# Trace Element Status and Environmental Implications of Soils andZea mays from Farmed Dumpsites in the Bamenda Metropolis, North-West Cameroon

Authors: Mofor Nelson Alakeh; Njoyim Estella Buleng Tamungang; Mbene Kenneth; Yuhinwenkeh Njumbo Blaise; Nchofua Festus Biosengazeh
Journal: Applied and Environmental Soil Science
 (2020)

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## Abstract

This study assessed some physicochemical and trace element properties of soils andZea mays from farmed dumpsites in the Bamenda metropolis, North-West Cameroon. The growth in population and metal workshops in Bamenda has resulted in the dumping of large quantities of wastes on agricultural soils. Thus, the fear of these agricultural soils and crops being contaminated by waste dumped on them is a call for concern because most of the populations rely on agriculture for survival. A soil and Zea mays sample each was collected from three farmed dumpsites (Nkwen, Mankon, and Bamendakwe) in the Bamenda metropolis and analyzed for physicochemical and trace element properties using standard procedures. The results of physicochemical analysis revealed that the soils had pH values ranging from 5.63 to 7.49, average organic matter, low total nitrogen, high C/N ratio, and high CEC, and the soil textural class was clay loam for soils of Nkwen and sandy loam for soils of Mankon and Bamendakwe. The content of bases in Zea mays was high compared to those in the soil. The concentration of Fe (14635.6 µg/g) in soils of Bamendakwe and Cu (157.17 µg/g) and Zn (1438.36 µg/g) in soils of Mankon had values which were above the permissible limit. The concentration of Zn (114.48 µg/g) in the plant sample of Mankon together with the concentration of Fe in all three plant samples had values above permissible limits. Natural origins and domestic waste were identified as the major sources of trace metals in the soils. Thus, there are potential health hazards related to consuming crops from such soils. Bioremediation techniques can be used to recover heavy metals from such soils. Furthermore, the mobilization of nutrient ions and immobilization of heavy metals by induced liming could be important in sustainable agricultural production and soil environmental protection of the soils studied.


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## Body

## 1. Introduction

Environmental pollution is a worldwide problem, and its potential in influencing public health is great [1–3]. The impact of pollution near congested cities has reached a disturbing magnitude, coupled with soil pollution which is arousing public awareness [4]. Soils may become contaminated through the accumulation of trace elements and metalloids resulting from wastes dumped on them. Trace metal soil contamination may result from natural sources such as weathering of parent materials at levels that are regarded as trace and rarely toxic, but upon constant accumulation, it reaches toxic levels [2, 5–7]. Trace element contamination of soils could also result from anthropogenic sources such as rapidly expanding industrial areas, disposal of high metal wastes, leaded gasoline and paints, land application of fertilizers, sewage sludge, pesticides, wastewater irrigation, coal combustion residues, spillage of petrochemicals, and atmospheric deposition [8, 9]. Some trace elements (Fe, Cu, Mn, and Zn, amongst others) function as essential nutrients to plants and can directly influence the growth and energy-generating processes of plants due to their high reactivity within the soil system [10]. When the concentration of these trace elements in the soil goes above permissible limits, it becomes toxic to plants [11]. Trace element solubility in soil and bioavailability to plants is mainly influenced by the chemical properties of soil such as soil pH, cation exchange capacity (CEC), soil texture, and organic matter (OM) [12].With increasing population growth and industrialization in the world today, there is an increase in anthropogenic activities which have resulted in soil pollution due to waste being dumped on soils [13]. In trying to sustain this increasing population, man turns to the soil for crop production, thus making the soil an indispensable tool for man’s survival. The fear of agricultural soils being contaminated by wastes dumped on them is a major concern.The city of Bamenda, North-West Cameroon, has witnessed a rapid increase in population over the years, and this has resulted in large quantities of wastes being dumped on and around farmlands. The population growth, metal workshops, and use of metal appliances have experienced an increase in this city, which has resulted in the dumping of large quantities of metallic wastes on agricultural farmlands. Confronted with the above problem, the objective of this research was to assess some physicochemical properties and trace element content of soil andZea mays (maize) samples from farmed dumpsites in the Bamenda metropolis and their environmental implications.


## 2. Materials and Methods

### 2.1. Site Descriptions and Sample Collection

The study area is located in the grass field zone of Cameroon, precisely in the Mezam Division of the North-West Region of Cameroon. Mezam is located on latitude 05°58′42.6″ N and longitude 1008′52″ E and has an elevation of 1229 m above sea level. The land surface area is about 1745 km2, and its population density as of the year 2005 stood at 300.35 habitants/km2 (Bamenda City Council Development Plan, 2015). The Mezam Division is made up of seven subdivisions, and three of these subdivisions (Bamenda I, Bamenda II, and Bamenda III) were selected for this study (Figure 1).Figure 1
Map of the northwest region showing the study area and the different sampling sites (Bamenda City Council Development Plan, 2015).Fieldwork was carried out in December 2018. Three representative sites were chosen for sampling, based on the consideration that the land was being cultivated and was previously or is still being used as a garbage dumping site. The sites are Nkwen (S1), Mankon (S2), and Bamendakwe (S3). For each sampling site, soil and maize samples were collected. The soil samples were collected to a depth of 30 cm.The first study site is located in Nkwen, Bamenda III subdivision. It lays directly behind the Mile four Nkwen market, about 100 m away from mile four junction. The study site is located on latitude 05°59′03.59″ N and longitude 10°11′03.5″ E, with an altitude of 1228 m above sea level. The vegetation is grassland type and the land is used for mixed cropping (maize—Zea mays, beans—Phaseolus vulgaris, and cocoyams—Colocasia esculenta).The second study site is found in Mankon, located in the Bamenda II subdivision. It is located about 70 m from mile six junction and about 10 m from the river Mezam. The study site is located on latitude 05°59′04.6″ N and longitude 10°07′43.1″ E, with an altitude of 1222 m above sea level. The vegetation type is mixed with different crops being cultivated on the soil.The third study site is found in Bamendakwe and is located in the Bamenda I subdivision. It is located at about 20 m away from the Dschang motor park, behind the Mazi voyage. The study site is located on latitude 05°56′35.9″ N and longitude 10°10′15.5″ E, with an altitude of 1520 m above sea level. The vegetation is grassland type, and maize is cultivated on the soil.


### 2.2. Laboratory Analyses

The collected soil samples were air-dried in the laboratory, ground in a ceramic mortar using a pestle, and sieved through a 2 mm sieve. Maize samples were washed using running tap water to eliminate dust, pesticides, fertilizers, mud, and any airborne pollutants that may be present. The maize samples were dried at room temperature. After that, the samples were sliced using a stainless steel knife, weighed, and oven-dried at 80°C for 72 hours. The oven-dried maize samples were then powdered and sieved through a 2 mm sieve. The less than 2 mm soil and plant samples were then analyzed for various physicochemical properties and heavy metals using international standard methods [14, 15].Soil pH was measured in a 1 : 2.5 soil solution ratio in distilled water (pH-H2O) and 1 N KCl (pH-KCl). Exchangeable bases were determined by the method of Schollenberger by percolating 2.5 g of soil sample with 100 mL of 1 N ammonium acetate, after which sodium and potassium ions were determined by flame photometry, while calcium and magnesium ions were estimated by complexometric titration. Cation exchange capacity (CEC) was estimated by percolating 2.5 g of soil sample with 100 mL of 1 N ammonium acetate and then with 1 N KCl, and the collected NH4+ ions were then determined by distillation and titration with a 0.01 N sulphuric acid. Total nitrogen was estimated by exploiting Kjeldahl’s distillation method, while soil organic carbon (SOC) was estimated by oxidation with potassium dichromate and titration with iron (II) sulphate. Particle size distribution was determined by the hydrometer method. The available phosphorus was determined by the Bray II method. The levels of trace elements were determined by atomic absorption spectrometric (AAS) analysis.


## 2.1. Site Descriptions and Sample Collection

The study area is located in the grass field zone of Cameroon, precisely in the Mezam Division of the North-West Region of Cameroon. Mezam is located on latitude 05°58′42.6″ N and longitude 1008′52″ E and has an elevation of 1229 m above sea level. The land surface area is about 1745 km2, and its population density as of the year 2005 stood at 300.35 habitants/km2 (Bamenda City Council Development Plan, 2015). The Mezam Division is made up of seven subdivisions, and three of these subdivisions (Bamenda I, Bamenda II, and Bamenda III) were selected for this study (Figure 1).Figure 1
Map of the northwest region showing the study area and the different sampling sites (Bamenda City Council Development Plan, 2015).Fieldwork was carried out in December 2018. Three representative sites were chosen for sampling, based on the consideration that the land was being cultivated and was previously or is still being used as a garbage dumping site. The sites are Nkwen (S1), Mankon (S2), and Bamendakwe (S3). For each sampling site, soil and maize samples were collected. The soil samples were collected to a depth of 30 cm.The first study site is located in Nkwen, Bamenda III subdivision. It lays directly behind the Mile four Nkwen market, about 100 m away from mile four junction. The study site is located on latitude 05°59′03.59″ N and longitude 10°11′03.5″ E, with an altitude of 1228 m above sea level. The vegetation is grassland type and the land is used for mixed cropping (maize—Zea mays, beans—Phaseolus vulgaris, and cocoyams—Colocasia esculenta).The second study site is found in Mankon, located in the Bamenda II subdivision. It is located about 70 m from mile six junction and about 10 m from the river Mezam. The study site is located on latitude 05°59′04.6″ N and longitude 10°07′43.1″ E, with an altitude of 1222 m above sea level. The vegetation type is mixed with different crops being cultivated on the soil.The third study site is found in Bamendakwe and is located in the Bamenda I subdivision. It is located at about 20 m away from the Dschang motor park, behind the Mazi voyage. The study site is located on latitude 05°56′35.9″ N and longitude 10°10′15.5″ E, with an altitude of 1520 m above sea level. The vegetation is grassland type, and maize is cultivated on the soil.


## 2.2. Laboratory Analyses

The collected soil samples were air-dried in the laboratory, ground in a ceramic mortar using a pestle, and sieved through a 2 mm sieve. Maize samples were washed using running tap water to eliminate dust, pesticides, fertilizers, mud, and any airborne pollutants that may be present. The maize samples were dried at room temperature. After that, the samples were sliced using a stainless steel knife, weighed, and oven-dried at 80°C for 72 hours. The oven-dried maize samples were then powdered and sieved through a 2 mm sieve. The less than 2 mm soil and plant samples were then analyzed for various physicochemical properties and heavy metals using international standard methods [14, 15].Soil pH was measured in a 1 : 2.5 soil solution ratio in distilled water (pH-H2O) and 1 N KCl (pH-KCl). Exchangeable bases were determined by the method of Schollenberger by percolating 2.5 g of soil sample with 100 mL of 1 N ammonium acetate, after which sodium and potassium ions were determined by flame photometry, while calcium and magnesium ions were estimated by complexometric titration. Cation exchange capacity (CEC) was estimated by percolating 2.5 g of soil sample with 100 mL of 1 N ammonium acetate and then with 1 N KCl, and the collected NH4+ ions were then determined by distillation and titration with a 0.01 N sulphuric acid. Total nitrogen was estimated by exploiting Kjeldahl’s distillation method, while soil organic carbon (SOC) was estimated by oxidation with potassium dichromate and titration with iron (II) sulphate. Particle size distribution was determined by the hydrometer method. The available phosphorus was determined by the Bray II method. The levels of trace elements were determined by atomic absorption spectrometric (AAS) analysis.


## 3. Results and Discussion

The soil physicochemical properties are presented in Table1, while plant physicochemical properties are presented in Table 2.Table 1
Soil physicochemical properties.
Nkwen (S1)Mankon (S2)Bamendakwe (S3)pH-H2O5.687.495.63pH-KCl4.87.454.45ΔpH−0.88−0.04−1.18% N0.130.200.15% OC2.224.443.89% OM3.837.666.70C/N182326CEC (cmol(+)/kg)50.8848.3242.72AP (mg kg−1)13.5952.584.51K (cmol(+)/kg)0.640.640.64Na (cmol(+)/kg)0.280.280.28Ca (cmol(+)/kg)5.605.384.64Mg (cmol(+)/kg)4.002.643.04SB (cmol(+)/kg)10.528.928.60TBS (%)20.6818.4620.13Sand (%)406263Silt (%)302418Clay (%)301419ΔpH = net charge (pH-KCl − pH-H2O), OC = organic carbon, N = total nitrogen, OM = organic matter, C/N = mineralization factor, CEC = cation exchange capacity, AP = available phosphorus, SB = sum of bases, TBS = total base saturation, CL = clay loam, and SL = sandy loam.Table 2
Maize plant physicochemical properties.
Nkwen (S1)Mankon (S2)Bamendakwe (S3)% ash content9117% WC955% N4.205.6012.60% OC22.1422.4523.26% OM38.1738.7040.09C/N5.274.011.85TP (mg kg−1)136.901830.151312.15K (cmol(+)/kg)35.8012.9021.70% DWK1.400.500.85Na (cmol(+)/kg)1.951.031.26% DWNa0.040.020.03Ca (cmol(+)/kg)54.8066.8030.80% DWCa1.101.340.62Mg (cmol(+)/kg)11.2011.207.20% DWMg0.140.140.09WC = water content, N = total nitrogen, OC = organic carbon, OM = organic matter, C/N = mineralization factor, TP = total phosphorus, DWK = dry weight of potassium, DWNa = dry weight of sodium, DWCa = dry weight of calcium, and DWMg = dry weight of magnesium.The results of soil analysis showed that soil pH ranged from 5.63 for soils of Bamendakwe to 7.49 for soils of Mankon (Table1). The soils of Nkwen and Bamendakwe were moderately acidic, while those of Mankon were slightly alkaline [16]. The soils of Nkwen and Bamendakwe were moderately acidic and high in organic matter. The decomposition of this high organic matter can likely release carbon dioxide that reacts with water to produce carbonic acid. The acid formed reduces soil pH and this adversely affects microorganisms and increases the solubility and mobility of heavy metals in soil [17]. The soil pH can be raised to acceptable levels by liming the soils. Since the pH of the soil sample of Mankon fell within the neutral zone (6–8), the soil may be favourable for plant growth [18]. The sign and magnitude of ΔpH, which corresponds to the sign and magnitude of soil surface charge, were negative for all the soils with values ranging from −1.18 to −0.04, indicating that these soils were above their point of zero charge. This shows that they had net negatively charged surfaces, resulting in a net CEC at field pH [19]. These soil pH values conform to those reported by Anikwe and Nwobodo [20] while investigating long-term effects of municipal waste disposal on soil properties and productivity of sites used for urban agriculture in Abakali, Nigeria.Organic matter ranged from 3.83% for soils of Nkwen to 7.66% for soils of Mankon (Table1). It was observed that the OM content of Nkwen was medium, while that of Mankon and Bamendakwe was high. The high OM matter content for the soils of Mankon and Bamendakwe was due to organic waste dumped directly on the surface of this farmed site which increases the organic matter content of the soil, while the medium value obtained for the soil of Nkwen could be due to the fact that organic waste was dumped around this farmed site and not directly on the surface of the farm site as observed in the field. The organic matter content of all the three soils was of poor quality. This poor quality could be due to their high mineralization factor (C/N ratio) which slowed down the decomposition rate of organic material with lower mobilization of nitrogen [21]. To lower the mineralization factor, nitrogen-containing fertilizers could be applied on such soils to help increase the decomposition of organic material and improve its quality. Soil organic matter positively influences the concentrations of other soil properties such as total nitrogen and available phosphorus [16, 17, 20]. Soil organic matter values are similar to those reported by Nimyel et al. [22] who studied heavy metal concentrations in some vegetables grown in farms treated with urban solid waste in Kuru, Jantai, Nigeria.The total nitrogen content was low in all the three soils. Its values ranged from 0.13 to 0.2% (Table1). The C/N ratio for the soils was high with values ranging from 18 to 26. High C/N ratios indicated that the organic matter content was poorly mineralized [23]. High soil C/N ratio could slow down the decomposition rate of organic matter. Wider C/N ratios, as shown by the results, indicate a shortage of nitrogen for microbial protein synthesis resulting in competition for the available nitrogen, and hence, it will become immobilized, thus unavailable to plants. The soil total nitrogen content (0.13 to 0.2%) in this study was different from the high values reported by Anikwe and Nwobodo [20] on the long-term effects of municipal waste disposal on soil properties and productivity of sites used for urban agriculture in Abakali, Nigeria.Cation exchange capacity was high for all three soils with values ranging from 40.88 to 48.32 cmol(+)/kg (Table1). The soils of Mankon and Bamendakwe had comparatively lower CEC values (48.32 and 42.72 cmol(+)/kg, respectively), indicating that these soils were made of sand with a low water and nutrient holding capacity, which implies soils of this nature are very susceptible to cation nutrient loss through leaching [24]. The soils of Nkwen had a comparatively higher CEC value (50.88 cmol(+)/kg) compared to that observed for Mankon and Bamendakwe, which indicates that the soils had more clay, high water, and nutrient holding capacity, which implies soils of this nature are not very susceptible to cation nutrient loss since the cation is tightly held by the clay [24]. The values of CEC obtained in this study are in conformity with those reported by Nimyel et al. [22].The sum of the exchangeable bases ranged from 8.60 to 10.52 cmol(+)/kg (Table1). The high values of exchangeable bases could have resulted from the input of solid waste dumped on these sites, which, upon microbial breakdown of organic waste, releases these macronutrients into the soil for plant absorption [17]. Base saturation, which is the percentage of the soil CEC that is occupied by basic cations (calcium, magnesium, potassium, and sodium) at the current soil pH value, was less than 50% for all three soils, a fact which shows that the majority of the soils studied are acidic in nature.The available phosphorus for all three soil samples ranged from 4.51 to 52.58 mg kg−1 (Table 1). Soils of Mankon had the highest available phosphorus (52.58 mg kg−1), which could be due to its high organic matter content resulting from waste dump on this site and almost neutral pH which positively influences the concentration of available phosphorus present [25]. The soils of Nkwen and Bamendakwe had low values of available phosphorus. This could be due to their slightly acidic nature which permits phosphorus fixation.Soil texture (Table1) showed that soils of Nkwen were clay loam, fine-textured soil with a high water and nutrient holding capacity, while those of Mankon and Bamendakwe were of soil type sandy loam, coarse-textured soils with a low water and nutrient holding capacity [26, 27].Ash content is a measure of the total amount of minerals present within a food or plant [28]. Ash content analysis for all three maize plant samples ranged from 7 to 11% (Table 2), with samples of Mankon having the highest ash content which could be due to its slightly alkaline pH that favoured mineral uptake. The plant samples of Nkwen and Bamendakwe had low ash content. The pH of acidic soils can be raised to a value around neutrality to increase the mineral content in plants since they are readily available at soil pH around neutrality [18].The WC in all three plants ranged from 5% to 9% (Table2). The plant samples of Nkwen had the highest water content (9%) which could be due to the nature of its soil which is clay loam with a high water holding capacity. The plant samples of Mankon and Bamendakwe had a water content of 5%, which could be due to the sandy nature of the soils with a low water holding capacity.The organic matter content for all three plant samples was found to be very high, with values ranging from 38.17% to 40.09% (Table2). This high value of OM in plants could mean that though the soil organic matter was poorly mineralized, plants were able to take up the maximum amount of mineralized organic matter from the soil.The total nitrogen content in all three plant samples ranges from 4.20% to 12.60%, which is by far greater than the values obtained for the soil nitrogen content at a depth of 30 cm. In addition to obtaining nitrogen from soil, plants can also obtain nitrogen from the atmosphere by nitrogen fixation. This high value for nitrogen obtained in plants might also be due to the fact that plant roots were capable of absorbing available nitrogen found within the depth of 30 cm and beneath [29].The total phosphorus in all three sampled plants was very high, ranging from 1312.15 to 1830.15 mg kg−1. These high values could be due to very high organic matter in the plant which also influences parameters like the available phosphorus [17].The exchangeable bases in the plant were higher compared to the amounts present in the soil. This result showed that basic cations were high in these dumpsites, which permitted the proper functioning of some enzymes in plants to be able to absorb these ions from the soil solution [11].The results of total heavy metal concentration in soil and plant samples are presented in Tables3 and 4, respectively. Each trace element is considered in a sequence for discussion:Table 3
Trace element content in soil.
Site (sample)Zn (µg/g)Cu (µg/g)Mn (µg/g)Fe (µg/g)Nkwen (S1)34.6118.9512233484.6Mankon (S2)1438.36157.17127335237.7Bamendakwe (S3)137.5420.041126146353.6MAC300100150050000MAC = maximum allowable concentration [7, 30].Table 4
Trace element content in plant.
Site (sample)Zn (µg/g)Cu (µg/g)Mn (µg/g)Fe (µg/g)Nkwen (S1)50.192.9258.863694.29Mankon (S2)114.403.4242.484308.39Bamendakwe (S3)94.763.4038.441817.87MAC10073500425MAC = maximum allowable concentration [7, 30].Zinc (Zn): the total concentrations of zinc in the soil samples were 34.61, 1438.36, and 137.54µg/g for Nkwen, Mankon, and Bamendakwe, respectively. The soil samples of Mankon had its concentration above the maximum permissible limit (300 µg/g) (Table 3), implying that the soils of Mankon are suffering from zinc pollution. The total concentrations of zinc in the plant samples were 50.19, 114.48, and 94.76 µg/g for Nkwen, Mankon, and Bamendakwe, respectively. The total concentration of Zn in the plant sample of Mankon was above the maximum permissible limit (100 µg/g) (Table 4). This shows that maize grown on this soils absorbs a good portion of the zinc found in the soil. These high levels of Zn in soils may inhibit many plant metabolic functions, resulting to retarded growth [31]. Zinc is an essential trace element for plants, animals, and humans found in virtually all food [32]. Zinc is used to form connective tissues like ligaments and tendons [33]. Zinc toxicity in humans is rare, but at higher concentrations, it may induce toxicity characterized by symptoms of irritability, muscular stiffness, and pain [34]. Thus, consumers of maize grown on the soils of Mankon are likely to suffer from diseases associated with Zn toxicity.Copper (Cu): the total concentrations of copper in the soil samples were 18.95, 157.17, and 20.04µg/g for Nkwen, Mankon, and Bamendakwe, respectively. The soil samples of Mankon had its concentration of Cu above the maximum permissible limit (100 µg/g) (Table 3). The total concentrations of copper in the plant samples were 2.92, 3.42, and 3.40 µg/g for Nkwen, Mankon, and Bamendakwe, respectively. The total concentrations of Cu in all plant samples were below the maximum permissible limit (73 µg/g) (Table 4) and present no risk of contamination at the moment. The soils of Mankon have to be continuously monitored because other crops grown on this soil may absorb Cu above permissible limits or leaching may occur into nearby water bodies that the population of the area depends on.Manganese (Mn): the total concentrations of manganese in the soil samples were 122, 1273, and 1126µg/g for Nkwen, Mankon, and Bamendakwe, respectively. The total concentrations of Mn in all soil samples were below the maximum permissible limit set (1500 µg/g) (Table 3). The total concentrations of manganese in the plant samples were 58.86, 42.48, and 38.44 µg/g for Nkwen, Mankon, and Bamendakwe, respectively. The total concentrations of Mn in all plant samples were equally below the maximum permissible limit (500 µg/g) (Table 4). Manganese is essential for the normal physiological functioning of humans and animals, and exposure to low levels of manganese in the diet is considered nutritionally essential in humans. However, chronic exposure to higher doses is detrimental to human health [35].Iron (Fe): the total concentrations of iron in the soil samples were 33484.6, 35237.7, and 146353.6µg/g for Nkwen, Mankon, and Bamendakwe, respectively. Soil samples of Nkwen and Mankon had their concentration of iron below the maximum permissible limits (50000 µg/g) (Table 3), while soils of Bamendakwe had concentration of iron above the maximum permissible limits. The total concentrations of iron in the plant samples were 3694.29, 4308.39, and 1817.87 µg/g for Nkwen, Mankon, and Bamendakwe. Very high total concentrations of total could be from the soil parent materials (basalt, trachytes, and rhyolite) which are natural sources of Fe in the soil, and it could also be emanating from organic wastes dumping [12, 36]. The total concentrations of Fe in all plant samples were above the maximum permissible limit (425 µg/g) (Table 4). Excess amount of iron causes a rapid increase in pulse rate and coagulation of blood in blood vessels, hypertension, and drowsiness [37]. Thus, consumers of maize grown on the soils of the three study sites are likely to suffer from diseases associated with Fe toxicity.Soil pollution by trace elements negatively affects plant growth and degrades soil quality and the quality of agricultural products [31, 38]. The mobilization of nutrient ions and immobilization of heavy metals by induced liming could be important in sustainable agricultural production and soil environmental protection of the soils studied.Significant correlationsp<0.05 were recorded between most soil physicochemical properties (Table 5). Soil organic matter was shown to correlate positively with the soil nitrogen (r = 0.866), suggesting that an increase in the soil’s organic matter also increases soil nitrogen since nitrogen is a macroplant nutrient, and this nutrient availability in a soil is said to increase with an increase in soil organic matter [17]. The above results show that there exists a relationship between the soil physicochemical properties which affects the availability of nutrients [39].Table 5
Correlation between soil physicochemical properties.
NpH-H2OpH-KClOMCECSBAPSandSiltClayN1—————————pH-H2O0.9541————————pH-KCl0.9260.9971———————OM0.866∗0.6770.6131——————CEC−0.0690.2330.313−0.5581—————SB−0.604−0.337−0.258−0.9210.8371————AP0.8970.9880.998∗0.5560.379−0.1891———Sand0.6930.4450.3690.961−0.767−0.9930.3031——Silt−0.2770.0240.107−0.7200.9780.9330.176−0.8851—Clay−0.898−0.725−0.665−0.998∗0.5010.893−0.611−0.9400.6721∗Correlation is significant at the 0.05 level (2-tailed).Significant correlationsp<0.05 were also observed between soil and plant physicochemical properties (Table 6).Table 6
Correlation between soil and plant physicochemical properties.
NsNpOMsOMpAPsAPpKpNapCasCapMgsMgpNs1———————————Np−0.0861——————————OMs0.866∗0.4231—————————OMp0.0300.993∗∗0.5251————————APs0.897∗−0.5180.556−0.4151———————APp0.895∗0.3680.998∗∗0.4730.6051——————Kp−0.930∗∗−0.285−0.989∗∗−0.394−0.672−0.996∗∗1—————Nap−0.866∗−0.423−1.000∗∗−0.526−0.556−0.998∗0.989∗1————Cas0.000−0.996∗∗−0.499−1.000∗0.442−0.4470.3670.5001———Cap0.545−0.882∗0.53−0.822∗0.859∗0.113−0.199−0.0520.839∗1——Mgs−0.889∗−0.380−0.999∗∗−0.485−0.595−1.000∗∗0.995∗∗0.999∗∗0.458−0.1001—Mgp0.240−0.988∗∗−0.277−0.963∗∗0.645−0.2190.1320.2770.971∗∗0.945∗∗0.2311Subscripts s and p stand for soil and plant, respectively.∗∗Correlation is significant at the 0.01 level (2-tailed). ∗Correlation is significant at the 0.05 level (2-tailed).The soil organic matter was shown to correlate positively with plant-available phosphorus (r = 0.998) and potassium (r = 0.989). Soil organic matter upon mineralization positively influences parameters like phosphorus and nitrogen availability. This is true because nitrogen, potassium, and phosphorus are the main plant macronutrients and are controlled by the amount of soil organic matter; therefore, the higher the soil organic matter, the fertile the soil; hence, the more available are the plant nutrients. The soil-plant correlation results showed that plants depend on the soil physicochemical properties for plant nutrients availability. The correlation results revealed that relationships existing between soil physicochemical properties interfered with nutrient availability. The positive correlation between soil organic matter and plant-available phosphorus agrees with the findings of Tsozue et al. [21] who reported that plant nutrient availability depends on the relationship existing between soil and physicochemical properties. The trace elements analyzed showed a significant correlation with one another p<0.05. Zn and Cu showed a positive correlation (r = 0.998, p=0.038), suggesting they could have a common origin [40].


## 4. Conclusion

The main aim of this study was to assess the physicochemical and trace element (Zn, Mn, Cu, and Fe) properties of some farmed dump soils and maize plants in the Bamenda metropolis. The results showed that the soils had pH values ranging from 5.63 to 7.49, average organic matter, medium total nitrogen, high C/N ratios, and high CEC values, and particle size analysis showed that the soil textural class was clay loam for soil samples of Nkwen and sandy loam for soil samples of Mankon and Bamendakwe, ash content was low in plants, and high values for OM, available phosphorus, and total nitrogen were observed in the plant samples. The results of trace elements showed that some soils and plant samples were contaminated to different levels by different trace elements. The results obtained in this study show that the concentrations of trace metals at dumpsites are higher, which calls for concern to the environment and humans who depend solely on the soil in the dumpsite zones for survival. Further research should aim to analyze nearby streams, those directly linked to farmed dumpsites, to evaluate potential risk of contamination of the water bodies.



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*Source: 8861102-2020-10-07.xml*