土壤水分特征曲线传递函数的研究进展
review of development in pedo-transfer functions about soil water characteristics curves
利用一些容易获取的土壤理化参数(如:颗粒组成、干容重组、有机质等)可以估算土壤的水力性质(土壤水分特征曲线、土壤导水系数),这些方法统称为土壤传递函数(Pedo-Transfer Functions, PTFs)。该文概述了国内外土壤水分特征曲线传递函数建立的方法、理论以及应用,根据其建立的理论基础以及基本假设将土壤水分特征曲线传递函数分为:统计模型、物理-经验模型、分形机理模型模型等。并对不同传递函数的优缺点作出评价,提出土壤水分特征曲线传递函数方法的不足之处,指出了今后的发展方向,并展望了土壤水分特征曲线传递函数的发展前景。
Use some easily available soil physical and chemical parameters (such as: particle composition, bulk density, organic matter, etc.) can be estimated hydraulic properties of soil (soil water characteristic curves and soil hydraulic conductivity), these methods are collectively referred to as soil Pedo-transfer function(PTFs).This paper provides as a review of the construct methods , theory and application of PTFs about the soil water characteristic curves. According to the theoretical background and the basic assumption, indirect methods may be classified into three categories, statistical models, physico-empirical method and fractal method. It also analyzed advantages and disadvantages of various PTFs, pointed out shortages of the PTFs, predicted directions of future development and foretold prospects of PTFs about the soil water characteristic curves.
姚姣转、刘小燕、段利民、刘廷玺
水利工程基础科学环境科学基础理论
土壤水分特征曲线土壤传递函数优缺点前景
soil water characteristic curves pedo-transfer functions advantages and disadvantages prospects
姚姣转,刘小燕,段利民,刘廷玺.土壤水分特征曲线传递函数的研究进展[EB/OL].(2014-11-07)[2025-08-02].http://www.paper.edu.cn/releasepaper/content/201411-125.点此复制
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