Effect of Land Use and Slope Position on Infiltration Characteristics on Sandstone-Derived Soils of Southern Nigeria

U. Utin
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Abstract

A study of some soil properties that influence infiltration under different land use types and slope positions in sandstone-derived soils was carried out in Akwa Ibom State, Southern Nigeria. Soil samples were collected in triplicate for laboratory analyses and infiltration tests were conducted using the double ring infiltrometer method. Analysis of variance, correlation and regression analyses were used to assess the data Oil Palm Plantation and Fallow Land increased the organic matter content of the soil, reduced bulk density, increased the soil porosity and aggregate stability over Continuously Cultivated Land. Downslope soil movement caused the upper slopes to lose their clay and organic matter to the middle and lower slope soils. Initial infiltration rate, final infiltration rate, cumulative infiltration, sorptivity and transmissivity varied highly across the studied locations but were not significantly (P ≤ 0.05) affected by land use, slope position and their interactions. Apparently higher infiltration rates were observed in all slope positions under Oil Palm Plantation and Fallow Land as a result of their apparently higher clay contents, total porosity, mean weight diameter, saturated hydraulic conductivity and organic matter contents over those of Continuously Cultivated Land. Heavier organic matter input will help to modify the upper slope soils for increased infiltration rates. Plantation agriculture should be adopted and continuous cultivation discouraged to increase water infiltration on sloppy terrains of the study area. Contribution/Originality: This study is one of very few studies which have investigated the combined effect of land use and slope position on infiltration characteristics and has demonstrated that infiltration tend to increase towards the lower slope position of vegetated lands compared to upper slopes rendered bare by continuous cultivation.
土地利用方式和坡位对尼日利亚南部砂岩土入渗特性的影响
在尼日利亚南部的阿夸伊博姆州进行了一项研究,研究了在不同土地利用类型和斜坡位置下影响砂岩土入渗的一些土壤特性。土壤样品一式三份进行实验室分析,采用双环渗透计法进行入渗试验。采用方差分析、相关分析和回归分析对数据进行了评价,结果表明:油棕种植和休耕增加了连续耕地土壤有机质含量,降低了容重,增加了土壤孔隙度和团聚体稳定性。下坡土壤运动导致上坡的粘土和有机质流失到中下坡土壤中。初始入渗速率、最终入渗速率、累积入渗速率、吸收率和透过率在不同研究地点间差异较大,但受土地利用方式、坡位及其相互作用的影响不显著(P≤0.05)。油棕地和休耕地各坡位土壤的入渗速率均明显高于连作地,其粘土含量、总孔隙度、平均重径、饱和导水率和有机质含量均明显高于连作地。较重的有机质输入将有助于改善上部坡面土壤,增加入渗速率。研究区泥泞地形应采用人工林农业,不提倡连作,以增加水分入渗。贡献/独创性:本研究是为数不多的研究土地利用和坡位对入渗特性的综合影响的研究之一,研究表明,与连续耕作导致裸露的上坡相比,植被覆盖的土地入渗倾向于向坡位下部增加。
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