Abstract

This study was carried out in order to assess soil structural stability under different land uses using predictive indices. Different land uses of forest land, cattle paddock, fallow land and continuously cultivated farmland were carefully identified within Abakaliki agroecology. Auger and core soil samples were collected at five sampling points using free survey technique in each land use. Core soil samples were used to determine predictive indices of bulk density, total porosity and hydraulic conductivity. Auger soil samples were bulked and used for determination of mean weight diameter (MWD), aggregate stability, dispersion ratio and particle size distribution. Data obtained were subjected to coefficient of variation (CV) analysis and standard deviation. Results showed that sand and clay fractions had little variation (%CV<7-8) but silt fraction varied moderately (%CV >28). Furthermore, bulk density, mean weight diameter, aggregate stability and hydraulic conductivity were highly varied (%CV >112-245), total porosity had moderate variation (%CV >30) and dispersion ratio, high variation (%CV >80), respectively. The different land uses are generally rated according to their performance in their structural stability using the predictive indices as forestland>cattle paddock>fallow land>farmland. It is recommended that the practice of forestry, grazing, fallowing and other management practices which encourage formation and stabilization of soil structural stability be adopted for sustenance of higher soil productivity.

Highlights

  • IntroductionSoil structural stability is a potential indicator for wide variety of choices to which it is used for ranging from agricultural to engineering considerations

  • Soil is fundamental and basic resource for agricultural practice

  • Percent sand fraction was highest under cattle paddock and slightly varied from that obtained in forest land

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Summary

Introduction

Soil structural stability is a potential indicator for wide variety of choices to which it is used for ranging from agricultural to engineering considerations. This is because the structural stability of soil influences its nutrient retention and supply, water storage and transmission, aeration propensity, strength and trafficability and capacity to support foundations (Obi, 2000). The primary purpose of soil is to hold and provide water and nutrients to plants, permit gas exchanges to and from their roots, as well as mechanical support. As corroborated by Ekpe (2002), soil structural stability strongly correlates with fertility, infiltration rate, flow of air or water and degree of ramification of network of roots. In assessing of soil structural stability the two major factors of interests are size, stability of aggregates, shaping or orientation of the aggregates (Ekpe, 2002)

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