Evaluation of Water Infiltration Equations on Fadama Soils of Jos – North, Plateau State, Nigeria

Abstract

The main purpose of this study is to obtain water infiltration parameters of the Fadama Soils on the Jos Plateau. Estimation of water infiltration on a soil is a major constraint due to its variability depending on local soil characteristics. This could be used in simulating infiltration for the Fadama soils when designing agricultural projects. Field measurement of infiltration were made using the double ring infiltrometer at the three locations (Rizek, Kerker and Shen – du) on the Jos Plateau. Readings were taken at intervals of 5, 10, 15, 20, 25, 30, 35, 40, 45, 50, 55, 60 65,70, 75, 80, 85, 90, 95, 100,105,  110, 115 and 120minutes. A set of field measured cumulative infiltration depths were used for the estimation of the model parameters for the five models, while the other set was used in simulating the infiltration equations. At Rizek, Horton and NCRS model performed better (0.997) followed by Philip’s model (0.973) while Kostiakov and modified Kostiakov’s model have the least value of 0.923 each. Philip’s model has the best fit (1.00) followed by the NCRS’s model (0.999) at Kerker while the Kostiakov and modifiedKostiakov’smodel had 0.997 each and Horton with the least value (0.986). At Shen – du, Kostiakov and modified Kostiakov performed better (0.997), then, Horton with (0.986), NCRS has 0.993 with Philip’s model having the least value (0.991).The study indicate that Kostiakov, Philip, Horton, NCRS and Modified Kostiakov’s models were capable of simulating infiltration for the Fadama soils (Rizek, Kerker and Shen – du) on the Jos, Plateau.

Keywords: Infiltration Equations, Fadama Soils, Kostiakov Equation, Infiltartion Models