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首页> 外文期刊>Pedosphere: A Quarterly Journal of Soil Science >Evaluation of Pedotransfer Functions for Estimating Soil Water Retention Curve of Saline and Saline-Alkali Soils of Iran
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Evaluation of Pedotransfer Functions for Estimating Soil Water Retention Curve of Saline and Saline-Alkali Soils of Iran

机译:评估伊朗盐碱土和盐碱土土壤水分保持曲线的Pedotransfer函数评估

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摘要

Soil water retention data are essential for irrigation scheduling and determination of irrigation frequency. However, direct measurement of this characteristic is time consuming and expensive and furthermore its spatial and temporal variabilities in field scales increase the number of measurements. Different pedotransfer functions, such as Saxton et al., Campbell, Vereecken at al., Rawls and Brakensiek, Wosten et al., Rajkai et al., Ghorbani Dashtaki and Homaee, Zacharias and Wessolek, and Rosetta, were evaluated to estimate soil water retention of saline and saline-alkali soils collected from south of Tehran, Iran. The saturation-extract conductivity of all the 68 samples and exchangeable sodium percentage of more than half of them were measured to be greater than 4 dS m(-1) and 15%, respectively. The calculated Akaike's information criterion values showed that Saxton at al. and Campbell models were the best in estimation of soil water retention curve and total available water, respectively.
机译:土壤保水数据对于灌溉计划和确定灌溉频率至关重要。然而,直接测量该特性是耗时且昂贵的,此外,其在田间尺度上的时空变化增加了测量的数量。评估了不同的pedotransfer函数,例如Saxton等人,Campbell,Vereecken等人,Rawls和Brakensiek,Wosten等人,Rajkai等人,Ghorbani Dashtaki和Homaee,Zacharias和Wessolek和Rosetta,以评估土壤水分保留从伊朗德黑兰南部收集的盐渍土和盐碱土。所有68个样品的饱和萃取电导率和其中一半以上的可交换钠含量分别被测量为大于4 dS m(-1)和15%。计算出的赤池信息标准值表明,萨克森等人。坎贝尔模型和坎贝尔模型分别在估计土壤保水曲线和总可用水量方面最好。

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