EVALUATION OF THE PHYSICO-CHEMICAL AND MORPHOLOGICAL PROPERTIES OF AN EXPOSED SOIL PROFILE IN AN EXCAVATED ACRISOL, SOUTHEAST NIGERIA

Nnabude, P.C., O. A.O, Ijeoma, E.O., M. C.O.
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Abstract

Increased population density has led to a lot of pressure on the limited natural/land resources of south-eastern Nigeria. This includes the need for laterite, sand, kaolin, gravel and clay for buildings, backfills and road construction. This has led to extensive unmoderated excavation of these resources, particularly in Anambra state. The excavation has in turns, culminated in increased intensity of land degradation in the state, underscoring the need to characterize and evaluate the land use potentials of such sites to better understand the nature of the soils and the impacts of the attendant land use. Samples were collected from the different horizons of the profile to evaluate the physical, chemical and morphological properties of the soils. Coefficient of variation was used to measure the soil variability within the profile. Land capability class was determined, which informed the land use and management recommendations. The results show that the soil is very deep (>21.5m). The soil texture ranged from sandy clay loam to sandy. Infiltration rate and saturated hydraulic conductivity decreased by up to 300 to 560 % with excavation. The soils were strongly acidic; organic carbon and total nitrogen was low but highly variable; Al, H, Ca, Mg, K, Na, and phosphorus were moderately variable while pH, CEC and base saturation (BS) were the least variable. The land capability class was IIIes. Given the evidence of erosion and preponderance of erodible Nanka sands in the subsoil, the site should be reclaimed as soon as the mining activities are discontinued.
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尼日利亚东南部发掘的阿克里索尔暴露土壤剖面的理化和形态特征评价
人口密度的增加给尼日利亚东南部有限的自然/土地资源带来了很大的压力。这包括建筑、回填和道路建设所需的红土、沙子、高岭土、砾石和粘土。这导致了对这些资源的大量无节制的挖掘,特别是在阿南布拉州。挖掘反过来又加剧了该州土地退化的强度,强调有必要描述和评估这些地点的土地利用潜力,以便更好地了解土壤的性质和随之而来的土地利用的影响。从剖面的不同层位采集样品,评价土壤的物理、化学和形态特征。变异系数用于测量剖面内的土壤变异。确定了土地能力等级,并据此提出了土地使用和管理建议。结果表明:土层很深(>21.5m);土壤质地从砂质粘土壤土到砂质。随着开挖,入渗速率和饱和水力导电性降低了300% ~ 560%。土壤呈强酸性;有机碳和全氮含量较低,但变化较大;Al、H、Ca、Mg、K、Na和磷变化中等,pH、CEC和碱饱和度(BS)变化最小。陆地能力等级是IIIes。鉴于有证据表明底土中有侵蚀和大量可侵蚀的南卡砂,一旦采矿活动停止,该地点应立即进行复垦。
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