尼日利亚内陆山谷萨瓦系统土壤的物理化学和地球化学性质

C. I. Alarima, M. Busari, J. Awotunde, O. O. Olaniyi, T. Masunaga, T. Wakatsuki
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摘要

研究了尼日利亚沙华下土壤的物理化学和地球化学性质。结果表明,沙洼下土壤主要为砂质壤土-砂质粘壤土,发生酸性反应,钙、镁、钾和钠的交换性较低。有效磷、SiO2、S、总氮和总碳均缺乏,而SiO2、Al2O3和Fe2O3占总元素组成的主导地位,累计平均占96.16%。除总元素TiO2和K2O平均值>1%外,MnO、MgO、CaO、Na2O和P2O5平均值均<1%。沙化作用下土壤表现为中度至极端风化程度,大部分土壤属于极端风化类型。随着极端程度的风化,土壤中碱性阳离子等可移动物种的迅速流失迫在眉睫,这可能是本研究结果的原因。因此,建议结合保守的农业实践。
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PHYSICO-CHEMICAL AND GEOCHEMICAL PROPERTIES OF SOILS UNDER SAWAH SYSTEM OF INLAND VALLEYS IN NIGERIA
This study investigated the physico-chemical and geochemical properties of soils under sawah in Nigeria. It was found that soils under sawah were majorly sandy loam to sandy clay loam having acidic reactions, low exchangeable Ca, Mg, K and Na. These soils were deficient in available P, SiO2, S, Total Nitrogen and Total Carbon while SiO2, Al2O3 and Fe2O3 dominated total elemental composition, accounting for a cumulative average of 96.16%. Except total elemental TiO2 and K2O which showed average values >1%, MnO, MgO, CaO, Na2O and P2O5 showed average values <1%. Soils under sawah exhibited intermediated to extreme weathering degree with majority of the soil sampled falling into the category of extreme weathering. With extreme degree of weathering, rapid loss of mobile species such as basic cations from soil is imminent which may account for the results observed in this study. Thus, combination of conservative agricultural practices is recommended.    
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