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缙云山典型林地根系分布对土壤土水特征和渗透性的影响

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森林土壤的土-水特征曲线和渗透系数是衡量土体非饱和特性中土壤持水能力和渗透能力的重要方式.为了了解不同林地根系表层土壤土水特征和渗透性,基于经典VG模型,通过土壤变水头渗透试验和离心机试验研究缙云山针阔混交林、常绿阔叶林、毛竹林和灌木林4种林地土土水特征和渗透性,同时建立土壤根系含量影响非饱和渗透系数的归一化数学模型.结果表明:1)毛竹林根系分布最多,且粗根比例较大,针阔混交林和常绿阔叶林各径级的根系分布范围均较广,但是每层数量较少;灌木林每层根系分布均数量较多,且细根分布范围最广;2)针阔混交林、常绿阔叶林、毛竹林和灌木林的表层饱和渗透系数 ks分别为7.00、7.04、0.69、3.70 μm/s,4种林地土壤的ks整体呈随深度增加而减小的趋势,毛竹林第一土层与此规律反常;3)4种林地土壤的进气参数值随土层深度整体呈现先增大后降低的趋势,孔径参数则基本随土层深度增大而减小;4)4种林地土壤的饱和渗透系数与根系数量均呈幂函数关系,R2≥0.959 76,考虑根系影响的林地土体非饱和渗透性函数可用归一化数学模型来描述和预测.研究结果可为含根土体水力特性及非饱和土渗流机理的研究提供理论基础.
Effects of root distribution on soil water characteristics and conductivity of typical forest land in Jinyun mountain
[Background]Soil-water characteristic curve and hydraulic conductivity of forest soil are important mathematical models,which play conversion roles in coupling analysis of water force coupling in porous media,but it is not deeply understood yet when the existence of plant roots was taken into account.[Methods]The soil water characteristics and hydraulic conductivity based on VG model of undisturbed soil for four stands(coniferous and broad-leaved mixed forest,evergreen broad-leaved forest,Phyllostachys pubescens forest,and shrub forest)were studied by centrifuge test and variable head permeability test.Meanwhile,the normalized mathematical model of unsaturated hydraulic conductivity versus soil root was established.[Results]1)P.pubescens forest has the most root amount especially in the aspect of coarse roots;the broad-leaved mixed forest has the widest distribution range of each diameter class,but the number of roots in each layer is not much,the number of roots in each layer of shrubbery is large,and the shrubbery has considerable.2)The saturated conductivities of four forests surface soil are 7.00 μm/s(coniferous and broad-leaved mixed forest),7.04 μm/s(evergreen broad-leaved forest),0.69 μm/s(P.pubescens forest)and 3.70 μm/s(shrub forest),respectively.And it is a decreasing tendency with soil depth,except for the second layer in P.pubescens forest.3)The air entry parameter of four forest stands increased firstly and then decreased with the soil depth,while the pore diameter parameter n decreased with the soil depth.The saturated conductivity of forest soil versus the number of roots can be regressed as power law function,R2 ≥0.959 76.[Conclusions]The saturated conductivity ks of soil in mixed coniferous and broad-leaved forests,evergreen broad-leaved forests,P.pubescens forests and shrub forests are closely related to the root distribution,and the saturated conductivity and root number are in the form of power function.The unsaturated conductivity of forest soil can be described and predicted by normalized model when plant roots are taken into account.

root-soil complexroot distribution characteristicsoil-water characteristic curveconductivity

祁子寒、王云琦、李通、李克文、闫相君、马磊、王太强、刘玉芳

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北京林业大学水土保持学院重庆三峡库区森林生态系统教育部野外科学观测研究站,100083,北京

北京林业大学水土保持学院重庆缙云山三峡库区森林生态系统国家定位观测研究站,100083,北京

自然资源部重庆典型矿区生态修复野外科学观测研究站(重庆地质矿产研究院),401120,重庆

重庆缙云山国家级自然保护区管理局,400700,重庆

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根-土复合体 根系分布特征 土-水特征曲线 渗透系数

国家自然科学基金

31971726

2024

中国水土保持科学
中国水土保持学会

中国水土保持科学

CSTPCD北大核心
影响因子:0.902
ISSN:1672-3007
年,卷(期):2024.22(4)