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预测生物炭添加对土壤饱和水力传导度的影响OA

Predicting the Effect of Biochar Addition on Soil Saturated Hydraulic Conductivity

中文摘要英文摘要

生物炭作为土壤改良剂,其施用对土壤饱和水力传导度的影响受施炭量、施炭类型、土壤质地等多因素制约,作用机制尚不明确.通过田间实验与三维模型模拟相结合,探究了稻杆炭与竹炭在不同添加量(3%,6%)下对屈家岭试验田土壤(粉壤土)饱和水力传导度的改良效果.田间实验结果表明,3%稻杆炭和6%竹炭处理提升了0~20 cm土层的土壤饱和水力传导度,而6%稻杆炭和3%竹炭则产生抑制作用.为揭示其内在机理,基于Blender构建了土炭混合体的三维孔隙结构模型,计算土炭混合物孔隙度,并结合Terzaghi模型和Chapuis模型预测了土壤水力传导度.对比发现,Terzaghi模型预测更接近实测值,而Chapuis模型则系统性偏低.模型复现了稻杆炭处理的实验趋势,证实适量稻杆炭通过优化孔隙连通性改善土壤饱和水力传导度;但两个模型对竹炭的预测存在一定偏差,这主要是模型并未考虑竹炭内部孔隙.

As a soil amendment,the effect of biochar application on soil saturated hydraulic conductivity is governed by multiple factors,such as application rate,biochar type,and soil texture,and the underlying mechanism remains poorly understood.This study combined field experiments with three-dimensional modeling to investigate the improvement effects of rice straw biochar and bamboo biochar at different addition rates(3%,6%)on the saturated hydraulic conductivity of silt loam soil in the Qujialing experimental field.Field results indicate that 3%rice straw charcoal and 6%bamboo charcoal treatments enhanced saturated hydraulic conductivity in the 0~20 cm soil layer,while 6%rice straw charcoal and 3%bamboo charcoal produced inhibitory effects.To elucidate the underlying mechanisms,a 3D pore structure model of the soil-biochar mixture was constructed using Blender software to calculate the mixture porosity.Subsequently,the Terzaghi and Chapuis models were applied to predict the soil hydraulic conductivity.Comparisons revealed that the Terzaghi model more closely approximated measured values,while the Chapuis model systematically underestimated them.Both models reproduced the experimental trends observed with rice straw charcoal treatment,confirming that moderate amounts of rice straw charcoal improve saturated hydraulic conductivity by optimizing pore connectivity.However,both models exhibited certain deviations in predicting bamboo charcoal effects,primarily due to their failure to account for internal bamboo charcoal porosity.

江振;谢华;黄爽;刘迪;郑文慧;孟卓文

武汉大学水利水电学院,湖北 武汉 430072武汉大学水利水电学院,湖北 武汉 430072武汉大学水利水电学院,湖北 武汉 430072武汉大学水利水电学院,湖北 武汉 430072武汉大学水利水电学院,湖北 武汉 430072武汉大学水利水电学院,湖北 武汉 430072

农业科技

生物炭饱和水力传导度田间实验孔隙度模型土壤改良

biocharsaturated hydraulic conductivityfield experimentporosity modelsoil amendment

《节水灌溉》 2026 (8)

73-79,7

国家自然科学基金项目(52509068)国家自然科学基金项目(52179040).

10.12396/jsgg.2025502

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