Land use induced changes in cation anion balance of southern laterite soils of Kerala
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Date
2026
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Department of Soil Science and Agricultural Chemistry, College of Agriculture,Vellayani
Abstract
The study entitled “Land use induced changes in cation anion balance of southern
laterite soils of Kerala” was conducted in the Department of Soil Science and Agricultural
Chemistry, College of Agriculture, Vellayani during 2024-2025 with the objective of
assessment of variability in the distribution of cations and anions as influenced by land use
systems and seasons in the southern laterite (AEU 8) of Kerala. Georeferenced soil samples
were collected from twenty different locations of four major land use systems (LUS) of the
southern laterite soils of Kerala viz., banana, coconut, vegetable and uncultivated fallow
lands, from the surface (0–15 cm) and sub-surface (15–30 cm) layers during both the pre-
monsoon and post-monsoon seasons. The collected soil samples were analysed for physical
properties, electrochemical properties, biological properties and cation- anion
concentrations.
An incubation experiment was conducted with the samples collected from the pre
monsoon season to find out the effect of moisture content on cation anion concentration.
During the incubation period, the concentrations of cations viz., NH₄⁺-N and Fe²⁺ displayed
a pronounced decrease with the reduction in moisture content and the values recorded were
statistically significant. Among the anions, NO₃⁻, SO₄²⁻ and PO₄³⁻ exhibited significant
reduction with decrease in moisture content.
Out of the five locations of the banana, coconut, vegetable and fallow land use
systems, three were classified as sandy clay loam, one as silty clay loam and one as clay
loam in texture. No variation in texture was observed in the sub surface layers. During the
pre and post monsoon season in surface soil, significantly higher bulk density was noticed
in the samples from banana LUS (1.20 Mg m-3) which was on par with coconut and
uncultivated fallow LUS and lowest was observed in vegetable LUS (1.03 Mg m-3).
Coconut LUS showed the highest pH (5.67) at 0-15 cm depth for pre and post monsoon.
Significantly higher CEC (6.30 cmol(+) kg⁻¹) was recorded in the surface soils of coconut
land use system. Conversely, vegetable LUS registered the maximum AEC (0.719 cmol(–
) kg⁻¹) in surface. Irrespective of the season and depth, the uncultivated fallow land showed
the lowest values for pH, CEC and AEC.
Coconut LUS recorded the significantly higher contents of Ca²⁺ (298 and 268 mg
kg⁻¹, respectively), Mg²⁺ (98 and 78 mg kg⁻¹, respectively), Na⁺ (58 and 40 mg kg⁻¹,
respectively) and Mn²⁺ (33.00 and 35.83 mg kg⁻¹, respectively) during pre- and post-
monsoon seasons, with values generally on par with the vegetable LUS in surface soil.
Surface Cu²⁺ content was also highest in coconut soils (2.66 mg kg⁻¹) and was comparable
to banana and vegetable systems. Vegetable LUS showed significantly higher K⁺ (144.00
and 125.50 mg kg⁻¹, respectively) and NH₄⁺-N (34.72 and 52.08 mg kg⁻¹, respectively) in
surface and sub-surface. It also had higher Fe²⁺ (28.52, 18.34 mg kg⁻¹) and Al³⁺ (7.37, 7.84
mg kg⁻¹), along with the highest surface Cu²⁺ (2.66 mg kg⁻¹, on par with banana and
coconut) and consistently highest Zn²⁺ in both seasons. Uncultivated fallow land recorded
the lowest concentrations of Ca²⁺, Mg²⁺, Na⁺, K⁺, NH₄⁺-N, Fe²⁺, Al³⁺, Cu²⁺, Mn²⁺ and Zn²⁺
during both the pre- and post-monsoon seasons. Irrespective of the land use systems, the
concentration of cations tends to decrease with the depth.
Irrespective of the season, concentration of anions like nitrates (84.56 and 64.40 mg
kg⁻¹, respectively), sulphates (31.15 and 28.15 mg kg⁻¹, respectively) and silicates (29.69
and 32.54 mg kg⁻¹, respectively) were significantly higher in the surface soils of vegetable
LUS. MoO₄²⁻ content was also greater under this system, measuring 389.85 μg kg-1 in
surface pre and post monsoon and 350.10 μg kg-1 in sub surface pre and post-monsoon.
However, banana LUS recorded the highest PO₄³⁻ levels in both seasons in surface, with
18.97 mg kg⁻¹ in surface soil and 16.55 mg kg⁻¹ in sub surface soil. Similarly, BO₃³⁻
concentrations were highest in banana LUS, with values of 0.667 mg kg⁻¹ in surface soil
pre and post monsoon and 0.618 mg kg⁻¹ in sub surface pre and post-monsoon. Irrespective
of the land use systems, the concentration of anions tends to decrease with the depth.
Across the land use systems, CAB values remained positive which indicates surplus
of cations over anions implying a change in ionic balance in these systems, which may lead
to nutrient imbalances. The CAB values were in the order of coconut ˃ vegetable ˃ banana
˃ uncultivated fallow which signifies that CAB in soil is influenced by both soil and crop
characteristics. Proper soil management practices are essential to maintain CAB and to
optimize soil health and crop productivity.
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Keywords
Soil Science and Agricultural Chemistry
Citation
176877