首页|雨滴击溅下表土孔隙变化及其对入渗能力的影响

雨滴击溅下表土孔隙变化及其对入渗能力的影响

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为探究雨滴击溅下土壤结构与入渗能力的变化规律,为雨滴击溅下土壤侵蚀状况预测提供参考,以黄土高原褐土为对象,基于雨滴击溅试验、土壤渗透试验和同步辐射CT扫描方法,对降雨条件下表土孔隙结构与土壤渗透能力的关系进行了分析。结果表明:①雨滴击溅导致土壤总孔隙度和渗透系数显著降低(P<0。05)。2。67、3。39 和 4。05 mm直径雨滴击溅后土壤的总孔隙度分别降低了20。64%、36。05%和44。88%,土壤渗透系数分别降低了15。69%、40。42%和71。77%。雨滴击溅后土壤孔隙的碎片化程度加剧,导致孔隙形状更不规则,连通性降低。②土壤孔隙大小、形状和连通性对土壤渗透能力有显著影响(P<0。01):孔隙越大,形状越规则,对土壤渗透能力的影响越大。从孔隙连通性角度看,土壤连通孔隙的孔喉半径和孔隙率对入渗能力的影响程度最大。基于以上分析,建立了土壤渗透系数(K)与总孔隙度(PT)、大孔隙率(Plp)、规则孔隙率(Prp)、连通孔隙率(Pcp)和孔喉半径(Rth)的预测模型:K=0。402PT+0。104Plp+0。1401Prp+0。350Pcp+0。003Rth-0。415,R2=0。93,P<0。05。综上可见,雨滴击溅通过改变土壤孔隙的大小、形状和连通状况,导致土壤孔隙结构破坏,从而降低了土壤入渗能力。
Topsoil Pore Change Under Raindrop Splashing and Its Effect on Soil Infiltration
To explore the changes in topsoil structure and infiltration capacity under raindrop splashing and provide reference for predicting soil erosion conditions under raindrop splashing,this study explored the relationship between topsoil pore structure and permeability under rainfall conditions by using the raindrop splash experiment,soil infiltration experiment and synchrotron radiation CT scanning technology.The results showed that:1)Raindrop splashing significantly reduced topsoil total porosity and permeability coefficient(P<0.05).The total porosity decreased by 20.64%,36.05%and 44.88%,respectively,and permeability coefficient decreased by 15.69%,40.42%and 71.77%,respectively,after the splashing of raindrops with diameters of 2.67,3.39 and 4.05 mm.The fragmentation level of pores intensified after raindrop impact,leading to a more irregular pore shape and connectivity reduction.2)The size,shape and connectivity of pores had significant effects on permeability(P<0.01),the larger the pores and the more regular the shape,the greater the impact on permeability.From the perspective of pore connectivity,the radius of connected pore throats and the porosity had the greatest impact on infiltration capacity.On this basis,a predictive model was established for permeability coefficient(K)in relation to the total porosity(PT),macroporosity rate(Plp),regular porosity rate(Prp),connected porosity rate(Pcp),and pore throat radius(Rth):K=0.402PT+0.104Plp+0.1401Prp+0.350Pcp+0.003Rth-0.415,R2=0.93,P<0.05.In conclusion,raindrop splashing alters the size,shape and connectivity of pores,leading to the disruption of pore structure and a decrease in infiltration capacity.

Raindrop splashPore microstructurePore network modelSoil infiltrationTopsoil

张晓茹、刘志强、焦钒栩、李光录

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西北农林科技大学资源环境学院,陕西杨凌 712100

西北农林科技大学水土保持研究所,陕西杨凌 712100

雨滴击溅 孔隙微观结构 孔隙网络模型 土壤渗透 表土

国家自然科学基金项目

41571262

2024

土壤
中国科学院南京土壤研究所

土壤

CSTPCD北大核心
影响因子:1.052
ISSN:0253-9829
年,卷(期):2024.56(3)