Contributions of soil chemical and physical properties in the dynamics of soil quality in the southern Cameroon plateau shifting agricultural landscape

Soil quality results from combination of chemical, physical and biological characteristics; according to ecosystems, some of these aspects become dominant. This Study was carried out on soils under 08 land cover types in the southern Cameroon ((bare soil with burned vegetation (FR1), bare soil with...

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Main Authors: Nyeck, B., Mbogba, M.N., Njilah, I.K., Yemefack, Martin, Bilong, P.
Format: Journal Article
Language:Inglés
Published: International Formulae Group 2018
Subjects:
Online Access:https://hdl.handle.net/10568/97643
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author Nyeck, B.
Mbogba, M.N.
Njilah, I.K.
Yemefack, Martin
Bilong, P.
author_browse Bilong, P.
Mbogba, M.N.
Njilah, I.K.
Nyeck, B.
Yemefack, Martin
author_facet Nyeck, B.
Mbogba, M.N.
Njilah, I.K.
Yemefack, Martin
Bilong, P.
author_sort Nyeck, B.
collection Repository of Agricultural Research Outputs (CGSpace)
description Soil quality results from combination of chemical, physical and biological characteristics; according to ecosystems, some of these aspects become dominant. This Study was carried out on soils under 08 land cover types in the southern Cameroon ((bare soil with burned vegetation (FR1), bare soil with unburned vegetation (FR), Chromolaena odorata fallow (JC), bush ligneous fallow (JR), secondary forest (FS), primary forest (FC), Gilbertiodendron dewevei forest (FG), and raffia forest (RA) to assess the contributions of soil chemical and physical indicators into global soil quality index (IQSg). Topsoil samples were analyzed for physico-chemical characterizations and IQSg computed. Multiples statistical tests were used to compare the contribution of soil quality indicators and to select those that contributed the most in IQSg. Thus, under FR1, FC, FG and RA, IQSg was relatively high and the main contributors were chemical, estimated at more than 70%. Under FR, IQSg remains high and chemical contribution predominant (65%) on physical (35%). On the contrary, under fallows, IQSg is relatively low; these two types of contributions are nearly equivalents. Thus, the main indicators helping to assess IQSg in lower cost, contributing significantly to global soil quality and representatives of indicators are: organic matter (MO), pHw, and C/N ratio. The difference in contribution is due to the types of cultural practices, quality and quantity of MO brought by land cover types and topographical position.
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spelling CGSpace976432024-04-12T20:35:48Z Contributions of soil chemical and physical properties in the dynamics of soil quality in the southern Cameroon plateau shifting agricultural landscape Nyeck, B. Mbogba, M.N. Njilah, I.K. Yemefack, Martin Bilong, P. soil land cover shifting cultivation fallow soil chemicophysical properties Soil quality results from combination of chemical, physical and biological characteristics; according to ecosystems, some of these aspects become dominant. This Study was carried out on soils under 08 land cover types in the southern Cameroon ((bare soil with burned vegetation (FR1), bare soil with unburned vegetation (FR), Chromolaena odorata fallow (JC), bush ligneous fallow (JR), secondary forest (FS), primary forest (FC), Gilbertiodendron dewevei forest (FG), and raffia forest (RA) to assess the contributions of soil chemical and physical indicators into global soil quality index (IQSg). Topsoil samples were analyzed for physico-chemical characterizations and IQSg computed. Multiples statistical tests were used to compare the contribution of soil quality indicators and to select those that contributed the most in IQSg. Thus, under FR1, FC, FG and RA, IQSg was relatively high and the main contributors were chemical, estimated at more than 70%. Under FR, IQSg remains high and chemical contribution predominant (65%) on physical (35%). On the contrary, under fallows, IQSg is relatively low; these two types of contributions are nearly equivalents. Thus, the main indicators helping to assess IQSg in lower cost, contributing significantly to global soil quality and representatives of indicators are: organic matter (MO), pHw, and C/N ratio. The difference in contribution is due to the types of cultural practices, quality and quantity of MO brought by land cover types and topographical position. 2018-04 2018-10-11T11:04:19Z 2018-10-11T11:04:19Z Journal Article https://hdl.handle.net/10568/97643 en Open Access International Formulae Group Nyeck, B., Mbogba, M.N., Njilah, I.K., Yemefack, M. & Bilong, P. (2018). Contributions of soil chemical and physical properties in the dynamics of soil quality in the southern Cameroon plateau shifting agricultural landscape. International Journal of Biological and Chemical Sciences, 12(2), 1042-1056.
spellingShingle soil
land cover
shifting cultivation
fallow
soil chemicophysical properties
Nyeck, B.
Mbogba, M.N.
Njilah, I.K.
Yemefack, Martin
Bilong, P.
Contributions of soil chemical and physical properties in the dynamics of soil quality in the southern Cameroon plateau shifting agricultural landscape
title Contributions of soil chemical and physical properties in the dynamics of soil quality in the southern Cameroon plateau shifting agricultural landscape
title_full Contributions of soil chemical and physical properties in the dynamics of soil quality in the southern Cameroon plateau shifting agricultural landscape
title_fullStr Contributions of soil chemical and physical properties in the dynamics of soil quality in the southern Cameroon plateau shifting agricultural landscape
title_full_unstemmed Contributions of soil chemical and physical properties in the dynamics of soil quality in the southern Cameroon plateau shifting agricultural landscape
title_short Contributions of soil chemical and physical properties in the dynamics of soil quality in the southern Cameroon plateau shifting agricultural landscape
title_sort contributions of soil chemical and physical properties in the dynamics of soil quality in the southern cameroon plateau shifting agricultural landscape
topic soil
land cover
shifting cultivation
fallow
soil chemicophysical properties
url https://hdl.handle.net/10568/97643
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