Krogba Yves Nangah, Yao
Kouman Nestor Kouakou, Kouamé Antoine
N’Guessan, and Albert Yao-Kouame, from the institute of the Côte d’Ivoire. Wrote
a research article about, Climate Shapes Manganese-Rich Soils in Côte d’Ivoire.
Entitle, Chemical variability of climate sequence of manganesiferous soil
derived from volcano-sedimentary materials in Côte d’Ivoire. This research
paper published by the Journal of Biodiversity and Environmental Sciences |JBES. an open access scholarly research journal on Environmental Sciences.
under the affiliation of the International Network For Natural Sciences|
INNSpub. an open access multidisciplinary research journal publisher
Abstract
Knowledge of limiting factors is an important prerequisite for ensuring efficient agricultural production, agronomically, economically and environmentally. The objective of this study is to determine the basic physicochemical properties of manganiferous soils derived from volcano-sedimentary material under different climatic facets. Three sites on different climatic facets were prospected. An analysis of soil samples was carried out in order to determine the physicochemical parameters (water pH, exchangeable bases, CEC, organic matter, phosphorus). The results show that soils are acidic with pH <5.5. The available phosphorus is better supplied with contents greater than 20mg.kg-1, while the complex is strongly desaturated. This study has highlighted the existence of a marked climatic gradient for organic matter and CEC. These elements follow a decreasing trend, from the North (Savannah zone and Sudanese climate) to the South (forest zone and Attiean climate). The forest area (Guitry) in Attiean Climate remains better enriched in bases compared to the other zones studied. The influence of microclimatic conditions on pedogenesis is important in the individualization of Cambisols.
Introduction
The soil is the
physical and nutritive support of living beings on the surface of the
continents, and, as a result, the life support of man. Although the man is in
permanent contact with the ground, it is still, in many ways, a black box whose
operation is still only partially known. The floors are constantly changing
under the combined action of the flow of materials and energy, which, when
applied to a parent material, gradually transforming the primary minerals into
secondary components (Chadwick and Chorover 2001; Cornu, 2005). These permanent
interactions give the soil a large spatial and temporal variability, which is
difficult to grasp. This complexity characterizes natural environments and
makes their study delicate.
Manganese soils in Côte
d'Ivoire are mainly formed on volcano-sedimentary complexes. These
volcanosedimentary complexes give rise to browned soils (Cambisols) (Perraud,
1971), and are under different climatic facets. The study of these soils has
been limited to morphological characterization and the study of metallic trace
elements (Nangah et al., 2019). This does not allow to apprehend the
physicochemical environment that reigns in these soils. In addition, they also
do not guide decision-making on the prevention of potential risks and the adoption
of adequate cropping systems by the majority of the population, which is rural.
However, failure to take into account the physico-chemical constraints of soils
is detrimental to the exploitation of these, because, certain soil parameters
play a preponderant role in the management of plant nutrition, and an adequate
supply of nutrients. nutrients depend on their optimization (Troeh and
Thompson, 2005). Knowledge of limiting factors is therefore an important
prerequisite for ensuring efficient agronomic, economic and environmental
agricultural production from reliable diagnoses (Dahnke and Olson 1990, Parent
and Dafir 1992).
The objective of this
study is to determine the basic physicochemical properties of manganese soils
derived from volcano-sedimentary material under different climatic facets.
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