Journal of Tianjin Agricultural University ›› 2023, Vol. 30 ›› Issue (2): 11-17.doi: 10.19640/j.cnki.jtau.2023.02.003

• Researches and Scientific Notes • Previous Articles     Next Articles

Experimental and simulation study on soil infiltration characteristics under varying initial moisture contents

Dou Jingjing, Zheng ZhiweiCorresponding Author, Gao Zhuozhuo   

  1. College of Water Conservancy Engineering, Tianjin Agricultural University, Tianjin 300392, China
  • Received:2021-09-17 Online:2023-04-30 Published:2023-06-28

Abstract: To study the influence of initial moisture content on soil infiltration characteristics, five different treatments were set up(the corresponding initial moisture contents were 1.5%, 7.5%, 13.5%, 19.5%, and 25.5%), and indoor soil column experiments were conducted. The infiltration time of each soil column and the amount of water injected every time were recorded. The planning-solving tools were used to determine the parameters of the Kostiakov-Lewis model, Horton model and Philip model. The results showed that: ① When the initial moisture content was constant, the cumulative infiltration volume gradually increased with time, and the infiltration rate gradually decreased. The initial moisture content had a significant effect on the fluctuation of the infiltration rate. ② When the initial moisture content was less than 19.5%, the applicability of the three models was good, whose correlation coefficients of the measured and simulated values were all above 0.99. When the initial moisture content was more than 19.5%, the applicability of the Kostiakov-Lewis model and the Philip model was good, but the Horton model was not so good as them. ③ In the Kostiakov-Lewis model, the fluctuation of infiltration coefficient k with different initial moisture contents was maximal, the stable permeability f0 was minimum, and infiltration index a was between them. In the Horton model, the fluctuation of the initial infiltration rate i0 with different initial moisture contents was the most obvious, the stable infiltration rate ic was the least significant, and the parameter β was between them. In the Philip model, the fluctuation of the soil absorption rate S with different initial moisture contents was bigger, and the stable infiltration rate A was smaller.

Key words: initial moisture content, infiltration characteristics, Kostiakov-Lewis model, Horton model, Philip model

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