Estimation of Infiltration Models’ Parameters Using Regression Analysis in Irrigation Fields of Northern Ghana

A. Salifu, F. K. Abagale, G. Kranjac-Berisavljevic
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引用次数: 3

Abstract

The quantification of soil infiltration is necessary for the estimation of water accessibility in soils for plant growth and development. Field infiltration tests runs were conducted on agricultural soils in three irrigation sites of Northern Ghana. The field data were fitted into Green and Ampt, Kostiakov, Philip, Holtan, Soil Conservation Service and Horton infiltration models for the determination of the unknown model parameters. Regression analysis at 95% confidence level using GraphPad Prism 8. Laboratory and field data on infiltration were used for the model fitting and the unknown parameters were determined using the calibrated models. The k and n parameters of Kostiakov model at Bontanga study site were found to be k = 28.0027 and n = 0.5902, k = 17.0294 and n = 0.4504 for Golinga and k = 23.0356 and n = 0.6339 for Libga. For all the models, the coefficient of determination ranged from 0.7612 to 0.9876 indicating strong relationships. Only Holtan model gave different values at all the three study sites. The parameter GIa and ic of the Holtan model drawn from hydrologic soil group were the same at all the study sites because of the same vegetative cover and surface conditions. The study observed the values of the parameters to have influenced the models’ performance.
加纳北部灌区入渗模型参数的回归分析
土壤渗透的量化对于估计植物生长和发育所需的土壤水分可及性是必要的。对加纳北部三个灌溉点的农业土壤进行了田间渗透试验。将现场数据拟合到Green和Ampt、Kostiakov、Philip、Holtan、土壤保护局和Horton渗透模型中,以确定未知的模型参数。使用GraphPad Prism 8在95%置信水平下进行回归分析。使用实验室和现场的渗透数据进行模型拟合,并使用校准模型确定未知参数。Bontanga研究地点的Kostiakov模型的k和n参数为:Golinga的k=28.027和n=0.5902,k=17.0294和n=0.4504,Libga的k=23.0356和n=0.6339。对于所有的模型,决定系数在0.7612到0.9876之间,表明有很强的相关性。只有Holtan模型在所有三个研究地点给出了不同的值。由于植被覆盖和地表条件相同,从水文土壤组中提取的Holtan模型的参数GIa和ic在所有研究地点都是相同的。该研究观察到了影响模型性能的参数值。
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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