe, Mn, Zn, Ni and Pb found in the present investigation were lower than those of above critical value set by the international guidelines and other researchers. Although their impact was negligible, variability in heavy metal content was revealed mainly due to factory effluents discharge and organic sources disposal from animal products. The role of natural resources such as soil sediments, rocks and soil contents to heavy metals variability is limited.
Land use type contributed to the variability of heavy metals, particularly Fe which was very lower in cultivated soils than in an area that had never been cultivated. This showed that cereal crops like teff with higher Fe, Cu, Zn, Mn and other micro-nutrients content in their grains and straw are heavily mining these soil nutrients. However, all the available micronutrient concentrations for the central Ethiopian highland soils seem to be adequate for plant growth, but the availability of heavy metals to plants nutrition is in critical condition possibility due to higher phosphorous fertilization and lower soil organic carbon content. A report from soil scientists indicated that grain and straw yield of cereals like teff crop had over quadrupled when supplemented by micro-nutrients such as Zn, Cu, Mg and S.
In the present study, the content of organic carbon in the soil is declining rapidly that will create further obstruction to the availability of micronutrients to plants in the future. For better crop productivity, more organic matter should be added to the soils of central Ethiopian highland. The traditional nutrient cycling practices, such as manure application, allow crop residue to decay on fields, fallow and rotational cropping has to be followed to rehabilitate the soil and buildup both macro-and micro-nutrients to their natural level.
We thank Mengistu Asfaw for payment of publication processing fee and Yasin Getahun for mapping sample sites.We gratefully acknowledge International Livestock Research Institute(ILRI) for supporting this research.
Nigatu Alemayehu Minase,Mary M. Masafu,Abule Ebro Geda,Azage Tegegne Wolde, (2016) Heavy Metals in Agricultural Soils of Central Ethiopia: The Contribution of Land Use Types and Organic Sources to Their Variability. Open Journal of Soil Science,06,99-112. doi: 10.4236/ojss.2016.66011