scholarly journals Modelling of Water Flow and Nitrate Dynamics Through Partially Saturated Porous Media in Laboratory Condition using Hydrus-2D

2018 ◽  
Vol 5 (2) ◽  
pp. 107-113 ◽  
Author(s):  
Jahangeer . ◽  
P.K. Gupta ◽  
B. Yadav

Due to the reducing availability of water resources and the growing competition for water between residential, industrial, and agricultural users, increasing irrigation efficiency, by several methods like drip irrigation, is a demanding concern for agricultural experts. The understanding of the water and contaminants flow through the subsurface is needed for the sustainable irrigation water management, pollution assessment, remediation, and groundwater recharge. In this study, the Windows-based computer software package HYDRUS-2D, which numerically simulates water and solute movement in two-dimensional, variably-saturated porous media, was used to evaluate the distribution of water and Nitrate in the sand tank. The laboratory and simulation experiments were conducted to evaluate the role of drainage, recharge flux, and infiltration on subsurface flow condition and subsequently, on nitrate movement in the subsurface. The water flow in the unsaturated zone was model by Richards’ equation, which was highly nonlinear and its parameters were largely dependent on the moisture content and pressure head of the partially saturated zone. Following different cases to be considered to evaluate- a) applying drainage and recharge flux to study domains, b) transient infiltration in a vertical soil column and c) subsequently, nitrate movement in a 2D sand tank setup. A single porosity model was used for the simulation water and nitrate flow in the study domain. The results indicate the transient water table position decreases as the time increase significantly by applying drainage flux at the bottom. Similarly, the water table positions in study domains increasing in the domain by applying recharge flux. Likewise, the water flow profile shows the decreasing water table elevation with increasing water content in the vertical domain. Furthermore, the nitrate transport dynamics was dominated by advective flux and highly affected by the recharge flux in the vertical direction. The findings of the study help to enhance the understanding of the sustainable soil-water resources management and agricultural practices.

Author(s):  
Nguyen Van Nghia A. ◽  
Damien Jougnot ◽  
Luong Duy Thanh ◽  
Phan Van Do ◽  
Tran Thi Chung Thuy ◽  
...  

2021 ◽  
Vol MA2021-01 (27) ◽  
pp. 961-961
Author(s):  
Marc Secanell ◽  
Seongyeop Jung ◽  
Alexandre Jarauta-Arabi ◽  
Fei Wei ◽  
Mayank Sabharwal ◽  
...  

Author(s):  
Yoram Rubin

Many of the principles guiding stochastic analysis of flow and transport processes in the vadose zone are those which we also employ in the saturated zone, and which we have explored in earlier chapters. However, there are important considerations and simplifications to be made, given the nature of the flow and of the governing equations, which we explore here and in chapter 12. The governing equation for water flow in variably saturated porous media at the smallest scale where Darcy’s law is applicable (i.e., no need for upscaling of parameters) is Richards’ equation (cf. Yeh, 1998)


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