长江上游低山丘陵区土壤水分特征曲线传递函数研究  

Pedo-transfer Function for Estimating Hydraulic Properties of Soils in Hilly Areas in the Upper Reach of the Yangtze River

作　　者：孙志祥 邓建波 吕玉娟[1,2] 崔俊芳 唐翔宇 SUN Zhixiang;DENG Jianbo;LYU Yujuan;CUI Junfang;TANG Xiangyu(Institute of Mountain Hazards and Environment,Chinese Academy of Sciences,Chengdu 610041,China;University of Chinese Academy of Sciences,Beijnig 100049,China;College of Water Resources and Hydropower,Sichuan Agricultural University,Ya’an 625000,China)

机构地区：[1]中国科学院水利部成都山地灾害与环境研究所,成都610041 [2]中国科学院大学,北京100049 [3]四川农业大学水利水电学院,四川雅安625000

出　　处：《灌溉排水学报》2022年第6期97-104,共8页Journal of Irrigation and Drainage

基　　金：中国科学院战略性先导科技专项(A类)(XDA23090202);国家自然科学基金重大项目课题(41790431);青藏科考重大山洪专题(2019QZKK0903)。

摘　　要：【目的】土壤水分特征曲线是定量研究土壤水分运动和溶质迁移的重要参数,为估算长江上游低山丘陵区土壤水力学参数提供实用的函数工具。【方法】以长江上游低山丘陵区盐亭万安小流域为研究区,测定3种不同土地利用类型(水田、旱地、林地)土壤水分特征曲线与土壤基本理化性质,在van Genuchten(1980)模型参数拟合及Pearson相关分析的基础上,运用多元逐步线性回归分析法,分别建立模型参数θ_(r)、θ_(s)、α和n的土壤传递函数,并进行准确度评估与分析。【结果】①研究区不同土地利用方式下土壤持水量的大小顺序为:水田>旱地>林地,但土壤供水能力差异不明显;②采用本研究建立的传递函数所得的土壤水分特征曲线估算与实测值对3种不同土地利用类型土壤的决定系数(R^(2))均高于0.97,旱地的估算效果最佳;③与4种常用传递函数(Vereecken(1989)、Wösten(1999)、Weynants(2009)和Schaap(2001))相比,采用本研究构建的土壤传递函数的估算准确度最高。【结论】本文构建的土壤传递函数可用作该地区土壤水分特征曲线模型参数估算的实用工具。【Objective】Soil water retention curve(SWRC)is an important parameter for studying subsurface hydrological processes and solute transport in soils,but its direct measurement is labor-intensive.For large scale applications,it is often estimated indirectly using some easy-to-measure soil properties.In this paper,we propose a pedo-transfer function to estimate hydraulic parameters of the soils in hilly regions in the upper reach of the Yangtze River.【Method】Soil samples were taken from three land usages in the Yanting Wan’as watershed:paddy field,upland and forest.We measured their SWRC and other chemical and physical properties;the measured SWRC was fitted to the van Genuchten formula,from which we derived a pedo-transfer function to estimate the van Genuchten parameters using multiple stepwise linear regression analysis.Accuracy of the function was evaluated using the Pearson correlation analysis.【Result】①Land use affects the ability of the soil to hold water.The land usage that affected water-holding capacity of the soil more was ranked in the order of paddy field>upland>forest land.In contrast,no significance was found in soil water supply capacity between different land usages.②The coefficient of determination between the measured and predicted SWRC using the pedo-transfer function was greater than 0.97,and the proposed model was most accurate for soils taken from the upland.③The proposed pedo-transfer function was more accurate than those proposed by Vereecken et al(1989),Wosten et al(1999),Weynants et al(2009)and Schaap et al(2001).【Conclusion】The pedo-transfer function proposed in this paper for estimating water release curve using easy-to-measure soil properties is accurate and efficient.It can be used to estimate hydraulic parameters of the soils in the hilly regions in the upper reach of the Yangtze River.

关 键 词：土壤水分特征曲线 van Genuchten模型 土壤传递函数 

分 类 号：X143[环境科学与工程—环境科学] P951[天文地球—自然地理学]