利用入渗速率预测Imo国土壤侵蚀。

G. Obiechefu, P. N. Egbuikwem, K. Emerson
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引用次数: 1

摘要

对尼日利亚伊莫州五种不同土壤类型的土壤侵蚀和入渗速率/能力进行了调查/测量,即:罗迪克硝硝土、中性硝硝土、岩石层土、中性硝硝土和中性硝硝土。测定了这些土壤在长时间湿润后的最终入渗速率。在已知的降雨强度和径流速率下,还测量了这些土壤组的土壤侵蚀量。测量了土壤的一些物理性质(容重、孔隙度、渗透性和粒度分布)。比较了不同土壤类型的入渗能力和土壤侵蚀量。5个土壤组中,Rhodic硝灰的入渗速率为132 ~ 820mm/hr, Eutric硝灰的入渗速率为5.64 ~ 450mm/hr。Dystric型ferrasol的渗透速率为82.8 mm/hr ~ 192mm/hr。岩石层的入渗速率为43.2 ~ 180mm/hr。Eutric凝胶的范围为46mm/hr到276mm/hr。Rhodic、Eutric nitosols、Lithosols、Eutric gleysols和Dystric ferrasols的土壤侵蚀(含沙量)平均值分别为150g/l、280g/l、750g/l、1008g/l和1250g/l。研究结果表明,伊莫国土壤入渗能力越强,土壤侵蚀程度越低。因此,这些土壤的入渗能力可用于评估或预测伊莫国土壤的侵蚀速率。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Prediction of Soil Erosion of Imo State Soils by Their Infiltration Rates.
: The soil erosion and infiltration rates/capacities of five different soil groups in Imo State Nigeria namely: Rhodic ferrasols, Eutric nitosols, Lithosols, Eutric gleysols and Dystric ferrasols were investigated / measured. The final infiltration rates of these soils after prolonged wetting were determined. The amount of soil erosion from these soil groups under known rainfall intensities and runoff rates were also measured. Some soil physical properties of the soils (bulk density, porosity, permeability and grain size distribution) were also measured. The infiltration capacities of the soil groups and the amount of soil erosion from the soil groups were compared. The infiltration rates from these five soil groups ranged from 132mm/hr to 820mm/hr for the Rhodic ferrasols, while that of Eutric nitosols ranged from 5.64mm/hr to 450mm/hr. The infiltration rates for the Dystric ferrasols ranged from 82.8 mm/hr to 192mm/hr. The infiltration rates for the Lithosols ranged from 43.2 mm/hr to 180mm/hr. The range for the Eutric gleysols was from 46mm/hr to 276mm/hr. The erosion from the soils (sediment concentration) were in the average of 150g/l, 280g/l, 750g/l, 1008g/l, and 1250g/l for the Rhodic ferrasols, Eutric nitosols, Lithosols, Eutric gleysols and Dystric ferrasols respectively. From this study, the soils of Imo State with higher infiltration capacities had lower soil erosion. Therefore, the infiltration capacities of these soils may be used to assess or predict the erosion rates of Imo State soils.
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