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首页> 外文期刊>Environmental Monitoring and Assessment >Variation of soil properties under different landscape positions and land use in Hunkuyi, Northern Guinea savanna of Nigeria
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Variation of soil properties under different landscape positions and land use in Hunkuyi, Northern Guinea savanna of Nigeria

机译:尼日利亚北部北几内亚大草原不同景观地位下土壤性质的变异与土地利用

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摘要

The food insecurity problem in developing countries has been linked to rapid rates of soil loss and decline in fertility in tropical environments which are characterized by insidious topography. This study was conducted to assess the relationship between topographic positions, land use, and soil characteristics. Three slope classes were considered with six pedons; two on each slope position were opened, described, sampled, and analysed for morphological and physicochemical properties. The results showed that the soils were deep to very deep with drainage improving from HK1 soils (very poorly drained) to HK3 (well-drained). The mean sand fraction ranged between 320 and 740 g kg(-1), while bulk density had values between 1.20 and 1.80 M gm(-3.) The cation exchange capacity (CEC) of the soils with values from 5.6 to 10.4 cmol (+) kg(-1) was generally lower on the surface than the subsurface soils. The different landscape positions alongside variation in land use substantially influence variations in soil properties of the study area. The influence of topography was noticed for sand values and soil reaction (pH) along the slope, as mean pH values were significantly (P = 0.05) higher for HK1 compared with HK2 and HK3. Intensive cultivation of soils due to rainfed and irrigated land use on middle slope position (HK2) alongside its strong slope gradient resulted in significant variation in total exchangeable bases (TEB) ((P = 0.05), base saturation (P = 0.05), available P ((P = 0.01), and exchangeable Ca and Mg (P = 0.05).
机译:发展中国家的粮食不安全问题已与热带环境中的土壤丧失和生育率下降的快速率有关,其特征在于阴险地形。进行本研究以评估地形位置,土地利用和土壤特征之间的关系。用六个施行考虑了三个坡度课程;每个斜坡位置上的两个打开,描述,取样和分析和分析形态学和物理化学性质。结果表明,土壤深入深深地深入,引流从HK1土壤(沥干非常不良)到HK3(良好排出)。平均砂级分在320和740g kg(-1)之间,而散装密度在1.20和1.80mg(-3.)的阳离子交换能力(CEC)之间的价值为5.6至10.4 cmol( +)+)kg(-1)在表面上通常低于地下土壤。不同的景观位置沿着土地的变化以及基本上影响研究区域的土壤性质的变化。对于沿斜坡的砂值和土壤反应(pH)表示,地形的影响,与HK2和HK3相比,HK1的平均pH值显着(p& = 0.05)。由于中坡位置(HK2)越雨和灌溉土地使用引起的土壤栽培,其强斜率梯度伴随着总可交换碱(TEB)的显着变化((P = 0.05),基础饱和度(P

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