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A generally applicable pedotransfer function that estimates field capacity and permanent wilting point from soil texture and bulk density

机译:一种普遍适用的pedotransfer函数,可根据土壤质地和堆积密度估算田间持水量和永久枯萎点

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Pollacco, J. A. P. 2008. A generally applicable pedotransfer function that estimates field capacity and permanent wilting point from soil texture and bulk density. Can. J. Soil Sci. 88: 761-774. Hydrological models require the determination of fitting parameters that are tedious and time consuming to acquire. A rapid alternative method of estimating the fitting parameters is to use pedotransfer functions. This paper proposes a reliable method to estimate soil moisture at -33 and -1500 kPa from soil texture and bulk density. This method reduces the saturated moisture content by multiplying it with two nonlinear functions depending on sand and clay contents. The novel pedotransfer function has no restrictions on the range of 3 the texture predictors and gives reasonable predictions for soils with bulk density that varies from 0.25 to 2.16 g cm(-3). These pedotransfer functions require only five parameters for each pressure head. It is generally accepted that the introduction of organic matter as a predictor improves the Outcomes; however it was found by using a porosity based pedotransfer model, using organic matter as a predictor only modestly improves the accuracy. The model was developed employing 18 559 samples from the IGBP-DIS soil data set for pedotransfer function development (Data and Information System of the International Geosphere Biosphere Programme) database that embodies all major soils across the United States of America. The function is reliable and performs well for a wide range of soils occurring in very dry to very wet climates. Climatical grouping of the IGBP-DIS soils was proposed (aquic, tropical, cryic, aridic), but the results show that only tropical soils require specific grouping. Among many other different non-climatical soil groups tested, only humic and vitric soils were found to require specific grouping. The reliability of the pedotransfer function was further demonstrated with an independent database from Northern Italy having heterogeneous soils, and was found to be comparable or better than the accuracy of other pedotransfer functions found in the literature.
机译:Pollacco,J. A. P.2008。一种普遍适用的pedotransfer函数,可根据土壤质地和堆积密度估算田间持水量和永久枯萎点。能够。 J.土壤科学。 88:761-774。水文模型需要确定拟合参数,而获取这些参数既繁琐又费时。估计拟合参数的一种快速替代方法是使用pedotransfer函数。本文提出了一种可靠的方法,可以根据土壤质地和堆积密度估算-33和-1500 kPa的土壤湿度。该方法通过将饱和水分含量乘以两个取决于沙子和粘土含量的非线性函数来降低饱和水分含量。新颖的pedotransfer函数对3个纹理预测因子的范围没有限制,并为堆积密度在0.25到2.16 g cm(-3)之间变化的土壤提供了合理的预测。这些pedotransfer功能每个压力头仅需要五个参数。人们普遍认为,引入有机物作为预测指标可以改善结果;但是,通过使用基于孔隙率的pedotransfer模型发现,仅将有机物用作预测因子会适度地提高准确性。该模型是使用IGBP-DIS土壤数据集的18 559个样本开发的,用于开发pedotransfer函数(国际地圈生物圈计划的数据和信息系统)数据库,该数据库包含了美国的所有主要土壤。该功能是可靠的,并且对于在非常干燥到非常潮湿的气候条件下发生的多种土壤都表现良好。提出了IGBP-DIS土壤的气候分组(潮,热带,冰冻,干旱),但结果表明,只有热带土壤需要特定的分组。在测试的许多其他不同的非气候土壤组中,仅腐殖土和玻璃土被发现需要特定的分组。 pedotransfer函数的可靠性进一步得到了来自意大利北部具有异质土壤的独立数据库的证实,并且发现其可比性或优于文献中发现的其他pedotransfer函数的准确性。

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