Abstract
Groundwater is a vital resource for human and environmental needs, and the periodic contamination poses a significant threat to groundwater resources. In this regard, to ensure its quality, the study of solute transport has gained significant attention in recent times. But accurate modeling is required to analyze the actual transport pattern of solute species. The present study focuses on multispecies solute transport through heterogeneous porous media, and a numerical approach to the decomposition method has been proposed. The governing equations of multispecies solute transport have been solved quantitatively using the implicit finite difference approach. An increasing exponential time-dependent dispersion describes the heterogeneity of porous media, and this dispersivity function has been further used to analyze the effect of time-dependent dispersion. The developed numerical model has been validated with the analytical solution, and this model evades the critical limitation of heterogeneity where the macrodispersion effect has been neglected. The study encompasses that the solute transport involves a series of first-order decay reactions, and migration of radionuclides and nitrification chain have been taken to carry out the analysis. Different decay rate constants have been used for the analysis to incorporate real field problems, and the results revealed that with the increase in decay rate constant, tailing is noticed in the solute concentration. Furthermore, the spatial moment analysis has been carried out on all species concentrations using these dispersivity functions, and the sensitivity analysis has been made using various breakthrough curves. The results of this analysis indicate that the variance and mean travel distance are susceptible to changes in dispersivity as a function of time and the transport pattern of its transformed species might not be the same. Thus, this study highlights the importance of considering the heterogeneities in the subsurface environment and can also inform the selection of monitoring strategies and remediation techniques for the contaminated sites, mainly where multiple species are involved in a chain reaction.
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Abbreviations
- \({C}_{i}\) :
-
Solute concentration of ith species [ML−3]
- \(D\) :
-
Hydrodynamic dispersion coefficient [L2T−1]
- \({D}_{\mathrm{inf}}\) :
-
Macrodispersion coefficient at the field scale [L2T−1]
- \({D}_{0}\) :
-
Sum of molecular diffusion and microdispersion [L2T−1]
- \(i\) :
-
Species index [ −]
- \({K}_{d,i}\) :
-
Distribution coefficient [L3/M]
- \(l\) :
-
Correlation length of hydraulic conductivity field or integral scale [L]
- \(L\) :
-
Domain length [L]
- \(M\) :
-
Zeroth spatial moment of solute concentration
- \(n\) :
-
Porosity of the porous media [ −]
- N :
-
Number of species [ −]
- \(R\) :
-
Retardation factor [ −]
- \(V\) :
-
Pore water velocity [LT−1]
- \({X}_{1}\) :
-
First spatial moment of solute concentration
- \({X}_{11}\) :
-
Second spatial moment of solute concentration
- \(Y\) :
-
Stoichiometric yield coefficient [ −]
- \(\alpha\) :
-
Dispersivity [L]
- \(\beta\) :
-
Rate of increase of dispersivity with time [T−1]
- \({\lambda }_{i}\) :
-
First-order reaction rates of ith species [T−1]
- \(\rho\) :
-
Bulk density of the porous medium [M/L3]
- \({\sigma }_{f}^{2}\) :
-
Variance of log hydraulic conductivity [–
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Key points of the research
1. A numerical solution is obtained for multispecies transport through heterogeneous porous media.
2. An exponential time-dependent dispersivity is considered to represent the heterogeneity of porous media.
3. Spatial moment analysis depicts the behavior of spreading of multispecies solute transport process in a comprehensive manner.
4. The variance and mean travel distance are susceptible to changes in dispersivity as a function of time, and the role of macrodispersion is significant in the migration of multispecies solute.
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Gupta, K.R., Sharma, P.K. Study on multispecies solute transport through heterogeneous porous media. Arab J Geosci 16, 452 (2023). https://doi.org/10.1007/s12517-023-11580-1
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DOI: https://doi.org/10.1007/s12517-023-11580-1