Physical properties of three soils in southern Nigeria

To determine their physical characteristics, we studied two Alfisols and an Ultisol in southern Nigeria. The soils are formed over different parent materials. Moisture retained at saturation, 0.1, and 0.3 bar suctions was significantly correlated with available water-holding capacities. The regressi...

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Autores principales: Mbagwu, J., Lal, R., Scott, T.W.
Formato: Journal Article
Lenguaje:Inglés
Publicado: 1983
Materias:
Acceso en línea:https://hdl.handle.net/10568/177237
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author Mbagwu, J.
Lal, R.
Scott, T.W.
author_browse Lal, R.
Mbagwu, J.
Scott, T.W.
author_facet Mbagwu, J.
Lal, R.
Scott, T.W.
author_sort Mbagwu, J.
collection Repository of Agricultural Research Outputs (CGSpace)
description To determine their physical characteristics, we studied two Alfisols and an Ultisol in southern Nigeria. The soils are formed over different parent materials. Moisture retained at saturation, 0.1, and 0.3 bar suctions was significantly correlated with available water-holding capacities. The regression models depicting the relationships between moisture equilibria and the sand, clay, and organic carbon contents had high and significant coefficients of determination and indicate that variations in soil particle size fractions and organic carbon contents accounted for over 70 percent of the variability in moisture retanined at different suctions. Significant correlation exists between organic carbon and macroporosity (r = 0.63*]) and saturated hydraulic conductivity (r = 0.88**]). Soil bulk density is negatively correlated with the organic matter content. Similarly, the percentage of clay is negatively correlated with macroporosity (r = —0.75**]) and with saturated hydraulic conductivity (r = —0.76**]), and the percentage of sand is positively correlated with these properties, with r values of 0.62**] and 0.67**], respectively.
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spelling CGSpace1772372025-11-11T11:07:22Z Physical properties of three soils in southern Nigeria Mbagwu, J. Lal, R. Scott, T.W. soil soil moisture correlation organic carbon To determine their physical characteristics, we studied two Alfisols and an Ultisol in southern Nigeria. The soils are formed over different parent materials. Moisture retained at saturation, 0.1, and 0.3 bar suctions was significantly correlated with available water-holding capacities. The regression models depicting the relationships between moisture equilibria and the sand, clay, and organic carbon contents had high and significant coefficients of determination and indicate that variations in soil particle size fractions and organic carbon contents accounted for over 70 percent of the variability in moisture retanined at different suctions. Significant correlation exists between organic carbon and macroporosity (r = 0.63*]) and saturated hydraulic conductivity (r = 0.88**]). Soil bulk density is negatively correlated with the organic matter content. Similarly, the percentage of clay is negatively correlated with macroporosity (r = —0.75**]) and with saturated hydraulic conductivity (r = —0.76**]), and the percentage of sand is positively correlated with these properties, with r values of 0.62**] and 0.67**], respectively. 1983-07 2025-10-21T12:06:54Z 2025-10-21T12:06:54Z Journal Article https://hdl.handle.net/10568/177237 en Limited Access application/pdf Mbagwu, J., Lal, R. & Scott, T.W. (1983). Physical properties of three soils in southern Nigeria. Soil Science, 136(1), 48-55.
spellingShingle soil
soil moisture
correlation
organic carbon
Mbagwu, J.
Lal, R.
Scott, T.W.
Physical properties of three soils in southern Nigeria
title Physical properties of three soils in southern Nigeria
title_full Physical properties of three soils in southern Nigeria
title_fullStr Physical properties of three soils in southern Nigeria
title_full_unstemmed Physical properties of three soils in southern Nigeria
title_short Physical properties of three soils in southern Nigeria
title_sort physical properties of three soils in southern nigeria
topic soil
soil moisture
correlation
organic carbon
url https://hdl.handle.net/10568/177237
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AT lalr physicalpropertiesofthreesoilsinsouthernnigeria
AT scotttw physicalpropertiesofthreesoilsinsouthernnigeria