首页|黄土高原梯田土壤饱和导水率长期变化及其影响因素

黄土高原梯田土壤饱和导水率长期变化及其影响因素

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[目的]探究黄土高原梯田土壤饱和导水率(Ks)的长期变化及其主控因素。[方法]选取农田、果园及草地3种土地利用类型的梯田,以坡面为对照,采集坡面及修筑年限为7,20,30,40年梯田的土壤样品,测定Ks及土壤理化性质。使用Kruskal-Wallis H检验、Spearman相关性分析、偏最小二乘路径模型(PLS-PM)分析修筑梯田对Ks的影响、Ks随时间的变化及其影响因素。[结果](1)不同利用类型梯田Ks随修筑年限增加表现出不同的规律。7,20,30,40年农田Ks持续增长,从0。18 mm/min增加至0。28 mm/min,增长率为55。56%。果园Ks先增加,30年后出现下降趋势,其中30年果园Ks显著高于7年果园Ks,从0。12 mm/min增加至0。35 mm/min,增长率为191。67%。草地Ks先增加,20年后则保持相对稳定,其中20年草地Ks显著高于7年草地Ks,从0。14 mm/min增加至0。31 mm/min,增长率为121。43%。(2)影响K,的主要因素为土壤粒径分布、土壤质量密度、团聚体平均重量直径,其路径系数分别为-0。431,-0。561,0。226。[结论]梯田利用类型对土壤性质影响程度的差异导致梯田Ks随修筑年限的增加呈现不同规律,研究结果可为梯田后续管理及发展高效旱作农业提供依据。
The Long-term Variations and Influencing Factors of Soil Saturated Hydraulic Conductivity in Terraces on the Loess Plateau
[Objective]The long-term variations of soil saturated hydraulic conductivity(Ks)and its primary controlling factors in terraces on the Loess Plateau were explored.[Methods]Terraces were selected for three land use types,i.e.farmland,orchard,and grassland,with slope designated as the control.Soil samples were collected from slopes and terraces with construction ages of 7,20,30 and 40 years to determine the Ks and soil physicochemical properties.The Kruskal-Wallis H test,Spearman correlation analysis,and partial least squares path model(PLS-PM)were conducted to examine the impact of terrace construction on Ks and its temporal variations,as well as the influencing factors.[Results](1)The K,of terraces under different land use types exhibited varying patterns with increasing ages of terrace construction.The Ks of farmland increased continuously with construction age of 7,20,30 and 40 years,increasing from 0.18 mm/min to 0.28 mm/min,with a growth rate of 55.56%.The Ks of orchard increased with the increase of construction years firstly,then showed a decreasing trend after 30 years,and the Ks of orchard with a construction age of 30 years was significantly higher than that of orchard with a construction age of 7 years,increasing from 0.12 mm/min to 0.35 mm/min,with a growth rate of 191.67%.The Ks of grassland increased with the increase of construction years firstly,then remained relatively stable after 20 years,and the Ks of grassland with a construction age of 20 years was significantly higher than that of grassland with a construction age of 7 years,increasing from 0.14 mm/min to 0.31 mm/min,with a growth rate of 121.43%.(2)The primary factors influencing Ks included soil particle size distribution,soil bulk density,and mean weight diameter of aggregates,with the path coefficients being-0.431,-0.561 and 0.226,respectively.[Conclusion]The variation in the impact of terrace land use types on soil properties resulted in varying patterns of Ks with increasing ages of terrace construction.The results can provide a basis for the subsequent management of terraces and the development of efficient dryland farming.

soil saturated hydraulic conductivityterracethe Loess Plateauland use

彭心、倪玲珊、纪柯言、戴伟、王卓霄、常恒、方怒放

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西北农林科技大学水土保持科学与工程学院,陕西杨凌 712100

中国科学院水利部水土保持研究所,黄土高原土壤侵蚀与旱地农业国家重点实验室,陕西杨凌 712100

西北农林科技大学水利与建筑工程学院,陕西杨凌 712100

土壤饱和导水率 梯田 黄土高原 土地利用

2024

水土保持学报
中国土壤学会 中国科学院水利部水土保持研究所

水土保持学报

CSTPCD北大核心
影响因子:1.226
ISSN:1009-2242
年,卷(期):2024.38(6)