Agriculture remains one of the major economic activities sustaining many economies in all parts of the world with cultivated land being a key resources for the agricultural society [
51], without which, no agronomic practices can be actualized. Globally, a lot of environmental damage in the past few decades has been associated with intensification of agricultural activities [
52]. This has made soil to be one of the resources most vulnerable to degradation through unsustainable land use conversion that has potential impacts on the physical and chemical properties of soils [
53]. Land use dynamics have the potential to influence the physical and chemical properties of the soil [
53]. For example, the conversion of forests into agroecosystems has been a worldwide concern as it alters nutrient cycles within the soil and contributes towards soil quality degradation in the long run. The impact of agricultural activities on soil quality can therefore be understood by conducting regular monitoring of soil quality.
4.1. Variations in pH, EC and Base Cation Concentrations
The PH, negative log
10 of the hydrogen ions present in a medium, is one of the basic soil properties that influence agricultural production [
55]. Its influence on agricultural productivity is based on the fact that many other chemical and biological processes taking place within the soil ecosystems. For example, pH has been found to influence microbial activity in biodegradation of organic wastes and mobility of certain nutrients and pollutants such as heavy metal within the soil sub system. Even though different crops have different pH requirements with some performing better under acidic conditions and others under alkaline conditions, the optimum pH range for most plants is 5.5-7.5. Many plants are affected by extreme changes in PH [
56]. For examples, at very low soil pH e.g. below 6, some important soil nutrients such as Mo, Ca, Mg, P, N, and K may become less available to plants while other toxic elements such as Al and Mn become available in large quantities that may negatively affect plant physiological processes [
57]. At high PH above 7.5, calcium may bind phosphorus, making it unavailable for plants. Very alkaline conditions may also lead to cobalt and zinc deficiency resulting in stunted growth of plants. Soil acidity can be attributed to many variables in the environment such as high acidic rainfall, use of inorganic fertilizers and oxidative weathering. However, in agricultural landscapes such as western Kenya where this study was conducted, excess use of fertilizer can be the major contributor to low soil PH recorded.
The higher the concentrations of hydrogen ions held through the exchange of complex soil processes in relation to base cation concentration, the more acidic the soil sample becomes. For example, some inorganic nitrogenous fertilizers contain ammonium ions (NH
4+) which during nitrification into NO
3- is accompanied with the production of hydrogen ions released into the soil. Due to continuous farming and soil exhaustion, many large scale famers in the study have resorted to periodic application of inorganic fertilizers [
47]. Therefore high application of inorganic fertilizers result in enhanced production of hydrogen ions thus low soil PH. This explains the lower soil pH values recorded under maize and sugarcane cropping systems (
Figure 2). The mineralization and transfer of the hydrogen ions is accelerated by the high rainfall experienced in the study area. In the study area, there is infrequent application of inorganic fertilizers in the orchards and coffee farms. Low production of hydrogen ions thus leads to relatively higher soil PH compared to other cropping systems (
Figure 2). Under maize cropping systems, there is annual land tillage which facilitates leaching of base cations to lower soil layers leaving H
+ and Al
3+ which are responsible for high acidity [
56]. Under sugar cane cropping systems, there is regular application of inorganic fertilizers to increase yields. Fertilizer residues, coupled with high mineralization of N under cane canopies increase H+ loads hence lowered PH. Contrastingly the shrub lands in the study area that were considered pristine and less disturbed equally recorded lower PH implying acidity. Similarly the pasture land with the paddocks recorded lower PH. The acidity of soil samples from the pasture land and shrub land areas can attributed to the presence of large deposits of organic matter/litter from plan leaves, decomposition and mineralization of which is accompanied with hydrogen ions production.
Soil EC is a measure of the availability of ions in a soil sample, thus convey an electric current. It is another important soil characteristic that influences plant growth. EC is associated by the concentration of dissolved ions in soil solution such as Na
+, K
+, Mg
2+,Ca
2+, Cl
- , SO
42−, HCO
3− and CO
32− [
55]. The higher the concentration of dissolved ion in a solution, the higher the EC of the soil sample. However, it is important to note that Na
+, K
+, Mg
2+ and Ca
2+ cations are basic. Increase in their concentration is therefore accompanied by a rise in PH. This explains the negative correlation between soil pH and EC (r =-0.510; p<0.05) as shown in
Table 3. The low EC observed in the shrub land area where there were no agricultural practices can be explained by the podological factors. Much of the hydrogen ions that lowered the PH in these locations could have been from pedologic processes as opposed to anthropogenic sources. Additionally, the pristine shrub lands where sampling was done for control purposes were not fully vegetated. The exposure of soil to the heavy rainfall experienced in the study are could possibly facilitate heavy leaching of the exchangeable base cations leading to lower PH. Within the coffee and grass cropping systems, the high EC could be attributed low use of inorganic fertilizers as coffee and grass do not require regular fertilizer application. The concentration of base cations at these sites are therefore relatively higher (
Figure 2).
Soil Organic Carbon is a measure of the amount of carbon contained in the soil organic matter. It is an important parameter that aids understanding of soil fertility [
58]. Understanding soil organic matter requires a combination of various factors such as soil type, vegetation cover and climate. This parameter has a very close relationship with land use and land cover dynamics. This has made soil quality degradation due to inappropriate cropping one of the recent developmental challenges that has attracted global attention [
59]. For example, in arable lands, soil organic matter content has been found to be lower compared to forested areas or natural grasslands. This is because routine harvesting reduces deposition of organic materials. This explains the low TOC recorded under maize cropping systems (
Figure 5). Continuous clearing of land exposes the soil to erosion that minimizes organic matter input and nutrient accumulation hence low soil organic matter content. Under sugar cane, coffee and grass cropping systems, the ground surfaces are covered for relative longer periods with continuous litter deposition. The high organic matter concentrations at these sites increase TOC. This further explains the TOC trend observed in
Figure 5. Decreased SOM and nutrient levels have direct impacts on soil productivity, biodiversity, buffering capacity, cation exchange capacity and infiltration. Soil organic matter constitutes all decomposed, partly decomposed and undecomposed organic materials from plant and animal origin within the soil [
60]. This parameter is one of the key indicators of soil quality which is central to agricultural productivity. Enhancement of soil organic matter content provides a favourable environment within the soil subsystem hence better crop yields [
60]. High levels of soil organic matter content improves soil water holding capacity, reduces soil erosion while enhancing plant nutrient retention [
60].
4.2. Soil Heavy Metal Pollution due to Agriculture
Soil is considered as one of the most basic resources on which the lives of plants, animal and humans depend [
61]. Soil pollution, denoting the contamination of the soil medium with substances that impair the survival of soil dwelling organisms and even humans, still remains a hidden danger as it cannot be visually observed [
61]. Due to the rapid industrialization and urbanization trajectories realized in the 20
th century, agricultural soil contamination through heavy deposition has been a global concern in both developed and developing countries [
59]. These metals and metalloids such as Mercury, Silver, Copper, Iron, Lead, and Cadmium [
6] when present in the environment above the background concentrations, pose potential health problems to plants, animals and humans. Their contamination is one of the factors that restrict agricultural productivity and compromises food safety [
62]. Their toxicity risks in different environmental compartments is complicated by the fact that most of them are non-biodegradable and bio cumulative within ecosystems. They therefore persist in biological systems and have the potential of being transferred along trophic levels can be toxic to plants, animals and humans [
63]. This is why currently, heavy metal contamination in agricultural soils and crops has attracted worldwide attention [
64].
Under normal circumstances, these metals occur naturally in the environment but at very low concentrations/background concentration [
3,
7,
44]. However, the rate at which these elements are released naturally in the soil depends on the chemical composition of the parent rock and the prevailing climatic and biotic factors that mediate pedologic and geologic process through which associated with heavy metal exudation [
65]. This explains why even non cultivated sites in the study area also recorded heavy metal residues (
Table 1). It further explains the observed spatial variation in heavy metal concentrations in soils collected from control, sites in the study area. However, the observed rise in heavy metal concentration in soils under maize, sugarcane, and orchard cropping systems area can be attributed to anthropogenic influxes that include agriculture, combustion of fossil fuel and agriculture. [
66] observed that soils under corn field production were slightly contaminated with lead (22–100 mg/kg), copper (31–64 mg/kg), and nickel (22–76 mg/kg) and moderately contaminated with zinc (112–635 mg/kg). Maize production cropping systems are hence more prone to soil heavy metal contamination.
Within the study area, there are low levels of industrialization, mining, transportation systems and human/industrial waste disposal. Most of the contamination is therefore attributable to agricultural sources. In many parts of the world, many empirical studies have documented heavy metal influxes in agricultural soils due to application of various classes of agrochemicals such as fertilizers and pesticides [
6,
67,
68]. High application of inorganic fertilizers such as lime, phosphatic, nitrate and potash fertilizers has been found to contribute to elevated levels of Cromium, Cadmium, Manganese, Zinc, Copper, Lead and Nickel [
6]. This explains the high mean levels of Mercury, Copper and Zinc recorded under maize and sugarcane cropping systems in the study area (
Table 1). With the introduction of fertilizer subsidy under Agricultural Sector Support Programme and other county government initiatives, most farmers in the study area have embraced the use of inorganic fertilizers due to the perceived high yields [
47]. This finding concurs with that of [
44] who reported that top soil samples collected from Nzoia sugarcane nucleus showed 42.38 mg/Kg, 59.12 mg/Kg, 116.27 mg/Kg and 409.84 mg/Kg of Cr, Pb, Cu, Zn and Fe, respectively. The study concluded that within the sugarcane farms, the heavy metal concentrations were above the international standards. These inorganic fertilizers re applied by farmers during planting and later for top dressing to boost productivity. [
33] reported that mean concentrations of Pb, Cr, Hg, As, and Se in soils sampled from cultivated areas exceeded the background values of Guizhou Province, China, by 1.12, 1.28, 2.36, 1.27, and 2.4 times, respectively.
Excess fertilizer residues remain within the soil ecosystem increasing soil acidity. This explains why relatively lower soil pH was recorded under maize and sugarcane cropping systems while grassland and control sites recorded relatively higher PH levels (
Figure 2). The mineral fertilizers contain traces of heavy metals such as Pb, Zn and Cd. As fertilizer application is intensified, accumulation of heavy metals in the soil rises. This is why high NPI value of 11.303 was observed within the maize cropping system with respect to cadmium (
Table 3).This finding concurs with [
69] that found out that even though soils sampled from orchards did not have heavy metal pollution threats with respect to Cu, Cr, Zn, Hg and Zn, 10.0% of the soil samples collected from the orchards were under threat from cadmium pollution with PI≥1. Even though cadmium is one of the non-essential plant elements, it is quite ubiquitous in the environment with its sources associated with human activities such as disposal of urban wastes, mining, metal manufacturing and use of phosphate fertilizers. Soil contamination through cadmium saturation may have adverse effects on plant physiology and possible transference to other trophic levels [
70]. Increased cadmium concentrations inhibits absorption and translocation of essential plant nutrients and water while also exposes plants to oxidative damage.
In orchards there is little routine application of fertilizers during the growing seasons compared to maize and sugarcane. Soils sampled from the orchards therefore recorded heavy metal concentrations that that are intermediate compared to maize cropping systems and the control sites. In china, empirical analysis found that even though soil heavy metal pollution in agricultural soils irrigated with sewage in Wuqing, Tianjin was mild except for Cd and Pb, PCA and PMF showed that soil parental material contributed significantly to Ca, Mg (23.46%) while agricultural activities contributed (29.97%) of Pb, Cu, and Zn pollution [
71]. [
69] also observed that concentration of Cr, Cu, Cd, Hg and Pb in orchard soils did not pose any soil pollution threats with NPI ≤ 1. However, 10.0% of the soil samples were under cadmium pollution. Besides the use of inorganic fertilizers, different types of pesticides including herbicides, fungicides and insecticides have also been found to contain traces of heavy metals such as Zinc, Copper, Nickel, Lead, Cadmium, Chromium, Arsenic and Mercury [
68,
72,
73]. With repeated application of these pesticides in large scale farms in the study area, there is continued deposition of heavy metal traces in agricultural soils posing potential ecological risks [
47].
Combined heavy metal residues from inorganic fertilizers and pesticides in these large scale farms therefore lead to elevated levels of the analyzed heavy metals in the soil (
Table 1). This is why higher levels of heavy metals were recorded under cultivated areas compared to the grassland and control plots. In the Wanshan Mining District of China, [
66] reported that soil under corn cropping system were moderately contaminated with lead (22–100 mg/kg), copper (31–64 mg/kg), and nickel (22–76 mg/kg) and moderately contaminated with zinc (112–635 mg/kg). Although the use of organic manures has been advocated for by environmentalists due to the perceived minimal environmental impacts, previous works have shown that application of biosolids and manures can lead to accumulation of Zinc, Nickel, Copper, Lead, Cadmium, Cromium and Mercury in agricultural soils [
6,
36].