坡向和降雨强度对酸性降雨土壤渗透性的交互作用

hamzeh saeediyan, Hamidreza Moradi
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摘要

坡向和降雨强度对酸性降雨土壤渗透性的交互作用。环境科学,19(4):131-144。与酸性降水相比,Gachsaran地层表现出均匀性变化,在几乎所有三种浓度下均表现出对坡向和雨强的正向影响以及坡向和雨强的交互效应。此外,随着酸雨渗透土壤的量的增加,土壤孔隙度的增加,这种情况是由于这种污染对土壤的主要成分和洗涤土壤的结合。当然,Aghajari和Gachsaran地层中不同粘土量的坡向受土壤渗透性的影响比酸性降水的影响更大。不同有机质在斜坡主要坡面,特别是北部坡面和东部坡面的存在,造成了较为复杂的电荷变化情况,需要进一步研究来了解这一复杂机制。结论:总的来说,随着酸性程度的增加和渗透时间的延长,土壤的特性发生了变化,包括土壤的抵抗特性和承载能力,而土壤的抵抗特性和承载能力又由于粘土的含量和有机质的不同,导致酸性降水对土壤渗透性的影响更大。
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Interactive effect of slope aspect and rainfall intensity on soil permeability compared to acidic rainfalls
Interactive effect of slope aspect and rainfall intensity on soil permeability compared to acidic rainfalls. Environmental Sciences. 19(4): 131-144 sensitivity to soil permeability compared to acid rains. However, the Gachsaran formation showed uniformity changes compared to acidic precipitation and showed positive effects on slope aspect and rain intensity and interactive effect of slope aspect and rain intensity in almost all three concentrations. In addition, by increasing the amount of soil permeated with acid rains, the amount of soil porosity increased, this case was due to this type of contamination on the main ingredients of soil and washing soil bonds. Of course, slope aspect different amounts of clays in both Aghajari and Gachsaran formations, is more influenced by soil permeability than acidic precipitations. The existence of different organic matter in the main aspects of the slopes, especially in the northern and eastern slope aspects, creates a more complex situation in electrical charge changes, which necessitates further research to understand this complex mechanism. Conclusion: In general, by increasing the acidic degree and increasing the penetration time, soil properties were changed, including the resistance characteristics and bearing capacity of the soil, which in turn, due to the amount of clay and different organic matter, caused more influence of acidic precipitation on soil permeability.
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