Extension of the Gardner exponential equation to represent the hydraulic conductivity curve: Inclusion of macropore flow effects

IF 3.1 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Theophilo Benedicto Ottoni Filho , Anderson Rodrigues Caetano , Marta Vasconcelos Ottoni
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Abstract

In soil hydraulics, it is crucial to establish an accurate representation of the relative hydraulic conductive curve (rHCC), K_r(h). This paper proposes a simple way to determine K_r(h), called the Modified Gardner Dual model (MGD), using a logarithmic extension of the classical Gardner exponential representation and including macropore flow effects. MGD has five parameters which are hydraulic constants clearly identified in the bilogarithmic representation of K_r(h). Two of them are related to the main inflection point coordinates of rHCC; from them, it is possible to determine the macroscopic capillary length of the infiltration theory. The model was tested in the suction interval 0 < h < 15,000 cm with a total of 249 soil samples from two databases, and employing a flexible representation of the Mualem-van Genuchten (MVG) equation as a reference. Using the RMSE statistics (with log base) to measure the fitting errors, we obtained a 31% reduction in errors (RMSE_MGD = 0.27, RMSE_MVG = 0.39). In 74% of the soils, including samples from the two databases, the reduction was 53% (RMSE_MGD = 0.19, RMSE_MVG = 0.40); the rHCC data fitting of this group was accurate over all the suction h intervals, with RMSE_MGD < 0.32 in each soil sample. In the remaining 26% of the samples, the quality of the MGD fitting degraded due mainly to the presence of multiple rHCC data inflection points. Therefore, in soils without this structural peculiarity, the proposed model revealed to be quite accurate in addition to being analytically simple. Another advantage of MGD is that its parameters depend mainly on the data with h around and lower than the main inflection suction value, which, in turn, never exceeded the 300-cm limit in this study. Hence, in soils that do not have multiple inflections, the extrapolations of the model in drier intervals (1000 cm < h < 15,000 cm) are reliable. The MGD parameter optimization software has been called KUNSAT. It is available in the Supplementary Material or from the corresponding author on request.

Gardner指数方程用于表示导水率曲线的扩展:包含大孔隙流动效应
在土壤水力学中,建立相对水力传导曲线(rHCC) K_r(h)的精确表示是至关重要的。本文提出了一种简单的方法来确定K_r(h),称为修正加德纳双模型(MGD),使用经典加德纳指数表示的对数扩展,并包括大孔流动效应。MGD有5个参数,它们是在K_r(h)的双对数表示中明确确定的水力常数。其中两个与rHCC的主拐点坐标有关;由此可以确定渗透理论的宏观毛细长度。在吸力区间0 <下对模型进行了试验;h & lt;从两个数据库中选取249个土壤样本,并采用Mualem-van Genuchten (MVG)方程的灵活表示作为参考。使用RMSE统计量(log base)来测量拟合误差,我们获得了31%的误差减少(RMSE_MGD = 0.27, RMSE_MVG = 0.39)。在74%的土壤中,包括来自两个数据库的样本,减少了53% (RMSE_MGD = 0.19, RMSE_MVG = 0.40);本组rHCC数据在所有吸痰h区间拟合准确,RMSE_MGD <每个土壤样品0.32。在其余26%的样本中,由于存在多个rHCC数据拐点,MGD拟合的质量下降。因此,在没有这种结构特性的土壤中,所提出的模型除了解析简单外,还显示出相当准确。MGD的另一个优点是其参数主要依赖于h左右且小于主弯吸力值的数据,而在本研究中,主弯吸力值从未超过300 cm的限制。因此,在没有多重折弯的土壤中,模型在干燥间隔(1000 cm <h & lt;15,000 cm)是可靠的。MGD参数优化软件被称为KUNSAT。它可以在补充材料中获得,也可以根据要求从通讯作者处获得。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Journal of Hydrology X
Journal of Hydrology X Environmental Science-Water Science and Technology
CiteScore
7.00
自引率
2.50%
发文量
20
审稿时长
25 weeks
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